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The Triassic Period
248 to 206 Million Years Ago
Established Theory:
Start: |
Conodont, lowest occurrence of Hindeodus parvus; termination of major negative carbon-isotope excursion. About 1 myr after peak of Late Permian extinctions. |
Index Fossils: |
Ammonites, Graptolites and Pelecypod |
Evolution: |
Early dinosaurs, crocodiles, turtles; first mammals |
Geography: |
Supercontinent Pangea, Formation of mountain ranges, erosion of mountains, semiarid to arid |
Rocks: |
Sandstone, shale, salt and gypsum |
Alternative Theory:
In Progress
Conclusions:
In Progress
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