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...

Volledige beschrijving

Bibliografische gegevens
Hoofdauteurs: Sweere, T, Dickson, A, Jenkyns, H, Porcelli, D, Elrick, M, van den Boorn, S, Henderson, G
Formaat: Journal article
Gepubliceerd in: Geological Society of America 2018