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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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| Udgivet i: | Sci Adv |
|---|---|
| Main Authors: | , , , , , |
| Format: | Artigo |
| Sprog: | Inglês |
| Udgivet: |
American Association for the Advancement of Science
2017
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| Fag: | |
| Online adgang: | 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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