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3. The second extinction pulse can be related to the release of thermogenic gases
from contact aureoles surrounding intrusions comagmatic with the main
sequence of tholeiitic basalts.
Acknowledgements
This study was partially supported by Agence Nationale de la Recherche, France,
Chair of Excellence grant (ANR-09-CEXC-003
01), Russian Foundation of Basic
Research grant (12-05-01154- а ) and Earth Sciences Department of Russian Acad-
emy grants to A.V.S and the U.S. National Science Foundation Continental
Dynamics Program grant 807585 to NTA. We are grateful to Y. R. Vasilev for
providing samples of Ayan River and Delkan section picrites and Stephen Self and
Kirsten Fristad for constructive reviews.
-
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