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首页> 外文期刊>Global change biology >Estuarine fish communities respond to climate variability over both river and ocean basins
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Estuarine fish communities respond to climate variability over both river and ocean basins

机译:河口鱼类群落对河流和海洋盆地的气候变化做出响应

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Estuaries are dynamic environments at the land-sea interface that are strongly affected by interannual climate variability. Ocean-atmosphere processes propagate into estuaries from the sea, and atmospheric processes over land propagate into estuaries from watersheds. We examined the effects of these two separate climate-driven processes on pelagic and demersal fish community structure along the salinity gradient in the San Francisco Estuary, California, USA. A 33-year data set (1980-2012) on pelagic and demersal fishes spanning the freshwater to marine regions of the estuary suggested the existence of five estuarine salinity fish guilds: limnetic (salinity=0-1), oligohaline (salinity=1-12), mesohaline (salinity=6-19), polyhaline (salinity=19-28), and euhaline (salinity=29-32). Climatic effects propagating from the adjacent Pacific Ocean, indexed by the North Pacific Gyre Oscillation (NPGO), affected demersal and pelagic fish community structure in the euhaline and polyhaline guilds. Climatic effects propagating over land, indexed as freshwater outflow from the watershed (OUT), affected demersal and pelagic fish community structure in the oligohaline, mesohaline, polyhaline, and euhaline guilds. The effects of OUT propagated further down the estuary salinity gradient than the effects of NPGO that propagated up the estuary salinity gradient, exemplifying the role of variable freshwater outflow as an important driver of biotic communities in river-dominated estuaries. These results illustrate how unique sources of climate variability interact to drive biotic communities and, therefore, that climate change is likely to be an important driver in shaping the future trajectory of biotic communities in estuaries and other transitional habitats.
机译:河口是陆海界面的动态环境,受到年际气候变化的强烈影响。海洋-大气过程从海洋传播到河口,陆地上的大气过程从集水区传播到河口。我们在美国加利福尼亚州旧金山河口沿盐度梯度考察了这两个单独的气候驱动过程对上层和深层鱼类群落结构的影响。关于淡水和河口鱼类的淡水到河口海洋区域的33年数据集(1980-2012)表明存在五个河口盐度鱼类行会:limnetic(盐度= 0-1),oligohaline(盐度= 1- 12),中盐(盐度= 6-19),多盐(盐度= 19-28)和真盐碱(盐度= 29-32)。由北太平洋回旋涛动(NPGO)索引的从邻近太平洋传播的气候影响影响了euhaline和polyhaline行会中的海底鱼类和中上层鱼类群落结构。气候影响在陆地上传播,指数表示为流域(OUT)的淡水流出,影响了寡卵,中卵,多卵和正卵行会中的海底鱼类和中上层鱼类群落结构。 OUT的影响比河口盐度梯度向上传播的NPGO的影响进一步向下扩散到河口盐度梯度,这例证了可变的淡水流出在河流控制的河口中作为生物群落重要驱动力的作用。这些结果说明了气候变化的独特来源如何相互作用以驱动生物群落,因此,气候变化可能是塑造河口和其他过渡性栖息地生物群落未来轨迹的重要驱动力。

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