New constraints on global geochemical cycling during oceanic anoxic event 2 (Late Cretaceous) from a 6-million-year long molybdenum-isotope record
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). However, th...
| Main Authors: | , , , , , , , , |
|---|---|
| Format: | Journal article |
| Language: | English |
| Published: |
American Geophysical Union
2021
|