Spatio-temporal variability of intertidal benthic primary production and respiration in the western part of the Mont Saint-Michel Bay (Western English Channel, France)

被引:23
作者
Davoult, D. [1 ]
Migne, A. [1 ,2 ]
Creach, A. [3 ]
Gevaert, F. [4 ]
Hubas, C. [1 ,5 ]
Spilmont, N. [4 ,5 ]
Boucher, G. [2 ]
机构
[1] Univ Paris 06, CNRS, UMR 7144 AD2M, UPMC,Stn Biol Roscoff, F-29682 Roscoff, France
[2] CNRS, UMR 5178, Museum Natl Hist Nat, F-75231 Paris 5, France
[3] Univ Sci & Technol Lille 1, CNRS, UMR 8016, GEPV, F-59655 Villeneuve Dascq, France
[4] Univ Sci & Technol Lille 1, CNRS, UMR 8187 LOG, Stn Marine Wimereux, F-62930 Wimereux, France
[5] Univ Littoral Cote dOpale, CNRS, UMR 8187 LOG, F-62930 Wimereux, France
关键词
In situ measurements; Microphytobenthos; Intertidal community metabolism; Benthic primary production ~; Community respiration; PAM fluorometry; IN-SITU MEASUREMENTS; CHLOROPHYLL FLUORESCENCE; PHOTOSYNTHETIC ACTIVITY; MARENNES-OLERON; EMERSED CONDITIONS; CRASSOSTREA-GIGAS; ORGANIC-MATTER; MICROPHYTOBENTHOS; TEMPERATURE; SEDIMENT;
D O I
10.1007/s10750-008-9626-3
中图分类号
Q17 [水生生物学];
学科分类号
071004 ;
摘要
In situ measurements of both community metabolism (primary production and respiration) and PAM fluorometry were conducted during emersion on intertidal sediments in the Mont Saint-Michel Bay, in areas where oysters and mussels were cultivated. Results highlighted a low benthic metabolism compared to other intertidal areas previously investigated with the same methods. Comparisons between gross community primary production and relative electron transport rates confirmed this statement. More specifically, primary productivity remained very low all over the year, whereas the associated microalgal biomass was estimated to be high. We suggest that the microphytobenthic community studied was characterized by a self-limitation of its primary productivity by its own biomass, as previously shown in Marennes-Ol,ron Bay for example. The almost permanent high biomass would represent a limiting factor for micromigration processes within the first millimetres of the sediment. This could be explained by very low resuspension processes occurring in the western part of the bay, enhanced by the occurrence of numerous aquaculture structures that could decrease tidal currents in the benthic boundary layer.
引用
收藏
页码:163 / 172
页数:10
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