2015年6月，第21卷，第2期，196-202页
June2015，Vol.21，No.2，pp.196202 DOI: 10.16108/j.issn10067493.2014193
高校地质学报
Geological Journal of China Universities
山东淄博太原组有孔虫及石炭系与二叠系界线
李守军1.2，原丽媛3，般天涛4，赵秀丽1,2，崔肖辉
1.山东科技大学地球科学与工程学院，青岛266590；
2.现代古生物学与地层学国家重点实验室（中国科学院南京地质古生物研究所），南京210008；
3.山东省核工业二七三地质大队，烟台264000； 4.中化地质矿山总局山东地质勘查院，济南250013
摘要：通过对山东省淄博地区太原组小有孔虫类动物群的系统研究，共鉴定出小有孔虫11属22种及部分未定种。根据有孔虫类化石在地层中的分布和垂向变化规律，建立了两个小有孔虫化石组合带：IBradyina-Plectogyra组合与IITetrataxis-Nodosaria-Palaeotextularia组合。通过与邻区及华中华北其它地区的有孔虫进行对比，并结合前人对本区类化石的研究结果，确定了各组合带的地质时代：太原组小有孔虫动物群第1组合带地质时代归为晚石炭世，第ⅡI组合带地质时代归为早二
叠世，其层位相当于山东地区太原组箍类Pseudoschaeagerina带之底，关键词：太原组；有孔虫动物群；石炭系与二叠系界线；淄博；山东
中图分类号：P534.4
文献标识码：A
文章编号：10067493（2015）02-0196-07
TheForaminiferalFaunaoftheTaiyuanFormationandthe Carboniferous-PermianBoundaryinZibo,ShandongProvince
LIShoujun.2,YUAN Liyuan',YINTiantao",ZHAOXiuli'2,CUIXiaohui
1. College of Earth Sciences & Engineering, Shandong University of Science and Technology, Qingdao 266590, China
2. State Key Laboratory of Palaeobiology and Stratigraphy (Nanjing Institute of Geology and Palaeontology, CAS), Nanjing 210008, China
3. Geological Group 273, Shandong Province Nuclear Industry, Yantai 264000, China
4, Shandong Geological Prospecting Institute of China Chemical Geology and Mine Bureau, Jinan 250013, China
Abstract: Through the systematic study of the foraminiferal fauna of the Taiyuan Formation in Zibo, Shandong Province, we have identified 11 genera, 22 species, and some undetermined species of small foraminiferal fossils. Based on the spatial distribution and stratigraphic variation in the foraminiferal fauna, two small foraminiferal assemblages are established from the bottom to the top, i.e., BradyinaPlectogyra assemblage and TetrataxisNodosariaPalaeotextularia assemblage. By comparing our fossil data with the foraminiferal fauna in the nearby regions and other areas in Central China and North China, and combining the previous results of fusulinid fossils, we have estimated the geological ages of the two fossil zones. The geological age of the BradyinaPlectogyra assemblage should be Late Carboniferous, and the geological age of the TetrataxisNodosariaPalaeotextularia assemblage should be
Early Permian, So the CarboniferousPermian boundary in Shandong Province lies at the bottom of Pseudoschwagerina zone. Key words: Taiyuan Formation; foraminiferal fauna; CarboniferousPermian boundary; Zibo; Shandong Province
First author: LI Shoujun, Profesor; E-mail: lishoujun@126.com 收稿日期：2014-11-08；修回日期：201504-16
基金项目：现代古生物学与地层学国家重点实验室（中国科学院南京地质古生物研究所）开放课题（123104）资助
作者介：李守军，男，1962年生，教投，博导，主要从事古生物地层学和油气地质学的教学与研究工作；E-mail：lishoujun@126.com