Stable oxygen isotope record and benthic foraminiferal abundances in Cretaceous sediments of Demerara Rise
During the mid-Cretaceous period, the global subsurface oceans were relatively warm, but the origins of the high temperatures are debated. One hypothesis suggests that high sea levels and the continental configuration allowed high-salinity waters in low-latitude epicontinental shelf seas to sink and...
Main Authors: | , , , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2008
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.768341 https://doi.org/10.1594/PANGAEA.768341 |