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...

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Detalles Bibliográficos
Autores principales: Gong, X., Lembke-Jene, L., Lohmann, G., Knorr, G., Tiedemann, R., Zou, J. J., Shi, X. F.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Article
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

Internet

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

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