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Efficient removal of recalcitrant deep-ocean dissolved organic matter during hydrothermal circulation
Uppsala University, Disciplinary Domain of Science and Technology, Chemistry, Department of Chemistry - BMC, Analytical Chemistry. Carl von Ossietzky Univ Oldenburg, Res Grp Marine Geochem, ICBM MPI Bridging Grp, Inst Chem & Biol Marine Environm ICBM, D-26129 Oldenburg, Germany..
Carl von Ossietzky Univ Oldenburg, Res Grp Marine Geochem, ICBM MPI Bridging Grp, Inst Chem & Biol Marine Environm ICBM, D-26129 Oldenburg, Germany.;Alfred Wegener Inst, HGF MPG Grp Deep Sea Ecol & Technol, D-27570 Bremerhaven, Germany..
Univ Georgia, Skidaway Inst Oceanog, Marine Sci, Savannah, GA 31411 USA..
Univ Washington, Joint Inst Study Atmosphere & Oceans, Seattle, WA 98115 USA.;NOAA PMEL, Seattle, WA 98115 USA..ORCID iD: 0000-0002-1595-9279
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2015 (English)In: Nature Geoscience, ISSN 1752-0894, E-ISSN 1752-0908, Vol. 8, no 11, 856-+ p.Article in journal (Refereed) Published
Abstract [en]

Oceanic dissolved organic carbon (DOC) is an important carbon pool, similar in magnitude to atmospheric CO2, but the fate of its oldest forms is not well understood(1,2). Hot hydrothermal circulation may facilitate the degradation of otherwise un-reactive dissolved organic matter, playing an important role in the long-term global carbon cycle. The oldest, most recalcitrant forms of DOC, which make up most of oceanic DOC, can be recovered by solid-phase extraction. Here we present measurements of solid-phase extractable DOC from samples collected between 2009 and 2013 at seven vent sites in the Atlantic, Pacific and Southern oceans, along with magnesium concentrations, a conservative tracer of water circulation through hydrothermal systems. We find that magnesium and solid-phase extractable DOC concentrations are correlated, suggesting that solid-phase extractable DOC is almost entirely lost from solution through mineralization or deposition during circulation through hydrothermal vents with fluid temperatures of 212-401 degrees C. In laboratory experiments, where we heated samples to 380 degrees C for four days, we found a similar removal efficiency. We conclude that thermal degradation alone can account for the loss of solid-phase extractable DOC in natural hydrothermal systems, and that its maximum lifetime is constrained by the timescale of hydrothermal cycling, at about 40 million years(3).

Place, publisher, year, edition, pages
2015. Vol. 8, no 11, 856-+ p.
National Category
Geochemistry
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URN: urn:nbn:se:uu:diva-304568DOI: 10.1038/NGEO2543ISI: 000367200000019OAI: oai:DiVA.org:uu-304568DiVA: diva2:1038855
Available from: 2016-10-20 Created: 2016-10-06 Last updated: 2016-10-20

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Hawkes, Jeffrey A.Butterfield, DavidDittmar, Thorsten
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