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Neodymium isotope evidence for glacial-interglacial variability of deepwater transit time in the Pacific Ocean
There is evidence for greater carbon storage in the glacial deep Pacific, but it is uncertain whether it was caused by changes in ventilation, circulation, and biological productivity. The spatial ε(Nd) evolution in the deep Pacific provides information on the deepwater transit time. Seven new foram...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group UK
2018
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6226442/ https://www.ncbi.nlm.nih.gov/pubmed/30413704 http://dx.doi.org/10.1038/s41467-018-07079-z |