江西上湖旧石器遗址沉积地层记录的环境演化及古人类行为适应研究<sup>&#x0002A;</sup>

doi:10.7605/gdlxb.2025.01.004

古地理学报 ›› 2025, Vol. 27 ›› Issue (1): 153-166. doi: 10.7605/gdlxb.2025.01.004

• 古今地理环境与人类文明 • 上一篇下一篇

江西上湖旧石器遗址沉积地层记录的环境演化及古人类行为适应研究^*

贾雅娜^1,2,3, 李三灵⁴, 赵文杰⁵, 朱艳¹, 刘翀昊¹, 涂华⁶, 李浩⁷, 张玉柱¹

1 西北大学城市与环境学院,陕西省地表系统与环境承载力重点实验室,陕西西安 710127;
2 中国科学院地球环境研究所,黄土与第四纪地质国家重点实验室,陕西西安 710061;
3 西安交通大学全球环境变化研究院,陕西西安 710049;
4 河南大学历史文化学院,河南开封 475001;
5 江西省文物考古研究院,江西南昌 330095;
6 汕头大学海洋科学研究院,广东汕头 515063;
7 中国科学院青藏高原研究所,青藏高原地球系统与资源环境全国重点实验室,北京 100101

收稿日期:2023-11-09 修回日期:2024-06-14 出版日期:2025-02-01 发布日期:2025-01-20
通讯作者: 张玉柱,男,1987年生,教授,博士生导师,长期从事环境变迁与自然灾害研究。E-mail: xbdzyz05@nwu.edu.cn。
作者简介:贾雅娜,女,1996年生,博士研究生,主要从事环境变迁与自然灾害研究。E-mail: nayajia@126.com。
基金资助:
*黄土与第四纪地质国家重点实验室开放基金项目(编号: SKLLQG2107)和国家自然科学基金项目(编号: 42277449)共同资助

Environmental evolution and hominin behavior adaptation of Shanghu Paleolithic site,Jiangxi Province

JIA Ya'na^1,2,3, LI Sanling⁴, ZHAO Wenjie⁵, ZHU Yan¹, LIU Chonghao¹, TU Hua⁶, LI Hao⁷, ZHANG Yuzhu¹

1 Shaanxi Provincial Key Laboratory of Earth Surface System and Environmental Carrying Capacity,College of Urban and Environmental Sciences,Northwest University,Xi'an 710127,China;
2 State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China;
3 Institute of Global Environmental Change,Xi'an Jiaotong University,Xi'an 710049,China;
4 School of History and Culture,Henan University,Henan Kaifeng 475001, China;
5 Jiangxi Provincial Institute of Cultural Heritage and Archaeology,Nanchang 330095,China;
6 Institute of Marine Science,Shantou University,Guangdong Shantou 515063, China;
7 State Key Laboratory of Tibetan Plateau Earth System,Environment and Resources,Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100101, China

Received:2023-11-09 Revised:2024-06-14 Online:2025-02-01 Published:2025-01-20
Contact: ZHANG Yuzhu,born in 1987,a professor,doctoral supervisor,is engaged in environmental change and natural disaster research. E-mail: xbdzyz05@nwu.edu.cn.
About author:JIA Ya'na,born in 1996,a Ph.D. candidate,is engaged in environmental change and natural disaster research. E-mail: nayajia@126.com.
Supported by:
Open Foundation of the State Key Laboratory of Loess and Quaternary Geology(No. SKLLQG2107)and the National Natural Science Foundation of China(No.42277449)

摘要/Abstract

摘要： 探究遗址沉积过程与古环境背景对于全面了解古人类生存行为信息具有重要意义。江西上湖遗址是中国南方地区新近发掘的一处旧石器时代旷野遗址,遗址均质红土B层中出土了丰富的石制品,表现出小型化特点,年代始于距今约 2.6万年前。本研究对上湖旧石器遗址沉积地层开展了野外考察和室内土壤微形态、磁化率、粒度和地球化学元素分析,同时对出土的石制品进行了考古埋藏学分析。地学和考古学方法二者相互印证,明确揭示出该遗址区均质红土B层仅受到了低能坡面流水作用,保存了较为完整的古人类技术行为信息。推测古人类在MIS2阶段频繁占据和使用上湖遗址等区域,可能与拥有小型石片石器技术的华北地区人群难以忍受该时段北方极端寒冷干燥的气候条件被迫向南迁徙、从而到达了气候相对干凉的长江中下游地区进行生产活动有关。并且上湖遗址古人类采取了偏后勤式流动策略,以应对异常极端气候带来的资源分布不均和可预测性降低等风险。

关键词: 上湖旧石器遗址, 地质考古, 人类行为适应, 小型石片石器, MIS2阶段

Abstract: Understanding the depositional process and paleoenvironment of the archaeological site is crucial for comprehending ancient human technology behavior. The Shanghu site,an open-air Paleolithic site,was newly discovered in southern China. Abundant stone artifacts,characterized by miniaturization,were unearthed from the homogeneous red soil B layer,dated to approximately 26 000 years ago. Integrated field investigation,micromorphology,magnetic susceptibility,grain size,geochemistry and archaeological taphonomy were comprehensively conducted. Our findings reveal that the homogeneous red soil B layer was primarily influenced by low-energy slope water processes,which allowed for the preservation of relatively intact records of ancient human technological behavior. The Shanghu site was frequently occupied by ancient humans during the MIS2 period. This may be related to the fact that ancient humans in North China with small flake tool industry were unable to withstand the extremely cold-dry climate,and were compelled to migrate southward,eventually arriving in the middle and lower reaches of the Yangtze River where the climate was relatively dry and cool. Moreover,ancient humans adopted a logistical mobility strategy to cope with the risks of uneven distribution and reduced predictability of resources caused by the extreme climate.

Key words: Shanghu Paleolithic site, geological archaeology, human behavior adaptation, small flake tool industry, MIS2

中图分类号:

贾雅娜, 李三灵, 赵文杰, 朱艳, 刘翀昊, 涂华, 李浩, 张玉柱. 江西上湖旧石器遗址沉积地层记录的环境演化及古人类行为适应研究^*[J]. 古地理学报, 2025, 27(1): 153-166.

JIA Ya'na, LI Sanling, ZHAO Wenjie, ZHU Yan, LIU Chonghao, TU Hua, LI Hao, ZHANG Yuzhu. Environmental evolution and hominin behavior adaptation of Shanghu Paleolithic site,Jiangxi Province[J]. Journal of Palaeogeography（Chinese Edition）, 2025, 27(1): 153-166.

http://www.gdlxb.cn/CN/Y2025/V27/I1/153

参考文献

[1] 陈铁汉,肖华. 1987. 江西锦江流域岩溶发育特征. 中国岩溶,6(3): 189-196.
[Chen T H,Xiao H.1987. The feature of karst development in Jinjiang Basin,Jiangxi. Carsologica Sinica,6(3): 189-196]
[2] 刁桂仪,文启忠. 1999. 黄土风化成土过程中主要元素迁移序列. 地质地球化学,27(1): 21-26.
[Diao G Y,Wen Q Z.1999. The migration series of major elements during loess pedogenesis. Geology-Geochemistry,27(1): 21-26]
[3] 杜水生,杨宇霞,王辉. 2019. 文化交流或适应趋同: 甘肃环县楼房子遗址2011—2012年发掘的新材料. 第四纪研究,39(6): 1443-1456.
[Du S S,Yang Y X,Wang H.2019. Cultural communication or convergent adaptation: new materials from Loufangzi site at Huanxian County,Gansu Province in 2011-2012. Quaternary Sciences,39(6): 1443-1456]
[4] 杜艳. 2013. 中国长江流域第四纪红土年代学研究及末次间冰期以来古气候演变. 上海大学博士学位论文: 109-110.
[Du Y.2013. OSL dating of the Quaternary red clay distributed in the reaches of the Yangtze River and paleoclimatic changes since the last interglacial period in mid-subtropical southeast China. Doctoral dissertation of Shanghai University: 109-110]
[5] 冯连君,储雪蕾,张启锐,张同钢. 2003. 化学蚀变指数(CIA)及其在新元古代碎屑岩中的应用. 地学前缘,10(4): 539-544.
[Feng L J,Chu X L,Zhang Q R,Zhang T G.2003. CIA(chemical index of alteration)and its applications in the Neoproterozoic clastic rocks. Earth Science Frontiers,10(4): 539-544]
[6] 高星. 2014. 更新世东亚人群连续演化的考古证据及相关问题论述. 人类学学报,33(3): 237-253.
[Gao X.2014. Archaeological evidence for evolutionary continuity of Pleistocene humans in China and East Asia and related discussions. Acta Anthropologica Sinica,33(3): 237-253]
[7] 黄旭华,王永文,李喻鑫. 2020. 江西省锦江流域降水变化特征研究. 中国农村水利水电,(1): 100-105.
[Huang X H,Wang Y W,Li Y X.2020. Research on the precipitation variation characteristics of Jinjiang River Basin in Jiangxi Province. China Rural Water and Hydropower,(1): 100-105]
[8] 黄镇国,张伟强,陈俊鸿,刘瑞华,何正翀. 1996. 中国南方红色风化壳. 北京: 海洋出版社,122-124.
[Huang Z G,Zhang W Q,Chen J H,Liu R H. 1996. Red Weathering Crust of Southern China. Beijing: China Ocean Press,122-124]
[9] 江西省地质矿产局. 1984. 江西省区域地质志. 北京: 地质出版社,1-706.
[Geology and Mineral Resources Bureau of Jiangxi Province. 1984. Regional Geology of Jiangxi Province. Beijing: Geological Publishing House,1-706]
[10] 江西省水利厅. 2010. 江西省河湖大典. 武汉: 长江出版社,202-270.
[Water Resources Department of Jiangxi Province. 2010. Records of Rivers and Lakes in Jiangxi Province. Wuhan: Changjiang Press,202-270]
[11] 靳桂云. 1999. 土壤微形态分析及其在考古学中的应用. 地球科学进展,14(2): 197-200.
[Jin G Y.1999. Soil micromorphology in archaeology. Advances in Earth Science,14(2): 197-200]
[12] 李凤全,叶玮,朱丽东,姜永见,李建武,伊继雪,袁双. 2010. 第四纪网纹红土的类型与网纹化作用. 沉积学报,28(2): 346-355.
[Li F Q,Ye W,Zhu L D,Jiang Y J,Li J W,Yi J X,Yuan S.2010. The types and formation of Quaternary plinthitic red earth. Acta Sedimentologica Sinica,28(2): 346-355]
[13] 李浩,李超荣,Kathleen Kuman.2016. 丹江口库区果茶场Ⅱ旧石器遗址形成过程研究. 江汉考古,(1): 42-50.
[Li H,Li C R,Kuman K.2016. Site formation analysis of Guochachang II palaeolithic site in Danjiangkou Reservoir Region. Jianghan Archaeology,(1): 42-50]
[14] 李浩,张玉柱,李意愿,李占扬,贾雅娜. 2021. 沉积物特征与旧石器遗址的形成过程. 人类学学报,40(3): 363-377.
[Li H,Zhang Y Z,Li Y Y,Li Z Y,Jia Y N.2021. Sediment characteristics and the formation processes of Paleolithic sites. Acta Anthropologica Sinica,40(3): 363-377]
[15] 李红琼,韩荣培. 2020. 赣南地区南方红壤粒度与磁化率特征研究. 绿色科技,(20): 34-38.
[Li H Q,Han R P.2020. Study on grain size and magnetic susceptibility of south red soil in southern Jiangxi Province. Journal of Green Science and Technology,(20): 34-38]
[16] 李建武. 2009. 金衢盆地红土的理化特征与形成环境. 浙江师范大学硕士学位论文: 23-34.
[Li J W.2009. The physical and geochemical characteristics and formative environment of red earth in Jinhua-Quzhou Basin. Masteral dissertation of Zhejiang Normal University: 23-34]
[17] 李三灵,赵文杰,高玉,李浩. 2023. 江西高安盆地旧石器遗址调查简报. 人类学学报,42(6): 807-814.
[Li S L,Zhao W J,Gao Y,Li H.2023. A preliminary report on the survey of Paleolithic sites in Gao'an Basin,Jiangxi Province. Acta Anthropologica Sinica,42(6): 807-814]
[18] 李徐生,杨达源,韩辉友. 1998. 皖南风尘堆积—古土壤序列磁化率初步研究. 安徽师大学报(自然科学版),21(1): 64-69.
[Li X S,Yang D Y,Han H Y.1998. A preliminary study on the magnetic susceptibility of aeolian dust deposition paleosol sequence in the south of Anhui Province. Journal of Anhui Normal University(Natural Science),21(1): 64-69]
[19] 李意愿. 2020. 石器工业与适应行为: 澧水流域晚更新世古人类文化研究. 上海: 上海古籍出版社,209-231.
[Li Y Y. 2020. Lithic Industries and Adaptation Behaviors: a Study of Late Pleistocene Hominin Culture in the Lishui River Basin. Shanghai: Shanghai Classics Publishing House,209-231]
[20] 刘东生. 1985. 黄土与环境. 北京: 科学出版社,191-208.
[Liu D S. 1985. Loess and Environment. Beijing: Science Press,191-208]
[21] 卢升高. 2007. 中国南方红土环境磁学. 第四纪研究,27(6): 1016-1022.
[Lu S G.2007. Environmental magnetism of Quaternary red earth in Southern China. Quaternary Sciences,27(6): 1016-1022]
[22] 鹿化煜,安芷生. 1998. 黄土高原黄土粒度组成的古气候意义. 中国科学(D辑: 地球科学),28(3): 278-283.
[Lu H Y,An Z S.1998. Paleoclimatic significance of grain size composition of loess on Loess Plateau. Scientia Sinica(Terrae),28(3): 278-283]
[23] 吕厚远,韩家懋,吴乃琴,郭正堂. 1994. 中国现代土壤磁化率分析及其古气候意义. 中国科学(B辑化学生命科学地学),24(12): 1290-1297.
[Lü H Y,Han J M,Wu N Q,Guo Z T.1994. Analysis of modern soil magnetic susceptibility in China and its paleoclimatic significance. Science in China,Ser B,24(12): 1290-1297]
[24] 裴树文. 2019. 旧石器时代旷野遗址形成过程研究综述. 人类学学报,38(1): 1-18.
[Pei S W.2019. A general study review of site formation processes for Paleolithic open-air sites. Acta Anthropologica Sinica,38(1): 1-18]
[25] 裴树文. 2021. 中国古人类活动遗址形成过程研究的进展与思考. 人类学学报,40(3): 349-362.
[Pei S W.2021. The progress and consideration on the study of site formation processes of early human occupation in China. Acta Anthropologica Sinica,40(3): 349-362]
[26] 饶志国,朱照宇,吴翼,杨恬,付淑清. 2007. 华南地区发育于不同母岩之上的表土磁化率特征及其意义. 第四纪研究,27(4): 651-652.
[Rao Z G,Zhu Z Y,Wu Y,Yang T,Fu S Q.2007. Character and significance of magnetic susceptibility of modern surface soils developed from different native rocks within South China. Quaternary Sciences,27(4): 651-652]
[27] 任进成,王法岗,李锋,杨庆江,陈福友,高星. 2021. 泥河湾盆地板井子旧石器时代遗址的形成过程. 人类学学报,40(3): 378-392.
[Ren J C,Wang F G,Li F,Yang Q J,Chen F Y,Gao X.2021. Formation processes of the Banjingzi Paleolithic site in the Nihewan Basin. Acta Anthropologica Sinica,40(3): 378-392]
[28] 王社江. 2005. 洛南花石浪龙牙洞1995年出土石制品的拼合研究. 人类学学报,24(1): 1-17.
[Wang S J.2005. The refitting of lithic artefacts from the Longyadong cave,Luonan Basin,China. Acta Anthropologica Sinica,24(1): 1-17]
[29] 王幼平. 2016. 华南晚更新世晚期人类行为复杂化的个案: 江西万年吊桶环遗址的发现. 人类学学报,35(3): 397-406.
[Wang Y P.2016. Behavioral modernity and variability of late Late Pleistocene humans in South China: a case study of Diaotonghuan in Wannian,Jiangxi Province. Acta Anthropologica Sinica,35(3): 397-406]
[30] 王幼平. 2021. 砾石工业传统与华南旧石器晚期文化. 南方文物,(1): 91-97.
[Wang Y P.2021. The gravel industry tradition and the late paleolithic culture in South China. Cultural Relics in Southern China,(1): 91-97]
[31] 王幼平,汪松枝,赵潮,陈宥成. 2018.2013年河南登封东施旧石器晚期遗址发掘简报. 中原文物,(6): 46-53.
[Wang Y P,Wang S Z,Zhao C,Chen Y C.2018. The excavation of the late-paleolithic-age Dongshi site at Dengfeng,Henan in 2013. Cultural Relics of Central China,(6): 46-53]
[32] 文启忠. 1989. 中国黄土地球化学. 北京: 科学出版社,1-234.
[Wen Q Z. 1989. Geochemistry of China Loess. Beijing: Science Press,1-234]
[33] 席承藩. 1991. 论华南红色风化壳. 第四纪研究,11(1): 1-8.
[Xi C F.1991. On the red weathering crusts of Southern China. Quaternary Sciences,11(1): 1-8]
[34] 熊平生. 2012. 赣南地区网纹红土的形成及其环境变化研究. 西南大学博士论文: 41-51.
[Xiong P S.2012. A study on patterned red clay formation and environment change in Gannan Region. Doctoral dissertation of Southwest University: 41-51]
[35] 杨立辉. 2017. 长江中下游地区第四纪红土沉积特征与成因机制研究. 华东师范大学博士学位论文: 22-24.
[Yang L H.2017. The study of sedimentary characteristics and genetic mechanism of the Quaternary red clay in the middle and lower reaches of Yangtze river. Doctoral dissertation of East China Normal University: 22-24]
[36] 应立朝,梁斌,王全伟,朱兵,郝雪峰,王鑫,刘亮,付小方. 2012. 川西平原中更新世网纹红土主量元素地球化学特征. 高校地质学报,18(4): 759-764.
[Ying L C,Liang B,Wang Q W,Zhu B,Hao X F,Wang X,Liu L,Fu X F.2012. Major elements characters of the Middle Pleistocene vermicular red clay from the western Sichuan Plain. Geological Journal of China Universities,18(4): 759-764]
[37] 俞劲炎,詹硕仁,吴劳生,朱祖祥. 1986. 亚热带和热带土壤的磁化率. 土壤学报,23(1): 50-56.
[Yu J Y,Zan S R,Wu L S,Zhu Z X.1986. The magnetic susceptibility of the soils in subtropical and tropical China. Acta Pedologica Sinica,23(1): 50-56]
[38] 张玉柱,黄春长,庞奖励,周亚利,周强,郭永强,尚瑞清. 2015. 青海民和官亭盆地喇家遗址古耕作土壤层微形态研究. 土壤学报,52(5): 1002-1013.
[Zhang Y Z,Huang C C,Pang J L,Zhou Y L,Zhou Q,Guo Y Q,Shang R Q.2015. Micromorphology of ancient plow layer of paleosol in the lajia Ruins in the Guanting Basin,Minhe County,Qinghai Province. Acta Pedologica Sinica,52(5): 1002-1013]
[39] 赵文杰,贾真秀,李三灵,李浩. 2023.2020年江西高安上湖旧石器遗址发掘报告. 人类学学报,42(3): 373-380.
[Zhao W J,Jia Z X,Li S L,Li H.2023. A report of the 2020 excavation of the Shanghu Paleolithic site in Gaoan city,Jiangxi Province. Acta Anthropologica Sinica,42(3): 373-380]
[40] 朱丽东,姜永见,张明强,叶玮,李凤全,冯义雄. 2011. 庐山JL剖面红土磁化率特征及古环境记录. 山地学报,29(4): 385-394.
[Zhu L D,Jiang Y J,Zhang M Q,Ye W,Li F Q,Feng Y X.2011. Characteristics of magnetic susceptibility and its paleoenvironmental records from JL red earth section,Lushan Area. Journal of Mountain Science,29(4): 385-394]
[41] 朱显谟. 1993. 中国南方的红土与红色风化壳. 第四纪研究,13(1): 75-84.
[Zhu X M.1993. Red clay and red residuum in South China. Quaternary Sciences,13(1): 75-84]
[42] Antón S C,Potts R,Aiello L C.2014. Evolution of early Homo: an integrated biological perspective. Science,345: e1236828.
[43] Berger L R,de Ruiter D J,Churchill S E,Schmid P,Carlson K J,Dirks P H G M,Kibii J M.2010. Australopithecus sediba: A new species of Homo-like australopith from South Africa. Science,328: 195-204.
[44] Binford L R.1980. Willow smoke and dogs' tails: Hunter-gatherer settlement systems and archaeological site formation. American Antiquity,45: 4-20.
[45] Chen F H,Welker F,Shen C C,Bailey S E,Bergmann I,Davis S,Xia H,Wang H,Fischer R,Freidline S E,Yu T L,Skinner M M,Stelzer S,Dong G R,Fu Q M,Dong G H,Wang J,Zhang D J,Hublin J J.2019. A late Middle Pleistocene Denisovan mandible from the Tibetan Plateau. Nature,569: 409-412.
[46] Clark P U,Dyke A S,Shakun J D,Carlson A E,Clark J,Wohlfarth B,Mitrovica J X,Hostetler S W,McCabe A M.2009. The last glacial maximum. Science,325: 710-714.
[47] Cornwall I.1958. Soils for the archaeologist. South African Archaeological Bulletin,13: 143.
[48] Dart R A.1925. Australopithecus africanus the man-ape of South Africa. Nature,115: 195-199.
[49] Dennell R,Roebroeks W.2005. An Asian perspective on early human dispersal from Africa. Nature,438: 1099-1104.
[50] Goldberg P.1980. Micromorphology in archaeology and prehistory. Paléorient,6: 159-164.
[51] Han J M,Lü H Y,Wu N Q,Guo Z T.1996. The magnetic susceptibility of modern soils in China and its use for paleoclimate reconstruction. Studia Geophysica et Geodaetica,40: 262-275.
[52] Heller F,Liu T S.1982. Magnetostratigraphical dating of loess deposits in China. Nature,300: 431-433.
[53] Hill A,Ward S,Deino A,Curtis G,Drake R.1992. Earliest Homo debate. Nature,358: 290.
[54] Jia Z X,Pei S W,Benito-Calvo A,Ma D D,Sanchez-Romero L,Wei Q.2019. Site formation processes at Donggutuo: a major Early Pleistocene site in the Nihewan Basin,North China. Journal of Quaternary Science,34: 621-632.
[55] Kuman K,Field A S. 2009. The oldowan industry from Sterkfontein caves,South Africa. In: Schick,K,Toth N(eds). The Cutting Edge: New Approaches to the Archaeology of Human Origins. Indiana: Stone Age Institute Press,151-169.
[56] Leakey M G,Spoor F,Dean M C,Feibel C S,Antón S C,Kiarie C,Leakey L N.2012. New fossils from Koobi Fora in northern Kenya confirm taxonomic diversity in early Homo. Nature,488: 201-204.
[57] Li H,Li Z Y,Lotter M G,Kuman K.2018. Formation processes at the early Late Pleistocene archaic human site of Lingjing,China. Journal of Archaeological Science,96: 73-84.
[58] Li H,Li Y Y,Yu L P,Tu H,Zhang Y Z,Sumner A,Kuman K.2022. Continuous technological and behavioral development of late Pleistocene hominins in central South China: multidisciplinary analysis at Sandinggai. Quaternary Science Reviews,298: 107850
[59] Li L,Lin S C,Peng F,Patania I,Guo J L,Wang H M,Gao X.2021. Simulating the impact of ground surface morphology on archaeological orientation patterning. Journal of Archaeological Science,126: 105310.
[60] Li Q,Wu H B,Yu Y Y,Sun A Z,Luo Y L.2019. Large-scale vegetation history in China and its response to climate change since the Last Glacial Maximum. Quaternary International,500: 108-119.
[61] Lu H Y,Wu N Q,Liu K B,Jiang H,Liu T S.2007. Phytoliths as quantitative indicators for the reconstruction of past environmental conditions in China Ⅱ: Palaeoenvironmental reconstruction in the Loess Plateau. Quaternary Science Reviews,26: 759-772.
[62] McLennan S M.1993. Weathering and global denudation. Journal of Geology,101: 295-303.
[63] Nesbitt H W,Young G M.1982. Early Proterozoic climates and plate motions inferred from major element chemistry of lutites. Nature,299: 715-717.
[64] Pei S W,Niu D W,Guan Y,Nian X M,Kuman K,Bae C J,Gao X.2014. The earliest Late Paleolithic in North China: site formation processes at Shuidonggou Locality 7. Quaternary International,347: 122-132.
[65] Schick K D. 1986. Stone Age Sites in the Making: Experiments in the Formation and Transformation of Archaeological Occurrences. Ann Arbor,MI: University of Michigan Press,1-313.
[66] Shick K D.1987. Modeling the formation of Early Stone Age artifact concentrations. Journal of Human Evolution,16: 789-807.
[67] Svendsen J I,Alexanderson H,Astakhov V I,Demidov I,Dowdeswell J A,Funder S,Gataullin V,Henriksen M,Hjort C,Houmark-Nielsen M,Hubberten H W,Ingólfsson Ó,Jakobsson M,Kjær K H,Larsen E,Lokrantz H,Lunkka J P,Lyså A,Mangerud J,Matiouchkov A,Murray A,Möller P,Niessen F,Nikolskaya O,Polyak L,Saarnisto M,Siegert C,Siegert M J,Spielhagen R F,Stein R.2004. Late Quaternary ice sheet history of northern Eurasia. Quaternary Science Reviews,23: 1229-1271.
[68] Thompson R,Oldfield F.1986. Environmental Magnetism. London: Allen & Unwin,1-227.
[69] Wood B.2014. Human evolution: Fifty years after Homo habilis. Nature,508: 31-33.
[70] Xiao J L,Porter S C,An Z S,Kumai H,Yoshikawa S.1995. Grain size of quartz as an indicator of winter monsoon strength on the Loess Plateau of central China during the last 130000 yr. Quaternary Research,43: 22-29.
[71] Xiao J Y,Xiao X Y,Zhang M H,Shang Z Y,Chen Y.2015. Late Pleistocene montane vegetation and climate history from the Dajiuhu Basin in the western Hubei Province of Central China. Review of Palaeobotany and Palynology,222: 22-32.
[72] Xie G M,Lin Q,Wu Y,Hu Z H.2020. The Late Paleolithic industries of Southern China(Lingnan region). Quaternary International,535: 21-28.
[73] Zhang D J,Xia H,Chen F H,Li B,Slon V,Cheng T,Yang R W,Jacobs Z,Dai Q Y,Massilani D,Shen X K,Wang J,Feng X T,Cao P,Yang M A,Yao J T,Yang J S,Madsen D B,Han Y Y,Ping W J,Liu F,Perreault C,Chen X S,Meyer M,Kelso J,Pääbo S,Fu Q M.2020. Denisovan DNA in late Pleistocene sediments from baishiya Karst cave on the Tibetan Plateau. Science,370: 584-587.
[74] Zhu R X,Potts R,Xie F,Hoffman K A,Deng C L,Shi C D,Pan Y X,Wang H Q,Shi R P,Wang Y C,Shi G H,Wu N Q.2004. New evidence on the earliest human presence at high northern latitudes in northeast Asia. Nature,431: 559-562.
[75] Zhu Z Y,Dennell R,Huang W W,Wu Y,Qiu S F,Yang S X,Rao Z G,Hou Y M,Xie J B,Han J W,Ouyang T P.2018. Hominin occupation of the Chinese Loess Plateau since about 2.1 million years ago. Nature,559: 608-612.

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江西上湖旧石器遗址沉积地层记录的环境演化及古人类行为适应研究^*

Environmental evolution and hominin behavior adaptation of Shanghu Paleolithic site,Jiangxi Province

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江西上湖旧石器遗址沉积地层记录的环境演化及古人类行为适应研究*

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江西上湖旧石器遗址沉积地层记录的环境演化及古人类行为适应研究^*