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Iron colloids dominate sedimentary supply to the ocean interior
Dissolution of marine sediment is a key source of dissolved iron (Fe) that regulates the ocean carbon cycle. Currently, our prevailing understanding, encapsulated in ocean models, focuses on low-oxygen reductive supply mechanisms and neglects the emerging evidence from iron isotopes in seawater and...
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| Τόπος έκδοσης: | Proc Natl Acad Sci U S A |
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| Κύριοι συγγραφείς: | , , , , , , |
| Μορφή: | Artigo |
| Γλώσσα: | Inglês |
| Έκδοση: |
National Academy of Sciences
2021
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| Θέματα: | |
| Διαθέσιμο Online: | https://ncbi.nlm.nih.gov/pmc/articles/PMC8020654/ https://ncbi.nlm.nih.gov/pubmed/33771922 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.2016078118 |
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