BIO102: Biology of the Organism - single or multicellular, in context with environment
II & III. Animal Biology... Diversity, Physiology, Reproduction & Development, Neurobiology
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Age of Earth |
4.5 billion years |
radioisotopic dating of meteorites formed during formation of solar system |
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Earliest Common Ancestor |
3.5-4 billion years |
formation of solid crust vs. observation of oldest fossils; carbon isotopes indicate 3.8by metebolic activity (Greenland) |
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Oldest Prokaryotic Fossils |
3.5 billion years |
possible cyanobacteria bacteria (autotrophic - photosynthetic). Western Austrailia stromatolites(Fig 26.1) |
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Oldest Eukaryotic Fossils |
2.1 billion years |
possible eukarytic algae, Michigan (Han & Runnegar, 1992, Science 257:232) |
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Multicellular Eukaryotes |
1-1.2 billion years |
projected from on DNA sequence analysis |
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Cambrian "Explosion" (Animals) |
500 million years |
Burgess Shale Fossils |
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Origins of Plants from green algae |
460 million years |
Fossil Record
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Vascular Plants |
400 million years |
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Gymnosperms |
360 million years |
"naked seeds", conifers, etc. |
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Angiosperms |
130 million years |
"contained seeds", flowering plants |
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Oldest Vertebrates |
500 million years |
jawless, fishlike, fig. 34-36 |
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Oldest Jawed Vertebrates |
500 million years |
Hox gene duplications |
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Oldest Bony Fishes |
425-450 million years |
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Oldest Amphibians |
365 million years |
fig. 34-36 |
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Oldest Reptiles |
300 million years |
fig. 34-36 |
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Oldest Birds |
150 million years |
fig. 34-36 |
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Oldest Mammals |
220 million years |
fig. 34-36 |
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Homo erectus |
1-2 million years |
fig. 34.30, 34.33 |
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Homo sapien |
100,000 years |
fig. 34.30, 34.33 |
1800s...James Hutton, Charles Lyell: geological chronology through studies of stratafication
2. Some of these variations are passed onto offspring.
....(Heritibility is based on variations being based on genetic differences.)
3. In every generation, more offspring are produced than can survive.
4. Survival and reproduction are not random.
....Individuals that survive and reproduce, or who reproduce the most, are those with the
most favorable variations. They are naturally selected.
....(Individuals have increased or decreased fitness)
If we have an organism (earliest common ancestor), evolution / natural selection is the mechanism that explains how organisms became increasingly complex and diverse.
Classification of organisms - should be based on evolutionary relationships.
Study relationships of ALL known organisms using DNA sequence analysis (Fig. 27.11)
|------- Bacteria (Prokaryotes)
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Earliest |
Common ------| |--- Archaea (extreme prokaryotes)
Ancestor | | (thermophyles, etc.)
|---|
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|--- Eucarya (Nucleus, organelles)
Microsporidia, Diplomonads,
Trichomonads, Flagellates,
Entamoebae, Slime molds,
Cilliates, Fungi,
Plants, Animals
Analysis is based on small subunit rRNAs. Support that the Earliest Common Ancestor of ALL extant organisms was "between" the Bacteria and the Archaea/Eucarya is based on using duplicated tRNA genes to root the tree. Arguement is that duplicate tRNA genes are present in all organisms, and therefore the duplications that gave rise to multiple tRNAs MUST have occured BEFORE the derivation of the Earliest Common Ancestor. Therefore, tRNA sequences can serve as a point of comparison of extant organisms with an organism that existed BEFORE the Earliest Common Ancestor.
THE MAJOR EVENTS:
1. Prokaryotic cell organization: membrane, DNA, protein synthesis, metabolic activities
2. Eukaryotic cell organization: nucleus, organelles (endosymbionts) -
Some words on Phylogenetic Trees...(p. 476-485)
These trees represent relationships based on the concept of "lineage by descent". Branches splitting from a common branch point are assumed to have a common ancestor represented by that branch point; the branches are thus (supposed to be) monophyletic. Phylogenetic trees are not necessarily true. They are constructed by choosing a character or several characters that are present in each of the branch tips (taxa) and can thus be compared; differences between character types are used to sort the taxa. There can be many assumptions made in choosing appropriate characters. For example, an untrue tree might be constructed if wings were used as a character and their presence or absence was then used to join birds and insects as closely related taxa. In the tree above, the characters used were nucleotides at corresponding positions within sequences of small subunit tRNA; each nucleotide position was a single character which could be either A G U or C. The phylogenetic trees can only represent time in two ways: (1) if there is some datable fossil record of when two taxa split, and (2) if you are using DNA data and are confident invoking "molecular clock".
Some words on Kingdoms... i.e. plant, animal, etc. (Fig. 26.10)
Kingdoms should be monophyletic. That is, a major lineage that derives from a single common ancestor. We will see, this is not so clearly applied anymore within the Eukaryotes. That is, there may be many Kingdoms within each of the above three domains, based on this criteria. Note that all the groups listed above under Eucarya are monophyletic, suggesting as many as 10 Kingdoms belonging to this Domain
1920s A.I. Oparin (Russia) and J.B.S. Haldane (Great Britain) independently postulated that the environmental conditions that originated in primitive earth favored chemical reactions that would synthesize organic compounds from inorganic compounds.
1. Nonbiological processes synthesized organic molecules such as nucleic and amino acids: organic building blocks or "pre-biotic soup"
2. Organic building blocks were assembled into polymers
3. Some combination of these biological polymers was able to self replicate
Once self-replication was "invented", then natural selection could act.
NOTE: O2 (molecular oxygen) did not appear until photosynthesis had evolved; plants produce O2 during photosynthesis. EARLY EARTH HAD A REDUCING ATMOSPHERE (NOT AN OXIDIZING ONE).
1. Formation of organic molecules. (See: Lazcano & Miller 1996, Cell 85:793.)
Additional experiments by Miller and others: diverse organic molecules, including amino acids, nucleotides, sugars
Presumption was that the early atmosphere contained water, methane, ammonia and hydrogen (No O2), with energy input from heat and UV radiation.
Concern: some current views suggest CO2 predominated over CH4. CO2 is much less reactive, much more difficult to generate organics using Miller's apparatus. Alternative suggestions are that meteors delivered organics. Early earth was heavily bombarded by meteors, and meteors have been shown to contain carbonaceous compounds. Difficulty is imagining stability during heat of entry.
Organic molecules / organisms may have been knocked out of another planet in our solar system, such as Mars or Jupiter's moon Europa, by meteor impact, and survived travel to earth. Possible fossils of Martian bacteria observed in Mars derived meteorite (McKay et al., 1996, Science 273:924).
Streptococus mitis (bacteria) survived 2.5 years on moon OUTSIDE unmanned Surveyor 3 probe on moon in foam insulation of a camera (shielded only by camera) (Mitchell & Ellis, 1972, In Analysis of Surveyor 3 Material and Photographs Returned by Apollo 12 (Washington DC: NASA), 239-248.
Spores from a source outside our solar system - would require sheielding. Might survive if shielded by film of carbonaceous material?