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Permian Extinction Tied to Wilson Supercontinent Cycle Through Pangea Integration
Source info:
| Author: | Will Baird |
|---|---|
| Date: | 2013-11-05 18:00:00 |
| Blog: | The Dragon’s Tales  |
| URL: | http://thedragonstales.blogspot.com/2013/11/permian-extinction-tied-to-wilson.html |
Summary:
Mass extinction and Pangea integration during the Paleozoic-Mesozoic transition Authors: YIN HongFu and SONG HaiJun Abstract: The greatest Phanerozoic mass extinction happened at the end-Permian to earliest Triassic. About 95% species, 82% genera, and more than half families became extinct, constituting the sole macro-mass extinction in geological history. This event not only causedContent analysis:
Stratigraphic context:
| Recognized stratigraphic terms [n]: | Phanerozoic [1] Mesozoic [1] Triassic [1] Paleozoic [1] Permian [2] |
|---|---|
| Agenames chronostratigraphy [rating]: | Phanerozoic [0.82] Mesozoic [0.5] Paleozoic [0.61] Triassic [0.1] Permian [0.33] |
Keywords:
earliest Triassic, geological history, geology, half families, Integration Mass extinction, mass extinction, Paleozoic-Mesozoic transition, pangea integration, Permian Extinction Tied, Permian Triassic Mass Extinction, Phanerozoic mass extinction, sole macro-mass extinction, SONG HaiJun, Wilson Supercontinent Cycle, YIN HongFu
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