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ways to determine ages
stratigraphy
relative dating
radiometric dating
stratigraphy
fossils in sedimentary rocks appear deeper in earth
relative dating
determine age of fossil based on position in stratigraphy
radiometric dating
age based on isotopic decay
forms into stable elements
half life
Abiogenesis hypothesis
living organisms arised from non living organic molecules
Archean eon
origin of life (prokaryotes)
anaerobic (glycolysis)
Proterozoic eon
first colonial cyanobacteria
first eukaryotes
invertebrates
bilateral symmetry
aerobic respiration
phanerozoic eon
3 eras: Paleozoic, Mesozoic, Cenozoic
Paleozoic era - Cambrian Period
Cambrian explosion: O2 ^ = new species (marine)
Paleozoic era - Ordovician Period
colonization of land by plants & animals
hard shelled marine
large glaciers = shallow oceans → mass extinction
Paleozoic era - Silurian Period
early vascular plants
more colonization of land by terrestrial plants & animals
seed plants
Paleozoic era - devonian period
gymnosperms emerged
insects
tetrapods
more extinctions of marine species
tetrapods
amphibians
gain of limbs
Paleozoic era - carboniferous period
flying insects emerged
more amphibians
larger plants/trees
amniotic egg
Paleozoic era - Permian period
Continental drift: Pangaea
more gymnosperms
reptiles dominant
mass extinction : 90-95% of marine/terrestrial
Mesozoic Era - Triassic Period
first dinosaurs
first mammals
Mesozoic era - Jurassic Period
dinosaurs and reptiles dominant
early birdlike animal
Mesozoic era - Cretaceous period
angiosperms emerged
mass extinction of dinosaurs and reptiles
Cenozoic era - tertiary period
mammals dominant
angiosperms dominant
hominoids (humans, chimps)
Cenozoic era - quaternary period
ice ages
extinction of large mammals
hominins diversified
homo sapiens