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Nature's patchwork: How water sources and soil salinity determine the distribution and structure of halophytic plant communities in arid environments of the Eastern Pamir

机译:大自然的拼凑而成:在帕米尔东部干旱环境中,水源和土壤盐分如何决定盐生植物群落的分布和结构

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摘要

The eastern part of the Pamir Mountains, located in Central Asia, is characterized by great climatic continentality and aridity. Wetlands developed in this hostile region are restricted to spring areas, terraces of shallow lakes or floodplains along rivers, and provide diversified ecosystem services e.g. as water reservoirs, refugia for rare species and pastures for domestic cattle. These ecosystems are particularly susceptible to climate changes, that in the Pamir Mountains result in increased temperatures, intense permafrost/glacial melt and alterations of precipitation patterns. Climatic changes affect pasture management in the mountains, causing overutilization of sites located at lower elevations. Thus, both climate and man-induced disturbances may violate the existing ecological equilibrium in high-mountain wetlands of the Eastern Pamir, posing a serious risk to their biodiversity and to food security of the local population. In this context, we sought to assess how environmental drivers (with special focus on soil features and potential water sources) shape the distribution and diversity of halophytic plant communities developed in valleys in the Eastern Pamir. This task was completed by means of a vegetation survey and comprehensive analyses of habitat conditions. The lake terraces and floodplains studied were covered by a repetitive mosaic of plant communities determined by differences in soil moisture and salinity. On lower, wetter sites, this patchwork was formed by Blysmus rufus dominated salt marshes, saline small sedge meadows and saline meadows with Kobresia royleana and Primula pamirica; and on drier, elevated sites, by endemic grasslands with Hordeum brevisubulatum and Puccinellia species and patches of xerohalophytic vegetation. Continuous instability of water sources and summer droughts occurring in the Pamir Mountains may lead to significant structural and functional transformations of described wetland ecosystems. Species more tolerant to decreased soil moisture and/or increased soil salinity will expand, leading to alterations of ecosystem services provided by the Pamirs’ wetlands. The described research will help to assess the current state of the wetlands and to predict directions of their future changes.
机译:帕米尔山脉东部位于中亚,具有巨大的气候大陆性和干旱性。在这个敌对地区开发的湿地仅限于春季地区,浅湖阶地或沿河的洪泛区,并提供多样化的生态系统服务,例如作为水库,稀有物种的避难所和家养牛的牧场。这些生态系统特别容易受到气候变化的影响,在帕米尔山区会导致温度升高,多年冻土/冰川融化以及降水模式的改变。气候变化影响山区的牧场管理,导致较低海拔地区的土地过度利用。因此,气候和人为干扰都可能破坏东帕米尔高原高山湿地现有的生态平衡,从而对其生物多样性和当地人口的粮食安全构成严重威胁。在这种情况下,我们试图评估环境驱动因素(特别关注土壤特征和潜在水源)如何影响东部帕米尔山谷中开发的盐生植物群落的分布和多样性。该任务通过植被调查和栖息地条件的综合分析完成。所研究的湖泊阶地和洪泛区覆盖着由土壤水分和盐分差异决定的植物群落的重复镶嵌。在下部较湿的地方,这种杂物是由野蔷薇(Blysmus rufus)主导的盐沼,盐碱小莎草草甸和盐碱草甸与小嵩草(Kobresia royleana)和报春花报春(primula pamirica)形成的。在较干燥的高地,由短草大麦和Puccinellia物种以及干盐生植物斑块的地方性草原组成。帕米尔山区的水资源持续不稳定和夏季干旱可能导致所述湿地生态系统发生重大的结构和功能转变。能够容忍土壤水分减少和/或土壤盐分增加的物种将会扩大,从而导致帕米尔高原湿地提供的生态系统服务发生变化。所描述的研究将有助于评估湿地的现状并预测其未来变化的方向。

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