姚付龙,朱诚,马春梅,蒋小芳,蔡天赦

• 1:伊犁师范学院生物与地理科学学院
• 2:南京大学地理与海洋科学学院

摘要(Abstract)：

长江三角洲西部地区对气候变化反应敏感,但由于缺乏高分辨率的研究材料使学者们对该区域的气候演变过程有着不同的解释,另外,新石器时代环境演变对长江两岸文化交流与传播的影响也还没有引起学者们的关注,为了解决上述科学问题我们在长江三角洲西部高淳地区获得了一个13200 cal a B.P.以来的406 cm厚湖泊沉积剖面,依据孢粉、腐殖化度、烧失量、元素地球化学等古气候记录重建了13200 cal a B.P.以来的气候演变过程并在此基础上探讨了长江两岸新石器时代文化交流与传播路线,研究表明:13200~4400 cal a B.P.期间气候以暖湿为主要特征,但在早期有波动,属于从冷干向暖湿转化的过渡期,4400 cal a B.P.以来以温凉湿润为主要特征,另外,长江三角洲西部地区13200 cal a B.P.以来的气候演变过程并不稳定,高淳剖面古气候代用指标记录了三次气候突变事件,分别为"新仙女木"事件、"8.2 ka"事件和"4.2 ka"事件,6000~4000 cal a B.P.期间的气候变化过程有利于长江三角洲西部长江两岸新石器时代文化之间的交流与传播,沿古中江两岸分布的考古遗址发掘出土的器物表明古中江是长江两岸文化交流与传播的重要通道。

关键词(KeyWords)： 古气候;环境演变;湖泊记录;气候突变事件;新石器时代;第四纪;长江三角洲

Abstract:

Keywords:

基金项目(Foundation): 国家自然科学基金项目(No.41571179);; 江苏省科技项目(BE2014705)联合资助

作者(Author): 姚付龙,朱诚,马春梅,蒋小芳,蔡天赦

DOI: 10.19839/j.cnki.dcxzz.2018.03.004

参考文献(References)：

• 安志敏.1997.良渚文化及其文明诸因素的剖析.考古,(9):77-81.
• 蔡天赦,朱诚,孙智彬等.2017.长江三峡地区全新世典型遗址与自然沉积剖面环境考古研究的意义.地层学杂志,41(1):32-38.
• 陈洪波.2006.从玉器纹饰看良渚文化宗教信仰中的两类因素.南方文物,(1):49-55.
• 陈杰.2015.崧泽文化的形成.东南文化,(1):57-65.
• 方向明.2010.崧泽文化玉器及其相关问题的研究.东南文化,(6):87-97.
• 方向明.2015.聚落变迁和统一信仰的形成:从崧泽到良渚.东南文化,(1):102-112.
• 郭明建.2014.良渚文化宏观聚落研究.考古学报,(1):1-32.
• 李冰.2014.太湖东部平原平望孔全新世环境演变地层记录.[南京大学博士学位论文].南京:南京大学.1-92.
• 陆福志,朱诚,马春梅等.2015.太湖西部地区8.2 ka BP以来的高分辨率孢粉记录.地层学杂志,39(1):116-123.
• 马雪,于俊杰,蒋仁等.2015.长江三角洲顶部ZKA4钻孔第四纪沉积物粒度特征及其古环境古气候意义.地层学杂志,39(4):423-432.
• 南京博物院,常州博物馆,溧阳文化局.2009.江苏溧阳神墩遗址发掘简报.东南文化,(5):45-58.
• 盛起新.2014.崧泽文化纹饰对良渚文化影响.东南文化,(5):65-79.
• 宋建.2000.关于崧泽文化至良渚文化过渡阶段的几个问题.考古,(11):49-57.
• 朔知,2015.松泽时代皖江两岸的聚落与文化.东南文化,(1):66-78.
• 田名利.1999.凌家滩墓地玉器渊源探寻.东南文化,(5):18-29.
• 唐领余,毛礼米,舒军武等.2016.中国第四纪孢粉图鉴.北京:科学出版社.1-580.
• 王伏雄,钱南芬,张玉龙等.1995.中国植物花粉形态.北京:科学出版社.1-446.
• 吴立,王新源,莫多闻等.2015.巢湖东部含山凌家滩遗址地层元素地球化学特征研究.地层学杂志,39(4):443-453.
• 吴永红,郑祥民,周立旻.2015.太湖8000年来沉积物元素变化特征及古环境指示.盐湖研究,(1):16-21.
• 许鹏飞.2015.试论良渚文化的去向--从良渚文化末期遗存的面貌谈起.东南文化,(5):75-85.
• 许雪珉,William Y B Chang,刘金陵.1996.11000年以来太湖地区的植被与气候变化.古生物学报,35(2):175-186.
• 姚付龙.2017.芜申运河所经古中江流域全新世环境考古研究.[南京大学博士学位论文].南京:南京大学.1-153.
• 张童心,王斌.2014.马家浜文化生成因素三题.东南文化,(1):65-71.
• 张敏.2015.崧泽文化三题.东南文化,(1):49-56.
• 张愈,马春梅,赵宁等.2015.浙江天目山千亩田泥炭晚全新世以来Rb/Sr记录的干湿变化.地层学杂志,39(1):97-107.
• 赵宝成,王张华,陈中原等.2007.太湖平原碟形洼地沉积物记录的距今8000年以来的植被、气候与地貌演变.古地理学报,9(3):321-330.
• 郑建明,陈淳.2005,马家浜文化研究的回顾与展望.东南文化,(4):16-25.
• 仲召兵.2013.环太湖地区崧泽文化末期考古学文化面貌及聚落的变迁--兼谈崧泽文化与良渚文化的分界.东南文化,(3):60-70.
• 周裕兴,王志高,张金喜.2000.江苏高淳县薛城新石器时代遗址发掘简报.考古,(5):1-20.
• 朱诚,吴立,李兰等.2016.对江苏新石器时代海面变化问题的再认识.科学通报,61(3):374-387.
• Blaauw M.2010.Methods and code for“classical”age modeling of radiocarbon sequences.Quaternary Geochronology,5(5):512-518.
• Blackford J J&Chambers F M.1993.Determining the degree of peat decomposition for peat-based palaeoclimatic studies.Int Peat,5:7-24.
• Blundell A,Charman D J&Barber K.2008.Multiproxy late Holocene peat records from Ireland:towards a regional palaeoclimate curve.Journal of Quaternary Science,23(1):59-71.
• Chen W,Wang W M&Dai X R.2009.Holocene vegetation history with implications of human impact in the Lake Chaohu area,Anhui Province,East China.Veget Hist Archaeobot,18(2):137-146.
• Chen X M,Chen F H,Zhou A F,Huang X Z,Tang L Y,Wu D&Zhang XJ.2014.Vegetation history,climate changes and Indian summer monsoon evolution during the Last Glacition(36,400-13,400 Cal yr BP)documented by sediments from Xingyun Lake,Yunnan,China.Palaeogeography,Palaeoclimatology,Palaeoecology,410:179-189.
• Fan J W,Xiao J L,Wen R L,Zhang S R,Wang X,Cui L L,Li H,Xue D S&Yamagata H.2016.Droughts in the East Asian summer monsoon margin during the last 6 kyrs:Link to the North Atlantic cooling events.Quaternary Science Review,151:88-99.
• Grimm E.2011.Tilia and Tiliagraph software 1.7.16.Illinois State Museum,Springfield.
• Grove M K&Bilotta G S.2014.On the use of loss-on-ignition techniques to quantify fluvial particulate organic carbon.Earth Surf.Process Landforms,39:1146-1152.
• Hoogsteen M J J,Lantinga E A,Bakker E J,Groot J C J&Tittonell C.2016.Estimating soil organic carbon through loss on ignition:effects of ignition conditions and structural water loss.European Journal of Soil Science,66:320-328.
• Klapyta P,Zasadni J,Pociask-Karteczka J&Franczak P.2016.Late Glacial and Holocene paleoenvironmental recorda in the Tatra Mountains,East-Central Europe,based on lake,peat bog and colluvial sedimentary data:a summary review.Quaterynary International,415(1):126-144.
• Kulkarni C,Peteet D&Boger R.2016.Exploring the role of humans and climate over the Balkan landscape:500 years of vegetational history of Serbis.Quaternary Science Review,144:83-94.
• Li Y P,Ma C M,Zhou B,Cui A N,Zhu C,Huang R&Zheng C G.2016.Environmental processes derived from peatland geochemistry since the last deglaciation in Dajiuhu,Shennongjia,central China.Boreas,45(3):423-438.
• Ma C M,Zhu C,Zheng C G,Yin Q&Zhao Z P.2009.Climate changes in East China since the Late-glacial inferred from high-resolution moution peat humification records,Science in China(Series D:Earth Science,52(1):118-131.
• Nakagawa T,Brugiapaglia E,Digerfeldt G&Yasuda Y.2010.Dense-media separation as a more efficient pollen extraction method for use with organic sediment samples:comparison with the conventional method.Boreas,27(1):15-24.
• Novenko E Y,Tsyganov A N,Volkova E M,Kupriyanov D A,Mironenko I V,Babeshko K V,Utkina A S,Popov V&Mazei Y A.2016.Mid-and Late Holocene vegetation dynamics and fire history in the boreal forest of European Russia:a case study from Meshchera Lowlands.Palaeogeography,Palaeoclimatology,Palaeoecology,459:570-584.
• Qiu Z W,Jiang H G,Ding J L,Hu Y&Shang X.2014.Pollen and phytolith Evidence for Rice Cultivation and Vegetation Change during the Mid-Late Holocene at the Jiangli Site,Suzhou,East China.Plos One,9(5):e97541.
• Qu W C,Xue B,Dickman M D,Wang S M,Fan C X,Wu R J,Zhang P Z,Chen J F&Wu Y H.2000.A 14000-year record of paleoenvironmental change in the western basin of China's third largest lake,Lake Taihu.Hydrobiologia,432(1-3):113-120.
• Ter Braak C J F&Smilauer P.2002.CANOCO Reference Manual and Canodrew for Windows User's Guide:Software for Canonical Community Ordination(Version 4.5).Ithaca,NY:Micorocomputer Power.
• Wang Q R,Li Y C&Wang Y.2011.Optimizing the weight loss-on-ignition methodology to quantify organic and carbonate carbon of sediments from diverse sources.Environ Monit Assess,174(1-4):241-257.
• Wu L,Li F,Zhu C&Li B.2012.Holocene environmental change and archaeology,Yangtze River Valley,China:review and prospects.Geoscience frontiers,3(6):875-892.
• Wu L,Zhu C,Zheng C G,Li F,Wang X H,Li L&Sun W.2014.Holocene environmental change and its impacts on human settlement in the Shanghai Area,East China.Catena,114(2):78-89.
• Wu L,Zhu C,Zheng C G,Ma C M,Wang X H,Li F,Li B&Li K F.2014b.Impact of Holocene climate change on the prehistoric cultures of Zhejiang region,East China.Journal of Geographical Sciences,24(4):669-688.
• Wu Y,Liang L P,Zhang Y F&Zhao Z.2014c.Morphological trend analysis of rice phytolith during the early Neolithic in the Lower Yangtze.Journal of Archaeological Science,49(1):326-331.
• Wu W X&Liu D S.2002.5500 a BP climatic event and its implications for the emergence of civilizations in Egypt and Mesopotamia and Neolithic cultural development in China.Earth Science Frontiers,(1):155-162.
• Yang X D,Wang S M&Tong G B.1996.Character of a nology and changes of monsoon climate over the last 10000 years in Gucheng Lake,Jiangsu province.Act a Botannica Sinica,38(7):576-581.
• Yao F L,Ma C M,Zhu C,Li J Y,Chen G,Tang L Y,Huang M,Jia T J&Xu J J.2017.Holocene climate change in the western part of Taihu Lake region,East China.Palaeogeography,Palaeoclimatology,Palaeoecology,485:963-973.