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;...

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Bibliographic Details
Main Authors: Holbourn, Ann E, Kuhnt, Wolfgang, Schulz, Michael, Erlenkeuser, Helmut
Format: Other/Unknown Material
Language:English
Published: PANGAEA 2005
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.738246
https://doi.org/10.1594/PANGAEA.738246