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...

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Main Authors: Sweere, T, Dickson, A, Jenkyns, H, Porcelli, D, Elrick, M, van den Boorn, S, Henderson, G
格式: Journal article
出版: Geological Society of America 2018