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Earth’s climate through time
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dinosaurs
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mammoths
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Geologic Time Scale
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Late Precambrian ice age
Cambrian explosion
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Late Precambrian ice age
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Cambrian explosion
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Cambrian explosion
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Cambrian explosion
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Cambrian explosion
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Cambrian explosion
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Ordovician ice age
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Ordovician
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Permo-Carboniferous ice age
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Devonian/Carboniferous
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Phanerozoic CO2
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Permo-Carboniferous ice age
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Permian
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Mesozoic - Age of the Dinosaurs
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Triassic
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Jurassic
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Cretaceous
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Cretaceous
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Cretaceous
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Cenozoic cooling
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Cenozoic cooling
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Eocene
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Miocene
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• position & size of continents
Key factors Radiative forcing • solar variability Greenhouse forcing • carbon dioxide • water vapor Tectonic forcing • position & size of continents • mountain building • ocean circulation
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CO2 - temp
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Plio-Pleistocene onset of northern hemisphere glaciation
41,000 year world 100,000 year world
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Plio-Pleistocene
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Vostok CO2
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100 kyr cycle global equatorial New Zealand 45 S 78 S
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Dansgaard-Oeschger events
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Bermuda Rise SST
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Northern hemisphere ice sheets at the last glacial maximum (LGM)
global temperature was 6˚C lower sea level was 120 m lower
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glacial - interglacial cycles over the last 2 million years
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120 meters lower at the LGM (20,000 year ago)
sea level 120 meters lower at the LGM (20,000 year ago)
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ice age cycles
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mammoths
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dry valleys
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West Antarctica
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abrupt climate change
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Heinrich events
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Heinrich events
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