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N. Adam Smith Postdoctoral Fellow National Evolutionary Synthesis Center. How do we Know ?. Measures of background radiation “cooling” and universal expansion rate agree that the Universe was formed ~13.7 Ga.
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N. Adam Smith Postdoctoral Fellow National Evolutionary Synthesis Center
How do we Know ? • Measures of background radiation “cooling” • and universal expansion rate agree that the • Universe was formed ~13.7 Ga. • Our solar system must be at least as old as the oldest thing in it and there are meteorites that have been dated to ~4.8 Ga. • The oldest known rocks on Earth are at least ~4.0 Ga. Radioactive d
Mars Rover Curiosity: landed 8/6/12
4.6 GaYears! (of Earth History)
Ammonites: go extinct 65 Ma along with non-avian dinosaurs
Geologic time intervals are recognized by characteristic faunas. • Paleozoic (old life): lack of dinosaurs, mammals, flowering plants….abundant horn corals, trilobites, etc… • Mesozoic (middle life): “Age of the Dinos” • Cenozoic (recent life): “Age of Mammals”
Major Evolutionary Events • Multicellular Life ~1 Gya (billion years ago) • Invasion of land by plants ~475 mya (million years ago) • Flowering plants ~130 mya • Demise of the dinos ~65mya (Chicxulub Crater) • Earliest “humans” ~5mya
Issues with Faunal Correlation • ~75% of all rocks on Earth do not contain fossils • Fossils only give relative age, not absolute dates • Solution = radiometric dating
How does all of this geology relate to Evolution? • In general, evolution happens at timescales • outside of human ability to observe • (not true for many viruses for example) • This often leads to doubt and frequently prompts questions about transitional forms or so-called “missing links”
Examples of “transitional forms” Archaeopteryx lithographica
Examples of “transitional forms” Proto-whales with legs
Examples of “transitional forms” Foraminifera (unicellular marine organisms)
Summary • The Universe and the Earth are very, very old. • Geologic time is divided based on major evolutionary and geologic events. • Fossils provide relative dates and isotopes provide absolute dates. • Evolution happens on long timescales in most cases, but there are numerous examples of evolutionary change in the fossil record.