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首页> 外文期刊>Marine ecology progress series >Ecological niche modelling of cold-water corals in the Southern Ocean (N Antarctic), present distribution and future projections due to temperature changes
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Ecological niche modelling of cold-water corals in the Southern Ocean (N Antarctic), present distribution and future projections due to temperature changes

机译:南大洋(南极)冷水珊瑚的生态位建模,温度变化引起的当前分布和未来预测

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An urgent necessity to understand the effect of climatic change on scleractinian coldwater coral (CWC) ecosystems has arisen due to increasing ocean warming and acidification over the last decades. Here, presence-absence records of 12 scleractinian CWC species from research expeditions and the literature were compiled and merged with model-generated pseudo-absence data and 14 environmental variables. The best-fitting results of 9 species distribution models (SDMs) were combined to an ensemble habitat suitability model for CWCs in the northern Southern Ocean (Weddell Sea and Antarctic Peninsula) by means of the open-source R package 'biomod2'. Furthermore, 2 future scenarios of increasing bottom sea temperature were used to investigate the spatial response of scleractinians to temperature change. The resulting (current scenario) potential ecological niches were evaluated with good to excellent statistical measures. The results predict that present areas of highest probability of CWC occurrence are around the Antarctic Peninsula, South Orkney Islands and Queen Maud Land, with preference to geomorphic features such as seamounts. The distribution of CWC habitats is mainly driven by distance to coast and ice shelves, bathymetry, benthic calcium carbonate, and temperature. Under warming conditions, CWCs are predicted to expand their distribution range by 6 and 10% in 2037 and 2150, respectively, compared to the present distribution. The future models using increased bottom temperature revealed a stable CWC distribution for most parts of the study area. However, habitat shifts are expected to the Filchner Trough region, the adjacent continental shelves, as well as to the eastern side of the Antarctic Peninsula.
机译:由于近几十年来海洋变暖和酸化增加,已经迫切需要了解气候变化对巩膜冷水珊瑚(CWC)生态系统的影响。在这里,从研究远征和文献中收集了12种Scleractinian CWC物种的不存在记录,并与模型生成的伪不存在数据和14个环境变量合并。通过开源R包“ biomod2”,将9种物种分布模型(SDM)的最佳拟合结果与南部海洋北部(Weddell海和南极半岛)的CWC的整体生境适宜性模型相结合。此外,还使用了两个未来海底温度升高的方案来研究巩膜菌对温度变化的空间响应。所产生的(当前情景)潜在的生态位已通过良好至极好的统计方法进行了评估。结果预测,目前发生CWC可能性最高的地区是南极半岛,南奥克尼群岛和毛德皇后地区,并且优先考虑海山等地貌特征。 CWC生境的分布主要受与海岸和冰架的距离,测深法,底碳酸钙和温度的影响。与目前的分布相比,预计在变暖的条件下,CWC在2037年和2150年的分布范围将分别扩大6%和10%。未来使用升高的底部温度的模型将在研究区域的大部分区域显示稳定的CWC分布。但是,栖息地将转移到Filchner槽地区,邻近的大陆架以及南极半岛的东部。

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