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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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Dades bibliogràfiques
Publicat a:Proc Natl Acad Sci U S A
Autors principals: Nishioka, Jun, Obata, Hajime, Ogawa, Hiroshi, Ono, Kazuya, Yamashita, Youhei, Lee, Keunjong, Takeda, Shigenobu, Yasuda, Ichiro
Format: Artigo
Idioma:Inglês
Publicat: National Academy of Sciences 2020
Matèries:
Accés en línia:https://ncbi.nlm.nih.gov/pmc/articles/PMC7293607/
https://ncbi.nlm.nih.gov/pubmed/32461367
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.2000658117
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