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Ch 25: History of Life
“There is nothing permanent but change.” (Heraclitus) “Chaos always defeats order because it is better organized.” (Terry Pratchett)
Louis Pasteur: Disproving spontaneous generation
Universe forms ~13.8 bya Early solar system formation ~ 4.5 bya
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Earth’s 1st 1 billion years
Moon formed by a collision
Radiometric Dating
Half-lives 14C: 5,730y 40K: 1.25 by 238U: 4.5 by
Index fossils
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Arrhenius & Mojzsis Some of the oldest fossils ~3.4 bya (Strelley Pool, Australia) organic trace fossils http://physicsforme.files.wordpress.com/ ~3.8 bya 2011/08/astrobiology3.jpg
Abiogenesis: First step- compounds of life from non-living 1920s
AJ Oparin
JBS Haldane
Miller-Urey experiment (1952/publ 1953)
Stanley Miller Harold Urey 10–15% of the carbon now in the form of organic compounds 2% of the carbon had formed amino acids, with glycine the most abundant (all 20 common ones were found) (In 2008, his student J. Bada reexamined some of Fig 4.2 the vials.)
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proteinoid Protobionts microspheres
vesicles
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Sidney Altman
Thomas Cech Other possibilities for early genetic material: PNAs (Miller)
Which came first?
Where do the materials come from? Earth “panspermia”
molecules on space rocks
Note: moves some of the origin question off earth but still have the question…
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Where did life begin? One hypothesis - deep, hot water
Early microfossils: stromatolites
Shark Bay, Australia (present day)
early O2 production Banded Iron Formations
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O2 production -> ! Sun Ozone (O3) shield protects us from UV ! Ultravioletrays
3(O2)! ! Upperatmosphere
2(O3)! ! Loweratmosphere SBMFig. 20.06!
Eukaryotes formation of organelles -> multicellularity
endosymbiosis
Grypania spiralis (filaments)
Lokiarchaeota discovery 2015 http://phenomena.nationalgeographic.com/2015/05/06/new-loki-microbe-is-closest-relative-to- all-complex-life/
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How are organisms related?
old26.21
Current trees of life (largely based on rRNA)
26.21
Horizontal gene But may not be a transfer (26.23) straightforward tree
Ring of life? (old26.23)
Snowball Earth
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Tour: Proterozoic Era: 2.5 bya -> 542 mya Ediacaran fauna
Paleozoic Era Cambrian Period 542 -> 488.3 mya all current major animal phyla have appeared
Cambrian Period 542 -> 488.3 mya fossil animal embryos Burgess shale
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Ordovician Period 488.3 -> 443.7 mya first plants?
Silurian Period 443.7 -> 416 mya
Devonian Period 416 -> 359.2 mya “Age of Fishes”
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Carboniferous Period 359.2 -> 299 mya (large amounts of forest -> major coal deposits)
Permian Period 299 -> 251 mya
Mesozoic Era “Age of Reptiles” Triassic Period 251 -> 199.6 mya Jurassic Period 199.6-> 145.5 mya Cretaceous Period 145.5 -> 65.5 mya
Fig. 20.13!
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Cenozoic Era (Age of Mammals, Insects, Birds, Flowering Plants) Paleogene Period Paleocene Epoch 65.5 -> 55.8 mya Eocene Epoch 55.8 -> 33.9 mya Oligocene Epoch 33.9 -> 23 mya
Cenozoic Era Neogene Period Miocene Epoch 23 -> 5 mya Pliocene Epoch 5 mya -> 1.8 mya Pleistocene Epoch 1.8 mya -> 10,000 ya Holocene Epoch 10,000 ya -> present? Anthropocene?
Land changes: continental plates and plate tectonics
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“Recent” continental drift
Mass extinctions: 5 – 8 events (note: appear different at different taxonomic levels)
Q: Is one happening now?
Opportunities & changes
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Development changes can change bodies Timing changes allometric growth
Development changes can change bodies Timing changes paedomorphosis
axolotl
Development changes can change bodies Changes in genes
Number of Hox genes
How Hox genes are used
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Evolution does not work toward a snail “goal” limpets eg: mollusk eyes – all useful Nautilus
snail
squids & octopi
Tree of Life video clip with D. Attenborough
http://www.wellcometreeoflife.org/video/
Interactive http://www.wellcometreeoflife.org/interactive/
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