89. What do the combination of Mg/Ca, clumped (∆47) and conventional (18O) stable isotope in planktonic foraminifera tell us about the mid-Pleistocene transition?
| Title: | 89. What do the combination of Mg/Ca, clumped (∆47) and conventional (18O) stable isotope in planktonic foraminifera tell us about the mid-Pleistocene transition? |
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| Authors: | Peral, Marion; Caley, Thibaut; Malaizé, Bruno; Blamart, Dominique; Massinot, Franck; Daëron, Mathieu |
| Publisher Information: | Zenodo |
| Publication Year: | 2022 |
| Collection: | Zenodo |
| Description: | Poster presentation |
| Document Type: | text |
| Language: | unknown |
| Relation: | https://zenodo.org/communities/ges12/; https://zenodo.org/records/6832870; oai:zenodo.org:6832870; https://doi.org/10.5281/zenodo.6832870 |
| DOI: | 10.5281/zenodo.6832870 |
| Availability: | https://doi.org/10.5281/zenodo.6832870; https://zenodo.org/records/6832870 |
| Rights: | Creative Commons Attribution 4.0 International ; cc-by-4.0 ; https://creativecommons.org/licenses/by/4.0/legalcode |
| Accession Number: | edsbas.53CCC266 |
| Database: | BASE |