Particle fluxes and geochemistry on the Canadian Beaufort Shelf: Implications for sediment transport and deposition

• Published in: Continental shelf research Vol. 26; no. 1; pp. 41 - 81
• Main Authors: O’Brien, M.C., Macdonald, R.W., Melling, H., Iseki, K.
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 2006
• Subjects: Aluminum; Beaufort; Biogenic; Calcium; Carbon; Fluxes; Freshwater; Iron; Isotope; Mackenzie; Marine; Nitrogen; Phosphorus; Sediment; Silica; Terrigenous; Transport; Trap; Canada, Northwest Terr., Mackenzie R; PNW, Beaufort Sea; Beaufort Sea; ANW, USA, North Carolina, Beaufort; PNW, Canada, Northwest Terr., Mackenzie; Biogenic; Sediment; Isotope; Calcium; Aluminum; Phosphorus; Trap; Iron; Beaufort; Fluxes; Nitrogen; Carbon; Silica; Terrigenous; Mackenzie; Transport
• ISSN: 0278-4343; 1873-6955
• DOI: 10.1016/j.csr.2005.09.007

Biogeochemical data from four sequential sediment traps deployed for one full year (April 1987–March 1988) at the shelf edge (200 m isobath) of the Canadian Beaufort Sea are presented. In addition, multi-traps and Kenney traps, which collect material suspended near the bottom, provided data from the inner shelf for short intervals in spring and summer. A novel aspect of this work is the discrimination of biogenic and terrigenous contributions to the total carbon using a relationship between terrigenous carbon and aluminum (Al). The vertical flux in the Beaufort Sea derives primarily from three sources: marine biological production, the Mackenzie River Plume, and coastal and seabed erosion. The material trapped at all shelf edge sites was predominantly biogenic and the seasonal fluxes of both biogenic and terrigenous matter varied with geographical location. In open-water conditions, deposition of terrigenous material can be attributed at various times and places to (1) transport by the Mackenzie Plume to the shelf edge during freshet; (2) resuspension of sediment during north-westerly gales; and (3) erosion of steep coastlines during south-easterly gales followed by northward transport. On the west side of the shelf, the biogenic and terrigenous fluxes were highest in summer and were primarily influenced by the Mackenzie River freshet, increased solar flux, available nutrients, sea ice break-up, and water column stability. On the east side of the shelf, biogenic and terrigenous fluxes were highest in the fall and the most important controlling factors were the extensive open water, intense resuspension events accompanying storms from the northwest, and the flow of the fresh, warm, turbid waters of Mackenzie River to the northeast. There was strong evidence of sediment transport in mid-water and bottom layers, but the mechanisms involved cannot be inferred from this study. Stable isotopes of carbon and nitrogen, C/N ratios, biogenic silica, and chlorophyll a measurements help to distinguish between marine autotrophic production and heterotrophic production, of which the latter appears to dominate in the fall and continue beneath the ice into the polar night. Al and iron correlate strongly and are primarily associated with the terrigenous fraction whereas calcium and phosphorus have both terrestrial and biogenic associations.