全新世以来浙江余姚河姆渡&#x02014;田螺山遗址的古环境演变及人类活动<sup>&#x0002A;</sup>

doi:10.7605/gdlxb.2016.05.067

古地理学报 ›› 2016, Vol. 18 ›› Issue (5): 879-894. doi: 10.7605/gdlxb.2016.05.067

• 古今地理环境及人类文明 • 上一篇下一篇

全新世以来浙江余姚河姆渡—田螺山遗址的古环境演变及人类活动^*

郑丽波¹, 郝秀东², 禚彬³, 柳云龙³, 王小龙¹, 朱立新¹, 余新波⁴, 张甬江⁵

1 浙江省水文地质工程地质大队,浙江宁波 315000;
2 同济大学海洋与地球科学学院,上海 200092;
3 上海师范大学旅游学院,上海 200234;
4 宁波乡旅投资开发有限公司,浙江宁波 315100;
5 余姚市旅游局四明山旅游开发建设办公室,浙江余姚 315400

收稿日期:2016-01-12 修回日期:2016-05-03 出版日期:2016-10-01 发布日期:2016-10-01
通讯作者: 郝秀东,男,1980年生,同济大学海洋与地球科学学院博士研究生,现主要从事孢粉学与环境考古研究。E-mail: xiudonghao@126.com。
作者简介:郑丽波,女,1973年生,教授级高级工程师,主要从事第四纪环境与水文地质研究。E-mail: 121837499@qq.com。
基金资助:
*余姚市人民政府“河姆渡文化遗址全新世地质环境研究”项目、国家科技支撑计划课题项目(编号:2011BAC09B01-16,2006BAC01A16)和重庆市自然科学基金重点项目(编号:CSTC2009BA0002)共同资助

Holocene palaeoenvironment evolution and human activity of the Hemudu-Tianluoshan Sites in Yuyao of Zhejiang Province

Zheng Libo¹, Hao Xiudong², Zhuo Bin³, Liu Yunlong³, Wang Xiaolong¹, Zhu Lixin¹, Yu Xinbo⁴, Zhang Yongjiang⁵

1 Zhejiang Hydrogeologic and Engineering Geological Brigade,Ningbo 315000,Zhejiang;
2 School of Ocean and Earth Science,Tongji University,Shanghai 200092;
3 College of Tourism,Shanghai Normal University,Shanghai 200234;
4 Ningbo Rural Tourism Investment &Development Co.,Ltd,Ningbo 315100,Zhejiang;
5 Siming Mountain Tourism Development Construction Office,Yuyao Tourism Bureau,Yuyao 315400,Zhejiang

Received:2016-01-12 Revised:2016-05-03 Online:2016-10-01 Published:2016-10-01
Contact: Zheng Libo,born in 1973,is a professor of Zhejiang Hydrogeologic and Engineering Geological Brigade.She is mainly engaged in researches on Quaternary environmental evolution and hydrogeology. E-mail: 121837499@qq.com.About the corresponding author Hao Xiudong,born in 1980,is a Ph. D. candidate of Tongji University. He is engaged in researches on palynology and environmental archaeology.E-mail:xiudonghao@126.com.
Supported by:
; [Co￣funded by the Project of Holocene Geological Environment in Hemudu Cultural Ruins of the People’s Government of Yuyao City, Zhejiang Province, the Key Projects of the National Science and Technology Pillar Program (Nos.2011BAC09B01-16, 2006BAC01A16) and the Natural Science Foundation Project of Chongqing Municipality (No.CSTC2009BA0002)]

摘要/Abstract

摘要： 通过对浙江余姚河姆渡—田螺山遗址附近的HMD1501和HMD1502两个钻孔的微体古生物学研究,揭示了该地区全新世以来的植被演变、气候变化、海平面变迁及人类活动。孢粉、海相沟鞭藻、淡水藻类及有孔虫内衬的记录表明: (1)在早全新世(对应于镇海组下部),植被群落属于常绿阔叶和针叶混交林,气候温暖潮湿,研究区属于海侵阶段。(2)在中全新世(对应于镇海组中部),植被群落虽仍为针阔叶混交林,但气候转为温和湿润,研究区仍属于海侵阶段。(3)由于人类活动的进一步加剧,在晚全新世(对应于镇海组上部)的植被群落中草地的面积也随之扩大,并在滨海地区开始有一些以莎草科为主的沼泽地形成,植被群落属于针阔叶混交林—草地,气候更加凉爽干燥,研究区转为海退阶段。(4)在~7235—3327 cal. yr B.P.期间,草本花粉的含量激增,特别是一些粒径不小于35,μm 的禾本科栽培作物花粉的含量增加,说明此时人类活动开始增强,河姆渡—田螺山遗址附近出现较多的水稻种植区。

关键词: 孢粉组合, 全新世, 田螺山遗址, 古环境演变, 人类活动

Abstract: Micropaleontological record of the two boreholes(HMD1501 and HMD502)from Hemudu-Tianluoshan Sites in Yuyao of Zhejiang Province,reveals a detailed vegetation history,paleo-vegetation evolutions,palaeoclimate change,fluctuating sea level and human activity in the study area during the Holocene.Palynological results(pollen,spores,dinoflagellate,freshwater algae and foraminifer linings)suggest that: (1)Evergreen coniferous and broadleaved mixed forest developed during the Early Holocene(corresponding to the lower of Zhenhai Formation),the climate was warm and humid,and the study area was belong to a transgression stage. (2)Evergreen coniferous and broadleaved mixed forest were still developed during the Middle Holocene(corresponding to the middle of Zhenhai Formation),the climate changed into moderate and humid,and the transgression continued. (3)Due to human activity,coniferous and broadleaved mixed forest-grassland developed during the Late Holocene(corresponding to the upper of Zhenhai Formation),the climate changed into cold and dry,however,the study area began to enter a regression stage. (4)Human activities began to strengthen,and high percentage Poaceae pollen(≥35,μm)indicates rice culture activity presented at Hemudu-Tianluoshan Sites during the ca.7235-3327 cal.yr B.P..

Key words: Pollen assemblage, Holocene, Tianluoshan Site, palaeoenvironmental evolution, human activity

中图分类号:

Q914.81
P532

郑丽波, 郝秀东, 禚彬, 柳云龙, 王小龙, 朱立新, 余新波, 张甬江. 全新世以来浙江余姚河姆渡—田螺山遗址的古环境演变及人类活动^*[J]. 古地理学报, 2016, 18(5): 879-894.

Zheng Libo, Hao Xiudong, Zhuo Bin, Liu Yunlong, Wang Xiaolong, Zhu Lixin, Yu Xinbo, Zhang Yongjiang. Holocene palaeoenvironment evolution and human activity of the Hemudu-Tianluoshan Sites in Yuyao of Zhejiang Province[J]. JOPC, 2016, 18(5): 879-894.

http://www.gdlxb.cn/CN/Y2016/V18/I5/879

参考文献

[1] 江大勇,王新平,郝维城. 1999. 浙江中全新世古气候古环境变化与河姆渡古人类. 北京大学学报(自然科学版),35(2): 248-253. [Jiang D Y,Wang X P,Hao W C. 1999. Mid-Holocene paleoclimatic-paleoenvironmental changes in Zhejiang Province and Hemudu ancients.Acta Scientiarum Naturalium Universitatis Pekinensis,35(2): 248-253]
[2] 黄翡,王伟铭,李民昌. 1998. 苏州草鞋山遗址新石器时代以来的植硅石研究. 微体古生物学报,15(1): 79-84. [Huang F,Wang W M,Li M C. 1998. A study on phytoliths at Caoxieshan Site of Suzhou,Jiangsu since Neolithic Age. Acta Micropalaeontologica Sinica,15(1): 79-84]
[3] 黄渭金. 2002. 试论河姆渡史前先民与自然环境的关系. 华夏考古,(1): 28-32. [Huang W J. 2002. On the relationship of the prehistoric Hemudupeople with natural environments. Huaxia Archaeology,(1): 28-32]
[4] 黄宣佩,张明华. 1980. 青浦县崧泽遗址第二次发掘. 考古学报,(1): 29-58. [Huang Y P,Zhang M H. 1980. The second season of excavation at Songze Site in Qingpu County,Shanghai. Acta Archaeologica Sinica,(1): 29-58]
[5] 郎鸿儒. 1987. 浙江余姚河姆渡新石器时代遗址与全新世海面的变化. 浙江地质,3(1): 5-13. [Lang H R. 1987. The Neolithic site in Hemudu,Yuyao County,Zhejiang Province and the change of sea level during Holocene. Geology of Zhejiang,3(1): 5-13]
[6] 劳伯敏. 1995. 河姆渡干栏式建筑遗迹初探. 南方文物,(1): 50-57. [Lao B M. 1995. Study of stilt houses relics in Hemudu Site. Relics from South,(1): 50-57]
[7] 李从先,范代读. 2009. 全新世长江三角洲的发育及其对相邻海岸沉积体系的影响. 古地理学报, 11(1): 115-122. [Li C X,Fan D D. 2009. Development of the Holocene Changjiang delta and its influence on adjacent coastal sedimentary systems. Journal of Palaeogeography(Chinese Edition), 11(1); 115-122]
[8] 李从先,闵秋宝. 1981. 全新世长江三角洲顶部的海进和海面位置. 同济大学学报,(3): 104-108. [Li C X,Min Q B. 1981. The time of Holocene transgression and sea level changes in apical area of Yangtze delta. Journal of Tongji University, (3): 104-108]
[9] 李明霖,莫多闻,孙国平,周昆叔,毛龙江. 2009. 浙江田螺山遗址古盐度及其环境背景同河姆渡文化演化的关系. 地理学报,64(7): 807-816. [Li M L,Mo D W,Sun G P,Zhou K S,Mao L J. 2009. Paleosalinity in Tianluoshan Site and the relation between Hemudu culture and its environmental background.Acta Geographica Sinica,64(7): 807-816]
[10] 刘进峰,陈杰,雷生学,侯康明. 2009. 南京市区埋藏古河道沉积物的年代. 第四纪研究,29(4): 837-844. [Liu J F,Chen J,Lei S H,Hou K M. 2009. Preliminary dating results for Qinhuai palaeochannel sediments in Nanjing city. Quaternary Sciences,29(4): 837-844]
[11] 刘军. 2006. 河姆渡文化. 北京: 文物出版社. [Liu J. 2006. Hemudu Culture. Beijing:Cultural Relics Press]
[12] 裴安平,熊建华. 2004. 长江流域的稻作文化. 河北石家庄: 河北教育出版社,35-46. [Pei A P,Xiong J H. 2004. The culture of rice cultivation in the Yangtze River. Shijiazhuang Hebei: Hebei Educational Publishing House, 35-46]
[13] 史威,马春梅,焦锋,朱诚,王富葆. 2008. 宁绍平原史前遗址、埋藏泥炭与中全新世海面变化. 海洋学报,30(4): 169-175. [Shi W,Ma C M,Jiao F,Zhu C,Wang F B. 2008. Archaeological sites,buried peat and fluctuation of sea-level in Holocene in the Ningshao Plain in Zhejiang Province, China. Acta Oceanologica Sinica,30(4): 169-175]
[14] 舒军武,王伟铭,陈炜. 2007. 太湖平原西北部全新世以来植被与环境变化. 微体古生物学报,24(2): 210-221. [Shu J W,Wang W M,Chen W. 2007. Holocene vegetation and environment changes in the Taihu Plain,Jiangsu Province,East China. Acta Micropalaeontologica Sinica,24(2): 210-221]
[15] 孙湘君,杜乃秋,陈明洪. 1981. “河姆渡”先人生活时期的古植被、古气候. 植物学报,23(2): 144-151. [Sun X J,Du N Q,Chen M H. 1981. The paleovegetation and paleoclimate during time of Homudu people. Acta Botanica Sinica,23(2): 144-151]
[16] 吴征镒. 1980. 中国植被. 北京: 科学出版社. [Wu Z Y. 1980. Vegetation of China. Beijing: Science Press]
[17] 萧家仪,郭平,王丹,张瑞虎,丁金龙. 2004. 太湖平原全新世中晚期古植被、古环境与古文化: 以苏州绰墩遗址为例. 南京师大学报(自然科学版),27(2): 91-97. [Xiao J Y,Guo P,Wang D,Zhang R H,Ding J L. 2004. Palaeovegetation and palaeoenvironment and palaeoculture at Chudun Site in Taihu Plain during Middle and Late Holocene: A case study of Chudun Site in Suzhou. Journal of Nanjing Normal University(Natural Science),27(2): 91-97]
[18] 俞为洁. 1993. 杭州湾地区新石器时代农业概述. 古今农业,(1): 8-16. [Yu W J. 1993. Agricultrue in both banks of Hangzhou Bay inNeolithic Age. Ancient and Modern Agriculture,(1): 8-16]
[19] 浙江省地质矿产局. 1989. 浙江省区域地质志. 北京: 地质出版社. [Bureau of Geologyand Mineral of Resources of Zhejiang Province. 1989. Regional Geology of Zhejiang Province. Beijing: Geological Publishing House]
[20] 《浙江森林》编辑委员会. 1993. 浙江森林. 北京: 中国林业出版社,8-58. [Editorial Committee of Forests in Zhejiang. 1993. Forests in Zhejiang. Beijing: China Forestry Publishing House]
[21] 浙江文物考古研究所,余姚市文物保护管理所,河姆渡遗址博物馆. 2007. 浙江余姚田螺山新石器时代遗址2004年发掘简报. 文物,(11): 4-24. [Zhenjiang Provincial Institute of Cultural Relics and Archaeology,Yuyao Municipal Office of the Preservation of Cultural Relics,Hemudu Site Museum. 2007. Brief report of the excavation on a Neolithic Site at Tianluoshan Hill in Yuyao City,Zhenjiang. Cultural Relics,(11): 4-24]
[22] 郑云飞,孙国平,陈旭高. 2007.7000年前考古遗址出土稻谷的小穗轴特征. 科学通报,52(9): 1037-1041. [Zheng Y F,Sun G P,Chen X G. 2007. Characteristics of the short rachillae of rice fromarchaeological sites dating to 7000 years ago. Chinese Science Bulletin,52(12): 1654-1660]
[23] 郑云飞,芮国耀,松井章,宇田津彻朗,藤原宏志. 2001. 罗家角遗址水稻硅酸体形状特征及其在水稻进化上的意义. 浙江大学学报,27(6): 691-696. [Zheng Y F,Rui G Y,Matsui A,Udatsu T,Fujiwara H. 2001. Morphological characteristics of silica bodies from motor cells of rice from Luojiajiao site and theirimplication on rice evolution. Journal of Zhejiang University,27(6): 691-696]
[24] 郑云飞,游修龄,徐建民,边其均,俞为洁. 1994. 河姆渡遗址稻的硅酸体分析. 浙江农业大学学报,2(1): 81-85. [Zheng Y F,You X L,Xu J M,Bian Q J,Yu W J. 1994. Silica body analysis on rice remains at Hemudu sites. Journal of Zhejiang Agricultural University,2(1): 81-85]
[25] 郑卓,邓韫,张华,余荣春,陈炽新. 2004. 华南沿海热带—亚热带地区全新世变化与人类活动的关系. 第四纪研究,24(4): 387-393. [Zheng Z,Deng Y,Zhang H,Yu R C,Chen C X. 2004. Holocene environmental changes in the tropical and subtropical areas of the south China and the relation to human activities. Quaternary Sciences,29(4): 837-844]
[26] 中国科学院中国植被图编辑委员会. 2007. 中华人民共和国植被图(1︰1000000). 北京: 地质出版社. [Editorial Committee of Vegetation Map of China,Chinese Academy of Sciences. 2007. Vegetation Map of the People’s Republic of China(1︰1000000). Beijing: Geological Publishing House]
[27] 周宗尧,余国春,董学发,骆丁,宋明义. 2012. 河姆渡早期文化发展间断原因新考. 中国地质,39(2): 550-558. [Zhou Z Y,Yu G C,Dong X F,Luo D,Song M Y. 2012. New Study of the reasons for the interruption of the earliest Hemudu Culture. Geology in China, 39(2): 550-558]
[28] 朱诚,郑朝贵,马春梅,杨晓轩,高锡珍,王海明,邵九华. 2003. 对长江三角洲和宁绍平原一万年来高海面问题的新认识. 科学通报,48(23): 2428-2438. [Zhu C,Zheng C G,Ma C M,Yang X X,Gao X Z, Wang H M,Shao J H. 2003. On the Holocene sea-level highstand along the Yangtze Delta and Ningshao Plain,East China. Chinese Science Bulletin,48(24): 2672-2683]
[29] Brown C A. 2008. Palynological techniques.College Station,Texas,American Association of Stratigraphic Palynologists Foundation.
[30] Chen Z Y,Stanley D J. 1998. Sea-level rise on eastern China’s Yangtze delta. Journal of Coastal Research,14: 360-366.
[31] Chen Z Y,Zong Y Q,Wang Z H,Wang H,Chen J. 2008. Migration patterns of Neolithic settlements on the abandoned Yellow and Yangtze River deltas of China. Quaternary Research,70: 301-314.
[32] Hori K,Saito Y,Zhao Q H,Cheng X R,Wang P X,Sato Y,Li C X. 2001. Sedimentary facies of the tide-dominated paleo-Changjiang(Yangtze)estuary during the last transgression. Marine Geology,177: 331-351.
[33] Jiang L P,Liu L. 2006. New evidence for the origins of sedentism and rice domestication in the Lower Yangzi River,China. Antiquity,80: 355-361.
[34] Li C H,Zhang G Y,Yang L Z. 2006. Pollenand phytolith analyses of ancient paddy fields at Chuodun site,the Yangtze River Delta. Pedosphere,17(2): 209-218.
[35] Maher L J. 1981. Statistics for microfossil concentration measurements employing samples spiked with marker grains. Review of Palaeobotany and Palynology,32: 153-158.
[36] McAndrews J H,Boyko-Diakonow M. 1989. Pollen analysis of varied sediment at Crawford Lake,Ontario: Evidence of Indian and European farming. In: Fulton R J(ed). Geology of Canada and Greenland. Ottawa: Geological Survey of Canada, 528-530.
[37] Morzadec-Kerfourn M T. 2005. Interaction between sea-level changes and the development of littoral herbaceous vegetation and autotrophic dinoflagellates. Quaternary International,133-134: 137-140.
[38] Pederson D C,Peteet D M,Kurdyla D,Guilderson T. 2005. Medieval Warming,Little Ice Age,and European impact on the environment during the last millennium in the lower Hudson Valley,New York,USA. Quaternary Research, 63: 238-249.
[39] Reimer P J,Bard E,Bayliss A,Beck J W,Blackwell P G,Ramsey C B,Buck C E,Cheng H,Edwards R,Friedrich M,Grootes P M,Guilderson T P,Haflidason H,Hajdas I,Hatté C,Heaton T J,Hoffmann D L,Hogg A G,Hughen K A,Kaiser K F. 2013. IntCal 13 and Marine 13 radiocarbon age calibration curves 0-50,000 years cal. B.P. Radiocarbon,55(4): 1869-1887.
[40] Ren G Y,Beug H J. 2002. Mapping Holocene pollen data and vegetation of China. Quaternary Science Reviews,21(12-13): 1395-1422.
[41] Scaife R G. 1988. The elm decline in the pollen record of South East England and its relationship to early agriculture. In: Jones M K(ed). Archaeology and the Flora of the British Isles. Oxford: Oxford University Committee for Archaeology,Monograph,21-33.
[42] Song B,Li Z,Saito Y,Okuno J,Li Z,Lu A Q,Hua D,Li J,Li Y X,Nakashima R. 2013. Initiation of the Changjiang(Yangtze)delta and its response to the mid-Holocene sea level change. Palaeogeography,Palaeoclimatology,Palaeoecology,388: 81-97.
[43] Talma A S,Vogel J C. 1993. A Simplified Approach to Calibrating 14 C Dates. Radiocarbon,35(2): 317-322.
[44] van Soelen E E,Lammertsma E I,Cremer H,Donders T H,Sangiorgi F,Brooks G R,Larson R A,Sinninghe Damsté J S,Wagner-Cremer F,Reichart G J. 2010. Late Holocene sea-level rise in Tampa Bay: Integrated reconstruction using biomarkers,pollen,organic-walled dinoflagellate cysts,and diatoms. Estuarine,Coastal and Shelf Science,86(2): 216-224.
[45] Whittington G,Edwards K J,Caseldine C J. 1991. Late-and postglacial pollen-analytical and environmental data from a near-coastal site in northeast Fife,Scotland. Review of Palaeobotany and Palynology,68(1-2): 65-85.
[46] Zheng Y F,Jiang L P. 2007. Remains of ancient rice unearthedfrom Shangshan site and their significance.Chinese Archaeology,9(1): 159-163.
[47] Zong Y Q. 2004. Mid-Holocene sea-level highstand along the Southeast Coast of China. Quaternary Research,117: 55-67.

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全新世以来浙江余姚河姆渡—田螺山遗址的古环境演变及人类活动^*

Holocene palaeoenvironment evolution and human activity of the Hemudu-Tianluoshan Sites in Yuyao of Zhejiang Province

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全新世以来浙江余姚河姆渡—田螺山遗址的古环境演变及人类活动*

Holocene palaeoenvironment evolution and human activity of the Hemudu-Tianluoshan Sites in Yuyao of Zhejiang Province

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全新世以来浙江余姚河姆渡—田螺山遗址的古环境演变及人类活动^*