Evolution Biol 4802 - Lecture 7
Topics for today
History of life on earth
- Archaean
- Proterozoic
- Paleozoic
Cambrian explosion
EvoBeaker: HIV
Why is there little evidence of early life?
- Earth
still volatile
- Erosion,
volcanoes, plate tectonics obliterated evidence
- Ongoing
bombardment by meteors
- Complex
aggregations of molecules that left no fossil record
Early organisms left chemical traces
- 13C:12C
ratio in atmosphere is ~1:99
- Living
organisms prefer 12C because its more reactive
- Graphite
deposits in 3.7 byo Greenland rock have
isotopic signature of life
Experimental conditions of early earth produced basic
building blocks of life
- Purines,
pyrimidines, and amino acids
Other experiments have synthesized
- Artificial
cells
- Artificial
cell membranes
- Chemical
reactions that could have built cellular material from nonliving sources
The chicken or the egg? Protein or DNA?
- Proteins
can do all kinds of complicated tasks except replicate themselves
- DNA
can storing and transmitting genetic information but cannot do any
biological work
- 1980s
small enzymes made of RNA, ribozymes, were discovered that could
break nucleic acid bonds
RNA can do it all! (Its not just the poor cousin of DNA!)
RNA world hypothesis
Ribosomes
mRNA
- short sequence of RNA
- Timeline from Big Bang to DNA based life
For >1/2 of lifes history only prokaryotes were
present
- Concept
single ancestor too simple
Deep roots of the tree are difficult to discern
- Different
genes tell a different story of relationship
- Early
prokaryotes swapped genes (horizontal gene transfer)
Prokaryotes continue to swap genes today
- Pathogenic - 1,387 different genes
- Benign - 528 different genes
Early life
- 3.5 byo stromatolite fossils have same
structure as those formed today by cyanobacteria
ARCHEAN
Origin
of life
Diversification
of bacteria
Increased
oxygen in atmosphere
Aerobic
respiration
PROTEROZOIC
Earliest
Eukaryotes
Origin
of Eukaryotic kingdoms
Multicellularity
Origin of the Eukaryotes
Advantages of endosymbiosis:
- Mitochonridia
provided aerobic metabolism
- Choloroplasts
provided autotrophy
Establishment of Eukaryotic Kingdoms
PALEOZOIC
Cambrian explosion
First large morphologically complex animals
Prior to the invasion of land
10-25 my period (geological blink of an eye)
Almost all modern phyla and classes of marine animals
and many now-extinct lineages appear
How do we know about the Cambrian explosion?
- 505
mya an enormous mud slide off the coast of Canada smothered teeming
marine life below
- Successive
mudslides created Burgess Shale
- Uplifted
2 miles into the Canadian Rockies
- Discovered
in 1909 but not understood until 1970s
Fossils of the Burgess Shale
- Fundamental
body plans
- Some
internal organs are preserved
Present during the Cambrian
- Earlier
fossils in Chengjiang,
China
- Later
fossils in Burgess shale, British Columbia,
Canada
Causes?
- Higher
oxygen concentration allowed
·
Higher metabolic rates
·
Larger size possible
·
Made tissue development possible
·
Efficient metabolism powered movement
How could we tell whether it was really explosive or just
had a long fuse?
- Molecular
clock
- Estimated
rate of hemoglobin evolution among vertebrate groups with known fossil
ages
- Compared
hemoglobin of vertebrates and invertebrates and back calculated the time
when they must have diverged
- Earliest
branching occurred 1000 my prior to fossil record evidence
- Progenitors
probably small and/or lacked skeletons
Evolution Biol 4802 - Lecture 7
Topics for today
History of life on
earth
- Archaean
- Proterozoic
- Paleozoic Cambrian explosion
EvoBeaker: HIV
The problem
- Recognized
1981
- Infected 60
million people
- Virtually
100% fatal
- 2020 AIDs
will kill 90 million
- 5% of all
deaths worldwide
- 70 % in
Sub-Saharan Africa
- Thought to be
most infectious disease to affect humankind
AIDs epidemic
- Infection
rates 15-45yr
- 2/3 in
sub-Sarahan Africa
- % adults
infected
·
39 Botswana
·
34 Zimbabwe
·
33 Swaziland
·
31 Lesothos
- Reduced life
expectancy from 62 to 47 years
- 90 % in poor
countries of Southern hemisphere
- Rapid
increase
What is HIV?
- Intracellular parasite
- Enters host through body fluids
- Parasitizes cells of human immune system
macrophages and T cells
- Simple structure
- Co-opts cells machinery for replication
How does your body react?
- Body
kills virions in blood stream and infected cells
- T
cells and macrophages essential for immune response
- Eventually
HIV depletes infected helper CD4 T cells and immune system collapses
- Opportunistic
infections by bacteria and fungus that do not normally cause disease
With-host evolution
- 9
patients taking AZT
- Viral
DNA sampled overtime
- What
should the phylogeny look like?
- Continual
immune drive selection
- Selective
replacement of strains overtime