华北克拉通南缘汝阳群大型具刺疑源类时代再厘定及早期真核生物群演化意义<sup>&#x0002A;</sup>

doi:10.7605/gdlxb.2018.04.043

古地理学报 ›› 2018, Vol. 20 ›› Issue (4): 595-608. doi: 10.7605/gdlxb.2018.04.043

• 中新元古代沉积地层研究 • 上一篇下一篇

华北克拉通南缘汝阳群大型具刺疑源类时代再厘定及早期真核生物群演化意义^*

彭楠¹, 旷红伟¹, 柳永清¹, 耿元生¹, 夏晓旭^1,2, 王玉冲^1,2, 陈骁帅¹, 郑行海²

1 中国地质科学院地质研究所,自然资源部地层与古生物重点实验室,北京 100037;
2 中国地质大学(北京),北京 100083

收稿日期:2018-04-22 修回日期:2018-05-20 出版日期:2018-08-01 发布日期:2018-07-31
通讯作者: 旷红伟,女,1969年生,教授,主要从事沉积地质学研究。E-mail: kuanghw@126.com。
作者简介:彭楠,男,1983年生,助理研究员,主要从事沉积地质学与古地理学研究。E-mail: pengnan19830120@126.com。
基金资助:
*国家重点研发计划深地资源勘查开采重点专项(编号:2016YFC0601001)、国家自然科学基金(编号:41472082)、中国地质调查局项目(编号:1212011120142,DD20160120-01)和神农架世界地质公园项目共同资助

Recognition of geological age for acanthomorphic acritarchs from the Ruyang Group,southern margin of North China Craton and its implication for evolution of early eukaryotes

Peng Nan¹, Kuang Hong-Wei¹, Liu Yong-Qing¹, Geng Yuan-Sheng¹, Xia Xiao-Xu^1,2, Wang Yu-Chong^1,2, Chen Xiao-Shuai¹, Zheng Hang-Hai²

1 Key Laboratory of Stratigraphy and Paleontology,Ministry of Natural Resources,Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037;
2 China University of Geosciences(Beijing),Beijing 100083

Received:2018-04-22 Revised:2018-05-20 Online:2018-08-01 Published:2018-07-31
Contact: Kuang Hong-Wei,born in 1969,is a professor and doctoral supervisor in the Institute of Geology,CAGS. She is mainly engaged in sedimentology. E-mail: kuanghw@126.com.
About author:Peng Nan,born in 1983,is a research assistant in the Institute of Geology,CAGS. He is mainly engaged in sedimentary geology and palaeogeography. E-mail: pengnan19830120@126.com.
Supported by:
Co-funded by the National Key Research and Development Program of China(No.2016YFC0601001),the National Natural Science Foundation of China(No.41472082),China Geological Survey Projects(Nos.1212011120142,DD20160120-01) and the Project of Shennongjia Global Geopark

摘要/Abstract

摘要： 华北克拉通南缘汝阳群中以大型具刺疑源类为代表的真核生物群的时代归属问题一直存在争议。新近在豫西汝州阳坡村洛峪群洛峪口组中获得的凝灰岩锆石SHRIMP U-Pb年龄为1639±13Ma,结合熊耳群和汝阳群已获得的其他年龄数据,将这类形态复杂的真核生物群出现的时间限定在1.75—1.64Ga,即中元古代的早期。这说明,过去一直被认为的代表进化程度较高但仅属于新元古代的一些真核生物群,其实在中元古代早期就已经出现了;由此可以进一步推测,在更古老的地层中应有更原始的微体化石出现,从而华北克拉通南缘中元古界(>1.60Ga)将成为探寻最古老真核生物祖先的重要窗口。同时,将这些在中元古代早期就已经出现并在以后较长地史时期都存在的真核生物群用于标定地层形成时代或作为相关地层的对比标志,值得重新考虑和商榷。

关键词: 大型具刺疑源类, 早期真核生物, 中元古代, 汝阳群, 华北克拉通

Abstract: The geological age of eukaryotes represented by large acanthomorphic acritarchs from the Ruyang Group,southern margin of North China Craton,has been controversial. New zircon SHRIMP U-Pb age of tuff(ca. 1639±13Ma)was obtained from the Luoyukou Formation of the Luoyu Group,Yangpo,Ruzhou,west Henan Province. This new age,combined with the ages from the Xiong'er and Ruyang Group,can well constraint the time of these eukaryotes with complex morphology from the Ruyang Group at 1.75-1.64Ga,which belongs to early Mesoproterozoic. Moreover,it shows that some eukaryotes with relatively higher degree of evolution,which were previously thought to be preserved in the Neoproterozoic,may have appeared in the Early Mesoproterozoic. We further suspect that there might be more primitive microfossils preserved in the older strata(>1.6Ga)in the southern margin of the North China Craton,which provides an important window to explore the ancestor of the eukaryote. Thus,caution should be taken when applying these Mesoproterozoic eukaryotes for stratigraphic correlation.

Key words: large acanthomorphic, early eukaryotes, Mesoproterozoic, Ruyang Group, North China Craton

中图分类号:

P512

彭楠, 旷红伟, 柳永清, 耿元生, 夏晓旭, 王玉冲, 陈骁帅, 郑行海. 华北克拉通南缘汝阳群大型具刺疑源类时代再厘定及早期真核生物群演化意义^*[J]. 古地理学报, 2018, 20(4): 595-608.

Peng Nan, Kuang Hong-Wei, Liu Yong-Qing, Geng Yuan-Sheng, Xia Xiao-Xu, Wang Yu-Chong, Chen Xiao-Shuai, Zheng Hang-Hai. Recognition of geological age for acanthomorphic acritarchs from the Ruyang Group,southern margin of North China Craton and its implication for evolution of early eukaryotes[J]. JOPC, 2018, 20(4): 595-608.

http://www.gdlxb.cn/CN/Y2018/V20/I4/595

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华北克拉通南缘汝阳群大型具刺疑源类时代再厘定及早期真核生物群演化意义^*