Sökning: WFRF:(Hulth Stefan 1965) > Macrofaunal reworki...
Fältnamn | Indikatorer | Metadata |
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000 | 03497naa a2200517 4500 | |
001 | oai:gup.ub.gu.se/56212 | |
003 | SwePub | |
008 | 240528s2004 | |||||||||||000 ||eng| | |
024 | 7 | a https://gup.ub.gu.se/publication/562122 URI |
024 | 7 | a https://doi.org/10.1016/j.seares.2004.02.0022 DOI |
040 | a (SwePub)gu | |
041 | a eng | |
042 | 9 SwePub | |
072 | 7 | a ref2 swepub-contenttype |
072 | 7 | a art2 swepub-publicationtype |
100 | 1 | a Caradec, S.4 aut |
245 | 1 0 | a Macrofaunal reworking activities and hydrocarbon redistribution in an experimental sediment system |
264 | 1 | b Elsevier BV,c 2004 |
520 | a The influence of macrofaunal reworking activities on the redistribution of particle associated hydrocarbon compounds (HC) was experimentally investigated. Two distinct hydrocarbon mixtures adsorbed on montmorillonite particles (< 4 gm diameter) were added to the surface and deeper (2.5 cm) sediment layers. For comparison, luminophores (100-160 mum diameter) were added in the two deposit layers. At the start of the experiment, four macrobenthic species (the bivalve Abra nitida, the polychaete Scalibregma inflatum, and the echmoderms Amphiura filiformis and Echinocardium cordatum) were added to the sediment surface. The macrofauna added rapidly transferred HC from the surface sediment down to similar to5 cm depth by both continuous (biodiffusion) and non-continuous (biotransport) transport. Hydrocarbon compounds initially added to the deeper sediment layer were only subject to biodiffusion-like transport. Apparent biodiffusion coefficients (Db) quantified by using a 1-D model were between 0.5 and 8.4 x 10(-3) cm(2) d(-1), and biotransport coefficients (r) ranged from 2.0 to 27.6 X 10(-3) d(-1). Thus, the four species studied did not have the same effect on particle redistribution and, consequently, on HC repartition in the sediments. E. cordatum was the most efficient reworker. The present study demonstrated the importance of particle size selectivity by benthic fauna, and verified that macrofaunal reworking activities may redeposit sediment from deeper sediment layers on the sediment surface. Both processes have obvious implications for rates and pathways during organic matter mineralisation in marine sediments. (C) 2004 Elsevier B.V. All rights reserved. | |
650 | 7 | a NATURVETENSKAPx Kemi0 (SwePub)1042 hsv//swe |
650 | 7 | a NATURAL SCIENCESx Chemical Sciences0 (SwePub)1042 hsv//eng |
653 | a bioturbation | |
653 | a hydrocarbons | |
653 | a sediment reworking | |
653 | a macrofauna | |
653 | a Gullmar | |
653 | a Fjord | |
653 | a DEPOSIT FEEDERS | |
653 | a MARINE SEDIMENT | |
653 | a ORGANIC-MATTER | |
653 | a CHLOROPHYLL-A | |
653 | a BIOTURBATION | |
653 | a PARTICLE | |
653 | a FATE | |
653 | a DEGRADATION | |
653 | a CARBON | |
653 | a QUANTIFICATION | |
700 | 1 | a Grossi, V.4 aut |
700 | 1 | a Hulth, Stefan,d 1965u Gothenburg University,Göteborgs universitet,Institutionen för kemi,Department of Chemistry4 aut0 (Swepub:gu)xhulst |
700 | 1 | a Stora, G.4 aut |
700 | 1 | a Gilbert, F.4 aut |
710 | 2 | a Göteborgs universitetb Institutionen för kemi4 org |
773 | 0 | t Journal of Sea Researchd : Elsevier BVg 52:3, s. 199-210q 52:3<199-210x 1385-1101 |
856 | 4 | u https://hal.archives-ouvertes.fr/hal-00757304/file/Gilbert_6099.pdf |
856 | 4 8 | u https://gup.ub.gu.se/publication/56212 |
856 | 4 8 | u https://doi.org/10.1016/j.seares.2004.02.002 |
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