Benthic O2 distribution and dynamics in a Mediterranean lagoon (Thau, France):: An in situ microelectrode study

被引:41
作者
Dedieu, K.
Rabouille, C.
Thouzeau, G.
Jean, F.
Chauvaud, L.
Clavier, J.
Mesnage, V.
Ogier, S.
机构
[1] CEA, CNRS, UMR 1572, Lab Sci Climat & Environm, F-91198 Gif Sur Yvette, France
[2] IPSL, F-91198 Gif Sur Yvette, France
[3] LEMAR, Inst Univ Europeen Mer, F-29240 Plouzane, France
[4] Univ Rouen, CNRS, UMR 6143, M2C, F-76821 Mont St Aignan, France
关键词
oxygen; sediment-water exchange; organic carbon mineralization; microelectrode; benthic recycling; coastal ocean;
D O I
10.1016/j.ecss.2006.11.010
中图分类号
Q17 [水生生物学];
学科分类号
071004 ;
摘要
Benthic oxygen profiles were acquired using microsensors over two seasonal cycles (December 2001, April and August 2002, January and May 2003) at two stations differently affected by shellfish farming activity in the Than lagoon (French Mediterranean coast). This study was part of the Microbent-PNEC Program on the study of biogeochemical processes at the sediment-water interface in an eutrophicated environment. We explored seasonal and spatial heterogeneity as well as the biogeochemical drivers of oxygen uptake, such as in situ temperature, bottom water oxygenation and organic matter deposition. O-2 consumption rates were determined by using a transport-reaction model. Maximum rates were reached in August and May and minimum rates in December, April or January. The effect of oyster farming on oxygen fluxes was clearly identified with higher diffusive oxygen uptake in the station inside the oyster parks (C5; 36.8 +/- 18.5-87.7 +/- 40.8 mmol m(-2) d(-1)), compared with the station lying outside the oyster parks (C4; 8.6 +/- 2.1-30.7 +/- 8.3 mmol m(-2) d(-1)). At C5, the large spatial heterogeneity was statistically concealing temporal variation, whereas a clear statistical difference between cold and warm periods appeared at C4. In these lagoon sediments, the seasonal dynamics of diffusive oxygen demand and consumption rates were mainly driven by seasonal temperature variation at both stations, as well as by seasonal organic matter delivery to the sediment at the station located outside the oyster parks. In the station located below the oyster parks, seasonal variation of organic matter deposition was dampened by oyster filtering activity. Seasonal temperature variation thus appeared as the major driver of oxygen dynamics in this station. Measurements of total O-2 uptake rates indicated a significant fraction of microbial recycling and diffusive transport in oxygen uptake at the station located close to the oyster parks. In the open water site, fauna-mediated O-2 transport prevailed in April 2002 (cold conditions), whereas the microbial recycling seemed to dominate in May 2003 (warm conditions). (c) 2006 Elsevier Ltd. All rights reserved.
引用
收藏
页码:393 / 405
页数:13
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