Isotopic evidence for changes in the zinc cycle during Oceanic Anoxic Event 2 (Late Cretaceous)
Widespread deposition of organic-rich shales during the Late Cretaceous Oceanic Anoxic Event 2 (OAE 2, ca. 94 Ma) occurred during a period of significant global paleo-environmental and geochemical change. It has been proposed that an increase in nutrient input to the ocean during OAE 2 was the key m...
| Hoofdauteurs: | , , , , , , |
|---|---|
| Formaat: | Journal article |
| Gepubliceerd in: |
Geological Society of America
2018
|