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Use of axial tomography to follow temporal changes of benthic communities in an unstable sedimentary environment (Baie des Ha! Ha!, Saguenay Fjord)

Authors :
Bernard Long
Jean-François Crémer
Emma Michaud
Émilien Pelletier
Laure de Montety
Georges Stora
Jacques Locat
Franck Gilbert
Gaston Desrosiers
Université du Québec à Rimouski (UQAR)
Laboratoire d'océanographie et de biogéochimie (LOB)
Université de la Méditerranée - Aix-Marseille 2-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
Institut National de la Recherche Scientifique [Québec] (INRS)
Université Laval [Québec] (ULaval)
Centre National de la Recherche Scientifique - CNRS (FRANCE)
Institut National de la Recherche Scientifique - INRS (CANADA)
Institut de Recherche pour le Développement - IRD (FRANCE)
Université de la Méditerranée - Aix-Marseille II (FRANCE)
Université du Québec à Rimouski - UQAR (CANADA)
Laboratoire d'Océanographie et de Biogéochimie - LOB (Marseille, France)
Source :
Journal of Experimental Marine Biology and Ecology, Journal of Experimental Marine Biology and Ecology, 2003, vol. 285-286, pp. 265-282. ⟨10.1016/S0022-0981(02)00532-4⟩, ResearcherID, Journal of Experimental Marine Biology and Ecology, Elsevier, 2003, vol. 285-286, pp. 265-282. ⟨10.1016/S0022-0981(02)00532-4⟩
Publication Year :
2003
Publisher :
HAL CCSD, 2003.

Abstract

International audience; In the upper layer of the sediment column, organic matter recycling is greatly influenced by bioturbation. However, there are many physical changes in the nature of the sediment that may disturb benthic communities and create a biogeochemical imbalance. Following a very heavy rainfall between 26 and 29 July 1996, an intense flash flood in the Saguenay Fjord caused discharges of 6 million cubic metres of sediments into Baie des Ha! Ha!. Unstable sediment deposits located at the top of the delta of the Rivie're des Ha! Ha! were sporadically exported to the deep basin. After this physical disturbance, meiobenthic and macrobenthic organisms progressively re-colonised the sediment column. To determine the impacts of such sedimentary depositions on benthic fauna, two stations, one at the head and one at the mouth of the Baie des Ha! Ha!, have been monitored since 1996. During this survey, we developed a new method for the quantification of biogenic structures using computer axial tomography (CAT-Scan). Benthic fauna analysis showed that the two stations were characterised by different temporal changes in the benthic dynamics according to their geographic location. Using CAT-Scan analysis of sediment cores, we were able to characterise the stability of the sediment column for the two stations in 1999 and 2000. Scan results suggest that colonisation processes were closely linked with the stability of the sediment column. Erosion and redeposition of surficial sediments caused a succession in the formation of biogenic structures. These variations were characterised for the first time using CAT-Scan, which is a nondestructive, rapid, and precise method. Tomographic analysis showed the importance of the production and destruction rates of biogenic structures and the sedimentation rate for the preservation of burrows and potentially reactive components. This study finally demonstrated that each erosional event could be followed by a rapid formation of biogenic structures, allowing the re-oxidation of old deposits.

Details

Language :
English
ISSN :
00220981
Database :
OpenAIRE
Journal :
Journal of Experimental Marine Biology and Ecology, Journal of Experimental Marine Biology and Ecology, 2003, vol. 285-286, pp. 265-282. ⟨10.1016/S0022-0981(02)00532-4⟩, ResearcherID, Journal of Experimental Marine Biology and Ecology, Elsevier, 2003, vol. 285-286, pp. 265-282. ⟨10.1016/S0022-0981(02)00532-4⟩
Accession number :
edsair.doi.dedup.....8982afed5bfa645c49d4b72c1fc41b87
Full Text :
https://doi.org/10.1016/S0022-0981(02)00532-4⟩