普氏原羚(Procapraprzewalskii)是青藏高原特有濒危物种,仅分布在青海湖周边区域,其生境动态变化对高原生态系统稳定性具有重要指示作用。研究气候变化对普氏原羚适生区及生境偏移的影响对于保护区域物种多样性、维持生态系统功能完整...普氏原羚(Procapraprzewalskii)是青藏高原特有濒危物种,仅分布在青海湖周边区域,其生境动态变化对高原生态系统稳定性具有重要指示作用。研究气候变化对普氏原羚适生区及生境偏移的影响对于保护区域物种多样性、维持生态系统功能完整性具有重要意义。本研究基于青海湖周边区域(共和县、海晏县、刚察县、天峻县、乌兰县和湟源县)野外调查和文献检索的物种分布记录(共计194个分布点位),选取适宜普氏原羚生境特征的环境变量构建最大熵(MaxEnt)模型,分析普氏原羚的适宜生境、识别栖息地斑块之间物种扩散的重要潜在路径,并结合第六次国际耦合模式比较计划(Coupled Model Intercomparison Project,CMIP6)中的4种共享社会经济路径(SSP126、SSP245、SSP370、SSP585)预测未来中期(2041-2060年)、远期(2061-2080年)普氏原羚的适宜分布区域,探求普氏原羚对气候变化响应的空间格局。结果表明:①MaxEnt模型预测普氏原羚适生分布区精度达到较高水平,模型ROC曲线下面积AUC均值达0.984。②当前气候条件下,研究区普氏原羚高适生区面积为1997.8 km^(2),占研究区总面积的2.85%,主要分布在青海湖东北区域、天峻县与乌兰县交界区域以及共和县西南区域。这3个区域之间存在较大的地理距离,基于生态廊道分析,青海湖东北区域通往共和县西南区域的生态廊道数量较多,普氏原羚迁徙较容易。③与当前气候条件相比,2041-2060年,在SSP126、SSP245、SSP370、SSP585四种温室气体排放情景下,普氏原羚适生面积缩小,高适生区域质心向西偏移;2061-2080年,高适生区域质心向北(高纬度)偏移,普氏原羚适生面积缩小明显。研究显示,伴随着气候的变化,普氏原羚适宜生境面积出现不同程度的减小趋势,需采取适应气候变化的预警保护措施。展开更多
During the years 2006–2009,lakes in the Qinghai-Tibetan Plateau(QTP)were investigated using satellite remote sensing strategies.We report the results of this investigation as well as follow-up research and expanded w...During the years 2006–2009,lakes in the Qinghai-Tibetan Plateau(QTP)were investigated using satellite remote sensing strategies.We report the results of this investigation as well as follow-up research and expanded work.For the investigation,we mainly focused on lakes whose areas are more than 1 km2.The remote sensing data that we used included 408 scenes of CBERS CCD images and 5 scenes of Landsat ETM?images in Qinghai Province and Tibet Autonomous Region.All these data were acquired around years 2005–2006.Besides remote sensing images,we also collected 1,259 topographic maps.Numbers and areas of lakes were analyzed statistically,which were then compared with those coming from the first lake investigation(implemented between the1960s and 1980s).According to our investigation,up to and around year 2005–2006,the total number of lakes in the QTP was 1,055(222 in Qinghai and 833 in Tibet),accounting for more than 30%of that of China.Thirty newborn lakes with area[1 km2were found,and 5 dead lakes with initial area[1 km2were also found.Among those 13 big lakes([500 km2),Yamzhog Yumco had seriously shrunk,and it has continued to shrink in recent years;Qinghai Lake had shrunk during the period,but some new researches indicated that it has been expanding since the year 2004;Siling Co,Nam Co,and Chibuzhang Co had expanded in the period.We divided the newborn lakes into six categories according to their forming reasons,including river expansion,wetland conversion,etc.The changes of natural conditions led to the death of four lakes,and human exploitation was the main reason for the death of Dalianhai Lake in Qinghai.We picked out three regions which were sensitive to the change of climate and ecological environment:Nagqu Region,Kekexili Region,and the source area of the Yellow River(SAYR).Lakes in both Nagqu and Kekexili have been expanded;meanwhile,most lakes in the SAYR have obviously been shrunk.These regional patterns of lake changes were highly related to variations of temperature,glacier,precipitation,and evaporation.Our investigation and analysis will provide references for researches related to lake changes in the QTP and the response to climate fluctuations.展开更多
Through comprehensive research on the various geophysical and geological data acquired recently, we consider that the Chasang area in the western uplift of Qiangtang is a huge south-dipping block which is overlapped b...Through comprehensive research on the various geophysical and geological data acquired recently, we consider that the Chasang area in the western uplift of Qiangtang is a huge south-dipping block which is overlapped by several east-west trending blocks rather than a simple and palaeo-doming existing for a long time. The structural and geophysical features of the area, which only alone limited between Shuanghu and Rongma districts, are of no regional significance. Their development is closely related with the approximately south-north trending transform faults developed during the Mesozoic era on the east and west sides of the area and their later continuous movement. The compressing, overlapping and uplifting of the Chasang area began at the stage of reversing of the Qiangtang Basin during the Lower Cretaceous, which is in direct relation with Bangonghu-Dingqing limited ocean's closure and the convergence of the neighboring blocks. The compression and overlapping of the area have further developed and reformed展开更多
文摘普氏原羚(Procapraprzewalskii)是青藏高原特有濒危物种,仅分布在青海湖周边区域,其生境动态变化对高原生态系统稳定性具有重要指示作用。研究气候变化对普氏原羚适生区及生境偏移的影响对于保护区域物种多样性、维持生态系统功能完整性具有重要意义。本研究基于青海湖周边区域(共和县、海晏县、刚察县、天峻县、乌兰县和湟源县)野外调查和文献检索的物种分布记录(共计194个分布点位),选取适宜普氏原羚生境特征的环境变量构建最大熵(MaxEnt)模型,分析普氏原羚的适宜生境、识别栖息地斑块之间物种扩散的重要潜在路径,并结合第六次国际耦合模式比较计划(Coupled Model Intercomparison Project,CMIP6)中的4种共享社会经济路径(SSP126、SSP245、SSP370、SSP585)预测未来中期(2041-2060年)、远期(2061-2080年)普氏原羚的适宜分布区域,探求普氏原羚对气候变化响应的空间格局。结果表明:①MaxEnt模型预测普氏原羚适生分布区精度达到较高水平,模型ROC曲线下面积AUC均值达0.984。②当前气候条件下,研究区普氏原羚高适生区面积为1997.8 km^(2),占研究区总面积的2.85%,主要分布在青海湖东北区域、天峻县与乌兰县交界区域以及共和县西南区域。这3个区域之间存在较大的地理距离,基于生态廊道分析,青海湖东北区域通往共和县西南区域的生态廊道数量较多,普氏原羚迁徙较容易。③与当前气候条件相比,2041-2060年,在SSP126、SSP245、SSP370、SSP585四种温室气体排放情景下,普氏原羚适生面积缩小,高适生区域质心向西偏移;2061-2080年,高适生区域质心向北(高纬度)偏移,普氏原羚适生面积缩小明显。研究显示,伴随着气候的变化,普氏原羚适宜生境面积出现不同程度的减小趋势,需采取适应气候变化的预警保护措施。
基金supported by the National Key Basic Research Program on Global Change of China(2011CB952001)the National Key Basic Research Special Foundation of China(2006FY1106000)the Project Funded by the Priority Academic Program Development of Jiangsu Higher Education Institutions(PAPD)and the Open Fund Program of the State Key Laboratory of RemoteSensing Science,China(OFSLRSS201112)
文摘During the years 2006–2009,lakes in the Qinghai-Tibetan Plateau(QTP)were investigated using satellite remote sensing strategies.We report the results of this investigation as well as follow-up research and expanded work.For the investigation,we mainly focused on lakes whose areas are more than 1 km2.The remote sensing data that we used included 408 scenes of CBERS CCD images and 5 scenes of Landsat ETM?images in Qinghai Province and Tibet Autonomous Region.All these data were acquired around years 2005–2006.Besides remote sensing images,we also collected 1,259 topographic maps.Numbers and areas of lakes were analyzed statistically,which were then compared with those coming from the first lake investigation(implemented between the1960s and 1980s).According to our investigation,up to and around year 2005–2006,the total number of lakes in the QTP was 1,055(222 in Qinghai and 833 in Tibet),accounting for more than 30%of that of China.Thirty newborn lakes with area[1 km2were found,and 5 dead lakes with initial area[1 km2were also found.Among those 13 big lakes([500 km2),Yamzhog Yumco had seriously shrunk,and it has continued to shrink in recent years;Qinghai Lake had shrunk during the period,but some new researches indicated that it has been expanding since the year 2004;Siling Co,Nam Co,and Chibuzhang Co had expanded in the period.We divided the newborn lakes into six categories according to their forming reasons,including river expansion,wetland conversion,etc.The changes of natural conditions led to the death of four lakes,and human exploitation was the main reason for the death of Dalianhai Lake in Qinghai.We picked out three regions which were sensitive to the change of climate and ecological environment:Nagqu Region,Kekexili Region,and the source area of the Yellow River(SAYR).Lakes in both Nagqu and Kekexili have been expanded;meanwhile,most lakes in the SAYR have obviously been shrunk.These regional patterns of lake changes were highly related to variations of temperature,glacier,precipitation,and evaporation.Our investigation and analysis will provide references for researches related to lake changes in the QTP and the response to climate fluctuations.
文摘Through comprehensive research on the various geophysical and geological data acquired recently, we consider that the Chasang area in the western uplift of Qiangtang is a huge south-dipping block which is overlapped by several east-west trending blocks rather than a simple and palaeo-doming existing for a long time. The structural and geophysical features of the area, which only alone limited between Shuanghu and Rongma districts, are of no regional significance. Their development is closely related with the approximately south-north trending transform faults developed during the Mesozoic era on the east and west sides of the area and their later continuous movement. The compressing, overlapping and uplifting of the Chasang area began at the stage of reversing of the Qiangtang Basin during the Lower Cretaceous, which is in direct relation with Bangonghu-Dingqing limited ocean's closure and the convergence of the neighboring blocks. The compression and overlapping of the area have further developed and reformed
