Sedimentology and Paleontology Lecture 10: The Cambrian Explosion Flashcards

1
Q

Describe the Cambrian explosion

A

The sudden apperance of Large and complex animals with mineralised skeletons

Rapid increase in taxonomic
diversity and abundance

Suggested that marine
ecosystem complexity in
the Cambrian was as
high as the present day

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2
Q

When was the Cambrian explosion

A

Between 540 - 520 million years ago

At the beginning of the Cambrian, in the Terreneuvian series/epoch.

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3
Q

How was the Cambrian dated?

A

Base of the Cambrian dated
by the first appearance of
Treptichnus pedum

  • A trace fossil – horizontal
    burrow with horizontal to
    vertical branches
  • Type section at Fortune
    Head in Newfoundland,
    Canada
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4
Q

What is the Burgess shale
And what is

A

Sites of exceptional preservation = Konservat Lagerstätten

The Burgess Shale is most famous example of this.

Burgess shale is dated to middle cambrian (508 Ma years)

Discovered in 1909 by Charles Doolittle Walcott

Primarily arthropods and sponges
(Porifera)

Dominated by epibenthic vagile
deposit feeders and sessile
suspension feeders

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5
Q

Describe the Doushanto formation

A

Doushantuo Fm, Guizhou Province, China
Doushanto formation is before the cambrian explosion.

635 - 551 Ma years

Phosphatic microfossils from middle unit (~570 Ma)
* Older than Ediacaran macrofossils

Vernanimalcula (micro-fossil found in the doushanto), Suggested to be the oldest
bilaterian (animals with
bilateral symmetry)

Interpreted to have different
layers, mouth, gut, anus,
and paired sensory pits

Weng’an Biota
(609-570 Ma)
* Algae and acritarchs
* Unlikely that embryolike fossils are sulphur bacteria, animals or
bilaterians

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6
Q

Describe the Ediacaran biota

A

Also before Cambrian explosion
(610-542 Ma)

First complex multicellular
macrofossils
* Worldwide distribution (Canada,
UK, Australia, Namibia, Russia)

Mistaken Point, Canada
* Type section for the PreCambrian-Cambrian
boundary
* Rangeomorphs (fractal
organisms that look like
sea-pens)
* Non-mobile animals that
lived on the seafloor

Similar deposits to Mistaken Point
* Rangeomorphs
* Discovered in 1957 and
identified as similar to
fossils from Australia and
Namibia – older than Cambrian age

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7
Q

Describe the Chengjiang biota

A

After cambrian explosion, before Burgess shale - (~518 Ma, Early Cambrian)

Oldest known assemblage of diverse metazoans. Soft-tissue preservation like Burgess Shale. 100 species in 11 phyla

Primarily arthropods but with
some assemblages with mostly priapulids or brachiopods

  • Dominated by epifaunal mobile
    hunters/scavengers, sessile
    suspension feeders, and
    infaunal mobile hunters/
    scavengers
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8
Q

Define SCF and SSF

A

Small shelly fossils (SSFs) - from the latest Ediacaran to
the end of the Early Cambrian

Small carbonaceous fossils (SCFs) – more continuous
record

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9
Q

Describe SSF’s

A

Small shelly fossils (SSFs) – mmsized biomineralized fossils

  • Latest Ediacaran to end of the Early Cambrian
  • Not a biological clade – whole or
    fragments/distarticulated remains
  • Biomineralization due to increase in
    calcium in the oceans or an
    evolutionary arms race
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10
Q

Describe SCF’s

A

Small carbonaceous
fossils (SCFs)

  • Fragile sub-mm remains
    of organisms
  • Scales, sclerites, and
    feeding appendages
  • Cryptic record of
    Cambrian biodiversity
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11
Q

Define a trace fossil and a body fossil

A

Trace fossils are evidence of the activities of organisms

Body fossils are bodily remains of organisms themselves.

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12
Q

What is the Agronomic revolution and its significance for the trace fossil record?

A

Agronomic revolution = change from a PreCambrian matground to Cambrian mixed ground seafloor.

  • Evolution of the ability for
    animals to move more
    and burrow vertically
    within the sediment

Therefore allowing significantly more trace fossils to be found in the sediment.

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13
Q

Define an ecosystem engineer

A

Ecosystem engineers =
modifying the environment
in ways that affect other
organisms

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14
Q

Describe the entire timing/timeline of the Cambrian explosion and relating biota’s/formations

A

Doushantuo Fm (635-551 Ma)
Ediacaran Biota (610-542 Ma)
SSFs (~550-520 Ma)
Cambrian explosion (Terreneuvian epoch)
First increase in trace fossils (Fortunian)
Chengjiang Biota (~518 Ma)
Burgess shale (508 Ma years)`

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15
Q

What are the supposed causes of the Cambrian explosion?

A

Unlikely to have been a single cause

Environmental triggers
* Availability of oxygen
* End of ‘Snowball Earth’

Genetic triggers
* Advent of ‘toolkits’ of developmental genes

Ecological triggers
* Co-evolutionary arms races
* Ecosystem engineering

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