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内蒙古韩家营玄武岩夹层中三趾马动物群化石

王倩 刘艳 王李花 傅明楷 张兆群

古脊椎动物学报2021,Vol.59Issue(2):125-137,13.
古脊椎动物学报2021,Vol.59Issue(2):125-137,13.DOI:10.19615/j.cnki.1000-3118.210323

内蒙古韩家营玄武岩夹层中三趾马动物群化石

An Upper Miocene"Hipparion fauna"locality sandwiched by basalt in Hanjiaying,Nei Mongol

王倩 1刘艳 2王李花 1傅明楷 3张兆群4

作者信息

  • 1. 中国科学院古脊椎动物与古人类研究所,中国科学院脊椎动物演化与人类起源重点实验室 北京100044
  • 2. 中国科学院大学地球与行星科学学院 北京100049
  • 3. 云南大学古生物研究院脊椎动物演化研究院 昆明650091
  • 4. 芬兰赫尔辛基大学地球科学与地理学系 赫尔辛基FIN-00014
  • 折叠

摘要

Abstract

Here we report a Hipparion fauna locality discovered in between two basalt layers near Hanjiaying Village,Jining District,Wulanchabu City,Nei Mongol.K-Ar isotopic dating of the lower and upper level of the basalt constrains the age of the fauna from 7.2 to 6.8 Ma.Compared with classical Hipparion fauna from northern China,the Hanjiaying fauna is closer to those from Baode of Shanxi,Siziwang Banner of Nei Mongol and the Linxia Basin of Gansu.It is similar to the Loc.43,44 and 49 from Baode by faunal composition,confirming their age to be~7.0 Ma rather than 5.5 Ma.The high similarity with the fossils from Wulanhua,Siziwang Banner,Nei Mongol,verified the age of Wulanhua fauna at about 7 Ma.Compared with faunas from the Linxia Basin,Gansu,it is more similar to those from the upper part of the Liushu Formation,especially the Yangjiashan fauna.Based on the faunal composition and their tooth morphology,the Hanjiaying fauna could be included in the"Gazella dorcadoides"fauna,which is supposed to be at the west paleobiome in northern China during the Late Miocene.

关键词

内蒙古/集宁区/晚中新世/三趾马动物群/K-Ar测年

Key words

Nei Mongol/Jining District/Late Miocene/Hipparion fauna/K-Ar dating

分类

生物科学

引用本文复制引用

王倩,刘艳,王李花,傅明楷,张兆群..内蒙古韩家营玄武岩夹层中三趾马动物群化石[J].古脊椎动物学报,2021,59(2):125-137,13.

基金项目

国家自然科学基金(批准号:41402003)、国家基础科学人才培养基金(批准号:J1210008)和中国科学院战略性先导科技专项(B类)(编号:XDB26030301)资助. (批准号:41402003)

古脊椎动物学报

OA北大核心CSCDCSTPCD

1000-3118

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