Basin-scale controls on the molybdenum-isotope composition of seawater during Oceanic Anoxic Event 2 (Late Cretaceous)
It is well established that the burial of organic carbon in marine sediments increased dramatically at a global scale at the Cenomanian-Turonian boundary (Oceanic Anoxic Event 2: OAE-2, ~94 Myr ago, Late Cretaceous). Many localities containing chemostratigraphic expressions of this event are not, ho...
| Main Authors: | , , , , |
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| Format: | Journal article |
| Published: |
Elsevier
2016
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