Mętrak Monika, Chachulski Łukasz, Navruzshoev Dovutsho, Pawlikowski Paweł, Rojan Elżbieta, Sulwiński Marcin, Suska-Malawska Małgorzata
Faculty of Biology, Biological and Chemical Research Centre, Department of Plant Ecology and Environmental Protection, University of Warsaw, Warsaw, Poland.
Warsaw University of Life Sciences, Faculty of Agriculture and Botany, Department of Botany, Warsaw, Poland.
PLoS One. 2017 Mar 30;12(3):e0174496. doi: 10.1371/journal.pone.0174496. eCollection 2017.
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.
位于中亚的帕米尔山脉东部,气候大陆性强且干旱。在这个恶劣地区形成的湿地仅限于泉水区域、浅湖阶地或河流沿岸的漫滩,它们提供了多种生态系统服务,比如作为水库、珍稀物种的避难所和家畜的牧场。这些生态系统对气候变化尤为敏感,帕米尔山脉的气候变化导致气温上升、多年冻土/冰川强烈融化以及降水模式改变。气候变化影响了山区的牧场管理,导致低海拔地区的牧场被过度利用。因此,气候和人为干扰都可能破坏东帕米尔高山湿地现有的生态平衡,对其生物多样性和当地居民的粮食安全构成严重风险。在此背景下,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)如何塑造东帕米尔山谷中盐生植物群落的分布和多样性。这项任务通过植被调查和对栖息地条件的综合分析来完成。所研究的湖阶地和漫滩被由土壤湿度和盐度差异决定的植物群落重复镶嵌覆盖。在较低、较湿润的地点,这种拼凑由以红褐草为主的盐沼、盐生小莎草草甸以及含有青藏嵩草和帕米尔报春的盐生草甸组成;在较干燥、较高的地点,则由含有短芒大麦草和碱茅属物种的特有草原以及旱生盐生植被斑块组成。帕米尔山脉水源的持续不稳定和夏季干旱可能导致上述湿地生态系统发生重大的结构和功能转变。对土壤湿度降低和/或土壤盐度增加更具耐受性的物种将会扩张,导致帕米尔湿地提供的生态系统服务发生改变。上述研究将有助于评估湿地的当前状态并预测其未来变化的方向。