地理学报 ›› 2020, Vol. 75 ›› Issue (3): 529-543.doi: 10.11821/dlxb202003007
收稿日期:
2019-07-12
修回日期:
2020-01-03
出版日期:
2020-03-25
发布日期:
2020-05-25
作者简介:
赵成双苹(1991-), 女, 河北新乐人, 博士, 研究方向为环境演变与环境考古。E-mail: zhaochengsp@pku.edu.cn
基金资助:
ZHAO Chengshuangping1, MO Duowen1,2()
Received:
2019-07-12
Revised:
2020-01-03
Published:
2020-03-25
Online:
2020-05-25
Supported by:
摘要:
本文基于长江中游江汉—洞庭盆地18个钻孔岩性、沉积特征及年代数据,结合研究区考古遗址点时空分布特征,恢复研究区全新世以来水文环境演变过程,并探讨了区域水文环境演变的成因机制及其与人类活动的关系。结果表明,受东海海面上升和泥沙淤积等因素影响,距今11.5—5.5 ka,长江中游地区河湖水位呈上升趋势,随着新石器文化的发展及稻作农业活动的增加,人类文化聚落自山前平原地带逐渐向盆地平原中部扩展;距今5.5—4.0 ka,长江中游河湖水位有所下降,新石器晚期的屈家岭—石家河文化迅速发展,聚落数量增多,平原腹地聚落比例增加;距今4.0 ka前后,河湖水位再次有所上升,洪泛过程加剧,可能是石家河文化快速衰落的主要原因。
赵成双苹, 莫多闻. 长江中游江汉—洞庭盆地全新世以来水文环境演变与人类活动[J]. 地理学报, 2020, 75(3): 529-543.
ZHAO Chengshuangping, MO Duowen. Holocene hydro-environmental evolution and its impacts on human activities in Jianghan-Dongting Basin, middle reaches of the Yangtze River, China[J]. Acta Geographica Sinica, 2020, 75(3): 529-543.
表1
钻孔数据列表
序号 | 钻孔名称 | 地点 | 数据来源 | 文献编号 |
---|---|---|---|---|
1 | 松滋八宝188孔 | 湖北省松滋市八宝镇 | 金伯欣, 1992 | [31] |
2 | MHK02孔 | 湖北省公安县麻豪口镇 | 陈思思等, 2014 | [32] |
3 | JZ-2010剖面 | 湖北省江陵县江北农场二砖厂 | Li F等, 2014 | [33] |
4 | 潜江张金海345孔 | 湖北省潜江市张金镇 | 金伯欣, 1992 | [31] |
5 | 江陵47号孔 | 湖北省江陵县六合垸农场场部 | 施之新, 1997 | [34] |
6 | QS01孔 | 湖北省江陵县秦市乡 | 陈思思等, 2014 | [32] |
7 | 新沟孔 | 湖北省监利县新沟市 | 王秋良等, 2009 | [35] |
8 | 周老孔 | 湖北省监利县内周老镇 | 张玉芬等, 2005 | [36] |
9 | WS03孔 | 湖北省监利县网市镇易家湾 | 陈思思等, 2014 | [32] |
10 | 沔城M1孔 | 湖北省仙桃市沔城镇 | 朱育新等, 1997 | [37] |
11 | DTH01孔 | 湖北省洪湖市大同湖农场四分厂 | 陈思思等, 2014 | [32] |
12 | 仙桃纯良岭454孔 | 湖北省仙桃市纯良岭 | 金伯欣, 1992 | [31] |
13 | ZK76孔 | 湖北省武汉市蔡甸区三河连 | 陈思思等, 2014 | [32] |
14 | ZK84孔 | 湖北省武汉市江夏区门塘湾 | 陈思思等, 2014 | [32] |
15 | 石首宛子口274孔 | 湖北省石首市宛子口 | 金伯欣, 1992 | [31] |
16 | CK37孔 | 湖南省西洞庭湖地区 | 张晓阳等, 1994 | [38] |
17 | CK21孔 | 湖南省华容县注滋口镇 | 张晓阳等, 1994 | [38] |
18 | 东洞庭湖ZK01孔 | 湖南省华容县注滋口镇 | 李俊, 2009 | [39] |
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