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1
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2
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- Early Cambrian- “Cambrian Explosion”
- Rising seas flooded continents, creating shallow seas, drowning
landmasses
- Late Cambrian- carbonate-secreting organisms flourish
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3
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- Late Proterozoic-
- By ~600 ma, Rodinia began breaking apart
- By Cambrian-
- New oceans basins formed
- Marine sediments were deposited across the newly rifted & subsiding
margins
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4
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- Were barren & devoid of all vegetation
- a barren landscape covered by blowing sand, silt & clay.
- Evidence: cross-stratification, extensive sorting, ripple marks
- Were low in relief
- Were characterized by raised areas (arches) and low areas (basins)
- Arch- broad, gentle warping of the crust
- Transcontinental Arch, North America-
- Single largest Cambrian craton feature in NA
- Extends from Lake Superior southwest towards AZ
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5
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- Dramatically thicken from craton interior towards the margins.
- Continents were periodically flooded creating shallow seas
- Sauk transgression-
- Cambrian cratonic sandstone
- one of the most mature in the world!
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6
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- North America was near the equator
- Had a warm climate
- Evidence- Cambrian oolites, shelly limestone & local evaporite
deposits
- Sauk sediments reveal consistent fair weather punctuated by violent,
hurricane-like storms
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7
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- An evolutionary burst that occurred in only 40 million years!!!
- Most of the major phyla began
- Includes annelids, arthropods, brachiopods, molluscs, vertebrates,
hemichordates, echinoderms and poriferans
- Not Bryozoa –not until early Ordivician
- All life was aquatic
- Most life was relatively small
- Many animals had unusual body layouts
- Many organisms are now extinct
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8
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- Brachiopods- (Phylum Inarticulata)
- Trilobites
- Archeocyathids
- Hyolithids
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9
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10
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- Some Cambrian organisms display unusual forms not comparable with
anything today
- Preserved in few locales worldwide
- Burgess Shale, British Columbia, Canada
- Utah, S. China, Greenland, Siberia
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11
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- Dawn Crinoid (Gogia spiralis), Middle Cambrian, Upper Wheeler Fm.,
Millard County, Utah
- Worm, Wheeler Fm.
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12
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