中国东部全新世以来海面波动特征探讨

doi:10.11867/j.issn.1001-8166.2002.06.0886

地球科学进展 ›› 2002, Vol. 17 ›› Issue (6): 886 -894. doi: 10.11867/j.issn.1001-8166.2002.06.0886

中国东部全新世以来海面波动特征探讨

沈明洁 ¹，谢志仁 ²，朱诚 ¹

1.南京大学城市与资源学系，江苏南京 210093；2.南京师范大学地理科学学院，江苏南京 210097

收稿日期:2002-01-04 修回日期:2002-06-11 出版日期:2002-12-20
通讯作者: 沈明洁（1977-），女，江苏太仓人，硕士研究生，主要从事第四纪环境演变及全球变化研究.E-mail:mjshen@sohu.com E-mail:mjshen@sohu.com
基金资助:
国家自然科学基金项目“长江三角洲全新世海侵和洪涝事件序列环境考古研究”（编号：40071083）；高校博士点基金项目“长江三角洲全新世海侵和洪涝事件序列环境考古研究”（编号：2000028414）；南京大学“985”项目“自然地理重点学科建设及南京大学现代分析中心测试基金”资助.

CHARACTERISTICS OF SEA-LEVEL FLUCTUATIONS SINCE HOLOCENE IN THE REGIONS OF EASTERN CHINA

SHEN Ming-jie ¹, XIE Zhi-ren ², ZHU Cheng ¹

1. Department of Urban and Resources Sciences, Nanjing University, Nanjing 210093,China;2.College of Geographical Science,Nanjing Normal University, Nanjing 210097,China

Received:2002-01-04 Revised:2002-06-11 Online:2002-12-20 Published:2002-12-01

对全新世以来中国东部海面变化的资料数据进行全面搜集，其中包括12条原始曲线和 600多个标志物点的多项信息，通过建立数据库、统计分析等多种方法与手段的运用，拟对全新世以来中国东部海面变化小尺度波动进行对比研究，并得出全新世以来中国东部海面波动的一系列特征。初步建立起中国东部全新世以来海面随时间变化的波动序列，即：大致以 6500aBP为界， 6500aBP之前海面在波动中快速上升；6500aBP之后海面波动频繁，变化幅度减弱，但其变化的总趋势呈现出在波动中微微上升的特点。中国东部全新世以来海面变化从总体上来讲共经历了 9个周期的波动变化。

关键词: 全新世, 中国东部, 海面变化, 波动特征

Sea-level changes have now become one of the hot issues in the current research of international global changes. And it has close relationships with human activities, including living, manufacturing and economic growth. Therefore the problem of sea-level changes, especially sea-level fluctuating during the Holocene is being always attached high importance by the academic circles and all governments. Some experts and investigators have done quite a few researches on the sea-level changes in China for a long time, adopting many means of age menstruating and biometrics, employing a lot of new techniques, and establishing the curves patterns of sea-level changes in the territorial regions or countrywide. They generally suggested that there are many fluctuations in sea-level changes since Holocene in the eastern China, but the general trend is unanimous on the whole. But among the fluctuations, the little ones are quite confusing and controversial. People have not come to an agreement on the frequencies, amounts, times and extents of these little fluctuations, and also some discrepancies still exist in many related problems.
To make further study about the sea-level changes trend in the study region aiming to reach a possible agreement, a large amount of data about sea-level changes in the regions of eastern China since Holocene including 12 original sea-level change curves and more than 600 sea-level indicators are collected. Then resettle these original data follow some methods like doing some statistic and digital calculation on a scale of 250 years during the past 10 ka. Rearrangement and systematic statistic analyses are made on the recollected data by Origin software. And comparison study is made on little-scale sea-level fluctuations in the regions of eastern China through building of databank, obtaining a series of fresh characteristics of sea-level fluctuations since Holocene in the regions of eastern China. In so doing, synthetic sea-level curves and temporal sequence with time since Holocene in the regions of eastern China is successfully constructed. 
Study results suggest that sea-level takes on the characteristics of persisting rise and fluctuating that is: 6 500 a BP, serves as demarcation of two fluctuation sequences. Sea-level rises quickly before 6 500 a BP, after 6 500 a BP, however, sea-level fluctuates frequently accompanying with small fluctuation ranges, but the general trend is characterized by slight rise in fluctuation. General speaking, sea-level changes in regions of eastern China since Holocene underwent 9 periods of sea-level fluctuations.

Key words: Holocene, Eastern China, Sea-level changes, Fluctuation characteristics.

中图分类号:

P731.2

［1］ Chen Zhongyuan, Daniel Jean Stanley. Sea-level rise on Eastern China’s Yangtze delta［J］. Journal of Coastal Research, 1998, 14: 360-366.
［2］ Pirazzoli P. World Atlas of Holocene sea-level changes［M］. Amsterdam: Elsevier Oceanographic Series, 1991. 58, 300.
［3］ Daniel Jean Stanley, Chen Zhongyuan. Neolithic settlement distribution as a function of sea-level-controlled topography in the Yangtze delta, China［J］. Geology, 1996, 24: 1 083-1 086.
［4］ Zhao Xitao，Zhang Jingwen. Basic Characteristics of the Holocene Sea-Level Changes along the Coast of China［J］. Chinese Quaternary Sciences，1982，6（2）: 104-109. ［赵希涛，张景文. 中国沿海全新世海面变化的基本特征［J］. 中国第四纪研究，1982，6（2）: 104-109.］
［5］ Shi Yafeng，Zhao Xitao. The Current and Influence of Climatic and Sea-Level Changes in China: Sea-Level Changes in China［M］. Jinan: Shandong Science and Technology Press, 1995. 3-8. ［施雅风，赵希涛. 中国气候与海面变化及其趋势和影响: 中国海面变化［M］. 济南: 山东科学技术出版社，1995. 3-8.］
［6］ Zhao Xitao，Zhang Jingwen. Basic Characteristics of the Holocene Sea-Level Changes in China［A］. In： Liu Tungsheng, et al eds. Quaternary Geology and Environment of China ［C］.Beijing: China Ocean Press, 1982. 155-160.
［7］ Xia Dongxing. Whence comes high sea-level during the Holocene? ［J］. Acta Oceanologica Sinica, 1981, 3(4): 601-609. ［夏东兴. 全新世高海面何在?［J］. 海洋学报，1981, 3(4): 601-609.］
［8］ Yan Qinshang, Hong Xueqing. Transgression problem during the Holocene in the south plain of Yangtze river delta［J］. Acta Oceanologica Sinica, 1987，9（6）: 744-762. ［严钦尚，洪雪晴. 长江三角洲南部平原全新世海侵问题［J］. 海洋学报，1987，9（6）: 744-762.］
［9］ Yang Huairen, Xie Zhiren. Sea-level changes along the east coast of China over the last 20000 years［J］. Oceanologia et Limnologia Sinica, 1984，15（1）：1-13. ［杨怀仁，谢志仁. 中国东部近20000年来的气候波动与海面升降运动［J］. 海洋与湖沼，1984，15（1）：1-13.］
［10］ Yang Dayuan. Preliminary study of a Falling of Sea-Level During the middle Holocene［J］. Journal of Oceanography of Huanghai and Bohai Seas, 1988，6（1）：24-30. ［杨达源. 论全新世的一次海面下落［J］. 黄渤海海洋，1988，6（1）：24-30.］
［11］ Li Hengpeng, Yang Guishan. Response of coast of sea-level rise: A review of study methods［J］. Advance in Earth Sciences, 2000，15（5）：598-602 ［李恒鹏，杨桂山. 海平面上升的海岸形态响应研究方法与进展［J］. 地球科学进展，2000，15（5）：598-602.］
［12］ Xie Zhiren. Sea-Level and Enviromental Changes (Discussing Sea-Level-Ground System and Sea-Gas-Ice System)［M］. Guiyang: Guizhou Science and Technology Press, 1995. 17-49. ［谢志仁. 海平面变化与环境变迁（海面—地面系统和海—气—冰系统初探）［M］. 贵阳：贵州科技出版社，1995. 17-49.］
［13］ Zhao Xitao, Yang Dayuan. Global Sea-Level Changes［M］. Beijing: Science Press, 1992. 71-75. ［赵希涛，杨达源. 全球海面变化［M］. 北京：科学出版社，1992. 71-75.］
［14］ Zhao Xitao, Geng Xiushan, Zhang Jingwen. Sea-level changes of eastan China during the past 20000 Years［J］. Acta Oceanica Sinica, 1979,1(2): 269-281. ［赵希涛，耿秀山，张景文. 中国东部20000年来的海面变化［J］. 海洋学报, 1979,1(2): 269-281.］
［15］ Shi Yafeng，Zhao Xitao. The Current and Influence of Climatic and Sea-Level Changes in China: Sea-Level Changes in China［M］. Jinan: Shandong Science and Technology Press, 1995.34-36. ［施雅风，赵希涛. 中国气候与海面变化及其趋势和影响: 中国海面变化［M］. 济南: 山东科学技术出版社, 1995.34-36.］
［16］ Shi Yafeng，Zhao Xitao. The Current and Influence of Climatic and Sea-Level Changes in China: Sea-Level Changes in China［M］. Jinan: Shandong Science and Technology Press, 1995. 51. ［施雅风，赵希涛. 中国气候与海面变化及其趋势和影响: 中国海面变化［M］. 济南: 山东科学技术出版社，1995. 51.］
［17］ Yang Dayuan, Lu Huayi. Sea-level changes along the coast of Jiangsu middle part over the last 2000 years［J］. Chinese Science Bullletin, 1991，36（20）：574-577. ［杨达源，鹿化煜. 江苏中部沿海近2000年来的海面变化［J］. 科学通报，1991，36（20）：574-577.］
［18］ Shi Yafeng，Zhao Xitao. The Current and Influence of Climatic and Sea-Level Changes in China: Sea-Level Changes in China［M］. Jinan: Shandong Science and Technology Press, 1995.114-115. ［施雅风，赵希涛. 中国气候与海面变化及其趋势和影响: 中国海面变化［M］. 济南: 山东科学技术出版社, 1995.114-115.］
［19］ Shi Yafeng，Zhao Xitao. The Current and Influence of Climatic and Sea-Level Changes in China: Sea-Level Changes in China［M］. Jinan: Shandong Science and Technology Press, 1995. 121-129. ［施雅风，赵希涛. 中国气候与海面变化及其趋势和影响: 中国海面变化［M］. 济南: 山东科学技术出版社, 1995. 121-129.］
［20］ Shi Yafeng，Zhao Xitao. The Current and Influence of Climatic and Sea-Level Changes in China: Sea-Level Changes in China［M］. Jinan: Shandong Science and Technology Press, 1995.144. ［施雅风，赵希涛. 中国气候与海面变化及其趋势和影响: 中国海面变化［M］. 济南: 山东科学技术出版社, 1995.144.］

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