(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...
Main Authors: | , , |
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Format: | Dataset |
Language: | English |
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PANGAEA
2002
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.844873 https://doi.org/10.1594/PANGAEA.844873 |