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:2015-06-11
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:2015-06-11
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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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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