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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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| Publicado no: | Proc Natl Acad Sci U S A |
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| Main Authors: | , , , , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
National Academy of Sciences
2020
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| Assuntos: | |
| Acesso em linha: | 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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