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追踪冰川径流输入到阿拉斯加沿海海洋食物网中的生源要素。

Tracing biogeochemical subsidies from glacier runoff into Alaska's coastal marine food webs.

机构信息

U.S. Geological Survey Alaska Science Center, Juneau, AK, USA.

Environment and Climate Change Canada, Saskatoon, SK, Canada.

出版信息

Glob Chang Biol. 2018 Jan;24(1):387-398. doi: 10.1111/gcb.13875. Epub 2017 Sep 23.

Abstract

Nearly half of the freshwater discharge into the Gulf of Alaska originates from landscapes draining glacier runoff, but the influence of the influx of riverine organic matter on the trophodynamics of coastal marine food webs is not well understood. We quantified the ecological impact of riverine organic matter subsidies to glacier-marine habitats by developing a multi-trophic level Bayesian three-isotope mixing model. We utilized large gradients in stable (δ C, δ N, δ H) and radiogenic (Δ C) isotopes that trace riverine and marine organic matter sources as they are passed from lower to higher trophic levels in glacial-marine habitats. We also compared isotope ratios between glacial-marine and more oceanic habitats. Based on isotopic measurements of potential baseline sources, ambient water and tissues of marine consumers, estimates of the riverine organic matter source contribution to upper trophic-level species including fish and seabirds ranged from 12% to 44%. Variability in resource use among similar taxa corresponded to variation in species distribution and life histories. For example, riverine organic matter assimilation by the glacier-nesting seabirds Kittlitz's murrelet (Brachyramphus brevirostris) was greater than that of the forest-nesting marbled murrelet (B. marmoratus). The particulate and dissolved organic carbon in glacial runoff and near surface coastal waters was aged (12100-1500 years BP C-age) but dissolved inorganic carbon and biota in coastal waters were young (530 years BP C-age to modern). Thus terrestrial-derived subsidies in marine food webs were primarily composed of young organic matter sources released from glacier ecosystems and their surrounding watersheds. Stable isotope compositions also revealed a divergence in food web structure between glacial-marine and oceanic sites. This work demonstrates linkages between terrestrial and marine ecosystems, and facilitates a greater understanding of how climate-driven changes in freshwater runoff have the potential to alter food web dynamics within coastal marine ecosystems in Alaska.

摘要

流入阿拉斯加湾的淡水中,近一半来自于冰川融水形成的流域景观,但河流有机物质的涌入对沿海海洋食物网的营养动态的影响还不太清楚。我们通过开发一个多营养层次贝叶斯三同位素混合模型,量化了河流有机物质对冰川-海洋生境的生态影响。我们利用稳定(δ C、δ N、δ H)和放射性(Δ C)同位素的大梯度,这些同位素可以追踪河流和海洋有机物质源,因为它们从冰川-海洋生境中的较低营养层次传递到较高营养层次。我们还比较了冰川-海洋生境与更具海洋性的生境之间的同位素比值。基于对潜在基线源、周围水和海洋消费者组织的同位素测量,河流有机物质对包括鱼类和海鸟在内的上层营养级物种的来源贡献估计在 12%到 44%之间。相似类群之间资源利用的变异性与物种分布和生活史的变异性相对应。例如,冰川筑巢海鸟——斑海雀(Brachyramphus brevirostris)对河流有机物质的同化作用大于森林筑巢海鸟——花斑海雀(B. marmoratus)。冰川径流和近岸海域的颗粒态和溶解态有机碳已老化(12100-1500 年 BP C 年龄),但沿海海域的溶解无机碳和生物群仍很年轻(530 年 BP C 年龄至现代)。因此,海洋食物网中的陆地衍生补贴主要由从冰川生态系统及其周围流域释放的年轻有机物质源组成。稳定同位素组成还揭示了冰川-海洋和海洋生境之间食物网结构的差异。这项工作证明了陆地和海洋生态系统之间的联系,并有助于更好地理解淡水径流的气候变化如何改变阿拉斯加沿海海洋生态系统内的食物网动态。

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