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Journal of Geographical Sciences 2020年第3期30卷 423-438页

作者： ZHAO Chengshuangping mo duowen Laboratory for Earth Surface Process Ministry of EducationCollege of Urban and Environmental SciencesPeking UniversityBeijing 100871China Institute of Geographical Sciences Henan Academy of SciencesZhengzhou 450052China

Based on the comprehensive analyses of 18 core profiles’sedimentary sequences and lithological characteristics in Jianghan-Dongting Basin of the middle reaches of the Yangtze River and the spatial-temporal distribution of archeological sites in this area,we reconstructed the Holocene hydro-environmental evolution,and its relationship with human *** comparison reveals:11.5–5.5 ka BP,the water level of rivers and lakes in the middle Yangtze River appeared a rising trend,concurrently,under the development of Neolithic culture and rice agricultural activities,human occupation extended from piedmont plain to inner basin plain in the study *** water level fell in 5.5–4.0 ka BP,meanwhile,the number of human settlements of Qujialing-Shijiahe culture rapidly increased,especially in the inner basin *** water level rose again around 4.0 ka BP,floods spread massively in this period,which led to the decline of Shijiahe *** main causes for hydro-environmental evolution in the study area are the fluctuation of sea level and the aggradation of fluvio-lacustrine sediments.

关键词： Jianghan-Dongting Basin Holocene hydrological environmental change human-environment interaction

RIVERS' FEATURES ON ALLUVIAL FANS IN NORTHWEST CHINA

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International Journal of Sediment Research 1999年第2期14卷 339-344页

作者： ZHU Zhongli mo duowen (Department of Geography, Peking University, China)

Braided river is considered as the main river pattern developed on alluvial fans. But this is not true in Northwest China. Analysis and correlations of the characteristics of more than 10 rivers show that straight river is the main river pattern and braided river only develops on middle segment of the river in this district. The main factor to shape this river pattern on alluvial fans is the standing incision due to changes in precipitation and sedimentary condition caused by climate change since Holocene. Because of the tectonic movement and boundary condition from gravel to loess-like sediment. some rivers have fan-head trenching and others have fan-toe trenching with the U-shaped cross section.

关键词： Alluvial fan River patterns Precipitation and sedimentary condition. Climate changes Boundary condition

Environmental Change and Human Occupation during Late Pleistocene in Hunan Province， South China

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Journal of Earth Science 2024年

作者： Aipeng Guo Longjiang Mao Yiyuan Li Haicheng Lai Jiafu Zhang duowen mo Institute of Scientific and Technical History， Nanjing University of Information Science and Technology School of Marine Science， Nanjing University of Information Science and Technology Hunan Institute of Archaeology College of Urban and Environmental Sciences， Peking University

The Paleolithic sites in South China have caused controversy regarding human behaviors in response to the rapidly shifting environment of the late Pleistocene. However， chronometric and high-resolution proxies are absent from interpreting the paleoenvironmental evolution. Here we present the chronology， grain size parameters， and geochemical elements records from the Hejialing (HJL) site in South China to reveal the crucial aspects of environmental evolution， and human occupation. The geochemical record shows that during MIS 5e–5a， northern Hunan experienced the influence of summer monsoon and maintained a warm and humid climate. The laterite layer began to develop. During MIS 4， the climate transitioned to dry and cold state， leading to the attraction of hominins to the HJL area due to the abundant water and lithic raw material resources， resulting in their establishment of a short-term camp. The HJL site was primarily inhabited by hunter-gatherer societies within a forested environment. From MIS 4 to MIS 2， Hunan experienced a prolonged period of dry and cold climatic conditions， with a brief rainfall recovery occurring in late MIS 3. Diminished vegetation and resource availability compelled human populations to broaden their activities and undertake migrations. The HJL site was abandoned amid the arid phase of MIS 2. The HJL area gradually became buried beneath eolian dust deposition (EM1) from distant sources and riverine dust from nearby sources (EM2)， and the site was informed. In MIS 1， During MIS 1， the climate shifted to a warm and humid state， marking the emergence of early agricultural practices. As an essential part of South China， the environmental evolution process and diverse survival strategies employed by hominins in Hunan are vital for explaining how the paleoenvironment drove human occupation during the Late Pleistocene.

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Paleosalinity in the Tianluoshan site and the correlation between the Hemudu culture and its environmental background

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Journal of Geographical Sciences 2010年第3期20卷 441-454页

作者： LI Minglin mo duowen MAO Longjiang SUN Guoping ZHOU Kunshu College of Urban and Environmental Sciences Peking University Beijing 100871 China College of Atmospheric Science Nanjing University of Information Science ＆ Technology Nanjing 210044 China Zhejiang Provincial Institute of Cultural Relics and Archaeology Hangzhou 310014 China Institute of Geology and Geophysics CAS Beijing 100029 China

Paleosalinity records of the Tianluoshan site are derived from measurations data of clay mineral, boron, strontium, barium, after field sampling in three profiles of the Tianluoshan site. The relative sea level changes are discussed according to the lab results. The record indicates that the region where the Tianluoshan site located has witnessed at least three times of relative sea level high-stand before, during and after the Hemudu period. Based on previous researches, this paper also focuses on discussing several environmental elements, the inter-relationships between environmental condition, human activities and development of the Hemudu culture comprehensively.

关键词： the Tianluoshan site the Hemudu culture paleosalinity environmental background relative sea level

Holocene aeolian activities linked to Indian summer monsoon in the middle reaches of the Yarlung Zangbo River

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Journal of Geographical Sciences 2020年第12期30卷 2002-2014页

作者： LI Tuoyu ZHANG Jifeng WU Yongqiu DU Shisong mo duowen LIAO Yinan CHEN Zhitong LIU Jianbao LI Qing Capital Normal University Beijing 100048China Key Laboratory of Alpine Ecology(LAE) Institute of Tibetan Plateau ResearchCASBeijing 100101China moE Engineering Center of Desertification and Blown-sand Control Beijing Normal UniversityBeijing 100875China Laboratory for Earth Surface Processes Ministry of EducationCollege of Urban and Environmental SciencesPeking UniversityBeijing 100871China Institute of Geographical Sciences Hebei Engineering Research Center of Geographic Information ApplicationHebei Academy of SciencesShijiazhuang 050011China

Widespread aeolian deposits on the Tibetan Plateau(TP)have provided valuable palaeoclimatic ***,the primary factors(e.g.,climate factors,human activity,and vegetation cover)controlling aeolian deposition remain *** this paper,we use a dataset that comprises new and published ages of Holocene aeolian sand and loess in the middle reaches of the Yarlung Zangbo River to identify the primary controlling factors and palaeoclimatic implications of aeolian *** intervals of enhanced aeolian accumulation centered at 8.5-7.8,6.4-5.8,4.5-4.0,3.1-1.8,and 0.9 ka are identified,generally consistent with regional low rainfall events and weak Indian summer monsoon(ISM).This suggests that regional wetness,dominated by the ISM,may play a key role in modulating dust emissions and aeolian deposition on centennial *** results show that on centennial-to millennial-scales,ISM activity can be reconstructed by non-continuous aeolian deposits in the monsoon dominated TP.

关键词： Holocene aeolian activity dust Indian summer monsoon Tibetan Plateau

Prehistoric damaging earthquake promoted the decline of"Heluo Ancient State"in Early China

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Science China Earth Sciences 2023年第5期66卷 1120-1132页

作者： Xiu HU Peng LU Youli LI duowen mo Wanfa GU Qingri LIU Ailun GUO Panpan CHEN Hui WANG Yan TIAN Xu WANG Yayi HU Jiqin ZHANG Zhen WANG Quanxing LUO Junjie XU School of Urban and Environmental Science Peking UniversityBeijing100871China Institute of Geography Henan Academy of SciencesZhengzhou450052China Zhengzhou Institute of Cultural Relics and Archaeology Zhengzhou450000China The Institute of Archaeology Chinese Academy of Social SciencesBeijing100710China College of History Zhengzhou UniversityZhengzhou450000China School of Earth Sciences and Engineering Sun Yat-Sen UniversityGuangzhou510275China

The emergence of the"Ancient State"is considered an important stage in the discourse on human *** on its complex and hierarchical social structure,the Shuanghuaishu site of Henan Province is regarded as an"Ancient state",specifically the"Heluo Ancient State".The site is situated in the middle reaches of the Yellow River region and played a key role in prehistoric ***,the reasons behind its decline are ***,we conducted an integrated investigation of the archaeological excavations and archaeoseismic analyses at the Shuanghuaishu *** identified paleoseismic remains within paleo-artificial moats,which were formed owing to off-fault structures of soil liquefaction,hillslope landslides,and related ground fractures,along with shake-related wall disruption and building collapse in the residential *** dating was conducted to constrain the age for this earthquake event,which was determined to be approximately 5.0 cal kyr ***,based on the practical curve for earthquake-induced liquefaction,the preliminary estimate of the magnitude of this paleo seismic event is greater than M_(s)*** propose that the Shuanghuaishu site experienced a recession after the earthquake event,which may have influenced the continuous development of the"Heluo Ancient State"as a regional center settlement.

关键词： Shuanghuaishu site Heluo Ancient State Yangshao culture Archaeoseismology Geohazards

长江中游江汉-洞庭盆地全新世以来水文环境演变与人类活动

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地理学报 2020年第3期75卷 529-543页

作者：赵成双苹莫多闻北京大学城市与环境学院/教育部地表过程分析与模拟重点实验室北京100871 河南科学院地理研究所郑州450052

本文基于长江中游江汉-洞庭盆地18个钻孔岩性、沉积特征及年代数据,结合研究区考古遗址点时空分布特征,恢复研究区全新世以来水文环境演变过程,并探讨了区域水文环境演变的成因机制及其与人类活动的关系。结果表明,受东海海面上升和泥... 详细信息

本文基于长江中游江汉-洞庭盆地18个钻孔岩性、沉积特征及年代数据,结合研究区考古遗址点时空分布特征,恢复研究区全新世以来水文环境演变过程,并探讨了区域水文环境演变的成因机制及其与人类活动的关系。结果表明,受东海海面上升和泥沙淤积等因素影响,距今11.5-5.5 ka,长江中游地区河湖水位呈上升趋势,随着新石器文化的发展及稻作农业活动的增加,人类文化聚落自山前平原地带逐渐向盆地平原中部扩展;距今5.5-4.0 ka,长江中游河湖水位有所下降,新石器晚期的屈家岭-石家河文化迅速发展,聚落数量增多,平原腹地聚落比例增加;距今4.0 ka前后,河湖水位再次有所上升,洪泛过程加剧,可能是石家河文化快速衰落的主要原因。

关键词：江汉-洞庭盆地全新世水文环境演变人地关系

Environmental change since mid-Pleistocene recorded in Shangshan achaeological site of Zhejiang

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Journal of Geographical Sciences 2008年第2期18卷 247-256页

作者： MAO Longjiang mo duowen JIANG Leping JIA Yaofeng LIU Xiaoyan LI Minglin ZHOU Kunshu SHI Chenxi College of Urban and Environmental Sciences Peking University Beijing 100871 China Zhejiang Provincial institute of Cultural Relics and Archaeology Hangzhou 310014 China Department of Tourism and Environment Shaanxi Normal University Xi＇an 710062 China Department of Resources Environment and Tourism Hengyang Normal University Hengyang 421008 China Institute of Geology and Geophysics CAS Beijing 100029 China

At about 173 ka BP of the late period of mid-Pleistocene, the second terrace of the river had been formed as a result of uplift happening in Shangshan area because of the climate, sea level change and tectonic action. Between 173-75 ka BP, aeolian deposited on the terrace, a layer of reticulate red clayey soil about 80-100 cm thick deposited and developed under the warmer and higher temperature. In the last glacial period, the drop of the temperature and the decrease of the precipitation induced the dust-storms increased, A layer of Xiashu loess about 1.0-1.5 m thick accumulated on Shangshan terrace in the last glacial, which has the reticulate red clayey soil buried. At the beginning of the Holocene （11500 a BP-）, temperature went higher gradually and precipitation got more, the pre-persons moved on the Shangshan terrace （11,400-8600 a BP）, which is one of the most important archaeological sites, and can connect the paleolithic culture with Neolithic culture. It could be assumed from the results that the lower reaches of the Yangtze River are the home of rice cultivation, too. The lower place to the west of the Shangshan site experienced the two cycles process of the fluvial facies and the lacustrine facies, indicating that the water source of the pre-historical Shangshan is the river water or lake water. Two AMS 14C age proved the water source disappeared more than 1000 years ago.

关键词： environmental change reticulate red clay TL/OSL dating mid-Pleistocene Shangshan culture Zhejiang

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王乃樑先生对中国地貌学发展的主要贡献

地理学报 2016年第11期71卷 2037-2048页

作者：莫多闻夏正楷朱诚北京大学城市与环境学院北京100871 南京大学地理与海洋科学学院南京210046

王乃樑先生是中国著名的地貌学家。20世纪40年代至90年代初期,先后在清华大学和北京大学任教。他对中国黄土高原、华北、东北、西北、四川、湖北和广西等广大地区进行了地貌和新生代沉积研究,在新生代沉积与地貌演化历史、新构造活动与... 详细信息

王乃樑先生是中国著名的地貌学家。20世纪40年代至90年代初期,先后在清华大学和北京大学任教。他对中国黄土高原、华北、东北、西北、四川、湖北和广西等广大地区进行了地貌和新生代沉积研究,在新生代沉积与地貌演化历史、新构造活动与构造地貌学、地貌学与沉积学基本理论与方法等诸多领域取得了一系列创新性的成果。在地貌学学科建设、人才培养、科学研究和国内外学术交流诸方面,为中国地貌学的发展做出了卓越贡献。

关键词：王乃樑地貌学家地貌演化史新生代沉积构造地貌地貌学理论与方法

Transmutation of ancient settlements and environmental changes between 6000-2000 aBP in the Chaohu Lake Basin, East China

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Journal of Geographical Sciences 2010年第5期20卷 687-700页

作者： WU Li WANG Xinyuan ZHOU Kunshu mo duowen ZHU Cheng GAO Chao ZHANG Guangsheng LI Lan LIU Li HAN Weiguang School of Geographic and Oceanographic Sciences Nanjing University Nanjing 210093 China College of Territorial Resources and Tourism Anhui Normal University Wuhu 241000 Anhui China Center for Earth Observation and Digital Earth CAS Beijing 100190 China Institute of Geology and Geophysics CAS Beijing 100029 China College of Urban and Environmental Sciences Peking University Beijing 100871 China Department of Urban Construction and Environment Science West Anhui University Lu' an 237012 Anhu China

Based on the temporal-spatial distribution features of ancient settlement sites from the middle and late Neolithic Age to the Han dynasty in the Chaohu Lake Basin of Anhui Province, East China, using the methods of GIS combined with the reconstructed paleoen- vironment by the records of lake sediment since Holocene, the transmutation of ancient set- tlements with response to environmental changes in this area has been discussed. Studies show that the main feature of transmutation of ancient settlements from the middle and late Neolithic Age to the Han Dynasty was that the distribution of settlements in this area changed from high altitudes to low ones and kept approaching the Chaohu Lake with the passage of time. These could be the response to the climate change from warm-moist to a relatively warm-dry condition during the middle Holocene, leading to the lake level fluctuations. The large area of exposed land provided enough space for human activities. These indicate that the above changes in geomorphologic evolution and hydrology influenced by climate condi- tions affected the transmutation of ancient settlements greatly. The distribution pattern of settlement sites was that the number of sites in the west was more than in the east. This pattern may be related to the geomorphologic conditions such as frequent channel shifting of the Yangtze River as well as flood disasters during the Holocene optimum. Therefore, climate change was the inducement of the transmutation of ancient settlements in the Chaohu Lake Basin, which exerted great influence on the distribution, expansion and development of the ancient settlements.

关键词： Chaohu Lake Neolithic Age Han Dynasty transmutation of settlements climate change