Production of bio-refractory fluorescent dissolved organic matter in the ocean interior (original) (raw)
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- Published: 17 August 2008
Nature Geoscience volume 1, pages 579–582 (2008)Cite this article
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Abstract
Dissolved organic matter in the ocean constitutes one of the largest pools of reduced carbon on the Earth’s surface1,2, but its role in the global carbon cycle is poorly understood. A large part of this pool is thought to be of marine origin2,3,4 and to be composed of constituents that are resistant to biological degradation3,4,5,6. It is not clear how this refractory fraction of the carbon pool is produced in the ocean. Here, we analyse observations of fluorescence intensity and apparent oxygen utilization in the interior of the Pacific Ocean, and find that the two parameters are linearly related in the mesopelagic and abyssal layers. We conclude that fluorescent dissolved organic matter is produced in situ in the ocean interior as organic matter is oxidized biologically, and that it is resistant to biological degradation on centennial to millennial timescales. The rate of production of bio-refractory fluorescent dissolved organic matter in the ocean interior is larger than the riverine input of terrestrial humic substances, suggesting that its in situ production is one of the key processes in maintaining the oceanic pool of refractory dissolved organic matter.
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Acknowledgements
We thank A. Tsukasaki for measurements of fluorescence intensity in samples obtained from the Southern Ocean and South Pacific; T. Nishida, N. Yamada, S. Tani and other participants and crews of cruises for assistance during observations; N. Handa and T. Suga for discussions; and R. Jaffé for reviewing the manuscript. This study was supported by Grants-in-Aid for Scientific Research (Nos 18651006, 20241005) from Japan Society for the Promotion of Science (JSPS).
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Author notes
- Youhei Yamashita
Present address: Present address: Southeast Environmental Research Center, and Department of Chemistry and Biochemistry, Florida International University, University Park, OE-148, Miami, Florida 33199, USA,
Authors and Affiliations
- Department of Earth and Environmental Sciences, Graduate School of Environmental Studies, Nagoya University, Furo-cho, Chikusa-ku, Nagoya 464-8601, Japan
Youhei Yamashita & Eiichiro Tanoue
Authors
- Youhei Yamashita
You can also search for this author inPubMed Google Scholar - Eiichiro Tanoue
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Contributions
Y.Y. and E.T. contributed to the project planning, data interpretation and preparation of the final draft of the manuscript. Y.Y. carried out most of the experiments and data analysis, and wrote the first draft of the manuscript.
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Correspondence toYouhei Yamashita.
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Yamashita, Y., Tanoue, E. Production of bio-refractory fluorescent dissolved organic matter in the ocean interior.Nature Geosci 1, 579–582 (2008). https://doi.org/10.1038/ngeo279
- Received: 14 May 2008
- Accepted: 16 July 2008
- Published: 17 August 2008
- Issue Date: September 2008
- DOI: https://doi.org/10.1038/ngeo279