U-Th dating of marine sediments from the Bahamas slope
In order to understand the driving forces for Pleistocene climate change more fully we need to compare the timing of climate events with their possible forcing. In contrast to the last interglacial (marine isotope stage (MIS) 5) the timing of the penultimate interglacial (MIS 7) is poorly constraine...
Main Authors: | , , |
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Format: | Other/Unknown Material |
Language: | English |
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PANGAEA
2002
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.710997 https://doi.org/10.1594/PANGAEA.710997 |