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Tidal day organic and inorganic material flux of ponds in the Liberty Island freshwater tidal wetland

机译:自由岛淡水潮汐湿地池塘潮汐日有机和无机物质通量

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摘要

The loss of inorganic and organic material export and habitat produced by freshwater tidal wetlands is hypothesized to be an important contributing factor to the long-term decline in fishery production in San Francisco Estuary. However, due to the absence of freshwater tidal wetlands in the estuary, there is little information on the export of inorganic and organic carbon, nutrient or phytoplankton community biomass and the associated mechanisms. A single-day study was conducted to assess the potential contribution of two small vegetated ponds and one large open-water pond to the inorganic and organic material flux within the freshwater tidal wetland Liberty Island in San Francisco Estuary. The study consisted of an intensive tidal day (25.5 h) sampling program that measured the flux of inorganic and organic material at three ponds using continuous monitoring of flow, chlorophyll a, turbidity and salt combined with discrete measurements of phytoplankton community carbon, total and dissolved organic carbon and nutrient concentration at 1.5 h intervals. Vegetated ponds had greater material concentrations than the open water pond and, despite their small area, contributed up to 81% of the organic and 61% of the inorganic material flux of the wetland. Exchange between ponds was important to wetland flux. The small vegetated pond in the interior of the wetland contributed as much as 72–87% of the total organic carbon and chlorophyll a and 10% of the diatom flux of the wetland. Export of inorganic and organic material from the small vegetated ponds was facilitated by small-scale topography and tidal asymmetry that produced a 40% greater material export on ebb tide. The small vegetated ponds contrasted with the large open water pond, which imported 29–96% of the inorganic and 4–81% of the organic material into the wetland from the adjacent river. This study identified small vegetated ponds as an important source of inorganic and organic material to the wetland and the importance of small scale physical processes within ponds to material flux of the wetland.
机译:据推测,淡水潮汐湿地造成的无机和有机材料出口和栖息地的丧失,是造成旧金山河口渔业产量长期下降的重要因素。但是,由于河口没有淡水潮汐湿地,关于无机和有机碳,养分或浮游植物群落生物量的出口以及相关机制的信息很少。进行了为期一天的研究,以评估两个小植物塘和一个大开放水塘对旧金山河口淡水潮汐湿地自由岛内无机和有机物质通量的潜在贡献。这项研究包括一个密集的潮汐日(25.5小时)采样程序,该程序使用连续监测流量,叶绿素a,浊度和盐以及对浮游植物群落碳,总和溶解的离散测量来测量三个池塘中无机和有机物质的通量有机碳和养分浓度间隔为1.5小时。植被池塘比开放水塘具有更大的物质集中度,尽管面积较小,但湿地的有机物通量贡献率高达81%,无机物贡献率达61%。池塘之间的交换对湿地通量很重要。湿地内部的小型植被塘占湿地总有机碳和叶绿素a的72-87%,硅藻通量的10%。小规模的地形和潮汐不对称促进了小型植被池塘的无机和有机物质的出口,潮汐导致物质出口增加了40%。小型的植被池塘与大型的开放水塘形成对比,大型的开放水塘从相邻的河中将29–96%的无机物和4–81%的有机物输入湿地。这项研究确定了小植被池塘是湿地无机和有机物质的重要来源,并且池塘中的小规模物理过程对湿地物质通量的重要性。

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