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...
Main Authors: | , , , , , |
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Format: | Other/Unknown Material |
Language: | English |
Published: |
PANGAEA
2009
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.753191 https://doi.org/10.1594/PANGAEA.753191 |