冰川冻土 ›› 2021, Vol. 43 ›› Issue (3): 809-817.doi: 10.7522/j.issn.1000-0240.2021.0022
收稿日期:
2021-05-12
修回日期:
2021-06-10
出版日期:
2021-06-30
发布日期:
2021-05-18
通讯作者:
张军
E-mail:shenml19@lzu.edu.cn;zj@lzu.edu.cn
作者简介:
沈曼丽,硕士研究生,主要从事气候变化研究. E-mail: 基金资助:
Manli SHEN1(),Jun ZHANG1(
),Zhengchuang HUI2
Received:
2021-05-12
Revised:
2021-06-10
Online:
2021-06-30
Published:
2021-05-18
Contact:
Jun ZHANG
E-mail:shenml19@lzu.edu.cn;zj@lzu.edu.cn
摘要:
为了更深入研究黄土高原西部地区第四纪气候演化历史,选取已建立可靠年代的兰州黄河南岸西津黄土钻孔剖面为研究载体,应用CM-700D型分光测色计对等间距取样的417个样品进行实验分析,获得了过去2.2 Ma的兰州地区色度指标记录序列。结合剖面已有其他古气候代用指标,与周边已有记录及全球深海氧同位素记录对比,发现2.2 Ma以来兰州地区气候演化整体呈现阶段性逐渐冷干化趋势,可能反映了全球第四纪气候长期变冷的影响。此外,在1.24 Ma和0.43 Ma左右经历了两次重要气候事件,1.24 Ma事件之后东亚冬季风和夏季风同时发生了增强,与“昆黄运动”起始时间一致,表明该事件可能受到了青藏高原隆升驱动;而0.43 Ma事件则是对全球中布容气候转型事件(MBE)的响应。因而,黄土高原西部地区第四纪气候演化可能受青藏高原隆升和全球变冷的双重调控,二者对不同气候事件的影响不同。
中图分类号:
沈曼丽,张军,惠争闯. 兰州西津黄土色度指标记录的第四纪气候演化[J]. 冰川冻土, 2021, 43(3): 809-817.
Manli SHEN,Jun ZHANG,Zhengchuang HUI. Quaternary climate evolution recorded by loess chromatic proxy in Xijin, Lanzhou[J]. Journal of Glaciology and Geocryology, 2021, 43(3): 809-817.
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