Oxygen isotope (δ¹⁸O) values of benthic ostracods from varved sediments from Mondsee (Austria) for the interval 7.7-8.7 ka BP
The so-called 8.2 ka event represents one of the most prominent cold climate anomalies during the Holocene warm period. Accordingly, several studies have addressed its trigger mechanisms, absolute dating and regional characteristics so far. However, knowledge about subsequent climate recovery is sti...
Main Authors: | , , , , , , , , , , , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2017
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.880316 https://doi.org/10.1594/PANGAEA.880316 |