Dias Ester, Morais Pedro, Antunes Carlos, Hoffman Joel C
CIIMAR - Interdisciplinary Centre of Marine and Environmental Research, University of Porto, Terminal de Cruzeiros do Porto de Leixões, Avenida Norton de Matos, 4450-208 Matosinhos, Portugal.
CCMAR - Centre of Marine Sciences, University of Algarve, Campus de Gambelas, 8005-139 Faro, Portugal.
Food Webs. 2023 Jun;35:e00282. doi: 10.1016/j.fooweb.2023.e00282. Epub 2023 Apr 5.
Energy flows from land to sea and between pelagic and benthic environments have the potential to increase the connectivity between estuaries and adjacent ecosystems as well as among estuarine habitats. To identify such energy flows and the main trophic pathways of energy transfer in the Minho River estuary, we investigated the spatial and temporal fluctuations of carbon and nitrogen stable isotope ratios in benthic (and their potential food sources) and epibenthic consumers. Sampling was conducted along the estuarine salinity gradient from winter to summer of 2011. We found that the carbon (δC = C/C) and nitrogen (δN = N/N) stable isotope ratios of the most abundant benthic and epibenthic consumers varied along the salinity gradient. The δC values increased seaward, whereas the opposite pattern was found for the δN, especially during the summer. The stable isotope ratios revealed two trophic pathways in the Minho estuary food web. The first pathway is supported by phytoplankton and represented by filter feeders such as zooplankton and some deposit feeders, particularly amphipods and polychaetes. The second pathway is supported by detritus and composed essentially of deposit feeders, which by being consumed, allow detritus to be incorporated into higher trophic levels. Spatial and temporal feeding variations in the estuarine benthic food web are driven by hydrology and proximity to adjacent ecosystems (terrestrial, marine). During high river discharge periods, the δC (ca. -28‰) and C: N (>10) values suggested an increase of terrestrial-derived OM to the particulate OM pool, which was then used by suspension feeders. During low river discharge periods, marine intrusion increased upriver, which was reflected in benthic consumers' C-enriched stable isotope values. No relationship was found between food quality (phytoplankton vs. detritus) and food chain length because the lowest and highest values were associated with freshwater and saltmarsh areas, respectively, both dominated by the detrital pathway. This study demonstrates that benthic consumers enhance the connectivity between estuaries and its adjacent ecosystems by utilizing subsidies of terrestrial and marine origin and that benthic-pelagic coupling is an important energy transfer mechanism to the benthic food web.
能量从陆地流向海洋,并且在远洋和底栖环境之间流动,这有可能增加河口与相邻生态系统之间以及河口栖息地之间的连通性。为了确定米尼奥河河口的此类能量流动以及能量转移的主要营养途径,我们研究了底栖生物(及其潜在食物来源)和浅水底栖消费者中碳和氮稳定同位素比率的时空波动。采样于2011年冬季至夏季沿着河口盐度梯度进行。我们发现,最丰富的底栖生物和浅水底栖消费者的碳(δC = C/C)和氮(δN = N/N)稳定同位素比率沿盐度梯度变化。δC值向海增加,而δN则呈现相反的模式,尤其是在夏季。稳定同位素比率揭示了米尼奥河口食物网中的两条营养途径。第一条途径以浮游植物为支撑,以浮游动物和一些沉积食性动物(特别是双足类动物和多毛类动物)等滤食性动物为代表。第二条途径以碎屑为支撑,主要由沉积食性动物组成,它们通过被消耗,使碎屑被纳入更高的营养级。河口底栖食物网中的时空摄食变化受水文状况以及与相邻生态系统(陆地、海洋)的距离驱动。在河流高流量期,δC(约-28‰)和C:N(>10)值表明陆地来源的有机物质向颗粒有机物质库增加,然后被悬浮食性动物利用。在河流低流量期,海洋入侵向上游增加,这反映在底栖消费者富含碳的稳定同位素值上。未发现食物质量(浮游植物与碎屑)与食物链长度之间的关系,因为最低值和最高值分别与淡水和盐沼区域相关,这两个区域均以碎屑途径为主导。这项研究表明,底栖消费者通过利用陆地和海洋来源的补贴增强了河口与其相邻生态系统之间的连通性,并且底栖-远洋耦合是底栖食物网的重要能量转移机制。