Basalt–seawater interaction, the Plenus Cold Event, enhanced weathering and geochemical change: Deconstructing OAE 2 (Cenomanian–Turonian, Late Cretaceous)
Oceanic Anoxic Event 2 (Cenomanian–Turonian: ca 94 Ma) represents a major palaeoceanographic phenomenon that took place during an interval of extreme global warmth when large amounts of organic matter entered the marine burial record, probably triggered by increased availability of nutrients for pla...
| Main Authors: | , , , |
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| Format: | Journal article |
| Published: |
Wiley
2016
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