早全新世季风演化的高分辨率石笋&delta;<sup>18</sup>O记录研究&mdash;&mdash;以河南老母洞石笋为例

张银环; 杨琰; 杨勋林; 殷建军; 黄帆; 任小凤; 赵景耀; 刘肖; 聂旭东

doi:10.14027/j.cnki.cjxb.2015.01.014

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

doi: 10.14027/j.cnki.cjxb.2015.01.014

张银环^1,2,
杨琰^1,2,,
杨勋林^1,2,
殷建军^1,2,
黄帆^1,2,
任小凤^1,2,
赵景耀^1,2,
刘肖^1,2,
聂旭东^1,2

1.
西南大学地理科学学院三峡库区生态与环境教育部重点实验室重庆 400715;
2.
西南大学地球化学与同位素实验室重庆 400715

基金项目: 国家自然科学基金(批准号:41372177,40902053,41272192)、高等学校博士学科点专项科研基金(编号:20090182120005)与教育部中央高校基本科研业务费基金(编号:XDJK2011B004)联合资助

详细信息

作者简介:
张银环女 1988年出生硕士研究生全球变化研究 E-mail: 1104134991@qq.com

通讯作者:
杨琰男副教授 E-mail: yy2954@gmail.com

中图分类号: P532

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文章访问数: 1164
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Early Holocene Monsoon Evolution of High-resolution Stalagmite δ¹⁸O Records: in Henan Laomu Cave

ZHANG YinHuan^1,2,
YANG Yan^{1,2
,},
YANG XunLin^1,2,
YIN JianJun^1,2,
HUANG Fan^1,2,
REN XiaoFeng^1,2,
ZHAO JingYao^1,2,
LIU Xiao^1,2,
NIE XuDong^1,2

1.
School of Geographical Sciences, Southwest University; Key Laboratory of the Three Gorges Reservoir Region's Eco-Environment, Chongqing University & Southwest University, Ministry of Education, Chongqing 400715;
2.
Laboratory of Geochemistry and Isotope, Southwest University, Chongqing 400715

摘要

摘要: 基于豫西老母洞LM2石笋8个高精度²³⁰Th年龄,449个氧碳同位素,建立了达十年际分辨率的8.2~10.9 ka B.P.亚洲季风变化的δ¹⁸O记录序列.老母洞石笋δ¹⁸O值最为偏负达-12.0‰,最偏正为-8.2‰,振幅达3.8‰.早全新世10.13~10.9 ka B.P.时段内,河南西部老母洞石笋和东石崖石笋,陕西九仙洞C996-2石笋δ¹⁸O曲线揭示该时段内季风稳定,而中国南方的衙门洞石笋、三宝洞石笋和极地冰芯GRIP记录揭示该时段季风逐渐增强;同时季风达到顶峰的时期也不相同,进一步说明中国南北方早全新世10.13~10.9 ka B.P.时段季风演变过程的差异,可能与中国南北方气候的响应机制有关.从早全新世平均分辨率10年的LM2石笋记录中识别出8.2 ka,9.5 ka,10.2 ka和10.9 ka显著弱季风事件,尤其是8.2 ka和9.5 ka事件.对比分析老母洞与已发表的高分辨率石笋δ¹⁸O记录发现:石笋所揭示的某些冷事件发生时间在亚洲季风区存在差异,主要表现在事件内部变化特征及趋势上.LM2石笋δ¹⁸O曲线并没有明显记录9.3 ka弱季风事件,而是在9.3~9.6 ka B.P.左右记录了一个弱季风事件,与DSY09(2009)、Y1、HS-4记录相似,表明在该时段内存在季风的减弱事件,但是氧同位素传输的复杂性,使其在南北方表现不同.此外,在LM2石笋δ¹⁸O的8.2 ka B.P.开始时段,氧同位素曲线阶段性下降,且变幅达3‰,与Zhang等研究万象洞石笋提出的“中国8 200阶段”吻合,表明中国北方地区的8.2 ka事件是阶段性的事件,而南方的石笋氧同位素记录揭示的8.2 ka事件并未表现出阶段性特征,其原因有待于更多北方高精度石笋记录来进一步研究.LM2石笋氧同位素记录进行功率谱分析发现:在短尺度上季风变化与太阳活动密切相关,这与近年来对早全新世极端气候变化研究的驱动机制是一致的,早全新世亚洲季风的演化与太阳活动变化引起的太阳辐射能量的变化和北半球高纬气候的变化状况有关.
- 石笋 /
- 亚洲季风 /
- &delta /
- ¹⁸O /
- 弱季风事件 /
- 太阳活动 /
- 老母洞
Abstract: Based on 8 U/Th dates, 449 oxygen and carbon isotopic data from stalagmite LM2 from Laomu Cave, West Henan Province, China, a record of the Asian monsoon inter- decadal resolution sequence during 8.2~10.9 ka B.P. was established. The minimum δ¹⁸O value is -12‰, the maximum value is -8.2‰ and the vibration amplitude reaches 3.8‰. In the 10.13~10.9 ka B.P. sessions of early Holocene, the stalagmites in Jiuxian Cave, Laomu Cave and Dongshiya Cave reveals that monsoon stable in the period, but the stalagmites of Yamen Cave and Sanbao Cave in the southern China, polar ice cores GRIP record monsoon gradually. Differences of monsoon process of evolution between north and south China in the period may be related to climate response mechanism on the North and South China. Stalagmites LM2 recorded 8.2 ka, 9.5 ka, 10.2 ka and 10.9 ka weak monsoon event. Comparisons of LM2 to previously published early Holocene records show significant phase differences. The record of 9.3 ka weak monsoon event is not obvious in LM-2 stalagmite δ¹⁸O curve, but it recorded a weak monsoon event in 9.3~9.6 ka B.P. and similar to DSY09 (2009), Y1, HS-4 record. This indicated there was a weakening monsoon event in this time. The complexity oxygen isotope transport make it the different performance in north and south. In addition, LM2 stalagmite records the beginning of 8.2 ka B.P., the oxygen isotope curve showing a decline stage, and luffing up to 3 ‰, with Zhang et al proposing China "8200 phase" agreement by studying similar Wanxiang Cave. Northern China stalagmite showed the 8.2 ka cold event was staged event, while the south records revealed no showing phase characteristics, the reason for this need to more northern precision stalagmite records for further studying. The LM2 correlate within errors with Greenland ice core records, illustrating Asian monsoon and the North Atlantic climate change have fast atmospheric transmission. The stalagmite in Laomu Cave record confirms earlier work that suggested that Asia Monsoon is closely related to solar activity. Early Holocene Asian monsoon related with changing in solar radiation energy and climate condition on the high northern latitudes.
- stalagmites /
- Asian Monsoon /
- &delta /
- ¹⁸O /
- weak monsoon events /
- solar activity /
- Laomu Cave

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参考文献(28)

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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

doi: 10.14027/j.cnki.cjxb.2015.01.014

作者简介:
张银环女 1988年出生硕士研究生全球变化研究 E-mail: 1104134991@qq.com

通讯作者:
杨琰男副教授 E-mail: yy2954@gmail.com

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Early Holocene Monsoon Evolution of High-resolution Stalagmite δ¹⁸O Records: in Henan Laomu Cave

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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

doi: 10.14027/j.cnki.cjxb.2015.01.014

1. 西南大学地理科学学院三峡库区生态与环境教育部重点实验室重庆 400715;

2. 西南大学地球化学与同位素实验室重庆 400715

作者简介:
张银环女 1988年出生硕士研究生全球变化研究 E-mail: 1104134991@qq.com

通讯作者: 杨琰男副教授 E-mail: yy2954@gmail.com

English Abstract

Early Holocene Monsoon Evolution of High-resolution Stalagmite δ¹⁸O Records: in Henan Laomu Cave

1. School of Geographical Sciences, Southwest University; Key Laboratory of the Three Gorges Reservoir Region's Eco-Environment, Chongqing University & Southwest University, Ministry of Education, Chongqing 400715;

2. Laboratory of Geochemistry and Isotope, Southwest University, Chongqing 400715

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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

doi: 10.14027/j.cnki.cjxb.2015.01.014

作者简介: 张银环 女 1988年出生 硕士研究生 全球变化研究 E-mail: 1104134991@qq.com

通讯作者: 杨琰 男 副教授 E-mail: yy2954@gmail.com

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Early Holocene Monsoon Evolution of High-resolution Stalagmite δ18O Records: in Henan Laomu Cave

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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

doi: 10.14027/j.cnki.cjxb.2015.01.014

1. 西南大学地理科学学院 三峡库区生态与环境教育部重点实验室 重庆 400715; 2. 西南大学地球化学与同位素实验室 重庆 400715

作者简介: 张银环 女 1988年出生 硕士研究生 全球变化研究 E-mail: 1104134991@qq.com

通讯作者: 杨琰 男 副教授 E-mail: yy2954@gmail.com

English Abstract

Early Holocene Monsoon Evolution of High-resolution Stalagmite δ18O Records: in Henan Laomu Cave

1. School of Geographical Sciences, Southwest University; Key Laboratory of the Three Gorges Reservoir Region's Eco-Environment, Chongqing University & Southwest University, Ministry of Education, Chongqing 400715; 2. Laboratory of Geochemistry and Isotope, Southwest University, Chongqing 400715

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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

作者简介:
张银环女 1988年出生硕士研究生全球变化研究 E-mail: 1104134991@qq.com

通讯作者:
杨琰男副教授 E-mail: yy2954@gmail.com

Early Holocene Monsoon Evolution of High-resolution Stalagmite δ¹⁸O Records: in Henan Laomu Cave

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

1. 西南大学地理科学学院三峡库区生态与环境教育部重点实验室重庆 400715;

2. 西南大学地球化学与同位素实验室重庆 400715

作者简介:
张银环女 1988年出生硕士研究生全球变化研究 E-mail: 1104134991@qq.com

通讯作者: 杨琰男副教授 E-mail: yy2954@gmail.com

Early Holocene Monsoon Evolution of High-resolution Stalagmite δ¹⁸O Records: in Henan Laomu Cave

1. School of Geographical Sciences, Southwest University; Key Laboratory of the Three Gorges Reservoir Region's Eco-Environment, Chongqing University & Southwest University, Ministry of Education, Chongqing 400715;

2. Laboratory of Geochemistry and Isotope, Southwest University, Chongqing 400715