Cambrian Explosion Flashcards

1
Q

Explosion in morphology (& trophic scaling), not genetics

A

Prokaryotes (bacteria/archaea)- most genetic and functional diversity, primary producers (make their own sugar) thrive

Eukaryotes are limited in genetic diversity, but their morphology is expansive

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2
Q

Trace fossils

A

Not organism itself, but a record of its activity
- Bilaterian animals from Ediacaran times- present by ~630 Ma
- Feeding traces- traces on sea floor demonstrate movement in search of food (likely dead organic matter)
- Long term C cycle- feeding traces reduces potential for organic matter burial, weakening organic matter sink

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3
Q

First carbonate shells at 549 Ma

A
  • Inorganic carbon
  • Ediacara- Cloudina, first biomineralized organism (~549 Ma)

Advantages of hard parts:
- Protection from predators- on land, protection from desiccation
- Anchoring (for immobile organisms)
- For predators, useful for attacking and feeding
- Shells create a holding tank for filter feeding
- Helps mobility (anchors for muscles)

Drawbacks of hard parts:
- Requires energy to create hard parts
- If anchored, limits mobility- less choice in face of environment change/predators
- For shelled organisms, slows down gas exchange (less oxygen diffusion in tight shell) and waste exchange

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4
Q

SSF

A

(Small shelly fossils)
Early Cambrian biomineralized fossils

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5
Q

Mass extinction at Proterozoic-Phanerozoic boundary?

A
  • Created ecospace for bilateral animals to fill in
  • Parallel to other mass extinction events
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6
Q

Carbon cycle upheaval around Proterozoic-Phanerozoic boundary

A

Changes in δ13C of surface earth system- large scale changes (as large as entire rest of the Phanerozoic)

Indicates changes/perturbations in carbon cycle
- Less OM burial, living biomass is killed and decomposes- C12 can go elsewhere on surface earth

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7
Q

Burgess Shale

A

Middle Cambrian (~505 Ma)

  • Contains soft-bodied fossils
  • Interpreted environment (where these animals were deposited)- base of a reef
  • Anomalocaris

Burgess shale is not unique- Ordovician lagerstatten (80-100 Ma after Burgess shale)
- Still showing strange forms- indicates these were successful for a long time

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