New Constraints on Global Geochemical Cycling During Oceanic Anoxic Event 2 (Late Cretaceous) From a 6‐Million‐year Long Molybdenum‐Isotope Record
Abstract Intervals of extreme warmth are predicted to drive a decrease in the oxygen content of the oceans. This prediction has been tested for the acme of short (<1 million years) episodes of significant marine anoxia in the Phanerozoic geological record known as Oceanic Anoxic Events (OAEs). Ho...
Main Authors: | , , , , , , , , |
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格式: | Article |
語言: | English |
出版: |
Wiley
2021-03-01
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叢編: | Geochemistry, Geophysics, Geosystems |
主題: | |
在線閱讀: | https://doi.org/10.1029/2020GC009246 |