Abstract This study assesses the historical lakes in the lower reaches of the Yellow River using ancient documents,estimating the general shape and approximate area of over 130 ancient lakes during historical times. We have meticulously analyzed the extinction process of these ancient lakes and discussed the factors contributing to their demise. Our findings reveal that during the historical period,there were at least 135 lakes in the lower reaches of the Yellow River,covering a total area of 16195.64 km2. These lakes were primarily situated along the ancient channel of the Yellow River,with small and medium-sized lakes(areas under 100 km2)constituting the majority. These smaller lakes accounted for 74.81% of the total number of lakes and 30.23% of the total area. Since the Song Dynasty,there has been a noticeable shrinkage in these ancient lakes. Among the smaller and medium-sized paleolakes,60.34% of 135 lakes have disappeared. Only 28 ancient lakes remain today,marking a decline of 79.26% in their number,and their total area has reduced to 4910.66 km2,a decrease of 69.68%. The study suggests climate change is the background for the extinction of ancient lakes. The sediment accumulation caused by the Yellow River avulsion and flooding is the direct reason for the disappearance of these ancient lakes. Meanwhile,human activities such as land reclamation around the lakes have accelerated this process.
Fund:National Natural Science Foundation of China(Nos. 41871073,41701101),the Postgraduate Research Innovation Program of Jiangsu Normal University(No.2022XKT0081),the Priority Academic Program Development of Jiangsu Higher Education Institutions
Corresponding Authors:
CHEN Shiyue,born in 1969,a professor of Jiangsu Normal University,is engaged in lacustrine sedimentology and environmental evolution. E-mail: chenshiyue@jsnu.edu.cn.
About author: RU Tinglin,born in 2000,a master degree candidate of Jiangsu Normal University,is engaged in lacustrine sedimentology. E-mail: rutinglin2021@163.com.
Cite this article:
RU Tinglin,CHEN Yingying,LI Xinze et al. Distribution and extinction of paleolakes in the lower reaches of Yellow River during historical period[J]. JOPC, 2024, 26(1): 230-240.
RU Tinglin,CHEN Yingying,LI Xinze et al. Distribution and extinction of paleolakes in the lower reaches of Yellow River during historical period[J]. JOPC, 2024, 26(1): 230-240.
[1] 陈蕴真. 2013. 黄河泛滥史: 从历史文献分析到计算机模拟. 南京大学博士学位论文: 1-188. [Chen Y Z.2013. Investigating the flood history of the Yellow River: from analyzing historical records to computer modeling. Doctoral dissertation of Nanjing University: 1-188] [2] 邓辉,罗潇. 2011. 历史时期分布在北京平原上的泉水与湖泊. 地理科学, 31(11): 1355-1361. [Deng H,Luo X.2011. Spatial distribution of the lakes and seepage springs on the Beijing Plain in history. Scientia Geographica Sinica, 31(11): 1355-1361] [3] 邓辉,李羿. 2018. 人地关系视角下明清时期京津冀平原东淀湖泊群的时空变化. 首都师范大学学报(社会科学版),(4): 95-105. [Deng H,Li Y.2018. On the spatiotemporal changes of the Dongdian Lake group in the Beijing-Tianjin-Hebei plain during the Ming and Qing Dynasties from the perspective of man-land relationship. Journal of Capital Normal University(Social Sciences Edition),(4): 95-105] [4] 邓辉,卜凡. 2020. 历史上冀中平原“塘泺”湖泊群的分布与水系结构. 地理学报, 75(11): 2332-2345. [Deng H,Bu F.2020. Spatial distribution of the Tang Po Lakes upon the Central Hebei Plain during the Northern Song Dynasty. Acta Geographica Sinica, 75(11): 2332-2345] [5] 方金琪. 1989. 我国历史时期的湖泊围垦与湖泊退缩. 地理环境研究, 1(1): 71-78. [Fang J Q.1989. Relationships between lake evolution and land reclamation in history of China. Geographic Environment Research, 1(1): 71-78] [6] 葛全胜,郑景云,郝志新,刘浩龙. 2012. 过去2000年中国气候变化的若干重要特征. 中国科学: 地球科学, 42(6): 934-942. [Ge Q S,Zheng J Y,Hao Z X,Liu H L.2012. General characteristics of climate changes during the past 2000 years in China. Science China: Earth Science, 42(6): 934-942] [7] 龚志强,封国林,万仕全,李建平. 2006. 基于启发式分割算法检测华北和全球气候变化的特征. 物理学报, 55(1): 477-484. [Gong Z Q,Feng G L,Wan S Q,Li J P.2006. Analysis of features of climate change of Huabei area and the global climate change based on heuristic segmentation algorithm. Acta Physica Sinica, 55(1): 477-484] [8] 古帅. 2021. 铜瓦厢决口后黄河下游河道沿岸区域地形与河湖环境(1855—1911). 历史地理研究, 41(3): 46-64,154. [Gu S.2021. Topography and river-lake environment along the lower Yellow River after tongwaxiang breach(1855-1911). The Chinese Historical Geography, 41(3): 46-64,154] [9] 郭永盛. 1990. 历史上山东湖泊的变迁. 海洋湖沼通报,(3): 15-22. [Guo Y S.1990. On historical change of lakes in Shandong Province. Transactions of Oceanology and Limnology,(3): 15-22] [10] 郭予庆. 1991. 河南地理环境的历史变迁. 河南大学学报(自然科学版), 21(1): 73-76,72. [Guo Y Q.1991. Historical changes of geographical environment in Henan Province. Journal of Henan University(Natural Science), 21(1): 73-76,72] [11] 何乃华,朱宣清. 1992. 白洋淀地区近3万年来的古环境与历史上人类活动的影响. 海洋地质与第四纪地质, 12(2): 79-88. [He N H,Zhu X Q.1992. Palaeoenvironment changes since 30 000 a B. P. and effects of human activities in the Baiyangdian area. Marine Geology & Quaternary Geology, 12(2): 79-88] [12] 侯战方,陈诗越,孟静静,刘加珍,刘晓迪,魏本杰,孙莉,陈影影,刘子亭,肖燕. 2018. 近1200a来黄河下游梁山泊沉积记录的环境变迁. 湖泊科学, 30(1): 245-255. [Hou Z F,Chen S Y,Meng J J,Liu J Z,Liu X D,Wei B J,Sun L,Chen Y Y,Liu Z T,Xiao Y.2018. Environmental changes in the lower reaches of Yellow River area during the last 1200 years revealed by multiple proxies from the Lake Liangshanpo. Journal of Lake Sciences, 30(1): 245-255] [13] 李明启,靳鹤龄,张洪. 2005. 小冰期气候的研究进展. 中国沙漠, 25(5): 731-737. [Li M Q,Jin H L,Zhang H.2005. Advances of climate research in the Little Ice Age. Journal of Desert research, 25(5): 731-737] [14] 李云鹏,郭姝姝,朱正强. 2021. 近2000年鲁西南地区河湖水系水环境变迁脉络研究. 中国水利水电科学研究院学报, 19(4): 381-389. [Li Y P,Guo S S,Zhu Z Q.2021. Study on water environmental changes of rivers and lakes in generalized southwest Shandong in almost 2000 years. Journal of China Institute of Water Resources and Hydropower Research, 19(4): 381-389] [15] 卢卓瑜,崔建新,张晓虹,李鹏. 2021. 清至民国毛乌素沙地佟哈拉克泊复原及演变研究. 干旱区地理, 44(4): 1083-1092. [Lu Z Y,Cui J X,Zhang X H,Li P.2021. Historical changes reconstruction of Tonghalake Lake in the Mu Us Sandy Land from Qing Dynasty to Republic of China. Arid Land Geography, 44(4): 1083-1092] [16] 秦磊. 2012. 天津七里海古潟湖湿地环境演变研究. 湿地科学, 10(2): 181-187. [Qin L.2012. The environmental evolution of the Qilihai ancient Lagoon Wetlands in Tianjin. Wetland Science, 10(2): 181-187] [17] 谭其骧. 1982. 中国历史地图集. 第一册. 北京: 中国地图出版社, 3-46. [Tan Q X.1982. The Historical Atlas of China.Volume 1. Beijing: China Cartographic Publishing House, 3-46] [18] 谭徐明. 2002. 海河流域水环境的历史演变及其主要影响因素研究. 水利发展研究, 2(12): 15-20. [Tan X M.2002. Study on the historical evolution of water environment in Haihe River Basin and its main influencing factors. Water Resources Development Research, 2(12): 15-20] [19] 田世英. 1982. 黄河流域古湖钩沉. 山西大学学报(哲学社会科学版), 5(2): 33-41. [Tian S Y.1982. The ancient lakes in the Yellow River Basin are hooked and sunk. Journal of Shanxi University(Philosophy and Social Science Edition), 5(2): 33-41] [20] 万玮,肖鹏峰,冯学智,李晖,马荣华,段洪涛,赵利民. 2014. 卫星遥感监测近30年来青藏高原湖泊变化. 科学通报, 59(8): 701-714. [Wan W,Xiao P F,Feng X Z,Li H,Ma R H,Duan H T,Zhao L M.2014. Monitoring lake changes of Qinghai-Tibetan Plateau over the past 30 years using satellite remote sensing data. Chinese Science Bulletin, 59(8): 701-714] [21] 王长松,段蕴歆,张然. 2021. 历史时期黄河流域城市空间格局演变与影响因素. 自然资源学报, 36(1): 69-86. [Wang C S,Duan Y X,Zhang R.2021. Spatial pattern evolution of cities and influencing factors in the historical Yellow River Basin. Journal of Natural Resources, 36(1): 69-86] [22] 王会昌. 1983. 一万年来白洋淀的扩张与收缩. 地理研究, 2(3): 8-18. [Wang H C.1983. Expansion and contraction of the Baiyangdian Lake since 10 000 years ago. Geographical Research, 2(3): 8-18] [23] 王苏民,窦鸿身. 1989. 中国湖泊志. 北京: 科学出版社, 1-531. [Wang S M,Dou H S.1989. Annals of Lakes in China. Beijing: Science Press, 1-531] [24] 魏显虎,杜耘,蔡述明,张婷婷,刘韬. 2007. 湖北省湖泊演变及治理对策. 湖泊科学, 19(5): 530-536. [Wei X H,Du Y,Cai S M,Zhang T T,Liu T.2007. On the evolution of lakes in Hubei Province and countermeasures. Journal of Lake Sciences, 19(5): 530-536] [25] 吴忱,许清海. 1998. “演变阶段”与“成因”不能混为一谈: 也谈白洋淀的成因. 湖泊科学, 10(3): 91-96. [Wu C,Xu Q H.1998. Formation or development stage: a discussion on the cause of the formation of Baiyangdian Lake,China. Journal of Lake Sciences, 10(3): 91-96] [26] 吴忱,许清海,刘劲松. 2017. 华北地貌新论. 北京: 科学出版社, 149-151. [Wu C,Xu Q H,Liu J S.2017. New Geomorphology of North China. Beijing: Science Press, 149-151] [27] 杨桂山,马荣华,张路,姜加虎,姚书春,张民,曾海鳌. 2010. 中国湖泊现状及面临的重大问题与保护策略. 湖泊科学, 22(6): 799-810. [Yang G S,Ma R H,Zhang L,Jiang J H,Yao S C,Zhang M,Zeng H A.2010. Lake status,major problems and protection strategy in China. Journal of Lake Sciences, 22(6): 799-810] [28] 尹玲玲. 2000. 从明代河泊所的置废看湖泊分布及演变: 以江汉平原为例. 湖泊科学, 12(1): 38-46. [Yin L L.2000. Lake evolution of Jianghan Plain: a case study of the Hebosuo reduction & emergence in the Ming Dynasty. Journal of Lake Sciences, 12(1): 38-46] [29] 喻宗仁,窦素珍,赵培才,刘桂成,张成,裴放. 2004. 山东东平湖的变迁与黄河改道的关系. 古地理学报, 6(4): 469-479. [Yu Z R,Dou S Z,Zhao P C,Liu G C,Zhang C,Pei F.2004. Relationship between changes of Dongping Lake and shifting of the Yellow River in Shandong Province. Journal of Palaeogeography(Chinese Edition), 6(4): 469-479] [30] 袁祖贵,楚泽涵,杨玉珍. 2005. 关于黄河三角洲地区莱州湾南岸平原湖泊消亡原因的讨论. 古地理学报, 7(2): 283-286. [Yuan Z G,Chu Z H,Yang Y Z.2005. Discussion on reasons of disappearance of lakes in south coast plain of Laizhou Bay near Yellow River Delta Area. Journal of Palaeogeography(Chinese Edition), 7(2): 283-286] [31] 张民服. 1988. 黄河下游段河南湖泽陂塘的形成及其变迁. 中国农史, 7(2): 40-47. [Zhang M F.1988. The formation and change of lakes in the lower reaches of the Yellow River in Henan. Agricultural History of China, 7(2): 40-47] [32] 张维英,韩美,李艳红. 2003. 山东莱州湾南岸平原古湖泊消亡原因初探. 古地理学报, 5(2): 224-231. [Zhang W Y,Han M,Li Y H.2003. The causes of disappearance of ancient lakes in south coast plain of Laizhou Bay,Shandong Province. Journal of Palaeogeography(Chinese Edition), 5(2): 224-231] [33] 张祖陆,聂晓红,卞学昌. 2004. 山东小清河流域湖泊的环境变迁. 古地理学报, 6(2): 226-233. [Zhang Z L,Nie X H,Bian X C.2004. Environmental change of lakes in Xiaoqinghe River drainage,Shandong Province. Journal of Paleogeography(Chinese Edition), 6(2): 226-233] [34] 朱玲玲,陈剑池,袁晶,董炳江. 2014. 洞庭湖和鄱阳湖泥沙冲淤特征及三峡水库对其影响. 水科学进展, 25(3): 348-357. [Zhu L L,Chen J C,Yuan J,Dong B J.2014. Sediment erosion and deposition in two lakes connected with the middle Yangtze River and the impact of Three Gorges Reservoir. Advances in Water Science, 25(3): 348-357] [35] 邹逸麟. 1980. 黄河下游河道变迁及其影响概述. 复旦学报(社会科学版),22(S1): 12-24. [Zou Y L.1980. A summary of the changes of the lower reaches of the Yellow River and its influence. Fudan Journal(Social Sciences Edition),22(S1): 12-24] [36] 邹逸麟. 1987. 历史时期华北大平原湖沼变迁述略. 历史地理,(1): 25-39. [Zou Y L.1987. A brief narration on the changes of the lakes and marshes on the Huabei Plain during the historical periods. The Chinese Historical Geography,(1): 25-39] [37] 邹逸麟. 1997. 黄淮海平原历史地理. 安徽合肥: 安徽教育出版社, 176-206. [Zou Y L.1997. Historical Geography of Huang-Huai-Hai Plain. Anhui Hefei: Anhui Education Press, 176-206] [38] 邹逸麟. 2013. 中国历史自然地理. 北京: 科学出版社, 3-511. [Zou Y L.2013. Historical Physical Geography in China. Beijing: Science Press, 3-511] [39] Ge Q S,Zheng J Y,Fang X Q,Man Z M,Zhang X Q,Zhang P Y,Wang W C.2003. Winter half-year temperature reconstruction for the middle and lower reaches of the Yellow River and Yangtze River,China,during the past 2000 years. The Holocene, 13(6): 933-940. [40] Chen Y Z,Syvitski J P M,Gao S,Overeem I,Kettner A J.2012. Socio-economic impacts on flooding: a 4000-year history of the Yellow River,China. AMBIO, 41(7): 682-698. [41] Li W J,Yu S Y,Pan J R,Cao X Y,Chen Y Y,Wang Y.2021. A 2000-year documentary record of levee breaches on the lower Yellow River and their relationship with climate changes and human activities. The Holocene, 31(3): 333-345. [42] Marshall M H,Lamb H F,Huws D,Davies S J,Bates R,Bloemendal J,Boyle J,Leng M J,Umer M,Bryant C.2011. Late Pleistocene and Holocene drought events at Lake Tana,the source of the Blue Nile. Global and Planetary Change, 78(3-4): 147-161.