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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...

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שמור ב:
מידע ביבליוגרפי
הוצא לאור ב:Sci Adv
Main Authors: Arakawa, Neal, Aluwihare, Lihini I., Simpson, Andre J., Soong, Ronald, Stephens, Brandon M., Lane-Coplen, Daniel
פורמט: Artigo
שפה:Inglês
יצא לאור: American Association for the Advancement of Science 2017
נושאים:
גישה מקוונת: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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