Evolution Biology 4250
Dr. Adams
Review Sheet 4.2 Test 4
The Original Biomolecular Evolution the Organic from Abiotic?
If we assume organics came from the Earths abiotic environment, then:
1. There must be some way of making these organics (without living organisms).
2. There must be a source of energy to build these larger molecules.
3. These larger organics must be able to polymerize.
4. These larger organics must be stabilized theyd have to persist in a harsh
environment.
Two major alternative hypotheses exist on the source of original simple organics:
1. Abiotic C, H, O & N components of early atmosphere combined somehow
debate rages
over the contents of the atmosphere and water early in Earths history.
After all, conditions were
extremely harsh, and it is unclear what the pressure, temperature and early
atmospheric components
were like.
2. Earth was "seeded" with organics from space; cometary dust, meteorites (still
leaves the
question of where and how these organics formed). For example, the 1969
Murchison, Australia
meteorite contained several amino acids (glycine, alanine, valine, proline,
etc.; pg. 651). Since life
produces almost exclusively L-stereoisomers of A. A.'s, and the meteorite
containedapprox. equal
amounts of L- and D-stereoisomers, then the source of the A. A.'s was unlikely
biological.
Experiments: Miller (1953, 1992); Fox 1972 ammonia, methane, and H.
Provide sparks
(lightning)/UV radiation tremendous number of organics (A.A.s,
sugars, nucleotides). However,
better understanding of the geochemical processes
suggest early atmosphere contained CO2 and
N2, much less conducive to organics
formation.
Still, the Oparin-Haldane Model was formulated, and can at least be used as a
null hypothesis
against which to test new findings. The model basically approaches the
three questions (and four
statements listed above): 1. biotic from abiotic; 2. polymers
assembled that can a) store information
and b) catalyze reactions; 3. add membranes (and energy sources) to get a
living organism (Fig. 17.12).
1. Biotic from abiotic: So far, experiments have not produced large amounts of
one stereoisomer
only of nucleotides or amino acids. Nor have large amounts of ribose (as
opposed to other sugars) been
made. Nucleotides can attach at several places to ribose
(and do so). And without a chemical energy
source, no polymerization takes place.
Getting to specific, self-replicating RNA molecules (with
appropriate chirality) seems difficult to say the least perhaps other
self-replicating systems evolved first
(3rd
paragraph, pg. 657) that in turn promoted development of RNA chains. Certainly, we dont
know
much (yet).
2. Polymerization: in water, although monomers can easily be polymerized (with
an energy source),
they also hydrolyze rapidly. Need some stability how? Ferris, et al,
have demonstrated that the
aluminum-silicate clay mineral Montmorillonite slows hydrolyzing decay, and short polynucleotides have
been formed (and remained) on clay surfaces; with repeated application of more
nucleotides, the clay
catalyzes the reaction and the polynucleotides can be made longer, now up to 50
nucleotides long.
Ferris
and others have similarly assembled polypeptides up to 55 A.A.s long. So, certainly
more
experimental support than for step one. Interestingly, the oldest known
exposed rocks on Earth (3.7
byo) already contain
evidence of life. Older rocks with evidence for life may be very difficult
to find
due to erosive/tectonic/volcanic disruptions, and the conditions were unlikely
conducive to life on the
planet much earlier than that.
3. Life becomes cellular --
the ancestor of all extant organisms: it seems pretty clear that,
regardless of how many times
life may have "started" on the planet, that eventually one main
interbreeding lineage may have become THE one the ancestor of all living things on the planet. We
all use the same
coding mechanism, the same A.A.s, etc., and this machinery is housed in a membrane
a cell.
Many experiments, particularly by Fox, et al, have generated protein containing
"membranes",
with, characteristics of cells (pick up other molecules, "division", etc.). As
you already know,
phospholipids thrown in water spontaneously organize into bilayers;
these protein/phospholipid
membranes can fuse. Still, even if "taken up" by these "cells",
how do DNA/RNA take control? Still
unanswered by anything experimental.
Who is/are the Common Ancestor(s)
Direct fossil evidence of life
begins between 3.2 and 3.5 bya, and appears to be similar to
extant
cyanobacteria (photosynthetic); this is already too advanced to give us a view of the
early common
ancestor(s) (cenancestor). Fossils cant help us here.
Phylogenetic reconstruction, however, can help out we look for the synapomorphies
to assemble
the Tree of Life. However, morphological characteristics of the primitive
prokaryotes lacked enough
diversity to assemble the tree. DNA/RNA/ Protein sequencing
techniques give us much more character
diversity similar (but not identical sequences
why?) for the same gene. The more the differences, the
longer the lineages have been apart
(straightforward) a sort of "molecular clock". Of course, if you
want to do this for all life,
you need a gene that codes for the same, and an essential, functioning molecule
in ALL
living things the gene for small subunit ribosomal RNA is such a molecule.
The phylogeny intimated by this rRNA, which is counter to the five kingdom
classification of life, is
shown in Fig. 17.18, 17.21, and 17.23-24 (but see fig. 17.22). Prokaryotes have two VERY
distinctive
separate evolutionary lines, one including virtually all the commonly known types,
the other represented
by "extremists", living in various harsh conditions (Archaea). Interestingly, these
Archaea (formerly
Archaebacteria) are apparently more closely related to Eukaryotes than
the "typical" Bacteria. Eukarya
are relative newcomers, with less than 10% of the variation
seen in the rRNA small subunit gene.
Interestingly, in analyzing some genes, some Archaea actually have what appear to
be Bacterial
genes why? Because they ARE bacterial, picked up by the organism from
another. This can happen
with these prokaryotic forms (lateral gene transfer). As for the common ancestor, all evidence points
to a
rather sophisticated, evolved organism, or SET of organisms, not unlike modern bacteria, sometime
as early
as perhaps 4 to as recently as 2 bya. It may very well be that extant
life's history does NOT
originate with a single life form, but an interconnected set of roots to the
tree, a community of interacting
species readily swapping genes (which, needless to say, makes for an interesting
base to the phylogeny
-- see Fig. 17.26
(Read pages 673 675 for date of oldest
known eukaryotes and cyanobacteria [almost
identifiable
to extant forms, and apparently largely unchanged for 2 by])
Hypotheses for the evolution of the "Tree of Life" -- the descent from
the "common" ancestor
1. The Universal Gene-Exchange
Pool -- three ancestors of todays domains emerged from the
pool at
different times, with later emergence of Archaea and Eucarya making them appear
more
more closely
related.
2. The Ring of Life -- the
first eukaryote arose by the fusion of an archaen and bacterium. Less
support for
this hypothesis (though see discussion of mitochondria, below), as there are
significant
gaps in molecular development with this theory, and no cytoskeletal control in
either makes
it difficult to envision the necessary phagocytotic event
3. The Chronocyte -- an
independent organism that developed a cytoskeleton and phagocytotic
capabilities.
Eventually, a digestion-resistant archaen is eaten and becomes the "nucleus".
Several holes
in this theory as well, including lack of evidence for such a chronocyte.
4. The Three Viruses/Three
Domains -- viruses, with RNA gene for reverse transcriptase, in
turn
generates host DNA from host RNA. Host, with developed resistance, in turn
has more
stable DNA
than RNA, and DNA becomes THE molecule.
Origin of Organelles
Mitochondria, widespread but not universal in Eukarya, and chloroplasts, more
restricted in their
distribution, are therefore not defining characteristics of the Eukarya.
Where did they come from? Both
have their own DNA, and analysis puts chloroplasts
rRNA small subunit gene with the cyanobacteria,
and that for mitochondria within the
Bacteria as well. Lynn Margulis endosymbiosis theory is correct!!
Chapter 18: The Cambrian Explosion and Beyond
The Nature of the Fossil Record: Understand how organic
remains fossilize, and that occasionally
flesh can be preserved under very restricted conditions.
Understand, also, that, like any data set,
fossils present a biased look at the history of life,
for several reasons. Different organisms/organs
fossilize or don't (presenting a DISTINCT taxonomic bias in
the fossil record), different conditions
at time of fossilization and after fossil formation,
different access to fossils, etc. See * below.
KNOW the following:
Timeline pages 692 & 693:
Time (mya) for beginning and end:
Proterozoic Precambrian times
Phanerozoic eon:
Paleozoic with Cambrian, Ordovician, Silurian, Devonian, Carboniferous (M & P), Permian
Mesozoic with Triassic, Jurassic, Cretaceous
Cenozoic with Paleocene, Eocene, Oligocene, Miocene, Pliocene, Quaternary
Know Laurasia, Gondwana, Pangaea, India colliding with Asia, beginning and end of
rise of
Appalachians, Alps/Himalayas rise,
formation of landbridge between North and South America
Know coelomate/acoelomate, diploblast/triploblast, protostome/deuterostome
Know times for:
Animals
First shelled organisms
First chordates and first vertebrates
First tetrapods (amphibians), reptiles, mammals, birds, placental mammals
First hominids, appearance of Homo (sapiens)
First insects, and first winged insects
Plants
First land plants
First vascular plants (ferns),
first seed plants, first flowering plants
You should also understand connections, such as why land animals came after land plants, and
why insect diversification really took off after evolution of flowering plants
*Understand what we know comes largely from fossils, which have some inherent biases
(geographical [require some minimal sedimentation at least], taxonomic [organisms with hard
parts preserved better], and temporal [older fossils less numerous]).
Some famous fossil deposits:
Ediacaran Hills in south Australia
Burgess Shales in British Columbia
Chengjiang deposits in Yunnan province, China
Was Cambrian Explosion really Explosive?
Molecular clocks suggest derivation of some lineages older than fossils suggest (NOT a
surprise). Older fossil finds starting to confirm these older dates.
Even so, there DOES appear to be a very rapid evolution of morphological traits, not only
in complexity (meaning more complex developmental program) but size as well.
Increasing
oxygen levels, more ecological interactions, etc. may have driven this evolution, but still there
would have had to have been some significant genetic variability available to ALLOW for this
evolution.
Macroevolutionary patterns -- know the following:
Radiations (why, for instance, mammals radiated significantly after the K-T asteroid)
"Stasis" and "zigzag" evolution
Gradualism
Punctuated Equilibrium (stasis [in morphology] followed by rapid diversification).
Mass Extinctions: The "Big Five" especially the K-T asteroid
Background Extinction
Human driven Extinction (see middle
paragraph page 719)
________________________________
One last tidbit:
C values (page 576 and handout) -- total DNA per cell does NOT correlate with
organisms
perceived morphological complexity or phylogenetic position.