(Table 3) Stable isotope record of Cretaceous foraminifera from DSDP Hole 44-392A

Mid-Cretaceous (Barremian-Turonian) plankton preserved in deep-sea marl, organic-rich shale, and pelagic carbonate hold an important record of how the marine biosphere responded to short- and long-term changes in the ocean-climate system. Oceanic anoxic events (OAEs) were short-lived episodes of org...

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Bibliographic Details
Main Authors: Leckie, R Mark, Bralower, Timothy J, Cashman, Katharine V
Format: Dataset
Language:English
Published: PANGAEA 2002
Subjects:
AGE
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.844873
https://doi.org/10.1594/PANGAEA.844873