大兴安岭中段晚二叠世林西组介形虫化石及环境意义

doi:10.13278/j.cnki.jjuese.20190086

摘要/Abstract

摘要： 晚二叠世-中三叠世在中亚造山带东段构造演化过程中是承上启下的关键地质时期，所以晚二叠世林西组沉积环境对研究古亚洲洋闭合这一重大问题具有重要意义。大兴安岭地区晚二叠世林西组曾有双壳、叶肢介、植物及孢粉化石记录，但鲜有介形虫化石报道。在大兴安岭中段林西组研究中首次发现介形虫化石，经初步研究，主要分子有Kemeroviana，Volganella，Iniella，Qitaina，Darwinuloides，Palaeocypridopsis，Tomiella，Darwinula和Urumqiella等，暂划为Volganella-Kemeroviana组合，其时代为晚二叠世。与俄罗斯地台晚二叠世介形虫化石群关系较为密切，部分属种曾见于我国新疆准噶尔盆地和塔里木盆地。从介形虫化石组合特征和保存特点来看，其生存环境为淡水湖泊，故认为这一地区的林西组为陆相沉积。

关键词: 大兴安岭中段, 晚二叠世, 林西组, 介形虫, 陆相

Abstract: The Late Permian to Middle Triassic is an important tectonic evolution period in the eastern segment of the Central Asia orogenic belt, which is related to the final closure of the Paleo-Asian Ocean and the sharp changes of the sedimentary environment. The well exposed Upper Permian Linxi Formation recorded the evolution history of the Da Hinggan Mountains. The fossils, including sporopollen, conchostracan, bivalves, and megaplants, are found in the Upper Permian Linxi Formation in the southern Da Hinggan Mountains, however only bivalves and a few megaplants are found in the central Da Hinggan Mountains. A total of nine genera ostracods Kemeroviana,Volganella,Iniella,Qitaina,Darwinuloides,Palaeocypridopsis,Tomiella,Darwinula and Urumqiella are found for the first time in the central Da Hinggan Mountains. The paleo-zoogeography of the ostracods assemblage is closely related to those Late Permian ostracods assemblages, which are widely distributed in Russian platform. The evidences of the fossil assemblages and their preservation suggest that Linxi Formation was deposited in a continental lacustrine environment.

Key words: the central Da Hinggan Mountains, Late Permian, Linxi Formation, ostracod, lacustrine facies

中图分类号:

郑月娟, 张健, 张海华, 张德军, 卞雄飞, 陈树旺, 苏飞, 黄欣, 宋绍钧. 大兴安岭中段晚二叠世林西组介形虫化石及环境意义[J]. 吉林大学学报(地球科学版), 2020, 50(6): 1776-1786.

Zheng Yuejuan, Zhang Jian, Zhang Haihua, Zhang Dejun, Bian Xiongfei, Chen Shuwang, Su Fei, Huang Xin, Song Shaojun. New Discovery of Ostracods of Upper Permian Linxi Formation in Central Da Hinggan Mountains and Its Significance[J]. Journal of Jilin University(Earth Science Edition), 2020, 50(6): 1776-1786.

参考文献

[1] Wang H, Liu X Y. Paleoplate Tectonics Between Cathasia and Angaraland in Inner Mongolia of China[J]. Tectonics, 1986, 5(7):1073-1088.
[2] Huang B H. Biogeography of Late Paleozoic Floras of Northeastern China[C]//Ishii K, Liu X Y, Ichikawa K, et al. Pre-Jurassic Geology of Inner Mongolia, China. Osaka:Osaka University, 1991:159-174.
[3] 王荃,刘雪亚,李锦轶.中国华夏与安加拉古陆间的板块构造[M].北京:北京大学出版社,1991:1-151. Wang Quan, Liu Xueya, Li Jinyi. Plate Tectonics of Cathysia and Angara[M]. Beijing:Peking University Press,1991:1-151.
[4] 孙德有,吴福元,张艳斌,等.西拉木伦河-长春-延吉板块缝合带的最后闭合时间:来自吉林大玉山花岗岩体的证据[J]. 吉林大学学报(地球科学版),2004,34(2):174-181. Sun Deyou, Wu Fuyuan, Zhang Yanbin, et al. The Final Closing Time of the West Lamulun River-Changchun-Yanji Plate Suture Zone Evidence from the Dayushan Granitic Pluton, Jilin Province[J]. Journal of Jilin University(Earth Science Edition), 2004, 34(2):174-181.
[5] 李锦轶,高立明,孙桂华,等.内蒙古东部双井子中三叠世同碰撞壳源花岗岩及其对西伯利亚与中朝古板块碰撞时限的约束[J].岩石学报,2007,23(3):565-582. Li Jinyi, Gao Liming, Sun Guihua, et al. Shuangjingzi Middle Triassic Syn-Collisional Crust-Derived Granite in the East Inner Mongolia and Its Constraint on the Timing of Collision Between Siberian and Sino-Korean Paleo-Plates[J]. Acta Petrologica Sinica, 2007, 23(3):565-582.
[6] 李宁,王成文.东北及邻区晚古生代地层接触关系与佳-蒙地块的形成和演化[J]. 吉林大学学报(地球科学版),2017,47(5):1331-1340. Li Ning, Wang Chengwen. Formation and Evolution of Jiamusi-Mongolia Block and Contact Relation Ship of Late Paleozoic Strata in Northeast China and Adjacent Region[J]. Journal of Jilin University(Earth Science Edition), 2017, 47(5):1331-1340.
[7] 周建波,曾维顺,曹嘉麟,等.中国东北地区的构造格局与演化:从500Ma到180Ma[J]. 吉林大学学报(地球科学版),2012,42(5):1298-1316. Zhou Jianbo, Zeng Weishun, Cao Jialin, et al. The Tectonic Framework and Evolution of the NE China from ~500 Ma to ~180 Ma[J]. Journal of Jilin University(Earth Science Edition), 2012, 42(5):1298-1326.
[8] 刘永江,张兴洲,迟效国,等.大兴安岭地区上古生界变形特征及构造层划分[J].吉林大学学报(地球科学版),2011,41(5):1304-1313. Liu Yongjiang, Zhang Xingzhou, Chi Xiaoguo, et al. Deformation and Tectonic Layer Division of the Upper Paleozoic in Daxing'anling Area[J]. Journal of Jilin University(Earth Science Edition), 2011, 41(5):1304-1313.
[9] 张兴洲,乔德武,迟效国,等.东北地区晚古生代构造演化及其石油地质意义[J].地质通报,2011,30(2/3):205-213. Zhang Xingzhou, Qiao Dewu, Chi Xiaoguo, et al. Late-Paleozoic Tectonic Evolution and Oil-Gas Potentiality in Northeastern China[J]. Geological Bulletin of China, 2011, 30(2/3):205-213.
[10] 黄本宏. 大兴安岭地区石炭、二叠系及植物群[M].北京:地质出版社,1993:1-141. Huang Benhong. Greater Khingan Range Carboniferous, Permian and Flora[M]. Beijing:Geological Publishing House, 1993:1-141.
[11] 辽宁省区域地层编写组. 东北地区区域地层表:辽宁省分册[M].北京:地质出版社, 1978:1-296. Liaoning Province Office for Stratigraphic Scale. The Northeast Regional Stratigraphic Table:Fascicule of Liaoning Province[M].Beijing:Geological Publishing House, 1978:1-296.
[12] 梁仲发. 东北北部及内蒙古东部晚二叠世的一些双壳类化石及几个有关地层问题[J].沈阳地质矿产研究所所刊,1982(4):130-148. Liang Zhongfa. The Bivalve Fossils and the Formation Problem of the Late Permian in Northeast Northern and Eastern Inner Mongolia[J]. Journal of Shenyang Institute of Geology and Mineral Resources, 1982(4):130-148.
[13] 王五力.内蒙古昭乌达盟上二叠统陶海营子组的叶肢介化石[J].古生物学报,1984,23(1):124-131. Wang Wuli. Late Permian Conchostraca from the Taohaiyingzi Formation in Juud Meng,Nei Mongol[J].Acta Palaeontologica Sinica,1984, 23(1):124-131.
[14] 内蒙古自治区地质矿产矿局. 内蒙古自治区岩石地层[M].武汉:中国地质大学出版社, 1996:1-344. Bureau of Geology and Mineral Resources of Nei Mongol Autonomous Region. Stratigraphy (Lithostratic) of Nei Mongol Autonomous Region[M]. Wuhan:China University of Geosciences Press, 1996:1-344.
[15] 黑龙江省地质矿产局. 黑龙江省岩石地层[M]. 武汉:中国地质大学出版社, 1997:1-298. Bureau of Geology and Mineral Resources of Heilongjiang Province. Stratigraphy (Lithostratic) of Heilongjiang Province[M]. Wuhan:China University of Geosciences Press, 1997:1-298.
[16] 刘永高,谭佐山,刘书金. 内蒙古东部的上二叠统林西组[J].内蒙古地质,1999(2):21-26. Liu Yonggao,Tan Zuoshan, Liu Shujin. Linxi Formation of Upper Permian Series in the Eastern Inner Mongola[J]. Geology of Inner Mangolia, 1999(2):21-26.
[17] 张永生,牛绍武,田树刚,等. 内蒙古林西地区上二叠统林西组叶肢介化石的发现及其意义[J]. 地质通报,2012:31(9):1394-1403. Zhang Yongsheng, Niu Shaowu, Tian Shugang, et al. The Discovery of Conchostracan Fossils in the Upper Permian Linxi Formation of Linxi Area, Inner Mongolia, and Its Geological Significance[J]. Geological Bulletin of China, 2012, 31(9):1394-1403.
[18] 郑月娟,张健,陈树旺,等.内蒙古阿鲁科尔沁旗陶海营子剖面林西组化石新发现[J]. 地质通报, 2013, 23(8):1269-1276. Zheng Yuejuan, Zhang Jian, Chen Shuwang, et al. New Fossil Discovery Along the Section of Linxi Formation at Taohaiyingzi in Arhorqin Banner, Inner Mongolia[J]. Geological Bulletin of China, 2013, 32(8):1269-1276.
[19] 杨兵,张雄华,葛梦春,等.内蒙古林西地区晚二叠世-早三叠世孢粉组合及三叠系的发现[J].地球科学:中国地质大学学报, 2014, 39(7):784-794. Yang Bing,Zhang Xionghua,Ge Mengchun,et al. Late Permian-Early Triassic Palynological Assemblages in Linxi,Inner Mongolia and Discovery of Triassic Strata[J]. Earth Science:Journal of China University of Geosciences,2014, 39(7):784-794.
[20] Zhang Dejun, Sun Yuewu, Ding Haisheng, et al. Lopinggian Mixed Floras from Linxi Formation in Soron Area, Inner Mongolia[J].Global Geology, 2014, 17(2):67-77.
[21] 黄本宏. 东北北部石炭二叠纪陆相地层及古地理概况[J].地质评论,1982,28(5):395-401. Huang Benhong. Permo-Carboniferous Terrestrial Deposits and Paleogeographic Features in the Northern Part of Northeast China[J]. Geological Review, 1982, 28(5):395-401.
[22] 王永争,覃功炯,欧强. 内蒙古林西大井铜锡多金属矿区上二叠统林西组之研究[J].矿产与地质, 2001,15(3):205-211. Wang Yongzheng, Qin Gongjiong, Ou Qiang. A Stady on the Upper-Permain Linxi Formation on the Dajing Copper-Tin Polymetallic Mine, Linxi, Inner Mongolia[J]. Mineral Resources and Geology,2001, 15(3):205-211.
[23] 李树才,张雄华,李元柏,等.内蒙古林西地区林西组地质时代及沉积环境[J].地质科技情报,2019,38(1):1-7. Li Shucai, Zhang Xionghua, Li Yuanbai, et al. Geological Age Linxi Formation in Linxi Inner Mongolia, and Its Sedimentary Environment[J]. Geological Science and Technology Information, 2019, 38(1):1-7.
[24] 李福来, 曲希玉, 刘立, 等. 内蒙古东北部上二叠统林西组沉积环境[J].沉积学报, 2009,27(2):265-272. Li Fulai, Qu Xiyu, Liu Li,et al. Sedimentary Environment on Upper Permain Linxi Group in Inner Mongolia[J]. Acta Sedimentological Sinica, 2009,27(2):265-272.
[25] 张健,李晓海,郑月娟,等.内蒙古扎鲁特地区上二叠统林西组古盐度分析[J].地质与资源,2013,23(6):471-477. Zhang Jian, Li Xiaohai, Zheng Yuejuan, et al. Analysis on the Paleosalinity of Upper of Permain Linxi Formation in Jarud Area, Inner Mengolia[J]. Geology and Resource, 2013,23(6):471-477.
[26] 于京都,张金川,毛俊丽,等.内蒙古扎鲁特旗林西组页岩沉积环境的地球化学表征[J]. 成都理工大学学报(自然科学版),2015, 42(3):279-287. Yu Jingdu, Zhang Jinchuan, Mao Junli, et al. Geochemical Representation of Sedimentary Environment of Linxi Formation Shale in Jarud Area, Inner Mengolia,China[J]. Journal of Chengdu University of Technology(Science & Technology Edition), 2015, 42(3):279-287.
[27] 孙鹏,唐友军,张永生,等. 林西县官地剖面林西组烃源岩生物标志化合物特征[J]. 长江大学学报(自然科学版),2016,13(32):1-6. Sun Peng, Tang Youjun, Zhang Yongsheng, et al. The Characteristics of Biomarker Compounds of Source Rocks in Linxi Formation in Guandi Section of Linxi County in the East of Inner Mongolia[J]. Journal of Yangtze University (Natureal Science Edition), 2016, 13(32):1-6.
[28] 徐浩, 解启来, 王嗣敏, 等.内蒙古东部中上二叠统烃源岩地化特征与生烃潜力评价[J].大庆石油地质与开发,2017, 36(1):35-42. Xu Hao, Xie Qilai, Wang Simin, et al. Geochemical Characteristics and Hydrocapbon-Generating Potential for Middle-Upper Permain Source Rocks in East Inner Mongolia[J]. Petroleum Geology and Oilfield Development in Daqing,2017,36(1):35-42.
[29] 和政军, 刘淑文, 任纪舜.内蒙古林西地区晚二叠世-早三叠世沉积演化及构造背景[J].中国区域地质,1997,16(4):403-427. He Zhengjun, Liu Shuwen, Ren Jishun,et al. Late Permian-Early Triassic Sedimentary Evolution and Tectonic Setting of the Linxi Region, Inner Mongolia[J]. Regional Geology of China, 1997, 16(4):403-427.
[30] 张永生,田树刚,李子舜,等. 兴蒙地区二叠系乐平统林西组上部发现海相化石[J].科学通报,2013,58(33):3429-3439. Zhang Yongsheng, Tian Shugang, Li Zishun, et al. Discovery of Marine Fossils in the Upper Part of the Permaian Linxi Formation in Lopingian, Xingmeng Area,China[J]. Chinese Science Bulletin, 2013, 58(33):3429-3439.
[31] 翟大兴, 张永生, 田树刚,等. 内蒙古林西地区上二叠统林西组沉积环境与演变[J].古地理学报,2015,17(3):359-370. Zhai Daxing, Zhang Yongsheng, Tian Shugang, et al. Sedimentary Environment and Evolution of the Upper Permian Linxi Formation in Linxi Area Inner Mongolia[J]. Journal of Palaeogeography, 2015, 17(3):359-370.
[32] 翟大兴, 张永生, 田树刚,等.兴蒙地区晚二叠世林西组灰岩微量元素与碳、氧同位素特征及沉积环境讨论[J].地球学报,2015, 36(3):332-342. Zhai Daxing, Zhang Yongsheng, Tian Shugang, et al. The Late Permain Sedimentary Environments of Linxi Formation in Xingmeng Area:Constraints from Carbon and Oxygen Isotopes and Trace Elements[J]. Acta Geoscientia Sinica, 2015, 36(3):332-342.
[33] 关少曾.新疆塔里木盆地西缘晚二叠世介形类[J].微体古生物学报,1985,2(3):239-247. Guan Shaozeng. Late Permain Ostracods from the Western Border of Tarim Basin, Xinjiang[J]. Acta Micropalaeontologica Sinica, 1985,2(3):239-247.
[34] 庞其清.新疆天山北麓陆相二叠-三叠系界线的初步探讨[J].新疆地质,1985,3(4):93-98. Pang Qiqing. Preliminary Discussion on the Contiental Permain-Trissic Boundary in the Northern Foot of Tianshan Mountains[J]. Xinjiang Geology, 1985, 3(4):93-98.
[35] 庞其清,金小赤.新疆吉木萨尔大龙口锅底坑组的介形虫及陆相二叠系-三叠系界限[C]//中国地质科学院地质研究所. 地层古生物论文集. 北京:地质出版社,2004:205-240. Pang Qiqing, Jin Xiaochi. Ostracoda of the Guodikeng Formation and the Continental Permo-Trisssic Boundary of Dalongkou Section, Jimsar, Xinjiang[C]//Institute of Geology,Chinese Academy of Geological Sciences. Professional Papers Stratigraphy and Palaeontology.Beijing:Geological Publishing House, 2004:205-240.
[36] 刘淑文, 李友桂, 王世涛, 等.新疆和田杜瓦二叠-三叠纪动物化石研究[J].新疆地质,1990,8(1):36-46. Liu Shuwen, Li Yougui, Wang Shitao, et al. Stady of Some Permain-Triassic Fauna Fossilis in Duwa Hotan Xinjiang[J]. Xinjiang Geology, 1990, 8(1):36-46.
[37] 周统顺,李佩贤,杨基端,等. 中国非海相二叠-三叠系界线层型剖面研究[J].新疆地质,1997,15(3):211-226. Zhou Tongshun, Li Peixian, Yang Jiduan, et al. Strato-Type Section of Non-Marine Permian-Triassic Boundary in China[J]. Xinjiang Geology, 1997, 15(3):211-226.
[38] 刘兵,温泉波,刘永江,等.大兴安岭中段上二叠统-下三叠统接触关系研究:来自碎屑锆石年代学的证据[J].大地构造与成矿学,2014,38(2):408-420. Liu Bing, Wen Quanbo, Liu Yongjiang, et al. Contact Relationship Between the Upper Permian and Lower Triassic Strata in the Central Great Xing'an Ranges and Its Tectonic Implication:Constraints from the Detrital Zircon U-Pb Ages[J]. Eotectonica et Metallogenia, 2014, 38(2):408-420.
[39] 王尚启. 非海相介形类一新科Panxianiidae[J].古生物学报, 1980, 19(4):302-310. Wang Shangqi. Panxianiidae, a New Family of Non-Marine Ostracoda[J].Acta Palaeontologica Sinica,1980, 19(4):302-310.
[40] 王尚启.黔西滇东北晚二叠世及早三叠世介形类化石[J].古生物学报,1978,17(3):277-308. Wang Shangqi. Late Permain and Early Triassic Costracods of Western Guizhou and Northeastern Yunnan[J]. Acta Palaeontologica Sinica, 1978, 17(3):277-308.
[41] Мандельштам М И. Остракоды Угленосных Отложени Кузнецкого Бассейна, Атлас Руководящих Форм Ископаемых Фауны И Флоры Пермских Отложений Кузницкого Бассейна[M]. Москва:ВСЕГЕИ, 1956:58-108.
[42] 蒋显庭, 周维芬, 林树磐, 等. 新疆地层及介形类化石[M].北京:地质出版社,1995:1-577. Jiang Xianting, Zhou Weifen, Lin Shupan, et al. Xinjiang Strata and Ostracod Fauna[M]. Beijing:Geological Publishing House, 1995:1-577.
[43] 王思恩.内蒙白彦花水塘中现生叶肢介的生态考察及其对古环境重建的意义[J].古地理学报,2008,10(2):203-206. Wang Sien. Ecology Investigation on Living Conchostracans in Pools of Inner Mongolia Baiyanhua and Its Implication for Palaeoenvironmental Reconstruction[J]. Journal of Palaeogeography,2008, 10(2):203-206.
[44] Chen Peiji. Cretaceous Conchostracan Biostratigraphy of China[J]. Journal of Stratigraphy, 2012, 36(2):300-313.
[45] 卢进才,牛绍武, 魏建设. 银额盆地西部蒙额地1井二叠纪叶肢介的发现及其意义[J].地质通报,2018, 31(1):16-25. Lu Jincai, Niu Shaowu, Wei Jianshe. The Discovery of Permian Estheria in the Core of No. 1 Meng'edi Well, Western Yingen-Ejin Basin, and Its Significance[J]. Geological Bulletin of China, 2018, 37(1):16-25.
[46] 王尚启.中国南方晚古生代介形类的某些集群及其生态探讨[J].古生物学报,1988,27(1):91-102. Wang Shangqi. Late Paleozoic Ostracode Associations from South China and Their Paleoecological Signification[J]. Acta Palaeontologica Sinica,1988, 27(1):91-102.
[47] 李军,余俊清.湖相介形虫古生态学在环境变化研究中的应用[J]. 盐湖研究, 2002, 10(1):66-72. Li Jun, Yu Junqing.Application of Lacustrine Ostracodes to the Study of Environmental Changes[J]. Journal of Salt Lake Research, 2002, 10(1):66-72.

Metrics

Viewed

Full text

Abstract

Cited

Shared

Discussed