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Sediment-water fluxes of dissolved inorganic carbon, O2, nutrients, and N2 from the hypoxic region of the Louisiana continental shelf

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Abstract

Globally, hypoxic areas (<63 mmol O2 m−3) in coastal waters are increasing in number and spatial extent. One of the largest coastal hypoxic regions has been observed during the summer in the bottom-water of the Louisiana continental shelf. The shelf receives the sediments, organic matter, and nutrients exported from the Mississippi River watershed, and much of this material is ultimately deposited to the sea floor. Hence, quantifying the rates of sediment-water dissolved inorganic carbon (DIC), oxygen (O2), and nutrient fluxes is important for understanding how these processes relate to the development and maintenance of hypoxia. In this study, the sediment-water fluxes of DIC, O2, nutrients, and N2 (denitrification) were measured on the Louisiana shelf during six cruises from 2005 to 2007. On each cruise, three to four sites were occupied in or directly adjacent to the region of the shelf that experiences hypoxia. DIC fluxes, a proxy for total sediment respiration, ranged from 7.9 to 21.4 mmol m−2 day−1 but did not vary significantly either spatially or as a function of bottom-water O2 concentration. Overall, sediment respiration and nutrient flux rates were small in comparison to water-column respiration and phytoplankton nutrient demand. Nitrate fluxes were correlated with bottom-water O2 concentrations (r = 0.69), and there was evidence that decreasing O2 concentrations inhibited coupled nitrification-denitrification. Denitrification rates averaged 1.4 mmol N m−2 day−1. Scaled to the area of the shelf, the denitrification sink represented approximately 39% of the N load from the Mississippi River watershed. The sediment-water fluxes reported from this study add substantial information on the spatial and temporal patterns in carbon, O2, and nutrient cycling available for the Louisiana continental shelf and, thus, improve the understanding of this system.

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Acknowledgments

We thank A. Almario, J. Aukamp, M. Barron, J. Campbell, G. Craven, L. Oliver, R. Quarles, J. Scott, and R. Stanley for assistance in the collection and analysis of sediment samples. We thank J. Cornwell and M. Owens for analyzing N2, O2, and Ar samples from several of the early cruises. We thank the US EPA Office of Water and Gulf of Mexico Program Office for their support of ship time, and the crews of the OSV Bold and the R/V Longhorn which made this work possible. We thank C. Peacher, P. Caraballo, D. Bullock, and the facilties’ staff for designing and building the sediment incubation systems, and for all the other facilities support for this work. Critical reviews by R. Greene, W. Gardner, J. Melack and three anonymous reviewers greatly improved this manuscript. We dedicate this contribution to the memory of our friend and EPA colleague R.L. Quarles. This study was funded, reviewed, and approved for publication by the US EPA, National Health and Environmental Effects Research Laboratory; however, the contents are solely the views of the authors. Use of trade names or commercial products does not constitute endorsement by the US EPA. Contribution number 1373 from the US EPA, Gulf Ecology Division.

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  1. Gulf Ecology Division, US EPA, NHEERL, 1 Sabine Island Drive, Gulf Breeze, FL, 32561, USA

    John C. Lehrter, David L. Beddick Jr., Richard Devereux, Diane F. Yates & Michael C. Murrell

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  1. John C. Lehrter
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Correspondence to John C. Lehrter.

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Lehrter, J.C., Beddick, D.L., Devereux, R. et al. Sediment-water fluxes of dissolved inorganic carbon, O2, nutrients, and N2 from the hypoxic region of the Louisiana continental shelf. Biogeochemistry 109, 233–252 (2012). https://doi.org/10.1007/s10533-011-9623-x

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