从第三极到北极： 热喀斯特及其对碳循环影响研究进展
贾麟1(
), 范成彦1, 母梅1, 陈旭1, 仲文1, 尚建国2, 张凤1, 李丽丽3, 彭小清1, 牟翠翠1,4,5(), 张廷军1,5
), 范成彦1, 母梅1, 陈旭1, 仲文1, 尚建国2, 张凤1, 李丽丽3, 彭小清1, 牟翠翠1,4,5(), 张廷军1,5
Studies of thermokarst and its effects on ecosystem carbon cycle in the Third Polar regions and the Arctic
Lin JIA1(), Chengyan FAN1, Mei MU1, Xu CHEN1, Wen ZHONG1, Jianguo SHANG2, Feng ZHANG1, Lili LI3, Xiaoqing PENG1, Cuicui MU1,4,5(), Tingjun ZHANG1,5
), Chengyan FAN1, Mei MU1, Xu CHEN1, Wen ZHONG1, Jianguo SHANG2, Feng ZHANG1, Lili LI3, Xiaoqing PENG1, Cuicui MU1,4,5(), Tingjun ZHANG1,5
图1. 典型的热喀斯特地貌
（a）Retrogressive thaw slump over the Heihe River basin on the northeast of Qinghai-Tibet Plateau （QTP）；（b）The thermokarst lake at Tuotuohe in the center of QTP；（c）The Batagaika crater， thaw slump on eastern Russia［
Fig.1. Typical thermokarst landforms
