TIMEEVENT DESCRIPTIONLOCATIONIMAGES

UNIVERSE
1,000,000,000,000 YBN
1) We are a tiny part of a universe
made of an infinite amount of space,
matter and time.




  
995,000,000,000 YBN
11) There is no time I can identify as
the start of the universe, the universe
has no beginning and no end; perhaps
the same photons that have always been
in the universe continue to move in the
space that has always been.




  
990,000,000,000 YBN
2) There is more space than matter.



  
980,000,000,000 YBN
3) All of the matter is made of
particles of light humans have named
"photons". Photons are the base unit
of all matter from the tiniest
particles to the largest galaxies.


  
960,000,000,001 YBN
5) Photons generally move 300 million
meters every second in a line, but as
pieces of matter, can be slightly
slowed from the force of gravity, and
stop for an instant when they collide.

Photons
move 300 million meters every second in
a line but as pieces of matter their
velocity changes slightly because of
gravity, and theoretically photons
bounce off each other, at which time
they come to a complete stop relative
to the rest of the universe for an
instant before bouncing and
accelerating away from each other in
the opposite direction.

  
950,000,000,000 YBN
6) Matter is attracted to other matter
and so photons form structures such as
protons, atoms, molecules, molecule
groups (like all of life of earth),
planets, stars, galaxies, and clusters
of galaxies.

Gravity is responsible for photons
forming Hydrogen, Hydrogen forming
nebulas, nebulas forming stars, and
stars forming galaxies.



  
940,000,000,000 YBN
7) All of the hundreds of billions of
galaxies we can see are only a tiny
part of the universe. Most of the
galaxies in the universe we will never
see because they are too far away for
even 1 particle of light from them to
be going in the exact direction of our
tiny location, or are captured by atoms
between here and there.

One estimate
has 70e21 (sextillion) stars in only
the universe we can see. That is 10
times more stars than grains of sand on
all the earth.



  
935,000,000,000 YBN
4) The patterns in the universe are
clear. Photons form gas clouds of
Hydrogen and Helium, these gas clouds,
called nebuli condense to form galaxies
of stars. The stars emit photons back
out into the rest of the universe,
where they collect and form clouds
again. Around each star are many
planets and pieces of matter. On many
of those planets intelligent life
evolves. This life moves their stars
out of spiral galaxies to form globular
clusters, and ultimately to transform
spiral galaxies into elliptical
galaxies that travel the universe
looking for more matter to fuel their
movement.
It may very well be that stars at this
scale are photons, spiral galaxies
charged particles, globular galaxies
neutral particles, and galactic
clusters atoms at a much larger scale
in an infinite macro and micro scale.


  
930,000,000,000 YBN
8) That the frequency of photons from
the most distant galaxies we can see
have a lower frequency may be due to
the effects of gravitation and/or
particle collision in the large
distance between source and observer.

  
880,000,000,000 YBN
13) The Milky Way Galaxy forms, perhaps
from a gas cloud that formed by
capturing matter in the form of light
from other stars, from the remains of a
previously destroyed galaxy, or some
combination of the two.




  
5,500,000,000 YBN
16) The yellow star earth will
eventually orbit forms, perhaps in a
nebula, when matter in the nebula
starts accumulating and rotating as a
result of gravity, or from the remains
of an exploded star that condensed
again under the influence of gravity.

My
opinion is that stars contain molten
iron in their center, similar to the
earth. {check with supernova remnants}
The density of the star the earth
rotates is similar to that of a liquid.
The most popular theory to explain how
stars give off so many photons is that
these photons exit as a result of
Hydrogen atomically fusing into Helium,
and I want to add my opinion that
potentially the pressure of gravity
simply separates atoms of Hydrogen and
helium into their source photons.
Perhaps the reaction is similar to the
center of the earth where red hot
liquid iron emits photons. We
obviously do not explain that red hot
molten metal as being the result of
nuclear fusion, but yet it is clearly
not oxygen combustion. Clearly there
are many photons exiting stars every
second, and each star is losing large
amounts of matter in the form of
photons. In addition, the most popular
theory explains that most atoms heavier
than Hydrogen and no heavier than Iron
are made in stars, and atoms larger
than iron can only be made in
supernovae.

  
5,000,000,000 YBN
22) Heavier atoms in the star system
move closer to the center and lighter
atoms are sent farther out.




  
4,600,000,000 YBN
17) Planets form around star.
Terrestrial planets are red hot, have
surface of melted rock, all lighter
atoms float to the surface of the
molten planets. All the H2O from the
first earth oceans and lakes is in the
atmosphere in gas form.




  
4,600,000,000 YBN
30) Moon of earth is formed by 1 of 3
ways:
1) spherical planet collides with
earth, moon forms from remaining matter
in ring around earth.
2) spherical planet is
caught in earth orbit
3) moon of earth forms
naturally from original matter of star
system in orbit around earth.

The Moon
orbiting 5 degrees from the axis of the
Earth's orbit implies that the Moon was
captured, although 5% is not a
particularly large difference from the
plane of the Earth's rotation. That the
Moon orbits in the same direction as
the Earth is evidence in favor of the
Moon forming around the Earth.

  
4,571,000,000 YBN
31) Oldest meteorite yet found on earth
4,571 million years old.


 
[1] The ''Zag'' meteorite fell to Earth
in 1988 COPYRIGHTED
source: http://news.bbc.co.uk/1/hi/sci/t
ech/783048.stm

4,530,000,000 YBN
33) Oldest Moon rock returned from
Apollo missions (4.53 billions old).




 
[1]
http://www.nasm.si.edu/exhibitions/attm/
atmimages/S73-15446.f.jpg
http://www.nasm.si.edu/exhibitions/attm/
nojs/wl.br.1.html
source:

4,500,000,000 YBN
24) Oldest meteor and moon (although no
earth) rocks date from this time 4.5
billion years before now.




  

LIFE
4,500,000,000 YBN
50) Start Precambrian Eon, Hadean Era.

  
4,450,000,000 YBN
21) Planet earth cools, molten rock
cools into thin crust, H2O condenses
from the atmosphere by raining, filling
the lowest parts of land to make the
first earth oceans, lakes, and rivers.


  
4,404,000,000 YBN
34) Oldest "terrestrial" (not from
meteorite) zircon yet found on earth,
4.404 billion years old, from Gneiss in
West Australia, is evidence that the
crust and liquid water were on the
surface of earth 4.4 billion years
before now.


 
[1]
http://www.geology.wisc.edu/zircon/Earli
est%20Piece/Images/8.jpg
source:

4,400,000,000 YBN
18) Amino acids, phosphates, and
sugars, the components of living
objects are created on earth. These
molecules are made in the oceans, fresh
water, and or atmosphere of earth (or
other planets) by lightning, photons
with ultraviolet frequency from the
star, or ocean floor volcanos.




  
4,395,000,000 YBN
19) How nucleic acids (polymers made of
nucleotides), proteins (polymers made
of amino acids), carbohydrates
(polymers made of sugars) and lipids
(glycerol attached to fatty acids)
evolved is not clearly known.

Some proteins and nucleic acids have
been formed in labs by using clay which
can dehydrate and which provides long
linear crystal structures to build
proteins and nucleic acids on. Amino
acids join together to form
polypeptides when an H2O molecule is
formed from a Hydrogen (H) on 1 amino
acid and a hydroxyl (OH) on the second.


Are all proteins, carbohydrates, lipids
and DNA the products of living objects?
Is RNA the only molecule of these that
was made without the help of living
objects?

The most popular theory now has RNA
(and potentially lipids) evolving first
before any living objects.

There is still a large amount of
experiment, exploration and education
that needs to be done to understand the
origins of living objects on planet
earth. My opinion is that as soon as
there was liquid water on the earth,
4.4 billion years before now, as zircon
crystals show, the construction of
living objects started on earth.


  
4,390,000,000 YBN
25) RNA duplication evolves.

Perhaps RNA molecules, called
"ribozymes" evolved which can make
copies of RNA, by connecting free
floating nucleotides that match a
nucleotide on the same or a different
RNA, without any proteins. But until
such ribozyme RNA molecules are found,
the only molecule known to copy nucleic
acids are proteins called polymerases.
If such ribozymes exist, then one of
the first coded instructions on the RNA
molecule that was the ancestor of every
living species, must have been the code
to make this ribozyme.

These early RNA molecules
may have been protected by liposomes
(spheres of lipids).

This process of RNA (and then later
DNA) duplication is the most basic
aspect of life on earth, and for all
the diversity, the one common element
of all life is this constant process of
DNA duplication, which will later
evolve to include cell division. This
starts the unbroken thread of copying
and division that connects the earliest
ancestor, some RNA molecule, to all
life on earth that has ever lived.



  
4,385,000,000 YBN
167) Protein assembly evolves with the
creation of various Transfer RNA (tRNA)
molecules.

Random mutations in the copying (and
perhaps even in the natural formation)
of RNA molecules probably created a
number of the necessary tRNAs (transfer
RNA, an RNA molecule responsible for
matching free floating amino acid
molecules to 3 nucleotide sequences on
other RNA molecules).

This would be a precellular protein
assembly system, where tRNA (transfer
RNA) molecules can build polypeptide
chains of amino acids by linking
directly to other RNA strands.

Part of each tRNA molecule bonds with a
specific amino acid, and a 3 nucleotide
sequence from a different part of the
tRNA molecule bonds with the opposite
matching 3 nucleotide sequence on an
(m)RNA molecule.

Since there are tRNA molecules for each
amino acid (although some tRNAs can
attach to more than one amino acid?),
there must have been a slow
accumulation of various tRNA molecules
for each of the 20 amino acids used in
constructing polypeptides in cells
living now. Perhaps after the
evolution of the first tRNA, the first
polypeptides were chains of all the
same one amino acid. With the
evolution of a second tRNA polypeptides
would have more variety because now two
amino acids would be available to build
polypeptides.

This polypeptide assembly system may
exist freely in water, or within a
liposome. This sytem builds many more
proteins than would be built without
such a system. The mRNA with the code
to make copier RNA, now also contains
the code to produce various tRNA
molecules. These molecules function as
a unit, and proto-cell, with the rest
of the mRNA initially containing random
codes for random proteins.

For the first time, RNA code represents
a template for other RNA molecules, but
also a template for building proteins
with the help of tRNA molecules.

There is some question of where the
origin of the first cell took place,
near volcanos on the ocean floor, or in
fresh water lakes and tidal pools near
volcanos on land, because unprotected
nucleic acids cannot exist for much
time in the ocean because of Sodium and
Chlorine.

What were the first amino acids
connected as proteins? Were the first
proteins all made with the same amino
acid?

  
4,380,000,000 YBN
168) Ribosomal RNA (rRNA) evolves.
Ribosomal RNA moves down mRNA molecules
functioning as a platform for bringing
the mRNA and tRNA molecules together to
assemble polypeptides (proteins).

This rRNA serves as an early ribosome;
objects that serve as sites for
building polypeptides and are found in
every cell. As time continues the
ribosome will grow to include two more
RNA molecules, some protein molecules,
and a second half that will make
polypeptide construction more
efficient.

The rRNA serves the purpose of bringing
amino acids close enough to bond with
each other to form polypeptides.

As an rRNA moves down an mRNA, tRNA
molecules bond with the mRNA and on the
opposite side of the tRNA, a matching
amino acid (separates? from the tRNA
and) attaches to a growing polypeptide
chain.

Now the mRNA that is the
ancestral/progenitor of all of life,
contains the code for the copier RNA,
tRNAs, and the rRNA molecule. These
nucleic acids function as a unit, and
proto-cell.




  
4,375,000,000 YBN
211) The first protein of real
importance is built, an RNA polymerase.
A molecule that can more efficiently
copy RNA.

The first protein of real
importance is evolved by RNA and
assembled by the early ribosome, an RNA
polymerase. A molecule that can more
efficiently copy RNA.



  
4,370,000,000 YBN
41) A ribonucleotide reductase protein
is built by the early ribosome protein
making protocell. This protein changes
ribonucleotides into
deoxyribonucleotides. This allows the
first DNA molecule on earth to be
assembled.

Ribonucleotide reductase may be the
molecule that allowed DNA to be the
template for the line of cells that
survived to now.




  
4,365,000,000 YBN
212) A DNA polymerase protein evolves
to copy DNA by assembling DNA
nucleotides from other DNA molecules.




  
4,360,000,000 YBN
166) An RNA molecule evolves that
causes the early ribosome to create
reverse transcriptase, a protein that
can assemble DNA molecules from an RNA
molecule template.

With this advance, a DNA molecule can
be constructed that has all of the code
that was stored on the long evolved RNA
molecule. DNA now serves as a more
stable template for making mRNA, each
tRNA, rRNA, and the RNA and DNA
polymerases.

RNA polymerase proteins build RNA
molecules using the new DNA template,
that still perform their original
polypeptide building function together
with the tRNA and rRNA molecules, but
are labeled "mRNA" (Messenger RNA)
because they move from DNA to ribosome.

Why DNA
serves as the template for all cells
and not mRNA is not fully understood,
but DNA is a more stable molecule than
the single stranded RNA. Perhaps the 2
legs of DNA serve some other important
reasons, for example, two legs may
allow two processes to happen at one
time.



  
4,355,000,000 YBN
20) The first cell membrane evolves
around DNA, made of proteins. This
membrane holds water inside a cell.
This is the first cell. rRNA
comparison shows that this is most
likely a eubacterium.

DNA produces instructions for
cytoplasm, the cytoplasm is assembled
from proteins made by the ribosome.
For the first time, DNA and ribosomes
are building cell structure. The
templates for each tRNA, rRNA, mRNA and
DNA polymerase proteins are already
coded in a central strand of DNA. DNA
protected by cytoplasm is more likely
to survive and copy. This cell is
heterotrophic and has no metabolism to
produce ATP. Amino acids, nucleotides,
H2O, and other molecules enter and exit
the cytoplasm only because of a
difference in concentration from inside
and outside the cell (passive
transport) and represent the beginnings
of the first digestive system. This
either happens in fresh water lakes or
in salty oceans, perhaps near lava
vents on or under the ocean floor. As
this line of DNA continues to make
copies of itself, all copies now have
cytoplasm. The DNA is composed mainly
of instructions to assemble the nucleic
acids and proteins needed to build
ribosomes, polymerases and cytoplasm.


This cell structure forms the basis of
all future cells of every living object
on earth. These first cells are
anaerobic (do not require free oxygen)
and heterotrophic, meaning that they do
not make their own food: amino acids,
nucleotides, phosphates, and sugars.
These bacteria depend on these
molecules and photons in the form of
heat to reproduce and grow.

A system of division must evolve which
attaches the original and newly
synthesized copy of DNA to the
cytoplasm, so that as the cell grows,
the two copies of DNA can be separated
and the first membraned cells can
divide into two cells. This is the
beginning of the "binary fission"
method of cell division. Division of
the cell begins with the division of
the DNA membrane-attachment site and
separates by the growth of new
cytoplasm.

DNA has 2 functions, 1) to be copied
by the polymerase protein, 2) to serve
as a code for assembling proteins.
Two
important evolutionary steps evolve:
DNA duplication in cytoplasm, and cell
(DNA with cytoplasm) division.

The process of DNA duplication is
probably similar if not the same
process using the same proteins that
were used to duplicate DNA without
cytoplasm.

  
4,350,000,001 YBN
26) Perhaps DNA that is connected in a
circle allows the DNA polymerase to
make continuous copies of the cell.

In
theory prokaryote cells do not
deteroiate from the effect of aging,
but they do endure mutations (from
photons with ultraviolet frequency, for
example), however, there are many other
ways prokaryotes can be destroyed (loss
of water, physically damaged by
nonliving objects, eaten by other
organisms, and other mechanisms).



  
4,345,000,000 YBN
195) Proteins that actively transport
molecules into and out of the cytoplasm
(facilitative diffusion) evolve.


 
[1] Uniporters are transport proteins
that transport a substance across a
membrane down a concentration gradient
from an area of greater concentration
to lesser concentration. The transport
is powered by the potential energy of a
concentration gradient and does not
require metabolic energy.
source: http://www.cat.cc.md.us/~gkaiser
/biotutorials/eustruct/cmeu.html


[2] Channel proteins transport water
or certain ions down a concentration
gradient from an area of higher
concentration to an area of lower
concentration. In the case of water,
the channel proteins are called
aquaporins. Water molecules are small
enough that they can also pass between
the phospholipids in the cytoplasmic
membrane by passive diffusion.
source:

4,340,000,000 YBN
23) The first viruses are made either
from bacteria, or are initially
bacteria. These cells depend on the
DNA duplicating and protein producing
systems of other cells to reproduce
themselves. Over time, more effective,
and efficient virus designs will
survive.


  
4,335,000,000 YBN
28) Glycolysis evolves in the
cytoplasm. Cells can now make ATP from
glucose and eventually other
monosaccharides, the end product is
pyruvate.

The glycolysis equation is:
C6H12O6
(glucose) + 2 NAD+ + 2 ADP + 2 P
-----> 2 pyruvic acid, (CH3(C=O)COOH +
2 ATP + 2 NADH + 2 H+




  
4,330,000,000 YBN
44) Fermentation evolves in the
cytoplasm. Cells (all anaerobic) can
now make more ATP and convert pyruvate
(the final product of glycolysis) to
lactate (an ionized form of lactic
acid).


  
4,325,000,000 YBN
213) A second kind of fermentation
evolves in the cytoplasm. Cells (all
anaerobic) can now convert pyruvate
(the final product of glycolysis) to
ethanol.


  
4,320,000,000 YBN
183) Cells evolve that make proteins
that can assemble lipids.


  
4,315,000,000 YBN
196) Cells that use both proteins and
metabolism (ATP) to transport molecules
into and out of the cytoplasm (active
transport) evolve.


 
[1] TP: not clear what the red circles
are, some kind of molecule I
guess. Antiporters are transport
proteins that simultaneously transport
two substances across the membrane in
opposite directions; one against the
concentration gradient and one with the
concentration gradient. Antiporters
typically use proton motive force to
transport a substrate across the
membrane. The movement of protons
across the membrane (proton motive
force) provides the energy for
transporting the substrate across the
membrane against its concentration
gradient..
source: http://www.cat.cc.md.us/~gkaiser
/biotutorials/eustruct/cmeu.html


[2] Symporters are transport proteins
that simultaneously transport two
substances across the membrane in the
same direction; one against the
concentration gradient and one with the
concentration gradient. Symporters
often use proton motive force to
transport a substrate across the
membrane. The movement of protons
across the membrane (proton motive
force) provides the energy for
transporting the substrate.
source:

4,310,000,000 YBN
40) One of the first useful proteins to
be created with an early precellular
protein production system must have
been a protein (like RNA polymerase)
that can make copies of RNA from mRNA
molecules. This protein may have
outperformed a ribozyme that was
performing the copying function.
Eventually mRNA that coded for tRNA
molecules and mRNA that coded for rRNA
molecules merged to form a template.
Now the entire protein production
system (the mRNA itself, tRNAs, rRNAs,
and the RNA polymerase) could be copied
many times by the RNA polymerase
protein.

This is before cytoplasm or any cell
wall has evolved. RNA and DNA copying
happens in water, the first cell has
not evolved yet.




  
4,310,000,000 YBN
76) Pili, plasmids and conjugation
evolves in prokaryotes. Now some
prokaryotes can exchange circular
pieces of DNA (plasmids), through tubes
(pili). Conjugation may be the process
that led to sex (cellular fusion) and
also the transition from a circle of
DNA to chromosomes in eukaryotes, since
some protists (cilliates and some
algae) reproduce sexually by
conjugation.

Archaeal flagellins are related to
members of the type IV pilin/transport
superfamily widespread in bacteria.
In addition
to pili and conjugation, proteins
evolve that can assist in splitting DNA
and also proteins that assist in
merging two strands of DNA together,
since some times the DNA in split and
the new plasmid is connected and the
DNA circle is sown back together.

 
[1] the fertility factor or F factor is
a very large (94,500 bp) circular dsDNA
plasmid; it is generally independent of
the host chromosome. COPYRIGHTED
source: http://www.mun.ca/biochem/course
s/3107/images/Fplasmidmap.gif


[2] conjugation (via pilus)
COPYRIGHTED EDU
source: http://www.bio.miami.edu/dana/16
0/conjugation.jpg

4,307,000,000 YBN
292) Prokaryote flagella evolve.
Perhaps pili
evolved into flagella, flagella into
pili, or the two systems are
unrelated.

Proteins in Archaebacteria flagella are
related to pili in bacteria.

This may be the beginning of motility.
Now for the first time, cells are not
completely controlled by surrounding
matter, but can make limited choices
about their location.

  
4,305,000,000 YBN
64) Operons, sequences of DNA that
allow certain proteins coded by DNA to
not be built, evolve. Proteins bind
with these DNA sequences to stop RNA
polymerase from building mRNA molecules
which would be translated into
proteins. Operons allow a bacterium to
produce certain proteins only when
necessary. Bacteria before now can
only build a constant stream of all
proteins encoded in their DNA.


  
4,304,500,000 YBN
322) Nitrogen fixation evolves in
eubacteria.

Without bacteria that convert N2 into
nitrogen compounds, the supply of
nitrogen necessary for much of life
would be seriously limited and would
drastically slow evolution on earth.

Nitrogen
fixation is the process by which
nitrogen is taken from its relatively
inert molecular form (N2) in the
atmosphere and converted into nitrogen
compounds useful for other chemical
processes (such as, notably, ammonia,
nitrate and nitrogen dioxide).

Nitrogen fixation is performed
naturally by a number of different
prokaryotes, including bacteria, and
actinobacteria certain types of
anaerobic bacteria. Many higher plants,
and some animals (termites), have
formed associations with these
microorganisms.



 
[1] This is an image of nitrogen cycle
taken from this [1] EPA website. PD
source: http://en.wikipedia.org/wiki/Ima
ge:Nitrogen_Cycle.jpg

4,304,000,000 YBN
287) Multicellularity in the form of
filment growth evolves in prokaryotes.

Cyanobacteria
grow in filaments.

Unlike eukaryotes, there is no
communication between cells in
prokaryote filments.



  
4,302,000,000 YBN
316) Cell differentiation in
prokaryotes evolve. Heterocysts evolve
in cyanobacteria.

Heterocysts are specialized
nitrogen-fixing cells formed by some
filamentous cyanobacteria during
nitrogen starvation.

What cell differentiation is
first is unknown, perhaps cells that
form spores, or cysts, or perhaps cell
differentiation that is observes in
cyanobacterial filamentous cells.

Heterocysts are specialized
nitrogen-fixing cells formed by some
filamentous cyanobacteria, such as
Nostoc punctiforme and Anabaena
sperica, during nitrogen starvation.
They fix nitrogen from dinitrogen (N2)
in the air using the enzyme
nitrogenase, in order to provide the
cells in the filament with nitrogen for
biosynthesis. Nitrogenase is
inactivated by oxygen, so the
heterocyst must create a microanaerobic
environment. The heterocysts' unique
structure and physiology requires a
global change in gene expression. For
example, heterocysts:

* produce three additional cell
walls, including one of glycolipid that
forms a hydrophobic barrier to oxygen
*
produce nitrogenase and other proteins
involved in nitrogen fixation
* degrade
photosystem II, which produces oxygen
* up
regulate glycolytic enzymes, which use
up oxygen and provide energy for
nitrogenase
* produce proteins that scavenge
any remaining oxygen

Cyanobacteria usually obtain a fixed
carbon (carbohydrate) by
photosynthesis. The lack of photosystem
II prevents heterocysts from
photosynthesising, so the vegetative
cells provide them with carbohydrates,
which is thought to be sucrose. The
fixed carbon and nitrogen sources are
exchanged though channels between the
cells in the filament. Heterocysts
maintain photosystem I, allowing them
to generate ATP by cyclic
photophosphorylation.

Single heterocysts develop about every
9-15 cells, producing a one-dimensional
pattern along the filament. The
interval between heterocysts remains
approximately constant even though the
cells in the filament are dividing. The
bacterial filament can be seen as a
multicellular organism with two
distinct yet interdependent cell types.
Such behaviour is highly unusual in
prokaryotes and may have been the first
example of multicellular patterning in
evolution. Once a heterocyst has
formed, it cannot revert to a
vegetative cell, so this
differentiation can be seen as a form
of apoptosis. Certain
heterocyst-forming bacteria can
differentiate into spore-like cells
called akinetes or motile cells called
hormogonia, making them the most
phenotyptically versatile of all
prokaryotes.

The mechanism of controlling
heterocysts is thought to involve the
diffusion of an inhibitor of
differentiation called PatS. Heterocyst
formation is inhibited in the presence
of a fixed nitrogen source, such as
ammonium or nitrate. The bacteria may
also enter a symbiotic relationship
with certain plants. In such a
relationship, the bacteria do not
respond to the availability of
nitrogen, but to signals produced by
the plant. Up to 60% of the cells can
become heterocysts, providing fixed
nitrogen to the plant in return for
fixed carbon.

The cyanobacteria that form heterocysts
are divided into the orders Nostocales
and Stigonematales, which form simple
and branching filaments respectively.
Together they form a monophyletic
group, with very low genetic
variability.

 
[1] Anabaena COPYRIGHTED EDU
source: http://home.manhattan.edu/~franc
es.cardillo/plants/monera/anabaena.gif


[2] Anabaena smitthi COPYRIGHTED
FRANCE
source: http://www.ac-rennes.fr/pedagogi
e/svt/photo/microalg/anabaena.jpg

4,300,000,000 YBN
58) First autotrophic cells, cells that
can produce some if not all of their
own food (amino acids, nucleotides,
sugars, phophates, lipids, and
carbohydrates), but require phosphorus,
nitrogen, CO2, water and light in the
form of heat.

There are only 2 kinds of autotrophy:
Lithotrophy and Photosynthesis. These
are lithotrophic cells that change
inorganic (abiotic) molecules into
organic molecules. These cells are
archaebacteria, called methanogens that
perform the reaction: 4H2 + CO2 -> CH4
+ 2H2O. They convert CO2 into Methane.
Methane is better than CO2 for
trapping heat, and could have
contributed to heating the earth.


  
4,295,000,000 YBN
49) First photosynthetic cells. These
cells only have Photosystem I.
Photosynthesis Photosystem I evolves in
early anaerobic prokaryote cells. One
of two photosythesis systems,
photosystem I uses a pigment
chlorophyll A, absorbs photons in 700
nm wave lengths best, breaking the bond
betwenn H2 and S. They are anaerobic
and perform the reaction: H2S
(Hydrogen Sulfide) + CO2 + light ->
CH2O (Formaldehyde) + 2S.

Only 5 phyla of
eubacteria can photosynthesize.

  
4,290,000,000 YBN
43) Photosynthesis Photosystem II
evolves in early prokaryote cells.
Photosystem 2 absorbs photons best at
680nm wavelengths, a higher frequency
of light than Photosystem I. These
cells can break the strong Hydrogen
bonds between Hydrogen and Oxygen in
water molecules (more abundant than
Sulphur). This system emits free
Oxygen.

The simple equation of photosynthesis
is: 6 H2O + 6 CO2 + photons = C6H12O6
(glucose) + 6O2. The detailed steps of
photosynthesis are called the "Calvin
Cycle". Prokaryote cells can now
produce their own glucose to store and
be converted to ATP by glycolysis and
fermentation later.

This sytem is the main system
responsible for producing the Oxygen
now in the air of earth.

Of the 5 phyla of
eubacteria that can photosynthesize,
only 1, cyanobacteria, produces oxygen.

  
4,280,000,000 YBN
57) Cellular Respiration (also called
the "Citric Acid Cycle", and the "Krebs
Cycle") evolves, probably in
cyanobacteria, as a substitute for
fermentaton, by using oxygen to break
down the products of glycolysis,
pyruvic acid, to CO2 and H2O, producing
18 more ATP molecules.
This is the
first aerobic cell, a cell that has an
oxygen based metabolism. This cell
uses oxygen to convert glucose (and
eventually other sugars and fats) into
CO2, H2O and ATP. For example, cells
that oxidize glucose perform the
reaction:
C6H12O6 + 6 O2 + 38 ADP + 38 phosphate
-> 6 CO2 + 6 H2O + 38 ATP
This reaction
(with glycolysis) can produce up to 36
ATP molecules. Cellular respiration is
the opposite (although the specific
reactions differ) of photosynthesis
which starts with H2O and CO2 and
produces glucose.

Steps are:
Glycolysis preparatory
phase
Glycolysis pay-off phase
Oxidative
carboxylation
Krebs cycle

 
[1] kreb cycle from
http://people.unt.edu/~hds0006/tca/
source:

4,260,000,000 YBN
27) DNA (or RNA) produces instructions
for a cell wall. The cell wall only
protects bacteria and does not filter
any molecules as the cytoplasm does.

is
first gram-negative cell wall?

1. Only contain a few layers of
peptidoglycan -- the building block for
strong, rigid cell walls
2. Contain an
outer membrane, external to the
peptidoglycan, called the
lipopolysaccharide
3. The space between the layers of
peptidoglycan and the secondary cell
membrane is called periplasmatic space
4.
The S-layer is directly attached to the
outer membrane, rather than the
peptidoglycan
5. Any flagella, if present, have 4
supporting rings instead of two
6. No
teichoic acids are present"



 
[1] one is indirectly
from http://www.cvm.uiuc.edu/courses/vp
331/index.html
source: file:/root/web/Structures_in_pat
hogenesi1.html



source: http://www.mansfield.ohio-state.
edu/~sabedon/biol1080.htm

4,250,000,000 YBN
29) There are many proteins and
secondary processes in cells that are
not fully understood yet.




  
4,250,000,000 YBN
42) More prokaryote cell fossils need
to be found, more DNA needs to be
sequenced, and more bacteria found and
grown to fully understand when bacteria
parts evolved. For example:
flagella
plasmids
pili and "conjugation" the trade of
pieces of plasmid DNA (this may be the
earliest form of sex {or syngamy})
changing into
spores

When gram-stain positive cell walls
evolved.

When the various shapes evolved:
spherical
(coccus,cocci)
rod (bacillus,bacilli)
spiral (spirilla)
other:
short rods (coccobacilli).
commas (vibrii).
squares (rare)
stars (rare)
irregula
r (rare)

Which specific bacteria of the Archaea
(if any) were first, which of the
Eubacteria and Cyanobacteria came
next.

When the "Nitrogen Cycle" or "Nitrogen
Fixing" evolved. Few cells can
separate N2 into N, (needed for nucleic
acids?). The waste product urea is
converted by one bacteria to ammonia, a
second bacteria converts the ammonia to
N2.

  
4,250,000,000 YBN
77) There are many widely varying
estimates of when the first Eubacteria
and Archaea evolved. Eubacteria and
Archaea (also called Archaebacteria)
are the two major lines of Prokaryotes.
Prokaryotes are the most primitive
living objects ever found. In contrast
to the later evolved Eukaryotes,
Prokaryotes have a circle of DNA
located in their cytoplasm (not
chromosomes) and have no nucleus. At
least one genetic comparison shows
Eubacteria and Archaea evolving now.

After the full genomes of all living
species are known, and understood we
will have more certainty about the
history of evolution. Many genetic
trees are based on DNA genes (sequences
of DNA that define nucleic acids or
proteins). In particular the genes for
ribosomal RNA are thought to be very
conserved over time, although perhaps
genes for reproduction, or cytoplasm,
for example may later prove to be more
conserved over time.

Only when the full
genomes of all living species are
known, and understood will we have
strong certainty about the history of
evolution. Many genetic trees are
based on DNA genes (sequences of DNA
that define nucleic acids or proteins),
in particular ribosomal RNA which is
thought to be highly conserved over the
eons of time. Ribosomal RNA may be the
best record of evolutionary history,
but perhaps other genes, for example,
those involved with reproduction, or
cytoplasm will prove to be more
conserved or better estimates of
evolutionary history. For example, I
think the method of reproduction would
be the most conserved, since that
process is the most necessary for
survival, changes to those genes may
stop continued existence, where changes
to rrna may not be as serious. In
addition, the vast diversity and change
in reproductive method over time,
should tell us that similar large scale
changes could have happened for rrna,
cytoplasm, and indeed any part of a
cell.


These early Archaea and Eubacteria are
"thermophile" bacteria, bacteria that
are found and grow best in hot water
(80+ degrees Celsius). That genetic
evidence puts these prokaryotes as the
oldest living prokaryotes is evidence
that the first prokaryotes on earth may
have lived in hot water, perhaps near
thermal springs or near ocean floor
volcanos. Perhaps the water on the
early earth was hot when these first
prokaryotes evolved.

 
[1] Figure 1) Changing views of the
tree and timescale of life. a) An
early-1990s view, with the tree
determined mostly from ribosomal RNA
(rRNA) sequence analysis. This tree
emphasizes vertical (as opposed to
horizontal) evolution and the close
relationship between eukaryotes and the
Archaebacteria. The deep branching
(>3.5 Giga (109) years ago, Gya) of
CYANOBACTERIA (Cy) and other Eubacteria
(purple), the shallow branching
(approx1 Gya) of plants (Pl), animals
(An) and fungi (Fu), and the early
origin of mitochondria (Mi), were based
on interpretations of the geochemical
and fossil record7, 8. Some deeply
branching amitochondriate (Am) species
were believed to have arisen before the
origin of mitochondria44. Major
symbiotic events (black dots) were
introduced to explain the origin of
eukaryotic organelles42, but were not
assumed to be associated with large
transfers of genes to the host nucleus.
They were: Eu, joining of an
archaebacterium host with a eubacterium
(presumably a SPIROCHAETE) to produce
an amitochondriate eukaryote; Mi,
joining of a eukaryote host with an
alpha-proteobacterium (Ap) symbiont,
leading to the origin of mitochondria,
and plastids (Ps), joining of a
eukaryote host with a cyanobacterium
symbiont, forming the origin of
plastids on the plant lineage and
possibly on other lineages. b) The
present view, based on extensive
genomic analysis. Eukaryotes are no
longer considered to be close relatives
of Archaebacteria, but are genomic
hybrids of Archaebacteria and
Eubacteria, owing to the transfer of
large numbers of genes from the
symbiont genome to the nucleus of the
host (indicated by coloured arrows).
Other new features, largely derived
from molecular-clock studies16, 39 (Box
1), include a relatively recent origin
of Cyanobacteria (approx2.6 Gya) and
mitochondria (approx1.8 Gya), an early
origin (approx1.5 Gya) of plants,
animals and fungi, and a close
relationship between animals and fungi.
Coloured dashed lines indicate
controversial aspects of the present
view: the existence of a
premitochondrial symbiotic event and of
living amitochondriate eukaryotes,
ancestors of which never had
mitochondria. c) The times of
divergence of selected model organisms
from humans, based on molecular clocks.
For the prokaryotes (red), because of
different possible origins through
symbiotic events, divergence times
depend on the gene of interest.
source: http://www.nature.com/nrg/journa
l/v3/n11/full/nrg929_fs.html


[2] Figure 2 A phylogeny of
prokaryotes. The relationships of
selected prokaryote model organisms
based on recent studies14-19. Times of
divergence (million years ago (Mya)
plusminus one standard error) are
indicated at nodes in the tree16, 39.
Branch lengths are not proportional to
time. Phyla and phylum-level groupings
are indicated on the right.
source: http://www.nature.com/nrg/journa
l/v3/n11/full/nrg929_fs.html

4,112,000,000 YBN
180) The Archaea Phylum, Euryarchaeotes
evolve.

Genetic comparison shows the Archaea
Phylum, Euryarchaeotes evolving now.

The Euryarchaeota are a major group of
Archaea. They include the methanogens,
which produce methane and are often
found in intestines, the halobacteria,
which survive extreme concentrations of
salt, and some extremely thermophilic
aerobes and anaerobes. They are
separated from the other archaeans
based mainly on rRNA sequences.

Euryarchaeota may contain the most
ancient DNA of any living object on
earth.

 
[1] tree of archaebacteria (archaea)
COPYRIGHTED
source: http://www.uni-giessen.de/~gf126
5/GROUPS/KLUG/Stammbaum.html


[2] A phylogenetic tree of living
things, based on RNA data, showing the
separation of bacteria, archaea, and
eukaryotes. Trees constructed with
other genes are generally similar,
although they may place some
early-branching groups very
differently, thanks to long branch
attraction. The exact relationships of
the three domains are still being
debated, as is the position of the root
of the tree. It has also been suggested
that due to lateral gene transfer, a
tree may not be the best representation
of the genetic relationships of all
organisms. NASA
source: http://en.wikipedia.org/wiki/Ima
ge:PhylogeneticTree.jpg

4,112,000,000 YBN
181) The Archaea Phylum, Crenarchaeotes
evolves.

Genetic comparison shows Archaea
Phylum, Crenarchaeotes evolving now.

The phylum Crenarchaeota, commonly
referred to as the crenarchaea, in the
domain Archaea, contains many extremely
thermophilic and psychrophilic
organisms. They were originally
separated from the other archaeons
based on rRNA sequences, since then
physiological features, such as lack of
histones have supported this division.
Until recently all cultured crenarchaea
have been thermophilic or
hyperthermophilic organisms, some of
which have the ability to grow up to
113 degrees C. These organisms stain
gram negative and are morphologically
diverse having rod, cocci, filamentous
and unusually shaped cells.

 
[1] tree of archaea ?
source: http://www.uni-giessen.de/~gf126
5/GROUPS/KLUG/Stammbaum.html


[2] Microscopia elettronica a
scansione dell'archeobatterio
termoacidofilo Sulfolobus solfataricus
COPYRIGHT ITALY
source: http://www.area.fi.cnr.it/r&f/n6
/ingrand.htm

4,030,000,000 YBN
35) Metamorphic rock, a Gneiss near
Acasta and Great Slave Lake in the
North West territories of Canada dates
from this time, 4030 million years
before now.

 

source: http://www.regione.emilia-romagn
a.it/geologia/divulgazione/pianeta_terra
/09_paesaggio/img/app/c09_a01_01.jpg



source:

3,977,000,000 YBN
193) Eubacteria "Hyperthermophiles"
(Aquifex, Thermotoga, etc.) evolve now.

Gene
tic comparison shows that Eubacteria
"Hyperthermophiles" (Aquifex,
Thermotoga, etc.) evolve now.

This may be the living object with the
most primitive DNA found on earth
(depending on the age of the archaea).

This group of eubacteria includes the
Phyla "Aquificae",
"Thermodesulfobacteria", and
"Thermotogae".

The Aquificae phylum is a diverse
collection of bacteria that live in
harsh environmental settings. They have
been found in hot springs, sulfur
pools, and thermal ocean vents. Members
of the genus Aquifex, for example, are
productive in water between 85 to 95
°C. They are the dominant members of
most terrestrial neutral to alkaline
hot springs above 60 degrees celsius.
They are autotrophs, and are the
primary carbon fixers in these
environments. They are true bacteria
(domain eubacteria) as opposed to the
other inhabitants of extreme
environments, the Archaea.

Thermotoga are thermophile or
hyperthermophile bacteria whose cell is
wrapped in an outer "toga" membrane.
They metabolize carbohydrates. Species
have varying amounts of salt and oxygen
tolerance. Thermotoga subterranea
strain SL1 was found in a 70°C deep
continental oil reservoir in the East
Paris Basin, France. It is anaerobic
and reduces cystine and thiosulfate to
hydrogen sulfide.

 
[1] Aquifex pyrophilus (platinum
shadowed). © K.O. Stetter & Reinhard
Rachel, University of Regensburg.
source: http://biology.kenyon.edu/Microb
ial_Biorealm/bacteria/aquifex/aquifex.ht
m


[2] Aquifex aeolicus. © K.O. Stetter
& Reinhard Rachel, University of
Regensburg.
source: http://biology.kenyon.edu/Microb
ial_Biorealm/bacteria/aquifex/aquifex.ht
m

3,850,000,000 YBN
36) The oldest sediment on earth is
also the oldest Banded Iron Formation,
on Akilia Island in Western Greenland.
The oldest evidence for life on earth
was found in this rock by measuring the
ratio of carbon 12 to carbon 13 in
grains of apatite (calcium phosphate)
from this rock. Life uses the lighter
Carbon-12 isotope and not Carbon-13 and
so the ratio of carbon-12 to carbon-13
is different from a nonliving source
(calcium carbonate or limestone).


 

source: nature 11/7/96

3,850,000,000 YBN
45) This marks the beginning of the
Banded Iron Formation Rocks. These
rocks are sedimentary. They are made
of iron rich chert (silicates, like
SiO2). These rocks have alternative
bands of orange or yellow and black.
In the red parts the iron is oxydized
(contains iron oxides, either hematite
{Fe2O3 = rust} or magnetite {Fe3O4]}).


These bands may have formed because
photosynthetic bacteria (in
stromatolites found in shallow ocean
shores, and purple bacteria floating in
water) produce oxygen from CO2 during
photosynthesis. When the level of
oxygen in the water became too high,
many bacteria died, and this cycle
created the BIF. But BIF also may form
naturally when photons in uv
frequencies split H2O into H2 and O2.
So perhaps the BIF bands represent
cycles of more or less uv light
reaching the earth. Perhaps the
alternating phenomenon is similar to
eukaryotic algal blooms. In any event,
this free oxygen bonded with the many
tons of iron dissolved in the water to
form insoluable iron oxide which then
fell to the ocean floor to form the
orange layers of Banded Iron Formation.
How these alternating bands are made
is not clear and has not yet been
duplicated in a lab.

This cycle of alternating orange and
black bands will continue for 2 billion
years until 1,800 million years before
now. This is the beginning of oxygen
production on earth, the atmosphere of
earth still has only small amounts of
oxygen at this time.

It is amazing that
people are still not certain what was
the cause of the oxygen, and the cycles
that deposited the banded Iron
Formation.

 

source: nature 11/7/96

3,850,000,000 YBN
189) Fossils from Isua Banded iron
formation, SW Greenland.

 
[1] Fig. 5. (a) Carbonaceous
microstructure from Isua Banded iron
formation, SW-Greenland (ca 3.85 Ga).
(b) Laser mass spectrum (negative ions)
from similar specimen. Field of
measurement ca 1 small mu, Greekm
diameter.
source: http://www.sciencedirect.com/sci
ence?_ob=MiamiCaptionURL&_method=retriev
e&_udi=B6VBP-42G6M5T-7&_image=fig7&_ba=7
&_user=4422&_coverDate=02%2F01%2F2001&_f
mt=full&_orig=browse&_cdi=5932&view=c&_a
cct=C000059600&_version=1&_urlVersion=0&
_userid=4422&md5=fe1052cbc18dba545ec95c2
e7ff3090b

3,800,000,000 YBN
51) End Hadean Era, start Archean Era.

  
3,800,000,000 YBN
185) Isoprene compounds from Isua,
Greenland Banded Iron Formation
sediment are evidence of the existence
of Archaea.


  
3,760,000,000 YBN
186) Sulfur isotope ratios (34S/32S)
and Hydrocarbon molecules (alkanes)
detected in 3760 billion year old Isua
Banded Iron Formation, indicate the
possibility of photosynthetic sulfate
reducing bacteria (Archaea, for example
Sulpholobus) and Cyanobacteria living
at that time.


  
3,700,000,000 YBN
184) Amount of Uranium isotope measured
in Isua, Greenland Banded Iron
Formation evidence of prokaryote Oxygen
photosynthesis.


  
3,700,000,000 YBN
215) C13/C12 ratio of 3700+ MYO
sediment in Australia shown to be
consistent with planktonic
photosynthesizing organisms.

 
[1] Figure 1. (A) Turbidite sedimentary
rocks from the Isua supracrustal belt,
west Greenland. The notebook is 17 cm
wide. (B) A close-up of finely
laminated slate representing pelagic
mud. The hammer is 70 cm long. (C)
Photomicrograph of sample 810213,
showing finely laminated pelagic mud.
The variation in color is mainly due to
variations in C abundance. (D)
Photomicrograph of C grains arranged
along a buckled stringer. (E)
Backscattered electron image of a
polished surface (sample 810213),
showing the distribution of C grains as
black areas. (F) Backscattered electron
image of a polished surface (sample
810213), showing the rounded shape of C
grains (black).
source: http://www.sciencemag.org/cgi/co
ntent/full/283/5402/674

3,566,000,000 YBN
78) Genetic comparison shows
Archaebacteria (Archaea) Phylum,
Korarchaeotes evolving now.

 
[1] DNA tree
source: http://www.uni-giessen.de/~gf126
5/GROUPS/KLUG/Stammbaum.html


[2] Scanning electron micrograph of
the Obsidian Pool enrichment culture.
Barns et al. discovered the
Korarchaeota lineage in Obsidian Pool
over a decade ago, using what were
highly innovative methods for the time.
Since their discovery, the Korarchaeota
group of microorganisms still remains
mostly uncharacterized. The group is
primarily defined only by 16S ribosomal
RNA sequences obtained from a variety
of marine and terrestrial hydrothermal
environments. The 16S-rRNA-based
phylogeny of the Korarchaeota suggests
that this group forms a very deep,
kingdom-level, major lineage within the
archaeal domain. PD
source: http://www.jgi.doe.gov/sequencin
g/why/CSP2006/korarchaeota.jpg

3,500,000,000 YBN
37) The oldest fossil evidence of life
yet found. Stromatolites made by
photosynthetic bacteria found in both
Warrawoona, Western Australia, and Fig
Tree Group, South Africa.


 
[1] image on left is from swaziland
source: nature feb 6



source: 1986

3,500,000,000 YBN
39) Oldest fossils of an organism,
thought to be cyanobacteria, found in
3,500 Million Year old chert from South
Africa and 3,465 Million year old Apex
chert of north-western Australia.

Oldest fossils
of an organism, thought to be
cyanobacteria, found in 3,500 Million
Year old chert from South Africa and
3,465 Million year old Apex chert of
the Pilbara Supergroup, Warrawoona
Group, northwestern Western Australia.

Some people argue that these are not
fossils of bacteria but abiotic
material. Most genetic timelines put
the origin of cyanobacteria much later
around 2,700mybn.

 
[1] Figure 1 Optical photomicrographs
showing carbonaceous (kerogenous)
filamentous microbial fossils in
petrographic thin sections of
Precambrian cherts. Scale in a
represents images in a and c-i; scale
in b represents image in b. All parts
show photomontages, which is
necessitated by the three-dimensional
preservation of the cylindrical sinuous
permineralized microbes. Squares in
each part indicate the areas for which
chemical data are presented in Figs 2
and 3. a, An unnamed cylindrical
prokaryotic filament, probably the
degraded cellular trichome or tubular
sheath of an oscillatoriacean
cyanobacterium, from the 770-Myr
Skillogalee Dolomite of South
Australia12. b, Gunflintia grandis, a
cellular probably oscillatoriacean
trichome, from the 2,100-Myr Gunflint
Formation of Ontario, Canada13. c, d,
Unnamed highly carbonized filamentous
prokaryotes from the 3,375-Myr Kromberg
Formation of South Africa14: the poorly
preserved cylindrical trichome of a
noncyanobacterial or oscillatoriacean
prokaryote (c); the disrupted,
originally cellular trichomic remnants
possibly of an Oscillatoria- or
Lyngbya-like cyanobacterium (d). e-i,
Cellular microbial filaments from the
3,465-Myr Apex chert of northwestern
Western Australia: Primaevifilum
amoenum4,5, from the collections of The
Natural History Museum (TNHM), London,
specimen V.63164[6] (e); P. amoenum4
(f); the holotype of P.
delicatulum4,5,15, TNHM V.63165[2] (g);
P. conicoterminatum5, TNHM V63164[9]
(h); the holotype of Eoleptonema apex5,
TNHM V.63729[1] (i).
source: Nature416


[2] Fig. 3 Filamentous microfossils:
a, cylindrical microfossil from
Hooggenoeg sample; b, threadlike and
tubular filaments extending between
laminae, Kromberg sample; c,d,e,
tubular filamnets oriented subparallel
to bedding, Kromberg sample; f,
threadlike filament flattened parallel
to bedding, Kromberg sample.
source: 73 - 76 (07 Mar 2002) Letters
to Nature
http://www.nature.com/nature/journal/v41
6/n6876/fig_tab/416073a_F1.html

3,470,000,000 YBN
182) Sulphate fossil molecular marker
evidence of moderate thermophile
sulphur reducing prokaryotes from North
Pole, Australia.


 
[1] get larger image
source: file:///root/web/fossils_biomark
er_science_v67_i22_nov_15_2003.html#bib9
9

3,470,000,000 YBN
216) Evidence of sulphate reduction by
bacteria.


 
[1] The tree is modified from ref. 2,
and abstracted from phylogenetic trees
presented in refs 26 and 27. The time
calibration points are from ref. 30,
with our additional constraint of 3.47
Gyr placed in the Bacterial domain.
Lineages housing sulphate-reducers
metabolizing at temperatures > 70 °C
are shown by broken black lines, while
lineages supporting sulphate-reducers
metabolizing at < 70 °C are shown by heavy black lines.
source: http://www.nature.com/nature/jou
rnal/v410/n6824/fig_tab/410077a0_F4.html

3,416,000,000 YBN
218) Fossil and molecular evidence of
photosynthetic, probably anoxygenic,
bacteria that lived in mats in the
ocean date to this time.


 
[1] a, Dark carbonaceous laminations
draping an underlying coarse detrital
carbonaceous grain (a), showing
internal anastomosing and draping
character (b) and, at the top (c)
draping irregularities in underlying
carbonaceous laminations. b, Dark
carbonaceous laminations that have been
eroded and rolled up by currents. c,
Bundled filaments in the rolled
laminations in b [tp: they should
have clearly indicated that they are
saying that these filaments are
bacteria].
source: http://www.nature.com/nature/jou
rnal/v431/n7008/fig_tab/nature02888_F4.h
tml

3,400,000,000 YBN
190) Fossils from Kromberg Formation,
Swaziland System, South Africa.

 
[1] Fig. 3. (a,b) Organic
microstructures from Kromberg
Formation, Swaziland System, South
Africa (ca 3.4 Ga). TEM-micrographs of
demineralized specimens. (c) Portion of
organic microstructure from Bulawaya
stromatolite (see Fig. 2). (d) Portion
of the mucilagenous sheath of recent
Anabaena sp., cyanobacteria (Fig. d
after Leak, 1967). For magnification of
Fig. c see scale of Fig. a.
source: http://www.sciencedirect.com/sci
ence?_ob=MiamiCaptionURL&_method=retriev
e&_udi=B6VBP-42G6M5T-7&_image=fig9&_ba=9
&_user=4422&_coverDate=02%2F01%2F2001&_f
mt=full&_orig=browse&_cdi=5932&view=c&_a
cct=C000059600&_version=1&_urlVersion=0&
_userid=4422&md5=27a45a0804747bb4b74eaac
305df2905

3,260,000,000 YBN
71) Budding evolves in prokayotes.
Different from binary division, where a
cell is split in half, in budding, a
new complete cell is made in the
original cell, and the new cell bursts
through the cell wall, the original
cell wall must then be repaired.

Budding is the
only other method of reproduction known
in prokaryotes besides binary fission.

The only major difference between
prokaryote budding and binary division
are that one or more new cells are
completely formed inside the original
cell, where in binary division part of
the original cell wall is used to make
the new cell.

In budding, a complete new cell is
synthesized from a DNA template, where
in binary division only the DNA is
duplicated and more cytoplasm and cell
wall is synthesized. So, budding
preserves organelles made by the main
DNA template that cannot duplicate
themselves and would not get duplicated
or synthesized in binary division, for
example, flagella.

 
[1] Evolutionary relationships of model
organisms and bacteria that show
unusual reproductive strategies. This
phylogenetic tree (a) illustrates the
diversity of organisms that use the
alternative reproductive strategies
shown in (b). Bold type indicates
complete or ongoing genome projects.
Intracellular offspring are produced by
several low-GC Gram-positive bacteria
such as Metabacterium polyspora,
Epulopiscium spp. and the segmented
filamentous bacteria (SFB). Budding and
multiple fission are found in the
proteobacterial genera Hyphomonas and
Bdellovibrio, respectively. In the case
of the Cyanobacteria, Stanieria
produces baeocytes and Chamaesiphon
produces offspring by budding.
Actinoplanes produce dispersible
offspring by multiple fission of
filaments within the sporangium.
source: http://www.nature.com/nrmicro/jo
urnal/v3/n3/full/nrmicro1096_fs.html
(Nature Reviews Microbiology 3


[2] Electron micrograph of a
Pirellula bacterium from giant tiger
prawn tissue (Penaeus monodon). Notice
the large crateriform structures (C) on
the cell surface and flagella. From
Fuerst et al.
source: 214-224 (2005);
doi:10.1038/nrmicro1096)

3,250,000,000 YBN
191) Fossils from Swartkoppie chert,
South Africa are oldest evidence of
procaryotes that reproduce by budding
and not binary fission.


 
[1] Fig. 4. (a-d) Organic
microstructures from Swartkoppie chert,
South Africa (ca 3.25 Ga).
TEM-micrographs of demineralized
specimen (a,b) Laser mass spectra
(negative ions) from clusters of
similar specimens. Field of measurement
ca 1 small mu, Greekm diameter. (c,d)
TEM-micrographs from demineralized Thin
section. (e) Recent budding iron
bacterium Pedomicrobium sp. (Fig. e
from Ghiorse and Hirsch, 1979).
source: http://www.sciencedirect.com/sci
ence?_ob=MiamiCaptionURL&_method=retriev
e&_udi=B6VBP-42G6M5T-7&_image=fig6&_ba=6
&_user=4422&_coverDate=02%2F01%2F2001&_f
mt=full&_orig=browse&_cdi=5932&view=c&_a
cct=C000059600&_version=1&_urlVersion=0&
_userid=4422&md5=801178ddb930bd041063bae
7a3e0e204

3,235,000,000 YBN
68) Thermophilic prokaryote fossils
found in 3235 million year old deep-sea
volcanogenic massive sulphide deposits
from the Pilbara Craton of Australia
may be oldest Archaea fossils.


 
[1] Photomicrographs of filaments from
the Sulphur Springs VMS deposit. Scale
bar, 10 µm. a-f, Straight, sinuous and
curved morphologies, some densely
intertwined. g, Filaments parallel to
the concentric layering. h, Filaments
oriented sub-perpendicular to
banding.
source:

2,923,000,000 YBN
178) Eubacteria Phylum Firmicutes (low
G+C {Guanine and Cytosine count} Gram
positive) evolve.

Genetic comparison shows
Eubacteria Phylum Firmicutes (low G+C
{Guanine and Cytosine count} Gram
positive) evolving here.

Firmicutes include the Classes:
Bacillus (anthrax), Listeria,
Mollicutes, and Stephylococcus.
Firmicutes may be the
first rod shaped bacteria, and first
bacteria to have a gram positive cell
wall.
The peptidoglycan layer is thicker in
Gram-positive bacteria (20 to 80 nm)
than in Gram-negative bacteria (7 to 8
nm)
Firmicultes form endospores, and is the
only phlyum of bacteria that evolved
the ability to build endospores.

 
[1] Listeria monocytogenes is a
Gram-positive bacterium, in the
division Firmicutes, named for Joseph
Lister. It is motile by means of
flagella. Some studies suggest that 1
to 10% of humans may carry L.
monocytogenes in their
intestines. Researchers have found L.
monocytogenes in at least 37 mammalian
species, both domesticated and feral,
as well as in at least 17 species of
birds and possibly in some species of
fish and shellfish. Laboratories can
isolate L. monocytogenes from soil,
silage, and other environmental
sources. L. monocytogenes is quite
hardy and resists the deleterious
effects of freezing, drying, and heat
remarkably well for a bacterium that
does not form spores. Most L.
monocytogenes are pathogenic to some
degree.
source: http://en.wikipedia.org/wiki/Ima
ge:Listeria.jpg


[2] These are bacteria (about 0.3 µm
in diameter) that do not have outer
walls, only cytoplasmic membranes.
However, they do have cytoskeletal
elements that give them a distinct
non-spherical shape. They look like
schmoos that are pulled along by their
heads. How they are able to glide is a
mystery.
source: http://webmac.rowland.org/labs/b
acteria/projects_glide.html

2,920,000,000 YBN
288) Eubacteria firmicutes evolve the
abililty to form endpospores.

 
[1] Spore forming inside a bacterium.
Stahly, MicrobeLibrary COPYRIGHTED
source: http://www.microbe.org/microbes/
spores.asp

2,800,000,000 YBN
177) Genetic comparison shows the
ancestor of all Proteobacteria
(Rickettsia {mitochondria}, gonorrhoea,
Salmonella, E coli) evolving now.

Proteobact
eria include 5 Classes:
CLASS Alpha
Proteobacteria (Rickettsia Prowazekii
{mitochondria/typhus})
CLASS Beta Proteobacteria (Neisseria
gonorrhoeae {gonorrhoea})
CLASS Gamma Proteobacteria
(Salmonella and Escherichia coli.)
CLASS Delta
Proteobacteria
CLASS Epsilon Proteobacteria

The Proteobacteria are a major group of
bacteria. They include a wide variety
of pathogens, such as Escherichia,
Salmonella, Vibrio, Helicobacter, and
many other notable genera. Others are
free-living, and include many of the
bacteria responsible for nitrogen
fixation. The group is defined
primarily in terms of ribosomal RNA
(rRNA) sequences, and is named for the
Greek god Proteus, who could change his
shape, because of the great diversity
of forms found in it.

All Proteobacteria are Gram-negative,
with an outer membrane mainly composed
of lipopolysaccharides. Many move about
using flagella, but some are non-motile
or rely on bacterial gliding. The last
include the myxobacteria, a unique
group of bacteria that can aggregate to
form multicellular fruiting bodies.
There is also a wide variety in the
types of metabolism. Most members are
facultatively or obligately anaerobic
and heterotrophic, but there are
numerous exceptions. A variety of
genera, which are not closely related,
can photosynthesize. These are called
purple bacteria, referring to their
mostly reddish pigmentation.

The delta-proteobacteria Myxobacteria
is capable of colonial multicellularity
and some view as possibly being the
bacteria that formed the cytoplasm in
eukaryotes.

 
[1] Figure 1. Transmission electron
micrograph of the ELB agent in XTC-2
cells. The rickettsia are free in the
cytoplasm and surrounded by an electron
transparent halo. Original
magnification X 30,000. CDC PD
source: www.cdc.gov/ncidod/
eid/vol7no1/raoultG1.htm


[2] Caulobacter crescentus. From
http://sunflower.bio.indiana.edu/~ybrun/
L305.html COPYRIGHTED EDU was in wiki
but appears to be removed
source: http://upload.wikimedia.org/wiki
pedia/en/4/42/Caulobacter.jpg

2,784,000,000 YBN
176) Genetic comparison shows
Eubacteria Phylum, Planctomycetes
(Planctobacteria) evolving now.

Planctomycet
es are a possible ancestor of all
eukaryotes because the circle of DNA
can sometimes be enclosed in a double
membrane.
Planctomycetes is a small phylum with
only 4 Genera, require oxygen for
growth (obligately aerobic), are found
in fresh and salt water. They reproduce
by budding. They have holdfast (stalk)
at the nonreproductive end that helps
them to attach to each other during
budding.

The life cycle involves alternation
between sessile cells and flagellated
swarmer cells. The sessile cells bud to
form the flagellated swarmer cells
which swim for a while before settling
down to attach and begin reproduction.

It is also possible, although unlikely,
that planctomycetes are descended from
a very early eukaryote that lost the
nucleus but retained the cytoplasmic
DNA, since budding may have evolved as
a method to duplicate a eukaryote cell
from the nucleus. (ok this is out
there...maybe t3)

 
[1] Electron micrographs of cells of
new Gemmata-like and Isosphaera-like
isolates. (A) Negatively stained cell
of the Gemmata-like strain JW11-2f5
showing crateriform structures
(arrowhead) and coccoid cell
morphology. Bar marker, 200 nm. (B)
Negatively stained budding cell of
Isosphaera-like strain CJuql1 showing
uniform crateriform structures
(arrowhead) on the mother cell and
coccoid cell morphology. Bar marker,
200 nm. (C) Thin section of
Gemmata-like cryosubstituted cell of
strain JW3-8s0 showing the
double-membrane-bounded nuclear body
(NB) and nucleoid (N) enclosed within
it. Bar marker, 200 nm. (D) Thin
section of Isosphaera-like strain C2-3
possessing a fibrillar nucleoid (N)
within a cytoplasmic compartment
bounded by a single membrane (M) only.
Bar marker, 200 nm. Appl Environ
Microbiol. 2002 January; 68(1):
417-422. doi:
10.1128/AEM.68.1.417-422.2002.
source: http://www.pubmedcentral.gov/art
iclerender.fcgi?tool=pubmed&pubmedid=117
72655


[2] Evolutionary distance tree
derived from comparative analysis of
16S rDNAs from freshwater and soil
isolates and reference strains of the
order Planctomycetales. Database
accession numbers are shown in
parentheses after species, strain, or
clone names. Bootstrap values of
greater than 70% from 100 bootstrap
resamplings from the distance analysis
are presented at nodes. Thermotoga
maritima was used as an outgroup.
Isolates from this study and
representative named species of the
planctomycetes are indicated in bold.
The scale bar represents 0.1 nucleotide
substitution per nucleotide
position. Appl Environ Microbiol.
2002 January; 68(1): 417-422. doi:
10.1128/AEM.68.1.417-422.2002.
source: http://florey.biosci.uq.edu.au/m
ypa/images/fuerst2.gif

2,784,000,000 YBN
179) Genetic comparison shows
Eubacteria Phylum, Actinobacteria (high
G+C, Gram positive) evolving now.

Actinobact
eria have 5 Orders:
ORDER Acidimicrobiales
ORDER
Actinobacteriales
ORDER Coriobacteriales
ORDER Rubrobacteriales
ORDER Sphaerobacteriales

Actinobacteria include the causes of
tuberculosis (Mycobacteria
tuberculosis) and leprosy (Mycobacteria
leprae).

The Actinobacteria or Actinomycetes are
a group of Gram-positive bacteria. Most
are found in the soil, and they include
some of the most common soil life,
playing an important role in
decomposition of organic materials,
such as cellulose and chitin. This
replenishes the supply of nutrients in
the soil and is an important part of
humus formation. Other Actinobacteria
inhabit plants and animals, including a
few pathogens, such as Mycobacterium.

 
[1] Frankia is a genus of
nitrogen-fixing soil bacteria, which
possesses a set of features that are
unique amongst symbiotic
nitrogen-fixing microorganisms,
including rhizobia, making it an
attractive taxon to study. These
heterotrophic Gram-positive bacteria
which are able to induce symbiotic
nitrogen-fixing root nodules
(actinorhizas) in a wide range of
dicotyledonous species (actinorhizal
plants), have also the capacity to fix
atmospheric nitrogen in culture and
under aerobic conditions.
source: http://www.ibmc.up.pt/webpagesgr
upos/cam/Frankia.htm


[2] Aerial mycelium and spore of
Streptomyces coelicolor. The mycelium
and the oval spores are about 1µm
wide, typical for bacteria and much
smaller than fungal hyphae and spores.
(Scanning electron micrograph, Mark
Buttner, Kim Findlay, John Innes
Centre). COPYRIGHT UK
source: http://www.sanger.ac.uk/Projects
/S_coelicolor/micro_image4.shtml

2,775,000,000 YBN
174) Genetic comparison shows
Eubacteria Phylum, Spirochaetes
(Syphilis, Lyme disease) evolving now.

Inclu
des leptospirosis (leptospira), Lyme
disease (Borrelia burgdorferi), and
Syphilis (Treponema pallidum).
Spirochaetes only
have one order:
ORDER Spirochaetales

This is when the first spiral shaped
bacteria evolve.

The spirochaetes (or spirochetes) are a
phylum of distinctive bacteria, which
have long, helically coiled cells. They
are distinguished by the presence of
flagella running lengthwise between the
cell membrane and cell wall, called
axial filaments. These cause a twisting
motion which allows the spirochaete to
move about. Most spirochaetes are
free-living and anaerobic, but there
are numerous exceptions.

 
[1] Syphilis is a complex, sexually
transmitted disease (STD) with a highly
variable clinical course. The disease
is caused by the bacterium, Treponema
pallidum. In the United States, 32,871
cases of syphilis, including 432 cases
of congenital syphilis, were detected
by public health officials in 2002.
Eight of the ten states with the
highest rates of syphilis are located
in the southern region of the United
States.
source: http://www.cdc.gov/nchstp/od/tus
kegee/syphilis.htm


[2] leptospirose 200x magnified with
dark-field microscope photo taken by
bluuurgh at the dutch royal tropical
institute (www.kit.nl) PD
source: http://uhavax.hartford.edu/bugl/
images/Treponema%20pallidum.jpg

2,775,000,000 YBN
175) Genetic comparison shows
Eubacteria Phyla Bacteroidetes and
Chlorobi (green sulphur bacteria)
evolving now.

PHYLUM Bacteroidetes
CLASS Bacteroides
ORDER
Bacteroidales
CLASS Flavobacteria
ORDER Flavobacteriales
CLASS
Sphingobacteria
ORDER Sphingobacteriales

PHLYUM Chlorobi (Green sulphur)
CLASS Chlorobia
ORDER
Chlorobiales


The phylum Bacteroidetes is composed of
three large groups of bacteria. By far,
more is written about and known about
the Bacteroides class, than the other
two, the Flavobacteria and the
Sphingobacteria classes. They are
related by the similarity in the
composition of the small 16S subunit of
their ribosomes. Members of the
bacteroides class are human commensals
(they benefit but humans receive no
effect) and sometimes pathogens.
Members of the other two classes are
rarely pathogenic to humans.

Chlorobi are the "green sulphur
bacteria", are a family of phototrophic
(photosynthesizing) bacteria. Green
sulfur bacteria are generally nonmotile
(one species has a flagellum), and come
in spheres, rods, and spirals. Their
environment must be oxygen-free, and
they need light to grow. They engage in
photosynthesis, using
bacteriochlorophylls c, d, and e in
vesicles called chlorosomes attached to
the membrane. They use sulfide ions as
electron donor, and in the process the
sulfide gets oxidized, producing
globules of elemental sulfur outside
the cell, which may then be further
oxidized. (By contrast, the
photosynthesis in plants uses water as
electron donor and produces oxygen.)

A species of green sulfur bacteria has
been found living near a black smoker
off the coast of Mexico at a depth of
2,500 meters beneath the surface of the
Pacific Ocean. At this depth, the
bacteria, designated GSB1, lives off
the dim glow of the thermal vent since
no sunlight can penetrate to that
depth.

 
[1] Bacteroides fragilis . From the
Zdravotni University
source: http://biology.kenyon.edu/Microb
ial_Biorealm/bacteria/bacteroidete_chlor
ob_group/bacteroides/bacteroides.htm


[2] Cross section of a Bacteroides
showing an outer membrane, a
peptidoglycan layer, and a cytoplasmic
membrane. From New-asthma
source: http://phil.cdc.gov/phil/details
.asp

2,775,000,000 YBN
217) Genetic comparison shows
Eubacteria Phyla Chlamydiae and
Verrucomicrobia evolving now.

Chlamydiae
includes (clamydia, trachoma {Chlamydia
trachomatis}, a form of pneumonia
{Chlamydophila pneumoniae}, psittacosis
{Chlamydophila psittaci}.

CLASS Chlamydiae
ORDER Chlamydiales

PHYLA Verrucomicrobia
ORDER Verrucomicrobiales

The Chlamydiae are a group of bacteria,
all of which are intracellular
parasites of eukaryotic cells. Most
described species infect mammals and
birds, but some have been found in
other hosts, such as amoebae.
Chlamydiae have a
life-cycle involving two distinct
forms. Infection takes place by means
of elementary bodies (EB), which are
metabolically inactive. These are taken
up within a cellular vacuole, where
they grow into larger reticulate bodies
(RB), which reproduce. Ultimately new
elementary bodies are produced and
expelled from the cell.

Verrucomicrobia is a recently described
phylum of bacteria. This phylum
contains only a few described species
(Verrucomicrobia spinosum, is an
example, the phylum is named after
this). The species identified have been
isolated from fresh water and soil
environments and human feces. A number
of as-yet uncultivated species have
been identified in association with
eukaryotic hosts including extrusive
explosive ectosymbionts of protists and
endosymbionts of nematodes residing in
their gametes.

Evidence suggests that verrucomicrobia
are abundant within the environment,
and important (especially to soil
cultures). This phylum is considered to
have two sister phyla Chlamydiae and
Lentisphaera.

 
[1] Chlamydia trachomatis wiki, is
copyrighted
source: http://en.wikipedia.org/wiki/Chl
amydia_trachomatis


[2] wiki, public domain
source: http://en.wikipedia.org/wiki/Ima
ge:Chlamydophila_pneumoniae.jpg

2,760,000,000 YBN
80) Endocytosis, a process where the
cell membrane folds around some
molecules to form a spherical vesicle
which enters the cytoplasm, and
exocytosis, the opposite process, where
a vesicle combines with a call membrane
to empty molecules outside a cell both
evolve in an early eukaryote cell.

Eukaryote cells can now swallow
bacteria (phagocytosis) and liquid
(pinocytosis). The cells can then
(heterotrophically) use the molecules
injested (for example a bacterium) for
copying and to make ATP. This is the
first time one cell can eat a different
living cell.

How similar endocytosis is to
conjugation is unknown at this time.

 
[1] Pinocytosis In the process of
pinocytosis the plasma membrane froms
an invagination. What ever substance
is found within the area of
invagination is brought into the
cell. In general this material will
be dissolved in water and thus this
process is also refered to as
''cellular drinking'' to indicate that
liquids and material dissolved in
liquids are ingested by the
cell. This is opposed to the
ingestion of large particulate material
like bacteria or other cells or cell
debris.
source: http://academic.brooklyn.cuny.ed
u/biology/bio4fv/page/endocytb.htm

2,750,000,000 YBN
207) Cytoskeleton evolves in eukaryote
cytoplasm.

One theory is that the cytoskeleton
formed from the eukaryote flagella
(cilia, undulipodia) tubules.
Cytoskeleton is a
single body with the endoplasmic
reticulum and nuclear membrane?

  
2,725,000,000 YBN
60) First eukaryotic cell evolves.
This cell has a nucleus, with either
single strands or a circle of DNA
inside. This is a single anaerobic
cell. This is the first protist.

This cell evolves either by:
1) two or more
bacteria joined, one with flagella
(perhaps a eubacteria) formed the
nucleus, a second formed the cytoplasm
outside the nucleus, eventually the
code to build the entire cell including
the instructions to build the symbiotic
captured bacteria was included in the
new nucleus,
2) the nucleus formed as
part of the cytoplasm lattice, perhaps
the outer wall folded in on itself
creating a double membrane, or a
membrane grew around the DNA (for
example like planctobacteria) which
provided more protection for the DNA
from the movement and digestive
activities of cytoplasm now without a
rigid cell wall,
3) a bacteria with
flagella that grew cytoplasm and a
secondary cell wall outside the
original cell wall,
4) a virus,
5) a
DNA strand from conjugation with a
different prokaryote stored in a
vesicle.

There are key features that are
different from eukaryotes and
prokaryotes:
1) Eukaryotes have a nucleus,
prokaryotes do not.
2) DNA in eukaryotes is
in the form of chromosomes, in
prokaryotes the DNA is in a circle.
3)
Eukaryotes can do endocytosis, fold
their cell membrane around some
external object and injest the object,
prokaryotes can not.
4) Eukaryotes have a
membrane lattice of proteins, actin and
myacin, prokaryotes do not.
5) Eukaryotes
have an endoplasmic reticulum and golgi
body.
6) Eukaryotes reproduce asexually by
dual binary division (both nucleus and
cell divide by binary division),
budding, or mitosis, prokaryotes
reproduce by budding or binary
division.

If the nucleus is an engulfed
prokaryote, this cell inherits the
processes of nuclear DNA duplication
and nucleus division (karyokinesis)
from prokaryote binary division.
Initially, both the nucleus and cell
divide by binary division.

Support for the
nucleus forming from a prokaryote is
that chromosomes in parabasalia and
dinoflagellates remain permanently
anchored to the nuclear membrane
(envelope?) by the kinetochores, the
same way prokaryote DNA anchors to the
cell membrane (wall?) during cell
division.

A theory of an archaebacteria (perhaps
an eocyte) forming the first eukaryote
nucleus and a gram-negative eubacteria
forming the cytoplasm of the first
eukaryote is supported by genetic
evidence.

This cell reproduces asexually by
either binary fission (both nucleus and
cytoplasm) or budding, or sexually by
conjugation or both cell and nuclei
fully merging.

If this cell has chromosomes, this is
the first (haploid) organism with
chromosomes.

Perhaps a sperm-like flagellated
prokaryote merged with an ovum-like
prokaryote from the same or a different
species, perhaps by the ovum opening a
pilus and the sperm-like cell entering
the pilus, and once inside opening a
pilus through which the DNA from the
two cells could merge. Many
diplomonads look like sperm cells stuck
in an ovum, with the still flagellated
sperm forming the nucleus, and some
diplomonads, for example, the oxymonad,
Saccinobaculus reproduce sexually.

An important evolutionary step had to
evolve here, and that is the evolution
of the prokaryote binary division
system: 1) duplicating DNA in the
cytoplasm, 2) separating the two copies
of DNA, and 3) the division of
cytoplasm into two cells to an adapted
process of eukaryote cell division: 1)
duplicating DNA in the nucleus, 2)
separating the DNA in the nucleus, 3)
dividing the nucleus into two nuclei,
4) separating the two nuclei, and then
5) dividing the cytoplasm into two
cells.

It appears in early eukaryote nuclei
(as seen in closed mitosis, where the
nuclear membrane persistes through
mitosis) that the nuclei divide by a
process similar to binary division (as
opposed to budding), which adds to the
support for the first nucleus being a
prokaryote and continuing to divide by
binary division.

Most people accept that the centrioles
from which grow the microtubule
spindles that pull apart chromosomes in
mitosis, evolved from the base pairs
which originally were, and on some
species still are, connected to a
cilium.

Perhaps there are some eukaryote nuclei
that duplicate by budding, although
this has never been found to my
knowledge. If ever found, that would
imply that budding evolved before the
first eukaryote, but could have
possibly evolved after by simply
dropping the instructions to copy
anything other than the nucleus.
Binary cell division in the most basic
form only synthesizes more cytoplasm
and cell wall, where budding reproduces
the entire body plan of a cell (or
nucleus in this case).

 
[1]
http://www.regx.de/m_organisms.php#planc
to
source: http://www.regx.de/m_organisms.p
hp#plancto


[2]
http://www.mansfield.ohio-state.edu/~sab
edon/biol1080.htm
source: http://www.mansfield.ohio-state.
edu/~sabedon/biol1080.htm

2,725,000,000 YBN
65) DNA in the nucleus changes from a
single circular chromosome to linear
chromosomes.

Possibly the prokaryote ancestor of the
first eukaryote had linear chromosomes
since some prokaryotes (although very
few) are known to have linear
chromosomes instead of or in addition
to a single circular chromosome.

Perhaps a DNA
strand entered a cell by conjugation,
the circle of DNA was cut to insert the
new DNA (plasmid), but the new DNA
strand was not sewn back into the
original strand of DNA creating two
strands of DNA which eventually evolved
into the first 2 chromosomes.

Perhaps the first eukaryote nucleus was
a virus, many of which have linear
chromosomes.

This includes the evolution of
histones, proteins which are packed in
between nucleotides in each
chromosome.

Presumably DNA duplication (sythesis)
of chromosomes (in the nucleus) is
initially identical to DNA duplication
of DNA strands or circular DNA.

Some prokaryotes do not have just one
circle of DNA. Brucella melitensis
has 2 circlular chromosomes.
Agrobacterium tumefaciens has a
circular and a linear chromosome.
Streptomyces griseus can have one
linear chromosome. Borrelia
burgdorferi contains a linear
chromosome and a number of variable
circular and linear plasmids. Most
eukaryote orgenelles have a single
circular chromosome except for the
mitochondria of most cnidarians and
some other forms which have linear
chromosomes.

  
2,720,000,000 YBN
208) A eukaryote flagellum (cilium,
undulipodium) evolves on early single
cell eukaryotes.

The eukaryote cilia (flagella,
undulipodia) may evolve from a
prokaryote flagella connected to the
nucleus, from the cytoskeleten, or a
symbiotic prokaryote.

Cilia and eukaryote flagella are
structurally the same, but have minor
functional differences. Cilia are a
special class of eukaryote flagella.
The
eukarote flagellum is different from
prokayote flagellum. The prokaryote
flagallum is a solid structures, made
of the protein flagellin, which
protrudes through the plasma membrane.

The eukaryote flagellum (and cilium)
contains a "9 plus 2 array", 9
microtubules in a circle with 2
microtubules in the center. Some
people think that the eukaryote
flagella and cilia should be called
"undulipodia".

In some species the spindles used in
mitosis connect to the bases of the
eukaryote cilia (undulipodia), which
leads some people to think that the
spindles of mitosis may have evolved
from the eukaryote cilia.

Some people think that the eukaryote
cilium (flagellum, undulipodia) was a
spirochete (prokaryote) that formed a
symbiotic relationship with a eukaryote
host, whose DNA was transfered to the
host nucleus. Other possibilities are
that the eukaryote flagellum evolved
from prokaryote flagellum, or simply
evolved over time through natural
selection.

The eukaryote flagellum protein
"tubulin" is thought to be related to a
bacterial replication/cytoskeletal
protein "FtsZ" found in some
archaebacteria (archaea).

What method of reproduction this first
nucleated cell used is a great mystery.
Among the choices are binary division,
budding, or mitosis. My own feeling is
that budding or dual binary division
(both nucleus and cytoplasm) was how
this cell initially copied.



  
2,720,000,000 YBN
291) For the first time, a cell is not
constantly synthesizing DNA and then
having a division period (as is the
case for all known prokaryotes), but
this cell has a period in between cell
division and DNA synthesis where DNA
synthesis is not performed. Later some
cells develop a stage after synthesis
and before cell division.

For the first time, a
cell is not constantly synthesizing DNA
(S) and then having a division period
(D) (as is the case for all known
prokaryotes), but this cell has a
period in between cell division and DNA
synthesis where DNA synthesis is not
performed (G1) . Later some cells
develop a stage after synthesis and
before cell division (G2).

  
2,719,000,000 YBN
302) If the first eukaryote nucleus was
a prokaryote, synchronized duplication
and division of organelle-nucleus and
cytoplasm of early eukaryote cell
evolves. Before this, eukaryote cell
division usually results in one cell
with no organelle-nuclei and a second
cell with 2 organelle-nuclei. Perhaps
the organelle-nuclei attach to the
outer cell membrane in the same way the
cytoplasmic DNA do, which allows new
cytoplasm growth to separate the two
organelle-nucleus in addition to the
cytoplasmic DNA.

Or perhaps the first
system of organized nuclei separation
originated with the organelle-nucleus
flagella microtubules grewing into the
cytoskeleton, and organized system
spindles and mitosis.

If the nuclear membrane was formed
around the DNA within a prokaryote,
then binary division had to adapt to
separate the duplicated DNA within the
proto-nucleus (not within the entire
cell) which may have been very simple
to evolve. If the cytoplasm grew
outside the cell wall of a prokaryote,
binary division would have to adapt to
separate that external cytoplasm.

 

source:



source:

2,715,000,000 YBN
72) Mitosis, asexual copying of a
haploid (single set of chomosomes)
eukaryote nucleus, evolves in
eukaryotes. Before mitosis, there is a
synthesis stage where DNA in the form
of chromosomes are duplicated in the
nucleus before the nucleus and cell
divide.

explain basic process of mitosis:
prophase,
metaphase, anaphase, telophase

Presumably no prokaryotes have ever
reproduced through mitosis. Only
eukaryotes reproduce asexually using
mitosis.

Most people accept that some protists
were sexual and later lost that
ability. But the majority view now is
that the first eukaryotes were asexual,
and that some protists still living now
have never had sexual ability.

Because mitosis is complex and similar
in detail in all species that do
mitosis, people think that mitosis only
evolved once, and was inherited by all
species that do mitosis.

The major differences between this new
method of copying, mitosis and the
older method, binary fission (add
budding?) are:
1) In mitosis, microtubule
spindles attach to the kinetochore (the
protein structure in eukaryotes which
assembles on the centromere and links
the chromosome to microtubule polymers
from the mitotic spindle during
mitosis) and pull apart the two DNA
copies, where in binary fission the DNA
(single chromosome) attaches to a part
of the cytoplasm which pulls apart the
two cells.
2) Chromosomes (linear pieces of
DNA), not a circle of DNA is being
copied.

People speculate that early mitosis had
spindles outside the nucleus, with
chromosomes fastened to the nuclear
membrane, as can still be seen in
parabasalia and dinoflagellates, which
appear to have primitive nuclei.

In more ancient species the nuclear
membrane persists through mitosis
(closed mitosis), but in more recent
species, like metazoa, land plants, and
many kinds of protists, the nuclear
membrane disintegrates before mitosis
and is rebuilt after (open mitosis).

Most people think that extranuclear
spindles (spindles that originate
outside of the nucleus) and closed
mitosis evolved first. Only later did
pleuromitosis (spindles rotate 90
degrees, nucleus can be semi-open, or
closed) and then orthomitosis (spindles
are on both sides of nucleus and
separate chromosomes in a straight
line, nucleus can be open, semi-open or
closed) evolve in later eukaryotes.

 
[1] Mitosis divides genetic information
during cell division Source:
http://www.ncbi.nlm.nih.gov/About/primer
/genetics_cell.html This image is
from the Science Primer, a work of the
National Center for Biotechnology
Information, part of the National
Institutes of Health. As a work of the
U.S. federal government, the image is
in the public domain.
source: http://en.wikipedia.org/wiki/Mit
osis


[2] Prophase: The two round objects
above the nucleus are the centrosomes.
Note the condensed chromatin. from
Gray's Anatomy. Unless stated
otherwise, it is from the online
edition of the 20th U.S. edition of
Gray's Anatomy of the Human Body,
originally published in 1918. Online
editions can be found on Bartleby and
also on Yahoo!
source:

2,711,000,000 YBN
303) Cytoplasmic cell fusion and
division evolves. Two eukaryote cells
can merge into one cell with 2 nuclei
and then divide back into single 1
nucleus cells.



  
2,710,000,000 YBN
73) Sex (cell and genetic fusion,
syngamy, gametogamy) evolves in
protists. Haploid (1 set of
chromosomes) eukaryote cells merge and
then their nuclei merge (karyogamy) to
form the first diploid (2 sets of
chromosomes) cells (the first zygote).

This fusion of 2 haploid cells results
in the first diploid single-celled
organism, which then immediately
divides (both nucleus and cytoplasm by
single-division meiosis) back to two
haploid cells.

Possibly first, only cytoplasmic
merging happened with nuclear merging
(karyogamy) and nuclear division
(karyokinesis) evolving later.
Now, two cells
with different DNA can mix providing
more chance of variety/mutation. Two
chromosome sets provides a backup copy
of important genes (sequences that code
for proteins, or nucleic acids) that
might be lost with only a set of single
chromosomes.

The life cycle of future organisms will
now have two phases, a gamophase (from
n to 2n (until syngamy)), and zygophase
(from 2n to n (until meiosis)). Gamoid
cells are not haploid in polyploid
organisms.

Potentially sexual cell and genetic
fusion is what made the first eukaryote
cell, and sex in protists may be
directly descended from conjugation in
prokaryotes, in other words not evolved
from a different method independently
of conjugation, because some
metamonads, for example Saccinobaculus
reproduce sexually, and look very much
like a prokaryote sperm cell which
formed the nucleus captured in an ovum
cell.

For sexual species there are 3 basic
life cycles:
1) Haploid (Haplontic) life cycle:
zygotic meiosis. Life as haploid
cells, cell division immediately after
creation of zygote from fusion. (All
fungi, Some green algae, Many
protozoa)
2) Diploid (Diplontic) life cycle:
gametic meiosis. Instead of immediate
cell division, zygote reproduces by
mitosis. Haploid gametes never copy by
mitosis. (animals, some brown algae)
3)
Haplodiploid (Haplodiplontic,
Diplohaplontic, Diplobiontic) life
cycle: sporic meiosis. Diploid cell
(sporocyte) meiosis results in 2
haploid sporophytes (gamonts), not 2
haploid gametes. These haploid cells
then differentiate? or mitosis? to form
haploid gametes. Haplodiplontic
organisms have alternation of
generations, one generation involves
diploid spore-producing single or
multicellular sporophytes (makes
spores) and the other generation
involves haploid single or
multicellular gamete-producing
multicellular gametophytes (makes
gametes). Pants and many algae have
this haplodiplontic life cycle.

These first sexual cells are haplontic,
with zygotic meiosis; they reproduce
asexually through mitosis as haploid
cells, fusing to a diploid cell without
mitosis, then dividing back into
haploid cells.

An important evolutionary step evolves
here in that now two cells can
completely merge into one cell. This
merge not only includes their nuclei,
but also their cytoplasm (althought the
DNA do not merge). Before now, as far
as has ever been observed, no two cells
have ever completely merged, although,
through conjugation some prokaryotes
have been observed to exchange DNA.

This marks the beginning of the
"haplonic lifestyle" with "zygotic
meosis", where the organism is haploid
until cell fusion which is immediately
followed by (one-step) meiosis of the
zygote, after which the haploid cells
continues to reproduce through
mitosis.

Possibly the first sexual organism
merged through a form of "autogamy"
(both haploid gametes originate from
the same individual, the opposite of
"allogamy" where the gametes originate
from different individuals). Some
species reproduce by a form of autogamy
(intracellular autogamy), where nuclei
(also called pronuclei) divide and then
merge within the same cell before the
entire cell divides. Some metamonads
(earliest still living eukaryotes),
like Oxymonas and Saccinobaculus can
reproduce asexually by mitosis, but
also can reproduce sexually using this
form of autogamy. This may be evidence
that some prokaryote could also merge
two entire cells (if the eukaryote
nucleus was a prokaryote). Perhaps
prokaryotes evolved full cellular
fusion before the first eukaryote. If
that is true, then this initial form of
nuclei dividing and merging
(intracellular autogamy) may have
existed for some time before full
eukaryote cell merging and synchronized
eukayote nucleus and cytoplasm division
evolved. It is difficult to see what
selective advantage autogamy could
possibly have since no new DNA is ever
introduced into the next generation of
organism, as opposed to "allogamy",
where DNA from different individuals is
merged, and which has a clear selective
advantage. So perhaps autogamy evolved
after allogamy, although to me it
appears that allogamy is more complex
than autogamy, and autogamy would be a
perfect starting step to develop the
needed proteins and processes for the
more complicated allogamy (autogamy
only involves the duplication and
merging of two nuclei, where allogamy
involves the merging of the cell walls,
and cytoplasm in addition to the two
nuclei.)

This is the beginning of the label
"gamete" for haploid cells that can
merge to form a diploid zygote. In
addition, the label "gametocyte" or
"gamont" is any polyploid cell that
divides (meiosis) into haploid gamete
cells which can merge to form a zygote.

 
[1] Zygotic Meiosis. GNU
source: http://en.wikipedia.org/wiki/Ima
ge:Zygotic_meiosis.png


[2] Gametic Meiosis. GNU
source: http://en.wikipedia.org/wiki/Ima
ge:Gametic_meiosis.png

2,710,000,000 YBN
206) Meiosis (one-step meiosis, one DNA
duplication and a cell division of a
diploid cell into 2 haploid cells)
evolves.

detail one-step meiosis:

The is no DNA crossover or chiasma
formation in one-division meiosis,
apparently because either duplication
of chromosomes or separation of
chromatids does not occurred.

As far as I know, mitosis and one-step
meiosis are the same with the only
exceptions that 1) in meiosis two
haploid cells join before cell
division, and 2) in mitosis the DNA is
duplicated before cell division, but in
meiosis the DNA is not duplicated
before cell division.

Meiosis can be one step (one DNA
duplication and then one cell division)
or two step (two DNA duplications and
then two divisions). Probably one step
meosis evolved first and two step
meiosis later.

Meiosis can only function on cells with
two or more sets of chromosomes.

 
[1] GametoGenesis. COPYRIGHTED EDU
source: http://www.bio.miami.edu/dana/10
4/gametogenesis.jpg


[2] Sexual cycle oxymonas, identical
to saccinobaculus, one step meiosis.
haploid. COPYRIGHTED CANADA
source: http://www.zoology.ubc.ca/~redfi
eld/clevelan/oxymonas.GIF

2,706,000,000 YBN
299) Duplication of diploid DNA (after
2 haploid cells fuse) evolves.

This is required
for diploid mitosis.

Duplication of diploid DNA may be very
similar to duplication of haploid DNA.

Initially perhaps the diploid DNA
duplicated, but still divided in
one-division meiosis.



  
2,705,000,000 YBN
210) Mitosis of diploid cells evolves.
This begins the "diplontic" life cycle
(with gametic meiosis), where diploid
cells (a zygote) can copy asexually
through mitosis after merging. This
organism, when haploid, cannot do
mitosis (presumably haploid gamete
mitosis will evolve much later in brown
algae), and this is still true in all
descendents (including humans) of this
single celled organism.

The proteins and
mechanism of mitosis of diploid cells
is probably very similar to mitosis of
haploid cells. The most primitive
organisms still alive that are
diplontic are the metamonads (e.g.
Oxymonads: Notila, Hypermastigotes:
Urinympha, Macrospironympha,
Rhynchonympha).



  
2,704,000,000 YBN
296) The origin of gender evolves: sex
(cell and nucleus fusion) between two
isogamous (same size) gametes but which
have 2 different (+ and -) forms
(genders).

Perhaps the invention of two different
genders originated when a flagellated
cell (or nucleus) divided by binary
division and only one half of the two
new cells retained the flagellum. Then
to differentiate the two cells even
more, but still keep the same DNA
template, different proteins could be
weighted on one half of the cell during
division to activate various operons in
one gender but not the other once the
two DNA pairs are separated.

Perhaps sex where the gametes are the
same size but cannot merge themselves
should be called "specific" or
"gendered" isogamy, and where any two
same sized gametes can merge called
"nonspecific" or "nongendered" isogamy.

  
2,703,000,000 YBN
297) Sex (cell and nucleus fusion)
between two different size gamete cells
(heterogamy or anisogamy) evolves in
protists.

Some species are heterogamous but two
of the same sized (gender) gametes can
fuse to form a zygote.

  
2,702,000,000 YBN
298) Sex (cell and nucleus fusion)
between one flagellated gamete and an
unflagellated gamete (oogamy, a form of
heterogamy) evolves in protists.

  
2,700,000,000 YBN
62) Oldest steranes (formed from
sterols, molecules made by mitochondria
in eukaryotes) found in northwestern
Australia.


  
2,700,000,000 YBN
192) Fossils from the Bulawaya
stromatolite, Zimbabwe.

 
[1] Fig. 2. Organic microstructure from
the Bulawaya stromatolite, Zimbabwe (ca
2.7 Ga). (a) TEM-micrograph from
demineralized rock section. (b) Laser
mass spectrum from individual specimen
of the same population (negative ions).
Field of measurement ca 1 small mu,
Greekm diameter. Attribution of
signals: 12: C−, 13: CH−,
14: CH−2, 16: O−, 17:
OH−, 19: F−, 24: C−2,
25: C2H−, 26: CN−, 28:
Si−, 36: C−3, 37:
C3H−, 40-42, 45: fragmental
carbonaceous groups, 48: C−4, 49:
C4H−, 50: C4H−2, 60:
SiO−2, resp. C−5, 61:
C5H−.
source: http://www.sciencedirect.com/sci
ence?_ob=MiamiCaptionURL&_method=retriev
e&_udi=B6VBP-42G6M5T-7&_image=fig5&_ba=5
&_user=4422&_coverDate=02%2F01%2F2001&_f
mt=full&_orig=browse&_cdi=5932&view=c&_a
cct=C000059600&_version=1&_urlVersion=0&
_userid=4422&md5=d9195635e48bcf1f817c009
69102189f

2,700,000,000 YBN
214) Biomarkers characteristic of
cyanobacteria, 2alpha -methylhopanes,
indicate that oxygenic photosynthesis
evolved well before the atmosphere
became oxidizing.

  
2,692,000,000 YBN
300) Diploid cell fusion (Gamontogamy)
evolves.

Only a few species exhibit this
property (e.g. the Oxymonad Notilla,
Diatoms, Dasicladales {Acetabularia},
in many foraminiferans, and in
gregarines).

Gamontogamy may have evolved into
two-step meiosis.

The vast majority of eukaryotes living
now that reproduce sexually fuse
haploid cells. All "gametes" are
haploid cells that can merge, diploid
cells that can merge are gamonts.
Gamonts (Meiocytes) are cells that
produce gametes.

In theory this should be very similar
if not exactly like haploid cell
fusion, so perhaps this is not a major
evolutionary step.

 
[1] The Oxymonad, Notila (diploid
Pacific form) life cycle. COPYRIGHTED
source: http://www.zoology.ubc.ca/~redfi
eld/clevelan/notila.GIF

2,690,000,000 YBN
295) Meiosis (two step meiosis, two
cell divisions with no stage in between
which result in one diplid cell
dividing into four haploid cells)
evolves.

Meiosis and mitosis are similar in
being process of nucleus and cell
division, but are different.
Differenc
es between meiosis and mitosis:
1) At least one
crossover per homologous pair happens
in 2 step meiosis but crossover usually
does not happen in mitosis.
2) Two step meiosis
involves cell divisions that happen one
after the other, where mitosis only
happens after one DNA duplication
(there are never 2 mitoses together
without a DNA duplication between them
to my knowledge).

The cell division in two step meiosis
that involves a separation of sister
chromatids (not homologous chromosome
pairs) is basically identical to
mitosis. For two step meiosis, this is
the second nucleus and cell division.

 
[1] GametoGenesis. COPYRIGHTED EDU
source: http://www.bio.miami.edu/dana/10
4/gametogenesis.jpg


[2] Sexual cycle oxymonas, identical
to saccinobaculus, one step meiosis.
haploid. COPYRIGHTED CANADA
source: http://www.zoology.ubc.ca/~redfi
eld/clevelan/oxymonas.GIF

2,650,000,000 YBN
170) First bacteria live on land.

  
2,558,000,000 YBN
171) Phylum Deinococcus-Thermus
(Thermus Aquaticus {used in PCR},
Deinococcus radiodurans {can survive
long exposure to radiation}) evolve
now.

PHYLUM Deinococcus-Thermus
CLASS Deinococci
ORDER Deinococcales
ORDER
Thermales

The Deinococcus-Thermus are a small
group of bacteria comprised of cocci
highly resistant to environmental
hazards. There are two main groups. The
Deinococcales include a single genus,
Deinococcus, with several species that
are resistant to radiation; they have
become famous for their ability to eat
nuclear waste and other toxic
materials, survive in the vacuum of
space and survive extremes of heat and
cold. The Thermales include several
genera resistant to heat. Thermus
aquaticus was important in the
development of the polymerase chain
reaction where repeated cycles of
heating DNA to near boiling make it
advantageous to use a thermo-stable DNA
polymerase enzyme. These bacteria have
thick cell walls that give them
gram-positive stains, but they include
a second membrane and so are closer in
structure to those of gram-negative
bacteria.

 
[1] D. radiodurans growing on a
nutrient agar plate. The red color is
due to carotenoid pigment. Links to
816x711-pixel, 351KB JPG. Credit: M.
Daly, Uniformed Services University of
the Health Sciences NASA
source: http://science.nasa.gov/newhome/
headlines/images/conan/D_rad_dish.jpg


[2] Photomicrograph of Deinococcus
radiodurans, from
www.ornl.gov/ORNLReview/ v34 The Oak
Ridge National Laboratory United
States Federal Government This work
is in the public domain because it is a
work of the United States Federal
Government. This applies worldwide. See
Copyright.
source: http://en.wikipedia.org/wiki/Ima
ge:Deinococcus.jpg

2,558,000,000 YBN
172) Genetic comparison shows
Eubacteria phylum, Cyanobacteria
(ancestor of all eukaryote chloroplasts
{plastids}) evolving now. There is a
conflict between the interpretation of
the geological and the genetic evidence
as to if oxygen photosynthesis and
cyanobacteria evolved earlier around
3800mybn or here at 2500mybn.

Cyanobacteria get
their energy from photosythesis.

Cyanobacteria include unicellular,
colonial, and filamentous forms. Some
filamentous cyanophytes form
differentiated cells, called
heterocysts, that are specialized for
nitrogen fixation, and resting or spore
cells called akinetes. Each individual
cell typically has a thick, gelatinous
cell wall, which stains gram-negative.
The cyanophytes lack flagella, but may
move about by gliding along surfaces.
Most are found in fresh water, while
others are marine, occur in damp soil,
or even temporarily moistened rocks in
deserts. A few are endosymbionts in
lichens, plants, various protists, or
sponges and provide energy for the
host.

Chloroplasts found in eukaryotes (algae
and higher plants) most likely
represent reduced endosymbiotic
cyanobacteria. This endosymbiotic
theory is supported by various
structural and genetic similarities.
Primary chloroplasts are found among
the green plants, where they contain
chlorophyll b, and among the red algae
and glaucophytes, where they contain
phycobilins. It now appears that these
chloroplasts probably had a single
origin. Other algae likely took their
chloroplasts from these forms by
secondary endosymbiosis or ingestion.

tenative:
CLASS Chroobacteria
CLASS Hormogoneae
CLASS
Gloeobacteria

 
[1] Oscillatoria COPYRIGHTED EDU
source: http://www.stcsc.edu/ecology/alg
ae/oscillatoria.jpg


[2] Lyngbya COPYRIGHTED EDU
source: http://www.stanford.edu/~bohanna
n/Media/LYNGB5.jpg

2,558,000,000 YBN
315) Phylum Chloroflexi, (Green
Non-Sulphur) evolve now.

PHYLUM Chloroflexi

CLASS Chloroflexi
CLASS Thermomicrobia

The Chloroflexi are a group of bacteria
that produce ATP through
photosynthesis. They make up the bulk
of the green non-sulfur bacteria,
though some are classified separately
in the Phylum Thermomicrobia. They are
named for their green pigment, usually
found in photosynthetic bodies called
chlorosomes.

Chloroflexi are typically filamentous,
and can move about through bacterial
gliding. They are facultatively
aerobic, but do not produce oxygen
during photosynthesis, and have a
different method of carbon fixation
than other photosynthetic bacteria.
Phylogenetic trees indicate that they
had a separate origin.

 
[1] Chloroflexus photomicrograph from
Doe Joint Genome Institute of US Dept
Energy PD
source: http://en.wikipedia.org/wiki/Ima
ge:Chlorofl.jpg

2,500,000,000 YBN
52) End Archean Era, Start Proterozoic
Era.


  
2,500,000,000 YBN
56) Banded Iron Formations start to
appear in many places.


  
2,400,000,000 YBN
59) Very large ice age that lasts 200
million years starts now.


  
2,335,000,000 YBN
290) The nucleolus, a sphere in the
nucleus that makes ribosomes, evolves.

In some
eukaryotes (thought to be more
ancient), the nucleolus just divides
during mitosis, but in other eukaryotes
the mitosis is dissolved and rebuilt
after nuclear division.

In euglenids, kinetoplastids,
dinoflagellates, some amoebae and some
coccidians, the nucleolus remains
visible throughout mitosis and divides
into two, but in the majority of groups
the nucleolus dissapears and reforms at
telophase. That the nucleolus can
divide by itself suggests that it was
once a free living cell.

 
[1] Nucleolus, COPYRIGHTED
source: http://www.eccentrix.com/members
/chempics/Slike/cell/Nucleolus.jpg


[2] With the combination of x-rays
from the Advanced Light Source and a
new protein-labeling technique,
scientists can see the distribution of
the nucleoli within the nucleus of a
mammary epithelial cell. USG PD
source: http://www.lbl.gov/Science-Artic
les/Archive/xray-inside-cells.html

2,330,000,000 YBN
198) Rough and smooth endoplasmic
reticulum evolves in eukaryote cell.

Rough
and smooth endoplasmic reticulum
evolves in eukaryote cell.

The rough ER manufactures and
transports proteins destined for
membranes and secretion. It synthesizes
membrane, organellar, and excreted
proteins. Minutes after proteins are
synthesized most of them leave to the
Golgi apparatus within vesicles. The
rough ER also modifies, folds, and
controls the quality of proteins.

The smooth ER has functions in several
metabolic processes. It takes part in
the synthesis of various lipids (e.g.,
for building membranes such as
phospholipids), fatty acids and
steroids (e.g., hormones), and also
plays an important role in carbohydrate
metabolism, detoxification of the cell
(enzymes in the smooth ER detoxify
chemicals), and calcium storage. It
also is a large transporter of nutrient
found in each cell.



 
[1] Figure 1 : Image of nucleus,
endoplasmic reticulum and Golgi
apparatus. (1) Nucleus. (2) Nuclear
pore. (3) Rough endoplasmic reticulum
(RER). (4) Smooth endoplasmic reticulum
(SER). (5) Ribosome on the rough ER.
(6) Proteins that are transported. (7)
Transport vesicle. (8) Golgi apparatus.
(9) Cis face of the Golgi apparatus.
(10) Trans face of the Golgi apparatus.
(11) Cisternae of the Golgi
apparatus. I am the copyright holder
of that image (I might even have the
CorelDraw file around somewhere:-), and
I hereby place the image and all
partial images created from it in the
public domain. So, you are free to use
it any way you like. In fact, I am
delighted that one of my drawings makes
it into print! I can mail you the
.cdr file, if you like (and if I can
find it), if you need a better
resolution for printing. Yours, Magnus
Manske Source: [1]. See also
User:Magnus Manske
source: http://en.wikipedia.org/wiki/Ima
ge:Nucleus_ER_golgi.jpg

2,325,000,000 YBN
199) Golgi Body (Golgi Apparatus,
dictyosome) evolves in eukaryote cell.

The
primary function of the Golgi apparatus
is to process proteins targeted to the
plasma membrane, lysosomes or
endosomes, and those that will be
formed from the cell, and sort them
within vesicles. It functions as a
central delivery system for the cell.

Most of the transport vesicles that
leave the endoplasmic reticulum (ER),
specifically rough ER, are transported
to the Golgi apparatus, where they are
modified, sorted, and shipped towards
their final destination. The Golgi
apparatus is present in most eukaryotic
cells, but tends to be more prominent
where there are many substances, such
as proteins, being secreted. For
example, plasma B cells, the
antibody-secreting cells of the immune
system, have prominent Golgi complexes.



 
[1] Figure 1: Image of nucleus,
endoplasmic reticulum and Golgi
apparatus: (1) Nucleus, (2) Nuclear
pore, (3) Rough endoplasmic reticulum
(RER), (4) Smooth endoplasmic reticulum
(SER), (5) Ribosome on the rough ER,
(6) Proteins that are transported, (7)
Transport vesicle, (8) Golgi apparatus,
(9) Cis face of the Golgi apparatus,
(10) Trans face of the Golgi apparatus,
(11) Cisternae of the Golgi apparatus,
(12) Secretory vesicle, (13) Plasma
membrane, (14) Exocytosis, (15)
Cytoplasm, (16) Extracellular space.
source: http://en.wikipedia.org/wiki/Ima
ge:Nucleus_ER_golgi_ex.jpg

2,310,000,000 YBN
200) The golgi body in eukaryote cells
makes lysosomes which fuse with
endosomes. The various molecules in
lysosomes digest the contents of the
endosome, which then exits the cell as
waste.




 
[1] Figure 1: Image of nucleus,
endoplasmic reticulum and Golgi
apparatus: (1) Nucleus, (2) Nuclear
pore, (3) Rough endoplasmic reticulum
(RER), (4) Smooth endoplasmic reticulum
(SER), (5) Ribosome on the rough ER,
(6) Proteins that are transported, (7)
Transport vesicle, (8) Golgi apparatus,
(9) Cis face of the Golgi apparatus,
(10) Trans face of the Golgi apparatus,
(11) Cisternae of the Golgi apparatus,
(12) Secretory vesicle, (13) Plasma
membrane, (14) Exocytosis, (15)
Cytoplasm, (16) Extracellular space.
source: http://sun.menloschool.org/~cwea
ver/cells/e/lysosomes/



source: http://en.wikipedia.org/wiki/Ima
ge:Nucleus_ER_golgi_ex.jpg

2,305,000,000 YBN
63) A parasitic bacterium, a bacterium
that can only live in other bacteria,
closely related to Rickettsia
prowazekii, an aerobic
alpha-proteobacteria that causes
louse-borne typhus, enters an early
eukaryote cell. As time continues a
symbiotic relationship evolves, where
the Rickettsia forms the mitochondria,
organelles of every euokaryote cell.
The mitochondria perform the Acid
Citric Cycle (Krebs Cycle), using
oxygen to breakdown glucose into CO2
and H2O, and provide up 38 ATP
molecules. Mitochondria reproduce by
themselves, and are not created by the
DNA in the cell nucleus. As time
continues some of the DNA from the
mitochondria merges with the cell
nucleus DNA. Mitochondria produce
sterol used to make the eukaryote cell
wall flexible. Because mitochondria
need Oxygen, but the level of oxygen is
very low on earth, oxygen may be
provided by photosynthesizing
cyanobacteria living near these cells.


All eukaryotes alive today either have
mitochondria except the amitochondriate
excavates (metamonads), the most
ancient of the eukaryotes alive today.
That parabasalids have hydrogenosomes,
anaerobic organelles that seem to have
evolved from mitochondria, many people
think amitochondriate species lost
their mitochondria over time.

This changes
the eukaryote cell from an anaerobic to
aerobic unicellular organism.
This early
mitochondria may have "tubular
christae".
Perhaps there was a period of time
where a system evolved to make sure
both halves received mitochondria
during cell division.

Protists with discoidal mitochondrial
cristea will later evolve from the
Bikont tubular mitochondrial christae
branch.

For the most part:
1) Excavates, Amoebozoa,
and Chromealveolates have or had
tubular christae,
2) Discicristata
(Euglenozoa) have discoidal christae.
3)
Cryptomonads, Glaucophytes, Red Algae,
Green Algae, Plants, Fungi, Animals all
have flat christae.

From this point on, all eukaryotes will
need Oxygen to use mitochondria and
receive the ATP made by mitochondria.



 
[1] Phylogenetic hypothesis of the
eukaryotic lineage based on
ultrastructural and molecular data.
Organisms are divided into three main
groups distinguished by mitochondrial
cristal shape (either discoidal,
flattened or tubular). Unbroken lines
indicate phylogenetic relationships
that are firmly supported by available
data; broken lines indicate
uncertainties in phylogenetic
placement, resolution of which will
require additional data. Color coding
of organismal genus names indicates
mitochondrial genomes that have been
completely (Table 1), almost completely
(Jakoba, Naegleria and
Thraustochytrium) or partially (*)
sequenced by the OGMP (red), the FMGP
(black) or other groups (green). Names
in blue indicate those species whose
mtDNAs are currently being sequenced by
the OGMP or are future candidates for
complete sequencing. Amitochondriate
retortamonads are positioned at the
base of the tree, with broken arrows
denoting the endosymbiotic origin(s) of
mitochondria from a Rickettsia-like
eubacterium. Macrophar.,
Macropharyngomonas.
source: http://nar.oxfordjournals.org/co
ntent/vol26/issue4/images/gkb18201.gif


[2] Figure 1 Phylogenetic tree of
eukaryotes based on ultrastructural and
molecular data. Organisms are
sub-divided into main groups as
discussed in the text. Only a few
representative species for which
complete (or almost complete) mtDNA
sequences are known are shown in each
lineage. In some cases, line drawings
or actual pictures of the organisms are
provided (Acanthamoeba, M. Nagata; URL:
http://protist.i.hosei.ac.jp/PDB/PCD3379
/htmls/21.html; Allomyces, Tom Volk;
URL:
http://botit.botany.wisc.edu/images/332/
Chytridiomycota/Allomyces_r_So_pa/A._arb
uscula_pit._sporangia_tjv.html;
Amoebidium, URL:
http://cgdc3.igmors.upsud.fr/microbiolog
ie/mesomycetozoaires.htm; Marchantia,
URL:
http://www.science.siu.edu/landplants/He
patophyta/images/March.female.JPEG
Scenedesmus, Entwisle et al.,
http://www.rbgsyd.gov.au/_data/page/1824
/Scenedesmus.gif). The color-coding of
the main groups (alternating between
dark and light blue) on the outer
circle corresponds to the color-coding
of the species names. Unbroken lines
indicate phylogenetic relationships
that are firmly supported by available
molecular data; broken lines indicate
uncertainties in phylogenetic
placement, resolution of which will
require additional sequence data. [t:
why not color code or add which type of
mito?]
source: http://arjournals.annualreviews.
org/doi/full/10.1146/annurev.genet.37.11
0801.142526

2,303,000,000 YBN
203) Bikonts (two cilia) evolve from
Unikonts (one cilium). Bikonts (also
called anterokonts for having anterior
{forward facing} cilia) will evolve
into the vast majority of the Protist
and all of the Plant Kingdoms. The
Unikonts will evolve into the ameobozoa
(tenatively), and the opisthokonts
(ancestrally posterior cilium) which
include the entire Fungi and Animal
Kingdoms.


 
[1] Figure 1. Phylogenetic hypothesis
of the eukaryotic lineage based on
ultrastructural and molecular data.
Organisms are divided into three main
groups distinguished by mitochondrial
cristal shape (either discoidal,
flattened or tubular). Unbroken lines
indicate phylogenetic relationships
that are firmly supported by available
data; broken lines indicate
uncertainties in phylogenetic
placement, resolution of which will
require additional data. Color coding
of organismal genus names indicates
mitochondrial genomes that have been
completely (Table 1), almost completely
(Jakoba, Naegleria and
Thraustochytrium) or partially (*)
sequenced by the OGMP (red), the FMGP
(black) or other groups (green). Names
in blue indicate those species whose
mtDNAs are currently being sequenced by
the OGMP or are future candidates for
complete sequencing. Amitochondriate
retortamonads are positioned at the
base of the tree, with broken arrows
denoting the endosymbiotic origin(s) of
mitochondria from a Rickettsia-like
eubacterium. Macrophar.,
Macropharyngomonas.
source:

2,300,000,000 YBN
47) Most recent evidence of uraninite,
a mineral that cannot exist for much
time if exposed to oxygen, indicating
that free oxygen is accumulating in the
air of earth for the first time.


  
2,300,000,000 YBN
48) Oldest Red Beds, iron oxide formed
on land, begin here and are evidence of
more free oxygen in the air of earth.


 
[1]
http://www.kgs.ukans.edu/Extension/redhi
lls/redhills.html
source:

2,300,000,000 YBN
219) Genetic comparison shows the
oldest line of eukaryotes still in
existence, the oldest living protists,
in the Phylum "Metamonada" (Excavates)
originating now. This is where the
eukaryote line is created and separates
from the archaebacteria (archaea) line.
Most of these species have an
excavated ventral feeding groove, and
all lack mitochondria. Mitochondria
are thought to have been lost
secondarily, although this is not
certain.

PHYLUM Metamonada
ORDER Carpediemondida
ORDER
Diplomonadida
ORDER Retortamonadida
CLASS Parabasalia
ORDER
Trichomonadida
ORDER Hypermastigida
CLASS Anaeromonada
ORDER Oxymonadida

ORDER Trimastigida
Includes Diplomonad
"Giardia", and Parabasalid "Trichomonas
vaginalis".
The trophozoite form of Giardia does
age and die.
Most Metamonads reproduce
asexually through closed (the nuclear
membrane does not dissolve during
mitosis) mitosis (and involves an
external spindle? is pluromitosis?),
but some species are "faculatively
sexual" (can reproduce sexually in
addition to asexually). So already by
the time of these most ancient of the
now living eukaryotes, sex had evolved.

eat bacteria?

 
[1] Giardia lamblia, a parasitic
flagellate that causes giardiasis.
Image from public domain source at
http://www.nigms.nih.gov/news/releases/i
mages/para.jpg
source: http://www.nigms.nih.gov/news/re
leases/images/para.jpg


[2] . The cysts are hardy and can
survive several months in cold water.
Infection occurs by the ingestion of
cysts in contaminated water, food, or
by the fecal-oral route (hands or
fomites) . In the small intestine,
excystation releases trophozoites (each
cyst produces two trophozoites) .
Trophozoites multiply by longitudinal
binary fission, remaining in the lumen
of the proximal small bowel where they
can be free or attached to the mucosa
by a ventral sucking disk .
Encystation occurs as the parasites
transit toward the colon. The cyst is
the stage found most commonly in
nondiarrheal feces . Because the cysts
are infectious when passed in the stool
or shortly afterward, person-to-person
transmission is possible. While
animals are infected with Giardia,
their importance as a reservoir is
unclear.
source: http://www.dpd.cdc.gov/dpdx/HTML
/Giardiasis.asp?body=Frames/G-L/Giardias
is/body_Giardiasis_page1.htm

2,000,000,000 YBN
293) Genetic comparison shows the the
Eukaryote Phylum "Loukozoa" (Jakobea
and Malawimonadea) originating now.
These species have mitochondria with
tubular cristae, and are the most
ancient species that still have
mitochondria.

This species is the most ancient known
species to have a shell. This first
hard shells (lorika) made of calcium
carbonate (Calcite CaCO3), plates of
silica (SiO2), or carbon-based
molecules evolve around the
single-celled species living in the
ocean.

Perhaps this shell served to protect
the cell from external damage from
being eaten by other eukaryotes
(zooplankton), infection by bacteria or
viruses, control of buoyancy, to filter
UV light, against damage by non-living
sources.

Jakobids and Malawimonads are
also grouped as Excavates because they
have a ventral feeding groove.

Jakobids are flagellates with two
flagella located at the anterior end of
a ventral feeding groove (i.e., are
excavate), with mitochondria, freely
swimming or loricate (with protective
shell).

Flagellar apparatus with two basal
bodies giving rise to two major
microtubular roots, which support the
margins of the ventral groove. Other
cytoskeletal microtubules arise
directly or indirectly from the basal
bodies, no extrusomes.

Jakobids have tubular mitochondrial
cristae (transforming to flat cristae
in Jakoba libera). (1) This indicates
that flat evolved from tubular
cristae.

PHYLUM Loukozoa
ORDER Jakobida
ORDER
Malawimonadida

 
[1] Histiona. This drawing was made by
D. J. Patterson. COPYRIGHTED EDU
source: http://microscope.mbl.edu/script
s/microscope.php?func=imgDetail&imageID=
3479


[2] Histiona (hist-ee-own-a) is a
jakobid flagellate related to Jakoba.
As with other excavates, there is a
ventral groove and the flagella insert
at the head of the groove. There are
two flagella, one lying in the groove
and one curving outwards from the point
of insertion. The margins of the groove
can be mistaken for flagella. Unlike
most other excavates, Histiona sits in
a stalked lorica when feeding. Lorica
with a cyst is evident. Phase contrast.
This picture was taken by David
Patterson, Linda Amaral Zettler, Mike
Peglar and Tom Nerad from cultures and
other materials maintained at the
American Type Culture Collection during
2001. COPYRIGHTED EDU
source: http://microscope.mbl.edu/script
s/microscope.php?func=imgDetail&imageID=
435

1,990,000,000 YBN
202) Eukaryotes with discoidal cristae
mitochondria split from the tubular
christae line.

This is the origin of the
Discicristata: species that have
discoid mitochondrial cristae and, in
some cases, a deep (excavated) ventral
feeding groove.

The Discicristata are Acrasid
slime molds, vahlkampfiid amoebas,
euglenoids, trypanosomes, and
leishmanias.

 
[1] Figure 1. Phylogenetic hypothesis
of the eukaryotic lineage based on
ultrastructural and molecular data.
Organisms are divided into three main
groups distinguished by mitochondrial
cristal shape (either discoidal,
flattened or tubular). Unbroken lines
indicate phylogenetic relationships
that are firmly supported by available
data; broken lines indicate
uncertainties in phylogenetic
placement, resolution of which will
require additional data. Color coding
of organismal genus names indicates
mitochondrial genomes that have been
completely (Table 1), almost completely
(Jakoba, Naegleria and
Thraustochytrium) or partially (*)
sequenced by the OGMP (red), the FMGP
(black) or other groups (green). Names
in blue indicate those species whose
mtDNAs are currently being sequenced by
the OGMP or are future candidates for
complete sequencing. Amitochondriate
retortamonads are positioned at the
base of the tree, with broken arrows
denoting the endosymbiotic origin(s) of
mitochondria from a Rickettsia-like
eubacterium. Macrophar.,
Macropharyngomonas.
source: http://nar.oxfordjournals.org/co
ntent/vol26/issue4/images/gkb18201.gif

1,990,000,000 YBN
301) Haplodiplontic (Diplohaplontic,
Diplobiontic) life cycle (organism with
both diploid and haploid "alternate
life stages" that reproduce asexually
by mitosis) with "sporic meiosis"
evolves.

In this life cycle haploid gametes fuse
to form a diploid zygote which divides
by meiosis producing haploid spores
that produce (differentiate?) gametes,
starting the cycle again.

Initially these species are single
celled in both stages (like
Haptophyta).

All plants, most brown algae,
blastocladiid chytrids, many red algae,
and some filamentous green algae (e.g.
Cladophora) and foraminifera have
haplodiploid life cycles.

Initially, these organisms are single
celled, but later the mitosis stages
will become multicellular when the
cells that result from mitosis stick
together. The only? example of this
is Haptophyta, where diploid cells
divide in sporic meiosis, into haploid
cells (gamonts) which then divide into
gametes.



 
[1] Figure 23.1.Plants have
haplodiplontic life cycles that involve
mitotic divisions (resulting in
multicellularity) in both the haploid
and diploid generations (paths A and
D). Most animals are diplontic and
undergo mitosis only in the diploid
generation (paths B and D).
Multicellular organisms with haplontic
life cycles follow paths A and C.
COPYRIGHTED EDU
source: http://zygote.swarthmore.edu/pla
ntfig1.gif


[2] Drawn by self for Biological life
cycle Based on Freeman & Worth's
Biology of Plants (p. 171). GNU
source: http://en.wikipedia.org/wiki/Ima
ge:Sporic_meiosis.png

1,988,000,000 YBN
317) Eukaryotes that have mitochondria
with flat christae evolve from those
with tubular christae.


 
[1] Figure 1. Phylogenetic hypothesis
of the eukaryotic lineage based on
ultrastructural and molecular data.
Organisms are divided into three main
groups distinguished by mitochondrial
cristal shape (either discoidal,
flattened or tubular). Unbroken lines
indicate phylogenetic relationships
that are firmly supported by available
data; broken lines indicate
uncertainties in phylogenetic
placement, resolution of which will
require additional data. Color coding
of organismal genus names indicates
mitochondrial genomes that have been
completely (Table 1), almost completely
(Jakoba, Naegleria and
Thraustochytrium) or partially (*)
sequenced by the OGMP (red), the FMGP
(black) or other groups (green). Names
in blue indicate those species whose
mtDNAs are currently being sequenced by
the OGMP or are future candidates for
complete sequencing. Amitochondriate
retortamonads are positioned at the
base of the tree, with broken arrows
denoting the endosymbiotic origin(s) of
mitochondria from a Rickettsia-like
eubacterium. Macrophar.,
Macropharyngomonas.
source: http://nar.oxfordjournals.org/co
ntent/vol26/issue4/images/gkb18201.gif

1,982,000,000 YBN
87) Genetic comparison shows the most
primitive living members of the Phylum
"Euglenozoa" (euglenids, leishmania,
trypanosomes, kinetoplastids) evolved
at this time.

This is the oldest eukaryote to exhibit
colonialism. Perhaps eukaryote
colonialism is partially or fully
inherited from prokaryotes, but
colonialism may have evolved
independently again in eukaryotes.

This is the most ancient species known
to have a cell covering, which is of
the type "pellicle".

No examples of sexual
reproduction in the group have been
found. Reproduction is through closed
mitosis and involves an internal
spindle. At least one account of a
sexual cycle has been reported in
Scytomonas.

The chloroplasts are contained in three
membranes and are pigmented similarly
to the plants, suggesting they were
retained from some captured green
alga.
All Euglenozoa have mitochondria with
discoid cristae, which in the
kinetoplastids characteristically have
a DNA-containing granule or kinetoplast
associated with the flagellar bases.
I think
they are still haploid, mitosis
duplicates in nucleus?
Euglenozoa age?

This group is sometimes called
"Discicristates" because all members
have mitochondria with "discoidal
cristae".

Euglenids are the first eukaryotes with
an eyespot. Most colored euglenids
also have a stigma or eyespot, which is
a small splotch of red pigment on one
side of the flagellar pocket. This
shades a collection of light sensitive
crystals near the base of the leading
flagellum, so the two together act as a
sort of directional eye. Euglenozoa
eyepots evolved from chloroplasts.
This is the beginning of a light
sensory system which evolves to eyes?

A small number of euglinids have
chloroplasts and can photosynthesize.
In these species, the chloroplasts
contain three membranes and are thought
to have evolved at least 900 million
years later from a captured green alga.


Euglenoids, however, share reproductive
habits with their kinetoplastid
relations by reproducing mainly by
asexual binary fission. Euglenoids
reproduce very rapidly, absorbing their
flagellum and dividing haploid cells
through mitosis. Mitosis produces 4-8
flagellated haploid cells, called
zoospores. The zoospores then break out
of the parent cell and grow to full
size.

condensed chromosomes: yes in all
kinetoplasts, and some euglenophyta.
pol
ar structures: none
number of flagella:
kinetoplastids=(1 in some) 2,
euglenophyta=2 (4 in some)
life forms:

unicellular: flagellated
multicellular:
colonial
cell covering: pellicle

2. Euglenoids are small (10-500
µm) freshwater unicellular organisms.
3.
One-third of all genera have
chloroplasts; those that lack
chloroplasts ingest or absorb their
food.
4. Their chloroplasts are
surrounded by three rather than two
membranes.
a. Their chloroplasts
resemble those of green algae.
b.
They are probably derived from a green
algae through endosymbiosis.
5. The pyrenoid
outside the chloroplast produces an
unusual type of carbohydrate polymer
(paramylon)
not seen in green algae.

6. They possess two flagella, one of
which typically is much longer and than
the other and projects
out of a
vase-shaped invagination; it is called
a tinsel flagellum because it has hairs
on it.
7. Near the base of the
longer flagellum is a red eyespot that
shades a photoreceptor for detecting
light.
8. They lack cell walls, but
instead are bounded by a flexible
pellicle composed of protein strips
side-by-side.
9. A contractile vacuole,
similar to certain protozoa, eliminates
excess water.
10. Euglenoids reproduce
by longitudinal cell division; sexual
reproduction is not known to occur.

PHYLUM Euglenozoa
CLASS Euglenoidea
CLASS Diplonemea
CLASS
Kinetoplastea
CLASS Postgaardea

 
[1] euglena
source: http://www.fcps.k12.va.us/Stratf
ordLandingES/Ecology/mpages/euglena.htm


[2] euglena
source: http://protist.i.hosei.ac.jp/PDB
/Images/Mastigophora/Euglena/genus1L.jpg

1,982,000,000 YBN
294) Genetic comparison shows the
Phylum "Percolozoa" (also called
"Heterolobosea") (acrasid slime molds)
evolved at this time.

Percolozoa are a group
of heterotrophic colourless protozoa,
including many that can transform
between amoeboid, flagellate, and
encysted stages. These are collectively
referred to as amoeboflagellates,
schizopyrenids, or vahlkampfids. They
also include the acrasids, a group of
social amoebae that aggregate to form
sporangia.

Very closely related to Euglenozoa.
All
characteristics are like Euglenozoa:
Percolozoa
have mitochondria with discoid
christae.
No examples of sexual reproduction in
the group have been found.
Reproduction is through closed mitosis
and involves an internal spindle.
No
chloroplasts (check) or (The
chloroplasts are contained in three
membranes and are pigmented similarly
to the plants, suggesting they were
retained from some captured green
alga.)
I think they are still haploid, mitosis
duplicates in nucleus?
Percolozoa age?
Percolozoa
are sometimes included in the group
"Discicristates" because all members
have mitochondria with "discoidal
cristae".
No eyespots.

closed mitosis with internal spindle.


The Percolozoa are the most ancient
species to have members that move by
pseudopodia, like amoeba.

PHYLUM Percolozoa
CLASS
Heterolobosea
ORDER Schizopyrenida Singh, 1952

ORDER Acrasida Shröter, 1886
(acrasids, cellular slime molds)
ORDER
Lyromonadida Cavalier-Smith, 1993
CLASS
Percolatea

ORDER Acrasida (acrasids, cellular
slime molds):
a. Cellular slime
molds (Phylum Acrasiomycota) (ORDER
Acrasida) exist as individual amoeboid
cells. (Plasmodial slime molds,
mycetozoa, which evolve later, exist as
a plasmodium. )
b. They live
in soil and feed on bacteria and
yeast.
c. As food runs out,
amoeboid cells release a chemical that
causes them to aggregate into a
pseudoplasmodium.
d. The pseudoplasmodium
stage is temporary; it gives rise to
sporangia that produce spores.
e.
Spores survive until more favorable
environmental conditions return; then
they germinate.
f. Spore germinate to
release haploid amoeboid cells, which
is again the beginning of asexual
cycle.
g. Asexual cycle occurs
under very moist conditions.

 
[1] Stages of Naegleria fowleri, a
member of the Percolozoa. Adapted from
Image:Free-living amebic
infections.gif, which is from the CDC.
PD
source: http://en.wikipedia.org/wiki/Ima
ge:Naegleria.png


[2] CLASS Heterolobosea ORDER
Schizopyrenida Heteramoeba: The
flagellated form is large (30
�m), two flagella, an elongate
cytostome curving around the anterior
of the cell and forming a groove.
Nucleus with peripheral chromatin.
Probably feeds and divides as a
flagellate. One species. This genus is
most like Paratetramitus from which it
can be distinguished by peripheral
location of chromatin material. Cysts
without pores, excystment through a
weak region of wall. Marine.
Heteramoeba (het-err-a-me-ba) a naked
heterolobose amoeba, distinguished from
other types of naked amoebae with
lobose pseudopodia largely by
ultrastructural features, but trophic
heterolobose amoebae tend to form their
pseudopodially suddenly rather than
progressively. Phase contrast. This
picture was taken by David Patterson,
Linda Amaral Zettler, Mike Peglar and
Tom Nerad from cultures and other
materials maintained at the American
Type Culture Collection during 2001.
NONCOMMERCIAL USE
source: http://microscope.mbl.edu/script
s/microscope.php?func=imgDetail&imageID=
413

1,980,000,000 YBN
38) Multicellularity evolves in a
protist.

Multicellularity is a very important
event in the evolution of life on
earth. With multicellular organisms,
larger sized organisms could evolve.

There are many uncertainties
surrounding the origin of
multicellularity. Multicellularity may
have evolved independently for Plants,
Fungi and Animals, or multicellularity
may have evolved only once in
eukaryotes.

The key feature of this cell is that a
multicellular organism is made from a
single cell and the multicellular
organism is not a collection of
independent cells (colonialism). The
main difference between this organism
and single-celled organisms is the way
the cells stay fastened together after
cell division.

Which species was the first
multicellular species is not clear.
Multicellularity is found in all 3 life
cycles (haplontic, diplontic,
haplodiplontic). The 3 main life cycle
types (haplontic, etc.) probably
evolved in single cell species before
multicellularity evolved. If
multicellularity evolved once and is
inherited, perhaps all multicellular
organism descended from a single
haplodiplontic organism.

These multicellular organisms have
undifferentiated cells in the
multicellular stage (all cells in the
haploid or diploid multicellular
organism are made of one kind of cell).

Dinoph
yta, and Fungi are multicellular
Haplontic species.
Most animals are
multicellular Diplontic species.
Most brown
algae and all plants are multicellular
Haplodiplontic species.

The vast majority of multicellular
organisms reproduce only through sex,
although there are exceptions (like
some plants and rotifers) which have
lost the ability to sexually reproduce
or can also reproduce asexually. In
multicellularity, one cell goes on to
produce all the cells in a
multicellular species, so that each
individual organism is genetically
unique. This cell is usually a diploid
zygote, but can be a haploid cell.

This protist is most likely sexual, and
multicellularity evolved only in a
species that reproduces sexually.

Some describe algae multicellularity as
"filamentous".

The first multicellular eukaryuotes are
presumably undifferentiated. For
haplontic these cells are all gametes,
for diplontic these cells are all
capable of meiosis to form gametes, for
haplodiplontic, in the haploid stage
the cells are all gamete producing, in
the diploid stage the cells are all
spore producing.

Some people think that multicellular
organisms arose at least six times: in
animals, fungi and several groups of
algae.

  
1,978,000,000 YBN
15) Multicellularity with
differentiation evolves.

Multicellular organisms are no longer
all haploid or diploid gamete producing
cells (or spore producing if
haplodiplontic), but are made of gamete
(or spore) producing cells in addition
to somatic cells which copy asexually
through mitosis.

Now, in addition to being large
multicell organisms, multicellular
organisms can have differentiated cells
that form a variety of different shaped
structures, and perform different
functions.

This process will evolve to the
metazoan multicellular differentiation
that arises from a single zygote cell,
where cells have different functions
and shapes.
Differentiation evolves for a
second time in eukaryotes?
this is not the first
monoadmulti one cell leading to a
multicellular organism (attached, free,
interchangible)?
where a multicellular organism is made
from one cell (interchangable, specific
cells: genetic specificity).

It is unknown how multicellular life
stages happen. For example, why one
specific cell line of many produced
from mitosis of a zygote will go on to
do meiosis producing the haploid gamete
cells which will fuse to form the next
zygote, but the many other cells made
from, for example, one of the two cells
made after the zygote divides, will not
contain the line of cells that
ultimately make the gamete producing
cells which continue the life cycle of
the organism. Since presumably each
cell in an organism contains an
identical genome, perhaps a gamete
producing cell can be made from any
cell if specific proteins are present,
or perhaps there is a protein which
simply points to a certain location in
the DNA which is located at a different
location in the DNA for every cell, or
perhaps some other explanation answers
the question of how cell
differentiation can happen when each
cell has the same genome.

A (diploid) zygote cell (the cell made
by two merging gamete cells) now
divides to form all cells in the
differentiated multicellular organism,
and is said to be "totipotent".
Totipotent cells differentiate into
"pluripotent" cells which can make most
but not all cells in the organism.
Pluripotent cells differentiate into
"multipotent" (can make a number of
cells) or "unipotent" cells (can only
make one kind of cell).

  
1,974,000,000 YBN
169) For those that think algae are
plants, this is where the plant kingdom
begins with the evolution of brown
algae (phaeophyta).

  
1,973,000,001 YBN
88) Genetic comparison shows the
ancestor of the "Chromalveolates"
evolving now. Chromalveolates include
the Chromista and Alveolata. The
Chromista include the 3 Phyla
Haptophyta, Cryptophyta (Cryptomonads),
and Heterokontophyta (brown algae
{kelp}, diatoms, water molds).
Alveolata include the 3 Phyla
Dinoflagellata, Apicomplexa (Malaria,
Toxoplasmosis), and Ciliophora
(ciliates).

Chromealveolates have mitochondria
with tubular cristae.

Thomas Cavalier-Smith writes: "The
chromalveolate clade (Cavalier-Smith
1999) and its constituent taxa, kingdom
Chromista (Cavalier-Smith 1981) and
protozoan infrakingdom Alveolata
(Cavalier-Smith 1991b), were all
proposed based on morphological,
biochemical, and evolutionary reasoning
about protein targeting before there
was sequence evidence for any of them.
Now all are strongly supported by such
evidence. Chromalveolates comprise all
algae with chlorophyll c (the
chromophyte algae) and all their
nonphotosynthetic descendants. They
arose by a single symbiogenetic event
in which an early unicellular red alga
was phagocytosed by a biciliate host
and enslaved to provide photosynthate
(Cavalier-Smith 1999, 2002c, 2003a).
The strongest evidence that this
occurred once only in their cenancestor
is the replacement of the red algal
plastid glyceraldehyde phosphate
dehydrogenase (GAPDH) by a duplicate of
the gene for the cytosolic version of
this enzyme in all four chromalveolate
groups with plastids: the alveolate
sporozoa and dinoflagellates and the
chromist cryptomonads and chromobiotes
(Fast et al. 2001). It would be
incredible for such gene duplication,
retargeting by acquiring bipartite
targeting sequences, and loss of the
original red algal gene to have
occurred convergently in four groups,
but it was already pretty incredible
that these groups would all have
evolved a similar protein-targeting
system independently and all happened
to enslave a red alga, evolve
chlorophyll c, and place their plastids
within the rough endoplasmic reticulum
(ER) independently. Yet many assumed
just this because of the false dogma
that symbiogenesis is easy and the
failure of all these groups to cluster
in rRNA trees. For chromobiotes this
retargeting of GAPDH has been
demonstrated only for
heterokonts-information is lacking for
haptophytes. However, there are five
strong synapomorphies for Chromobiota,
making it highly probable that the
group is holophyletic (Cavalier-Smith
1994). They share the presence of the
periplastid reticulum in the
periplastid space instead of a
nucleomorph like cryptomonads, they
uniquely make the carotenoid
fucoxanthin and chlorophyll c3, they
uniquely have a single autofluorescent
cilium, and they have tubular
mitochondrial cristae with an
intracristal filament. Five plastid
genes now extremely robustly support
the monophyly of both chromists and
chromobiotes (Yoon et al. 2002). We are
confident that comparable sequence
evidence from nuclear genes will also
eventually catch up with the general
biological evidence for the holophyly
of chromobiotes to convince even the
most skeptical, who ignore or discount
such valuable evidence that
chromobiotes are holophyletic."

Chromista include phyla:
Heterokontophyta
(heterokonts) (many classes) (includes
colored: golden algae, axodines,
diatoms, yellow-green algea, brown
algae, colorless: water moulds, slime
nets)
Haptophyta
Cryptophyta (cryptomonads) (many
genera)

Alveolates include the phyla:
Dinoflagellata
(Dinoflagellates)
Apicomplexa (Apicomplexans)
Ciliophora (ciliates)

In 1981 Cavalier-Smith created a new
kingdom called "Chromista" in which all
chromalveolates are placed.

 
[1] Fig. 1. A consensus phylogeny of
eukaryotes. The vast majority of
characterized eukaryotes, with the
notable exception of major subgroups of
amoebae, can now be assigned to one of
eight major groups. Opisthokonts (basal
flagellum) have a single basal
flagellum on reproductive cells and
flat mitochondrial cristae (most
eukaryotes have tubular ones).
Eukaryotic photosynthesis originated in
Plants; theirs are the only plastids
with just two outer membranes.
Heterokonts (different flagellae) have
a unique flagellum decorated with
hollow tripartite hairs (stramenopiles)
and, usually, a second plain one.
Cercozoans are amoebae with filose
pseudopodia, often living with in tests
(hard outer shells), some very
elaborate (foraminiferans). Amoebozoa
are mostly naked amoebae (lacking
tests), often with lobose pseudopodia
for at least part of their life cycle.
Alveolates have systems of cortical
alveoli directly beneath their plasma
membranes. Discicristates have discoid
mitochondrial cristae and, in some
cases, a deep (excavated) ventral
feeding groove. Amitochondrial
excavates lack substantial molecular
phylogenetic support, but most have an
excavated ventral feeding groove, and
all lack mitochondria. The tree shown
is based on a consensus of molecular
(1-4) and ultrastructural (16, 17) data
and includes a rough indication of new
ciPCR ''taxa'' (broken black lines)
(7-11). An asterisk preceding the taxon
name indicates probable paraphyletic
group
source: http://www.sciencemag.org/cgi/co
ntent/full/300/5626/1703


[2] Beautiful marine diatoms as seen
through a microscope. These tiny
phytoplankton are encased within a
silicate cell wall. Image ID: corp2365,
NOAA Corps Collection Photographer: Dr.
Neil Sullivan, University of Southern
Calif. NOAA This image is a work of
the National Oceanic and Atmospheric
Administration, taken or made during
the course of an xxxxx? official
duties. As works of the U.S. federal
government, all NOAA images are in the
public domain.
source: http://en.wikipedia.org/wiki/Ima
ge:Diatoms_through_the_microscope.jpg

1,972,000,000 YBN
304) Genetic comparison shows the
ancestor of Chromalveolate Phlyum
Haptophyta evolving now.

Some Haptophytes
are haplodiploid (alternate between
haploid and diploid cycles that both
have mitosis), and this group is the
most primitive with a haplodiploid life
cycle.

Haptophytes are single cellular.

Haptophytes are found only in all
oceans (marine) and are flagellates,
almost all with plastids with
chlorophylls a and c, with two flagella
and one additional locomotor/feeding
organelle, the haptonema.

Haptophyta are a group of algae
(phytoplankton).
The chloroplasts are pigmented
similarly to those of the heterokonts,
such as golden algae, but the structure
of the rest of the cell is different,
so it may be that they are a separate
line whose chloroplasts are derived
from similar endosymbionts.
The cells typically have
two slightly unequal flagella, both of
which are smooth, and a unique
organelle called a haptonema, which is
superficially similar to a flagellum
but differs in the arrangement of
microtubules and in its use.
Haptophytes
have tubular mitochondria cristae.
Most
haptophytes are coccolithophores, which
live strictly in the oceans (marine)
and are ornmmented with calcified
scales called coccoliths, which are
sometimes found as microfossils. Other
planktonic haptophytes of note include
Chrysochromulina and Prymnesium, which
periodically form toxic marine algal
blooms. Both molecular and
morphological evidence supports their
division into five orders.

Emiliania is a small organism that is
famous for turning huge portions of the
ocean bright turquoise during its
blooms. They are also known for
contributing to the white cliffs of
Dover because of the calcite in their
coccolith cell structure. They play a
very important role in the carbon cycle
in the ocean because they form calcium
carbonate exoskeletons that sink to the
bottom of the ocean floor when they
die. They are also one of the worlds
major calcite producers.

Sexual reproduction: Asexual, Open
mitosis with spindle nucleating
(originating?) in cytoplasm.
Phaeocystis colonial
cells diploid, motile cells haploid or
diploid; reproduction by vegetative
division of non-motile cells and
fragmentation of colonies, vegetative
division of motile cells, or by fusion
of gametes.

Members of the Haptophytes Genus
"Phaocystis" form colonies (see
photo).

Haptophytes are also called
"Prymnesiophytes"

Some Haptophyta have hard shell made of
calcium carbonate evolves around the
single-celled species living in the
ocean.

 
[1] Fig. 1. A consensus phylogeny of
eukaryotes. The vast majority of
characterized eukaryotes, with the
notable exception of major subgroups of
amoebae, can now be assigned to one of
eight major groups. Opisthokonts (basal
flagellum) have a single basal
flagellum on reproductive cells and
flat mitochondrial cristae (most
eukaryotes have tubular ones).
Eukaryotic photosynthesis originated in
Plants; theirs are the only plastids
with just two outer membranes.
Heterokonts (different flagellae) have
a unique flagellum decorated with
hollow tripartite hairs (stramenopiles)
and, usually, a second plain one.
Cercozoans are amoebae with filose
pseudopodia, often living with in tests
(hard outer shells), some very
elaborate (foraminiferans). Amoebozoa
are mostly naked amoebae (lacking
tests), often with lobose pseudopodia
for at least part of their life cycle.
Alveolates have systems of cortical
alveoli directly beneath their plasma
membranes. Discicristates have discoid
mitochondrial cristae and, in some
cases, a deep (excavated) ventral
feeding groove. Amitochondrial
excavates lack substantial molecular
phylogenetic support, but most have an
excavated ventral feeding groove, and
all lack mitochondria. The tree shown
is based on a consensus of molecular
(1-4) and ultrastructural (16, 17) data
and includes a rough indication of new
ciPCR ''taxa'' (broken black lines)
(7-11). An asterisk preceding the taxon
name indicates probable paraphyletic
group
source: http://www.sciencemag.org/cgi/co
ntent/full/300/5626/1703


[2] Emiliania huxleyi, a
coccolithophore. Photo courtesy Dr.
Markus Geisen - photographer, and The
Natural History Museum. PD
source: http://en.wikipedia.org/wiki/Ima
ge:Emiliania_huxleyi_3.jpg

1,971,000,000 YBN
305) Genetic comparison shows the
ancestor of the Chromalveolate Phylum
"Cryptophyta" (Cryptomonads) evolving
now.

The cryptomonads are a small group of
flagellates, most of which have
chloroplasts. They are common in
freshwater, and also occur in marine
and brackish habitats. Each cell has an
anterior groove or pocket with
typically two slightly unequal flagella
at the edge of the pocket.
Cryptomonads
distinguished by the presence of
characteristic extrusomes called
ejectisomes, which consist of two
connected spiral ribbons held under
tension. If the cells are irritated
either by mechanical, chemical or light
stress, they discharge, propelling the
cell in a zig-zag course away from the
disturbance. Large ejectisomes, visible
under the light microscope, are
associated with the pocket; smaller
ones occur elsewhere on the cell.
Crypto
monads have one or two chloroplasts,
except for Chilomonas which has
leucoplasts and Goniomonas which lacks
plastids entirely. These contain
chlorophylls a and c, together with
phycobilins and other pigments, and
vary in color from brown to green. Each
is surrounded by four membranes, and
there is a reduced cell nucleus called
a nucleomorph between the middle two.
This indicates that the chloroplast was
derived from a eukaryotic symbiont,
shown by genetic studies to have been a
red alga.

A few cryptomonads, such as
Cryptomonas, can form palmelloid
stages, but readily escape the
surrounding mucus to become free-living
flagellates again. Cryptomonad flagella
are inserted parallel to one another,
and are covered by bipartite hairs
called mastigonemes, formed within the
endoplasmic reticulum and transported
to the cell surface. Small scales may
also be present on the flagella and
cell body. The mitochondria have flat
cristae, and mitosis is open; sexual
reproduction has also been reported.

Originally the cryptomonads were
considered close relatives of the
dinoflagellates because of their
similar pigmentation. Later botanists
treated them as a separate division,
Cryptophyta, while zoologists treated
them as the flagellate order
Cryptomonadida. There is considerable
evidence that cryptomonad chloroplasts
are closely related to those of the
heterokonts and haptophytes, and the
three groups are sometimes united as
the Chromista. However, the case that
the organisms themselves are related is
not very strong, and they may have
acquired chloroplasts independently.

Crytomonads often forms blooms in
greater depths of lakes, or during
winter beneath the ice. The cells are
usually brownish in color, and have a
slit-like furrow at the anterior. They
are not known to produce any toxins and
are used to feed small zooplankton,
which is the food source for small fish
in fish farming.

Reproduction:
Number of species:
Size and shape: 10-50 μm
in size and flattened in shape
Mitochondria
Christae: flat (which is unusual, as
most chromalveolates have tubular
christae). Cryotphyta may be more
closely related to the Plant Kingdom
and nearest Glaucophyta which also have
flat christae.

After one species of jakobid that
changes tubular to flat christae,
cryptophyta are the most ancient phylum
to have flat christae.

 
[1] Fig. 1. A consensus phylogeny of
eukaryotes. The vast majority of
characterized eukaryotes, with the
notable exception of major subgroups of
amoebae, can now be assigned to one of
eight major groups. Opisthokonts (basal
flagellum) have a single basal
flagellum on reproductive cells and
flat mitochondrial cristae (most
eukaryotes have tubular ones).
Eukaryotic photosynthesis originated in
Plants; theirs are the only plastids
with just two outer membranes.
Heterokonts (different flagellae) have
a unique flagellum decorated with
hollow tripartite hairs (stramenopiles)
and, usually, a second plain one.
Cercozoans are amoebae with filose
pseudopodia, often living with in tests
(hard outer shells), some very
elaborate (foraminiferans). Amoebozoa
are mostly naked amoebae (lacking
tests), often with lobose pseudopodia
for at least part of their life cycle.
Alveolates have systems of cortical
alveoli directly beneath their plasma
membranes. Discicristates have discoid
mitochondrial cristae and, in some
cases, a deep (excavated) ventral
feeding groove. Amitochondrial
excavates lack substantial molecular
phylogenetic support, but most have an
excavated ventral feeding groove, and
all lack mitochondria. The tree shown
is based on a consensus of molecular
(1-4) and ultrastructural (16, 17) data
and includes a rough indication of new
ciPCR ''taxa'' (broken black lines)
(7-11). An asterisk preceding the taxon
name indicates probable paraphyletic
group COPYRIGHTED
source: http://www.sciencemag.org/cgi/co
ntent/full/300/5626/1703


[2] Figure 1. Phylogenetic hypothesis
of the eukaryotic lineage based on
ultrastructural and molecular data.
Organisms are divided into three main
groups distinguished by mitochondrial
cristal shape (either discoidal,
flattened or tubular). Unbroken lines
indicate phylogenetic relationships
that are firmly supported by available
data; broken lines indicate
uncertainties in phylogenetic
placement, resolution of which will
require additional data. Color coding
of organismal genus names indicates
mitochondrial genomes that have been
completely (Table 1), almost completely
(Jakoba, Naegleria and
Thraustochytrium) or partially (*)
sequenced by the OGMP (red), the FMGP
(black) or other groups (green). Names
in blue indicate those species whose
mtDNAs are currently being sequenced by
the OGMP or are future candidates for
complete sequencing. Amitochondriate
retortamonads are positioned at the
base of the tree, with broken arrows
denoting the endosymbiotic origin(s) of
mitochondria from a Rickettsia-like
eubacterium. Macrophar.,
Macropharyngomonas. COPYRIGHTED
source: http://nar.oxfordjournals.org/cg
i/content/full/26/4/865

1,970,000,000 YBN
306) Genetic comparison shows the
ancestor of the Chromalveolate Phylum
"Heterokontophyta" (Heterokonts also
called Stramenopiles) evolving now.
Heterokonts include brown algae,
diatoms, golden algae, axodines,
yellow-green algae, water moulds and
slime nets.

Heterkonts evolved very near the
same time as the Euglinozoa did.
Heterokonts
all have mitochondria with tubular
christae. The motile cells of
heterokonts all have two unequal cilia
(flagella), one "tinsel" (covered with
hairs {mastigonemes}) cilium and one
"whiplash" (free of hair) cilium.

 
[1] Fig. 1. A consensus phylogeny of
eukaryotes. The vast majority of
characterized eukaryotes, with the
notable exception of major subgroups of
amoebae, can now be assigned to one of
eight major groups. Opisthokonts (basal
flagellum) have a single basal
flagellum on reproductive cells and
flat mitochondrial cristae (most
eukaryotes have tubular ones).
Eukaryotic photosynthesis originated in
Plants; theirs are the only plastids
with just two outer membranes.
Heterokonts (different flagellae) have
a unique flagellum decorated with
hollow tripartite hairs (stramenopiles)
and, usually, a second plain one.
Cercozoans are amoebae with filose
pseudopodia, often living with in tests
(hard outer shells), some very
elaborate (foraminiferans). Amoebozoa
are mostly naked amoebae (lacking
tests), often with lobose pseudopodia
for at least part of their life cycle.
Alveolates have systems of cortical
alveoli directly beneath their plasma
membranes. Discicristates have discoid
mitochondrial cristae and, in some
cases, a deep (excavated) ventral
feeding groove. Amitochondrial
excavates lack substantial molecular
phylogenetic support, but most have an
excavated ventral feeding groove, and
all lack mitochondria. The tree shown
is based on a consensus of molecular
(1-4) and ultrastructural (16, 17) data
and includes a rough indication of new
ciPCR ''taxa'' (broken black lines)
(7-11). An asterisk preceding the taxon
name indicates probable paraphyletic
group COPYRIGHTED
source: http://www.sciencemag.org/cgi/co
ntent/full/300/5626/1703


[2] Figure 1. Phylogenetic hypothesis
of the eukaryotic lineage based on
ultrastructural and molecular data.
Organisms are divided into three main
groups distinguished by mitochondrial
cristal shape (either discoidal,
flattened or tubular). Unbroken lines
indicate phylogenetic relationships
that are firmly supported by available
data; broken lines indicate
uncertainties in phylogenetic
placement, resolution of which will
require additional data. Color coding
of organismal genus names indicates
mitochondrial genomes that have been
completely (Table 1), almost completely
(Jakoba, Naegleria and
Thraustochytrium) or partially (*)
sequenced by the OGMP (red), the FMGP
(black) or other groups (green). Names
in blue indicate those species whose
mtDNAs are currently being sequenced by
the OGMP or are future candidates for
complete sequencing. Amitochondriate
retortamonads are positioned at the
base of the tree, with broken arrows
denoting the endosymbiotic origin(s) of
mitochondria from a Rickettsia-like
eubacterium. Macrophar.,
Macropharyngomonas. COPYRIGHTED
source: http://nar.oxfordjournals.org/cg
i/content/full/26/4/865

1,969,000,000 YBN
307) Chromalveolate Heterokont, Brown
Algae (Phaeophyta) evolves now.

Brown Algae is the most genetically
ancient multicellular organism still
living on earth. In addition to being
first to evolve multicellularity, cell
differentiation (cells of different
types) is already present in all brown
algae.

Genetic comparison shows the ancestor
of the Chromalveolate Heterokont Brown
Algae (Phaeophyta) evolving now.

Brown Algae is the most genetically
ancient multicellular organism still
living on earth. In addition to being
first to evolve multicellularity, cell
differentiation (cells of different
types) is already present in all brown
algae.

Brown algae belong to a large group
called the heterokonts, most of which
are colored flagellates. Most contain
the pigment fucoxanthin, which is
responsible for the distinctive
greenish-brown color that gives brown
algae their name. Brown algae are
unique among heterokonts in developing
into multicellular forms with
differentiated tissues, but they
reproduce by means of flagellate
spores, which closely resemble other
heterokont cells. Genetic studies show
their closest relatives are the
yellow-green algae.

Most Brown algae are haplodiplontic.

 
[1] Fig. 1. A consensus phylogeny of
eukaryotes. The vast majority of
characterized eukaryotes, with the
notable exception of major subgroups of
amoebae, can now be assigned to one of
eight major groups. Opisthokonts (basal
flagellum) have a single basal
flagellum on reproductive cells and
flat mitochondrial cristae (most
eukaryotes have tubular ones).
Eukaryotic photosynthesis originated in
Plants; theirs are the only plastids
with just two outer membranes.
Heterokonts (different flagellae) have
a unique flagellum decorated with
hollow tripartite hairs (stramenopiles)
and, usually, a second plain one.
Cercozoans are amoebae with filose
pseudopodia, often living with in tests
(hard outer shells), some very
elaborate (foraminiferans). Amoebozoa
are mostly naked amoebae (lacking
tests), often with lobose pseudopodia
for at least part of their life cycle.
Alveolates have systems of cortical
alveoli directly beneath their plasma
membranes. Discicristates have discoid
mitochondrial cristae and, in some
cases, a deep (excavated) ventral
feeding groove. Amitochondrial
excavates lack substantial molecular
phylogenetic support, but most have an
excavated ventral feeding groove, and
all lack mitochondria. The tree shown
is based on a consensus of molecular
(1-4) and ultrastructural (16, 17) data
and includes a rough indication of new
ciPCR ''taxa'' (broken black lines)
(7-11). An asterisk preceding the taxon
name indicates probable paraphyletic
group COPYRIGHTED
source: http://www.sciencemag.org/cgi/co
ntent/full/300/5626/1703


[2] Figure 1. Phylogenetic hypothesis
of the eukaryotic lineage based on
ultrastructural and molecular data.
Organisms are divided into three main
groups distinguished by mitochondrial
cristal shape (either discoidal,
flattened or tubular). Unbroken lines
indicate phylogenetic relationships
that are firmly supported by available
data; broken lines indicate
uncertainties in phylogenetic
placement, resolution of which will
require additional data. Color coding
of organismal genus names indicates
mitochondrial genomes that have been
completely (Table 1), almost completely
(Jakoba, Naegleria and
Thraustochytrium) or partially (*)
sequenced by the OGMP (red), the FMGP
(black) or other groups (green). Names
in blue indicate those species whose
mtDNAs are currently being sequenced by
the OGMP or are future candidates for
complete sequencing. Amitochondriate
retortamonads are positioned at the
base of the tree, with broken arrows
denoting the endosymbiotic origin(s) of
mitochondria from a Rickettsia-like
eubacterium. Macrophar.,
Macropharyngomonas. COPYRIGHTED
source: http://nar.oxfordjournals.org/cg
i/content/full/26/4/865

1,968,000,000 YBN
308) Chromalveolate Heterokont, Diatoms
evolve.

Genetic comparison shows the ancestor
of the Chromalveolate Heterokont
Diatoms evolving now.

Diatoms are diplontic.

Diatoms are a very common types of
phytoplankton. Most diatoms are
unicellular, although some form chains
or simple colonies. A characteristic
feature of diatom cells is that they
are encased within a unique cell wall
made of silica. These walls show a wide
diversity in form, some quite beautiful
and ornate, but usually consist of two
symmetrical sides with a split between
them, hence the group name.

Life Cycle
When a cell divides each new cell
takes as its epitheca a valve of the
parent frustule, and within ten to
twenty minutes builds its own
hypotheca; this process may occur
between one and eight times per day.
Availability of dissolved silica limits
the rate of vegetative reproduction,
but also because this method
progressively reduces the average size
of the diatom frustule in a given
population there is a certain threshold
at which restoration of frustule size
is neccesary. Auxospores are then
produced, which are cells that posses a
different wall structure lacking the
siliceous frustule and swell to the
maximum frustule size. The auxospore
then forms an initial cell which forms
a new frustule of maximum size within
itself.

 
[1] Fig. 1. A consensus phylogeny of
eukaryotes. The vast majority of
characterized eukaryotes, with the
notable exception of major subgroups of
amoebae, can now be assigned to one of
eight major groups. Opisthokonts (basal
flagellum) have a single basal
flagellum on reproductive cells and
flat mitochondrial cristae (most
eukaryotes have tubular ones).
Eukaryotic photosynthesis originated in
Plants; theirs are the only plastids
with just two outer membranes.
Heterokonts (different flagellae) have
a unique flagellum decorated with
hollow tripartite hairs (stramenopiles)
and, usually, a second plain one.
Cercozoans are amoebae with filose
pseudopodia, often living with in tests
(hard outer shells), some very
elaborate (foraminiferans). Amoebozoa
are mostly naked amoebae (lacking
tests), often with lobose pseudopodia
for at least part of their life cycle.
Alveolates have systems of cortical
alveoli directly beneath their plasma
membranes. Discicristates have discoid
mitochondrial cristae and, in some
cases, a deep (excavated) ventral
feeding groove. Amitochondrial
excavates lack substantial molecular
phylogenetic support, but most have an
excavated ventral feeding groove, and
all lack mitochondria. The tree shown
is based on a consensus of molecular
(1-4) and ultrastructural (16, 17) data
and includes a rough indication of new
ciPCR ''taxa'' (broken black lines)
(7-11). An asterisk preceding the taxon
name indicates probable paraphyletic
group COPYRIGHTED
source: http://www.sciencemag.org/cgi/co
ntent/full/300/5626/1703


[2] Figure 1. Phylogenetic hypothesis
of the eukaryotic lineage based on
ultrastructural and molecular data.
Organisms are divided into three main
groups distinguished by mitochondrial
cristal shape (either discoidal,
flattened or tubular). Unbroken lines
indicate phylogenetic relationships
that are firmly supported by available
data; broken lines indicate
uncertainties in phylogenetic
placement, resolution of which will
require additional data. Color coding
of organismal genus names indicates
mitochondrial genomes that have been
completely (Table 1), almost completely
(Jakoba, Naegleria and
Thraustochytrium) or partially (*)
sequenced by the OGMP (red), the FMGP
(black) or other groups (green). Names
in blue indicate those species whose
mtDNAs are currently being sequenced by
the OGMP or are future candidates for
complete sequencing. Amitochondriate
retortamonads are positioned at the
base of the tree, with broken arrows
denoting the endosymbiotic origin(s) of
mitochondria from a Rickettsia-like
eubacterium. Macrophar.,
Macropharyngomonas. COPYRIGHTED
source: http://nar.oxfordjournals.org/cg
i/content/full/26/4/865

1,967,000,000 YBN
309) Chromalveolate Heterokont, Water
molds (Oomycetes OemISETEZ) evolve.

Genetic
comparison shows the ancestor of the
Chromalveolate Heterokont Water molds
(Oomycetes OemISETEZ) evolving now.

Oomycetes (Water molds), with about 580
species, vary from unicellular, to
multicellular highly brached
filamentous forms. The filamentous
form is called "coenocytic" (grows as a
large multinucleate cell that results
from multiple nuclear divisions without
cell divisions, also called "mycelium"
in fungi) Oomycetes grow by closed
(or nearly closed) mitosis with pairs
of centrioles near the poles .
Filamentous forms grow by mitosis, but
only the nucleus is duplicated
(karyokinesis), no septa (horizontal
cell wall) is constructed, making these
multinucleate very large single cells.
Technically, filamentous oomycetes are
3 celled multicellular organisms
because a septa forms between the
vegetative filament and the diploid
sporangium (and oogonium) cells (and
the haploid antheridium multinucleate
cells are not free swimming), but many
people label oomycetes as single celled
organism. But it appears clear that
oomycetes would be constructed of many
cells if a cell wall was built at
mitosis. Sexual forms are diploid and
reproduce by conjugation.

Water Molds are microscopic organisms
that reproduce both sexually and
asexually and are composed of mycelia,
or a tube-like vegetative body (all of
an organism's mycelia are called its
thallus). The name "water mould" refers
to the fact that they thrive under
conditions of high humidity and running
surface water.

Water molds were originally classified
as fungi, but are now known to have
developed separately and show a number
of differences. Their cell walls are
composed of cellulose rather than
chitin and lack septa (a wall that
divides two spaces) except where
reproductive cells are produced, in
addition to having gene sequences more
closely related to brown algae than
fungi. Also, in the vegetative state
they have diploid nuclei, whereas fungi
have haploid nuclei.

The oomycetes include the water molds,
white rusts and the downy mildews. Many
oomycetes are multinucleate filaments
(hyphae) that resemble fungi. These
hyphae have no cross walls, but are one
long hollow tube and are called
"coenocytic". They were once thought to
be related to the fungi, but their cell
walls are made of cellulose, not chitin
as they are in the true fungi. The
superficial resemblance of the fungi
and the oomycetes is likely a case of
convergent evolution. Both groups have
a filamentous (hyphal) body form with a
high surface area to volume ration
which facilitates uptake of nutrients
from their surroundings.

The oomycetes are saprobic and
parasitic forms, including water molds
like Saprolegnia and downey mildews
like Peronospora.

1. These organisms (and slime
molds) resemble fungi but all have
flagellated cells which fungi never
do.
2. Water molds possess a cell
wall but it is made of cellulose, not
chitin as in fungi.
3. Water molds
produce diploid (2n) zoospores and
meiosis produces the gametes.

2. Aquatic water molds
parasitize fishes, forming furry
growths on their gills, and decompose
remains.
3. Terrestrial water molds
parasitize insects and plants; a water
mold caused the 1840s Irish potato
famine.
4. Water molds have a
filamentous body but cell walls are
composed largely of cellulose.
5. During
asexual reproduction, they produce
diploid motile spores (2n zoospores)
with flagella.
6. Unlike fungi, the adult
is diploid; gametes are produced by
meiosis.
7. Eggs are produced in
enlarged oogonia.

 
[1] Fig. 1. A consensus phylogeny of
eukaryotes. The vast majority of
characterized eukaryotes, with the
notable exception of major subgroups of
amoebae, can now be assigned to one of
eight major groups. Opisthokonts (basal
flagellum) have a single basal
flagellum on reproductive cells and
flat mitochondrial cristae (most
eukaryotes have tubular ones).
Eukaryotic photosynthesis originated in
Plants; theirs are the only plastids
with just two outer membranes.
Heterokonts (different flagellae) have
a unique flagellum decorated with
hollow tripartite hairs (stramenopiles)
and, usually, a second plain one.
Cercozoans are amoebae with filose
pseudopodia, often living with in tests
(hard outer shells), some very
elaborate (foraminiferans). Amoebozoa
are mostly naked amoebae (lacking
tests), often with lobose pseudopodia
for at least part of their life cycle.
Alveolates have systems of cortical
alveoli directly beneath their plasma
membranes. Discicristates have discoid
mitochondrial cristae and, in some
cases, a deep (excavated) ventral
feeding groove. Amitochondrial
excavates lack substantial molecular
phylogenetic support, but most have an
excavated ventral feeding groove, and
all lack mitochondria. The tree shown
is based on a consensus of molecular
(1-4) and ultrastructural (16, 17) data
and includes a rough indication of new
ciPCR ''taxa'' (broken black lines)
(7-11). An asterisk preceding the taxon
name indicates probable paraphyletic
group COPYRIGHTED
source: http://www.sciencemag.org/cgi/co
ntent/full/300/5626/1703


[2] Figure 1. Phylogenetic hypothesis
of the eukaryotic lineage based on
ultrastructural and molecular data.
Organisms are divided into three main
groups distinguished by mitochondrial
cristal shape (either discoidal,
flattened or tubular). Unbroken lines
indicate phylogenetic relationships
that are firmly supported by available
data; broken lines indicate
uncertainties in phylogenetic
placement, resolution of which will
require additional data. Color coding
of organismal genus names indicates
mitochondrial genomes that have been
completely (Table 1), almost completely
(Jakoba, Naegleria and
Thraustochytrium) or partially (*)
sequenced by the OGMP (red), the FMGP
(black) or other groups (green). Names
in blue indicate those species whose
mtDNAs are currently being sequenced by
the OGMP or are future candidates for
complete sequencing. Amitochondriate
retortamonads are positioned at the
base of the tree, with broken arrows
denoting the endosymbiotic origin(s) of
mitochondria from a Rickettsia-like
eubacterium. Macrophar.,
Macropharyngomonas. COPYRIGHTED
source: http://nar.oxfordjournals.org/cg
i/content/full/26/4/865

1,966,000,000 YBN
310) Chromalveolate Alveolata
(Ciliates, Dinoflagellates,
Apicomplexans) evolve.

Genetic comparison
shows the ancestor of the
Chromalveolate Alveolata (Ciliates,
Dinoflagellates, Apicomplexans)
evolving now.

The alveolates are a major line of
protists. There are three main groups,
which are very divergent in form, but
are now known to be close relatives
based on various ultrastructural and
genetic similarities:
Ciliates Very common protozoa,
with many short cilia arranged in rows
Apicom
plexa Parasitic protozoa that lack
locomotive structures except in
gametes
Dinoflagellates Mostly marine
flagellates, many of which have
chloroplasts

The most notable shared characteristic
is the presence of cortical alveoli,
flattened vesicles packed into a
continuous layer supporting the
membrane, typically forming a flexible
pellicle. In dinoflagellates they often
form armor plates. Alveolates have
mitochondria with tubular cristae, and
their flagella or cilia have a distinct
structure.

The Apicomplexa and dinoflagellates may
be more closely related to each other
than to the ciliates. Both have
plastids, and most share a bundle or
cone of microtubules at the top of the
cell. In apicomplexans this forms part
of a complex used to enter host cells,
while in some colorless dinoflagellates
it forms a peduncle used to ingest
prey.

 
[1] Fig. 1. A consensus phylogeny of
eukaryotes. The vast majority of
characterized eukaryotes, with the
notable exception of major subgroups of
amoebae, can now be assigned to one of
eight major groups. Opisthokonts (basal
flagellum) have a single basal
flagellum on reproductive cells and
flat mitochondrial cristae (most
eukaryotes have tubular ones).
Eukaryotic photosynthesis originated in
Plants; theirs are the only plastids
with just two outer membranes.
Heterokonts (different flagellae) have
a unique flagellum decorated with
hollow tripartite hairs (stramenopiles)
and, usually, a second plain one.
Cercozoans are amoebae with filose
pseudopodia, often living with in tests
(hard outer shells), some very
elaborate (foraminiferans). Amoebozoa
are mostly naked amoebae (lacking
tests), often with lobose pseudopodia
for at least part of their life cycle.
Alveolates have systems of cortical
alveoli directly beneath their plasma
membranes. Discicristates have discoid
mitochondrial cristae and, in some
cases, a deep (excavated) ventral
feeding groove. Amitochondrial
excavates lack substantial molecular
phylogenetic support, but most have an
excavated ventral feeding groove, and
all lack mitochondria. The tree shown
is based on a consensus of molecular
(1-4) and ultrastructural (16, 17) data
and includes a rough indication of new
ciPCR ''taxa'' (broken black lines)
(7-11). An asterisk preceding the taxon
name indicates probable paraphyletic
group COPYRIGHTED
source: http://www.sciencemag.org/cgi/co
ntent/full/300/5626/1703


[2] Figure 1. Phylogenetic hypothesis
of the eukaryotic lineage based on
ultrastructural and molecular data.
Organisms are divided into three main
groups distinguished by mitochondrial
cristal shape (either discoidal,
flattened or tubular). Unbroken lines
indicate phylogenetic relationships
that are firmly supported by available
data; broken lines indicate
uncertainties in phylogenetic
placement, resolution of which will
require additional data. Color coding
of organismal genus names indicates
mitochondrial genomes that have been
completely (Table 1), almost completely
(Jakoba, Naegleria and
Thraustochytrium) or partially (*)
sequenced by the OGMP (red), the FMGP
(black) or other groups (green). Names
in blue indicate those species whose
mtDNAs are currently being sequenced by
the OGMP or are future candidates for
complete sequencing. Amitochondriate
retortamonads are positioned at the
base of the tree, with broken arrows
denoting the endosymbiotic origin(s) of
mitochondria from a Rickettsia-like
eubacterium. Macrophar.,
Macropharyngomonas. COPYRIGHTED
source: http://nar.oxfordjournals.org/cg
i/content/full/26/4/865

1,964,000,000 YBN
312) Ciliates evolve.
Genetic comparison shows
the ancestor of the Chromalveolate
Alveolata Ciliates evolving now.

The ciliates are one of the most
important groups of protists, common
almost everywhere there is water -
lakes, ponds, oceans, and soils, with
many ecto- (lives on host) and
endosymbiotic (lives in host) members,
as well as some obligate (depends on
host for survival) and opportunistic
parasites (does not depend on host for
survival). Ciliates tend to be large
protists, a few reaching 2 mm in
length, and are some of the most
complex in structure. The name ciliate
comes from the presence of hair-like
organelles called cilia, which are
identical in structure to flagella but
typically shorter and present in much
larger numbers. Cilia occur in all
members of the group, although the
peculiar suctoria only have them for
part of the life-cycle, and are
variously used in swimming, crawling,
attachment, feeding, and sensation.

Unlike other eukaryotes, ciliates have
two different sorts of nuclei: a small,
diploid micronucleus (reproduction),
and a large, polyploid macronucleus
(general cell regulation). The latter
is generated from the micronucleus by
amplification of the genome and heavy
editing. The high degree of polyploidi
allows the cell to sustain an
appropriate level of transcription.
Division of the macronucleus does not
occur by a mitotic process but
segregation of the chromosomes is by a
different process, whose mechanism is
unknown. This process is not perfect,
and after about 200 generations the
cell shows signs of aging (has so many
mutations that it does not function
properly). Periodically the macronuclei
is (must be?) regenerated from the
micronuclei. In most, this occurs
during sexual reproduction, which is
not usually through syngamy but through
conjugation. Here two cells line up,
the micronuclei undergo meiosis, some
of the haploid daughters are exchanged
and then fuse to form new micro- and
macronuclei.

With a few exceptions, there is a
distinct cytostome or mouth where
ingestion takes place. Food vacuoles
are formed through phagocytosis and
typically follow a particular path
through the cell as their contents are
digested and broken down via lysosomes
so the substances the vacuole contains
are then small enough to diffuse
through the membrane of the food
vacuole into the cell. Anything left in
the food vacuole by the time it reaches
the cytoproct (anus) is discharged via
exocytosis. Most ciliates also have one
or more prominent contractile vacuoles,
which collect water and expel it from
the cell to maintain osmotic pressure,
or in some function to maintain ionic
balance. These often have a distinctive
star-shape, with each point being a
collecting tube.

Most ciliates feed on smaller organisms
(heterotrophic), such as bacteria and
algae, and detritus swept into the
mouth by modified oral cilia. These
usually include a series of
membranelles to the left of the mouth
and a paroral membrane to its right,
both of which arise from polykinetids,
groups of many cilia together with
associated structures. This varies
considerably, however. Some ciliates
are mouthless and feed by absorption,
while others are predatory and feed on
other protozoa and in particular on
other ciliates. This includes the
suctoria, which feed through several
specialized tentacles.

Ciliates and Amoeboids have in common:
Food is
digested in food vacuoles.
Excess water is
expelled by contractile vacuoles.

 
[1] Fig. 1. A consensus phylogeny of
eukaryotes. The vast majority of
characterized eukaryotes, with the
notable exception of major subgroups of
amoebae, can now be assigned to one of
eight major groups. Opisthokonts (basal
flagellum) have a single basal
flagellum on reproductive cells and
flat mitochondrial cristae (most
eukaryotes have tubular ones).
Eukaryotic photosynthesis originated in
Plants; theirs are the only plastids
with just two outer membranes.
Heterokonts (different flagellae) have
a unique flagellum decorated with
hollow tripartite hairs (stramenopiles)
and, usually, a second plain one.
Cercozoans are amoebae with filose
pseudopodia, often living with in tests
(hard outer shells), some very
elaborate (foraminiferans). Amoebozoa
are mostly naked amoebae (lacking
tests), often with lobose pseudopodia
for at least part of their life cycle.
Alveolates have systems of cortical
alveoli directly beneath their plasma
membranes. Discicristates have discoid
mitochondrial cristae and, in some
cases, a deep (excavated) ventral
feeding groove. Amitochondrial
excavates lack substantial molecular
phylogenetic support, but most have an
excavated ventral feeding groove, and
all lack mitochondria. The tree shown
is based on a consensus of molecular
(1-4) and ultrastructural (16, 17) data
and includes a rough indication of new
ciPCR ''taxa'' (broken black lines)
(7-11). An asterisk preceding the taxon
name indicates probable paraphyletic
group COPYRIGHTED
source: http://www.sciencemag.org/cgi/co
ntent/full/300/5626/1703


[2] Figure 1. Phylogenetic hypothesis
of the eukaryotic lineage based on
ultrastructural and molecular data.
Organisms are divided into three main
groups distinguished by mitochondrial
cristal shape (either discoidal,
flattened or tubular). Unbroken lines
indicate phylogenetic relationships
that are firmly supported by available
data; broken lines indicate
uncertainties in phylogenetic
placement, resolution of which will
require additional data. Color coding
of organismal genus names indicates
mitochondrial genomes that have been
completely (Table 1), almost completely
(Jakoba, Naegleria and
Thraustochytrium) or partially (*)
sequenced by the OGMP (red), the FMGP
(black) or other groups (green). Names
in blue indicate those species whose
mtDNAs are currently being sequenced by
the OGMP or are future candidates for
complete sequencing. Amitochondriate
retortamonads are positioned at the
base of the tree, with broken arrows
denoting the endosymbiotic origin(s) of
mitochondria from a Rickettsia-like
eubacterium. Macrophar.,
Macropharyngomonas. COPYRIGHTED
source: http://nar.oxfordjournals.org/cg
i/content/full/26/4/865

1,963,000,000 YBN
313) Dinoflagellates evolve.
Genetic Ribosomal
RNA comparison shows Chromalveolate
Alveolata, Dinoflagellates evolve.
Dinoflagellat
es reproduce mainly by haploid mitosis,
but also reproduce sexually.

In dinoflagellates, the chromosomes are
always visible and do not condense
prior to mitosis. The chromosomes are
attached to the nuclear envelope, which
persists during mitosis.

The main method of reproduction of the
dinoflagellates is by longitudinal cell
division, with each daughter cell
receiving one of the flagella ad a
portion of the theca and then
constructing the missing parts in a
very intricate sequence. Some
nonmotile species form zoospores, which
may be colonial. A number of species
reproduce sexually, mostly by isogamy,
but a few species reproduce by
heterogamy (anisogamy).

Dinoflagellate zygotes are similar to
some acritarchs (early eukaryote
fossils).

Some Dinoflagellates produce cysts.

The dinoflagellates are a large group
of flagellate protists. Most are marine
plankton, but they are common in fresh
water habitats as well; their
populations are distributed depending
on temperate, saltiness, or depth.
About half of all dinoflagellates are
photosynthetic, and these make up the
largest group of eukaryotic algae aside
from the diatoms. Being primary
producers make them an important part
of the food chain. Some species, called
zooxanthellae, are endosymbionts of
marine animals and protozoa, and play
an important part in the biology of
coral reefs. Other dinoflagellates are
colorless predators on other protozoa,
and a few forms are parasitic.

Some dinoflagellates are reported to be
filamentous (multicellular).
Mitochondri
a christae are tubular.
Dinoflagellates
are haploid (haplontic).

 
[1] Fig. 1. A consensus phylogeny of
eukaryotes. The vast majority of
characterized eukaryotes, with the
notable exception of major subgroups of
amoebae, can now be assigned to one of
eight major groups. Opisthokonts (basal
flagellum) have a single basal
flagellum on reproductive cells and
flat mitochondrial cristae (most
eukaryotes have tubular ones).
Eukaryotic photosynthesis originated in
Plants; theirs are the only plastids
with just two outer membranes.
Heterokonts (different flagellae) have
a unique flagellum decorated with
hollow tripartite hairs (stramenopiles)
and, usually, a second plain one.
Cercozoans are amoebae with filose
pseudopodia, often living with in tests
(hard outer shells), some very
elaborate (foraminiferans). Amoebozoa
are mostly naked amoebae (lacking
tests), often with lobose pseudopodia
for at least part of their life cycle.
Alveolates have systems of cortical
alveoli directly beneath their plasma
membranes. Discicristates have discoid
mitochondrial cristae and, in some
cases, a deep (excavated) ventral
feeding groove. Amitochondrial
excavates lack substantial molecular
phylogenetic support, but most have an
excavated ventral feeding groove, and
all lack mitochondria. The tree shown
is based on a consensus of molecular
(1-4) and ultrastructural (16, 17) data
and includes a rough indication of new
ciPCR ''taxa'' (broken black lines)
(7-11). An asterisk preceding the taxon
name indicates probable paraphyletic
group COPYRIGHTED
source: http://www.sciencemag.org/cgi/co
ntent/full/300/5626/1703


[2] Figure 1. Phylogenetic hypothesis
of the eukaryotic lineage based on
ultrastructural and molecular data.
Organisms are divided into three main
groups distinguished by mitochondrial
cristal shape (either discoidal,
flattened or tubular). Unbroken lines
indicate phylogenetic relationships
that are firmly supported by available
data; broken lines indicate
uncertainties in phylogenetic
placement, resolution of which will
require additional data. Color coding
of organismal genus names indicates
mitochondrial genomes that have been
completely (Table 1), almost completely
(Jakoba, Naegleria and
Thraustochytrium) or partially (*)
sequenced by the OGMP (red), the FMGP
(black) or other groups (green). Names
in blue indicate those species whose
mtDNAs are currently being sequenced by
the OGMP or are future candidates for
complete sequencing. Amitochondriate
retortamonads are positioned at the
base of the tree, with broken arrows
denoting the endosymbiotic origin(s) of
mitochondria from a Rickettsia-like
eubacterium. Macrophar.,
Macropharyngomonas. COPYRIGHTED
source: http://nar.oxfordjournals.org/cg
i/content/full/26/4/865

1,962,000,000 YBN
314) Apicomplexans evolve.
Genetic comparison
shows Apicomplexans evolve.
The
Apicomplexa are a large group of
protozoa, characterized by the presence
of an apical complex at some point in
their life-cycle. They are exclusively
parasitic, and completely lack flagella
or pseudopods except for certain gamete
stages. Diseases caused by Apicomplexa
include:

* Babesiosis (Babesia)
*
Cryptosporidiosis (Cryptosporidium)
* Malaria
(Plasmodium)
* Toxoplasmosis (Toxoplasma
gondii)

Most members have a complex life-cycle,
involving both asexual and sexual
reproduction. Typically, a host is
infected by ingesting cysts, which
divide to produce sporozoites that
enter its cells. Eventually, the cells
burst, releasing merozoites which
infect new cells. This may occur
several times, until gamonts are
produced, forming gametes that fuse to
create new cysts. There are many
variations on this basic pattern,
however, and many Apicomplexa have more
than one host.

 
[1] Fig. 1. A consensus phylogeny of
eukaryotes. The vast majority of
characterized eukaryotes, with the
notable exception of major subgroups of
amoebae, can now be assigned to one of
eight major groups. Opisthokonts (basal
flagellum) have a single basal
flagellum on reproductive cells and
flat mitochondrial cristae (most
eukaryotes have tubular ones).
Eukaryotic photosynthesis originated in
Plants; theirs are the only plastids
with just two outer membranes.
Heterokonts (different flagellae) have
a unique flagellum decorated with
hollow tripartite hairs (stramenopiles)
and, usually, a second plain one.
Cercozoans are amoebae with filose
pseudopodia, often living with in tests
(hard outer shells), some very
elaborate (foraminiferans). Amoebozoa
are mostly naked amoebae (lacking
tests), often with lobose pseudopodia
for at least part of their life cycle.
Alveolates have systems of cortical
alveoli directly beneath their plasma
membranes. Discicristates have discoid
mitochondrial cristae and, in some
cases, a deep (excavated) ventral
feeding groove. Amitochondrial
excavates lack substantial molecular
phylogenetic support, but most have an
excavated ventral feeding groove, and
all lack mitochondria. The tree shown
is based on a consensus of molecular
(1-4) and ultrastructural (16, 17) data
and includes a rough indication of new
ciPCR ''taxa'' (broken black lines)
(7-11). An asterisk preceding the taxon
name indicates probable paraphyletic
group COPYRIGHTED
source: http://www.sciencemag.org/cgi/co
ntent/full/300/5626/1703


[2] Figure 1. Phylogenetic hypothesis
of the eukaryotic lineage based on
ultrastructural and molecular data.
Organisms are divided into three main
groups distinguished by mitochondrial
cristal shape (either discoidal,
flattened or tubular). Unbroken lines
indicate phylogenetic relationships
that are firmly supported by available
data; broken lines indicate
uncertainties in phylogenetic
placement, resolution of which will
require additional data. Color coding
of organismal genus names indicates
mitochondrial genomes that have been
completely (Table 1), almost completely
(Jakoba, Naegleria and
Thraustochytrium) or partially (*)
sequenced by the OGMP (red), the FMGP
(black) or other groups (green). Names
in blue indicate those species whose
mtDNAs are currently being sequenced by
the OGMP or are future candidates for
complete sequencing. Amitochondriate
retortamonads are positioned at the
base of the tree, with broken arrows
denoting the endosymbiotic origin(s) of
mitochondria from a Rickettsia-like
eubacterium. Macrophar.,
Macropharyngomonas. COPYRIGHTED
source: http://nar.oxfordjournals.org/cg
i/content/full/26/4/865

1,961,000,000 YBN
89) Genetic comparison shows Rhizaria
(the Phyla "Radiolaria", "Cercozoa",
and "Foraminifera") evolve now.

This marks the beginning of the
protists described as "amoeboid",
because they have pseudopods.

5. Amoeboids
phagocytize their food; pseudopods
surround and engulf prey.
6. Food is digested
inside food vacuoles.
7. Freshwater amoeboids
have contractile vacuoles to eliminate
excess water.

Some foraminifera are haplodiploid
(alternate between haploid and diploid
cycles that both have mitosis).

The Rhizaria are a major line of
protists. They vary considerably in
form, but for the most part they are
amoeboids with filose, reticulose, or
microtubule-supported pseudopods. Many
produce shells or skeletons, which may
be quite complex in structure, and
these make up the vast majority of
protozoan fossils. Nearly all have
mitochondria with tubular cristae.
There
are three main groups of Rhizaria:
Cercozoa
Various amoebae and flagellates,
usually with filose pseudopods and
common in soil
Foraminifera Amoeboids with
reticulose pseudopods, common as marine
benthos
Radiolaria Amoeboids with axopods,
common as marine plankton

The name Rhizaria was created recently
by Cavalier-Smith in 2002. Most are
biciliate amoeboflagellates at some
point in the life cycle. Pseudopodia
are root-like reticulopodia, filopodia
and/or axopodia - not broad lobopodia
as in Amoeba. All of these features
can, however, be found in members of
other clades. Nevertheless, the
Rhizaria are supported by both rRNA and
actin trees (Cavalier-Smith & Chao,
2003; Nikolaev et al. 2004).

 
[1] FIG. 2. The tree of life based on
molecular, ultrastructural and
palaeontological evidence. Contrary to
widespread assumptions, the root is
among the eubacteria, probably within
the double-enveloped Negibacteria, not
between eubacteria and archaebacteria
(Cavalier-Smith, 2002b); it may lie
between Eobacteria and other
Negibacteria (Cavalier-Smith, 2002b).
The position of the eukaryotic root has
been nearly as controversial, but is
less hard to establish: it probably
lies between unikonts and bikonts (Lang
et al., 2002; Stechmann and
Cavalier-Smith, 2002, 2003). For
clarity the basal eukaryotic kingdom
Protozoa is not labelled; it comprises
four major groups (alveolates, cabozoa,
Amoebozoa and Choanozoa) plus the small
bikont phylum Apusozoa of unclear
precise position; whether Heliozoa are
protozoa as shown or chromists is
uncertain (Cavalier-Smith, 2003b).
Symbiogenetic cell enslavement occurred
four or five times: in the origin of
mitochondria and chloroplasts from
different negibacteria, of
chromalveolates by the enslaving of a
red alga (Cavalier-Smith, 1999, 2003;
Harper and Keeling, 2003) and in the
origin of the green plastids of
euglenoid (excavate) and chlorarachnean
(cercozoan) algae-a green algal cell
was enslaved either by the ancestral
cabozoan (arrow) or (less likely) twice
independently within excavates and
Cercozoa (asterisks) (Cavalier-Smith,
2003a). The upper thumbnail sketch
shows membrane topology in the
chimaeric cryptophytes (class
Cryptophyceae of the phylum Cryptista);
in the ancestral chromist the former
food vacuole membrane fused with the
rough endoplasmic reticulum placing the
enslaved cell within its lumen (red) to
yield the complex membrane topology
shown. The large host nucleus and the
tiny nucleomorph are shown in blue,
chloroplast green and mitochondrion
purple. In chlorarachneans (class
Chlorarachnea of phylum Cercozoa) the
former food vacuole membrane remained
topologically distinct from the ER to
become an epiplastid membrane and so
did not acquire ribosomes on its
surface, but their membrane topology is
otherwise similar to the cryptophytes.
The other sketches portray the four
major kinds of cell in the living world
and their membrane topology. The upper
ones show the contrasting ancestral
microtubular cytoskeleton (ciliary
roots, in red) of unikonts (a cone of
single microtubules attaching the
single centriole to the nucleus, blue)
and bikonts (two bands of microtubules
attached to the posterior centriole and
an anterior fan of microtubules
attached to the anterior centriole).
The lower ones show the single plasma
membrane of unibacteria (posibacteria
plus archaebacteria), which were
ancestral to eukaryotes and the double
envelope of negibacteria, which were
ancestral to mitochondria and
chloroplasts (which retained the outer
membrane, red).
source: http://aob.oxfordjournals.org/cg
i/content/full/95/1/147/FIG2


[2] Fig. 1. A consensus phylogeny of
eukaryotes. The vast majority of
characterized eukaryotes, with the
notable exception of major subgroups of
amoebae, can now be assigned to one of
eight major groups. Opisthokonts (basal
flagellum) have a single basal
flagellum on reproductive cells and
flat mitochondrial cristae (most
eukaryotes have tubular ones).
Eukaryotic photosynthesis originated in
Plants; theirs are the only plastids
with just two outer membranes.
Heterokonts (different flagellae) have
a unique flagellum decorated with
hollow tripartite hairs (stramenopiles)
and, usually, a second plain one.
Cercozoans are amoebae with filose
pseudopodia, often living with in tests
(hard outer shells), some very
elaborate (foraminiferans). Amoebozoa
are mostly naked amoebae (lacking
tests), often with lobose pseudopodia
for at least part of their life cycle.
Alveolates have systems of cortical
alveoli directly beneath their plasma
membranes. Discicristates have discoid
mitochondrial cristae and, in some
cases, a deep (excavated) ventral
feeding groove. Amitochondrial
excavates lack substantial molecular
phylogenetic support, but most have an
excavated ventral feeding groove, and
all lack mitochondria. The tree shown
is based on a consensus of molecular
(1-4) and ultrastructural (16, 17) data
and includes a rough indication of new
ciPCR ''taxa'' (broken black lines)
(7-11). An asterisk preceding the taxon
name indicates probable paraphyletic
group.
source: http://www.sciencemag.org/cgi/co
ntent/full/300/5626/1703

1,961,000,000 YBN
320) Rhizaria Phylum "Cercozoa" evolve
now.

The Cercozoa are a group of protists,
including most amoeboids and
flagellates that feed by means of
filose pseudopods. These may be
restricted to part of the cell surface,
but there is never a true cytostome or
mouth as found in many other protozoa.
They show a variety of forms and have
proven difficult to define in terms of
structural characteristics, although
their unity is strongly supported by
genetic studies.

 
[1] FIG. 2. The tree of life based on
molecular, ultrastructural and
palaeontological evidence. Contrary to
widespread assumptions, the root is
among the eubacteria, probably within
the double-enveloped Negibacteria, not
between eubacteria and archaebacteria
(Cavalier-Smith, 2002b); it may lie
between Eobacteria and other
Negibacteria (Cavalier-Smith, 2002b).
The position of the eukaryotic root has
been nearly as controversial, but is
less hard to establish: it probably
lies between unikonts and bikonts (Lang
et al., 2002; Stechmann and
Cavalier-Smith, 2002, 2003). For
clarity the basal eukaryotic kingdom
Protozoa is not labelled; it comprises
four major groups (alveolates, cabozoa,
Amoebozoa and Choanozoa) plus the small
bikont phylum Apusozoa of unclear
precise position; whether Heliozoa are
protozoa as shown or chromists is
uncertain (Cavalier-Smith, 2003b).
Symbiogenetic cell enslavement occurred
four or five times: in the origin of
mitochondria and chloroplasts from
different negibacteria, of
chromalveolates by the enslaving of a
red alga (Cavalier-Smith, 1999, 2003;
Harper and Keeling, 2003) and in the
origin of the green plastids of
euglenoid (excavate) and chlorarachnean
(cercozoan) algae-a green algal cell
was enslaved either by the ancestral
cabozoan (arrow) or (less likely) twice
independently within excavates and
Cercozoa (asterisks) (Cavalier-Smith,
2003a). The upper thumbnail sketch
shows membrane topology in the
chimaeric cryptophytes (class
Cryptophyceae of the phylum Cryptista);
in the ancestral chromist the former
food vacuole membrane fused with the
rough endoplasmic reticulum placing the
enslaved cell within its lumen (red) to
yield the complex membrane topology
shown. The large host nucleus and the
tiny nucleomorph are shown in blue,
chloroplast green and mitochondrion
purple. In chlorarachneans (class
Chlorarachnea of phylum Cercozoa) the
former food vacuole membrane remained
topologically distinct from the ER to
become an epiplastid membrane and so
did not acquire ribosomes on its
surface, but their membrane topology is
otherwise similar to the cryptophytes.
The other sketches portray the four
major kinds of cell in the living world
and their membrane topology. The upper
ones show the contrasting ancestral
microtubular cytoskeleton (ciliary
roots, in red) of unikonts (a cone of
single microtubules attaching the
single centriole to the nucleus, blue)
and bikonts (two bands of microtubules
attached to the posterior centriole and
an anterior fan of microtubules
attached to the anterior centriole).
The lower ones show the single plasma
membrane of unibacteria (posibacteria
plus archaebacteria), which were
ancestral to eukaryotes and the double
envelope of negibacteria, which were
ancestral to mitochondria and
chloroplasts (which retained the outer
membrane, red).
source: http://aob.oxfordjournals.org/cg
i/content/full/95/1/147/FIG2


[2] Fig. 1. A consensus phylogeny of
eukaryotes. The vast majority of
characterized eukaryotes, with the
notable exception of major subgroups of
amoebae, can now be assigned to one of
eight major groups. Opisthokonts (basal
flagellum) have a single basal
flagellum on reproductive cells and
flat mitochondrial cristae (most
eukaryotes have tubular ones).
Eukaryotic photosynthesis originated in
Plants; theirs are the only plastids
with just two outer membranes.
Heterokonts (different flagellae) have
a unique flagellum decorated with
hollow tripartite hairs (stramenopiles)
and, usually, a second plain one.
Cercozoans are amoebae with filose
pseudopodia, often living with in tests
(hard outer shells), some very
elaborate (foraminiferans). Amoebozoa
are mostly naked amoebae (lacking
tests), often with lobose pseudopodia
for at least part of their life cycle.
Alveolates have systems of cortical
alveoli directly beneath their plasma
membranes. Discicristates have discoid
mitochondrial cristae and, in some
cases, a deep (excavated) ventral
feeding groove. Amitochondrial
excavates lack substantial molecular
phylogenetic support, but most have an
excavated ventral feeding groove, and
all lack mitochondria. The tree shown
is based on a consensus of molecular
(1-4) and ultrastructural (16, 17) data
and includes a rough indication of new
ciPCR ''taxa'' (broken black lines)
(7-11). An asterisk preceding the taxon
name indicates probable paraphyletic
group.
source: http://www.sciencemag.org/cgi/co
ntent/full/300/5626/1703

1,960,000,000 YBN
319) Rhizaria Phylum "Radiolaria"
evolve now.

Ribosomal RNA indicates that
Rhizaria Phylum "Radiolaria" evolve
now.

Radiolarians (also radiolaria) are
amoeboid protozoa that produce
intricate mineral skeletons, typically
with a central capsule dividing the
cell into inner and outer portions,
called endoplasm and ectoplasm. They
are found as plankton throughout the
ocean, and their shells are important
fossils found from the Cambrian
onwards.

Move by pseudopodia.
external tests
made of silica (glass).

Radiolaria have a test composed of
silica or strontium sulfate.
Most have a radial
arrangement of spines.
Pseudopods (actinopods)
project from an external layer of
cytoplasm and are supported by rows of
microtubules.
Tests of dead foraminiferans and
radiolarians form deep layers of ocean
floor sediment.
Back to the Precambrian, each
layer has distinctive foraminiferans
which helps date rocks.
Over hundreds of
millions of years, the CaCO3 shells
have contributed to the formation of
chalk deposits (i.e. White Cliffs of
Dover, limestone of pyramids).

Lifecycle
Simple asexual fission of radiolarian
cells has been observed. Sexual
reproduction has not been confirmed but
is assumed to occur; possible
gametogenesis has been observed in the
form of "swarmers" being expelled from
swellings in the cell. Swarmers are
formed from the central capsule after
the ectoplasm has been discarded. The
central capsule sinks through the water
column to depths hundreds of meters
greater than the normal habitat and
swells, eventually rupturing and
releasing the flagellated cells.
Recombination of these cells, which are
assumed to be haploid, to produce
diploid "adults" has not been observed
however and is only inferred to occur.
Comparisons of standing crops within
the water column and sediment trap
samples have ascertained that the
average life span of radiolarians is
about two weeks, ranging from a few
days to a few weeks.

 
[1] FIG. 2. The tree of life based on
molecular, ultrastructural and
palaeontological evidence. Contrary to
widespread assumptions, the root is
among the eubacteria, probably within
the double-enveloped Negibacteria, not
between eubacteria and archaebacteria
(Cavalier-Smith, 2002b); it may lie
between Eobacteria and other
Negibacteria (Cavalier-Smith, 2002b).
The position of the eukaryotic root has
been nearly as controversial, but is
less hard to establish: it probably
lies between unikonts and bikonts (Lang
et al., 2002; Stechmann and
Cavalier-Smith, 2002, 2003). For
clarity the basal eukaryotic kingdom
Protozoa is not labelled; it comprises
four major groups (alveolates, cabozoa,
Amoebozoa and Choanozoa) plus the small
bikont phylum Apusozoa of unclear
precise position; whether Heliozoa are
protozoa as shown or chromists is
uncertain (Cavalier-Smith, 2003b).
Symbiogenetic cell enslavement occurred
four or five times: in the origin of
mitochondria and chloroplasts from
different negibacteria, of
chromalveolates by the enslaving of a
red alga (Cavalier-Smith, 1999, 2003;
Harper and Keeling, 2003) and in the
origin of the green plastids of
euglenoid (excavate) and chlorarachnean
(cercozoan) algae-a green algal cell
was enslaved either by the ancestral
cabozoan (arrow) or (less likely) twice
independently within excavates and
Cercozoa (asterisks) (Cavalier-Smith,
2003a). The upper thumbnail sketch
shows membrane topology in the
chimaeric cryptophytes (class
Cryptophyceae of the phylum Cryptista);
in the ancestral chromist the former
food vacuole membrane fused with the
rough endoplasmic reticulum placing the
enslaved cell within its lumen (red) to
yield the complex membrane topology
shown. The large host nucleus and the
tiny nucleomorph are shown in blue,
chloroplast green and mitochondrion
purple. In chlorarachneans (class
Chlorarachnea of phylum Cercozoa) the
former food vacuole membrane remained
topologically distinct from the ER to
become an epiplastid membrane and so
did not acquire ribosomes on its
surface, but their membrane topology is
otherwise similar to the cryptophytes.
The other sketches portray the four
major kinds of cell in the living world
and their membrane topology. The upper
ones show the contrasting ancestral
microtubular cytoskeleton (ciliary
roots, in red) of unikonts (a cone of
single microtubules attaching the
single centriole to the nucleus, blue)
and bikonts (two bands of microtubules
attached to the posterior centriole and
an anterior fan of microtubules
attached to the anterior centriole).
The lower ones show the single plasma
membrane of unibacteria (posibacteria
plus archaebacteria), which were
ancestral to eukaryotes and the double
envelope of negibacteria, which were
ancestral to mitochondria and
chloroplasts (which retained the outer
membrane, red).
source: http://aob.oxfordjournals.org/cg
i/content/full/95/1/147/FIG2


[2] Fig. 1. A consensus phylogeny of
eukaryotes. The vast majority of
characterized eukaryotes, with the
notable exception of major subgroups of
amoebae, can now be assigned to one of
eight major groups. Opisthokonts (basal
flagellum) have a single basal
flagellum on reproductive cells and
flat mitochondrial cristae (most
eukaryotes have tubular ones).
Eukaryotic photosynthesis originated in
Plants; theirs are the only plastids
with just two outer membranes.
Heterokonts (different flagellae) have
a unique flagellum decorated with
hollow tripartite hairs (stramenopiles)
and, usually, a second plain one.
Cercozoans are amoebae with filose
pseudopodia, often living with in tests
(hard outer shells), some very
elaborate (foraminiferans). Amoebozoa
are mostly naked amoebae (lacking
tests), often with lobose pseudopodia
for at least part of their life cycle.
Alveolates have systems of cortical
alveoli directly beneath their plasma
membranes. Discicristates have discoid
mitochondrial cristae and, in some
cases, a deep (excavated) ventral
feeding groove. Amitochondrial
excavates lack substantial molecular
phylogenetic support, but most have an
excavated ventral feeding groove, and
all lack mitochondria. The tree shown
is based on a consensus of molecular
(1-4) and ultrastructural (16, 17) data
and includes a rough indication of new
ciPCR ''taxa'' (broken black lines)
(7-11). An asterisk preceding the taxon
name indicates probable paraphyletic
group.
source: http://www.sciencemag.org/cgi/co
ntent/full/300/5626/1703

1,960,000,000 YBN
321) Rhizaria Phylum "Foraminifera"
evolve now.

Ribosomal RNA shows Rhizaria
Phylum "Foraminifera" (also known as
"Granuloreticulosea") evolve now.

Forminifera are catagorized as amoeboid
because they have pseudopods.

The Foraminifera, or forams for short,
are a large group of amoeboid protists
with reticulating pseudopods, fine
strands that branch and merge to form a
dynamic net. They typically produce a
shell, or test, which can have either
one or multiple chambers, some becoming
quite elaborate in structure. About 250
000 species are recognized, both living
and fossil. They are usually less than
1 mm in size, but some are much larger,
and the largest recorded specimen
reached 19 cm. As fossils, foraminifera
are extremely useful.
Foraminifera are
haplodiploid.
Most have a kind of shell
called a "test", which is composed of
calcium carbonate.

move by pseudopodia
most are marine
test
s are major components of limestone
used
to date marine sediments.

Foraminifera, especially the calcareous
forms, have a fossil record stretching
back to the Cambrian (Lee, 1990), and
are especially important
biostratigraphically.

b. Foraminiferans have a
multi-chambered CaCO3 (calcium
carbonate) shell; thin pseudopods
extend through holes.

Of the approximately 4000 living
species of foraminifera the life cycles
of only 20 or so are known. There are a
great variety of reproductive, growth
and feeding strategies, however the
alternation of sexual and asexual
generations is common throughout the
group and this feature differentiates
the foraminifera from other members of
the Granuloreticulosea. An asexually
produced haploid generation commonly
form a large proloculus (initial
chamber) and are therefore termed
megalospheric. Sexually produced
diploid generations tend to produce a
smaller proloculus and are therefore
termed microspheric. Importantly in
terms of the fossil record, many
foraminiferal tests are either
partially dissolved or partially
disintegrate during the reproductive
process.The planktonic foraminifera
Hastigerina pelagica reproduces by
gametogenesis at depth, the spines,
septa and apertural region are resorbed
leaving a tell-tale test.
Globigerinoides sacculiferproduces a
sac-like final chamber and additional
calcification of later chambers before
dissolution of spines occurs, this
again produces a distinctive test,
which once gametogenesis is complete
sinks to the sea bed. Since the
meiosis products have to differentiate
or mature into gametes, meiosis does
not result directly in gametes, these
species are haplodipoid
(haplodiplontic).

 
[1] FIG. 2. The tree of life based on
molecular, ultrastructural and
palaeontological evidence. Contrary to
widespread assumptions, the root is
among the eubacteria, probably within
the double-enveloped Negibacteria, not
between eubacteria and archaebacteria
(Cavalier-Smith, 2002b); it may lie
between Eobacteria and other
Negibacteria (Cavalier-Smith, 2002b).
The position of the eukaryotic root has
been nearly as controversial, but is
less hard to establish: it probably
lies between unikonts and bikonts (Lang
et al., 2002; Stechmann and
Cavalier-Smith, 2002, 2003). For
clarity the basal eukaryotic kingdom
Protozoa is not labelled; it comprises
four major groups (alveolates, cabozoa,
Amoebozoa and Choanozoa) plus the small
bikont phylum Apusozoa of unclear
precise position; whether Heliozoa are
protozoa as shown or chromists is
uncertain (Cavalier-Smith, 2003b).
Symbiogenetic cell enslavement occurred
four or five times: in the origin of
mitochondria and chloroplasts from
different negibacteria, of
chromalveolates by the enslaving of a
red alga (Cavalier-Smith, 1999, 2003;
Harper and Keeling, 2003) and in the
origin of the green plastids of
euglenoid (excavate) and chlorarachnean
(cercozoan) algae-a green algal cell
was enslaved either by the ancestral
cabozoan (arrow) or (less likely) twice
independently within excavates and
Cercozoa (asterisks) (Cavalier-Smith,
2003a). The upper thumbnail sketch
shows membrane topology in the
chimaeric cryptophytes (class
Cryptophyceae of the phylum Cryptista);
in the ancestral chromist the former
food vacuole membrane fused with the
rough endoplasmic reticulum placing the
enslaved cell within its lumen (red) to
yield the complex membrane topology
shown. The large host nucleus and the
tiny nucleomorph are shown in blue,
chloroplast green and mitochondrion
purple. In chlorarachneans (class
Chlorarachnea of phylum Cercozoa) the
former food vacuole membrane remained
topologically distinct from the ER to
become an epiplastid membrane and so
did not acquire ribosomes on its
surface, but their membrane topology is
otherwise similar to the cryptophytes.
The other sketches portray the four
major kinds of cell in the living world
and their membrane topology. The upper
ones show the contrasting ancestral
microtubular cytoskeleton (ciliary
roots, in red) of unikonts (a cone of
single microtubules attaching the
single centriole to the nucleus, blue)
and bikonts (two bands of microtubules
attached to the posterior centriole and
an anterior fan of microtubules
attached to the anterior centriole).
The lower ones show the single plasma
membrane of unibacteria (posibacteria
plus archaebacteria), which were
ancestral to eukaryotes and the double
envelope of negibacteria, which were
ancestral to mitochondria and
chloroplasts (which retained the outer
membrane, red).
source: http://aob.oxfordjournals.org/cg
i/content/full/95/1/147/FIG2


[2] Fig. 1. A consensus phylogeny of
eukaryotes. The vast majority of
characterized eukaryotes, with the
notable exception of major subgroups of
amoebae, can now be assigned to one of
eight major groups. Opisthokonts (basal
flagellum) have a single basal
flagellum on reproductive cells and
flat mitochondrial cristae (most
eukaryotes have tubular ones).
Eukaryotic photosynthesis originated in
Plants; theirs are the only plastids
with just two outer membranes.
Heterokonts (different flagellae) have
a unique flagellum decorated with
hollow tripartite hairs (stramenopiles)
and, usually, a second plain one.
Cercozoans are amoebae with filose
pseudopodia, often living with in tests
(hard outer shells), some very
elaborate (foraminiferans). Amoebozoa
are mostly naked amoebae (lacking
tests), often with lobose pseudopodia
for at least part of their life cycle.
Alveolates have systems of cortical
alveoli directly beneath their plasma
membranes. Discicristates have discoid
mitochondrial cristae and, in some
cases, a deep (excavated) ventral
feeding groove. Amitochondrial
excavates lack substantial molecular
phylogenetic support, but most have an
excavated ventral feeding groove, and
all lack mitochondria. The tree shown
is based on a consensus of molecular
(1-4) and ultrastructural (16, 17) data
and includes a rough indication of new
ciPCR ''taxa'' (broken black lines)
(7-11). An asterisk preceding the taxon
name indicates probable paraphyletic
group.
source: http://www.sciencemag.org/cgi/co
ntent/full/300/5626/1703

1,900,000,000 YBN
66) Oldest Acritarch (eucaryote)
fossils.

These fossils are reported to be both
in Chuanlinggou Formation, China and in
Russia.

Acritarchs, the name coined by Evitt in
1963 which means "of uncertain origin",
are an artificial group. The group
includes any small (most are between
20-150 microns across), organic-walled
microfossil which cannot be assigned to
a natural group. They are characterised
by varied sculpture, some being spiny
and others smooth. They are believed to
have algal affinities, probably the
cysts of planktonic eukaryotic algae.
They are valuable Proterozoic and
Palaeozoic biostratigraphic and
palaeoenvironmental tools.

 
[1] Figure 1 Protistan microfossils
from the Roper Group. a, c, Tappania
plana, showing asymmetrically
distributed processes and bulbous
protrusions (arrow in a). b, detail of
a, showing dichotomously branching
process. d, Valeria lophostriata. e,
Dictyosphaera sp. f, Satka favosa. The
scale bar in a is 35 µm for a and c;
10 µm for b; 100 µm for d; 15 µm for
e; and 40 µm for f.
source: Nature 412


[2] Diagram showing basic
morphological classification of
acritarchs. COPYRIGHTED
source: http://www.ucl.ac.uk/GeolSci/mic
ropal/acritarch.html

1,874,000,000 YBN
61) Oldest non-acritarch Eukaryote
fossil Grypania spiralis (an alga 10 cm
long) from BIF in Michigan. Oldest
algae fossil.

The date of this fossil
was originally 2100mybn, but Schneider
measured the Marquette Range Supergroup
(MRS), A rhyolite in the Hemlock
Formation, a mostly bimodal submarine
volcanic deposit that is laterally
correlative with the Negaunee
Iron-formation, yields a sensitive
high-resolution ion microprobe (SHRIMP)
U-Pb zircon age of 1874 ± 9 Ma.

In 1992, Han and Runnegar, finders of
this fossil, compared the fossil to
Acetabularia, a single-celled green
algae. If true, this would make
Grypania the oldest green algae fossil.



 

source: file:/root/web/Grypania_spiralis
_wmel0000.htm



source: http://www.peripatus.gen.nz/pale
ontology/lrgGrypaniaspiralis.jpg

1,800,000,000 YBN
46) End of the Banded Iron Formation
Rocks.


 

source:

1,576,000,000 YBN
67) A eukaroyte cell forms a symbiotic
relationship with cyanobacteria, which
form plastids (chloroplasts). Like
mitochondria, these organelles copy
themselves and are not made by the cell
DNA.

Depending on their morphology and
function, plastids are commonly
classified as chloroplasts,
leucoplasts, amyloplasts or
chromoplasts.

  
1,513,000,000 YBN
221) First fungi evolve.
Genetic comparison
shows fungi evolving now. This begins
the fungi kingdom. Perhaps fungi
evolved from the amoebozoa slime mold
line, because the sporangiophore
(stalk) and sporangium (ball on top) of
slime molds look very similar to many
fungi.

  
1,500,000,000 YBN
323) First plant (single cell, similar
to glaucophytes) evolves.

Ribosomal RNA place
first plant (single cell, similar to
glaucophytes) evolving here. This
begins the plant kingdom.

Cavelier-Smith and Ema E. -Y. Chao
write: "Kingdom Plantae
(sensuCavalier-Smith 1981) was
originally defined as comprising all
eukaryotes with chloroplasts possessing
an envelope of two membranes and
mitochondria with (irregularly) flat
cristae. It originally included
Viridaeplantae (green algae and
embryophyte or "higher" plants),
Rhodophyta (red algae), and Glaucophyta
(e.g., Cyanophora, Glaucocystis). It
was argued that all three groups
diverged from a single primary
symbiogenetic origin of plastids
(Cavalier-Smith 1982). Both the
monophyly of plastids and that of
Glaucophyta and Plantae long met
unreasonably strong opposition because
of widespread false dogma that
symbiogenesis is easy and because the
three taxa usually do not group
together in 18S rRNA trees. Now,
however, derived features of all
plastids compared with cyanobacteria
and numerous molecular trees have led
to the acceptance of plastid monophyly
(Delwiche and Palmer 1998) and to the
monophyly of glaucophyte algae.
Furthermore, a sister relation between
red algae and Viridaeplantae is
strongly supported by concatenated
protein trees for nuclei (Moreira et
al. 2000; Baldauf et al. 2000) and
chloroplasts (Martin et al. 1998;
Turmel et al. 1999). The sister
relationship between them and
glaucophytes is convincingly, but
significantly more weakly, supported by
the same trees. Thus the case of
Plantae shows that arguments from
morphology and evolutionary
considerations of protein targeting
during symbiogenesis (Cavalier-Smith
2000b) gave the correct answer much
more rapidly than single-gene trees,
which still do not clearly group all
three taxa together. In all our trees
in the present study (and the recent
tree of Edgcomb et al. 2002),
Rhodophyta and Viridaeplantae are
sisters, but with weak support.
Glaucophyta wander aimlessly from one
place to another in different trees."

  
1,492,000,000 YBN
173) Roper Group eukaryote algea
microfossils.

  
1,400,000,000 YBN
86) Glaucophyta evolve.
Genetic comparison
shows Phylum Glaucophyta evolving at
this time.
Some people catagorize Glaucophyta
in the kingdom Plantae instead of
Protista, and label glaucophyta the
most ancient living plants.

The glaucophytes, also referred to as
glaucocystophytes or glaucocystids, are
a tiny group of freshwater algae. They
are distinguished mainly by the
presence of cyanelles, primitive
chloroplasts which closely resemble
cyanobacteria and retain a thin
peptidoglycan wall between their two
membranes.

It is thought that the green algae
(from which the higher plants evolved),
red algae and glaucophytes acquired
their chloroplasts from endosymbiotic
cyanobacteria. The other types of algae
received their chloroplasts through
secondary endosymbiosis, by engulfing
one of those types of algae along with
their chloroplasts.

The glaucophytes are of obvious
interest to biologists studying the
development of chloroplasts: if the
hypothesis that primary chloroplasts
had a single origin is correct,
glaucophytes are closely related to
both green plants and red algae, and
may be similar to the original alga
type from which all of these developed.


Glaucophytes have mitochondria with
flat cristae, and undergo open mitosis
without centrioles. Motile forms have
two unequal flagella, which may have
fine hairs and are anchored by a
multilayered system of microtubules,
both of which are similar to forms
found in some green algae.

 
[1] ? COPYRIGHTED
source: http://protist.i.hosei.ac.jp/PDB
3/PCD3711/htmls/86.html


[2] ? COPYRIGHTED
source: http://protist.i.hosei.ac.jp/PDB
/Images/Others/Glaucocystis/

1,400,000,000 YBN
197) Opisthokonts (posterior cilium)
evolve from Unikonts (ancestrally only
one cilium). Opisthokonts have flat
mitochondrial cristae and go on to form
the Animal and Fungi kingdoms.

Thomas
Cavalier-Smith and Ema E.-Y. Chao
write: "The term opisthokont,
signifying "posterior cilium," was
applied to animals, Choanozoa, and
Fungi because all three groups
ancestrally had a single posterior
cilium (Cavalier-Smith 1987b). They
were argued to be a clade because they
also were characterized (uniquely at
the time) by flat, nondiscoid
mitochondrial cristae that were not
irregularly inflated like the flat
cristae of Plantae (Cavalier-Smith
1987b). Four other characters also
suggested that animals and fungi were
more closely related to each other than
plants (chitinous exoskeletons; storage
of glycogen, not starch; absence of
chloroplasts; and UGA coding for
tryptophane, not chain termination).
However, the first three were probably
ancestral states for eukaryotes and the
last convergent, so the ciliary and
cristal morphology were stronger
indications. Although early rRNA trees
did not group animals and fungi
together, the opisthokonts are now
consistently supported by all
well-sampled rRNA trees and trees using
several or many proteins, as discussed
above. Moreover a derived 12-amino acid
insertion in translation elongation
factor 1agr and three small gaps in
enolase clearly indicate that animals
and fungi have a common ancestor not
shared with plants (or other bikonts)
or Amoebozoa (Baldauf and Palmer 1993;
Baldauf 1999). Thus opisthokonts are
now well accepted as a robust clade of
eukaryotes (Patterson 1999)."

 
[1] cavalier-smith diagram COPYRIGHTED
source: cavalier_jmolevol_2003_56_540-56
3.pdf


[2] Figure 1. Phylogenetic hypothesis
of the eukaryotic lineage based on
ultrastructural and molecular data.
Organisms are divided into three main
groups distinguished by mitochondrial
cristal shape (either discoidal,
flattened or tubular). Unbroken lines
indicate phylogenetic relationships
that are firmly supported by available
data; broken lines indicate
uncertainties in phylogenetic
placement, resolution of which will
require additional data. Color coding
of organismal genus names indicates
mitochondrial genomes that have been
completely (Table 1), almost completely
(Jakoba, Naegleria and
Thraustochytrium) or partially (*)
sequenced by the OGMP (red), the FMGP
(black) or other groups (green). Names
in blue indicate those species whose
mtDNAs are currently being sequenced by
the OGMP or are future candidates for
complete sequencing. Amitochondriate
retortamonads are positioned at the
base of the tree, with broken arrows
denoting the endosymbiotic origin(s) of
mitochondria from a Rickettsia-like
eubacterium. Macrophar.,
Macropharyngomonas.
source: unknown

1,400,000,000 YBN
220) Amoebozoa (amoeba, slime molds)
evolve now.

Ribosomal RNA shows the Protist
Phylum Amoebozoa (also called
Ramicristates) which includes amoeba
and slime molds evolving now.

The Amoebozoa are a major group of
amoeboid protozoa, including the
majority that move by means of internal
cytoplasmic flow. Their pseudopodia are
characteristically blunt and
finger-like, called lobopodia. Most are
unicellular, and are common in soils
and aquatic habitats, with some found
as symbiotes of other organisms,
including several pathogens. The
Amoebozoa also include the slime
moulds, multinucleate or multicellular
forms that produce spores and are
usually visible to the unaided eye.

Mycetozoa are the slime molds.
4. Plasmodial
Slime Molds
a. Plasmodial
slime molds exist as a plasmodium. (the
earlier evolved acrasid cellular slime
molds exist as individual amoeboid
cells.)
b. This diploid
multinucleated cytoplasmic mass creeps
along, phagocytizing decaying plant
material.
c. Fan-shaped plasmodium
contains tubules of concentrated
cytoplasm in which liquefied cytoplasm
streams.
d. Under unfavorable
environmental conditions (e.g.,
drought), the plasmodium develops many
sporangia
that produce spores by
meiosis.
e. When mature, spores are
released and survive until more
favorable environmental conditions
return;
then each releases a
haploid flagellated cell or an amoeboid
cell.
f. Two flagellated or
amoeboid cells fuse to form diploid
zygote that produces a multi-nucleated
plasmodium.

Nuclear division in giant amoebas
(Peolobiont/Amoebozoa) is neither
mitosis nor binary fission, but
incorporates aspects of both (Fig.
3-7). Chromosomes are attached
permanently to the nuclear membrane by
their centromeres (MTOCs, microtubule
organizing centers), and the nuclear
membrane remains intact throughout
division. After DNA duplication
produces two chromatids, the point of
attachment, the MTOC duplicates or
divides, and microtubules are assembled
between the two resulting MTOCs.
Elongating microtubules form something
akin to a spindle within the nuclear
membrane that pushes the daughter
chromosomes apart and elongate the
membrane-bounded nucleus until it blebs
in half in something akin to binary
fission. Simple assembly of
microtubules accomplishes the
separation of daughter genomes in this
simple nuclear division. In typical
eukaryotic mitosis, the separation of
daughter chromosomes is accomplished by
a dual action, the disassembly of
spindle fibers connecting the daughter
chromosome to the polar MTOC, and
assembly of spindle fibers running pole
to pole.

amoeba haplodiploid?

 
[1] SUBPHYLUM Lobosa CLASS Amoebaea
Chaos diffluens, an amoeba. Photo
released by Dr. Ralf Wagner.
source: http://en.wikipedia.org/wiki/Ima
ge:Chaos_diffluens.jpg


[2] CLASS Amoebaea Mayorella
(may-or -ell-a) a medium sized
free-living naked amoeba with conical
pseudopodia. Central body is the
nucleus. Phase contrast. This picture
was taken by David Patterson of
material from Limulus-ridden sediments
at Plum Island (Massachusetts USA) in
spring and summer, 2001. NONCOMMERCIAL
USE
source: http://microscope.mbl.edu/script
s/microscope.php?func=imgDetail&imageID=
515

1,300,000,000 YBN
188) Green Algae, composed of the 2
Phlya Chlorophyta (volvox, sea lettuce)
and Charophyta (Spirogyra) evolve.

Gene
tic comparison shows Green Algae,
composed of the 2 Phlya Chlorophyta
(volvox, sea lettuce) and Charophyta
(Spirogyra) evolving now.

The Green Algae are the large group of
algae from which the embryophytes
(higher plants) emerged. As such they
form a paraphyletic group, some people
placing them in the Plantae Kingdom,
while others placing them in the
Protist Kingdom.

Almost all forms have chloroplasts.
They are bound by a double membrane, so
presumably were acquired by direct
endosymbiosis of cyanobacteria.

All green algae have mitochondria with
flat cristae. When present flagella are
typically anchored by a cross-shaped
system of microtubules, but these are
absent among the higher plants and
charophytes. They usually have cell
walls containing cellulose, and undergo
open mitosis without centrioles. Sexual
reproduction varies from fusion of
identical cells (isogamy) to
fertilization of a large non-motile
cell by a smaller motile one (oogamy).
However, these traits show some
variation, most notably among the basal
green algae, called prasinophytes.

The first land plants most likely
evolved from green algae.

Here is where the green algae separate
from the ancestor of the first land
plants.

Spirogyra reproduce through
conjugation, which either was inherited
from prokaryotes or evolved a second
time in eukaryotes.

Some filamentous green algae (e.g.
cladophora) are haplodiploid (alternate
between haploid and diploid cycles that
both have mitosis).

 
[1] Micrograph of Volvox aureus.
Copyright held by Dr. Ralf Wagner,
uploaded to German Wikipedia under
GFDL. Permission is granted to copy,
distribute and/or modify this document
under the terms of the GNU Free
Documentation License, Version 1.2 or
any later version published by the Free
Software Foundation; with no Invariant
Sections, no Front-Cover Texts, and no
Back-Cover Texts. Subject to
disclaimers.
source: http://en.wikipedia.org/wiki/Vol
vox


[2] Photo of green algal growth
(Enteromorpha sp.) on rocky areas of
the ocean intertidal shore, indicating
a nearby nutrient source (in this case
land runoff). Photographed by Eric
Guinther near Kahuku, O'ahu,
Hawai'i. GFDL Permission is granted
to copy, distribute and/or modify this
document under the terms of the GNU
Free Documentation License, Version 1.2
or any later version published by the
Free Software Foundation; with no
Invariant Sections, no Front-Cover
Texts, and no Back-Cover Texts Subject
to disclaimers
source: http://en.wikipedia.org/wiki/Ima
ge:Intertidal_greenalgae.jpg

1,300,000,000 YBN
209) Red Algae (Rhodophyta) evolve now.
Gene
tic comparison show Phylum Rhodophyta
(red algae) evolves now.

There are between 2500 and 6000 species
in about 670 largely marine genera.

Many red algae are haplodiploid
(alternate between haploid and diploid
cycles that both have mitosis).

The red algae (Rhodophyta) are a large
group of mostly multicellular, marine
algae, including many notable seaweeds.
Most of the coralline algae, which
secrete calcium carbonate and play a
major role in building coral reefs,
belong here. Red algae such as dulse
and nori are a traditional part of
European and Asian cuisine and are used
to make certain other products like
agar and food additives.

Many red algae have multicellular
stages but these lack differentiated
tissues and organs. Unlike most other
algae, no cells with a flagellum are
found in any member of the group.
Unicellular forms typically live
attached to surfaces rather than
floating among the plankton, and both
the larger female and smaller male
gametes are non-motile, so that most
have a low chance of fertilization.
They have cell walls are made out of
cellulose and thick gelatinous
polysaccharides, which are the basis
for most of the industrial products
made from red algae.

The chloroplasts of red algae are bound
by a double membrane, like those of
green plants; both groups
(Archaeplastida) probably share a
common origin. Their plastids formed by
direct endosymbiosis of a
cyanobacteria, and in red algae are
pigmented with chlorophyll a and
various proteins called phycobilins,
which are responsible for their reddish
color. Other algae that lack
chlorophyll b appear to have acquired
their chloroplasts from red algae,
although their pigmentations are
somewhat different.

unicellular to multicellular (up to 1
m) mostly free-living but some
parasitic or symbiotic, with
chloroplasts containing phycobilins.
Cell walls made of cellulose with
mucopolysaccharides penetrated in many
red algae by pores partially blocked by
proteins (complex referred to as pit
connections). Usually with separated
phases of vegetative growth and sexual
reproduction. Common and widespread,
ecologically important, economically
important (source of agar). No
flagella. Ultrastructural identity:
Mitochondria with flat cristae,
sometimes associated with forming faces
of dictyosomes. Thylakoids single, with
phycobilisomes, plastids with
peripheral thylakoid. During mitosis,
nuclear envelope mostly remains intact
but some microtubules of spindle extend
from noncentriolar polar bodies through
polar gaps in the nuclear envelope.
Synapomorphy: No clear-cut feature
available; possibly pit connections
Composition: About 4,000 species.

CLASS Florideophyceae
CLASS Bangiophyceae
CLASS Rhodellophyceae

 
[1] Close-up of a red alga (Genus?
Laurencia), Class Florideophyceae,
Order=? a marine seaweed from Hawaii.
GNU
source: http://en.wikipedia.org/wiki/Ima
ge:Laurencia.jpg


[2] Bangia atropurpurea Profile:
unbranched filaments in tufts. Often
forming dense fringes in the spalsh
zone. Uniseriate at base, multiseriate
above with protoplasts separate in a
firm gelatinous sheath. Stellate
chloroplasts. US NOAA PD
source: http://www.glerl.noaa.gov/seagra
nt/GLWL/Algae/Rhodophyta/Cards/Bangia.ht
ml

1,280,000,000 YBN
187) A eukaryote rhodophyte (red alga)
is enslaved by a chromealveolate
eukaryote to form a plastid in the
chromealveolate. This kind of plastid
is presumably inherited by all other
chromalveolates (brown algae, diatoms,
water molds, Dinoflagellata,
Apicomplexa, ciliates) that have
plastids.

If this red alga endosymbiosis occured
only once, then all chromalveolates
with plastids inherited them and all
without lost them. Ciliates presumably
lost any inherited plastids.

  
1,250,000,000 YBN
201) Oldest widely accepted Rhodophyta
(red algae) fossils (Bangiomorpha
pubescens) from Hunting Formation,
Somerset Island, arctic Canada.

This
is the oldest multicellular eukaryote
fossil and the oldest fossil of a
sexual species found yet.

 
[1] get images from Life on a Young
Planet, Knoll
source: Science 1990 vol 250
Butterfield N. J. A. H. Knoll K. Swett
1990 A bangiophyte red alga from the
Proterozoic of Arctic Canada. Science
250: 104-107[ISI][Medline]


[2] Figure 2. Griffithsia pacifica
(Florideophyceae). Electron micrograph
showing cytoplasm with numerous
chloroplasts (C) and starch (S). Starch
is the photosynthetic reserve and is
deposited free in the cytoplasm.
source: (American Journal of Botany.
2004;91:1494-1507.)

1,100,000,000 YBN
75) Most ancient living fungi phylum
"Microsporidia" evolves.

Ribosomal RNA shows
most ancient living fungi phylum
"Microsporidia" evolving now.

Microsporidia are parasites of animals,
now considered to be extremely reduced
fungi. Most infect insects, but they
are also responsible for common
diseases of crustaceans and fish, and
have been found in most other animal
groups, including humans and other
mammals which can be parasitized by
species of Encephalitozoon. Replication
takes place within the host's cells,
which are infected by means of
unicellular spores. These vary from
1-40 μm, making them some of the
smallest eukaryotes. They also have the
shortest eukaryotic genomes.

Microsporidia are unusual in lacking
mitochondria, and also lack motile
structures such as flagella. The spores
are protected by a layered wall
including proteins and chitin. Their
interior is dominated by a unique
coiled structure called a polar tube
(not to be confused with the polar
filaments of Myxozoa). In most cases
there are two closely associated
nuclei, forming a diplokaryon, but
sometimes there is only one.

Intracellular parasites, no
mitochondria, ribosomes are unusual in
being of prokaryotic size (70S) and
lacking characteristic eukaryotic 5.8S
ribosomal RNA as a separate molecule in
the microsporidia but is incorporated
into the 23S r RNA.

binucleate haploid?

 
[1] Sporoblast of the Microsporidium
Fibrillanosema crangonycis. Electron
micrograph taken by Leon White. GNU
source: http://en.wikipedia.org/wiki/Ima
ge:Fibrillanosema_spore.jpg


[2] Spironema
multiciliatum Spironema:
Octosporoblastic sporogony producing
horseshoe-shaped monokaryotic spores in
sporophorous vesicles; monomorphic,
diplokaryotic and monokaryotic;
merogony - last generation merozoites
are diplokaryotic; sporogony - initial
division of the sporont nuclei is
meiotic as indicated by the occurrence
of synaptonemal complexes; spores are
horse-shoe-shaped, with swollen ends in
T. variabilis and have one elongate
nucleus; exospore with three layers,
endospore is of medium thickness;
polaroplast composed of two lamellar
parts, an anterior part of closely
packed lamellae and a posterior part of
wider compartments; polar tube is
isofilar and forms, in the posterior
quarter of the spore, 3-4 coils in a
single rank (T. variabilis) or 8-10
coils in a single rank (T. chironomi);
type species Toxoglugea vibrio in
adipose tissue of larvae of Ceratopogon
sp. (Diptera, Ceratopogonidae).
Spironema (spire-oh-knee-ma)
multiciliatum Klebs, 1893. Cells are
lanceolate, relatively flattened and
flexible. The cells have a spiral
groove, long kinetics and a tail, which
tapers posteriorly, and are about 15 -
21 microns without the tail. The
nucleus is located anteriorly or near
the centre of the cell. When the cells
are squashed, the cells are more
flexible. Food materials are seen under
the cell surface. Rarely observed.
This picture was taken by Won Je Lee
using conventional photographic film
using a Zeiss Axiophot microscope of
material collected in marine sediments
of Botany Bay (Sydney, Australia). The
image description refers to material
from Botany Bay. NONCOMMERCIAL USE
source: http://microscope.mbl.edu/script
s/microscope.php?func=imgDetail&imageID=
3928

1,000,000,000 YBN
223) Fungi phylum "Chytridiomycota"
evolves.

Ribosomal RNA place fungi phylum
"Chytridiomycota" evolving now.

Many chytrids are haplodiploid
(alternate between haploid and diploid
cycles that both have mitosis).

Chytridiomycota is a division of the
Fungi kingdom and contains only one
class, Chytridiomycetes. The name
refers to the chytridium (from the
Greek, chytridion, meaning "little
pot"): the structure containing
unreleased spores.
The chytrids are the
most primitive of the fungi and are
mostly saprobic (feed on dead species,
degrading chitin and keratin). Many
chytrids are aquatic (mostly found in
freshwater). There are approximately
1,000 chytrid species, in 127 genera,
distributed among 5 orders. Both
zoospores and gametes of the chytrids
are mobile by their flagella, one
whiplash per individual. The thalli are
coenocytic and usually form no true
mycelium (having rhizoids instead).
Some species are unicellular.

 
[1] Chytrids (Chytridiomycota): The
Primitive Fungi These fungi are
mostly aquatic, are notable for having
a flagella on the cells (a flagella is
a tail, somewhat like a tail on a sperm
or a pollywog), and are thought to be
the most primitive type of
fungi. actual photo comes
from: http://www.csupomona.edu/~jcclark
/classes/bot125/resource/graphics/chy_al
l_sph.html
source: http://www.davidlnelson.md/Cazad
ero/Fungi.htm


[2] Chytridiomycota - Blastocladiales
- zoospore of Allomyces (phase contrast
illumination) X 2000
source: http://www.mycolog.com/chapter2b
.htm

1,000,000,000 YBN
324) Phylum Choanozoa
(Mesomycetozoea/DRIPs,
Choanoflagellates) evolves.


  
1,000,000,000 YBN
325) The Choanozoan "Mesomycetozoaea"
(DRIPs) evolve.

The Mesomycetozoea or
DRIP clade are a small group of
protists, mostly parasites of fish and
other animals. One species,
Rhinosporidium seeberi, infects birds
and mammals, including humans. They are
not particularly distinctive
morphologically, appearing in host
tissues as enlarged spheres or ovals
containing spores, and most were
originally classified in various groups
of fungi, protozoa, and algae. However,
they form a coherent group on molecular
trees, closely related to both animals
and fungi and so of interest to
biologists studying their origins.

The name DRIP is an acronym for the
first protozoa identified as members of
the group - Dermocystidium, the rosette
agent, Ichthyophonus, and
Psorospermium. Cavalier-Smith later
treated them as the class
Ichthyosporea, since they were all
parasites of fish. Since other new
members have been added, Mendoza et al.
suggested changing the name to
Mesomycetozoea, which refers to their
evolutionary position. Note the name
Mesomycetozoa (without a second e) is
also used to refer to this group, but
Mendoza et al. use it as an alternate
name for the phylum Choanozoa.

Assemblage identified from molecular
studies, mostly pathogens, a few
genera, no synapomorphy. Grouping
formalized by Herr, Ajello, Taylor,
Arseculeratne & Mendoza, 1999.



 
[1] Ichthyophonus, a fungus-like
protistan that occurs in high
prevalence in Pacific Ocean perch
(Sebastes aultus) and yellowtail
rockfish (Sebastes flavedus). Note the
parasite forms branching hyphae-like
structures. Ichthyophonus hoferi has
caused massive mortalities in herring
in the Atlantic ocean, and has recently
been reported to cause disease in wild
Pacific herring from Washington through
Alaska. COPYRIGHTED EDU
source: http://oregonstate.edu/dept/salm
on/projects/images/16Ichthyophonus.jpg


[2] Microscopic appearence of the
organism is dependent on its stage of
development. The stages include (1)
spore at ''resting'' stage, (2)
germinating spore, (3) hyphal
stage. It is believed that there are
two forms of Ichthyophonus, both
belonging to one genus. One of them is
known as the ''salmon'' form, occuring
in freshwater and cold-preferring sea
fishes: this form is characterized by
its ability to produce long tubulose
germ hyphae. The other is called the
''aquarium fish'' form, typical of the
tropical freshwater fishes. This form
is completely devoid of hyphae.
Developmental cycle of Ichthyophonus
hoferi: 1-5 - development of
''daughter'' spores, 7-11 - development
of resting spore from the ''daughter''
spore, 12-19 - development of resting
spore by fragmentation. COPYRIGHTED
source: http://www.fao.org/docrep/field/
003/AC160E/AC160E02.htm

1,000,000,000 YBN
585) The Neoproterozoic (1.0-0.65Ga) is
a period of dramatic global change and
quickening reef evolution. The
appearance of heavily calcified
microbial elements (calcimicrobes; e.g.
Girvanella and Renalcis) in the Tonian
(1.0-0.85Ga), coincident with the
disappearance of conical elements and
decline in stromatolites, is a critical
event.



  
967,000,000 YBN
97) A lens and light sensitive area
evolve in unicellular eukaryote living
objects. This is the first proto eye.

The
eye spot probably evolved from a
plastid, and plastids may have only
formed symbiotic relationships in
euglenozoa much later, since the
plastids in euglenozoa are enclosed in
3 membranes (the same as chloroplasts
in plants), they are thought to have
been formed from captured green algae
which evolve much later.

  
900,000,000 YBN
326) The Choanozoans
"Choanoflagellates" and "Acanthoecida"
evolve.

The choanoflagellates are a
group of flagellate protozoa. They are
considered to be the closest relatives
of the animals, and in particular may
be the direct ancestors of sponges.

Each choanoflagellate has a single
flagellum, surrounded by a ring of
hairlike protrusions called microvilli,
forming a cylindrical or conical collar
(choanos in Greek). The flagellum pulls
water through the collar, and small
food particles are captured by the
microvilli and ingested. It also pushes
free-swimming cells along, as in animal
sperm, whereas most other flagellates
are pulled by their flagella.

Most choanoflagellates are sessile,
with a stalk opposite the flagellum. A
number of species are colonial, usually
taking the form of a cluster of cells
on a single stalk. Of special note is
Proterospongia, which takes the form of
a glob of cells, of which the external
cells are typical flagellates with
collars, but the internal cells are
non-motile.

The choanocytes (also known as
"collared cells") of sponges have the
same basic structure as
choanoflagellates. Collared cells are
occasionally found in a few other
animal groups, such as flatworms. These
relationships make colonial
choanoflagellates a plausible candidate
as the ancestors of the animal kingdom.

 
[1] DOMAIN Eukaryota - eukaryotes
KINGDOM Protozoa (Goldfuss, 1818) R.
Owen, 1858 - protozoa SUBKINGDOM
Sarcomastigota (means=?) PHYLUM
Choanozoa CLASS
Choanoflagellatea (Choanoflagellates
and Acanthoecida) ORDER
Acanthoecida Saepicula: Cells
solitary, lorica funnel-shaped, 2
chambers delimited by a waist;
constructed of rod-shaped costal
strips; posterior chamber obconical
with 2 series of costae located more or
less regularly around chamber, one
series almost parallel to the long axis
of cell and second series almost
perpendicular to long axis; anterior
chamber formed by ring of equally
spaced longitudinal costae surmounted
by single transverse costa; marine
This image is based on a drawing
provided by Won Je Lee. NONCOMMERCIAL
USE
source: http://microscope.mbl.edu/script
s/microscope.php?func=imgDetail&imageID=
3229


[2] Choanoeca: Cells solitary with
distinct, firm flask-shaped theca more
or less closely investing protoplast,
with short pedicel; collar relatively
long, widely expanded; flagellum absent
in adult, but produced prior to cell
division for locomotory use by juvenile
cell; in marine and brackish habitats,
frequently attached to filamentous
algae and hydrozoa Choanoeca
(ko-an-o-eek-a), an unusual loricate
collar flagellate (choanoflagellate) in
that the usual form is without a
flagellum. Flagellated motile stage is
occasionally produced. Widely dispersed
pseudopodial elements of the collar are
evident in this image. Differential
interference contrast. This picture
was taken by David Patterson and Aimlee
Laderman of material collected from a
freshwater Atantic white cedar swamp at
Cumloden near Woods Hole in
Massachusetts, USA in spring and
summer, 2001. NONCOMMERCIAL USE
source: http://microscope.mbl.edu/script
s/microscope.php?func=imgDetail&imageID=
170

855,000,000 YBN
286) A key step in metazoan
multicellularity evolves, where a
zygote produces differentiated cells
that stick together to form one
organism.

Metazoan multicellularity appears to
be different from colonialism (where
independent cells of the same species
work together and function as one
unit), because one zygote produces all
the cells in the organism.

  
850,000,000 YBN
81) First animal and first metazoan
evolve. Metazoans are multicellular,
but their cells perform different
functions and originate from one
cell(?). This is`also the beginning of
the Animal Subkingdom "Radiata",
species with radial symmetry. These are
the sponges. There are only 3 kinds of
metazoans: sponges, cnidarians, and
bilaterians (which include all insects
and vertibrates). Sponges are the
first organisms whose DNA codes for
more than one kind of cell. Sponges
have 3 different cell types. Some
cells form a body wall, some digest
food, some form a skeletal frame.

All sponge
cells are totipotent and are capable of
regrowing a new sponge.
The two major
subkingdoms of the Kingdom Animalia are
Radiata (the radiates) and Bilateria
(the bilaterians).

 
[1]
source: http://www.museums.org.za/bio/me
tazoa.htm


[2]
source: http://www.museums.org.za/bio/me
tazoa.htm

850,000,000 YBN
101) First homeobox, or "hox" genes
evolve. These genes regulate the
building of major body parts.


  
850,000,000 YBN
224) Genetic comparison shows Fungi
division "Zygomycota" (bread molds, pin
molds, microsporidia,...) evolving now.


 
[1] Figure 2. Zygomycota A: sporangia
of Mucor sp. B: whorl of sporangia of
Absidia sp. C: zygospore of
Zygorhynchus sp. D: sporangiophore and
sporangiola of Cunninghamella sp.
source: http://www.botany.utoronto.ca/Re
searchLabs/MallochLab/Malloch/Moulds/Cla
ssification.html


[2] Figure 3. Syncephalis, a member
of the Zygomycota parasitic on other
Zygomycota
source: http://www.botany.utoronto.ca/Re
searchLabs/MallochLab/Malloch/Moulds/Cla
ssification.html

780,000,000 YBN
79) Animal Phylum "Placozoa" evolves.
Placozoans
look like amoebas but are
multicellular.

There is only one known species,
"Tricoplax adhaerens", and one other
potential species "Tricoplax reptans"
in the entire Placozoa phylum.

Putative eggs have been observed, but
they degrade at the 32-64 cell stage.
Neither embryonic development nor sperm
have been observed, however Trichoplax
genomes show evidence of sexual
reproduction. Asexual reproduction by
binary fission is the primary mode of
reproduction observed in the lab.

The haploid number of chromosomes is
six. It has the smallest amount of DNA
yet measured for any animal with only
50 megabases (80 femtograms per cell).
A trichoplax genome project is
currently underway.

  
750,000,000 YBN
83) Animal Phlyum Ctenophora (comb
jellies) evolves.


  
750,000,000 YBN
225) Genetic comparison shows Fungi
division "Glomeromycota" (Arbuscular
mycorrhizal fungi) evolving now.


 
[1] germinating Gigaspora decipiens
source: http://pages.unibas.ch/bothebel/
people/redecker/ff/glomero.htm


[2] Archaeospora leptoticha spores
source: http://pages.unibas.ch/bothebel/
people/redecker/ff/glomero.htm

700,000,000 YBN
82) First cnidarians (coelantrates),
jellyfish evolves. Jellyfish have
photon detecting cells and a lens made
of ?.


  
700,000,000 YBN
226) The second largest group of Fungi,
the phylum "Basidiomycota" (most
mushrooms, rusts, club fungi) evolve.

Genetic
comparison shows the second largest
group of Fungi, the phylum
"Basidiomycota" (most mushrooms, rusts,
club fungi) evolving now.

The Division Basidiomycota is a large
taxon within the Kingdom Fungi that
includes those species that produce
spores in a club-shaped structure
called a basidium. Essentially the
sibling group of the Ascomycota, it
contains some 30,000 species (37% of
the described fungi)

 
[1] Amanita muscaria
(Homobasidiomycetes)
source: http://en.wikipedia.org/wiki/Ima
ge:Agaricales.jpg


[2] Basidiomycete Life Cycle tjv
source: http://botit.botany.wisc.edu/ima
ges/332/Basidiomycota/General_basidio/Ba
sidiomycete_Life_Cycle_tjv.php?highres=t
rue

700,000,000 YBN
227) The largest Fungi phylum
"Ascomycota" (yeasts, truffles,
Penicillium, morels, sac fungi)
evolves.

Genetic comparison shows the largest
Fungi phylum "Ascomycota" (yeasts,
truffles, Penicillium, morels, sac
fungi) evolving now.
47,000 described
species.

 
[1] white truffle
cutted photographed by
myself GNU head Permission is
granted to copy, distribute and/or
modify this document under the terms of
the GNU Free Documentation License,
Version 1.2 or any later version
published by the Free Software
Foundation; with no Invariant Sections,
no Front-Cover Texts, and no Back-Cover
Texts. A copy of the license is
included in the section entitled ''Text
of the GNU Free Documentation
License.''
source: http://upload.wikimedia.org/wiki
pedia/commons/f/fd/Truffle_washed_and_cu
tted.jpg


[2] EColi-Scerevisiae.jpg (50KB, MIME
type: image/jpeg) Wikimedia Commons
logo This is a file from the Wikimedia
Commons. The description on its
description page there is shown
below. Escherichia coli (little
forms) & Saccharomyces cerevisiae (big
forms) by MEB Public domain This file
has been released into the public
domain by the copyright holder, its
copyright has expired, or it is
ineligible for copyright. This applies
worldwide. brewer's yeast/baker's
yeast
source: http://en.wikipedia.org/wiki/Ima
ge:EColi-Scerevisiae.jpg

700,000,000 YBN
228) Genetic comparison shows the
largest and second largest lines of
Fungi (Ascomycota and Basidiomycota)
splitting now.


  
680,000,000 YBN
222) Genetic comparison shows the Class
of Ascomycota Fungi called
"Archaeascomycetes" (fission yeast,
pneumonia fungus) evolving now.

  
650,000,000 YBN
69) Start of Varanger Ice Age (650-590
mybn).

  
650,000,000 YBN
229) Genetic comparison shows the
Ascomycota Fungi "Hemiascomycetes"
evolving now.

  
630,000,000 YBN
91) First bilateral (has 2 sided
symmetry) species evolves. Animal
phylum Acoelomorpha (acoela flat worms
and nemertodermatida) evolves.
This
begins the Subkingdom "Bilateria".

lack
a digestive track, anus and coelom.

 
[1] Convoluta pulchra Smith and Bush
1991, a typical mud-inhabiting acoel
that feeds on diatoms
source: ?

600,000,000 YBN
231) Basidiomycota Fungi
"Ustilaginomycetes" (corn smut fungus)
and "Hymenomycetes" (white rot fungus)
evolve.

  
590,000,000 YBN
70) End of Varanger Ice Age (650-590
mybn).

  
590,000,000 YBN
93) Protostomes evolve. Many phyla
evolve at this time. Protostomes
include the 3 infrakingdoms Ecdysozoa
(a variety of worms and the arthropods
{a huge group including all insects and
crustaceans}), Platyzoa (rotifers and
flatworms), and Lophotrochozoa
(brachiopods {clams}, molluscs
{snails}, and a variety of worms).


  
580,000,000 YBN
94) Earliest animal fossil from
Doushantuo formation in China.


  
580,000,000 YBN
165) Earliest bilaterian fossil,
Vernanimalcula, 178 um in length, from
Doushantuo Formation, China. First
fossil of organism with bilateral
symmetry, mouth, digestive track, gut
and anus.


 
[1] Fig. 2. Close-up images of
prominent anatomical features of
Vernanimalcula guizhouena. The scale
bar represents 18 µm in (A), 32 µm in
(B), 24 µm in (C), and 28 µm in (D).
SO, sensory organ, i.e., external pit;
LU, lumen; PH, pharynx; MO, mouth; CO,
coelomic lumen; CW, mesodermal coelomic
wall; GU, gut. (A) Detail of collared
mouth, multilayered pharynx, and one
anterior surface pit. In this image,
which is from the holotype specimen
(Fig. 1A), the floor of the pit can be
seen to be composed of a specialized
concave layer. Note the coelomic wall,
which here as elsewhere in these
specimens has a thickness of about 5 to
6 µm. (B) Mouth of a fourth specimen,
Q3105, displaying collared mouth and
pharynx, ventral view. (C) Lumen of
pharynx from a fifth specimen, X10419,
secondarily encrusted but revealing
morphology of opening of pharynx into
gut similar to that seen in the
specimens shown in Fig. 1. (D) Close-up
of spaced external pits, interpreted as
possible sensory organs, from the same
specimen as shown in Fig. 1B [compare
(A)].
source: http://www.sciencemag.org/cgi/co
ntent/full/sci;305/5681/218


[2] Fig. 1. Images of three
different, fairly well preserved
specimens of the bilaterally organized
fossil animal Vernanimalcula
guizhouena. Left panels show digitally
recorded, transmitted light images of
sections about 50 µm thick, which had
been ground from larger rock samples,
mounted on slides, and viewed through a
light microscope. Right panels show
color-coded representations of the
images on the left. These were prepared
by digital image overlay. Yellow,
external ectodermal layer; ochre,
coelomic mesodermal layer; red, surface
pits; mauve, pharynx; light tan,
endodermal wall of gut; gray-green,
lumen of mouth; dark gray, paired
coelomic cavities; lighter gray, lumen
of gut; brown, ''gland-like''
structures, with central lumen (B);
light green, mineral inclusions (C).
The scale bar represents 40 µm in (A),
55 µm in (B), and 46 µm in (C). (A)
Holotype specimen, X00305, slightly
tilted, almost complete ventral level
coronal section, passing through the
ventrally located mouth. (B) Coronal
section of second specimen, X08981,
passing through dorsal wall of pharynx
and displaying complete A-P length of
digestive tract, including posterior
end [not visible in (A)]. (C) Tilted
coronal section of third specimen,
X10475, possibly slightly squashed,
passing through dorsal wall of pharynx
and through the dorsal wall of the gut.
For dimensions, see Table 1.
source:

580,000,000 YBN
318) Protostome Infrakingdom Ecdysozoa
evolves. Ecdysozoa are animals that
molt (lose their outer skins) as they
grow.
Ecdysozoa include:
the Phylum "Chaetognatha"
(Arrow Worms),
the Superphylum
"Aschelminthes", containing the 5
Phlya:
"Kinorhyncha" (kinorhynchs)
"Loricifera"
(loriciferans)
"Nematoda" (round worms)
"Nematomorpha"
(horsehair worms),
"Priapulida" (priapulids)
the
Superphlyum "Panarthropoda" containing
the 3 Phyla:
"Arthropoda" (arthropods:
insects, shell fish)
"Onychophora"
(onychophorans)
"Tardigrada" (tardigrades)


  
575,000,000 YBN
107) Start of fossils in Ediacaran
fauna near Adelaide, Australia.

  
574,000,000 YBN
96) First neuron, nerve cell, and
nervous system evolves in bilaterians.


  
570,000,000 YBN
95) Fluid filled cavity, coelom evolves
in early bilaterians.


  
570,000,000 YBN
105) Deuterostomes evolve. This is the
beginning of the Subkingdom
Deuterostomia and Infrakingdom
"Coelomopora" (Ambulacraria) with the
two Phyla "Hemichordata" (acorn worms)
and "Echinodermata" (sea cucumbers, sea
urchins, starfish).




  
570,000,000 YBN
311) Ecdysozoa phylum Chaetognatha
(Arrow Worms) evolves.


  
570,000,000 YBN
345) Deuterostome Coelomorpha Phylum
Hemichordonia (acorn worms) evolves.


  
570,000,000 YBN
346) Deuterostome Coelomorpha Phylum
Echinodermata (sea cucumbers, sea
urchins, sand dollars, star fish)
evolves.


  
565,000,000 YBN
98) First circulatory system and red
blood cells evolve in bilaterian worms.


  
565,000,000 YBN
327) Infrakingdom Platyzoa (includes
Superphylum Gnathifera {gnathiferans},
Phylum Gastrotricha {gastrotrichs}, and
Phylum Platyhelminthes {flatworms})
evolve.


  
565,000,000 YBN
347) Deuterostome Phylum Chordata
evolves. Chordata is a very large
group that contains all fish,
amphibians, reptiles and mammals.


  
565,000,000 YBN
348) Deuterstome Chordata Subphylum
Tunicata (tunicates {sea squirts})
evolves.


  
562,000,000 YBN
99) Segmentation evolves.

  
561,000,000 YBN
100) Filter feeding, filtering food and
oxygen from water through a digestive
system, evolves in segmented worms.


  
560,000,000 YBN
117) Oldest fossil of chordate,
Ediacaran fossil.

 
[1] from adelaide, australia
source: http://news.bbc.co.uk/1/hi/sci/t
ech/3208583.stm

560,000,000 YBN
330) The two Ecdysozoa Superphyla
Ashelminthes (round worms, horsehair
worms, priapulids) and Pananthropoda
(arthropods, onychophorans,
tardigrades) separate.


  
560,000,000 YBN
349) Deuterstome Chordata Subphylum
Cephalochordata (lancelets) evolves.
This is the first fish.


  
550,000,000 YBN
328) Ecdysozoa Superphylum
"Ashelminthes" evolves. This includes
the 5 Phyla:
Kinorhyncha (kinorhynchs),

Loricifera (loriciferans),
Nematoda (round worms),
Nematomorpha
(horsehair worms),
Priapulida (priapulids).


  
550,000,000 YBN
329) Platyzoa Superphylum "Gnathifera"
evolves. This includes the 5 Phyla:
Gna
thostomulida (gnathostomulids),
Cycliophora
(cycliophorans),
Micrognathozoa,
Rotifera (rotifers),
Acanthocephala
(acanthocephalans).


  
547,000,000 YBN
331) The Protostome Infrakingdom
Lophotrochozoa evolves. This includes
brachiopods, bryozoans, clams, squids
and octopuses (cephalopods), and
snails.

This infrakingdom is made of:
Superphylum
Lophophorata,
Phylum Bryozoa (bryozoans),
Phylum Entoprocta
(entoprocts),
Superphylum Eutrochozoa.

  
547,000,000 YBN
332) The Lophotrochozoa Superphylum
Lophophorata evolves. This includes
the two Phyla Phoronida (phoronids) and
Brachiopoda (brachiopods {clams,
oysters, muscles}).


  
547,000,000 YBN
333) The Lophotrochozoa Phyla Phoronida
(phoronids) evolves.


  
547,000,000 YBN
334) The Lophotrochozoa Phylum
Brachiopoda (brachiopods {clams,
oysters, muscles}) evolves.


  
545,000,000 YBN
335) The Lophotrochozoa Phylum
Entoprocta (entoprocts) evolves.


  
543,000,000 YBN
53) End Precambrian Eon, start
Phanerozoic Eon. End Proterozoic Era,
start Paleozoic Era.


  
543,000,000 YBN
104) The Platyzoa Phyla Platyhelminthes
(flatworms) and Gastrotricha
(gastrotrichs) evolve.


  
543,000,000 YBN
120) Start Cambrian period (543-490
mybn).


  
543,000,000 YBN
336) The Lophotrochozoa Phylum Bryozoa
(Bryozoans or moss animals) evolves.


  
543,000,000 YBN
337) The Ecdysozoa Superphylum
Panarthropoda (Arthropods, Onychophora,
Tardigrada) evolves.


  
543,000,000 YBN
338) The Ecdysozoa Phylum Arthropoda
(insects, crustaceans) evolve.


  
543,000,000 YBN
339) The Ecdysozoa Phylum Onychophora
(onychophorans) evolves.


  
543,000,000 YBN
340) The Ecdysozoa Phylum Tardigrada
(tardigrades) evolves.


  
542,000,000 YBN
131) First shell (or skeleton) evolves.

 
[1] Aldanella may be mollusc, if
mollusc may be first known snail.
shell is 1.5 mm in diameter.
source: http://www.geology.ucdavis.edu/~
cowen/HistoryofLife/CH05images.html

541,000,000 YBN
102) The Lophotrochozoa Superphylum
Eutrochozoa (molluscs, ribbon, peanut,
spoon, and segmented worms) evolves.


  
541,000,000 YBN
132) Archaeocyatha (early sponges)
evolve.


 
[1]
http://www.ucmp.berkeley.edu/porifera/ar
chaeo.html
source: http://www.ucmp.berkeley.edu/por
ifera/archaeo.html


[2]
http://www.geology.ucdavis.edu/~cowen/Hi
storyofLife/CH05images.html
source: http://www.geology.ucdavis.edu/~
cowen/HistoryofLife/CH05images.html

541,000,000 YBN
341) The Lophotrochozoa Phylum Nemertea
(ribbon worms) evolves.


  
540,000,000 YBN
133) Earliest trilobite fossil.

  
539,000,000 YBN
342) The Lophotrochozoa Phylum Mollusca
(brachiopods, bryozoans, clams,
mussels, squids and octopuses
{cephalopods}, and snails) evolves.


  
537,000,000 YBN
343) The Lophotrochozoa Phylum Annelida
(segmented worms) evolve.


  
537,000,000 YBN
344) The Lophotrochozoa Phylum
Sipuncula (peanut worms) evolve.


  
530,000,000 YBN
350) Deuterstome Chordata Subphylum
Vertebrata evolves. This Subphylum
contains most fish, all amphibians,
reptiles, and mammals.


  
530,000,000 YBN
351) Subphylum Vertebrata jawless fish
(agnatha) evolve.


  
530,000,000 YBN
386) Oldest fossil vertebrate and fish.
Haiko
uichthys ercaicunensis: About 25 mm in
length.

 
[1] Figure 4 The Lower Cambrian
agnathan vertebrate Haikouichthys
ercaicunensis Luo, Hu & Shu gen. et sp.
nov. from Haikou, Yunnan. Specimen
HZ-f-12-127. a, Entire specimen,
anterior to the left; more posterior
region appears to fade out into
sediment, possibly representing decay
of body; attempts to excavate this area
were not successful. Scale bar
equivalent to 5 mm. b, Detail of
anterior to show putative gill bars,
possible elements of cranial
endoskeleton, and pericardic area;
scale bar equivalent to 5 mm. c,
Camera-lucida drawing of specimen to
show interpretation. Numbers 1-6
indicate units of the branchial basket
that are identified with some
confidence; ?A-?C refer to less secure
identifications. Two possible areas
representing the pericardic cavity are
indicated. To the anterior of ?C a
triangular area with patches of
diagenetic mineralization is one
possibility; a fainter region to the
posterior is the alternative location.
COPYRIGHTED
source: http://www.nature.com/nature/jou
rnal/v402/n6757/fig_tab/402042a0_F4.html

520,000,000 YBN
205) Dinoflagellate biological markers
measured in Kopli quarry, Tallinn,
Estonia.


  
507,000,000 YBN
140) Aysheaia (onychophoran, also
described as lobopod) fossil, from
Burgess shale.

 

source: 1 & 2
http://www.nmnh.si.edu/paleo/shale/paysh
ia.htm



source: 3
http://www.ucmp.berkeley.edu/onychoph/on
ychophorafr.html

507,000,000 YBN
145) Priapulid worm fossils of Burgess
Shale.

 
[1] Ottoia, showing muscle bands and
gut. Ottoia is a priapulid worm found
commonly in the Burgess Shale. It was
carnivorous, and probably lived in a
burrow like modern priapulids. This
specimen has been wetted and oriented
to reflect the light, in order to show
a delicate irridescent film which
preserves details of muscle bands, the
gut, and even the small hooks at one
end of the worm (on the right --
unfortunately out of focus). Walcott
quarry.
source: http://www.geo.ucalgary.ca/~macr
ae/Burgess_Shale/Ottoia_muscle.gif


[2] Phylum
Priapulida Ottoia Priapulid worm.
Note the anterior proboscis (on the
left) and the dark trace of the
interior digestive tract. Ottoia was
carnivorous.
source: http://www.gpc.edu/~pgore/geolog
y/geo102/burgess/burgess.htm

507,000,000 YBN
146) Opabinia fossils of Burgess Shale.
 

source: http://www.nmnh.si.edu/paleo/sha
le/popabin.htm



source: http://www.nmnh.si.edu/paleo/sha
le/popabin.htm

507,000,000 YBN
147) Animalocaris fossils of Burgess
Shale.

 
[1] diagram
source: http://www.nmnh.si.edu/paleo/sha
le/panomal.htm


[2] jaws
source: http://www.nmnh.si.edu/paleo/sha
le/panomal.htm

507,000,000 YBN
149) Marrella (Arthropod) fossils in
Burgess Shale.


 
[1] diagram
source: http://www.nmnh.si.edu/paleo/sha
le/pmarella.htm


[2] fossil
source: http://www.nmnh.si.edu/paleo/sha
le/pmarella.htm

505,000,000 YBN
74) Oldest fossil of an artropod
moulting.

 
[1] a, Specimen of M. splendens (ROM
56781) emerging and pulling out the
flexible lateral spines from the old
exoskeleton (exuvia). b, Camera lucida
drawing of the same specimen. Scale bar
for a and b, 5 mm. c, Reconstruction of
Marrella (modified from ref.
8). COPYRIGHTED
source: http://www.nature.com/nature/jou
rnal/v429/n6987/fig_tab/429040a_F1.html

500,000,000 YBN
230) Ascomycota Fungi "Pyrenomycetes"
(head scab fungus, orange bread mold,
rice blast fungus) and "Plectomycetes"
(aspergillus, penicilin fungus,
coccidiodomycosis fungus) evolve.

  
490,000,000 YBN
121) Start Ordovician (490-443 mybn),
end Cambrian period (543-490 mybn).


  
475,000,000 YBN
90) Genetic comparison shows the
ancestor of all plants (Kingdom
Plantae) evolving at this time (in the
view that algae are protists and not
plants).

Genetic comparison shows the ancestor
of all plants (Kingdom Plantae)
evolving at this time (in the view that
algae are single and multicellular
protists and not plants).

 

source: http://protist.i.hosei.ac.jp/PDB
3/PCD3711/htmls/86.html



source: http://protist.i.hosei.ac.jp/PDB
/Images/Others/Glaucocystis/

475,000,000 YBN
232) Genetic comparison shows the
non-vascular plant and vascular plant
lines splitting now.


  
475,000,000 YBN
233) Genetic comparison shows
Liverworts (Plant Division
Marchantiophyta) evolving now.

 
[1] A thallose liverwort, Lunularia
cruciata public domain
source: http://en.wikipedia.org/wiki/Liv
erworts


[2] Arachniopsis diacantha is an
algae-like leafy liverwort of the
family Lepidoziaceae. Arachniopsis
diacantha, a liverwort from brazilian
rain forest by J. Z. Berger public
domain
source: same

475,000,000 YBN
244) Genetic comparison shows
non-vascular plants (Bryophytes)
(Liverworts, Hornworts, Mosses)
evolving now.

Many people view these plants
and the beginning of the Plant kingdom
and algae as being in the Protista
kingdom.
These plants lack vascular tissue that
circulates liquids. They neither flower
nor produce seeds, reproducing via
spores.
The order these three divisions evolved
in is not fully known.

 
[1] Phaeoceros laevis (L.) Prosk. gnu
source: http://en.wikipedia.org/wiki/Ima
ge:Anthoceros_levis.jpg


[2] Image of Phaeoceros (hornwort)
spores taken by J. Ziffer. public
domain
source: wiki

475,000,000 YBN
352) Subphylum Vertebrata jawless fish
lampreys and hagfish lines separate.


  
470,000,000 YBN
234) Genetic comparison shows Hornworts
(division Anthocerotophyta) evolving
now.

 
[1] Phaeoceros laevis (L.) Prosk. gnu
source: http://en.wikipedia.org/wiki/Ima
ge:Anthoceros_levis.jpg


[2] Image of Phaeoceros (hornwort)
spores taken by J. Ziffer. public
domain
source: wiki

464,000,000 YBN
398) Earliest fossil spore belonging to
land plants.

These spores look like
the spores of living liverworts.

  
460,000,000 YBN
84) Earliest fungi fossil.
 
[1] Figure 1. (A to C and E to G)
Fossil hyphae and spores from the
Ordovician and (D and H) spores formed
by extant glomalean fungi. (A and B)
Overviews of the fossilized material.
(C, E, F, and G) Fossil spore details.
(C) Detail of (B). (D) A spore of
present-day Glomus sp. S328 with
layered wall structure. In (G), the
arrow shows walls of a subtending hypha
in connection with the spore wall. (H)
A spore of present-day Glomus
leptotichum, a member of the deeply
divergent glomalean lineages. Images
were obtained by light microscopy (28)
of the specimens in air (A, C, F, and
G), differential interference contrast
microscopy of the specimens in
polyvinylalcohol-lactoglycerol (D, E,
and H), and confocal laser scanning
microscopy with the autofluorescence of
the material (B). All scale bars are 50
µm.
source:

460,000,000 YBN
235) Genetic comparison shows Mosses
(division Bryophyta) evolving now.

 
[1] A moss covered log. Photo by sannse
at Mistley, England. GNU
source: http://en.wikipedia.org/wiki/Mos
s


[2] life cycle of
moss ladyofhats public domain
source: same

460,000,000 YBN
353) Jawed vertebrates (Infraphylum
Gnathostomata) evolve. This large group
includes all jawed fish, all
amphibians, reptiles, and mammals.


  
460,000,000 YBN
354) Jawed vertebrate (Infraphylum
Gnathostomata) Class Chondrichthyes
(cartilaginous fishes) evolve.


  
450,000,000 YBN
106) First chordates. The Chordata
phylum includes all tunicates, fishes,
amphibians, reptiles, birds, and
mammals. The living chordate with the
oldest DNA design are tunicates.


  
443,000,000 YBN
122) Start Silurian period (443-417),
end Ordovician period (490-443 mybn).


  
440,000,000 YBN
360) In the Jawed Fishes, the
Ray-finned fishes (Subclass
Actinopterygii) evolve.

Ray-finned fishes
(Subclass Actinopterygii) are in Class
Osteichthyes.

  
428,000,000 YBN
401) Oldest fossil of vascular land
plants, Cooksonia.

Oldest fossil of
vascular land plants, Cooksonia
pertoni.

They have been found in an area
stretching from Siberia to the Eastern
USA, and in Brazil. They are found
mostly in the area of Euramerica, and
most of the type specimens are from
Britain.

Cooksonia were very small plants, only
a few centimetres tall, and had a
simple structure: They didn't have
leaves, flowers or seeds. They had a
simple stalk, that branched a few
times. Each branch ended in a
sporangium, a rounded structure that
contained the spores. No specimen has
been found attached to roots. Either it
connected to the ground with very fine
root hairs, the fossils are of
fragments, or something entirely
unanticipated. Some specimens have a
dark stripe in the centre of their
stalks which is interpreted as being
the remains of water carrying tissue.
Not all specimens have this stripe,
either some Cooksonia lacked vasular
tissue, or it was destroyed in the
fossilization process.

 
[1] Cooksonia pertoni with three
sporangia. Height of the plant 2.5
cm Pridolian (Upper
Silurian) Shropshire, England.
COPYRIGHTED
source: http://www.xs4all.nl/~steurh/eng
cook/ecookwal.html


[2] Cooksonia pertoni, fossilised
plant COPYRIGHTED UK
source: http://owen.nhm.ac.uk/piclib/web
images/0/0/900/936_sml.jpg

428,000,000 YBN
402) Oldest fossil land animal, the
millipede Pneumodesmus.




  
425,000,000 YBN
377) Coelacanths evolve.
2 living species
known.

  
417,000,000 YBN
123) Start Devonian period (417-354
mybn), end Silurian period (443-417
mybn).


  
417,000,000 YBN
378) Lungfishes evolve.

  
412,000,000 YBN
403) Oldest fossil lung fish.



  
409,000,000 YBN
404) Oldest fossil shark.



  
400,000,000 YBN
85) Earliest lichen fossil.
  
400,000,000 YBN
236) Genetic comparison shows the
oldest line of living vascular plants
from the Division "Lycophyta" evolving
now.

Genetic comparison shows the oldest
line of living vascular plants
(Tracheophytes) from the Division
"Lycophyta" evolving now.

 
[1] Lycopodiella cernua (L.) Pic. Serm.
plant from windward O'ahu (Hawai'i)
taken in December 2003 by Eric Guinther
and released under the GNU Free
Documentation License. gnu
source: http://en.wikipedia.org/wiki/Lyc
ophyte


[2] Fossil trunk of Lepidodendron
aculeatum showing leaf scars gnu
source: http://en.wikipedia.org/wiki/Lep
idodendron

400,000,000 YBN
399) Earliest fossil of an insect.
This
fossil also could have been winged.



 
[1] Rhyniognatha hirsti. COPYRIGHTED
source: http://www.nhm.ac.uk/nature-onli
ne/earth/fossils/article-oldest-insect-f
ossil/the-oldest-fossil-insect-in-the-wo
rld.html

390,000,000 YBN
355) Cartilaginous Fishes (Class
Chondrichthyes) Subclass
Subterbranchialia and Subclass
Elasmobranchii (shark-like fishes)
separate.


  
390,000,000 YBN
356) Subclass Subterbranchialia
Superorder Holocephali (chimaeras: eg.
elephant fish) evolves.


  
380,000,000 YBN
243) Genetic comparison shows the Fern
line and the line that leads to Seed
Plants (Gymnosperms and Angiosperms)
separating now.


  
380,000,000 YBN
246) Genetic comparison shows the Spore
producing and Seed producing plant
lines separating now.

Genetic comparison
shows the Spore producing (ferns and
all earlier plants) and Seed producing
(Spermatophyta, Gymnosperms and
Angiosperms) plant lines separating
now.

  
380,000,000 YBN
405) Oldest fossil large trees. First
forests.




  
380,000,000 YBN
406) Oldest fossil spider.



  
375,000,000 YBN
407) Oldest fossil amphibian, and land
vertebrate.

Oldest fossil amphibian,
Acanthostega , from Greenland Also, the
oldest evidence of land vertebrates.



  
360,000,000 YBN
237) Genetic comparison shows Ferns
(Plant Division "Pteridophyta")
evolving now.

Genetic comparison shows the
Plant Division "Pteridophyta" (Ferns)
evolving now.
Whisk and Ophioglossiod
ferns, Marattiod ferns, Horsetails,
Lepto. ferns.

 
[1] Ferns, Melbourne Botanical
Gardens gnu
source: http://en.wikipedia.org/wiki/Fer
n


[2] An Australian tree fern growing
on O'ahu, Hawai'i. Photographed by Eric
Guinther. A tree fern unrolling a new
frond GNU
source: same

360,000,000 YBN
408) Devonian mass extinction caused by
ice age.




  
354,000,000 YBN
124) Start Carboniferous period
(354-290 mybn), end Devonian period
(417-354 mybn).


  
350,000,000 YBN
361) In the Ray-finned fishes
Superdivision Chondrostei (sturgeons
and paddlefish) evolves.


  
350,000,000 YBN
362) In the Ray-finned fishes
Infradivsion Cladistia (Bichirs)
evolves.


  
340,000,000 YBN
379) Tetrapods evolve.
(Superclass Tetrapoda)
  
340,000,000 YBN
380) Amphibians (Caecillians, frogs,
toads, Salamanders) evolve.

(Superclass
Tetrapoda, Class Amphibia)

  
330,000,000 YBN
409) Oldest fossil conifer.



  
325,000,000 YBN
381) The Amphibians Caecillians evolve.
(Superc
lass Tetrapoda, Class Amphibia)

  
320,000,000 YBN
238) Genetic comparison shows the
oldest living Gymnosperms from the
Plant Kingdom evolving now.

Genetic
comparison shows the oldest living
Gymnosperms (Greek for "Naked Seed"),
Cycads, from the Plant Kingdom evolving
now. These are the first seed bearing
plants.

Gymnosperm Plant Divisions are:
Pinophyta -
Conifers "Pinaceae" 220 "Other
conifers" 400 species
Ginkgophyta - Ginkgo 1
species
Cycadophyta - Cycads 130 species
Gnetophyta -
Gnetum, Ephedra, Welwitschia 80 species

 
[1] Leaves and female cone of Cycas
revoluta GNU
source: http://en.wikipedia.org/wiki/Cyc
ad


[2] Leaves and male cone of Cycas
revoluta Photo of Cycas (sago cycad)
inflorescence, taken July 2001 by
User:Stan Shebs Cycas revoluta - male
plant GNU
source: same

318,000,000 YBN
242) Genetic comparison shows the
Gymnosperms and Angiosperms lines
separating now.


  
315,000,000 YBN
410) Oldest fossil reptile.
Hylonomus
was a small lizard-like reptile that
was trapped in the trunk of a swamp
tree in what is now Nova Scotia ,
Canada.



  
315,000,000 YBN
411) Oldest fossil of flying insect
(mayfly?).

Oldest fossil of flying
insects (unless Devonian Rhyniognatha
had wings). Fossil wings on giant
mayflies, dragonflys, and
dragonfly-like arthropods.



  
315,000,000 YBN
453) Allegheny mountains form as a
result of the collision of Europe and
eastern North America.




  
310,000,000 YBN
384) Egg evolves.
This group, the Amniota, will
branch into the 3 major Classes:
Reptiles (Sauropsida), Birds (Aves),
and Mammals (Synapsida).


  
310,000,000 YBN
385) Reptiles evolve.

  
305,000,000 YBN
382) The Amphibians Frogs and Toads
evolve.

(Superclass Tetrapoda, Class Amphibia)
  
305,000,000 YBN
383) Amphibians Salamanders evolve.
(Superclass
Tetrapoda, Class Amphibia)

  
300,000,000 YBN
387) Turtles, Tortoises and Terrapins
evolve.


  
290,000,000 YBN
125) Start Permian period (290-248
mybn), end Carboniferous period
(354-290 mybn).


  
290,000,000 YBN
239) Genetic comparison shows the
second oldest living Gymnosperm, Ginkgo
from the Plant Kingdom evolving now.

 
[1] * Description: Leaves of Ginkgo
biloba. * Source: picure taken by
Reinhard Kraasch in his own garden in
August 2003 (from German wikipedia)
* Licence: released per the GNU Free
Documentation License by the
photographer
source: http://en.wikipedia.org/wiki/Gin
kgo


[2] Name Ginkgo biloba Family
Ginkgoaceae Image no. 1 Permission
granted to use under GFDL by Kurt
Stueber GNU Ginkgo fruit and leaves
source: same

280,000,000 YBN
388) Anapsids (iguanas and snakes) and
diapsids (crocodiles) separate.


  
270,000,000 YBN
240) Genetic comparison shows the third
oldest living Gymnosperms, Conifers
(Plant division "Pinophyta") evolving
now.

 
[1] Closeup shot of a stem of needles
(perhaps Norway spruce?) by USFWS and
obtained from the GIMP photo
library. United States Federal
Government This work is in the
public domain because it is a work of
the United States Federal Government.
This applies worldwide. See
Copyright Close-up of pinophyte leaves
(needles): Norway Spruce (Picea abies)

source: http://en.wikipedia.org/wiki/Pin
ophyta


[2] Native Pinus sylvestris forest,
Scotland: Deeside, Mar Lodge, April
2005 GNU 1.2
source: http://en.wikipedia.org/wiki/Pin
aceae

260,000,000 YBN
363) In the Ray-finned fishes
Infradivision Actinopteri evolves.


  
260,000,000 YBN
364) In the Ray-finned fishes
Infradivision Actinopteri, Gars evolve.


  
255,000,000 YBN
389) Tuataras evolve.

  
251,000,000 YBN
452) The supercontinent Pangea forms.



  
250,000,000 YBN
241) Genetic comparison shows the
fourth oldest living Plant Division
"Gnetales" evolving now.

 
[1] Photo of a Welwitschia mirabilis,
taken in the Ugab River valley in
Namibia in October 2004 by Muriel
Gottrop. The photo shows a female
plant, recognizable by the oval shaped
seed pods. Creative Commons
License Creative Commons Attribution
iconCreative Commons Share Alike icon
This image is licensed under the
Creative Commons Attribution
ShareAlike License v.
1.0: http://creativecommons.org/license
s/by-sa/1.0/
source: http://en.wikipedia.org/wiki/Wel
witschia


[2] Wikimedia Commons logo This is a
file from the Wikimedia Commons. The
description on its description page
there is shown below. Genus
Welwitschia Gnetopsida Oroginally
uploaded by User:Roger_Zenner at the
German Wikipedia on 24 Sept. 2004.
Caption says it was photographed by
Freddy Weber for User:Robert_Zenner in
Auhust 2004 in Namibia. Info from
German Wikipedia: Lizenz: Gemeinfrei
(Public Domain), fotografiert von
Freddy Weber (für
Benutzer:Roger_Zenner) im August 2004
in Namibia. public domain
source: same

250,000,000 YBN
396) The Permian mass extinction event
happens. This is the most devastating
mass extinction event in the history of
earth.

Trilobites become extinct.


 
[1] Timeloine of mass extinctions.
COPYRIGHTED Benjamin Cummings.
source: http://io.uwinnipeg.ca/~simmons/
16cm05/1116/16macro.htm

248,000,000 YBN
54) End Paleozoic Era, start Mesozoic
Era.


  
248,000,000 YBN
126) Start Triassic period (248-206
mybn), end Permian period (290-248
mybn).


  
245,000,000 YBN
392) Crocodiles, allegators, caimans
evolve.


  
245,000,000 YBN
393) Birds evolve.

  
240,000,000 YBN
365) Actinopteri Superdivision
Neopterygii evolves.


  
240,000,000 YBN
366) In Superdivision Neopterygii,
Subdivision Halecomorphi, Bow fish
(Amiiformes) evolve.


  
240,000,000 YBN
367) Bow fish evolve.
In Superdivision
Neopterygii, Division Halecostomi,
Subdivision Halecomorphi, Bow fish
(Amiiformes) evolve.

  
228,000,000 YBN
412) Oldest dinosaur fossil, Eorapter
was found in South America.

Oldest
dinosaur fossil. Eoraptor was found in
South America . This little dinosaur
was a cat-sized meat eater.



  
220,000,000 YBN
400) Oldest mammal fossil.
This is a
fingernail-sized skull found in Texas.



  
215,000,000 YBN
428) Oldest Pterosaur fossil.



  
210,000,000 YBN
368) Subdivision Teleostei (eels,
herrings, anchovies, carp, minnows,
piranha, salmon, trout, pike, perch,
seahorse, cod) evolves.

In Superdivision
Neopterygii, Division Halecostomi,
Subdivision Halecomorphi, Bow fish
(Amiiformes) evolve.

  
210,000,000 YBN
369) Bonytongues evolve.
In Subdivision
Teleostei Bonytongues evolve.

  
210,000,000 YBN
390) Iguanas, chamaeleons, spiny
lizards evolve.


  
210,000,000 YBN
391) Snakes, Skinks, Geckos evolve.

  
210,000,000 YBN
413) Oldest turtle fossil.
Oldest
turtle fossil, Proganochelys.



  
209,500,000 YBN
489) Triconodonta (extinct mammals)
evolve.




  
206,000,000 YBN
127) Start Jurassic period (206-144
mybn), end Triassic period (248-206
mybn).


  
200,000,000 YBN
370) Eels and tarpons (Elopocephala)
evolve.

In Subdivision Teleostei Eels and
tarpons (Elopocephala) evolve.

  
199,000,000 YBN
414) End of Triassic mass extinction,
because of climate (temperature?,
weather?) changes. Large outpourings
of lava from break-up of Pangea may
have caused climate change.

50% of
life went extinct, including thecodonts
and synapsids.



  
190,000,000 YBN
357) Subclass Elasmobranchii
(shark-like fishes) divides into 2
divisions Squalea (rays, skates) and
Galeomorphii (great white, hammerhead,
nurse, sand tiger sharks).


  
190,000,000 YBN
358) Division Squalea (rays, skates)
evolve.


  
190,000,000 YBN
359) Division Galeomorphii (great
white, hammerhead, nurse, sand tiger
sharks) evolve.


  
190,000,000 YBN
371) Herrings and anchovies evolve.
Herrings
and anchovies (Division Clupeomorpha)
evolve.

  
185,000,000 YBN
194) Oldest diatom (Heterokonts or
Chromalveolates) fossils.


 

source: http://www.nature.com/news/2003/
030217/images/diatom_180.jpg



source: http://www.ucmp.berkeley.edu/chr
omista/diatoms/diatomdiverse.jpg

180,000,000 YBN
456) First mammals, Monotremes evolves.
Monotremes lay eggs and are the
oldest warm blooded species of record.

Order:
Monotremata (C.L. Bonaparte, 1837)
or

Subclass Prototheria (Gill, 1872:vi)



  
175,000,000 YBN
245) Genetic comparison shows the most
ancient flowering plant (Angiosperm)
still alive, "Amborella" evolving now.

This
begins the "broad-leaf" plants.
There is only 1
species of Amborella still living.
Angiosperms
(flowering plants) are the first plant
to produce fruits. A fruit is the
ripened ovary, together with seeds, of
a flowering plant. In many species, the
fruit incorporates the ripened ovary
and surrounding tissues. Fruits are the
means by which flowering plants
disseminate seeds.
Class is "Palaeodicots"?

 
[1] Photo of Amborella trichopoda
(Amborellaceae; photo © Sangtae Kim).
source: http://tolweb.org/tree?group=ang
iosperms


[2] none
source: http://www.ucsc.edu/currents/99-
00/08-30/amborella.photo2.htm

170,000,000 YBN
372) Carp, minnows, Piranhas evolve.

  
170,000,000 YBN
373) Salmon, Trout, Pike evolve.

  
165,000,000 YBN
247) Genetic comparison shows the
second oldest line of Angiosperms, the
Water Lilies ("Nymphaeales") evolving
now.

70 species.
 
[1] Nymphaea alba Nymphaea alba -
image taken on 29 August 2004 in the
outdoor botanical garden of Technion -
Haifa, Israel public domain
source: http://en.wikipedia.org/wiki/Nym
phaeaceae


[2] Nymphaea colorata from
Africa presume is gnu or pd
source: same

150,000,000 YBN
374) Lightfish and Dragonfish evolve.

  
150,000,000 YBN
394) Oldest bird fossil, Archaeopteryx.
The
Archaeopteryx fossil is from the
Solnhofen Limestone of the Upper
Jurassic of Germany.

Archaeopteryx is a member of the
extinct Subclass Archaeornithes.

There are many unsolved questions about
birds. Did birds evolve flight from
trees or from the ground? From what
part of the body did feathers evolve?
What colors were the first birds? Was
Archaeopteryx warm blooded?

 
[1] Archaeopteryx siemensii HMN
1880/81 (Berlin) COPYRIGHTED EDU
source: http://www.oucom.ohiou.edu/dbms-
witmer/dinoskulls02.htm


[2] Archaeopteryx sp. JM 2257
(Eichstätt) COPYRIGHTED EDU
source: http://www.oucom.ohiou.edu/dbms-
witmer/dinoskulls02.htm

150,000,000 YBN
395) Bird Confuciusornis fossil.

Unlike Archaeopteryx, Confuciusornis
had no teeth.




 
[1] Confuciusornis
source: http://www.ucmp.berkeley.edu/dia
psids/birds/confuciusornislg.jpg

146,000,000 YBN
490) Multituberculata (extinct major
branch of mammals) evolve.




  
145,000,000 YBN
415) Oldest flower fossil.
Oldest
flower fossil, Archaefructus, in China,
a submerged wetland plant.



 
[1] Archaefructus liaoningensis. The
leaf-like structures on the stem of
this 140 million year old fossil are
pods containing the seeds, a
characteristic unique to flowering
plants. Credit: University of Florida.
PD?
source: http://science.nasa.gov/headline
s/y2001/ast17apr_1.htm?list118443


[2] Archaefructus liaoningensis Sun,
Dilcher, Zheng et Zhou (Sun et al.,
1998). Fruiting axes and remains of two
subtending leaves (Photo courtesy of
David Dilcher). COPYRIGHTED EDU
source: http://www.flmnh.ufl.edu/deeptim
e/virtualfossilcollection/Archaeofructus
.html

144,000,000 YBN
128) Start Cretaceous period (144-65
mybn), end Jurassic period (206-144
mybn).


  
140,000,000 YBN
457) Marsupials evolve.

  
140,000,000 YBN
458) Metornithes (early birds) evolve.



 
[1] Alvarezsaurid. COPYRIGHTED
source: http://www.palaeos.com/Vertebrat
es/Units/350Aves/350.200.html

138,000,000 YBN
459) Ornithothoraces (early birds)
evolve.




 
[1] Iberomesornis
COPYRIGHTED, Iberomesornis
COPYRIGHTED
source: http://www.dinosauromorpha.de/th
eropoda/iberomesornis.JPG



source: http://www.lemanlake.com/photos/
biotope/biodiversite/iberomesornis.gif

136,000,000 YBN
460) Enantiornithes (early birds)
evolve.




 
[1] Sinornis santensis Artist: James
Reece COPYRIGHTED AUSTRALIA
source: http://www.amonline.net.au/chine
se_dinosaurs/feathered_dinosaurs/photo07
.htm

134,000,000 YBN
461) Ornithurae (early birds) evolve.



 
[1] fossil specimen of Chaoyangornis
COPYRIGHTED
source: http://www.sino-collector.com/en
g/_private/cjyd/zjlt/hjs-hs/pic-l/hs0016
.jpg


[2] Chaoyangia, modified from Hou et
al. (1996) COPYRIGHTED EDU
source: http://rainbow.ldeo.columbia.edu
/courses/v1001/clover16.html

132,000,000 YBN
462) Hesperornithiformes (early birds)
evolve.




 
[1] Hesperornis. COPYRIGHTED
source: http://www.savageancientseas.com
/images/labels/hesperornis.jpg


[2] Detail of a painting by Ely Kish,
Copyright © Ely Kish; used with
permission of Ely Kish (EMAIL)
Hesperornis regalis Hesperornis
(pronounced HES-per-OR-nis) means
''western bird''. Toothed marine birds
of the Late Cretaceous
seas COPYRIGHTED
source: http://www.oceansofkansas.com/He
sperornis/kish-01.jpg

130,000,000 YBN
375) Perch, Plaice, seahorses evolve.

  
130,000,000 YBN
376) Cod, hake, anglerfish evolve.

  
128,000,000 YBN
248) Genetic comparison shows the
Angiosperm "Austrobaileyales" evolving
now.

 
[1] Austrobaileya scandens
(Austrobaileyaceae) mature
fruit Lamins Hill via Malanda,
Queensland date uncertain Larger
image (81K) Robust vine in rainforest
canopy. It is a single species in an
Australian endemic family. Its pollen
is the oldest recorded flowering plant
pollen in Australia. See reference
under Image 7-93. Mesophyll/notophyll
vine forest.
source: http://www.gu.edu.au/ins/collect
ions/webb/html/6-15.html


[2] Austrobaileya scandens C.T.
White * Query NCU-3e or IPNI
* Common Name: * Family:
Austrobaileyaceae (Croiz.) Croiz.
* Country of Origin: Australia -
Queensland * Habitat: Mesophyll /
notophyll vine forest *
Eco-region(s): o AA0117 -
Queensland tropical rain forests
* Description: Evergreen, woody vines
with loosely twining main stem and
straight, leafy lateral branches
endemic to the rainforests of northeast
Queensland, Australia. This species is
the only member of the genus and the
genus is the only member of the family,
Austrobaileyaceae. It is a very
primitive angiosperm family although it
is sometimes placed in the Magnoliales
(Cronquist) or Laurales. Cronquist
considers it an ''isolated small group,
not wholly compatible with the bulk of
either the Laurales or Magnoliales, but
not sufficiently distinctive to
constitute a family of its own.''
The flowers are rather large,
solitary in the axils of the leaves,
with a putrescent odor, probably
pollinated by flies. Its
pollen is the oldest recorded flowering
plant pollen in Australia.
source: http://florawww.eeb.uconn.edu/im
ages/byspecies/AUSTROBAILEYA_SCANDENS_01
.JPG

128,000,000 YBN
249) Genetic comparison shows the
Angiosperm "Chloranthaceae" evolving
now.

 
[1] Hedyosmum scaberrimum AB201a is
from arizona.edu
source: http://eebweb.arizona.edu/grads/
alice/Chloranthaceae/Hedyosmum%20scaberr
imum%20AB201a.html


[2] Scientific Name Chloranthus
japonicus Location Vityaz inlet,
Gamov Peninsula, Khasansky distr.,
Primorsky Territory (Russian
Federation) Acknowledgements courtesy
CalPhotos Copyright © 2001 Nick
Kurzenko
source: http://tolweb.org/tree?group=Chl
oranthaceae

128,000,000 YBN
250) Genetic comparison shows the
Angiosperm group "Magnoliids" evolving
now.

 
[1] Magnolia This photo is a part of
the Wikipedia:Plant photo collection
I. Downloaded URL:
http://tencent.homestead.com/files/magno
lia.jpg Warning sign This image has
no source information. Source
information must be provided so that
the copyright status can be verified by
others. Unless the copyright status is
provided and a source is given, the
image will be deleted seven days after
this template was added (see page
history). If you just added this
template, please use {{no source
source: http://en.wikipedia.org/wiki/Mag
noliales


[2] ~~~~~}} (to include the date
here). Please consider using {{no
source notified
source: same

128,000,000 YBN
251) Genetic comparison shows the
Angiosperm "Ceratophyllaceae" evolving
now.

 
[1] Ceratophyllum
submersum Description: Ceratophyllum
submersum; an aquatic plant. GNU
source: http://en.wikipedia.org/wiki/Cer
atophyllaceae


[2] Ceratophyllum
demersum Ceratophyllum_demersum3.jpg
(78KB, MIME type: image/jpeg) Common
Hornwort (Ceratophyllum
demersum) usgs
source: same

128,000,000 YBN
252) Genetic comparison shows the
Angiosperm group "Monocotyledons"
(Monocots) evolving now. Monocots are
the second largest lineage of flowers
after the Eudicots, and include lilies,
palms, orchids, and grasses.

Monocots are the
second largest lineage of flowers after
the Eudicots (formally Dicotyledons)
with
70,000 living species (20,000
species of orchids, and 15,000 species
of grasses).
The two main orders of Monocots are
"Base Monocots" and "Commelinids".
All the grasses on
earth come from this line of flowers
(check).

Base Monocots
(Family Petrosaviaceae)
Acorales
Alismatales
Asparagales
(asparagus, onion, garlic, chives,
agave, yucca, aloe, hyacinth, orchids,
iris, saffron)
Dioscoreales (yam)
Liliales
(lillies)
Pandanales
Commelinids
(Family Dasypogonaceae)
Arecales (palms,date palm,
rattan, coconut)
Commelinales
Poales (grasses: maize
{corn}, rice, barley, oat, millet,
wheat, rye, sorghum, sugarcane, bamboo,
grass, pineapple, water chestnut,
papyrus {many alcohols, breads})
Zingiberales
(cardamom, tumeric, myoga, banana,
ginger, arrowroot)

 
[1] Sweet Flag (Acorus calamus) -
spadix Spadix of Sweet Flag. usgs
public domain
source: http://en.wikipedia.org/wiki/Aco
rus


[2] Ivy Duckweed (Lemna
trisulca) Name Lemna
trisulca Family Lemnaceae
source: http://en.wikipedia.org/wiki/Ali
smatales

128,000,000 YBN
253) Genetic comparison shows the
Angiosperm group Eudicots (includes
most former dicotyledons) evolving now.
Eudicots are the largest lineage of
flowers.

eudicots are also called "tricolpates"
which refers to the structure of the
pollen.
The two main groups are the "rosids"
and "asterids".

  
128,000,000 YBN
254) Genetic comparison shows the
Angiosperm "Basal Eudicots" evolving
now.

 
[1] Creeping butercup (Ranunculus
repens). GNU
source: http://en.wikipedia.org/wiki/Ima
ge:Creeping_butercup_close_800.jpg


[2] Clematis hybrid from
http://www.ars.usda.gov/is/graphics/phot
os/ public domain
source: http://en.wikipedia.org/wiki/Cle
matis

128,000,000 YBN
255) Genetic comparison shows the
Angiosperm groups "Asterids" and
"Rosids" evolving and separating now.


  
128,000,000 YBN
256) Genetic comparison shows the
Angiosperm "Basal Rosids" evolving now.

 
[1] A photo of the tree Staphylea
colchica taken by me in Århus, Denmark
GNU
source: http://en.wikipedia.org/wiki/Cro
ssosomatales


[2] Blossom of Geranium sylvaticum,
closeup, GNU
source: http://en.wikipedia.org/wiki/Cra
nesbill

128,000,000 YBN
257) Genetic comparison shows the
Angiosperm "Eurosids I" evolving now.

 
[1] Oriental Staff Vine Celastrus
orbiculatus US NPS public domain
source: http://en.wikipedia.org/wiki/Sta
ff_vine


[2] Northern Grass of Parnassus
(Parnassia palustris) GNU
source: http://en.wikipedia.org/wiki/Par
nassiaceae

128,000,000 YBN
258) Genetic comparison shows the
Angiosperm "Eurosids I" Order
"Celastrales" evolving now.

 
[1] Oriental Staff Vine Celastrus
orbiculatus US NPS public domain
source: http://en.wikipedia.org/wiki/Sta
ff_vine


[2] Northern Grass of Parnassus
(Parnassia palustris) GNU
source: http://en.wikipedia.org/wiki/Par
nassiaceae

128,000,000 YBN
259) Genetic comparison shows the
Angiosperm "Eurosids I" Order
"Malpighiales" evolving now.

 
[1] mangosteen public domain
source: http://en.wikipedia.org/wiki/Gar
cinia


[2] Mangosteen fruit public domain
source: http://en.wikipedia.org/wiki/Man
gosteen

128,000,000 YBN
260) Genetic comparison shows the
Angiosperm, "Eurosids I" Order
"Oxalidales" evolving now.

 
[1] Oxalis regnellii atropurpurea
(Regnell's Sorrel) GNU
source: http://en.wikipedia.org/wiki/Oxa
lidaceae


[2] Common wood sorrel GNU
source: http://en.wikipedia.org/wiki/Com
mon_wood_sorrel

128,000,000 YBN
261) Genetic comparison shows the
Angiosperm, "Eurosids I" Order
"Fabales" evolving now.

 
[1] Abrus precatorius (Black-eyed
Susan) USGS public domain
source: http://en.wikipedia.org/wiki/Abr
us


[2] Desert false indigo (Amorpha
fruticosa) public domain
source: http://en.wikipedia.org/wiki/Amo
rpha

128,000,000 YBN
262) Genetic comparison shows the
Angiosperm, "Eurosids I" Order
"Rosales" evolving now.

 
[1] U.S. 'Marihuana' production permit,
from the film Hemp for Victory. In the
U.S.A., hemp is legally prohibited, but
during World War II, farmers were
encouraged to grow hemp for cordage, to
replace manila hemp from
Japanese-controlled areas. public
domain
source: http://en.wikipedia.org/wiki/Hem
p


[2] Cannabis sativa, US Fish and
wildlife service public domain
source: http://en.wikipedia.org/wiki/Can
nabis_sativa

128,000,000 YBN
263) Genetic comparison shows the
Angiosperm, "Eurosids I" Order
"Cucurbitales" evolving now.

 
[1] White bryony (Bryonia dioica). GNU
source: http://en.wikipedia.org/wiki/Ima
ge:White_bryony_male_800.jpg


[2] watermelon public domain
source: http://en.wikipedia.org/wiki/Ima
ge:Vampire_watermelon.jpg

128,000,000 YBN
264) Genetic comparison shows the
Angiosperm, "Eurosids I" Order
"Fagales" evolving now.

 
[1] Alnus serrulata (Tag Alder) Male
catkins on right, mature female catkins
left Johnsonville, South Carolina GFDL
source: http://en.wikipedia.org/wiki/Ima
ge:Tagalder8139.jpg


[2] Speckled Alder (Alnus incana
subsp. rugosa) - leaves GNU
source: http://en.wikipedia.org/wiki/Ima
ge:Alnus_incana_rugosa_leaves.jpg

128,000,000 YBN
265) Genetic comparison shows the
Angiosperm "Monocotyledon" (Monocot)
group "Base Monocots" evolving now.

 
[1] Sweet Flag (Acorus calamus) -
spadix Spadix of Sweet Flag. usgs
public domain
source: http://en.wikipedia.org/wiki/Aco
rus


[2] Ivy Duckweed (Lemna
trisulca) Name Lemna
trisulca Family Lemnaceae
source: http://en.wikipedia.org/wiki/Ali
smatales

128,000,000 YBN
266) Genetic comparison shows the
Angiosperm "Monocotyledon" (Monocot)
group "Commelinids" evolving now.

Commelinid
s
Arecales (palms,date palm, rattan,
coconut)
Commelinales
Poales (grasses: maize {corn}, rice,
barley, oat, millet, wheat, rye,
sorghum, sugarcane, bamboo, grass,
pineapple, water chestnut, papyrus
{many alcohols, breads})
Zingiberales
(cardamom, tumeric, myoga, banana,
ginger, arrowroot)
(Family Dasypogonaceae) (new
order?)

 
[1] Manila dwarf coconut palm from
http://www.ars.usda.gov/is/graphics/phot
os/ Manila dwarf coconut palm
thumbnail A Manila dwarf coconut palm
on the grounds of the Tropical
Agriculture Research Station in
Mayaguez, Puerto Rico. dept of
ag public domain
source: http://en.wikipedia.org/wiki/Are
cales


[2] coconut GOV public domain
source: http://www.nps.gov/kaho/KAHOckLs
/KAHOplnt/images/IMG_03957.jpg

128,000,000 YBN
267) Genetic comparison shows the
Angiosperm "Core Eudicots" evolving
now.

Includes carnation, cactus, caper,
buckwheat, rhubarb, sundew, venus
flytrap, pitcher plants {old world},
beet, quinoa, spinach, currant, sweet
gum, peony, with-hazel, mistletoe,
grape.

 
[1] Carnation in flower Beschreibung:
Gartennelke (Dianthus caryophyllus)
creative commons
source: http://en.wikipedia.org/wiki/Car
nation


[2] Beets GNU
source: http://en.wikipedia.org/wiki/Bee
t

128,000,000 YBN
268) Genetic comparison shows the
Angiosperm "Eurosids I" Order
"Zygophyllales" evolving now.

 
[1] Bulnesia sarmientoi is a South
American tree species that inhabits the
north of Argentina as well as southern
Brazil and Paraguay. It is one of
several species known as palo santoin
Spanish. [1] Source: Libro del Árbol,
Tome II, edited by Celulosa Argentina
S. A., Buenos Aires, Argentina, October
1975. The visual material is not
explicitly copyrighted, but the editors
thank Mr. Jorge Vallmitjana for his
''photographic
contribution''. Argentina copyright
source: http://en.wikipedia.org/wiki/Ima
ge:Bulnesia_sarmientoi.jpg


[2] Fagonia, US NPS public domain
source: http://www.nps.gov/jotr/activiti
es/blooms/flwrpix/fagonia.jpg

128,000,000 YBN
269) Genetic comparison shows the
Angiosperm "Eurosids II" evolving now.

  
128,000,000 YBN
270) Genetic comparison shows the
Angiosperm "Eurosids II" Order
"Brassicales" evolving now.

 
[1] Aethionema grandiflora, GFDL by
Kurt Stueber
source: http://en.wikipedia.org/wiki/Ima
ge:Aethionema_grandiflora0.jpg


[2] Arabidopsis thaliana, GNU
source: http://en.wikipedia.org/wiki/Ima
ge:Arabidopsis_thaliana.jpg

128,000,000 YBN
271) Genetic comparison shows the
Angiosperm "Eurosids II" Order
"Malvales" evolving now.

 
[1] Bixa orellana L., floro en Lavras,
Minas Gerais, Brazilo, GNU
source: http://en.wikipedia.org/wiki/Ima
ge:Bixa.jpg


[2] Cistus incanus - image taken on
30 March 2004, on the slopes of Mount
Carmel, Israel. public domain
source: http://en.wikipedia.org/wiki/Ima
ge:Cistus_incanus.jpg

128,000,000 YBN
272) Genetic comparison shows the
Angiosperm "Eurosids II" Order
"Sapindales" evolving now.

 
[1] Field Maple foliage and flowers,
Acer campestre. GNU
source: http://en.wikipedia.org/wiki/Ima
ge:Acer-campestre.JPG


[2] Sugar Maple from
www.dnr.cornell.edu NOT GNU
source: http://www.dnr.cornell.edu/ext/f
orestrypage/sfda/graphics/crop%20tree%20
sugar%20maple.jpg

128,000,000 YBN
273) Genetic comparison shows the
Angiosperm "Basal Asterids" evolving
now.

  
128,000,000 YBN
274) Genetic comparison shows the
Angiosperm "Basal Asterids" Order
"Cornales" evolving now.

 
[1] European Cornel (Cornus mas) Paris,
France, cc
source: http://en.wikipedia.org/wiki/Ima
ge:Cornus_mas_flowers.jpg


[2] Common Dogwood flowering (Cornus
sanguinea) non commercial
source: http://en.wikipedia.org/wiki/Ima
ge:Cornussanguinea1web.jpg

128,000,000 YBN
275) Genetic comparison shows the
Angiosperm "Basal Asterids" Order
"Ericales" evolving now.

 
[1] Actinidia fruit. kiwifruit. public
domain
source: http://en.wikipedia.org/wiki/Ima
ge:Actinidia_fruit.jpg


[2] Actinidia deliciosa. kiwifruit,
cc
source: http://en.wikipedia.org/wiki/Ima
ge:Kiwi_aka.jpg

128,000,000 YBN
276) Genetic comparison shows the
Angiosperm "Euasterids I" evolving now.

  
128,000,000 YBN
277) Genetic comparison shows the
Angiosperm "Euasterids I" order
"Garryales" evolving now.

 
[1] Garrya elliptica foliage and
catkins. GNU
source: http://en.wikipedia.org/wiki/Ima
ge:Garrya_elliptica.jpg


[2] Aucuba japonica. GFDL by Kurt
Stueber
source: http://en.wikipedia.org/wiki/Ima
ge:Aucuba_japonica1.jpg

128,000,000 YBN
278) Genetic comparison shows the
Angiosperm "Euasterids I" order
"Solanales" evolving now.

 
[1] Atropa belladonna. Deadly
nightshade. GFDL by Kurt Stueber
source: http://en.wikipedia.org/wiki/Ima
ge:Atropa_bella-donna1.jpg


[2] Berries of the belladonna. Atropa
bella-donna. Deadly nightshade. GFDL by
Kurt Stueber
source: http://en.wikipedia.org/wiki/Ima
ge:Atropa_bella-donna0.jpg

128,000,000 YBN
279) Genetic comparison shows the
Angiosperm "Euasterids I" order
"Gentianales" evolving now.

 
[1] Anthocleista grandiflora. PD
source: http://en.wikipedia.org/wiki/Ima
ge:Anthocleista_grandiflora.jpg


[2] bartonia virginica. PD
source: http://en.wikipedia.org/wiki/Ima
ge:Bartonia_virginica.jpg

128,000,000 YBN
280) Genetic comparison shows the
Angiosperm "Euasterids I" order
"Lamiales" evolving now.

 
[1] Common Bugle (Ajuga reptans) GNU
source: http://en.wikipedia.org/wiki/Ima
ge:Ajuga-reptans01.jpg


[2] Calamintha grandiflora. GFDL by
Kurt Stueber
source: http://en.wikipedia.org/wiki/Ima
ge:Calamintha_grandiflora2.jpg

128,000,000 YBN
281) Genetic comparison shows the
Angiosperm "Euasterids I" (unplaced)
family "Boraginaceae" evolving now.

 
[1] Fiddleneck, species not determined.
in Claremont Canyon Regional Preserve,
Alameda County, California. GNU
source: http://en.wikipedia.org/wiki/Ima
ge:Fiddleneck.jpg


[2] Italian Bugloss (Anchusa azurea).
GNU
source: http://en.wikipedia.org/wiki/Ima
ge:Anchusa_azurea_flores.jpg

128,000,000 YBN
282) Genetic comparison shows the
Angiosperm "Euasterids II" order
"Aquifoliales" evolving now.

 
[1] English holly (female), GNU FDL.
source: http://en.wikipedia.org/wiki/Ima
ge:English_holly.jpg


[2] Ilex aquifolium (L.) GNU
source: http://en.wikipedia.org/wiki/Ima
ge:Acebo.jpg

128,000,000 YBN
283) Genetic comparison shows the
Angiosperm "Euasterids II" order
"Apiales" evolving now.

 
[1] Variegated Ground-elder (Aegopodium
podagraria L.) in flower. GNU
source: http://en.wikipedia.org/wiki/Ima
ge:Ground-elder_bloom.jpg


[2] An established spread of
variegated Ground-elder (Aegopodium
podagraria L.). GNU
source: http://en.wikipedia.org/wiki/Ima
ge:Ground-elder.jpg

128,000,000 YBN
284) Genetic comparison shows the
Angiosperm "Euasterids II" order
"Dipsacales" evolving now.

 
[1] Adoxa moschatellina (L.). 2005
Vellefrey et Vellefrange (France). GNU
source: http://en.wikipedia.org/wiki/Ima
ge:Adoxa_moschatellina01.jpg


[2] Danewort inflorescence. Sambucus
ebulus (L.). European Dwarf Elder. GNU
source: http://en.wikipedia.org/wiki/Ima
ge:Sambucus_nigra_flori_bgiu.jpg

128,000,000 YBN
285) Genetic comparison shows the
Angiosperm "Euasterids II" order
"Asterales" evolving now.

 
[1] Ray floret, typical for flowers of
the family Asteraceae. GNU
source: http://en.wikipedia.org/wiki/Ima
ge:Ray.floret01.jpg


[2] disc floret, typical part of a
flower of the family Asteraceae. GNU
source: http://en.wikipedia.org/wiki/Ima
ge:Disc_floret01.jpg

120,000,000 YBN
463) Neornithes (modern birds) evolve.
More
important anatomical characteristics
include horn beak; teeth absent; fused
limb bones. In addition Neornithes have
a fully-separated four-chambered heart
and typically exhibit complex social
behaviors.



  
112,000,000 YBN
481) Steropodon galmani, an extinct
monotreme, the earliest platypus-like
species, lives.



  
110,000,000 YBN
416) Sauroposiedon, a long-neck
brachiosaur (sauropod) fossil.

Sauropos
iedon fossil, a long-neck (sauropod)
brachiosaur from Oklahoma, possibly the
tallest animal of all time, at an
estimated height of 60 feet.



  
105,000,000 YBN
417) Argentinosaurus, a long-neck
titanosaur (sauropod) fossil.

Argentino
saurus, a long-neck (sauropod)
titanosaur from South America, possibly
the longest animal of all time, at an
estimated 130 to 140 feet length.



  
105,000,000 YBN
491) Afrotheres (elephants, manatees,
aardvarks) evolve.


  
100,000,000 YBN
418) Carnotaurus fossil, a horned,
meat-eating (theropod) dinosaur from
South America.

Carnotaurus fossil, a
horned, meat-eating (theropod) dinosaur
from South America. The fossil
includes skin impressions of its face.



  
100,000,000 YBN
464) Tinamiformes (modern birds)
evolve.

More important anatomical
characteristics include horn beak;
teeth absent; fused limb bones. In
addition Neornithes have a
fully-separated four-chambered heart
and typically exhibit complex social
behaviors.



 
[1] Phylum : Chordata - Class : Aves -
Order : Tinamiformes - Family :
Tinamidae - Species : Crypturellus
tataupa (Tataupa tinamou) Given to the
wikipedia by the owner, Marcos
Massarioli. Status GNU
source: http://pt.wikipedia.org/wiki/Ima
gem:Crypturellus_tataupa.JPG

100,000,000 YBN
465) Ratites (ostrich, emu, cassowary,
kiwis) evolve.




  
100,000,000 YBN
480) Kollikodon ritchiei, an extinct
monotreme lives.



  
95,000,000 YBN
419) Spinosaurus fossil, perhaps the
largest meat-eating dinosaur, estimated
to have been 45 to 50 feet long.

Spinos
aurus fossil, perhaps the largest
meat-eating dinosaur, estimated to have
been 45 to 50 feet long. The only
skeleton ever found was destroyed
during World War 2.



  
95,000,000 YBN
498) Xenarthrans (Sloths, Anteaters,
Armadillos) evolve.


  
85,000,000 YBN
466) Galliformes (Chicken, Duck, Goose,
Turkey, Pheasants, Peacocks, Quail)
evolve.




  
85,000,000 YBN
467) Anseriformes (water birds) evolve.



  
85,000,000 YBN
499) Laurasuatheres evolve. This is a
major line of mammals that include:
bats, camels, pigs, deer, sheep,
hippos, whales, horses, rhinos, cats,
dogs, bears, seals, walrus).


  
84,000,000 YBN
454) Laramide (Rocky) mountains form.



  
82,000,000 YBN
420) Hadrosaurs, duck-billed dinosaurs
are common.

Duck-billed dinosaurs
(hadrosaurs) were common like
Corythyosaurus , Edmontosaurus ,
Lambeosaurus , Maiasaurus , and
Parasaurolophus . Maiasaurs are
examples of dinosaurs from which fossil
nests, eggs, and baby dinosaurs have
been found.



  
82,000,000 YBN
500) Shrews, moles, hedgehogs
(Laurasuatheres) evolve.


  
80,000,000 YBN
421) Protoceratops, an early
shield-headed (ceratopsian) dinosaur
fossil.

Protoceratops, an early
shield-headed (ceratopsian) dinosaur
fossil. It was the first dinosaur
discovered with fossil eggs. These eggs
and nests were found in Mongolia in the
1920's.



  
80,000,000 YBN
422) Raptor (dromaeosaur) fossils.
Rapt
ors (dromaeosaurs) are Cretaceous
dinosaurs, which had large, hook claws
on their feet. Velociraptor is one
example. The most famous Velociraptor
is a skeleton preserved in combat with
a Protoceratops from Mongolia, China .




  
80,000,000 YBN
482) American and true opossums
(American Marsupials) evolve.

This is
the Marsupial Order Didelphimorphia.



  
80,000,000 YBN
501) Bats (Laurasuatheres) evolve.

  
78,000,000 YBN
502) Camels, Pigs, Deer, Sheep, Hippos,
Whales (Laurasuatheres) evolve.


  
77,000,000 YBN
483) Shrew opossums (American
Marsupials) evolve.

This is the
Marsupial Order Paucituberculata. 6
surviving species confined to Andes
mountains in South America.



  
76,000,000 YBN
503) Horses, Tapirs, Rhinos
(Laurasuatheres) evolve.


  
75,000,000 YBN
204) Oldest fossil of testate amoeba
from Grand Canyon, USA.

 

source: Life on a Young Planet

75,000,000 YBN
423) Ceratopsian (shield-headed)
dinosaurs are common.

Ceratopsian
(shield-headed) dinosaurs were common
in the late Cretaceous. Examples are
Monoclonius , and Styrakosaurus .
Triceratops, which lived at the end of
Cretaceous, was the largest of its
kind, reaching 30 feet in length.



  
75,000,000 YBN
492) Aardvark (Afrotheres) evolves.

  
75,000,000 YBN
504) Cats, Dogs, Bears, Weasels,
Hyenas, Seals, Walruses
(Laurasuatheres) evolve.


  
75,000,000 YBN
505) Pangolins (Laurasuatheres) evolve.

  
75,000,000 YBN
506) Euarchontoglires evolve. This is
a major line of mammals that includes
rats, squirrels, rabbits, lemurs,
monkeys, apes, and humans.


  
73,000,000 YBN
484) Bandicoots and Bilbies (Australian
Marsupials) evolve.

This is the
Marsupial Order Peramelemorphia.



  
70,000,000 YBN
424) Two of the largest meat-eating
dinosaurs of all time exist.
Tyrannosaurus rex is the top predator
in North America and Giganotosaurus is
in South America.




  
70,000,000 YBN
425) Ankylosaurs (shield back and/or
club tails) evolve.

The armored
ankylosaurs (had a shield back or
clubbed tail) was the most heavily
armored land-animals in the history of
earth. These plant-eating were low to
the ground for optimal protection.
Many had spikes that stuck out from
their bone-covered back. Ankylosaurus
even had bony plates on its eyelids.



  
70,000,000 YBN
426) Mososaurs, sea serpents evolve.



  
70,000,000 YBN
493) Tenrecs and golden moles
(Afrotheres) evolve.


  
70,000,000 YBN
494) Elephant Shrews (Afrotheres)
evolve.


  
70,000,000 YBN
507) The ancestor of all rabbits, hares
and pikas evolve.


  
70,000,000 YBN
516) The ancestor of Tree Shrews and
Colugos evolves.


  
65,500,000 YBN
397) End of Cretaceous mass extinction
event happens.

Dinosaurs become
extinct.
Also called the K-T
(Kretaceous-Tertiary) extinction.
Huge
amounts of lava erupted from India, and
a comet or meteor collided with the
Earth in what is now the Yucatan
Peninsula of Mexico. No large animals
survived on land, in the air, or in the
sea.



 
[1] Timeline of mass extinctions.
COPYRIGHTED Benjamin Cummings.
source: http://io.uwinnipeg.ca/~simmons/
16cm05/1116/16macro.htm


[2] Cretaceous meteor impact.
COPYRIGHTED Benjamin Cummings.
source: http://io.uwinnipeg.ca/~simmons/
16cm05/1116/16macro.htm

65,000,000 YBN
55) End Mesozoic Era, start Cenozoic
Era.


  
65,000,000 YBN
129) Start Tertiary period (65-1.8
mybn), end Cretaceous period (144-65
mybn).


  
65,000,000 YBN
427) Largest Pterasaur, Quetzalcoatlus
evolve.

Pterasaurs, the flying
reptiles of the Mesozoic reached their
largest size with Quetzalcoatlus, which
had a wing span of 40 ft. This was the
largest flying animal of all time.



  
65,000,000 YBN
429) Rapid increase in new species of
fossil mammals after the extinction of
the dinosaurs.

Most early Cenozoic
mammal fossils are small.



  
65,000,000 YBN
468) Gruiformes (cranes and rails)
evolve.




  
65,000,000 YBN
470) Strigiformes (owls) evolve.



  
65,000,000 YBN
485) Marsupial moles (Australian
marsupials) evolve.

This is the
Marsupial Order Peramelemorphia.



  
65,000,000 YBN
486) Tasmanian Devil, Numbat
(Australian marsupials) evolve.

This
is the Marsupial Order Dasyuromorphia.




  
65,000,000 YBN
487) Monita Del Monte (Australian
marsupial) evolves.

This is the
Marsupial Order Microbiotheria.



  
65,000,000 YBN
488) Wombats, Kangeroos, Possums,
Koalas (Australian marsupials) evolve.


Genetic comparison show Wombats,
Kangeroos, Possums, Loalas (Australian
marsupials) evolve.
This is the
Marsupial Order Diprotodontia.



  
65,000,000 YBN
508) The ancestor of all rats, mice,
gerbils, voloes, lemmings, and hamsters
evolves.


  
65,000,000 YBN
509) The ancestor of all Beavers,
Pocket gophers, Pocket mice and
kangaroo rats evolves.


  
65,000,000 YBN
807) Cetardiodactyla branch. The
ancestor of camels and llamas splits
with the ancestor of the rest of the
Even-Toed Ungulates
(Cetardiodactyla/Artiodactyla: pigs,
ruminants, hippos, dolphins and
whales).

This is just after death of
dinosaurs. Both these ancestors are
still small and probably look like
shrews.

 
[1] Fig. 2. Molecular time scale for
the orders of placental mammals based
on the 16,397-bp data set and maximum
likelihood tree of ref. 14 with an
opossum outgroup (data not shown), 13
fossil constraints (Materials and
Methods), and a mean prior of 105 mya
for the placental root. Ordinal
designations are listed above the
branches. Orange and green lines denote
orders with basal diversification
before or after the K/T boundary,
respectively. Black lines depict orders
for which only one taxon was available.
Asterisks denote placental taxa
included in the ''K/T body size'' taxon
set. The composition of chimeric taxa,
including caniform, caviomorph,
strepsirrhine, and sirenian, is
indicated elsewhere (14). Numbers for
internal nodes are cross-referenced in
the supporting information.
COPYRIGHTED
source: http://www.pnas.org/content/vol1
00/issue3/images/large/pq0334222002.jpeg

63,000,000 YBN
510) The ancestor of all Springhares
and Scaly-tailed Squirrels evolves.


  
63,000,000 YBN
517) The ancestor of Lemurs evolves.

  
63,000,000 YBN
587) Primates evolve.
Most likely in
Africa or the Indian subcontinent.



  
63,000,000 YBN
588) Widespread appearance of primates
starts at base of Eocene.



 
[1] Smilodectes (lemur-like family
Adapidae from the Eocene Epoch)
COPYRIGHTED EDU
source: http://anthro.palomar.edu/earlyp
rimates/first_primates.htm

62,000,000 YBN
495) Elephants (Afrotheres) evolve.

  
60,000,000 YBN
430) In South America, Andes mountians
begin to form.




  
60,000,000 YBN
431) Oldest fossil rodent.



  
60,000,000 YBN
432) Creodont, cat-like species, like
Oxyaena are common.



  
60,000,000 YBN
586) Oldest potential primate fossil in
Morocco.

Genus Altialasius , known
only from several isolated teeth.

  
60,000,000 YBN
796) Largest terrestrial carnivorous
mammal yet found, Andrewsarchus skull
dates from now {verify}.

Andrewsarchus
lived 60-32 mybn.



  
60,000,000 YBN
808) The ancestors of pigs splits from
the line that leads to the Ruminants
(cattle, goats, sheep, giraffes, bison,
buffalo, deer, wildebeast, antelope),
hippos, dolphins, and whales.


 
[1] Fig. 2. Molecular time scale for
the orders of placental mammals based
on the 16,397-bp data set and maximum
likelihood tree of ref. 14 with an
opossum outgroup (data not shown), 13
fossil constraints (Materials and
Methods), and a mean prior of 105 mya
for the placental root. Ordinal
designations are listed above the
branches. Orange and green lines denote
orders with basal diversification
before or after the K/T boundary,
respectively. Black lines depict orders
for which only one taxon was available.
Asterisks denote placental taxa
included in the ''K/T body size'' taxon
set. The composition of chimeric taxa,
including caniform, caviomorph,
strepsirrhine, and sirenian, is
indicated elsewhere (14). Numbers for
internal nodes are cross-referenced in
the supporting information.
COPYRIGHTED
source: http://www.pnas.org/content/vol1
00/issue3/images/large/pq0334222002.jpeg

59,000,000 YBN
496) Hyraxes (Afrotheres) evolve.

  
59,000,000 YBN
497) Manatees and Dugong (Afrotheres)
evolve.


  
58,000,000 YBN
511) The ancestor of all Dormice,
Mountain Beaver, Squirrels and Marmots
evolves.


  
58,000,000 YBN
524) Primate Tarsiers evolve.



  
57,000,000 YBN
433) Oldest hooved mammal fossil.
This
is the ancestor of all hooved mammals,
including cows, deer, horses and pigs.



  
55,000,000 YBN
435) Unitatherium are largest land
animals.



  
55,000,000 YBN
436) Oldest horse fossil.
Oldest
fossil horse, Hyractotherium , the
oldest horse was tiny, about the size
of a dog).



  
55,000,000 YBN
512) Gundis evolves.

  
55,000,000 YBN
809) Lines that lead to Ruminants and
Hippos split.


 
[1] Fig. 2. Molecular time scale for
the orders of placental mammals based
on the 16,397-bp data set and maximum
likelihood tree of ref. 14 with an
opossum outgroup (data not shown), 13
fossil constraints (Materials and
Methods), and a mean prior of 105 mya
for the placental root. Ordinal
designations are listed above the
branches. Orange and green lines denote
orders with basal diversification
before or after the K/T boundary,
respectively. Black lines depict orders
for which only one taxon was available.
Asterisks denote placental taxa
included in the ''K/T body size'' taxon
set. The composition of chimeric taxa,
including caniform, caviomorph,
strepsirrhine, and sirenian, is
indicated elsewhere (14). Numbers for
internal nodes are cross-referenced in
the supporting information.
COPYRIGHTED
source: http://www.pnas.org/content/vol1
00/issue3/images/large/pq0334222002.jpeg

54,970,000 YBN
434) Oldest primate skull.
From the
Hunan Province, China. Other fossils
from the same genus are found in
Europe.
the earliest euprimates can be
distinguished as Cantius, Donrussellia
and Teilhardina.



 
[1] Figure 3: Strict consensus of 33
equally parsimonious trees with the
optimization of activity patterns.
COPYRIGHTED
source: http://www.nature.com/nature/jou
rnal/v427/n6969/fig_tab/nature02126_F3.h
tml


[2] FIGURE 1. The skull of Teilhardina
asiatica sp. nov. (IVPP V12357). a,
Dorsal view of the skull. b,
Reconstruction of the skull based on
IVPP V12357, with grey shadow
indicating the missing parts. Scale
bar, 5 mm. COPYRIGHTED
source: http://www.nature.com/nature/jou
rnal/v427/n6969/fig_tab/nature02126_F1.h
tml

54,000,000 YBN
810) The line that leads to Hippos and
the line to dolphins and whales split.


 
[1] Fig. 2. Molecular time scale for
the orders of placental mammals based
on the 16,397-bp data set and maximum
likelihood tree of ref. 14 with an
opossum outgroup (data not shown), 13
fossil constraints (Materials and
Methods), and a mean prior of 105 mya
for the placental root. Ordinal
designations are listed above the
branches. Orange and green lines denote
orders with basal diversification
before or after the K/T boundary,
respectively. Black lines depict orders
for which only one taxon was available.
Asterisks denote placental taxa
included in the ''K/T body size'' taxon
set. The composition of chimeric taxa,
including caniform, caviomorph,
strepsirrhine, and sirenian, is
indicated elsewhere (14). Numbers for
internal nodes are cross-referenced in
the supporting information.
COPYRIGHTED
source: http://www.pnas.org/content/vol1
00/issue3/images/large/pq0334222002.jpeg

53,500,000 YBN
812) Oldest fossils of dolphins and
whales semiaquatic "Pakicetus".




 
[1] Fig. 2. Molecular time scale for
the orders of placental mammals based
on the 16,397-bp data set and maximum
likelihood tree of ref. 14 with an
opossum outgroup (data not shown), 13
fossil constraints (Materials and
Methods), and a mean prior of 105 mya
for the placental root. Ordinal
designations are listed above the
branches. Orange and green lines denote
orders with basal diversification
before or after the K/T boundary,
respectively. Black lines depict orders
for which only one taxon was available.
Asterisks denote placental taxa
included in the ''K/T body size'' taxon
set. The composition of chimeric taxa,
including caniform, caviomorph,
strepsirrhine, and sirenian, is
indicated elsewhere (14). Numbers for
internal nodes are cross-referenced in
the supporting information.
. COPYRIGHTED
source: http://www.pnas.org/content/vol1
00/issue3/images/large/pq0334222002.jpeg


[2] Illustration by Carl Buell, and
taken from
http://www.neoucom.edu/DEPTS/ANAT/Pakice
tid.html This image is copyrighted.
The copyright holder allows anyone to
use it for any purpose, provided that
this statement is added to its caption:
''Illustration by Carl Buell, and taken
from
http://www.neoucom.edu/Depts/Anat/Pakice
tid.html ''
source: http://en.wikipedia.org/wiki/Ima
ge:Pakicetus.jpg

51,000,000 YBN
513) OW Porcupines evolve.

  
50,000,000 YBN
437) Oldest elephant fossil.
Oldest
elephant fossil, an unnamed fossil from
Algeria.