Eocene sedimentary calcium carbonate contents and stable isotope composition of benthic foraminifera
'Hyperthermals' are intervals of rapid, pronounced global warming known from six episodes within the Palaeocene and Eocene epochs (~65-34 million years (Myr) ago) (Zachos et al., 2005, doi:10.1126/science.1109004; 2008, doi:10.1038/nature06588; Roehl et al., 2007, doi:10.1029/2007GC001784;...
Main Authors: | , , , , , , , |
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Format: | Other/Unknown Material |
Language: | English |
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PANGAEA
2011
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.763158 https://doi.org/10.1594/PANGAEA.763158 |