地理研究 ›› 2014, Vol. 33 ›› Issue (6): 1167-1177.doi: 10.11821/dlyj201406016
郑秋凤, 张茂恒, 李吉均, 舒强, 陈晔, 萧家仪, 赵志军
收稿日期:
2013-10-10
修回日期:
2014-03-23
出版日期:
2014-06-10
发布日期:
2014-06-10
通讯作者:
赵志军(1973-),男,副教授,从事地貌学与第四纪地质学研究。E-mail:zhao1029@gmail.com
作者简介:
:郑秋凤(1987-),女,江苏常州人,博士研究生,从事气候变化研究。E-mail:zhengqf611@163.com
基金资助:
ZHENG Qiufeng, ZHANG Maoheng, LI Jijun, SHU Qiang, CHEN Ye, XIAO Jiayi, ZHAO Zhijun
Received:
2013-10-10
Revised:
2014-03-23
Online:
2014-06-10
Published:
2014-06-10
摘要: 运用孢粉浓缩物AMS 14C测年和氨基酸测年方法结合气候地层对比,建立神农架地区大九湖盆地DJH-2 孔的地层年代序列。依据孢粉分析结果并结合沉积环境,将大九湖盆地中更新世晚期以来的植被演替和古气候演化划分为六个阶段:① 275.0-188.0 ka,寒冷偏干,寒温带针叶林、高山草甸;② 245.0-188.0 ka,暖湿偏干,常绿、落叶阔叶混交林;③ 188.0-129.0 ka,冷干,寒温带针叶林为主,过渡为高山草甸为主;④ 129.0-71.8 ka,暖湿,暖温带落叶阔叶林;⑤71.8-15 ka,冷干,寒温带针叶林与高山草甸间隔发育,中间有喜暖种属增多的迹象;⑥ 15.0-1.0 ka,暖湿,亚热带常绿、落叶阔叶林。孢粉组合特征及单种属特征所显示的盆地气候变化反映了良好的全球冰期、间冰期气候旋回。孢粉浓度特征反映大九湖盆地气候变化受北半球高纬冰量与低纬太阳辐射的双重控制。
郑秋凤, 张茂恒, 李吉均, 舒强, 陈晔, 萧家仪, 赵志军. 大九湖钻孔记录的神农架地区中更新世晚期以来的气候环境变化[J]. 地理研究, 2014, 33(6): 1167-1177.
ZHENG Qiufeng, ZHANG Maoheng, LI Jijun, SHU Qiang, CHEN Ye, XIAO Jiayi, ZHAO Zhijun. The climate and environment change of Shennongjia area recorded in the core of Dajiuhu Basin since the late Middle Pleistocene[J]. GEOGRAPHICAL RESEARCH, 2014, 33(6): 1167-1177.
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