Contrasting geochemical signatures on land from the Middle and Late Permian extinction events
The end of the Palaeozoic is marked by two mass-extinction events during the Middle Permian (Capitanian) and the Late Permian (Changhsingian). Given similarities between the two events in geochemical signatures, such as large magnitude negative C-13 anomalies, sedimentological signatures such as cla...
Main Authors: | , , , |
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Format: | Article in Journal/Newspaper |
Language: | unknown |
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WILEY-BLACKWELL
2014
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Online Access: | http://eprints.iisc.ernet.in/50227/ http://dx.doi.org/ 10.1111/sed.12117 |