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Carotenoids are the likely precursor of a significant fraction of marine dissolved organic matter
The ocean’s biota sequester atmospheric carbon dioxide (CO(2)) in part by producing dissolved organic matter (DOM) that persists in the ocean for millennia. This long-term accumulation of carbon may be facilitated by abiotic and biotic production of chemical structures that resist degradation, conse...
Uloženo v:
| Vydáno v: | Sci Adv |
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| Hlavní autoři: | , , , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
American Association for the Advancement of Science
2017
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5617377/ https://ncbi.nlm.nih.gov/pubmed/28959723 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1126/sciadv.1602976 |
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