Bioturbation and particle transport in Carolina slope sediments: A radiochemical approach

Citation:
Fornes, WL, Demaster DJ, Levin LA, Blair NE.  1999.  Bioturbation and particle transport in Carolina slope sediments: A radiochemical approach. Journal of Marine Research. 57:335-355.

Date Published:

Mar

Keywords:

continental-slope, deep-sea sediments, diagenesis, early, equatorial pacific, marine-sediments, mixing rates, north-carolina, organic-matter, pb-210, spatial heterogeneity

Abstract:

In situ tracer experiments investigated short-term sediment mixing processes at two Carolina continental margin sites (water depth = 850 m) characterized by different organic C fluxes, (234)Th mixing coefficients (D(b)) and benthic assemblages. Phytoplankton, slope sediment, and sand-sized glass beads tagged with (210)Pb, (113)Sn, and (228)Th, respectively, were placed via submersible at the sediment-water interface at both field sites (Site I off Cape Fear, and Site m off Cape Hatteras). Experimental plots were sampled at 0, 1.5 days, and 90 days after tracer emplacement to examine short-term, vertical transport. Both sites are initially dominated by nonlocal mixing. Transport to the bottom of the surface mixed layer at both sites occurs more rapidly than (234)Th-based D(b) values predict; after 1.5 days, tagged particles were observed 5 cm below the sediment-water interface at Site I and 12 cm below at Site III. Impulse tracer profiles after 90 days at Site m exhibit primarily diffusive distributions, most likely due to a large number of random, nonlocal mixing events. The D(b) values determined from 90-day particle tagging experiments are comparable to those obtained from naturally occurring (234)Th profiles (similar to 100-day time scales) from nearby locations. The agreement between impulse tracer mixing coefficients and steady-state natural tracer mixing coefficients suggests that the diffusive analogue for bioturbation on monthly time scales is a realistic and useful approach. Tracer profiles from both sites exhibit some degree of particle selective mixing, but the preferential transport of the more labile carbon containing particles only occurred 30% of the time. Consequently, variations in the extent to which age-dependent mixing occurs in marine sediments may depend on factors such as faunal assemblage and organic carbon flux.

Notes:

n/a

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DOI:

10.1357/002224099321618245