Hadean (4.5 to 3.96 bya). Earth accreted from bolides. Material differentiated into core, mantle, crust and atmosphere. Hostile conditions. Early crust formation (detrital zircon grains dating to 4.2 bya found in sedimentary rocks), but no rocks still exist in the geologic record.
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Earth accreted from bolides.
Material differentiated into core, mantle, crust and atmosphere.
Early crust formation (detrital zircon grains dating to 4.2 bya found in sedimentary rocks), but no rocks still exist in the geologic record.
Cratons form (continental accretion).
Early atmosphere (outgassing).
First organisms (3.3 to 3.5 bya)
Origin of life?
once there is a self-replicating molecule,
there is natural selection
Transition from Archaen type crustal evolution to current pattern of tectonic cycle.
Banded iron formations (red beds)
Prokaryototes (3.3 to 3.8 bya?)Photosynthesis (2.3 bya?)Eukaryotes (2.1 bya?) endosymbiosis sexual reproduction multicelled organismsEdiacaran faunaSnowball earth?Early invertebrates?Ozone
Emergence of shelley fauna
near shore (neritic)
deep water (pelagic)
Trophic levels - PREDATION!
Experimentation of body plans
Brachiopods - chitinous, inarticulated
Archaeocyathids (reef building)
(jawless fish - ostracoderms)
Conodonts (early chordata)
(ostracoderms, first land plants, first land animals)
Major reef building
tabulate and rugose coral
Ammonites (mollusca - cephalapoda)
Devonian mass extinction
reef and pelagic communities
(age of fishes, first jawed fish, first amphibians, first seed plants)
(first reptiles, first gymnosperms)
50% marine vertebrates
90% marine invertebrates
Widespread marine regression
Methyl hydrates ?
Ocean turnover ?
Flood basalts ?
Rudists (main reef builders)
epifaunal and infaunal
(all major vertebrate groups, angiosperms)
75% of marine organisms
including ammonites, rudists, marine reptiles)
Bolide impact (Chicxulub crater)
nuclear winter ?
Climatic boundary conditions