地理学报 ›› 2015, Vol. 70 ›› Issue (5): 751-765.doi: 10.11821/dlxb201505007
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
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:
基金资助:
Jianhui JIN1,2,3(), Zhizhong LI1,2,3(
), Fangen Hu2,4, Hui ZHANG2,5, Xianli WANG2, Jing XIA2, Feng JIANG2, Tao DENG2, Shuyu JIN2, Xiuming LIU1,2,3
Received:
2015-01-09
Revised:
2015-02-06
Online:
2015-05-20
Published:
2015-05-20
Supported by:
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。
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.
表3
东山剖面光释光测年结果"
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 |
表4
DS剖面沉积环境与人类活动记录"
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; |
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