豫北平原全新世孢粉记录气候变化与古文化演替

doi:10.13278/j.cnki.jjuese.201605115

吉林大学学报(地球科学版) ›› 2016, Vol. 46 ›› Issue (5): 1449-1457.doi: 10.13278/j.cnki.jjuese.201605115

豫北平原全新世孢粉记录气候变化与古文化演替

李贶家^1,2, 顾延生^2,3, 刘红叶²

1. 天津大学环境科学与工程学院, 天津 300072;
2. 中国地质大学(武汉)生物地质与环境地质国家重点实验室, 武汉 430074;
3. 中国地质大学(武汉)湿地演化与生态恢复湖北省重点实验室, 武汉 430074

收稿日期:2015-02-21 出版日期:2016-09-26 发布日期:2016-09-26
通讯作者: 顾延生(1970-),男,教授,博士,主要从事全球变化与生态响应研究,E-mail:ysgu@cug.edu.cn E-mail:ysgu@cug.edu.cn
作者简介:李贶家(1989-),男,博士研究生,主要从事环境科学领域学习与研究,E-mail:eugenevanlee@gmail.com
基金资助:
国家自然科学基金项目（41072261，40930210）；生环国重自主课题（GBL11203）

Holocene Climate Changes Derived from Spore-Pollen Records and Neolithic Culture Succession in Northern Henan Plain

Li Kuangjia^1,2, Gu Yansheng^2,3, Liu Hongye²

1. School of Environmental Science and Engineering, Tianjin University, Tianjin 300072, China;
2. State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China;
3. Hubei Key Laboratory of Wetland Evolution & Eco-Restoration(WEER), China University of Geosciences, Wuhan 430074, China

Received:2015-02-21 Online:2016-09-26 Published:2016-09-26
Supported by:
Supported by National Natural Science Foundation of China (41072261, 40930210) and Autonomous Subject of State Key Laboratory of Biogeology and Environmental Geology (GBL11203)

摘要/Abstract

摘要：

在¹⁴C测年和岩石学的基础上，对豫北平原全新世钻孔沉积物孢粉分析，发现了蒿属、藜科、禾本科、菊科、莎草科、香蒲属6大科属草本，桦属、栎属、榆属3大科属阔叶类，以及裸子植物和蕨类各2种。孢粉含量具有6阶段的组合特征，分别对应6个时期的古气候与古环境演化：10 200~8 200 cal BP，气候冷湿，8 200 cal BP处指示了一次较大的降温事件；8 200~4 000 cal BP，温湿条件有波动，整体上显示了全新世中期整体暖湿气候的特征；4 000~3 300 cal BP，湿度较4 000 cal BP时降低，气候由冷湿向冷干转变；3 300~2 400 cal BP，整体呈寒冷干旱的气候特征；2 400~1 350 cal BP，温度小幅回升，降水增加，气候变暖变湿；1 350 cal BP迄今，温度小幅回落，气候较为干凉。总体上呈“凉湿-暖湿-凉干”的变化特征，各对应时期的裴李岗文化、仰韶文化和龙山文化分别呈现出“欠兴旺-兴旺-衰落”的景象。全新世气候的变化对古文化的兴衰演替有着决定性的影响。温度和湿度升高时期，受水热配置影响，喜湿热动植物增多，植被茂盛，原始农牧业生产力上升，物质相对丰富，人口增加，文化遗址单个规模、密度增大，显示出古文化兴旺的景象；反之，原始农牧业生产力下降，物质相对匮乏，文化遗址单个规模、密度相对变小，显示出古文化衰落的景象。本文研究结果初步表明中原地区中、晚全新世古气候变化与古文化兴衰之间有着很好的耦合关系。

关键词: 豫北平原, 全新世, 孢粉记录, 考古记录, 气候变化, 文化演替

Abstract:

Based on lithology and ¹⁴C dating survey, a spore-pollen analysis of Holocene sediments in northern Henan Plain was conducted. 6 grass, species, 3 species broad-leaved tree species, 2 gymnosperm tree species, and 2 fern species are found. The spore-pollen assemblages are divided into 6 zones that demonstrate a history of palaeoclimate and palaeoenvironment changes, which indicates an evolvement trend of cool-wet→warm-humid→cool-dry. 10 200-8 200 cal BP,the temperature and humidity were both low, a significant cooling event could be found in 8 200 cal BP;8 200-4 000 cal BP,the spore-pollen assemblage indicated the humid-warm climate in the mid Holocene;4 000-3 300 cal BP,the humidity was lower than that of 4 000 cal BP, the paleoclimate was becoming cold-dry;3 300-2 400 cal BP,the palaeoclimate remained cold-dry in this period; 2 400-1 350 cal BP, climate got warm and humid; from 1 350 cal BP up to now, temperature fell down. The corresponding Peiligang culture, Yangshao culture and Longshan culture, showed a "less developed→prosperous→decayed" trend. The Holocene climate changes had a decisive influence on the ancient culture succession. During the period of high temperature and humidity, the increasing of vegetation, primitive farming productivity, population, and ancient cultural sites indicates the ancient cultural prosperity. On the contrary, primitive farming productivity, population and ancient cultural sites decreased when temperature and humidity drop. This indicates a decay of the ancient cultures. Generally speaking, ancient cultural development corresponds to the paleoclimate changes.

Key words: northern Henan Plain, Holocene, spore-pollen, archaeological sites, climate change, culture succession

中图分类号:

P534.63

李贶家, 顾延生, 刘红叶. 豫北平原全新世孢粉记录气候变化与古文化演替[J]. 吉林大学学报(地球科学版), 2016, 46(5): 1449-1457.

Li Kuangjia, Gu Yansheng, Liu Hongye. Holocene Climate Changes Derived from Spore-Pollen Records and Neolithic Culture Succession in Northern Henan Plain[J]. Journal of Jilin University(Earth Science Edition), 2016, 46(5): 1449-1457.

参考文献

[1] 吴文祥, 刘东生. 5500aBP气候事件在三大文明古国古文明和古文化演化中的作用[J]. 地学前缘,2002, 9(1):155-162. Wu Wenxiang, Liu Tungsheng. 5500aBP Climate Event and Its Implications for the Emergence of Civilizations in Egypt and Mesopotamia and Neolithic Cultural Development in China[J]. Earth Science Frontiers, 2002, 9(1):155-162.

[2] Weiss H, Bradley R. What Drives Societal Collapse?[J]. Science, 2001, 291(5504):609-610.

[3] Perry C A, Hsu K J. Geophysical, Archaeological, and Historical Evidence Support a Solar-Output Model for Climate Change[J]. Proc Natl Acad Sci U S A, 2000, 97(23):12433-12438.

[4] Demenocal P B. Cultural Responses to Climate Change During the Late Holocene[J]. Science, 2001, 292(5517):667-673.

[5] Sandweiss Daniel H, Maasch Kirk A, Anderson David G. Transitions in the Mid-Holocene[J]. Science, 1999, 283(5401):499-500.

[6] 吴文祥, 刘东生. 4000aB.P.前后降温事件与中华文明的诞生[J]. 第四纪研究, 2001, 21(5):443-451. Wu Wenxiang, Liu Tungsheng. 4000aB.P. Event and Its Implications for the Origin of Ancient Chinese Civilization[J]. Quaternary Sciences, 2001, 21(5):443-451.

[7] 吴文祥, 葛全胜. 全新世气候事件及其对古文化发展的影响[J]. 华夏考古, 2005(3):60-67. Wu Wenxiang, Ge Quansheng. Climatic Events of the Recent Epoch and Their Influence upon the Development of Ancient Culture[J]. Huaxia Archaeology, 2005(3):60-67.

[8] 江林昌. 夏商周文明新探[M]. 杭州:浙江人民出版社, 2001. Jiang Linchang. New Exploration of Xia, Shang, Zhou Civilization[M]. Hangzhou:Zhejiang People's Publishing House, 2001.

[9] 张立原. 中国黄土高原洛川剖面S5以来的孢粉学记录[J].吉林大学学报(地球科学版), 2014, 44(1):222-229. Zhang Liyuan. Palynological Records from the Luochuan Section of the Chinese Loess Plateau Since S5 Stage[J]. Journal of Jilin University(Earth Science Edition), 2014, 44(1):222-229.

[10] Chen Zhongyuan, Wang Zhanghua, Schneiderman Jill, et al. Holocene Climate Fluctuations in the Yangtze Delta of Eastern China and the Neolithic Response[J]. The Holocene, 2005, 15(6):915-924.

[11] 羊向东, 王苏民, 薛滨, 等. 晚更新世以来呼伦湖地区孢粉植物群发展与环境变迁[J]. 古生物学报, 1995, 34(5):647-656. Yang Xiangdong, Wang Sumin, Xue Bin, et al. Vegetational Development and Environmental Changes in Hulun Lake Since Late Pleistocene[J]. Acta Palaeontologica Sinica, 1995, 34(5):647-656.

[12] 顾延生, 喻建新, 谢树成, 等. 江汉平原5000年来气候演变的孢粉、植硅体记录[J]. 地球科学:中国地质大学学报, 2007, 32(增刊1):133-140. Gu Yansheng, Yu Jianxin, Xie Shucheng, et al. Palaeoclimate Changes Derived from the Records of Core Sediments Spore-Pollen and Phytolith in the Jianghan Plain over the Past 5000 Years[J]. Earth Science:Journal of China University of Geosciences, 2007, 32(Sup.1):133-140.

[13] Huang Xianyu, Xue Jiantao, Wang Xinxin, et al. Paleoclimate Influence on Early Diagenesis of Plant Triterpenes in the Dajiuhu Peatland, Central China[J]. Geochimica et Cosmochimica Acta, 2013, 123:106-119.

[14] Xie Shucheng, Zhang Shihong, Gu Yansheng, et al. Concordant Monsoon-Driven Postglacial Hydrological Changes in Peat and Stalagmite Records and Their Impacts on Prehistoric Cultures in Central China[J]. Geology, 2013, 41(8):827.

[15] 杨育彬, 袁广阔. 20世纪河南考古发现与研究[M]. 郑州:中州古籍出版社, 1997. Yang Yubin, Yuan Guangkuo. The Archaeological Discoveries and Studies of Henan in the 20th Century[M]Zhengzhou:Zhongzhou Ancient Books Publishing House, 1997.

[16] 张居中, 潘伟彬. 河南舞阳贾湖遗址2001年春发掘简报[J]. 华夏考古, 2002(2):14-30. Zhang Juzhong, Pan Weibin. Henan Jiahu Excavation Report in the Spring of 2001[J]. Huaxia Archaeology, 2002(2):14-30.

[17] 耿青岩. 河南淇县花窝遗址试掘[J]. 考古, 1981(3):279-281. Geng Qingyan. Excavation of Huawo Site in Qixian, Henan[J]. Archaeology, 1981(3):279-281.

[18] 郭书元, 孙长虹. 河南濮阳西水坡新石器时代遗址瓣鳃类动物群的生态环境分析[J]. 古地理学报, 2003, 5(4):450-460. Guo Shuyuan, Sun Changhong. An Ecological Environmental Analysis of Pelecypoda from Neolithic Xihuipo Site in Puyang City of Henan Province[J]. Journal of Palaeogeography, 2003, 5(4):450-460.

[19] 贾兰坡, 张振标. 河南淅川县下王岗遗址中的动物群[J]. 文物, 1977(6):41-49. Jia Lanpo, Zhang Zhenbiao. Fauna of Xiawanggan Site in Xichuan, Henan[J]. Cultural Relics, 1977(6):41-49.

[20] 朱彦民. 商代晚期中原地区生态环境的变迁[J]. 南开学报(哲学社会科学版), 2006(5):54-61. Zhu Yanmin. The Ecological Changing of North China in Late Shang Period[J]. Nankai Journal(Philosophy, Literature and Social Science Edition), 2006(5):54-61.

[21] 刘东生, 丁梦麟. 黄土高原·农业起源·水土保持[M]. 北京:地震出版社, 2004. Liu Dongsheng, Ding Mengli n. Loess Plateau·Agriculture Origin·Water and Soil Conservation[M]. Beijing:Seismological Publishing House, 2004.

[22] 俞伟超. 龙山文化与良渚文化衰变的奥秘[J]. 文物天地, 1992(3):9-11. Yu Weichao. Mystery of Longshan Culture and Liangzhu Culture Decay[J]. Cultural Relics World, 1992(3):9-11.

[23] 施雅风, 孔昭宸. 中国全新世大暖期的气候波动与重要事件[J]. 中国科学:B辑, 1992(12):1300-1308. Shi Yafeng, Kong Zhaochen. Climate Fluctuations and Important Events of China Holocene Megathermal[J]. Science in China:Series B, 1992(12):1300-1308.

[24] 高广仁. 海岱区先秦考古论集[M]. 北京:科学出版社, 2000. Gao Guangren. Treatises on Archaeology of the Haidai Region in Pre-Qin Times[M]. Beijing:Science Press, 2000.

[25] 施少华. 中国全新世高温期中的气候突变事件及其对人类的影响[J]. 海洋地质与第四纪地质, 1993,13(4):65-73. Shi Shaohua. Climatic Abrupt Change Events and Their Impact on Human Civilization During Holocene Megathermal in China[J]. Marine Geology & Quaternary Geology, 1993, 13(4):65-73.

[26] 靳桂云, 刘东生. 华北北部中全新世降温气候事件与古文化变迁[J]. 科学通报, 2001, 46(20):1725-1730. Jin Guiyun, Liu Dongsheng. Holocene Cold Events and Ancient Cultural Transition in the Northern Part of North China[J]. Chinese Science Bulletin, 2001, 46(20):1725-1730.

[27] 方修琦, 葛全胜, 郑景云. 环境演变对中华文明影响研究的进展与展望[J]. 古地理学报, 2004, 6(1):85-94. Fang Xiuqi, Ge Quansheng, Zheng Jingyun. Progress and Prospect of Researches on Impacts of Environmental Changes on Chinese Civilization[J]. Journal of Palaeogeography, 2004, 6(1):85-94.

[28] 杨钟健, 刘东生. 安阳殷墟哺乳动物群補遗[J]. 考古学报, 1949(4):145-153. Yang Zhongjian, Liu Dongsheng. Additional Mammalian Fauna of the Yin Ruins in Anyang[J]. Acta Archaeologica Sinica, 1949(4):145-153.

[29] 马世之. 新郑郑韩故城[J]. 中原文物, 1978(2):54-55. Ma Shizhi. Zheng-Han Gucheng in Xinzheng[J]. Cultural Relics of Central China, 1978(2):54-55.

[30] 宋治民. 战国秦汉考古[M]. 成都:四川大学出版社, 1993. Song Zhimin. Archaelogy of Warring States Period, Qin and Han Dynasties[M]. Chengdu:Sichuan University Press, 1993.

[31] 吴文祥, 刘东生. 4000 aB.P.前后东亚季风变迁与中原周围地区新石器文化的衰落[J]. 第四纪研究, 2004, 24(3):278-284. Wu Wenxiang, Liu Dongsheng. Variations in East Asia Monsoon Around 4000 aB.P. and the Collapse of Neolithic Cultures Around Central Plain[J]. Quaternary Sciences, 2004, 24(3):278-284.

[32] 吴文祥, 葛全胜. 夏朝前夕洪水发生的可能性及大禹治水真相[J]. 第四纪研究, 2005, 25(6):741-749. Wu Wenxiang, Ge Quansheng. The Possibility of Occurring of the Extraordinary Floods on the Eve of Establishment of the Xia Dynasty and the Historical Truth of Dayu's Successful Regulating of Floodwaters[J]. Quaternary Sciences, 2005, 25(6):741-749.

[33] 许清海, 曹现勇, 王学丽, 等. 殷墟文化发生的环境背景及人类活动的影响[J]. 第四纪研究, 2010, 30(2):273-286. Xu Qinghai, Cao Xianyong, Wang Xueli, et al. Generation of Yinxu Culture:Environmental Background and Impacts of Human Activities[J]. Quaternary Sciences, 2010, 30(2):273-286.

[34] 张振卿, 许清海, 李月丛, 等. 殷墟地区土壤剖面孢粉组合特征及环境意义[J]. 第四纪研究, 2007, 27(3):461-468. Zhang Zhenqing, Xu Qinghai, Li Yuecong, et al. Environmental Changes of the Yin Ruins Area Based on Pollen Analysis[J]. Quaternary Sciences, 2007, 27(3):461-468.

[35] 陈钦龙. 郑韩故城考古发现与初步研究[D]. 郑州:郑州大学, 2007. Chen Qinlong. Archaeological Discovery and Preliminary Study in Zheng-Han Gucheng[D]. Zhengzhou:Zhengzhou University, 2007.

[36] 刘雄. 山彪镇与玻璃阁再研究[D]. 北京:首都师范大学, 2009. Liu Xiong. Further Study of Town Shanbiao and Glass Pavilion[D]. Beijing:Capital Normal University, 2009.

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豫北平原全新世孢粉记录气候变化与古文化演替

Holocene Climate Changes Derived from Spore-Pollen Records and Neolithic Culture Succession in Northern Henan Plain

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