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Spatial Variation in Sediment Organic Carbon Distribution across the Alaskan Beaufort Sea Shelf

Department of Physical and Environmental Sciences, Texas A&M University-Corpus Christi, Corpus Christi, TX 78412, USA
Department of Oceanography, US Naval Academy, Annapolis, MD 21402, USA
Hawaii Natural Energy Institute, University of Hawaii, Honolulu, HI 96822, USA
Marine Biogeochemistry, Naval Research Laboratory, Washington, DC 20375, USA
Author to whom correspondence should be addressed.
Energies 2017, 10(9), 1265;
Received: 17 June 2017 / Revised: 22 August 2017 / Accepted: 23 August 2017 / Published: 25 August 2017
In September 2009, a series of sediment cores were collected across the Alaskan Beaufort Sea shelf-slope. Sediment and porewater organic carbon (OC) concentrations and stable carbon isotope ratios (δ13C) were measured to investigate spatial variations in sediment organic matter (OM) sources and distribution of these materials across the shelf. Cores were collected along three main nearshore (shelf) to offshore (slope) sampling lines (transects) from east-to-west along the North Slope of Alaska: Hammerhead (near Camden Bay), Thetis Island (near Prudhoe Bay), and Cape Halkett (towards Point Barrow). Measured sediment organic carbon (TOC) and porewater dissolved organic carbon (DOC) concentrations and their respective δ13C values were used to investigate the relative contribution of different OM sources to sediment OC pool cycled at each location. Sources of OM considered included: water column-sourced phytodetritus, deep sediment methane (CH4), and terrestrial, tundra/river-sourced OM. Results of these measurements, when coupled with results from previous research and additional analyses of sediment and porewater composition, show a pattern of spatial variation in sediment OC concentrations, OM source contributions, and OM cycled along the Alaskan Beaufort Sea shelf. In general, measured sediment total organic carbon (TOC) concentrations, δ13CTOC values, porewater DOC concentrations, and δ13CDOC values are consistent with an east-to-west transport of modern Holocene sediments with higher OC concentrations primarily sourced from relatively labile terrestrial, tundra OM sources and phytodetritus along the Alaskan Beaufort shelf. Sediment transport along the shelf results in the medium-to-long term accumulation and burial of sediment OM focused to the west which in turn results in higher biogenic CH4 production rates and higher upward CH4 diffusion through the sediments resulting in CH4AMO-sourced contribution to sediment OC westward along the shelf. Understanding current OM sources and distributions along the Alaskan Beaufort shelf is important for enhancing models of carbon cycling in Arctic coastal shelf systems. This will help support the prediction of the climate response of the Arctic created in the face of future warming scenarios. View Full-Text
Keywords: Beaufort Sea; methane; tundra; organic carbon; stable isotopes; sediment; porewater Beaufort Sea; methane; tundra; organic carbon; stable isotopes; sediment; porewater
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Coffin, R.B.; Smith, J.P.; Yoza, B.; Boyd, T.J.; Montgomery, M.T. Spatial Variation in Sediment Organic Carbon Distribution across the Alaskan Beaufort Sea Shelf. Energies 2017, 10, 1265.

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