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Penultimate deglacial warming across the Mediterranean Sea revealed by clumped isotopes in foraminifera
The variability of seawater temperature through time is a critical measure of climate change, yet its reconstruction remains problematic in many regions. Mg/Ca and oxygen isotope (δ(18)O(C)) measurements in foraminiferal carbonate shells can be combined to reconstruct seawater temperature and δ(18)O...
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| Veröffentlicht in: | Sci Rep |
|---|---|
| Hauptverfasser: | , , , , , , , |
| Format: | Artigo |
| Sprache: | Inglês |
| Veröffentlicht: |
Nature Publishing Group UK
2017
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| Schlagworte: | |
| Online Zugang: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5707372/ https://ncbi.nlm.nih.gov/pubmed/29185446 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-017-16528-6 |
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