西藏中部是西风与季风相互作用的关键区域,对气候变化响应极为敏感。以该区域当惹雍错西北部T1阶地的沉积剖面为研究对象,利用光释光测年确立年代标尺,通过沉积物粒度、TOC、TN等代用指标分析,对当惹雍错地区中晚全新世以来的古气候变...西藏中部是西风与季风相互作用的关键区域,对气候变化响应极为敏感。以该区域当惹雍错西北部T1阶地的沉积剖面为研究对象,利用光释光测年确立年代标尺,通过沉积物粒度、TOC、TN等代用指标分析,对当惹雍错地区中晚全新世以来的古气候变化进行研究。结果显示,T1阶地代表了约6 ka BP^1.4 ka BP期间的湖相沉积;记录了该区域中晚全新世的两个主要气候阶段。阶段I(约6 ka BP^3.4 ka BP期间)气候温暖湿润,湖泊水位较高且稳定;阶段II(约3.4 ka BP^1.4 ka BP)气候朝着干冷方向发展,水位下降明显,并在2.4 ka BP左右达到最低水位。通过该剖面揭示的当惹雍错中晚全新世以来的气候变化与周边区域的湖泊沉积记录进行对比,表明该地区湿度变化受季风影响较为明显;为季风在高原上的作用范围提供了证据。展开更多
The lakes on the Tibetan Plateau(TP)account for 57%of the total lake area in China[1],which is a key component of the Asia water tower[2-4].A recent study showed that there are 1424 lakes greater than 1 km^(2) on the ...The lakes on the Tibetan Plateau(TP)account for 57%of the total lake area in China[1],which is a key component of the Asia water tower[2-4].A recent study showed that there are 1424 lakes greater than 1 km^(2) on the TP,while the total lake area reached 5.0-10^(4)±791.4 km^(2) in 2018[5].Most lakes on the TP are closed and are less disturbed by human activities than the other inland water bodies in China.展开更多
文摘西藏中部是西风与季风相互作用的关键区域,对气候变化响应极为敏感。以该区域当惹雍错西北部T1阶地的沉积剖面为研究对象,利用光释光测年确立年代标尺,通过沉积物粒度、TOC、TN等代用指标分析,对当惹雍错地区中晚全新世以来的古气候变化进行研究。结果显示,T1阶地代表了约6 ka BP^1.4 ka BP期间的湖相沉积;记录了该区域中晚全新世的两个主要气候阶段。阶段I(约6 ka BP^3.4 ka BP期间)气候温暖湿润,湖泊水位较高且稳定;阶段II(约3.4 ka BP^1.4 ka BP)气候朝着干冷方向发展,水位下降明显,并在2.4 ka BP左右达到最低水位。通过该剖面揭示的当惹雍错中晚全新世以来的气候变化与周边区域的湖泊沉积记录进行对比,表明该地区湿度变化受季风影响较为明显;为季风在高原上的作用范围提供了证据。
基金This work was supported by the Strategic Priority Research Program of Chinese Academy of Sciences(XDA19020303)the National Natural Science Foundation of China(41831177)+1 种基金the Second Tibetan Plateau Scientific Expedition and Research(2019QZKK0202)the Alliance of Field Observation Stations of Chinese Academy of Sciences(KFJ-SW-YW038).
文摘The lakes on the Tibetan Plateau(TP)account for 57%of the total lake area in China[1],which is a key component of the Asia water tower[2-4].A recent study showed that there are 1424 lakes greater than 1 km^(2) on the TP,while the total lake area reached 5.0-10^(4)±791.4 km^(2) in 2018[5].Most lakes on the TP are closed and are less disturbed by human activities than the other inland water bodies in China.