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Longitudinal distribution of macroinvertebrates in snowmelt streams in northeast Greenland: understanding biophysical controls

机译:格陵兰东北部融雪流中大型无脊椎动物的纵向分布:了解生物物理控制

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摘要

In a changing climate, Arctic streams are expected to show more influence from snowmelt, rainfall and groundwater, and less domination from glacial meltwater sources. Snowmelt streams are characteristic features of Arctic ecosystems, yet our current understanding of longitudinal patterns in benthic macroinvertebrate assemblages in these systems is limited when compared to glacier-fed systems. This study characterised longitudinal patterns of macroinvertebrate communities in snowmelt streams in northeast Greenland to provide novel insights into Arctic stream communities as dominant water sources shift with climate change. Benthic macroinvertebrates and environmental variables were sampled at three sites along five streams. Taxa diversity, evenness and abundance were expected to increase with distance from the stream source due to enhanced channel stability and warmer water temperature. This expectation for diversity and evenness was found in two streams, but abundance was up to ten times higher at the upstream sites compared to downstream, where biofilm biomass and ionic load were also highest. Here communities were largely dominated by the genus Eukiefferiella (Chironomidae). In the other three streams, no clear pattern in longitudinal macroinvertebrate community composition was evident due to low channel stability along the entire stream length. This study highlights the considerable variation in macroinvertebrate zonal distribution between snowmelt streams in northeast Greenland. A change towards more snowmelt-dominated streams in the Arctic could lead to shifts in the longitudinal organisation of macroinvertebrate community assemblages and the dominant species as a function of channel stability characteristics.Electronic supplementary materialThe online version of this article (doi:10.1007/s00300-017-2212-2) contains supplementary material, which is available to authorized users.
机译:在不断变化的气候中,预计北极溪流将受到融雪,降雨和地下水的更多影响,而来自冰川融水源的主导作用将减少。融雪流是北极生态系统的特征,但是,与冰川喂养的系统相比,我们目前对这些系统底栖大型无脊椎动物集合体的纵向模式的了解有限。这项研究描绘了格陵兰岛东北部融雪河中大型无脊椎动物群落的纵向格局,从而为北极河流群落提供了新颖的见解,因为主要的水源随着气候变化而变化。底栖无脊椎动物和环境变量是在沿着五个河流的三个地点取样的。由于增强的河道稳定性和较暖的水温,分类单元的多样性,均匀度和丰度预计会随着与流源距离的增加而增加。在两条流中发现了对多样性和均匀性的期望,但是与下游位置相比,上游位置的丰度最多高十倍,后者的生物膜生物量和离子负载也最高。在这里,社区主要由Eukiefferiella(Chironomidae)属主导。在其他三个溪流中,由于沿整个溪流长度的低河道稳定性,在纵向大型无脊椎动物群落组成中没有明显的模式。这项研究强调了格陵兰岛东北部融雪流之间的大型无脊椎动物地带分布的巨大差异。北极地区更多的融雪为主的河流可能会导致大型无脊椎动物群落组合和优势物种的纵向组织发生变化,这取决于渠道稳定性特征。电子补充材料本文的在线版本(doi:10.1007 / s00300- 017-2212-2)包含补充材料,授权用户可以使用。

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