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河北阳原槽村剖面孢粉组合特征及古气候意义

Characteristics of a sporo-pollen assemblage in the section of Caocun,Yangyuan, Hebei, and its paleoclimatic significance

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【作者】 王燕王书兵蒋复初童国榜赵志中

【Author】 WANG Yan1, WANG Shubing1, JIANG Fuchu1,2, TONG Guobang3, ZHAO Zhizhong1(1 Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China;2 State Key Laboratory of Loess and Quaternary Geology, Chinese Academy of Sciences, Xi′an 710075, Shaanxi, China;3 Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences,Zhengding 050803, Hebei, China)

【机构】 中国地质科学院地质力学研究所中国地质科学院水文地质环境地质研究所中国地质科学院地质力学研究所 北京100081北京100081北京100081中国科学院黄土与第四纪地质国家重点实验室陕西西安710075河北正定050803

【摘要】 阳原槽村剖面的孢粉分析表明,阳原盆地晚更新世晚期以来的气候环境经历了温凉偏干—温暖稍湿—温凉偏干—冷凉偏干等4个演化阶段,植被亦相应地经历了疏林草原—森林草原—疏林草原—森林草原等4个演化过程。但总的说来,阳原盆地的植被自始至终都是以藜、蒿等草本植物占重要地位,气候总体表现为凉偏干。

【Abstract】 A sporo-pollen analysis of the Caocun section, Yangyuan, Hebei, shows that the climate and environment since the latest Pleistocene in the Yangyuan basin have gone through four evolutionary stages, i.e. temperate-cool and dry, warm and slightly wet, temperate-cool and dry, and cold and dry, and accordingly vegetation has also gone through four evolutionary stages from sparse sylvosteppe→sylvosteppe→sparse sylvosteppe→sylvosteppe. However, generally the vegetation in the Yangyuan basin has been dominated by herbs, such as Artemisia and Chenopodiaceae, and the paleoclimate has been generally cool-dry.

【基金】 国家自然科学基金项目(编号:40002014);中国科学院知识创新工程项目(批准号:KZCX2—108);国土资源部基础研究项目(批准号:991005)资助。
  • 【文献出处】 地质通报 ,Regional Geology of China , 编辑部邮箱 ,2003年09期
  • 【分类号】P532;Q915
  • 【被引频次】12
  • 【下载频次】198
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