...
首页> 外文期刊>Global change biology >Tracing biogeochemical subsidies from glacier runoff into Alaska's coastal marine food webs
【24h】

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

机译:从冰川径流追踪生物地球化学补贴,进入阿拉斯加的沿海海洋食品网

获取原文
获取原文并翻译 | 示例
   

获取外文期刊封面封底 >>

       

摘要

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 glaciermarine habitats by developing a multi-trophic level Bayesian three-isotope mixing model. We utilized large gradients in stable (delta C-13, delta N-15, delta H-2) and radiogenic (Delta C-14) 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-14-age) but dissolved inorganic carbon and biota in coastal waters were young (530 years BP C-14-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.
机译:近一半的淡水排放到阿拉斯加湾源自景观排放冰川径流,但河流有机物涌入对沿海海洋食品网的滋润动力学的影响并不顺利。我们通过开发多营养水平贝叶斯三同位素混合模型来量化河流有机物补贴对冰川汞栖息地的生态影响。我们利用稳定(Delta C-13,Delta N-15,Delta H-2)和辐射(Delta C-14)同位素的大型梯度,其追踪河流和海洋有机物来源,因为它们被从较低到更高的营养水平降低冰川海洋栖息地。我们还比较了冰川海洋和更多海洋栖息地之间的同位素比率。基于对海洋消费者的潜在基线来源的同位素测量,海洋消费者的环境水和组织,河流有机物源对上部营养水平物种的贡献,包括鱼类和海鸟的水平物种范围从12%到44%。类似的分类群之间资源使用的可变性对应于物种分布和寿命历史的变化。例如,冰川嵌套Seabirds Kittlitz的Murrelet(Brachyramphus Brevirostris)的河流有机物同化大于森林嵌套大理石米列尔(B.Marmoratus)的河流的同化。冰川径流和近表面沿海水域中的颗粒和溶解的有机碳(12100-1500岁,BP C-14岁),但沿海水域溶解无机碳和生物群是年轻的(530岁,BP C-14岁) )。因此,海洋食品网中的陆地衍生补贴主要由冰川生态系统及其周围流域释放的年轻有机物质来源组成。稳定的同位素组合物还揭示了冰河 - 海洋和海洋部位之间的食物网结构的分歧。这项工作展示了地面和海洋生态系统之间的联系,并促进了对淡水径流的气候驱动变化如何更好地了解淡水径流的变化有可能在阿拉斯加沿海海洋生态系统中改变食物网络动态。

著录项

相似文献

  • 外文文献
  • 中文文献
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号