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4. 热融滑塌影响生态系统碳循环示意［
黑色箭头代表溶解性有机质的输入， 白色箭头代表垂直方向碳分配过程及温室气体释放过程
Fig.4. A schematic of thaw slumps influencing the ecosystem carbon cycle［
The black arrows represent the input of dissolved organic matter，and the white arrows represent the vertical carbon distribution process and the greenhouse gas emissions
