干旱区研究 ›› 2022, Vol. 39 ›› Issue (1): 10-20.doi: 10.13866/j.azr.2022.01.02
收稿日期:
2021-05-28
修回日期:
2021-10-08
出版日期:
2022-01-15
发布日期:
2022-01-24
作者简介:
田庆春(1982-),男,博士,副教授,研究方向为全球变化与第四纪环境演化. E-mail: 基金资助:
TIAN Qingchun1,2(),YIN Jianan1,HAO Xiaolong1
Received:
2021-05-28
Revised:
2021-10-08
Online:
2022-01-15
Published:
2022-01-24
摘要:
关于MIS3阶段的气候问题目前仍没有完全解决,需要更多区域的沉积记录分析。黄土被公认为第四纪气候研究的优秀载体,选择黄土高原东南缘的临汾盆地为研究区,通过对该区黄土沉积物磁化率、全铁、总有机碳和粒度系统研究,结合光释光年代学数据,初步讨论了MIS3阶段临汾盆地气候变化特征。MIS3阶段临汾盆地气候变化可分为3个阶段:56~45 ka BP气候为弱温湿,对应于MIS3c;45~41 ka BP呈现短暂的冷干,对应于MIS3b;41~25 ka BP表现为较强的温湿,对应于MIS3a。MIS3阶段全球气候表现出相对温湿,但临汾盆地在MIS3气候波动与其他地质记录表现出一定差异,造成这种结果的原因可能是在北半球冰盖和地表接收太阳辐射量共同作用下,热量和水分在各区域配置不同,导致各区域间表现出较大的环境差异,具体的耦合机制还需开展进一步研究工作。
田庆春,尹佳男,郝晓龙. 临汾盆地黄土沉积记录的MIS3气候变化[J]. 干旱区研究, 2022, 39(1): 10-20.
TIAN Qingchun,YIN Jianan,HAO Xiaolong. MIS3 climate change assessed according to loess deposition in the Linfen Basin, China[J]. Arid Zone Research, 2022, 39(1): 10-20.
表1
丁村剖面样品信息、环境剂量及OSL定年"
样品 | 深度/m | U /(mg·kg-1) | Th /(mg·kg-1) | K/% | 环境剂量率 /(Gy·ka-1) | 含水量/% | 测片 | 等效剂量/Gy | 年代/ka |
---|---|---|---|---|---|---|---|---|---|
DC1-1 | 1.35 | 2.46±0.4 | 11.41±0.7 | 2.03±0.04 | 3.85±0.20 | 15±7 | 6 | 160.61±2.74 | 41.8±2.4 |
DC3-1 | 3 | 2.20±0.4 | 12.21±0.7 | 2.12±0.04 | 3.87±0.20 | 15±7 | 6 | 247.30±13.38 | 63.9±5.0 |
DC5-1 | 4 | 2.17±0.4 | 12.34±0.7 | 2.16±0.04 | 3.87±0.21 | 15±7 | 6 | 279.23±7.88 | 72.1±4.6 |
DC7-1 | 5 | 2.04±0.4 | 10.26±0.7 | 1.94±0.04 | 3.53±0.19 | 15±7 | 6 | 345.19±8.10 | 97.8±6.0 |
DC8-1 | 5.5 | 1.86±0.3 | 11.09±0.7 | 1.93±0.04 | 4.09±0.24 | 15±7 | 6 | 449.59±20.94 | 110.0±8.7 |
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