248-65 mya: evolution reptiles, “Age of the Reptiles”, ferns, mammals, ended with dinosaur extinction
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Paleozoic
544-248 mya: all animal phyla develop: “Cambrian explosion”, early land plants develop, ended: mass extinction
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early earth
began forming 4.6 bya: not suitable for life, very hot, little O2
cooled 3.8 bya: oceans formed
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Miller-Urey experiment
simulation of early earth’s conditions
organic compounds made by passing electrical current to stimulate lightning, through closed system: held gas mixture
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meteorite hypothesis
amino acids arrived on Earth through meteorite impact
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iron-sulfide bubbles hypothesis
biomolecules formed in compartments on ocean floor
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lipid membrane hypothesis
lipid spheres form around organic molecules: cell membrane
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RNA
1st genetic material, ribozymes: self replicate
DNA: needs enzymes to replicate
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cyanobacteria
oldest known fossils, prokaryotic cells, add O2 to \n atmosphere, deposited minerals
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endosymbiosis
relationship: 1 organism lives within body of another mitochondria/chloroplasts: developed: forming eukaryotes
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sexual reproduction evolution
increased diversity/variation: advantage, led evolution of multicellular life
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multicellularity
more complex organisms: 100 million yrs after sexual reproduction began: evolution occur quickly.
organisms more fit: better competitors
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pseudogenes
like vestigial structures: no longer function carried w/ DNA, change as passed through generations: figure evolutionary relationships, similarities: reflect common ancestor
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protein comparisons
similarities among cell types revealed by comparing proteins: molecular finger-printing, unique set of proteins found types, computers search databases look for homologous sequences