Cross-slope zonation of erosion and deposition in the Faeroe-Shetland Channel,North Atlantic Ocean |
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| Institution: | 1. School of Coastal and Marine Systems Science, Coastal Carolina University, Conway, SC 29526, United States;2. Pacific Coastal and Marine Science Center, U.S. Geological Survey, Santa Cruz, CA 95060, United States;3. Woods Hole Coastal and Marine Science Center, U.S. Geological Survey, Woods Hole, MA 02543, United States;1. Department of Earth and Environmental Science, Vanderbilt University, PMB 351805, 2301 Vanderbilt Place, Nashville, TN 37235-1805, USA;2. Geological Survey of Bangladesh, 153 Pioneer Road, Segunbagicha, Dhaka 1000, Bangladesh |
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| Abstract: | Boundary currents and internal waves determine cross-slope zonation of erosion and deposition in the Faeroe-Shetland Channel. Currents were measured at 8 and 34–50 m above the bottom at three mooring sites (502, 595 and 708 m depth) for 14 days. The structure of the water column was evaluated from CTD sections, and included nepheloid layers and particulate matter concentrations. Indicators for recent deposition in the sediment (organic carbon, phytopigments, 210Pb) were measured at eight stations across the slope. Strong near-bottom currents at the upper slope sustain down-slope particle transport in a benthic nepheloid layer, which is eroded under the influence of critically reflecting M2 internal tidal waves at 350–550 m, where the major pycnocline meets the sloping bottom. Beam attenuation profiles confirmed the presence of intermediate nepheloid layers intruding into the Channel along the major pycnocline, and elevated concentrations of particulate matter and chlorophyll-a were measured at this depth. Near-bottom currents decreased with depth, thus allowing particle deposition down the slope. Inventories of excess 210Pb activity in the sediment deeper than 600 m were higher than what was expected on the basis of atmospheric input of 210Pb and production in the water column, thus indicating additional lateral inputs. Simple calculations showed that off-slope input of particles from areas shallower than 600 m may be responsible for the enhanced deposition at greater depths. |
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