Geology 143: History of Life

Lecture 9 Notes

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Late Neoproterozoic (Early Proterozoic ~ 1 ­ 0.5 BYA)

The beginnings of modern life took place in the late Neoproterozoic

Explosive animal evolution in the last 30 MYA of the Neoproterozoic
trace fossils
imprints of soft bodied animals ­ most related to jellyfish (Phylum Cnidaria) Ediacaran Fauna but also included annelid worms and arthropods (crabs, lobsters, insects)
skeletal fossils ­ calcium carbonate vase- and tube-shaped skeletons

The Cambrian Explosion (0.5 BYA)

Early Paleozoic life fossil record is all from marine deposits, but it is assumed that protests and fungi inhabited freshwater terrestrial environments by this time

First time that modern fauna occurred

Early Cambrian ­ tube or vase-shaped, or teeth (Fig. 13.1)

Tommotian Fauna ­ (Fig. 13.2) lasted 3 or 4 million years,
Small animals including the first sponges and first mollusks with skeletons were composed of calcium carbonate and calcium phosphate

skeletons support tissue and permit locomotion

Large Animals with Skeletons ­ last few million years of the Late Cambrian, larger animals that belong to phyla that have lived into the modern

Large predators may have lead to the demise of the Ediacara fauna
Anomalocarids ­ large predatory arthropods (Fig. 13.6)

Trilobites ­ (Fig. 13.3) arthropods with segmented skeletons that survived to the end of the Paleozoic, most were benthic epifauna, but some were planktonic

Mollusks - monoplacophorans

Brachiopods ­ (Fig. 13.5)

Eocrinoids ­ (Fig. 13.7)

Stromatolites ­ much less abundant in the Cambrian than in the Proterozoic, probably due animal grazing

Reefs ­ early mounds formed by archeocyathids (sponge-like suspension feeders; Fig. 13.8)

Middle and Late Cambrian ­ spanned ~ 15 MYA

Marked by expansion of several pre-existing groups, especially the trilobites, echinoderms and brachiopods

Conodonts ­ (Fig. 13.00) earliest vertebrates with abundant teeth

Fish evolved at this time ­ fossil record of tiny bone plates (13.10)

Burgess Shale Fauna ­ (Fig. 13.11) spectacular fauna of soft-bodied animals, best preserved in the Rocky Mountains of British Columbia


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