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Published byPhilip Maxwell Modified over 9 years ago
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Evolutionary History – part 2 Chapter 20
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History of Life Fossils: Any record of past life Hard body parts: shells, bones, teeth Traces or impressions: trails, footprints Mostly found in sedimentary rock Layers of sediments that have been compressed and hardened The Law of Superposition: older strata below, younger strata above However, strata may be disturbed by geological processes
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Dating fossils Relative dating – fossils found together are from the same time period Index fossils – used to identify deposits made at the same time in different places on Earth; fossils found with the index fossils are from the same time period
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Dating fossils… Absolute dating – to tell the actual age of a fossil Uses the decay of radioactive isotopes These breakdown to a stable element at a known rate Radiocarbon dating: C-14 is a rare isotope of C-12 and is present in all living things (and most fossils) It breaks down to N-14 5,730 year half-life (one half of the C-14 in an organism will be gone after that amount of time) We compare the ratio of C-14 to C-12 in the fossil and this ratio to a living organism to calculate the age of the fossil This is only good for fossils < 100,000 years old Older fossils can use different radioactive elements
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Other dating methods… Molecular clock Mutations in certain parts of the genome They occur at a fixed rate They are not tied to natural selection (which would cause the allele frequencies to change) The number of DNA base-pair differences tells how long two species have been evolving separately
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The geologic time scale Precambian Time Prokaryotes ~ 3.5 BYA Eukaryotes ~ 2.1 BYA (endosymbiotic theory) Multicellular protists ~ 1.4 BYA Paleozoic Era Cambrian explosion – lots of variation in ocean life ~ 500 MYA life on land Mesozoic Era Flowering plants, dinosaurs Cenozoic Era Mammals
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Mass extinctions Large-scale extinctions over a relatively short period of time The fossil record shows 5 Caused by either cataclysmic events (asteroid hitting Earth) or more gradual environmental change We are currently in another one but this one is human-caused.
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