吉林大学学报(地球科学版) ›› 2019, Vol. 49 ›› Issue (5): 1350-1361.doi: 10.13278/j.cnki.jjuese.20180190

• 地质与资源 • 上一篇    下一篇

大兴安岭南部二叠纪-三叠纪之交孢粉化石及古气候环境分析

张德军, 张健, 郑月娟, 陈树旺, 苏飞, 黄欣, 张海华, 甄甄   

  1. 中国地质调查局沈阳地质调查中心, 沈阳 110034
  • 收稿日期:2018-07-17 发布日期:2019-10-10
  • 通讯作者: 张健(1980-),男,高级工程师,硕士,主要从事沉积学研究,E-mail:48487885@qq.com E-mail:48487885@qq.com
  • 作者简介:张德军(1987-),男,工程师,硕士,主要从事古生物学与地层学研究,E-mail:532413639@qq.com
  • 基金资助:
    中国地质调查局项目(DD20190097,DD20160198,DD20160163),国家自然科学基金项目(31670215,41702032)

Discovery and Paleoclimatic Significances of Permian-Triassic Sporopollen Fossils from Southern Da Hinggan Mountains

Zhang Dejun, Zhang Jian, Zheng Yuejuan, Chen Shuwang, Su Fei, Huang Xin, Zhang Haihua, Zhen Zhen   

  1. Shenyang Center, China Geological Survey, Shenyang 110034, China
  • Received:2018-07-17 Published:2019-10-10
  • Supported by:
    Supported by Projects of China Geological Survey (DD20190097,DD20160198,DD20160163) and National Natural Science Foundation of China(31670215,41702032)

摘要: 大兴安岭南部巴林右旗幸福之路苏木查干布拉格村老龙头组(原幸福之路组模式)剖面首次发现孢粉化石18属21种,以Cyclogranisporites sp.,Alisporites parvus De Jersey,Alisporites circulicorpus Clarke,Sulcatisporites rhombicus Qu,Lueckisporites virkkiae R.Potonie et Klaus,Piceites sp.为主。通过典型属种对比,结合已发现的动植物化石、孢粉组合及同位素测年结果分析,确定幸福之路地区老龙头组的时代为晚二叠世-早三叠世,即二叠系-三叠系界限存在于这套陆相连续沉积内部。孢粉化石的亲缘母体以发育种子蕨纲和松柏纲的针叶植物为主,指示当时研究区处于暖温带的干旱-半干旱的古气候环境。

关键词: 老龙头组, 孢粉, 古气候环境, 二叠纪-三叠纪界限, 大兴安岭南部

Abstract: A total of 21 species of the 18 genera sporopollen fossils are discovered for the first time from the section of the Laolongtou Formation (stratotype section of Xingfuzhilu Formation) in Chaganbulage Village, Xingfuzhilu Town, Bairin Right Banner, Southern Da Hinggan Mountains, including Cyclogranisporites sp., Alisporites parvus De Jersey, Alisporites circulicorpus Clarke, Sulcatisporites rhombicus Qu, Lueckisporites virkkiae R. Potonie et Klaus, Piceites sp., et al. Comparing the typical members with the contemporaneous sporopollen assemblages, and combining with the research results,such as the fauna, flora, sporopollen assemblages and LA-ICP-MS zircon geochronology, the Laolongtou Formation should be formed in the Latest Permian to Early Triassic. The botanical affinities of the sporopollen fossils mainly consist of conifers, belonging to a dry-semi arid and hot-worm climate environment prevailing from the Latest Permian to Early Triassic in Xingfuzhilu area.

Key words: Laolongtou Formation, spores and pollen, paleo-climatic environment, Permian-Triassic boundary, Southern Da Hinggan Mountains

中图分类号: 

  • P52
[1] 朱儒峰, 郑广瑞. 大兴安岭南部下三叠统幸福之路组的建立及其地质意义[J]. 中国区域地质, 1992(3):219-225. Zhu Rufeng, Zheng Guangrui. The Establishment of the Lower Triassic Xingfuzhilu Formation in the Southern Sector of the Greater Khingan Mountains and Its Geological Implications[J]. Regional Geology of China, 1992(3):219-225.
[2] 杨雅军,张立东,张立君,等. 大兴安岭地区三叠系划分与对比[J]. 地质与资源, 2012, 21(1):67-73. Yang Yajun, Zhang Lidong, Zhang Lijun, et al. Division and Correlation of the Triassic Strata in Daxinganling Region[J]. Geology and Resources, 2012, 21(1):67-73.
[3] 聂立军,于宏斌,张建泽,等. 吉林省下三叠统卢家屯组LA-ICP-MS锆石U-Pb定年及其地质意义[J]. 吉林大学学报(地球科学版), 2015, 45(2):453-470. Nie Lijun, Yu Hongbin, Zhang Jianze, et al. Zircons LA-ICP-MS U-Pb Ages of the Lower Triassic Lujiatun Group and Its Geological Significance in Jilin Province[J]. Journal of Jilin University (Earth Science Edition), 2015, 45(2):453-470.
[4] 郑月娟,苏飞,陈树旺,等. 内蒙古巴林右旗下三叠统幸福之路组化石新发现[J]. 地质通报, 2013, 32(9):1423-1435. Zheng Yuejuan, Su Fei, Chen Shuwang, et al. New Discovery of Fossils in the Lower Triassic Xingfuzhilu Formation, Bairin Right Banner, Inner Mongolia[J]. Geological Bulletin of China, 2013, 32(9):1423-1435.
[5] 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.
[6] 钟筱春, 赵传本, 杨时中, 等. 中国北方侏罗系:Ⅱ:古环境与油气[M]. 北京:石油工业出版社, 2003:1-201. Zhong Xiaochun, Zhao Chuanben, Yang Shizhong, et al. Jurassic System in the North of China:Ⅱ:Palaeoenvironment and Oil-Gas Source[M]. Beijing:Petroleum Industry Press, 2003:1-201.
[7] 吉利明,吴涛,李林涛. 陇东三叠系延长组主要油源岩发育时期的古气候特征[J]. 沉积学报, 2006, 24(3):426-431. Ji Liming, Wu Tao, Li Lintao. Paleoclimatic Characteristics During Sedimentary Period of Main Source Rocks of Yanchang Formation (Triassic) in Eastern Gansu[J]. Acta Sedimentologica Sinica, 2006, 24(3):426-431.
[8] Evelyn K,Johanna H A, Konijnenburg-van C, et al. Macrofloras and Palynomorphs As Possible Proxies for Palaeoclimatic and Palaeoecological Studies:A Case Study from the Pelsonian (Middle Triassic) of Kühwiesenkopf/Monte Prà Della Vacca (Olang Dolomites, N-Italy)[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2010, 290(1):71-80.
[9] Mader A F. A Record of Climatic Changes in the Triassic Palynological Spectra from Poland[J]. Geological Quarterly, 2015, 59(4):615-653.
[10] Hochuli P A, Vigran J O, Hermann E, et al. Multiple Climatic Changes Around the Permian-Triassic Boundary Event Revealed by an Expanded Palynological Record from Mid-Norway[J]. Geological Society of America Bulletin, 2010, 122(5/6):884-896.
[11] Elke S H, Wolfram K M, Hans Kerp, et al. Vegetation History Across the Permian-Triassic Boundary in Pakistan (Amb Section, Salt Range)[J]. Gondwana Research, 2013, 27(3):911-924.
[12] 江德昕, 王永栋, 魏江. 新疆乌恰早白垩世孢粉植物群及其环境意义[J]. 古地理学报, 2007, 9(2):185-196. Jiang Dexin, Wang Yongdong, Wei Jiang. Palynofloras and Their Environmental Significance of the Early Cretaceous in Wuqia, Xinjiang Autonomous Region[J]. Journal of Palaeogeography, 2007, 9(2):185-196.
[13] Zhang Mingzhen, Dai Shuang, Heimhofer U, et al. Palynological Records from Two Cores in the Gongpoquan Basin, Central East Asia:Evidence for Floristic and Climatic Change During the Late Jurassic to Early Cretaceous[J]. Review of Palaeobotany and Palynology, 2014, 204:1-17.
[14] Wang Yongdong, Mosbrugger V, Zhang Hong. Early to Middle Jurassic Vegetation and Climatic Events in the Qaidam Basin, Northwest China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2005, 224(1):200-216.
[15] Takahashi K. Palynologic Study of the Akkeshi and Tokotan Formations of the Nemuro Group, Eastern Hokkaido[J]. Nagasaki University's Academic Output SITE, 1991, 31(2):169-513.
[16] 王成文, 孙跃武, 李宁,等. 东北地区晚古生代地层分布规律[J]. 地层学杂志, 2009, 33(1):56-61. Wang Chengwen, Sun Yuewu, Li Ning, et al. On the Distributiong of Late Palaeozoic Strata in Northeast China[J]. Journal of Stratigraphy, 2009, 33(1):56-61.
[17] 内蒙古自治区地质矿产局.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. Inner Mongolia Burau of Geology and Mineral Resources. Lithostratigraphy of Inner Mongolia[M]. Wuhan:China University of Geoscience Press, 1996:1-344.
[18] 郑月娟,黄欣,陈树旺,等. 内蒙古巴林右旗下三叠统幸福之路组凝灰岩LA-ICP-MS锆石U-Pb年龄及其地质意义[J]. 地质通报, 2014, 33(2/3):370-377. Zheng Yuejuan, Huang Xin, Chen Shuwang, et al. LA-ICP-MS Zircon U-Pb Age of the Tuffs of the Lower Triassic Xingfuzhilu Formation in Bairin Right Banner, Inner Mongolia[J]. Geological Bulletin of China, 2014, 33(2/3):370-377.
[19] 和政军, 刘淑文, 王瑜, 等. 内蒙古巴林右旗三叠纪化石的新发现[J]. 地层学杂志, 1998, 22(4):55-56. He Zhengjun, Liu Shuwen, Wang Yu, et al. A New Discovery of Triassic Fossils in Bairin Youqi, Inner Mongolia[J]. Journal of Stratigraphy, 1998, 22(4):55-56.
[20] 张海华, 郑月娟, 陈树旺, 等. 大兴安岭南部幸福之路组的时代及二叠-三叠系界线研究:来自凝灰岩LA-ICP-MS锆石U-Pb年龄的证据[J]. 中国地质, 2015, 42(6):1754-1764. Zhang Haihua, Zheng Yuejuan, Chen Shuwang, et al.Age of Xingfuzhilu Formation and Contact Relationship Between Permian and Triassic Strata in Southern Da Hinggan Mountains:Constraints from the Tuff Zircon U-Pb Ages[J]. Geology in China, 2015, 42(6):1754-1764.
[21] 丁秋红, 陈树旺, 张立君, 等. 松辽盆地外围油气新区中生代地层研究新进展[J]. 地质通报, 2013, 32(8):1159-1176. Ding Qiuhong, Chen Shuwang, Zhang Lijun, et al. New Research Rrogress of the Mesozoic Strata in New Areas on the Periphery of Songliao Basin[J]. Geological Bulletin of China, 2013, 32(8):1159-1176.
[22] 欧阳舒, 朱怀诚, 詹家桢, 等. 新疆准噶尔盆地和塔里木盆地二叠纪孢粉组合的比较及其植物区系和地层意义[J]. 地层学杂志, 2004, 28(3):194-207. Ouyang Shu, Zhu Huaicheng, Zhan Jiazhen, et al. Comparison of Permian Palynofloras from the Junggar and Tarim Basins and Its Bearing on Phytoprovincialism and Stratigraphy[J]. Journal of Stratigraphy, 2004, 28(3):194-207.
[23] 朱文伟, 卜军. 安徽省华北型石炭-二叠纪年代地层划分[J]. 安徽地质, 2011, 21(3):176-179. Zhu Wenwei, Bu Jun. North China-Type Carbonaeous-Permian Chronostratiraphic Divisions in Anhui Province[J]. Geology of Anhui, 2011, 21(3):176-179.
[24] Zhu Huaicheng, Ouyang Shu, Zhan Jiazhen, et al. Comparison of Permian Palynological Assemblages from the Junggar and Tarim Basins and Their Phytoprovincial Significance[J]. Review of Palaeobotany and Palynology, 2005, 136(3):181-207.
[25] Yin Hongfu, Yang Fengqing, Yu Jianxin, et al. An Accurately Delineated Permian-Triassic Boundary in Continental Successions[J]. Science in China:Series D:Earth Sciences, 2007, 50(9):1281-1292.
[26] Spina A, Cirilli S, Utting J, et al. Palynology of the Permian and Triassic of the Tesero and Bulla Sections (Western Dolomites, Italy) and Consideration About the Enigmatic Species Reduviasporonites Chalastus[J]. Review of Palaeobotany and Palynology, 2015, 218:3-14.
[27] Mangerud G. Palynostratigraphy of the Permian and Lowermost Triassic Succession, Finnmark Platform, Barents Sea[J]. Review of Palaeobotany and Palynology, 1994, 82(3):317-349.
[28] Ouyang Shu, John U. Palynology of Upper Permian and Lower Triassic Rocks, Meishan, Changxing County, Zhejiang Province, China[J]. Review of Palaeobotany and Palynology, 1990, 66(1):6-103.
[29] 欧阳舒,王智,詹家祯,等.新疆北部石炭纪-二叠纪孢子花粉研究[M]. 合肥:中国科学技术大学出版社, 2003:1-700. Ouyang Shu, Wang Zhi, Zhan Jiazhen, et al. Palynology of the Carboniferous and Permian Strata of Northern Xinjiang, Northwestern China[M]. Hefei:University of Science and Technology of China Press, 2003:1-700.
[30] 宋之琛, 尚玉珂, 刘兆生,等. 中国孢粉化石:第二卷:中生代孢粉[M]. 北京:科学出版社, 2000:1-710. Song Zhichen, Shang Yuke, Liu Zhaosheng, et al. Fossil Spores and Pollen of China:Vol 2:The Mesozoic Spores and Pollen[M]. Beijing:Science Press, 2000:1-710.
[31] Diez J B, Broutin J, Ferrer J. Difficulties Encountered in Defining the Permian-Triassic Boundary in Buntsandstein Facies of the Western Peritethyan Domain Based on Palynological Data[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2005, 229(1):40-53.
[32] Diez J B, Broutin J, Grauvogel-Stamm L, et al. Anisian Floras from the NE Iberian Peninsula and Balearic Islands:A Synthesis[J]. Review of Palaeobotany and Palynology, 2010, 162(3):522-542.
[33] 陈丕基, 董洁.吉林早三叠世叶肢介的发现及其意义[J]. 科学通报, 1981(18):1128-1130. Chen Peiji, Dong Jie. Discovery and Their Significances of the Early Triassic Conchostracans from Jilin Province[J]. Chinese Science Bulletin, 1981(18):1128-1130.
[34] Preto N, Kustatscher E, Wignall P B. Triassic Climates-State of the Art and Perspectives[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2010, 290(1):1-10.
[35] 王自强. 华北二叠纪大型古植物事件[J]. 古生物学报, 1989, 28(3):314-343. Wang Ziqiang. Permian Gigantic Palaeobotanical Events in North China[J]. Acta Palaeontologica Sinica, 1989, 28(3):314-343.
[36] Retallack G J, Veevers J J, Morante R. Global Coal Gap Between Permian-Triassic Extinction and Middle Triassic Recovery of Peat-Forming Plants[J]. Geological Society of America Bulletin, 1996, 108(2):195-207.
[37] Woods A D. Paleoceanographic and Paleoclimatic Context of Early Triassic Time[J]. Comptes Rendus Palevol, General Paleontology (Paleoecology), 2005, 4:463-472.
[38] Linol B, Bercovici A, Bourquin S, et al. Late Permian to Middle Triassic Correlations and Palaeogeographical Reconstructions in South-Western European Basins:New Sedimentological Data from Minorca (Balearic Islands, Spain)[J]. Sedimentary Geology, 2009, 220(1):77-94.
[39] Durand M. Permian to Triassic Continental Successions in Southern Province (France):An Overview[J]. Bollettino Della Società Geologica Italiana, 2008, 127(3):697-716.
[40] 陈旭, Boucot A J, Scotese C R, 等. 显生宙全球古气候重建[M]. 北京:科学出版社, 2009:1-173. Chen Xu, Boucot A J, Scotese C R, et al. Phanerozoic Global Palaeoclimate Reconstruction[M]. Beijing:Science Press, 2009:1-173.
[1] 李贶家, 顾延生, 刘红叶. 豫北平原全新世孢粉记录气候变化与古文化演替[J]. 吉林大学学报(地球科学版), 2016, 46(5): 1449-1457.
[2] 谭思哲, 高顺莉, 葛和平, 付焱鑫. 南黄海盆地二叠系烃源岩孢粉相特征及其形成环境[J]. 吉林大学学报(地球科学版), 2015, 45(3): 691-700.
[3] 张立原. 中国黄土高原洛川剖面S5以来的孢粉学记录[J]. 吉林大学学报(地球科学版), 2014, 44(1): 222-229.
[4] 黄昌庆, Liu Kambiu, 冯兆东, 冉敏, 杨奇丽, 张晓森. 哈萨克斯坦Tramplin剖面孢粉记录的MIS3a环境变化[J]. 吉林大学学报(地球科学版), 2013, 43(1): 149-154.
[5] 王丹萍, 王锡魁, 江裕标. 长春地区中更新世晚期古环境重建的沉积地球化学与孢粉学证据[J]. J4, 2010, 40(5): 1066-1074.
[6] 张世广, 卢双舫, 邵明礼, 王立武, 仲维维, 申家年, 张学娟, 吴高平, 王民. 松辽盆地南部英台断陷龙深1井深层层位归属[J]. J4, 2010, 40(2): 298-304.
[7] 李秉成. 10 000 aB.P.关中蓝田的植被和气候[J]. J4, 2010, 40(1): 109-113.
[8] 赵炜, 沈如江, 廖文波, 金建华. 海南岛长昌盆地始新世孢粉植物区系[J]. J4, 2009, 39(3): 379-385.
[9] 刘玉英,刘嘉麒,汉景泰. 吉林辉南二龙湾玛珥湖12.0 ka B.P.以来孢粉记录与气候变化[J]. J4, 2009, 39(1): 93-0098.
[10] 史冀忠,刘招君,柳蓉,杜江峰,张健,刘沣. 辽宁抚顺盆地始新世古气候定量研究[J]. J4, 2008, 38(1): 50-0055.
[11] 李 秉 成. 宁夏灵武水洞沟遗址全新世的古气候环境[J]. J4, 2006, 36(01): 49-0053.
[12] 张新荣,胡克,介冬梅,王东坡,刘莉莉. 泥炭沉积中植硅体对环境指示的意义——以吉林敦化泥炭剖面为例[J]. J4, 2005, 35(06): 694-0698.
[13] 田 梦,张梅生,任延广,乔秀云,万传彪,刘鹏举. 松辽盆地新站地区嫩江组三段孢粉-藻类组合及其环境[J]. J4, 2005, 35(04): 449-0455.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] 杨俊鹏,胡 克,刘玉英. 吉林西部盐碱化土壤碳酸盐的碳稳定同位素特征[J]. J4, 2006, 36(02): 245 -0249 .
[2] 郝琦,刘震,查明,李春霞. 辽河茨榆坨潜山太古界裂缝型储层特征及其控制因素[J]. J4, 2006, 36(03): 384 -390 .
[3] 何朋朋,姚磊华,刘立鹏,陈庆. 地下水位随机性影响下的边坡可靠性分析[J]. J4, 2009, 39(2): 288 -0293 .
[4] 任丽华,林承焰,李 辉,王海涛,张荻楠,崔宝文. 海拉尔盆地苏德尔特构造带布达特群裂缝发育期次研究[J]. J4, 2007, 37(3): 484 -0490 .
[5] 杨立英,李瑞磊. 松辽盆地南部深层火山岩、火山机构和火山岩相地质-地震综合识别[J]. J4, 2007, 37(6): 1083 -1090 .
[6] 鲍长利,张建会,刘招君,王影,盛江,王朋,兰心俨. 利用油页岩研制多孔建筑陶瓷[J]. J4, 2008, 38(4): 600 -0603 .
[7] 郝立波, 刘海洋, 陆继龙, 孙淑梅, 潘志恒, 赵玉岩. 松花湖沉积物137Cs和210Pb分布及沉积速率[J]. J4, 2009, 39(3): 470 -473 .
[8] 吴小斌, 侯加根, 孙卫, 雷甜. 基于层次分析方法对姬塬地区流动单元的研究[J]. J4, 2011, 41(4): 1013 -1019 .
[9] 王德利,程浩,朱恒,冯飞. 基于反褶积算法的地震干涉技术被动源成像[J]. 吉林大学学报(地球科学版), 2012, 42(6): 1920 -1926 .
[10] 陈启林,白云来,马玉虎,刘晓光. 再论鄂尔多斯盆地寒武纪岩相古地理及沉积构造演化[J]. 吉林大学学报(地球科学版), 2013, 43(6): 1697 -1715 .