Barium concentrations and GDGT abundances across the PETM
Current climate change may induce positive carbon cycle feedbacks that amplify anthropogenic warming on time scales of centuries to millennia. Similar feedbacks might have been active during a phase of carbon cycle perturbation and global warming, termed the Paleocene-Eocene Thermal Maximum (PETM, 5...
Main Authors: | , , , , , , |
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Format: | Other/Unknown Material |
Language: | English |
Published: |
PANGAEA
2019
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.899283 https://doi.org/10.1594/PANGAEA.899283 |