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Synchronous deglacial thermocline and deep-water ventilation in the eastern equatorial Pacific
The deep ocean is most likely the primary source of the radiocarbon-depleted CO(2) released to the atmosphere during the last deglaciation. While there are well-documented millennial scale Δ(14)C changes during the most recent deglaciation, most marine records lack the resolution needed to identify...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group
2017
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5264251/ https://www.ncbi.nlm.nih.gov/pubmed/28112161 http://dx.doi.org/10.1038/ncomms14203 |