石笋灰度和同位素对末次冰期气候事件的响应
王萌1,2,3(
), 陈仕涛1,2,3(), 黄琬淳1,2,3, 蔡雯沁4, 龚清霖1,2,3, 梁怡佳1,2,3, 王先锋5, 汪永进1,2,3
), 陈仕涛1,2,3(), 黄琬淳1,2,3, 蔡雯沁4, 龚清霖1,2,3, 梁怡佳1,2,3, 王先锋5, 汪永进1,2,3
The response of stalagmite gray-level and isotopes to the climatic events during the last glacial period
WANG Meng1,2,3(), CHEN Shi-tao1,2,3(), HUANG Wan-chun1,2,3, CAI Wen-qin4, GONG Qing-lin1,2,3, LIANG Yi-jia1,2,3, WANG Xian-feng5, WANG Yong-jin1,2,3
), CHEN Shi-tao1,2,3(), HUANG Wan-chun1,2,3, CAI Wen-qin4, GONG Qing-lin1,2,3, LIANG Yi-jia1,2,3, WANG Xian-feng5, WANG Yong-jin1,2,3
图3. 永兴洞石笋YX55 δ13C、δ18O、灰度深度序列及其剖面图
注：绿色曲线为YX55的δ13C深度序列,深绿色曲线为7点平滑;红色曲线为δ18O深度序列,深红色曲线为7点平滑曲线;灰色曲线为灰度深度序列,黑色曲线为7点平滑曲线;虚线和蓝色数字指示沉积旋回及其序号。
Fig. 3. The δ13C, δ18O and gray-level records and the polished section of YX55 stalagmite
