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...

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Bibliographic Details
Main Authors: Friedrich, Oliver, Erbacher, Jochen, Moriya, Kazuyoshi, Wilson, Paul A, Kuhnert, Henning
Format: Dataset
Language:English
Published: PANGAEA 2008
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.768341
https://doi.org/10.1594/PANGAEA.768341