EGU21-6510, updated on 04 Mar 2021
https://doi.org/10.5194/egusphere-egu21-6510
EGU General Assembly 2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Benthic Nepheloid Layers along the U.S. GEOTRACES GA03 Transect in the Western North Atlantic: Characterization and Influence on 230Th and 231Pa Cycling

Siyuan Sean Chen1, Olivier Marchal2, Paul Lerner3, Daniel McCorkle2, and Michiel Rutgers van der Loeff4
Siyuan Sean Chen et al.
  • 1Massachusetts Institute of Technology, MIT-WHOI Joint Program in Oceanography, MA, U.S.A. (osean@mit.edu)
  • 2Department of Geology and Geophysics, Woods Hole Oceanographic Institution, MA, U.S.A.
  • 3NASA Goddard Institute for Space Studies, NY, U.S.A.
  • 4Alfred Wegner Institute for Polar and Marine Research, Bremerhaven, Germany

Benthic nepheloid layers (BNLs) are particle-rich layers that can extend over a thousand meter or more above the seafloor and are thought to be produced by the resuspension of fine sediments from strong bottom currents. They can often be subdivided into two sublayers: (i) a lower sublayer in contact with the seabed, where particle concentrations are the largest and which roughly coincides with the bottom mixed layer (BML); and (ii) an upper sublayer in which particle concentration decreases up to a clear water minimum (CWM). Although BNLs have long been recognised in vertical traces of optical instruments lowered to abyssal depths, their influence on ocean biogeochemical cycles – on the cycling of particle-reactive metals in particular – remains poorly understood.

In this study, we characterize the BNLs observed between the New England continental shelf and Bermuda and explore their influence on the cycling of 230Th and 231Pa – two naturally-occurring particle-reactive radionuclides that have found different applications in chemical oceanography and paleoceanography. To this end, we use concomitant measurements of temperature, salinity, particle concentration derived from light beam transmissometry, and 230Th and 231Pa activities in the dissolved and particulate fractions, which have been collected along the western segment of the U.S. GEOTRACES GA03 transect. We estimate that the thickness of strong BNLs (particle concentration > 20 µg l-1) varied from about 72 to 1358 m between different deep stations. At all stations, particle concentrations below the CWM were the highest in the BML, whose thickness ranged from 95 to 320 m, and decreased generally with height above the seafloor. A simplified model of particle-radionuclide cycling in the deep water column, which includes a particle source representing sediment resuspension at topographic reliefs and their subsequent lateral transport, is fitted to observed profiles of particle concentration and radionuclide activities at two selected stations. The model can reproduce simultaneously the increase of particle concentration with depth, the low dissolved activities in the BNLs, and the extremely large particulate activities near the bottom. Analysis of 230Th and 231Pa budgets reveals that the behaviour of both radionuclides in the BNL is fundamentally different from that envisioned in reversible exchange theory. Sensitivity tests with the model suggest that lateral particle sources near continental slopes and similar reliefs can produce significant biases in the paleoceanographic applications of both radionuclides, including the 230Th-normalization method and the interpretation of sediment 231Pa/230Th records.

How to cite: Chen, S. S., Marchal, O., Lerner, P., McCorkle, D., and Rutgers van der Loeff, M.: Benthic Nepheloid Layers along the U.S. GEOTRACES GA03 Transect in the Western North Atlantic: Characterization and Influence on 230Th and 231Pa Cycling, EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-6510, https://doi.org/10.5194/egusphere-egu21-6510, 2021.

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