Geochemistry and stable isotope record of benthic foraminifera of Miocene sediments
The processes causing the middle Miocene global cooling, which marked the Earth's final transition into an 'icehouse' climate about 13.9 million years ago (Myr ago) (Flower and Kennett, 1993, doi:10.1029/93PA02196; 1995 doi:10.1029/95PA02022; Miller et al., 1991, doi:10.1029/90JB0201;...
Main Authors: | , , , |
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Format: | Other/Unknown Material |
Language: | English |
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PANGAEA
2005
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.738246 https://doi.org/10.1594/PANGAEA.738246 |