湖北高分辨率石笋记录的DO18事件特征

张伟宏; 廖泽波; 陈仕涛; 邵庆丰; 段福才; 朱丽东; 王天阳

doi:10.14027/j.issn.1000-0550.2018.051

ISSN 1000-0550 CN 62-1038/P

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湖北高分辨率石笋记录的DO18事件特征

张伟宏, 廖泽波, 陈仕涛, 邵庆丰, 段福才, 朱丽东, 王天阳

文章导航 > 沉积学报 > 2018 > 36(4): 674-683

张伟宏, 廖泽波, 陈仕涛, 邵庆丰, 段福才, 朱丽东, 王天阳. 湖北高分辨率石笋记录的DO18事件特征[J]. 沉积学报, 2018, 36(4): 674-683. doi: 10.14027/j.issn.1000-0550.2018.051

引用本文:

ZHANG WeiHong, LIAO ZeBo, CHEN ShiTao, SHAO QingFeng, DUAN FuCai, ZHU LiDong, WANG TianYang. DO18 Event Depicted by a High-resolution Stalagmite Record from Yongxing Cave, Hubei Province[J]. Acta Sedimentologica Sinica, 2018, 36(4): 674-683. doi: 10.14027/j.issn.1000-0550.2018.051

Citation:

ZHANG WeiHong, LIAO ZeBo, CHEN ShiTao, SHAO QingFeng, DUAN FuCai, ZHU LiDong, WANG TianYang. DO18 Event Depicted by a High-resolution Stalagmite Record from Yongxing Cave, Hubei Province[J]. Acta Sedimentologica Sinica, 2018, 36(4): 674-683. doi: 10.14027/j.issn.1000-0550.2018.051

引用本文:

Citation:

ZHANG WeiHong, LIAO ZeBo, CHEN ShiTao, SHAO QingFeng, DUAN FuCai, ZHU LiDong, WANG TianYang. DO18 Event Depicted by a High-resolution Stalagmite Record from Yongxing Cave, Hubei Province[J]. Acta Sedimentologica Sinica, 2018, 36(4): 674-683. doi: 10.14027/j.issn.1000-0550.2018.051

湖北高分辨率石笋记录的DO18事件特征

doi: 10.14027/j.issn.1000-0550.2018.051

1.
浙江师范大学地理与环境科学学院, 浙江金华 321004;
2.
南京师范大学地理科学学院, 南京 210023

基金项目: 国家自然科学基金项目（41602350，41602181，41572340）；浙江省自然科学基金项目（LY16D010001）

详细信息

作者简介:
张伟宏,女,1987年出生,博士,讲师,全球气候环境变化,E-mail:zhangwh@zjnu.cn

中图分类号: P532

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DO18 Event Depicted by a High-resolution Stalagmite Record from Yongxing Cave, Hubei Province

1.
College of Geography and Environmental Sciences, Zhejiang Normal University, Jinhua, Zhejiang 321004, China;
2.
College of Geography Science, Nanjing Normal University, Nanjing 210023, China

Funds: National Natural Science Foundation of China, No. 41602350, 41602181, 41572340; Zhejiang Provincial Natural Science Foundation of China, No. LY16D010001

摘要

摘要: 研究冰量较大时期千年尺度事件的区域响应和结构特征有助于进一步理解和验证千年尺度事件的驱动机制。基于湖北永兴洞一支石笋的5个高精度²³⁰Th年龄和323个氧同位素数据，重建了Dansgaard-Oeschger（DO）18事件发生时高分辨率的东亚水文循环变化的过程和特征。结合同一洞穴另两支石笋记录，发现永兴洞石笋δ¹⁸O在~64.7 ka迅速负偏1.5‰，指示在MIS4阶段东亚季风区确实发生了持续时间较短的DO18事件。石笋δ¹⁸O结果精确标定了DO18事件的结束时间为~63.0 ka，结束过程呈现出5个百年尺度的季风增强振荡。在形态特征上，不同于格陵兰冰芯DO18事件的快速开始和快速结束（~60 a）的对称变化，季风区DO18事件呈现出快速增强但缓慢结束（持续达1500 a）的显著不对称特征。但是，石笋δ¹⁸O与北大西洋温盐环流（AMOC）变化在形态特征和持续时间上高度一致，暗示了AMOC对东亚季风区DO事件的重要调控作用。DO18事件时东亚季风与北大西洋气候的不同结构特征可归于高低纬气候系统对AMOC响应方式的差异。石笋δ¹⁸O功率谱结果呈现出208 a、150 a、52 a和14~12 a的变化周期，分别接近于太阳活动的207 a、149 a、57 a和11 a周期，说明在冰量较大的MIS4阶段太阳活动仍控制着东亚季风短尺度的波动。
- 石笋 /
- 高分辨率 /
- DO18 /
- 东亚季风 /
- AMOC
Abstract: It helps further understand and test forcing mechanisms behind millennial-scale events to decipher their regional responses and structures during the periods of large ice sheets. Using 323 stable oxygen isotope ratios and 5 ²³⁰Th ages of a stalagmite in Yongxing Cave, central China, we reconstruct a detailed history of the East Asian hydrological cycle during the time span surrounding the Dansgaard-Oeschger (DO) 18 event. The calcite δ¹⁸O profile, together with another two stalagmite records from the same cave, shows a rapid decrease of 1.5‰ at~64.7 ka, confirming the occurrence of DO18 in the East Asian monsoon (EAM) region. The ending limb of DO18 in the EAM regime is characterized by five centennial-scale monsoon enhancing events, and finally culminates at~63.0 ka. Divergent from a rapid temperature increasing followed by a similarly rapid cooling (~60 a) back to stadial environments of the Greenland DO18 event, the DO18 event in the monsoon region exhibits a significant asymmetric feature with a sharp EAM strengthening but then a smoothing, lasting 1 500 a, decrease. Nonetheless, our stalagmite δ¹⁸O records mirror, in shape and timing, the variations of Atlantic meridional overturning circulation (AMOC) estimated by the ratio of ²³¹Pa/²³⁰Th and recovered from the deep western North Atlantic. This similarity suggests that the AMOC played an important role in regulating the DO18 event in the EAM region. On the other hand, the discrepancy in the pattern of DO18 between the EAM and the North Atlantic climate systems can be attributed to the different regional response to the AMOC change in the high-and low-latitude climate systems. Spectral analysis of the stalagmite δ¹⁸O record denotes significant cycles at the 90% confidence level at 208, 150, 52 and 14-12 a, close to the previously reported solar cycles at 207, 149, 57 and 11 a. This consistency of cyclical variabilities between the EASM intensity and solar activity might indicate that solar forcing of centennial-and decadal-scale EASM variation still existed during the MIS4 interval with larger ice volumes.
- stalagmite /
- high resolution /
- DO18 /
- EAM /
- AMOC

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[1]	陈公哲, 陈仕涛, 刘笑, 赵侃, 王真军, 张振球, 汪永进. 倒数第三次冰消期气候变化的石笋多指标分析 . 沉积学报, 2023, 41(4): 992-1001. doi: 10.14027/j.issn.1000-0550.2022.020
[2]	张振球, 张伟宏, 刘树双, 翟秀敏, 邵庆丰. 贵州石笋记录的中晚全新世东亚夏季风变化 . 沉积学报, 2023, 41(1): 196-205. doi: 10.14027/j.issn.1000-0550.2021.077
[3]	张晗, 黄伟, 蒋莹, 陈子元, 沈川洲, 董进国. 亚洲夏季风DO12气候事件的响应模式 . 沉积学报, 2022, 40(3): 765-773. doi: 10.14027/j.issn.1000-0550.2021.005
[4]	陈剑舜, 张伟宏, 陈仕涛, 邵庆丰, 赵侃, 尹敬文, 朱丽东. 小冰期气候的湖北石笋碳同位素记录 . 沉积学报, 2020, 38(3): 497-504. doi: 10.14027/j.issn.1000-0550.2019.058
[5]	车印平, 肖海燕, 崔梦月, 姜修洋, 蔡炳贵. 闽西仙云洞石笋记录的Heinrich2事件年龄及亚旋回特征 . 沉积学报, 2018, 36(6): 1139-1147. doi: 10.14027/j.issn.1000-0550.2018.143
[6]	张华生, 殷建军, 程海, R Lawrence Edwards, 林玉石, 唐伟, 杨会, 涂林玲, 王华, 潘谋成, 吴夏. 全新世早期弱夏季风事件的精确定位及机制探讨——以湖南莲花洞LHD5石笋为例 . 沉积学报, 2016, 34(2): 281-291. doi: 10.14027/j.cnki.cjxb.2016.02.007
[7]	张银环, 杨琰, 杨勋林, 殷建军, 黄帆, 任小凤, 赵景耀, 刘肖, 聂旭东. 早全新世季风演化的高分辨率石笋δ¹⁸O记录研究——以河南老母洞石笋为例 . 沉积学报, 2015, 33(1): 134-141. doi: 10.14027/j.cnki.cjxb.2015.01.014
[8]	. 长江口泥质区沉积物颜色反射率指示的近百年来东亚季风变迁 . 沉积学报, 2013, 31(2): 331-339.
[9]	蒋凌志. 松辽南部四方坨子地区井-震统一的高分辨率层序划分与对比 . 沉积学报, 2009, 27(3): 470-478.
[10]	. 末次间冰期东亚季风气候不稳定的神农架洞穴石笋记录 . 沉积学报, 2008, 26(1): 139-143.
[11]	管清玉. 末次冰期东亚季风快速波动的模式与成因 . 沉积学报, 2007, 25(3): 429-436.
[12]	淡卫东. 川西白马庙气田上侏罗统蓬莱镇组高分辨率层序地层对比 . 沉积学报, 2007, 25(5): 708-715.
[13]	刘殿兵. 神农架天鹅洞石笋76～58 kaB.P.时段DO事件 . 沉积学报, 2007, 25(1): 131-138.
[14]	. 岩溶地区现代土壤与洞穴石笋中单甲基支链烷烃与烷基环己烷对比研究 . 沉积学报, 2006, 24(05): 740-746.
[15]	张美良. 贵州荔波地区2000年来石笋高分辨率的气候记录 . 沉积学报, 2006, 24(3): 339-348.
[16]	郑荣才, 彭军. 陕北志丹三角洲长6油层组高分辨率层序分析与等时对比 . 沉积学报, 2002, 20(1): 92-100.
[17]	张美良, 袁道先, 林玉石, 覃嘉铭. 贵州荔波董哥洞3号石笋的同位素年龄及古气候信息 . 沉积学报, 2001, 19(3): 425-432.
[18]	张美良, 林玉石, 覃嘉铭. 桂林水南洞石笋的沉积学特征 . 沉积学报, 1999, 17(2): 233-239.
[19]	王兆荣, 支霞臣, 张汉昌. 杭州地区石笋稳定同位素古气候探索 . 沉积学报, 1997, 15(1): 77-79.
[20]	李平, 彭子成, 文启彬, 李玉成, 杨辉, 洪阿实, 许志峰, 王明亮, 业渝光, 和杰, 刁少波. 福建宁化天鹅洞石笋年代和古温度 . 沉积学报, 1996, 14(1): 149-155.

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湖北高分辨率石笋记录的DO18事件特征

doi: 10.14027/j.issn.1000-0550.2018.051

1. 浙江师范大学地理与环境科学学院, 浙江金华 321004;

2. 南京师范大学地理科学学院, 南京 210023

基金项目: 国家自然科学基金项目（41602350，41602181，41572340）；浙江省自然科学基金项目（LY16D010001）

作者简介:
张伟宏,女,1987年出生,博士,讲师,全球气候环境变化,E-mail:zhangwh@zjnu.cn

收稿日期: 2017-05-24
修回日期: 2017-08-31
刊出日期: 2018-08-10

中图分类号: P532

关键词:

石笋 /

高分辨率 /

DO18 /

东亚季风 /

AMOC

摘要: 研究冰量较大时期千年尺度事件的区域响应和结构特征有助于进一步理解和验证千年尺度事件的驱动机制。基于湖北永兴洞一支石笋的5个高精度²³⁰Th年龄和323个氧同位素数据，重建了Dansgaard-Oeschger（DO）18事件发生时高分辨率的东亚水文循环变化的过程和特征。结合同一洞穴另两支石笋记录，发现永兴洞石笋δ¹⁸O在~64.7 ka迅速负偏1.5‰，指示在MIS4阶段东亚季风区确实发生了持续时间较短的DO18事件。石笋δ¹⁸O结果精确标定了DO18事件的结束时间为~63.0 ka，结束过程呈现出5个百年尺度的季风增强振荡。在形态特征上，不同于格陵兰冰芯DO18事件的快速开始和快速结束（~60 a）的对称变化，季风区DO18事件呈现出快速增强但缓慢结束（持续达1500 a）的显著不对称特征。但是，石笋δ¹⁸O与北大西洋温盐环流（AMOC）变化在形态特征和持续时间上高度一致，暗示了AMOC对东亚季风区DO事件的重要调控作用。DO18事件时东亚季风与北大西洋气候的不同结构特征可归于高低纬气候系统对AMOC响应方式的差异。石笋δ¹⁸O功率谱结果呈现出208 a、150 a、52 a和14~12 a的变化周期，分别接近于太阳活动的207 a、149 a、57 a和11 a周期，说明在冰量较大的MIS4阶段太阳活动仍控制着东亚季风短尺度的波动。

English Abstract

DO18 Event Depicted by a High-resolution Stalagmite Record from Yongxing Cave, Hubei Province

1. College of Geography and Environmental Sciences, Zhejiang Normal University, Jinhua, Zhejiang 321004, China;

2. College of Geography Science, Nanjing Normal University, Nanjing 210023, China

Funds: National Natural Science Foundation of China, No. 41602350, 41602181, 41572340; Zhejiang Provincial Natural Science Foundation of China, No. LY16D010001

Received Date: 2017-05-24
Rev Recd Date: 2017-08-31
Publish Date: 2018-08-10

Keywords:

stalagmite /
high resolution /
DO18 /
EAM /
AMOC

Abstract: It helps further understand and test forcing mechanisms behind millennial-scale events to decipher their regional responses and structures during the periods of large ice sheets. Using 323 stable oxygen isotope ratios and 5 ²³⁰Th ages of a stalagmite in Yongxing Cave, central China, we reconstruct a detailed history of the East Asian hydrological cycle during the time span surrounding the Dansgaard-Oeschger (DO) 18 event. The calcite δ¹⁸O profile, together with another two stalagmite records from the same cave, shows a rapid decrease of 1.5‰ at~64.7 ka, confirming the occurrence of DO18 in the East Asian monsoon (EAM) region. The ending limb of DO18 in the EAM regime is characterized by five centennial-scale monsoon enhancing events, and finally culminates at~63.0 ka. Divergent from a rapid temperature increasing followed by a similarly rapid cooling (~60 a) back to stadial environments of the Greenland DO18 event, the DO18 event in the monsoon region exhibits a significant asymmetric feature with a sharp EAM strengthening but then a smoothing, lasting 1 500 a, decrease. Nonetheless, our stalagmite δ¹⁸O records mirror, in shape and timing, the variations of Atlantic meridional overturning circulation (AMOC) estimated by the ratio of ²³¹Pa/²³⁰Th and recovered from the deep western North Atlantic. This similarity suggests that the AMOC played an important role in regulating the DO18 event in the EAM region. On the other hand, the discrepancy in the pattern of DO18 between the EAM and the North Atlantic climate systems can be attributed to the different regional response to the AMOC change in the high-and low-latitude climate systems. Spectral analysis of the stalagmite δ¹⁸O record denotes significant cycles at the 90% confidence level at 208, 150, 52 and 14-12 a, close to the previously reported solar cycles at 207, 149, 57 and 11 a. This consistency of cyclical variabilities between the EASM intensity and solar activity might indicate that solar forcing of centennial-and decadal-scale EASM variation still existed during the MIS4 interval with larger ice volumes.

引用本文:

Citation:

ZHANG WeiHong, LIAO ZeBo, CHEN ShiTao, SHAO QingFeng, DUAN FuCai, ZHU LiDong, WANG TianYang. DO18 Event Depicted by a High-resolution Stalagmite Record from Yongxing Cave, Hubei Province[J]. Acta Sedimentologica Sinica, 2018, 36(4): 674-683. doi: 10.14027/j.issn.1000-0550.2018.051

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湖北高分辨率石笋记录的DO18事件特征

doi: 10.14027/j.issn.1000-0550.2018.051

作者简介:
张伟宏,女,1987年出生,博士,讲师,全球气候环境变化,E-mail:zhangwh@zjnu.cn

计量

DO18 Event Depicted by a High-resolution Stalagmite Record from Yongxing Cave, Hubei Province

计量

目录

湖北高分辨率石笋记录的DO18事件特征

doi: 10.14027/j.issn.1000-0550.2018.051

1. 浙江师范大学地理与环境科学学院, 浙江金华 321004;

2. 南京师范大学地理科学学院, 南京 210023

作者简介:
张伟宏,女,1987年出生,博士,讲师,全球气候环境变化,E-mail:zhangwh@zjnu.cn

English Abstract

DO18 Event Depicted by a High-resolution Stalagmite Record from Yongxing Cave, Hubei Province

1. College of Geography and Environmental Sciences, Zhejiang Normal University, Jinhua, Zhejiang 321004, China;

2. College of Geography Science, Nanjing Normal University, Nanjing 210023, China

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湖北高分辨率石笋记录的DO18事件特征

doi: 10.14027/j.issn.1000-0550.2018.051

作者简介: 张伟宏,女,1987年出生,博士,讲师,全球气候环境变化,E-mail:zhangwh@zjnu.cn

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DO18 Event Depicted by a High-resolution Stalagmite Record from Yongxing Cave, Hubei Province

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出版历程

目录

湖北高分辨率石笋记录的DO18事件特征

doi: 10.14027/j.issn.1000-0550.2018.051

1. 浙江师范大学地理与环境科学学院, 浙江金华 321004; 2. 南京师范大学地理科学学院, 南京 210023

作者简介: 张伟宏,女,1987年出生,博士,讲师,全球气候环境变化,E-mail:zhangwh@zjnu.cn

English Abstract

DO18 Event Depicted by a High-resolution Stalagmite Record from Yongxing Cave, Hubei Province

1. College of Geography and Environmental Sciences, Zhejiang Normal University, Jinhua, Zhejiang 321004, China; 2. College of Geography Science, Nanjing Normal University, Nanjing 210023, China

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
张伟宏,女,1987年出生,博士,讲师,全球气候环境变化,E-mail:zhangwh@zjnu.cn

1. 浙江师范大学地理与环境科学学院, 浙江金华 321004;

2. 南京师范大学地理科学学院, 南京 210023

作者简介:
张伟宏,女,1987年出生,博士,讲师,全球气候环境变化,E-mail:zhangwh@zjnu.cn

1. College of Geography and Environmental Sciences, Zhejiang Normal University, Jinhua, Zhejiang 321004, China;

2. College of Geography Science, Nanjing Normal University, Nanjing 210023, China