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Enhanced North Pacific deep-ocean stratification by stronger intermediate water formation during Heinrich Stadial 1
The deglacial history of CO(2) release from the deep North Pacific remains unresolved. This is due to conflicting indications about subarctic Pacific ventilation changes based on various marine proxies, especially for Heinrich Stadial 1 (HS-1) when a rapid atmospheric CO(2) rise occurs. Here, we use...
| Autores principales: | , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2019
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6368553/ https://www.ncbi.nlm.nih.gov/pubmed/30737377 http://dx.doi.org/10.1038/s41467-019-08606-2 |