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...

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Bibliographic Details
Main Authors: Thunell, Robert C, Poli, Maria-Serena, Rio, Domenico
Format: Dataset
Language:English
Published: PANGAEA 2002
Subjects:
AGE
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.758847
https://doi.org/10.1594/PANGAEA.758847