Dissolved Organic Carbon Production and Consumption in Anoxic Marine Sediments: A Pulsed-Tracer Experiment

The degradation of phytoplankton and seagrass organic carbon (OC) in sulfate-reducing (SR) and methane-producing (MP) sediments was tracked by measuring concentrations of particulate OC (POC), hydrolysis products (HP), fermentation products (FP), and inorganic end products (EP). This experiment used...

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Bibliographic Details
Published in:	Limnology and oceanography Vol. 46; no. 8; pp. 1908 - 1920
Main Authors:	Hee, Carol A., Pease, Tamara K., Alperin, Marc J., Martens, Christopher S.
Format:	Journal Article
Language:	English
Published:	Waco, TX American Society of Limnology and Oceanography 01-12-2001
Subjects:	Algae Carbon Carbon dioxide Earth sciences Earth, ocean, space Exact sciences and technology Flasks Hydrolysis Isotope geochemistry Isotope geochemistry. Geochronology Marine Marine and continental quaternary Marine sediments Methane Oxygen Phytoplankton Sediments Sulfates Surficial geology North Carolina North Atlantic United States Northwest Atlantic experimental studies particulate matters stable isotopes C-13/C-12 Atlantic Ocean sulfates North America drill cores chemical reduction organic materials methane phytoplankton anaerobic environment plankton dissolved materials organic carbon hydrolysis marine sediments
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Summary:	The degradation of phytoplankton and seagrass organic carbon (OC) in sulfate-reducing (SR) and methane-producing (MP) sediments was tracked by measuring concentrations of particulate OC (POC), hydrolysis products (HP), fermentation products (FP), and inorganic end products (EP). This experiment used the novel approach of amending sediment with organic substrates having δ13C values unique from that of the OC pool originally present in the sediment. As a result, we could monitor changes in the dynamic dissolved OC pool and gain insight into processes that control the fate of OC. Rates of hydrolysis, fermentation, and terminal metabolism were greater in the phytoplankton-amended treatments than in the seagrass-amended treatments during the period of active decomposition. At the end of the incubation, concentrations of HP and FP in amended treatments were not significantly different from those in the controls. An analysis of the δ13C values of HP from the amended treatments indicated that the addition of fresh organic matter stimulated the decomposition of carbon present in the sediment at the time of collection. Hydrolysis of this carbon accounted for ≥50% of the total carbon hydrolyzed in the sediment amended with seagrass.
Bibliography:	ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23
ISSN:	0024-3590 1939-5590
DOI:	10.4319/lo.2001.46.8.1908