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地下水排泄导致北方森林溪流网络中河岸植物物种丰富度的热点地区形成。

Groundwater discharge creates hotspots of riparian plant species richness in a boreal forest stream network.

出版信息

Ecology. 2014 Mar;95(3):715-25. doi: 10.1890/13-0363.1.

Abstract

Riparian vegetation research has traditionally focused on channel-related processes because riparian areas are situated on the edge of aquatic ecosystems and are therefore greatly affected by the flow regime of streams and rivers. However, due to their low topographic position in the landscape, riparian areas receive significant inputs of water and nutrients from uplands. These inputs may be important for riparian vegetation, but their role for riparian plant diversity is poorly known. We studied the relationship between the influx of groundwater (GW) from upland areas and riparian plant diversity and composition along a stream size gradient, ranging from small basins lacking permanent streams to a seventh-order river in northern Sweden. We selected riparian sites with and without GW discharge using a hydrological model describing GW flow accumulation to test the hypothesis that riparian sites with GW discharge harbor plant communities with higher species richness. We further investigated several environmental factors to detect habitat differences between sites differing in GW discharge conditions. Vascular plant species richness was between 15% and 20% higher, depending on the spatial scale sampled, at riparian sites with GW discharge in comparison to non-discharge sites, a pattern that was consistent across all stream sizes. The elevated species richness was best explained by higher soil pH and higher nitrogen availability (manifested as lower soil C/N ratio), conditions which were positively correlated with GW discharge. Base cations and possibly nitrogen transported by groundwater may therefore act as a terrestrial subsidy of riparian vegetation. The stable isotopes 15N and 13C were depleted in soils from GW discharge compared to non-discharge sites, suggesting that GW inputs might also affect nitrogen and carbon dynamics in riparian soils. Despite the fact that many flows of water and nutrients reaching streams are filtered through riparian zones, the importance of these flows for riparian vegetation has not been appreciated. Our results demonstrated strong relationships between GW discharge, plant species richness and environmental conditions across the entire stream size gradient, suggesting that both river hydrology and upland inputs should be considered to fully understand riparian vegetation dynamics.

摘要

河岸植被研究传统上侧重于与河道相关的过程,因为河岸带处于水生生态系统的边缘,因此受到溪流和河流水流模式的极大影响。然而,由于其在景观中的低地形位置,河岸带从高地接收大量的水和养分。这些输入可能对河岸植被很重要,但它们对河岸植物多样性的作用知之甚少。我们研究了从高地输入的地下水 (GW) 与溪流大小梯度沿河岸植被多样性和组成之间的关系,范围从小到没有永久性溪流的盆地到瑞典北部的第七级河流。我们使用描述 GW 水流累积的水文模型选择有和没有 GW 排放的河岸地点,以测试以下假设:具有 GW 排放的河岸地点拥有具有更高物种丰富度的植物群落。我们进一步调查了几个环境因素,以检测 GW 排放条件不同的地点之间的栖息地差异。与非排放地点相比,具有 GW 排放的河岸地点的维管束植物物种丰富度高 15%至 20%,具体取决于采样的空间尺度,这种模式在所有溪流大小上都是一致的。这种升高的物种丰富度主要是由较高的土壤 pH 值和较高的氮供应(表现为较低的土壤 C/N 比)解释的,而这些条件与 GW 排放呈正相关。因此,地下水中可能还有基性阳离子和氮作为河岸植被的陆地补贴。与非排放地点相比,来自 GW 排放的土壤中的稳定同位素 15N 和 13C 被消耗,这表明 GW 输入可能也会影响河岸土壤中的氮和碳动态。尽管许多到达溪流的水和养分流都经过河岸带过滤,但这些流对河岸植被的重要性尚未得到重视。我们的结果表明,在整个溪流大小梯度上,GW 排放、植物物种丰富度和环境条件之间存在很强的关系,这表明应该同时考虑河流水文学和高地输入,以充分了解河岸植被动态。

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