Ch 4 - Fossils and Timescales Flashcards
Alfred Wegener
Proposed continental drift in 1915
Fossils and methods of formation
Animals trapped in sediments; compression (imprint), permineralisation (precipitation of mineral replaces the tissue), unaltered remains
Dating
Isotopes half life (1/2^n, n = # half lives); formed by nuclear reactions in magma core
Geological time periods
Paleozoic: Cambrian, Ordovician, Silurian, Devonian, Carboniferous, Permian; Mezozoic: Triassic, Jurassic, Cretaceous; Cenozoic: Tertiary, Quaternary
Cambrian
542 Mya; marine animals diversify
Odrovician
488 Mya; Echinoderms and invertebrate diversify, cephalopods; extinction at end of period (Gondwana over south pole)
Silurian
444 Mya; Jawed fish, early terrestrial plants and arthropods
Devonian
416 Mya; Bony fish diversify; amphibians, insects, ferns, seed plants originate; mass extinction near end
Carboniferous
359 Mya; small continents; plants increase, winged insects, amphibians diverse, first reptiles
Permian
299 Mya; Pangaea; glaciations; reptiles and mammal forms diversify; mass extinction (esp marine)
Triassic
251 Mya; separation of Pangaea starts; gymnosperms dominant, first dinos and mammals
Jurassic
200 Mya; separation continues; dinos; first birds; Mesozoic marine revolution
Cretaceous
145 Mya; most continents separated; mammals, birds diversify; mass extinctions of ammonoids and dinos
Tertiary
65.5 Mya; Cooling, drier climate; mammals, birds, insects radiate
Quaternary
1.8 Mya; Continents in modern places; glaciations and extinctions; Homo sapiens, agriculture, civilization