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MEPS 291:23-33 (2005)
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Abstract
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Role of pelletization in mineralization of fine-grained coastal sediments
Christian Wild1,3,*, Hans Røy1, Markus Huettel1,2
1Max Planck Institute for Marine Microbiology, Celsiusstraße 1, 28359 Bremen, Germany 2Department of Oceanography, Florida State University, Tallahassee, Florida 32306-4320, USA 3Present address: Ocean
Sciences Section, Intergovernmental Oceanographic Comission, UNESCO, 1 rue Miollis, 75015 Paris, France
*Email: c.wild@lrz.uni-muenchen.de

ABSTRACT: This study investigates how pellet deposition caused by the head-down deposit feeding polychaete Heteromastus filiformis enhances sediment surface layer permeability and thereby the degradation of organic matter contained in that layer.
The permeability of pellet accumulations on the sediment surface was 2 orders of magnitude higher than that of the non-pelletized sediment surface, which also had a 30% lower porosity. Freshly deposited organic-rich pellets initially consumed
approximately 10 times more O2 than an equivalent volume of the ambient, oxic, surface sediment. As a consequence of the deposition of the relatively large (400 to 500 µm) grain-like pellets in small mounds, topographical structures are
generated on the originally rather flat surface, which cause advective pore water flow through the pellet mounds as soon as the latter are exposed to boundary layer flows. At a flow velocity of 70 mm s1 at 5 mm above the sediment, pore
water flow velocity through pellet accumulations ranged from 1 to 2 mm s1, transporting oxygenated water to the pellets. Incubation experiments in flow-through columns showed that the O2 consumption of pellet accumulations
increases by approximately 100 µmol (g dry mass)1 d1 when the flow rate is increased from 10 to 20 ml h1. A faster degradation of reduced organic C and N contained in the fecal pellets was observed
under the influence of flow (70% of C and 68% of N degraded) compared to stagnancy (44% of C and 40% of N degraded) in a 3 wk flume incubation. Degradation of organic C and N in the surrounding, flat, surface sediment, which was not flushed by water flow,
was not detectable during the same time period. We conclude that pelletization enhances organic matter turnover in fine-grained deposits through generation of a high secondary permeability of the sediment surface layer that permits advective pore water
exchange, enhancing mineralization of the deposited organic-rich pellets.
KEY WORDS: Heteromastus filiformis · Fecal pellets · Permeability · Advective flow · Oxygen profiles · Organic matter degradation
Full text in pdf format

Published in MEPS Vol.
291
(2005) on April 28
Print ISSN: 0171-8630; Online ISSN: 1616-1599.
Copyright © Inter-Research, Oldendorf/Luhe, 2005
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