The short‐term fate of fresh algal carbon in continental slope sediments

Limnology and Oceanography - Tập 41 Số 6 - Trang 1208-1219 - 1996
Neal E. Blair1, Lisa A. Levin2, David J. DeMaster3, Gayle R. Plaia3
1Department of Marine, Earth and Atmospheric Sciences, North Carolina State University, Raleigh 27695-8208
2Marine Life Research Group, Scripps Institution of Oceanography, UCSD, La Jolla, California 92093-0218
3Department of Marine, Earth and Atmospheric Sciences, North Carolina State University

Tóm tắt

Emplacement of a tracer mixture containing 13C‐labeled green algae on the sea floor of the continental slope offshore of Cape Hatteras, North Carolina, elicited a rapid response over 1.5 d from the dense benthic community. Certain deposit‐feeding annelids (e.g. Scalibregma inflatum and Aricidea quadrilobata) became heavily labeled with 13C as a result of ingestion of the algae. “C‐labeled organic matter was transported to a depth of at least 4–5 cm into the seabed during the 1.5‐d period, presumably as a consequence of a feeding‐associated activity. Nonlocal transport produced subsurface peaks in organic 13C at 2–3 cm. Dissolved inorganic 13C, produced by the oxidation of the labeled algae, penetrated to 10‐cm depth. The transport of highly reactive organic matter from the sediment surface at initial velocities ≥3 cm d‒1 is expected to be an important control of subsurface benthic processes in slope environments characterized by abundant macrofaunal populations. Anaerobic processes, which are enhanced on the Cape Hatteras slope relative to adjacent areas, may be promoted by the rapid injection of reactive material into subsurface sediments. The transport, in turn, is a consequence of the dense infaunal populations that are supported by the rapid deposition of organic carbon in this region.

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Limnology and Oceanography

Tập 41 Số 6

1208-1219

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