古地理学报 ›› 2014, Vol. 16 ›› Issue (2): 217-226. doi: 10.7605/gdlxb.2014.02.020

• 生物古地理学及古生态学 • 上一篇    下一篇

黔北务川—正安—道真地区下二叠统大竹园组和梁山组孢粉学研究

史骁1, 喻建新1, 陈斌2, 黄程1, 顾松竹1, 李慧1, 迟鸿飞1   

  1. 1 生物地质与环境地质国家重点实验室,中国地质大学(武汉),湖北武汉 430074;
    2 中国地质大学(武汉)地球科学学院,湖北武汉 430074
  • 收稿日期:2013-03-18 修回日期:2013-12-05 出版日期:2014-04-01 发布日期:2014-04-01
  • 通讯作者: 喻建新,女,1966年生,博士,中国地质大学(武汉)教授,主要从事孢粉学和古植物学研究。E-mail:yujx_cug@aliyun.com。
  • 作者简介:史骁,男,1988年生,中国地质大学(武汉)博士生,现从事地层古生物学研究。E-mail:570066@163.com。
  • 基金资助:
    贵州省地勘基金项目“黔北务—正—道地区铝土矿基础地质和成矿背景研究”资助

Palynology of the Lower Permian Dazhuyuan and Liangshan Formations in Wuchuan-Zheng′an-Daozhen area,northern Guizhou Province

Shi Xiao1, Yu Jianxin1, Chen Bin2, Huang Cheng1, Gu Songzhu1, Li Hui1, Chi Hongfei1   

  1. 1 State Key Laboratory of Biogeology and Environmental Geology,China University of Geosciences(Wuhan),Wuhan 430074,Hubei;
    2 Faculty of Earth Sciences,China University of Geosciences(Wuhan),Wuhan 430074,Hubei
  • Received:2013-03-18 Revised:2013-12-05 Online:2014-04-01 Published:2014-04-01
  • About author:Shi Xiao,born in 1988,is a Ph.D. candidate of China University of Geosciences(Wuhan)and is mainly engaged in research of paleontology. E-mail:570066@163.com.   About the corresponding author Yu Jianxin,born in 1966,is a professor of China University of Geosciences(Wuhan)and is mainly engaged in researches of palynology and paleobotany. E-mail:yujx_cug@aliyun.com.

摘要: 文中材料采自黔北务川—正安—道真地区下二叠统大竹园组和梁山组。大竹园组孢粉化石类型单调,保存较差;而梁山组孢粉化石丰富,保存良好。孢粉组合特征为:(1)大竹园组包含丰富的CalamosporaFlorinites及少量Torispora verrucosa,Gulisporites,Alisporites,HamiapollenitesStriatopodocarpites,这一孢粉组合主要出现在上石炭统至下二叠统。按照大竹园组层位和孢粉化石特征,其地质时代应为早二叠世Asselian期—Artinskian期(相当于紫松期—隆林期)。(2)梁山组中可建立孢粉组合Laevigatosporites vulgaris-Gulisporites-Florinites ovalis,共计发现孢粉化石34属49种,其中蕨类植物孢子含量为51.6%~56.1%,裸子植物花粉含量为43.9%~48.4%。与大竹园组沉积时期相比,这一时期植被极为繁盛。根据孢粉组合特征,梁山组地质时代可能为早二叠世隆林期,即Kungurian期。

关键词: 孢粉组合, 下二叠统, 大竹园组, 梁山组, 黔北

Abstract: The materials in this paper were collected from the Lower Permian Dazhuyuan and Liangshan Formations in Wuchuan-Zheng′an-Daozhen area,northern Guizhou Province. The sporo-pollen assemblages are diverse,abundant,and well preserved in Liangshan Formation,but conversed to those in Dazhuyuan Formation. The palynological characteristic of the mentioned Formations can be summarized as follows:(1)The miospore populations of the Dazhuyuan Formation contain examples of species such as abundant Calamospora and Florinites,a little Torispora verrucosa,Gulisporites,Alisporites,Hamiapollenites and Striatopodocarpites,mainly occurring in the Upper Carboniferous to Lower Permian. According to the stratigraphic position of the Dazhuyuan Formation and miospore collected,its age should be correspond to the Early Permian Asselian to Artinskian(equivalent to the Zisong-Longlin stage).(2)The Liangshan Formation contains miospores collectively named Laevigatosporites vulgaris-Gulisporites-Florinites ovalis assemblage. Compared with the preceding Dazhuyuan Formation,the vegetation became extremely diversified,as reflected by the numerous taxa of both pteridophytic spores and gymnospermous pollen-attaining to 49 species in 34 genera, and quantitatively to 51.6%~56.1% and 43.9%~48.4% respectively. Judging from the characteristic components of this assemblage,the Liangshan Formation is possibly correlated with Early Permian Longlinian of southern China(equivalent to the Kunguria Stage).

Key words: sporo-pollen, Lower Permian, Dazhuyuan Formation, Liangshan Formation, northern Guizhou Province

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