Oxic facies and the Late Devonian mass extinction, Canning Basin, Australia
The close association of anoxic or dysoxic sedimentary rocks and the major Late Devonian (Frasnian–Famennian) mass extinction has focused considerable attention on anoxia as the major cause or as a major factor in a multicausal scenario. The record of the Late Devonian biotic crisis in the well-know...
| Main Authors: | , , |
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| Format: | Journal Article |
| Published: |
Geological Society of America
2014
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| Online Access: | http://hdl.handle.net/20.500.11937/25315 |