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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Detalles Bibliográficos
Autores principales: Rodríguez-Sanz, L., Bernasconi, S. M., Marino, G., Heslop, D., Müller, I. A., Fernandez, A., Grant, K. M., Rohling, E. J.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2017
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5707372/
https://www.ncbi.nlm.nih.gov/pubmed/29185446
http://dx.doi.org/10.1038/s41598-017-16528-6

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5707372/
https://www.ncbi.nlm.nih.gov/pubmed/29185446
http://dx.doi.org/10.1038/s41598-017-16528-6

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