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Elevational Shifts of Freshwater Communities Cannot Catch up Climate Warming in the Himalaya

机译:喜马拉雅山淡水社区的快速变化无法赶上气候变暖

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Climate warming threatens biodiversity at global, regional and local levels by causing irreversible changes to species populations and biological communities. The Himalayan region is highly vulnerable to climate warming. This calls for efficient environmental management strategies because biodiversity monitoring is costly, particularly for the developing countries of the Himalaya. Species distribution modeling (SDM) represents a tool that can be used to identify vulnerable areas where biodiversity monitoring and conservation are required most urgently and can be prioritized. Here, we investigated the potential present-day community compositions of river invertebrates in the central and eastern Himalayas and predicted changes in community compositions in future decades using SDMs. We then quantified the climate-induced range shifts of benthic invertebrates along the elevational gradient and tested whether the predicted community shift is fast enough to fully compensate for the projected climate warming. Our model predicts future increases in benthic invertebrate taxonomic richness. Further, projected community shifts are characterized by the movement of warm-dwellers to higher elevations and losses in cold-dwellers. The predicted model shows that benthic invertebrate communities would not be able to compensate climate warming through uphill migration and thus would accumulate climatic debts. Our findings suggest that the ongoing warming effect would cause continued elevational range shifts of mountain river communities.
机译:气候变暖通过对物种种群和生物群落造成不可逆转的变化,威胁着全球,区域和地方各级的生物多样性。喜马拉雅地区极易受到气候变暖的影响。这要求采取有效的环境管理战略,因为生物多样性监测的成本很高,特别是对于喜马拉雅山的发展中国家而言。物种分布建模(SDM)代表一种工具,可用于识别最迫切需要生物多样性监测和保护并可以优先处理的脆弱地区。在这里,我们调查了喜马拉雅中部和东部地区河无脊椎动物的潜在当今社区组成,并使用SDM预测了未来几十年的社区组成变化。然后,我们量化了底栖无脊椎动物在海拔高度梯度上由气候引起的范围变化,并测试了预测的群落移动是否足够快以完全补偿预计的气候变暖。我们的模型预测了底栖无脊椎动物分类学丰富度的未来增长。此外,预计的社区迁移的特征是温暖的居民向更高海拔的迁徙以及寒冷居民的损失。预测模型表明,底栖无脊椎动物社区将无法通过上坡迁徙来补偿气候变暖,因此将积累气候债务。我们的发现表明,持续的变暖效应将导致山区河流社区的海拔高度范围不断变化。

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