Black shale deposition during Toarcian super-greenhouse driven by sea level
One of the most elusive aspects of the Toarcian oceanic anoxic event (T-OAE) is the paradox between carbon isotopes that indicate intense global primary productivity and organic carbon burial at a global scale, and the delayed expression of anoxia in Europe. During the earliest Toarcian, no black sh...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2013-12-01
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| Series: | Climate of the Past |
| Online Access: | http://www.clim-past.net/9/2703/2013/cp-9-2703-2013.pdf |