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内蒙古东部霍林河盆地霍林河组的年龄:来自锆石U-Pb测年和孢粉组合的证据
引用本文:史恭乐,李建国,谭覃,董重,李秋立,吴琼,章伯乐,尹素心,HERRERA Fabiany,HERENDEEN Patrick S.,CRANE Peter R..内蒙古东部霍林河盆地霍林河组的年龄:来自锆石U-Pb测年和孢粉组合的证据[J].地层学杂志,2021,45(1):69-81.
作者姓名:史恭乐  李建国  谭覃  董重  李秋立  吴琼  章伯乐  尹素心  HERRERA Fabiany  HERENDEEN Patrick S.  CRANE Peter R.
作者单位:中国科学院南京地质古生物研究所,现代古生物学和地层学国家重点实验室 江苏南京 210008;中国科学院生物演化与环境卓越创新中心 江苏南京 210008;中国科学院南京地质古生物研究所,现代古生物学和地层学国家重点实验室 江苏南京 210008;中国科学院生物演化与环境卓越创新中心 江苏南京 210008;中国科学院大学 北京 100049;中国科学院地质与地球物理研究所,岩石圈演化国家重点实验室 北京 100029;中国科学院大学 北京 100049;南京大学地球科学与工程学院 江苏南京 210023;青岛市勘察测绘研究院 山东青岛 266030;芝加哥植物园,Glencoe,伊利诺伊60022,美国;耶鲁大学环境学院,纽黑文,康涅狄格06511,美国;橡树泉园林基金会,Upperville,弗吉尼亚20184,美国
摘    要:内蒙古东部霍林河盆地霍林河组是我国最重要的下白垩统含煤地层之一.该组产出大量不同种类且保存完好的植物化石,但因为缺乏海相沉积和火山岩夹层,我们对这套地层的精确年龄认知不足.我们最近在扎鲁特旗扎哈淖尔露天煤矿霍林河组发现了火山灰层,基于钻孔数据的地层分析显示该火山灰层位于霍林河组下含煤段的底部.二次离子质谱(SIMS)锆...

关 键 词:霍林河组  早白垩世  含煤盆地  U-Pb地质年代学  孢子花粉  内蒙古

AGE OF THE HUOLINHE FORMATION IN THE HUOLINHE BASIN,EASTERN INNER MONGOLIA,CHINA: EVIDENCE FROM U-Pb ZIRCON DATING AND PALYNOLOGICAL ASSEMBLAGES
SHI Gong Le,LI Jian Guo,TAN Tan,DONG Chong,LI Qiu Li,WU Qiong,ZHANG Bo Le,YIN Su Xin,HERRERA Fabiany,HERENDEEN Patrick S.,CRANE Peter R..AGE OF THE HUOLINHE FORMATION IN THE HUOLINHE BASIN,EASTERN INNER MONGOLIA,CHINA: EVIDENCE FROM U-Pb ZIRCON DATING AND PALYNOLOGICAL ASSEMBLAGES[J].Journal of Stratigraphy,2021,45(1):69-81.
Authors:SHI Gong Le  LI Jian Guo  TAN Tan  DONG Chong  LI Qiu Li  WU Qiong  ZHANG Bo Le  YIN Su Xin  HERRERA Fabiany  HERENDEEN Patrick S  CRANE Peter R
Abstract:The Huolinhe Formation in the Huolinhe Basin,eastern Inner Mongolia is one of the most im-portant Lower Cretaceous coal-bearing strata in China,yielding abundant,diverse,and well-preserved plant fossils.Its precise age,however,is poorly known due to lack of associated marine deposits and volcanic beds.Here we present U-Pb zircon ages,and the associated palynological assemblages of an ash layer of the Huolinhe Formation recently discovered at the Zhahanaoer open-cast coal mine in Jarud Banner.Strati-graphic analyses based on boreholes suggest that the ash layer occurs near the bottom of the"lower coal-bearing member"of the Huolinhe Formation.U-Pb zircon geochronology using the SIMS method con-strains the depositional age of the ash layer to be 125.6±1.0 Ma(late Barremian-earliest Aptian),and this is consistent with the result from LA-ICP-MS analyses of the same sample.A late Barremian-earliest Aptian age for the ash layer is also supported by the palynological assemblage associated with the layer,in which the pollen of gymnosperms and the spores of ferns and bryophytes are dominant,angiosperm pollen is very rare and represented by only Clavatipollenites.This study contributes important new data for understanding the age of the entire Huolinhe Formation and also provides a more precise maximum age for the key plant fossils preserved in the deposits above the ash layer.
Keywords:Huolinhe Formation  Early Cretaceous  coal-bearing basin  U-Pb geochronology  pollen and spores  Inner Mongolia
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