Stable carbon isotope ratios of Cibicidoides wuellerstorfi of MIS 2 time slices
The interval of time represented by marine isotope stages 11 and 12 (~360–470 ka) contains what may be the most extreme glacial and interglacial climate conditions of the Late Pleistocene. It has been suggested that sea level rose by ~160 m at the termination of glacial stage 12. This is 30% greater...
Main Authors: | , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2002
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.758847 https://doi.org/10.1594/PANGAEA.758847 |