Atmospheric d13CO2 and d13C in planktonic foraminifera during the last 150 kyr partly reconciled by the carbonate ion effect on isotopic fractionation during calcite formation
The d13C from CO2 (d13CO2) in ice cores covering the last 150 kyr contains, besides other variabilities, a 0.4permil trend between the Penultimate and the Last Glacial Maximum (PGM and LGM) and a wide and deep minimum around 60 kyr BP, both of which are still not understood. Here we use BICYCLE-SE,...
| Main Authors: | , |
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| Format: | Conference Object |
| Language: | unknown |
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2022
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| Subjects: | |
| Online Access: | https://epic.awi.de/id/eprint/57402/ https://hdl.handle.net/10013/epic.12cea345-be68-4c1f-86c1-fdae5fdd1263 |