DO4事件的精确定年及亚旋回特征: 来自福建龙岩仙云洞石笋的证据<sup>*</sup>

doi:10.7605/gdlxb.2020.04.045

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Abstract The Dansgaard-Oeschger event 4(DO4 event) is a significant warming event that occurred in the late Marine Isotope Stage 3. At present,there are different understandings about the detailed characteristics and internal structures of the DO4 event. Based on 6 precisely-dated ²³⁰Th ages and 188 oxygen isotope data of a stalagmite(No.XYⅢ-28)from the Xianyun Cave,Fujian Province,we present δ¹⁸O time series with an average resolution of 7 yr from 29.13 to 27.94 kyr B.P. Our new stalagmites δ¹⁸O records uncover the detailed processes of the DO4 event. The onset and end time of the DO4 event recorded by the stalagmite δ¹⁸O is 28.83±0.06 and 28.46±0.06 kyr B.P.,respectively, and the duration is 0.37±0.06 kyr. Differential with abrupt change of NGRIP ice core δ¹⁸O record at the onset of DO4 based on the GICC05 layer count time scale,the Xianyun Cave δ¹⁸O shows a relatively slow change. The Xianyun stalagmite δ¹⁸O values negatively shift by 0.4‰ within 145±60 yr,which indicates that the Xianyun Cave was likely affected by the ocean-atmosphere coupling of the tropical. In addition,the Xianyun stalagmite δ¹⁸O reveals a series of sub-million-scale summer monsoon enhancement events in and around the DO4 event,corresponding to the NGRIP ice core δ¹⁸O record and the Arabian Sea basin record. Our results suggest that the East Asian summer monsoon is related to the north-high latitude temperature and the ITCZ position changes on the sub-millennium-scale event.

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	Articles by authors
	Che Yin-Ping
	Xiao Hai-Yan
	Jiang Xiu-Yang
	Cai Bing-Gui

Key words： Dansgaard-Oeschger event 4 stalagmite East Asian Monsoon Xianyun Cave sub-cycles

Received: 26 April 2019

ZTFLH:

P532

Fund:Co-funded by the National Natural Science Foundation of China(No.41672170),Natural Science Foundation of Fujian Province,China(No.2017J01654),Program for New Century Excellent Talents in Fujian Province University and Program for Innovative Research Team of Fujian Normal University(No. IRTL1705)

Corresponding Authors: Xiao Hai-Yan,female,born in 1960,doctor,an associate professor of engineering,is mainly engaged in research on global change and region response. E-mail: xhy@fjnu.edu.cn. Jiang Xiu-Yang,male,born in 1981,doctor,professor,is mainly engaged in research on karst environment and past climate changes. E-mail: xyjiang@fjnu.edu.cn.

About author: Che Yin-Ping,male,born in 1992,a master degree candidate,is mainly engaged in research on global change and Quaternary. E-mail: 1204492631@qq.com.

Cite this article:

Che Yin-Ping,Xiao Hai-Yan,Jiang Xiu-Yang et al. Precise dating of the Dansgaard-Oeschger event 4 and its sub-cycles: Evidence from a stalagmite from Xianyun Cave in Longyan City,Fujian Province[J]. JOPC, 2020, 22(2): 377-384.

URL:

http://journal09.magtechjournal.com/gdlxb/EN/10.7605/gdlxb.2020.04.045 OR http://journal09.magtechjournal.com/gdlxb/EN/Y2020/V22/I2/377

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