全新世中晚期福建海岸沙丘记录的海岸环境与人类活动

doi:10.11821/dlxb201505007

地理学报 ›› 2015, Vol. 70 ›› Issue (5): 751-765.doi: 10.11821/dlxb201505007

全新世中晚期福建海岸沙丘记录的海岸环境与人类活动

靳建辉^1,^2,³(), 李志忠^1,^2,³(), 胡凡根^2,⁴, 张辉^2,⁵, 王贤立², 夏菁², 姜锋², 邓涛², 靳姝豫², 刘秀铭^1,^2,³

1. 福建师范大学地理研究所,福州 350007
2. 福建师范大学地理科学学院,福州 350007
3. 湿润亚热带生态-地理过程教育部重点实验室,福州 350007
4. 中国科学院地质与地球物理研究所,北京 100029
5. 贵州师范学院地理与旅游学院,贵阳 550018

收稿日期:2015-01-09 修回日期:2015-02-06 出版日期:2015-05-20 发布日期:2015-05-20
作者简介:
作者简介：靳建辉(1981-), 男, 山西陵川人, 博士研究生, 讲师, 主要从事海岸风沙地貌与第四纪环境演变研究。E-mail: geojjh@fjnu.edu.cn
基金资助:
国家自然科学基金(41271031, 41301012);国家自然科学基金委员会-福建省人民政府促进海峡两岸科技合作联合基金(U1405231);福建省自然科学基金(2013J01153);福建省科技厅公益类科研院所专项基金(2013R09)

Mid-Holocene coastal environment and human activities recorded by a coastal dune in Fujian Province, China

Jianhui JIN^1,^2,³(), Zhizhong LI^1,^2,³(), Fangen Hu^2,⁴, Hui ZHANG^2,⁵, Xianli WANG², Jing XIA², Feng JIANG², Tao DENG², Shuyu JIN², Xiuming LIU^1,^2,³

1. Institute of Geography, Fujian Normal University, Fuzhou 350007, China
2. School of Geography Science, Fujian Normal University, Fuzhou 350007, China
3. Key Laboratory of Humid Subtropical Ecosystem and Geography, Ministry of Education, Fuzhou 350007, China
4. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
5. School of geography and tourism, Guizhou Normal College, Guiyang 550018, China

Received:2015-01-09 Revised:2015-02-06 Online:2015-05-20 Published:2015-05-20
Supported by:
National Natural Science Foundation of China, No.41271031, No.41301012;NSFC-Fujian Province United Foundation, No;U1405231;Natural Science Foundation of Fujian Province, No.2013J01153;Key Scientific and Technological Project of Fujian Province, No.2013R09

摘要/Abstract

摘要：

选取福建长乐典型海岸沙丘进行研究,在光释光（OSL）年代学基础上,结合环境代用指标分析和地质雷达图像,探讨研究区晚全新世以来沙丘发育历史及其古环境意义。结果显示：① 东山（DS）沙丘发育过程主要存在5个沉积期和3个沉积间断。主要反映了东亚季风强度变化,是东亚冬季风的区域响应结果。同时与火山活动、中国东部冬半年气温、夏季风降水具有良好对应关系;② DS剖面保存了近6 ka以来福州盆地海平面变化信息。清晰记录了存在于闽粤台地区的大范围的高海面期,分别是5.6~2.8 ka BP、2.8~1.7 ka BP、1.7~0.8 ka BP,其中1.7~0.8 ka BP阶段最为明显。③ DS沙丘发育过程与闽东北区域人类活动记录以及新石器文化序列具有良好对应关系。5.6~2.8 ka BP、2.8~1.7 ka BP阶段的人类活动主要受到自然环境影响。~1.7 ka BP之后,唐代至五代是福建社会经济的复苏阶段。

关键词: 海岸沙丘, OSL, 海平面变化, 东亚季风, 人类活动

Abstract:

A coastal dune, Dongshan (DS) dune in Changle of China's Fujian Province is selected as a research object based on the systematic field investigation. Combined with the environmental index analysis and geological radar images, the dune development history and paleoenvironment significance in the study area since the late Holocene are explored through optically stimulated luminescence (OSL) chronology. Results are shown as follows. (1) Five sedimentary periods and three sedimentary discontinuity in the DS dune can be defined, which reflects that the change of the East Asian monsoon, and the developmental process of DS dune are the result of regional response to the East Asian winter monsoon, and they are well correlated with volcanic activity, winter temperatures of East China and precipitation of summer monsoon at the same time. (2) Meanwhile, DS profile has preserved the sea-level change information of the Fuzhou Basin since nearly 6 ka BP. The widespread thalassocratic periods were recorded clearly in South China at 5.6-2.8 ka BP, 2.8-1.7 ka BP and 1.7-0.8 ka BP, respectively. (3) Artificiality and the mark of human activity are observed in the DS dune, and porcelain shards and conchs have been found in the cultural layer. The development processes of the DS dune accord well with the records of human activities and neolithic cultural sequences in northeast Fujian. The human activities are mainly affected by the natural environment at 5.6-2.8 ka BP and 2.8-1.7 ka BP, respectively. Tang and the Five Dynasties were the recovery stages of social economy in Fujian after 1.7 ka BP.

Key words: coastal dune, OSL, sea level, East Asia monsoon, human activities

靳建辉, 李志忠, 胡凡根, 张辉, 王贤立, 夏菁, 姜锋, 邓涛, 靳姝豫, 刘秀铭. 全新世中晚期福建海岸沙丘记录的海岸环境与人类活动[J]. 地理学报, 2015, 70(5): 751-765.

Jianhui JIN, Zhizhong LI, Fangen Hu, Hui ZHANG, Xianli WANG, Jing XIA, Feng JIANG, Tao DENG, Shuyu JIN, Xiuming LIU. Mid-Holocene coastal environment and human activities recorded by a coastal dune in Fujian Province, China[J]. Acta Geographica Sinica, 2015, 70(5): 751-765.

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参考文献 50

[1]	Costas I, Reimann T, Tsukamoto S, et al.Comparison of OSL ages from young dune sediments with a high-resolution independent age model. Quaternary Geochronology, 2012: 16-23.
[2]	Zhang Jiangfu, Mo Duowen, Xia Zhengkai, et al.Optical dating of sediments from China and its implication for depositonal processes. Quaternary Sciences, 2009, 29(1): 23-33.
	[张家富, 莫多闻, 夏正楷, 等. 沉积物的光释光测年和对沉积过程的指示意义. 第四纪研究, 2009, 29(1): 23-33.]
[3]	Tamura T, Mark D B, Yoshinori K, et al.Building of shore-oblique transverse dune ridges revealed by ground-penetrating radar and optical dating over the last 500 years on Tottori coast, Japan Sea. Geomorphology, 2011, 132(3/4): 153-166.
[4]	Chen Y W, Chen Y G, Murray A S, et al.Luminescence dating of neotectonic activity on the southwestern coastal plain, Taiwan. Quaternary Science Reviews, 2003, 22: 1223-1229.
[5]	Wu Z, Wang W, Tan H H et al. The age of the 'old red sand' on the coasts of south Fujian and west Guangdong, China. Chinese Science Bulletin, 2000, 45: 1216-1221.
[6]	Zhang J F, Yuan B Y, Zhou L P.Luminescence chronology of "Old Red Sand" in Jinjiang and its implications for optical dating of sediments in South China. Chinese Science Bulletin, 2008, 53: 591-601.
[7]	Hu Fangen, Li Zhizhong, Jin Jianhui, et al.A primary research on multiphase development pattern of ‘old red sand’ in Jinjiang coast of southeast Fujian. Quaternary Sciences, 2012, 32(6): 1207-1220.
	[胡凡根, 李志忠, 靳建辉, 等. 福建晋江海岸带老红砂多期发育模式初步研究. 第四纪研究, 2012, 32(6): 1207-1220.]
[8]	Li Congxian, Chen Gang, Yang Hongjun.Eolian deposits in coastal zones of Fujian Province. Journal of Desert Research, 1989, 9(4): 8-18.
	[李从先, 陈刚, 杨红君. 福建海岸的风成沉积. 中国沙漠, 1989, 9(4): 8-18.]
[9]	Zhang Mingshu, Li Shaoquan, Liu Jian.Sedimentary zones, sequential features and climatic-environmental significance of Late Pleistocene eolian deposits along coastal areas of China. Quaternary Sciences, 1996, 16(1): 31-41.
	[张明书, 李绍全, 刘健. 中国海岸带晚更新世风成沉积分区、序列特征及其气候环境意义. 第四纪研究, 1996, 16(1): 31-41.]
[10]	Chen Fang, Zhu Dakui.Dune formation and evolution along the south coastal of Minjiang Estuary. Journal of Desert Research, 1996, 16(3): 228-234.
	[陈方, 朱大奎. 闽江口海岸沙丘的形成与演化. 中国沙漠, 1996, 16(3): 228-234.]
[11]	Zhou Dingcheng.Ages of coastal wind sand disasters in central south of Fujian. Journal of Oceanography in Taiwan Strait, 2010, 29(1): 94-98.
	[周定成. 闽中南海岸风沙灾害的形成于年代. 台湾海峡, 2010, 29(1): 94-98.]
[12]	Liu Jianhui.Origin and characteristics of coastal dunes in eastern Changle of Fujian Province. Geology of Fujian, 2006, 25(4): 185-191.
	[刘建辉. 福建长乐东部海岸沙丘发育成因及特征. 福建地质, 2006, 25(4): 185-191.]
[13]	Dong Yuxiang, Ma Jun, Huang Dequan.Distribution model of grain size on coastal transverse foredune at Changle in Fujian Province. Acta Sedimentologica Sinica, 2008, 26(5): 813-819.
	[董玉祥, 马骏, 黄德全. 福建长乐海岸横向前丘表面粒度分异研究. 沉积学报, 2008, 26(5): 813-819.]
[14]	Murray A S, Wintle A G.Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol. Radiation Measurements, 2000, 32(1): 57-73.
[15]	Murray-Wallace C V, Banerjee D, Bourman R P, et al. Optically stimulated luminescence dating of Holocene relict foredunes, Guichen Bay, South Australia. Quaternary Science Reviews, 2002, 21(8): 1077-1086.
[16]	Zhang Jiafu, Yuan Baoyin, Zhou Liping.Luminescence chronology of “Old Red Sand” in Jinjiang and its implications for optical dating of sediments in South China. Chinese Science Bulletin, 2008, 53(4): 591-601.
	[张家富, 袁宝印, 周力平. 福建晋江“老红砂” 的释光年代学及对南方第四纪沉积物释光测年的指示意义. 科学通报, 2008, 52(22): 2646-2654.]
[17]	Hu Fangen, Li Zhizhong, Jin Jianhui, et al.A primary research on multiphase development pattern of “old red sand” in Jinjiang coast of south east Fujian. Quaternary Sciences, 2012, 32(6): 1207-1220.
	[胡凡根, 李志忠, 靳建辉, 等. 福建晋江海岸带老红砂多期发育模式初步研究. 第四纪研究, 2012, 32(6): 1207-1220.]
[18]	Aitken M J.An introduction to optical dating: The dating of Quaternary sediments by the use of photon-stimulated luminescence. New York: Oxford University Press, 1998.
[19]	Osmond J K, Ivanovich M.Uranium-series mobilization and surface hydrology//Uranium-series Disequilibrium: Applications to Earth, Marine, and Environmental Sciences. 2.ed. Oxford: Clarendon Press, 1992: 260-289.
[20]	Zhang Jiafu, Miao Jianmin.Optical dating of tamped earth from the Yanshi walled city. Nuclear Techniques, 2003, 26(1): 40-44.
	[张家富, 苗建民. 偃师商城宫城建筑基址夯土的光释光测年初步研究. 核技术, 2003, 26(1): 40-44.]
[21]	Chabaux F, Dequincey O, Lévèque J J.Tracing and dating recent chemical transfers in weathering profiles by trace-element geochemistry and 238U-234U-230Th disequilibria. Comptes Rendus Geoscience, 2003, 335(16): 1219-1231.
[22]	Tang Wenwu, Zhu Dakui, Ge Chendong, et al.The application of ground penetrating radar to the survey of the coast environment. Marine Geology and Quaternary Geology, 2001, 21(2): 99-105.
	[唐文武, 朱大奎, 葛晨东, 等. 探地雷达 (GPR) 在海岸环境勘测中的应用. 海洋地质与第四纪地质, 2001, 21(2): 99-105.]
[23]	Reineck H E, Singh I B.Depositional Sedimentary Environments with Reference to Terrigenous Clastics. New York, Heidelberg, Berlin: Spring-Verlag, 1973: 201-203.
[24]	Wu Zheng, Huang Shan, Hu Shouzhen.Research on the Landforms of the Wind-drift Sand in South China Coast. Beijing: Science Press, 1995: 114-118.
	[吴正, 黄山, 胡守真. 华南海岸风沙地貌研究. 北京: 科学出版社, 1995: 114-118.]
[25]	Morrill C, Overpeck J T, Cole J E.A synthesis of abrupt changes in the Asian summer monsoon since the last deglaciation. The Holocene, 2003, 13(4): 465-476.
[26]	Wang Shaohong, Yang Jianming, Sun Henglun, et al.Sea-level changes at the downstream of Minjiang and adjacent areas post glacial period. Acta Oceanologica Sinica, 1990, 12(1): 64-74.
	[王绍鸿, 杨建明, 孙亨伦, 等. 闽江下游及邻近地区冰后期海平面变化. 海洋学报, 1990, 12(1): 64-74.]
[27]	Rolett BV, Zheng Z, Yue Y.Holocene sea-level change and the emergence of Neolithic seafaring in the Fuzhou Basin (Fujian, China). Quaternary Science Reviews, 2011, 30(7/8): 788-797.
[28]	Lee Chengyi, Liew Pingmei, Lee Teh-quei.Pollen records from southern Taiwan: Implications for East Asian summer monsoon variation during the Holocene. The Holocene, 2010, 20(1): 81-89.
[29]	Cheng Qiansheng.The Holocene stratigraphic classification and correlation in Changle Fujian province. Geology of Fujian, 1989, 8(2): 100-110.
	[程乾盛. 福建长乐全新世地层划分与对比探讨. 福建地质, 1989, 8(2): 100-110.]
[30]	Yin Xi, Zhu Cheng, Ma Chunmei, et al.Holocene climate change recorded in peat humification in Tianmu mountain region .Marine Geology and Quaternary Geology, 2006, 26(6): 117-122.
	[尹茜, 朱诚, 马春梅, 等. 天目山千亩田泥炭腐殖化度记录的中全新世气候变化. 海洋地质与第四纪地质, 2006, 26(6): 117-122.]
[31]	Wang Yuzhuo.The Quaternary stratigraphy of Fujian province. Geology of Fujian, 1990, 9(4): 289-306.
	[王雨灼. 福建省第四纪地层划分. 福建地质, 1990, 9(4): 289-306.]
[32]	Cai Aizhi, Gong Jinmei, Cai Yuee.Transgression and eolian sand sequence in Luyangpu plain, Haitan island, Fujian. Journal of Oceanography in Taiwan Strait, 1992, 11(2): 112-117.
	[蔡爱智, 龚金美, 蔡月娥. 海坛岛芦洋浦平原的海进沙与风沙层序. 台湾海峡, 1992, 11(2): 112-117.]
[33]	Chen Chenghui.Studies of Holocene geochronology in the coastal regions of southern Fujian. Journal of Oceanography in Taiwan Strait, 1982, 1(2): 64-73.
	[陈承惠. 闽南沿海全新世地质年代学研究. 台湾海峡, 1982, 1(2): 64-73.]
[34]	Hu Fangen, Li Zhizhong, Jin Jianhui, et al.Coastal environment evolution record from Anshan coastal aeolian sand of Jinjiang, Fujian Province, based on the OSL dating. Acta Geographica Sinica, 2013, 68(3): 343-356.
	[胡凡根, 李志忠, 靳建辉, 等. 基于释光测年的福建晋江海岸沙丘粒度记录的风沙活动. 地理学报, 2013, 68(3): 343-356.]
[35]	Huang Zhenguo.Comparison of the paleodune formed during the Late Pleistocene between China and Japan. Tropical Geography, 1993, 13(1): 1-12.
	[黄镇国. 中国、日本晚更新世海岸古沙丘之比较. 热带地理, 1993, 13(1): 1-12.]
[36]	Wu Zheng, Wang Wei.Factor and ancient geography of old red sand in southern coastal. Science in China (Series D), 1997, 27(6): 537-542.
	[吴正, 王为. 华南沿海老红砂的成因与古地理环境. 中国科学(D辑), 1997, 27(6): 537-542.]
[37]	Yuan Baoyin, Xia Zhengkai, Li Baosheng, et al.Chronostratigraphy and stratigraphic division of red soil in Southern China. Quarternary Sciences, 2008, 28(1): 1-13.
	[袁宝印, 夏正楷, 李保生, 等. 中国南方红土年代地层学与地层划分问题. 第四纪研究, 2008, 28(1): 1-13.]
[38]	Zeng Congsheng.A summary of "old red sand" research in coastal southeast China. Journal of Oceanography in Taiwan Strait, 1997, 16(3): 363-370.
	[曾从盛. 中国东南沿海老红砂研究综述. 台湾海峡, 1997, 16(3): 363-370.]
[39]	Wu Zheng, Feng Wenke, Liao Bingliang, et al.Palaeogeographic study in the continental shelf of the northern South China sea during the last stage of the Late Pleistocene. Acta Geographica Sinica, 1993, 48(6): 491-496.
	[吴正, 冯文科, 廖秉良, 等. 晚更新世末期南海北部陆架的古地理探讨. 地理学报, 1993, 48(6): 491-496.]
[40]	Yang Jianming, Zheng Xiaoyun.Sea-level fluctuations during the past 6000 years along the coast of Fujian. Marine Geology and Quaternary Geology, 1990, 10(4): 67-75.
	[杨建明, 郑晓云. 福建沿岸6000年以来的海平面波动. 海洋地质与第四纪地质, 1990, 10(4): 67-75.]
[41]	Zhang Weiqiang, Huang Zhenguo.Holocene sea level changes along the coasts of Taiwan. Tropical Geography, 1996, 16(3): 226-235.
	[张伟强, 黄镇国. 台湾沿岸全新世海平面波动. 热带地理, 1996, 16(3): 226-235.]
[42]	Tankard A J, Schweitzer F R.The geology of Die Kelders Cave and environs: A palaeoenvironmental study. South African Journal of Science, 1974, 70: 365-369.
[43]	Yancheva G.Influence of the intertropical convergence zone on the East-Asian monsoon. Nature, 2007, 445:74-77.
[44]	Dong Jinguo, Kong Xinggong, Wang Yongjin.The East Asian monsoon climate changes at Mt. Shengnongjia and its relation to shift of intertropical convergence zone during the Holocene. Quaternary Sciences, 2006, 26(5): 827-834.
	[董进国, 孔兴功, 汪永进. 神农架全新世东亚季风演化及其热带辐合带控制. 第四纪研究, 2006, 26(5): 827-834.]
[45]	Bauer B O, Davidson-Arnott R G D, Hesp P A, et al. Aeolian sediment transport on a beach: Surface moisture, wind fetch, and mean transport. Geomorphology, 2009, 105: 106-116.
[46]	Wu Zheng.Eolian Geomorphology and Sand Calamity Engineering Science. Beijing, Science Press, 2003: 36-99.
	[吴正. 风沙地貌与治沙工程学. 北京: 科学出版社, 2003: 36-99.]
[47]	Sherman D J, Hotta S.Aeolian sediment transport: Theory and measurement//Nordstrom K F, Psuty K F, Carter R W G. Coastal Dunes: Form and Process. Chichester: John Wiley and Sons, 1990: 17-37.
[48]	Zheng Zhuo, Deng Yun, Zhang Hua, et al.Holocene environmental changes in the tropical and subtropical areas of the South China and the relation to human activities. Quaternary Sciences, 2004, 24(4): 387-393.
	[郑卓, 邓韫, 张华, 等. 华南沿海热带-亚热带地区全新世环境变化与人类活动的关系. 第四纪研究, 2004, 24(4): 387-393.]
[49]	Fujian Museum.Archaeological Excavation Reports on the China Site of Fuzhou. Fujian Wenbo, 1996, (1): 29.
	[福建省博物馆. 福州怀安窑址发掘报告. 福建文博, 1996, (1): 29.]
[50]	Ge Quansheng.Climate Change of Different Dynasties in China. Beijing: Science Press, 2011: 314-322.
	[葛全胜. 中国历朝气候变化. 北京: 科学出版社, 2011: 314-322.]

样品	出土地点	碳十四年代 (BP)	树轮校正后年代
样品	出土地点	碳十四年代 (BP)	1σ (68.2%)	2σ (95.4%)
贝壳	长乐东山海岸沙丘	1395±35	620AD (68.2%) 655AD	585AD (95.4%) 680AD

出土样品名称	器型描述	考古学年代
碗 (残片)	饼足、施青釉,未及底、底足露胎、内有支钉痕;	唐末宋初
罐 (残片)	施青釉、四系罐,未及底,底足露胎;	唐末宋初
瓮 (残片)	部分施青釉瓷器残片,部分陶器残片,器型无法辨认	?

野外编号	埋深(m)	U(µg/g)	Th(µg/g)	K(%)	等效剂量E.D(Gy)	年剂量Dy(Gy/ka)	含水量(%)	年龄(Ka)
FS01	8.5	1.38	8.14	1.4	15.18±0.97	2.70±0.11	8	5.6±0.4
FS02	8.0	0.87	4.39	1.52	6.32±0.20	2.30±0.09	8	2.8±0.1
FS04	7.0	1.53	7.94	1.73	5.23±0.19	3.07±0.12	8	1.7±0.1
FS05	6.5	1.25	8.82	1.90	0.78±0.05	3.24±0.13	8	0.2±0.02
FS06	6.0	0.72	3.68	2.16	1.09±0.01	2.83±0.11	8	0.4±0.02
FS07	5.5	0.94	4.63	2.08	1.38±0.13	2.92±0.12	8	0.5±0.05
FS08	5.0	0.74	3.38	2.22	1.58±0.10	2.92±0.12	8	0.5±0.04
FS12	3.0	0.92	4.26	2.15	1.80±0.07	2.98±0.12	8	0.6±0.03
FS15	1.5	0.79	3.19	2.04	2.14±0.34	2.76±0.11	8	0.8±0.06

绝对年龄	公元纪年	剖面发育期	海平面变化	闽东北沿海人类活动
0.2 ka BP-至今	1810 AD~	Ⅴ (风沙活动期)	海进期、接近现代海面	《福建沿海图说》：数十年前,东海滨田舍相望,今则一片平沙。
0.8 ka~0.2 ka BP	1210 AD~1810 AD	Ⅳ (风沙稳定期)	海退期、低海面期	港湾淤浅,海滩成陆,围垦开始,流沙遂起;
1.7 ka~0.8 ka BP	310 AD~1210 AD	沉积间断	海进期、高海面期	施青釉饼足碗,施青釉四系罐,贝类壳体宋初设“牧监”,风沙下覆泥炭土
~1.7 ka BP	~310 AD	Ⅲ (潮滩沉积期)	海退期	——
2.8~1.7 ka BP	——	沉积间断	高海面期	——
~2.8 ka BP	——	Ⅱ (潮滩沉积期)	海退期	黄土仑晚期文化;
5.6~2.8 ka BP	——	沉积间断	高海面期	昙石山文化 (昙石山遗址,庄边山下层遗址);黄瓜山文化 (庄边山上层遗址,黄瓜山遗址);黄土仑文化 (古洋遗址,黄土仑遗址);
~5.6 ka BP	——	Ⅰ (潮滩沉积期)	海退期	壳丘头文化 (平潭壳丘头下层遗址);台湾大坌坑文化;福建闽侯白沙溪头遗址;

全新世中晚期福建海岸沙丘记录的海岸环境与人类活动

Mid-Holocene coastal environment and human activities recorded by a coastal dune in Fujian Province, China

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