Stable oxygen and carbon isotope data for planktic and benthic foraminifera from southern Atlantic of DSDP Hole 74-525A and ODP Hole 113-690C

Published stable isotope records in marine carbonate are characterized by a positive d18O excursion associated with a negative d13C shift during the early Maastrichtian. However, the cause and even the precise timing of these excursions remain uncertain. We have generated high-resolution foraminifer...

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Bibliographic Details
Main Authors: Friedrich, Oliver, Herrle, Jens O, Wilson, Paul A, Cooper, Matthew J, Erbacher, Jochen, Hemleben, Christoph
Format: Other/Unknown Material
Language:English
Published: PANGAEA 2009
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.753191
https://doi.org/10.1594/PANGAEA.753191