Lithium and osmium isotopes, and trace element ratios in bulk carbonates of different ODP Sites across the Middle Eocene Climatic Optimum
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| Main Authors: | , , , , |
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| Format: | Dataset Open Access |
| Language: | en |
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PANGAEA
2023
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| _version_ | 1867171377747853312 |
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| author | Krause, Alexander Sluijs, Appy Van der Ploeg, Robin Lenton, Timothy M Pogge von Strandmann, Philip A E |
| author_facet | Krause, Alexander Sluijs, Appy Van der Ploeg, Robin Lenton, Timothy M Pogge von Strandmann, Philip A E |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | The Middle Eocene Climatic Optimum (MECO) was a ~400,000-year-long global warming event which occurred ~40 million years ago and interrupted the Eocene's long-term cooling trend. We investigated silicate weathering dynamics during the MECO by measuring lithium isotope ratios and elemental ratios (Li/Ca, Al/Ca, Mn/Ca, Sr/Ca, Rb/Ca) from a suite of open-ocean carbonate-rich sediments. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_962646 |
| institution | PANGAEA |
| language | en |
| publishDate | 2023 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Lithium and osmium isotopes, and trace element ratios in bulk carbonates of different ODP Sites across the Middle Eocene Climatic Optimum Krause, Alexander Sluijs, Appy Van der Ploeg, Robin Lenton, Timothy M Pogge von Strandmann, Philip A E Clay formation; Climate changes; Congruent weathering; Lithium isotopes; MECO; Middle Eocene Climatic Optimum; Ocean Drilling Program; ODP; reverse weathering; Silicate weathering The Middle Eocene Climatic Optimum (MECO) was a ~400,000-year-long global warming event which occurred ~40 million years ago and interrupted the Eocene's long-term cooling trend. We investigated silicate weathering dynamics during the MECO by measuring lithium isotope ratios and elemental ratios (Li/Ca, Al/Ca, Mn/Ca, Sr/Ca, Rb/Ca) from a suite of open-ocean carbonate-rich sediments. |
| title | Lithium and osmium isotopes, and trace element ratios in bulk carbonates of different ODP Sites across the Middle Eocene Climatic Optimum |
| topic | Clay formation; Climate changes; Congruent weathering; Lithium isotopes; MECO; Middle Eocene Climatic Optimum; Ocean Drilling Program; ODP; reverse weathering; Silicate weathering |
| url | https://doi.org/10.1594/PANGAEA.962646 |