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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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| Udgivet i: | Proc Natl Acad Sci U S A |
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| Main Authors: | , , , , , , , |
| Format: | Artigo |
| Sprog: | Inglês |
| Udgivet: |
National Academy of Sciences
2020
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| Fag: | |
| Online adgang: | 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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