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:0
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作者
D. Davoult
A. Migné
A. Créach
F. Gévaert
C. Hubas
N. Spilmont
G. Boucher
机构
[1] UPMC Univ Paris 6,
[2] UMR CNRS 7144 AD2M,undefined
[3] Station Biologique de Roscoff,undefined
[4] CNRS,undefined
[5] UMR 7144 AD2M,undefined
[6] Station Biologique de Roscoff,undefined
[7] Muséum National d’Histoire Naturelle,undefined
[8] UMR CNRS 5178 BOME,undefined
[9] Université des Sciences et Technologies de Lille 1,undefined
[10] UMR CNRS 8016,undefined
[11] GEPV,undefined
[12] Bat SN2,undefined
[13] Université des Sciences et Technologies de Lille I,undefined
[14] UMR CNRS 8187 LOG,undefined
[15] Station Marine de Wimereux,undefined
[16] Université du Littoral Côte d’Opale,undefined
[17] UMR CNRS 8187 LOG,undefined
[18] Maison de la Recherche en Environnement Naturel,undefined
来源
Hydrobiologia | 2009年 / 620卷
关键词
In situ measurements; Microphytobenthos; Intertidal community metabolism; Benthic primary production; Community respiration; PAM fluorometry;
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学科分类号
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-Oléron 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.
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页码:163 / 172
页数:9
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