Geological and Geomorphological Environment in Shuilian Cave Area, Pingshan County,Hebei Province

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  • 1. Hebei Key Laboratory of Environmental Change and Ecological Construction, Hebei Normal University, Shijiazhuang, Hebei 050016;
    2. Shijiazhuang University of Economics, Shijiazhuang, Hebei 050031

Received date: 2009-12-19

  Revised date: 2010-03-19

  Online published: 2010-07-20

Abstract

A paleoanthropological site was discovered in the Shuilian cave which is behind the Jiutianmuyu waterfall of Huhushui ecological spot, Southwest Pingshan County, Hebei Province. A lot of animal bone fossils and stone implements were dug out in ash layers which were the vestiges of the ancients. Study on geological-geomorphological evolution, fossils, stones and pollen analysis indicated roughlly that the ancients were lived in the period of the late Palaeolithic Age about 30 kyr B.P. probably. Pollen analysis reflected further that the climate was mildness in the period of the ancients living. The investigation in and around the cave showed that Shuilian cave was formed in tectonic quiet periods during the Middle and Late Pleistocene, which provided a good place for ancients to exist and live in. It was probably that the ancients lived in this area from the late Pleistocene and migrated to other place while the caves broken during the early Holocene.

Cite this article

HUANG Hua-fang, LI Zhi-guang, WANG Jian, XU Qinghai . Geological and Geomorphological Environment in Shuilian Cave Area, Pingshan County,Hebei Province[J]. SCIENTIA GEOGRAPHICA SINICA, 2010 , 30(4) : 630 -635 . DOI: 10.13249/j.cnki.sgs.2010.04.630

References

[1] 许刘兵,周尚哲.河流阶地形成过程及其驱动机制再研究[J].地理科学,2007,27(5):672~677
[2] 高红山,潘保田,邬光剑,等.祁连山东段河流阶地的形成时代与机制探讨[J].地理科学,2005,25(2):197~202.
[3] 吴忱.华北地貌环境及其形成演化[M].北京:科学出版社,2008:123~183.
[4] 吴忱,马永红,张秀清,等.华北山地地形面、地文期与地貌发育史[M].石家庄:河北科学技术出版社,1999:190~196.
[5] 程绍平,冉勇康.滹沱河太行山山峡段河流阶地和第四纪构造运动[J].地震地质,1981,3(1):29~39.
[6] 马寅生,赵逊,赵希涛,等.太行山南缘新生代的隆升与断陷过程[J].地球学报,2007,28(3):219~233.
[7] 邬光剑,潘保田,管清玉,等.中更新世气候转型与100 ka周期研究[J].地球科学进展.2002,17(4):605~611.
[8] 王建力,王丽,何潇,等.重庆地区末次冰期气候变化的石笋记录研究[J].地理科学,2006,26(5):580~585.
[9] 周廷儒.中国第四纪古地理环境的分异[J].地理科学,1983,3(3):191~206.
[10] 郑朝贵,朱诚,高华中,等.南京江北地区晚更新世末期以来泥炭层δ13C记录的古气候变化[J].地理科学,2006,26(3):328~334.
[11] 申洪源,朱诚,贾玉连.太湖流域地貌与环境变迁对新石器文化传承的影响[J].地理科学,2004,24(5):580~585.
[12] 武仙竹,裴树文,吴秀杰,等.郧西人遗址洞穴发育与埋藏环境初步观察[J].第四纪研究,2007,27(3):444~452.
[13] 陈铁梅,HedgesR E M,袁振新.山顶洞遗址的第二批加速器质谱14C年龄数据与讨论[J].人类学学报,1992,11(2):112~115.
[14] 安志敏.河南安阳小南海旧石器时代洞穴堆积的试掘[J].考古学报,1965,(1):1~28.
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