首页> 外文会议>International GeologicalCongress >Palynological Study of the Devonian - Carboniferous Boundary in the Vicinity of the International Auxiliary Stratotype Section, Guilin, China
【24h】

Palynological Study of the Devonian - Carboniferous Boundary in the Vicinity of the International Auxiliary Stratotype Section, Guilin, China

机译:中国桂林桂林国际辅助划线附近的探索 - 石炭系边界的蛋白学研究

获取原文

摘要

Palynological data from Guping Section in the vicinity of the International Auxiliary Stratotype Section of the Devonian -Carboniferous Boundary, Guilin, China, have been obtained for the first time. Two miospore zones have been established: Pmr, Pml. These two assemblages, which contain latest Devonian palynomorphs, can be correlated very well with those in Byelorussia, Poland, and West Europe, as well as Central Hunan in China. Consequently, four miospore evolutionary stages in the above mentioned areas are proposed, i.e. (1) Retispora lepidophyta dominant stage; (2)R. lepidophyta and Vallatisporites pusillites coexisting stage; (3) V. pusillites dominant stage; (4) R. lepidophyta reoccurring stage. The Pmr and Pml zones in Guilin may be attributed to stage (3) and stage (4) respectively. The disadvantage of using the disappearance of R. lepidophyta and V. pusillites as the criterion for recognizing Devonian -Carboniferous boundary has also been discussed.
机译:从德文尼亚 - 羰基划线附近的普京段的宫颈数据是第一次获得桂林桂林的杜松子林边界附近。已经建立了两个Miospore区:PMR,PML。这两个含有最新的德文尼亚·帕诺瓜(Palynomorphs)的组装可以与百万罗斯,波兰和西欧以及中国中央湖南的相关联。因此,提出了在上述区域中的四个MioSpore进化阶段,即(1)retiSpora Lepidophyta显性阶段; (2)r。 Lepidophyta和Vallatisporites血毛石共存舞台; (3)V. Pusillites主导阶段; (4)R.Lepidophyta重新灼热阶段。桂林中的PMR和PML区分别归因于阶段(3)和阶段(4)。还讨论了利用R.Lepidophyta和V. Pusillites消失的缺点作为识别郡 - 碳酸德林边界的标准。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号