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南极半岛西部快速变暖峡湾中的大型动物群落:丰度热点和β多样性

Megafaunal communities in rapidly warming fjords along the West Antarctic Peninsula: hotspots of abundance and beta diversity.

作者信息

Grange Laura J, Smith Craig R

机构信息

Department of Oceanography, University of Hawaii at Manoa, Honolulu, Hawaii, United States of America.

出版信息

PLoS One. 2013 Dec 3;8(12):e77917. doi: 10.1371/journal.pone.0077917. eCollection 2013.

Abstract

Glacio-marine fjords occur widely at high latitudes and have been extensively studied in the Arctic, where heavy meltwater inputs and sedimentation yield low benthic faunal abundance and biodiversity in inner-middle fjords. Fjord benthic ecosystems remain poorly studied in the subpolar Antarctic, including those in extensive fjords along the West Antarctic Peninsula (WAP). Here we test ecosystem predictions from Arctic fjords on three subpolar, glacio-marine fjords along the WAP. With seafloor photographic surveys we evaluate benthic megafaunal abundance, community structure, and species diversity, as well as the abundance of demersal nekton and macroalgal detritus, in soft-sediment basins of Andvord, Flandres and Barilari Bays at depths of 436-725 m. We then contrast these fjord sites with three open shelf stations of similar depths. Contrary to Arctic predictions, WAP fjord basins exhibited 3 to 38-fold greater benthic megafaunal abundance than the open shelf, and local species diversity and trophic complexity remained high from outer to inner fjord basins. Furthermore, WAP fjords contained distinct species composition, substantially contributing to beta and gamma diversity at 400-700 m depths along the WAP. The abundance of demersal nekton and macroalgal detritus was also substantially higher in WAP fjords compared to the open shelf. We conclude that WAP fjords are important hotspots of benthic abundance and biodiversity as a consequence of weak meltwater influences, low sedimentation disturbance, and high, varied food inputs. We postulate that WAP fjords differ markedly from their Arctic counterparts because they are in earlier stages of climate warming, and that rapid warming along the WAP will increase meltwater and sediment inputs, deleteriously impacting these biodiversity hotspots. Because WAP fjords also provide important habitat and foraging areas for Antarctic krill and baleen whales, there is an urgent need to develop better understanding of the structure, dynamics and climate-sensitivity of WAP subpolar fjord ecosystems.

摘要

峡湾型冰川海洋环境广泛分布于高纬度地区,并且在北极地区已经得到了广泛研究,在北极地区,大量融水的注入和沉积作用导致峡湾中部和内部的底栖动物丰度和生物多样性较低。南极亚极地地区的峡湾底栖生态系统,包括南极半岛西部(WAP)广阔峡湾中的生态系统,仍然研究较少。在这里,我们对来自北极峡湾的生态系统预测,在WAP沿岸的三个亚极地峡湾型冰川海洋环境进行了测试。通过海底摄影调查,我们评估了安德沃德湾、佛兰德斯湾和巴里拉里湾软质沉积盆地中,深度在436 - 725米的底栖大型动物的丰度、群落结构和物种多样性,以及底栖游泳生物和大型藻类碎屑的丰度。然后,我们将这些峡湾区域与三个深度相似的开阔陆架站点进行对比。与北极地区的预测相反,WAP峡湾盆地的底栖大型动物丰度比开阔陆架高3至38倍,并且从峡湾外部到内部,当地物种多样性和营养复杂性仍然很高。此外,WAP峡湾拥有独特的物种组成,对WAP沿线400 - 700米深度的β和γ多样性有显著贡献。与开阔陆架相比,WAP峡湾中的底栖游泳生物和大型藻类碎屑的丰度也显著更高。我们得出结论,由于融水影响较弱、沉积干扰较小以及食物输入丰富多样,WAP峡湾是底栖生物丰度和生物多样性的重要热点地区。我们推测,WAP峡湾与北极地区的峡湾显著不同,因为它们处于气候变暖的早期阶段,并且WAP沿线的快速变暖将增加融水和沉积物输入,对这些生物多样性热点地区产生有害影响。由于WAP峡湾还为南极磷虾和须鲸提供了重要的栖息地和觅食区域,因此迫切需要更好地了解WAP亚极地峡湾生态系统的结构、动态和气候敏感性。

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