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首页> 外文期刊>Estuarine Coastal and Shelf Science >Community structure of shoreline nekton in the estuarine portion of the Alafla River, Florida: Differences along a salinity gradient and inflow-related changes
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Community structure of shoreline nekton in the estuarine portion of the Alafla River, Florida: Differences along a salinity gradient and inflow-related changes

机译:佛罗里达阿拉法拉河河口部分海岸线上的线虫群落结构:盐度梯度差异和与入流有关的变化

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Determination of baseline biological conditions in Florida's rivers is required prior to increased water withdrawals for the rapidly growing human population. We studied the small-bodied shoreline nekton community of the estuarine portion of the Alafia River (a tributary of Tampa Bay, SW Florida) from 1998 to 2003 using 21.3-m seines of 3.2-mm stretched mesh. Community structure along the estuarine salinity gradient changed from dominance by marine and estuarine transients from river km 0 to 9.3 to greater abundances of resident low-salinity and freshwater forms near the tidal—freshwater interface (river km 9.3—14). There was evidence that the magnitude of the freshwater inflow influenced nekton community patterns along the estuary, with the center of abundance of many species shifting in response to inflow. The community structure of the nekton of river km 0—9.3 showed regular seasonal changes that were of greater importance than was temporal correlation with abiotic variables (temperature, salinity, inflow); these changes can be explained by predictable spawning patterns of transient species. In contrast, changes in the structure of the nekton community in river km 9.3—14 were well correlated with changes in salinity and, to a lesser extent, inflow. The sensitivity of the nekton to relatively small changes in salinity near the tidal—freshwater interface is of importance given that comparatively minor changes in freshwater inflow could markedly affect salinities in this upstream region.
机译:在快速增长的人口增加取水量之前,需要确定佛罗里达河流的基准生物学条件。我们研究了1998年至2003年间阿拉法河(佛罗里达州西南佛罗里达州坦帕湾的支流)河口部分的小岸线尼克顿群落,使用了3.2毫米长的3.2毫米围网围网。河口盐度梯度上的群落结构从海洋和河口瞬态的主导作用(从公里数0到9.3)改变为潮汐-淡水界面附近的居民低盐度和淡水形式的丰度更大(河面9.3-14)。有证据表明,淡水的流入量影响沿河口的尼克顿群落模式,许多物种的丰度中心随流入而变化。 0-9.3公里处的nekton河流的群落结构显示出规律的季节性变化,而与非生物变量(温度,盐度,入流量)的时间相关性比季节性变化更重要。这些变化可以通过瞬时物种的可预期产卵模式来解释。相反,在9.3-14公里的河中,尼克顿群落的结构变化与盐度变化以及入水量的变化相关性很强。考虑到淡水流入量的相对较小变化会显着影响该上游地区的盐度,因此,尼克顿对潮汐-淡水界面附近盐度变化相对较小的敏感性非常重要。

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