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Human activity and climate change triggered the expansion of rocky desertification in the karst areas of Southwestern China

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Science China Earth Sciences 2021年第10期64卷 1761-1773页

作者： Chaojun CHEN Daoxian YUAN Hai CHENG Tsailuen YU chuanchou shen RLawrence EDWARDS Yao WU Siya XIAO Jian ZHANG Tao WANG Ran HUANG Ziqi LIU Tingyong LI Junyun LI Chongqing Key Laboratory of Karst Environment School of Geographical SciencesSouthwest UniversityChongqing 400715China Key Laboratory of Karst Dynamics MNRGuangxiInstitute of Karst GeologyChinese Academy of Geological SciencesGuilin 541004China Yunnan Key Laboratory of Plateau Geographical Processes&Environmental Changes Faculty of GeographyYunnan Normal UniversityKunming 650500China Institute of Global Environmental Change Xi’an Jiaotong UniversityXi’an 710049China High-precision Mass Spectrometry and Environment Change Laboratory(HISPEC) Department of GeosciencesTaiwan UniversityTaipei 10617China Research Center for Future Earth Taiwan UniversityTaipei 10617China Global Change Research Center Taiwan UniversityTaipei 10617China Department of Earth Sciences University of MinnesotaMinneapolisMN 55455USA Environnements et Paléoenvironnements Océaniques et Continentaux(EPOC) UMR CNRS 5805Universitéde BordeauxPessac 33600France School of Karst Science Guizhou Normal UniversityGuiyang 550001China

It is conducive to the sustainable development of human beings in karst regions to research the mechanism of karst rocky desertification(KRD)expansion.Whether the large-scale KRD in southwestern China is caused by climate change or human activities is still controversial.In this study,the evolution of the KRD in southwestern China over the past 2000 years was reconstructed through the high-precisionδ^(13)C record of stalagmites from Shijiangjun(SJJ)Cave,Guizhou Province,China.Theδ^(13)C of the stalagmites from SJJ Cave exhibited heavy values from the Medieval Warm Period(MWP)to the Little Ice Age(LIA).Furthermore,theδ^(13)C records of other stalagmites and tufa from southwestern China also showed the same significant heavy trend.Because the stalagmiteδ^(13)C could record the change of ecological environment,it indicated that the consistent change of the stalagmitesδ^(13)C may record the process of KRD expansion in the karst regions of southwestern China.During the MWP,the stronger Asian summer monsoon and the northward movement of the rain belt led to a dry period in southwestern China and a wet period in northern China.In contrast,it was wet in southwestern China and dry in northern China during the LIA.In addition,after the Jing-Kang event(JK event,AD1127)occurred at the end of the Northern Song dynasty,the political and economic center of China migrated to southern China for the first time,which changed the population distribution pattern of larger population in the north and smaller population in the south.Therefore,the expansion of KRD in southwestern China was exacerbated in the MWP due to the change of climate in southwestern China,the migration of a large number of people,wars,the large-scale reclamation of arable land,and the cultivation of large areas of crops.

关键词： Karst rocky desertification Jing-Kang event Stalagmiteδ13C record Medieval Warm Period Little Ice Age

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Stalagmite-inferred Holocene precipitation in northern Guizhou Province, China, and asynchronous termination of the Climatic Optimum in the Asian monsoon territory

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Chinese Science Bulletin 2012年第7期57卷 795-801页

作者： JIANG XiuYang HE YaoQi shen chuanchou KONG XingGong LI ZhiZhong CHANG YuWei Key Laboratory of Humid Subtropical Eco-geographical Processes Ministry of EducationCollege of Geography ScienceFujian Normal Uni-versityFuzhou 350007China College of Tourism and Air Service Guizhou Minzu UniversityGuiyang 550025China High-Precision Mass Spectrometry and Environment Change Laboratory(HISPEC) Department of GeosciencesTaiwan UniversityTaipei 106China College of Geography Science Nanjing Normal UniversityNanjing 210046China

An absolute-dated, bi-decadal-resolution, stalagmite oxygen-isotopic time series from Shigao Cave reveals the evolution of summer monsoon precipitation over the past 9.9 ka BP in northern Guizhou Province, Southwest China. The  18O-inferred climate conditions are divisible into three distinct stages: (1) a maximum humid era from 9.9-6.6 ka BP; (2) a gradual declining precipitation interval between 6.6-1.6 ka BP; and (3) a relatively low precipitation time window after 1.6 ka BP. Consistency of contemporaneous stalagmite Holocene 18O records between Shigao and other caves in the Indian and East Asian monsoon realms support the effect of primary orbital solar forcings on monsoonal precipitation. However, statistical analysis shows a significant spatial asynchroneity of the Holocene Optimum termination in the Asian monsoon territory. The Holocene Optimum ended at 7.2-7.4 ka BP in Oman, located in the Indian monsoon region, and at 5.6-5.8 ka BP in Central China, in the East Asian monsoon zone. In Southwest China, the termination occurred between these periods, at 6.6-7.0 ka BP, and was influenced by both monsoon systems. We propose that this spatially asynchronous ending of Holocene Optimum in Asia may be attributed to sea surface temperature changes in the western tropical Pacific, which is a primary moisture source for the East Asian monsoon.

关键词：中国西南地区亚洲季风区季风降水洞穴石笋气候条件全新世贵州省异步

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亚洲夏季风DO12气候事件的响应模式——来自山西石笋的证据

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沉积学报 2022年第3期40卷 765-773页

作者：张晗黄伟蒋莹陈子元沈川洲董进国南通大学地理科学学院江苏南通226007 宜春学院地理科学系江西宜春336000 台湾大学地质科学系中国台北10617

亚洲季风气候响应的Dansgaard-Oeschger(DO)事件模式是目前古气候研究的热点之一,其是否表现为单一模式,还是存在多种模式仍有争议。基于山西龙洞13个铀钍年代和239个氧同位素(δ^(18)O)数据重建了末次冰期48~41 ka B.P.时段东亚夏季风... 详细信息

亚洲季风气候响应的Dansgaard-Oeschger(DO)事件模式是目前古气候研究的热点之一,其是否表现为单一模式,还是存在多种模式仍有争议。基于山西龙洞13个铀钍年代和239个氧同位素(δ^(18)O)数据重建了末次冰期48~41 ka B.P.时段东亚夏季风演化历史。石笋L2清晰记录了H5、DO12和DO11等千年尺度气候事件,其变化特征与亚洲其他石笋记录呈现出良好的一致性,并与格陵兰冰芯记录一一对应,表明高、低纬之间紧密的气候联系。在DO12事件过程中,L2δ^(18)O值先是持续偏轻后又逐渐变重,指示亚洲夏季风强度持续增强后略有减弱,与格陵兰冰芯记录的温度持续降低模式迥异;不同区域记录对比发现,亚洲夏季风和热带低纬水文过程响应的DO12事件过程表现为不对称倒“V”形,这可能与南大洋潜热释放及越赤道气流强/弱变化、低纬热带辐合带逐步北进/南退有关。

关键词：末次冰期黄土高原石笋东亚夏季风 DO12事件

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黔北石笋记录的MIS 5d/5c季风突变过程

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科学通报 2014年第27期59卷 2698-2706页

作者：姜修洋王晓艳杨邦何尧启沈川洲李志忠福建师范大学地理科学学院湿润亚热带生态地理过程教育部重点实验室福州350007 贵州民族大学旅游与航空服务学院贵阳550025 台湾大学地质科学系高精度质谱与环境变迁实验室台北10617

基于黔北三星洞石笋（SX29）9个铀钍年龄和420个氧同位素分析,获得了113.6±0.3-106.2±0.4 ka BP（相对于1950年）10年际分辨率的δ18O时间序列.该石笋δ18O时间序列记录了MIS 5d/5c转换时亚洲夏季风强度变化的突变过程.根据突变过程... 详细信息

基于黔北三星洞石笋（SX29）9个铀钍年龄和420个氧同位素分析,获得了113.6±0.3-106.2±0.4 ka BP（相对于1950年）10年际分辨率的δ18O时间序列.该石笋δ18O时间序列记录了MIS 5d/5c转换时亚洲夏季风强度变化的突变过程.根据突变过程中间点的年龄确定MIS5d/5c突变时间为108.1±0.3 ka BP.石笋记录对MIS 5d/5c突变时间的精确标定可以作为MIS 5阶段重要的年龄控制点,用以校正南北极冰芯记录和深海沉积记录的时间标尺.季风MIS5d/5c转换阶段也表现为类似过去4个冰消期的2个阶段变化过程：阶段Ⅰ为夏季风较弱时期,而南极温度缓慢上升;阶段Ⅱ为夏季风快速增强时期,与甲烷浓度突变同步,南极温度则上升至最高值.

关键词：黔北 MIS 5d/5c 亚洲季风三星洞石笋氧同位素

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