Planktonic foraminifera and sea surface temperature reconstruction of sediments from the Mediterranean Sea
Water exchange between the Black Sea and the Mediterranean Sea has been a major focus of the paleohydrography of the eastern Mediterranean. Glacial melt water released from the Black Sea is a potential factor in the formation of sapropel S1, an organic-rich sediment layer that accumulated during the...
Main Authors: | , , , , , |
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Format: | Other/Unknown Material |
Language: | English |
Published: |
PANGAEA
2003
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.736518 https://doi.org/10.1594/PANGAEA.736518 |