Heinrich event 4 and Dansgaard/Oeschger events 5–10 recorded by high-resolution speleothem oxygen isotope data from central China

• Published in: Quaternary Research
• Main Authors: Zhou, Houyun, Zhao, Jian-xin, Feng, Yuexing, Chen, Qiong, Mi, Xiaojian, Shen, Chuan-Chou, He, Haibo, Yang, Liang, Liu, Shuhua, Chen, Lin, Huang, Jiayi, Zhu, Liyan
• Other Authors: NNSFC, Key Project of Guangdong Natural Science Foundation, State Key Laboratory of Loess and Quaternary Geology, Australian Research Council, ROC MOST
• Format: Article in Journal/Newspaper
• Language: English
• Published: Cambridge University Press (CUP) 2014
• Subjects: Dansgaard-Oeschger events
• Online Access: http://dx.doi.org/10.1016/j.yqres.2014.07.006; http://api.elsevier.com/content/article/PII:S0033589414000908?httpAccept=text/xml; http://api.elsevier.com/content/article/PII:S0033589414000908?httpAccept=text/plain; https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400000788

Abstract A 50-yr resolution reconstruction of climate and environment variability during the period 43–14 ka was developed using 26 high-precision U/Th dates and 390 oxygen isotope (δ 18 O) data of a stalagmite (SJ1) collected from Songjia Cave in central China, which is close to the northwestern boundary of the Asian summer monsoon (ASM). The δ 18 O record in SJ1 displays significant millennial-scale changes that correlate well in timing and duration with Dansgaard/Oeschger (D/O) events 5–10 and Heinrich event 4 (H4) identified in high-latitude regions of the Northern Hemisphere. Four 230 Th dates constrain the H4 event precisely to the period of 39.7 to 38.3 ka. Notable centennial variations of the ASM activity could be observed within the H4 event. The magnitude and duration of D/O event 4.1 recorded in SJ1 are similar to those archived in east China but different from those documented in southwest China, suggesting that the manifestation of this event may be regionally different. The timing, duration and structure of D/O events 5–10 and Heinrich event 4 suggest that temperature changes in both hemispheres have exerted significant influences on the ASM variations in central China.