Subpolar marginal seas fuel the North Pacific through the intermediate water at the termination of the global ocean circulation

The mechanism by which nutrients in the deep ocean are uplifted to maintain nutrient-rich surface waters in the subarctic Pacific has not been properly described. The iron (Fe) supply processes that control biological production in the nutrient-rich waters are also still under debate. Here, we repor...

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Detalles Bibliográficos
Autores principales: Nishioka, Jun, Obata, Hajime, Ogawa, Hiroshi, Ono, Kazuya, Yamashita, Youhei, Lee, Keunjong, Takeda, Shigenobu, Yasuda, Ichiro
Formato: Online Artículo Texto
Lenguaje:English
Publicado: National Academy of Sciences 2020
Materias:
Physical Sciences
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7293607/
https://www.ncbi.nlm.nih.gov/pubmed/32461367
http://dx.doi.org/10.1073/pnas.2000658117

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7293607/
https://www.ncbi.nlm.nih.gov/pubmed/32461367
http://dx.doi.org/10.1073/pnas.2000658117

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