Université de Caen Basse-Normandie, FRE3484 BioMEA, Caen, France.
PLoS One. 2012;7(8):e44155. doi: 10.1371/journal.pone.0044155. Epub 2012 Aug 29.
The high degree of physical factors in intertidal estuarine ecosystem increases material processing between benthic and pelagic compartments. In these ecosystems, microphytobenthos resuspension is a major phenomenon since its contribution to higher trophic levels can be highly significant. Understanding the sediment and associated microphytobenthos resuspension and its fate in the water column is indispensable for measuring the food available to benthic and pelagic food webs. To identify and hierarchize the physical/biological factors potentially involved in MPB resuspension, the entire intertidal area and surrounding water column of an estuarine ecosystem, the Bay des Veys, was sampled during ebb tide. A wide range of physical parameters (hydrodynamic regime, grain size of the sediment, and suspended matter) and biological parameters (flora and fauna assemblages, chlorophyll) were analyzed to characterize benthic-pelagic coupling at the bay scale. Samples were collected in two contrasted periods, spring and late summer, to assess the impact of forcing variables on benthic-pelagic coupling. A mapping approach using kriging interpolation enabled us to overlay benthic and pelagic maps of physical and biological variables, for both hydrological conditions and trophic indicators. Pelagic Chl a concentration was the best predictor explaining the suspension-feeders spatial distribution. Our results also suggest a perennial spatio-temporal structure of both benthic and pelagic compartments in the ecosystem, at least when the system is not imposed to intense wind, with MPB distribution controlled by both grain size and bathymetry. The benthic component appeared to control the pelagic one via resuspension phenomena at the scale of the bay. Co-inertia analysis showed closer benthic-pelagic coupling between the variables in spring. The higher MPB biomass observed in summer suggests a higher contribution to filter-feeders diets, indicating a higher resuspension effect in summer than in spring, in turn suggesting an important role of macrofauna bioturbation and filter feeding (Cerastoderma edule).
潮间带河口生态系统中高度的物理因素增加了底栖和浮游生物区系之间的物质处理。在这些生态系统中,微藻床的再悬浮是一个主要现象,因为它对更高营养级的贡献可能非常显著。了解沉积物和相关微藻床的再悬浮及其在水柱中的归宿,对于测量底栖和浮游食物网可用的食物是必不可少的。为了确定和分层潜在参与微藻床再悬浮的物理/生物因素,对河口生态系统的整个潮间带区域及其周围水层,在退潮时进行了采样。分析了广泛的物理参数(水动力状态、沉积物的粒度和悬浮物)和生物参数(动植物群落、叶绿素),以在海湾尺度上表征底栖-浮游耦合。在两个对比时期(春季和夏末)采集样本,以评估强迫变量对底栖-浮游耦合的影响。使用克立格插值的映射方法,我们能够将物理和生物变量的底栖和浮游地图叠加起来,同时考虑到水文学条件和营养指标。浮游叶绿素 a 浓度是解释滤食性动物空间分布的最佳预测因子。我们的结果还表明,生态系统中的底栖和浮游区系至少在不受强风影响时具有常年的时空结构,微藻床的分布受粒度和水深的共同控制。底栖部分通过在海湾尺度上的再悬浮现象控制着浮游部分。共协方差分析表明,春季变量之间的底栖-浮游耦合更紧密。夏季观察到的较高的微藻床生物量表明,它对滤食者饮食的贡献更高,这表明夏季的再悬浮效应高于春季,这反过来又表明大型动物生物扰动和滤食作用( Cerastoderma edule )的重要作用。