Paleo-climate reconstruction on sediment core M72/5_628-1 (25-GC-1), Black Sea
The Marine Isotope Stage (MIS) 3 stands out due to its abrupt changes from cold and dry stadials to warm and humid interstadials, the so-called Dansgaard-Oeschger cycles that also affected temperature and rainfall in the Black Sea region. This study is based on a gravity core from the southeastern (...
Main Authors: | , , , , , |
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Format: | Other/Unknown Material |
Language: | English |
Published: |
PANGAEA
2016
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.871241 https://doi.org/10.1594/PANGAEA.871241 |