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The Ordovician Period
490 to 443 Million Years Ago
Established Theory:
Start: |
Conodont, lowest occurrence of Iapetognathus fluctivagus; just above base of Cordylodus lindstromi conodont Zone. Just below lowest occurrence of planktonic graptolites. |
Index Fossils: |
Trilobites, Graptolites |
Evolution: |
Diverse marine life, including vertebrates; vascular plants |
Geography: |
Similar to the preceding Cambrian period, irratic climate changes |
Rocks: |
Limestone and Shale |
Alternative Theory:
In Progress
Conclusions:
In Progress
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