鲁西地区仙人洞剖面凤山组大型柱状叠层石沉积特征
|
摘要
鲁西地区仙人洞剖面寒武系出露连续且沉积现象丰富,芙蓉统凤山组中部发育大型柱状叠层石。在层序地层框架下,基于野外观察,研究大型柱状叠层石的沉积特征。结果表明:寒武系凤山组大型柱状叠层石宏观上呈局部集中产出,柱状体边界清晰,纹层精美,横截面呈圆饼状,相对较大的柱状体直径代表华北地台寒武系叠层石的特殊类型。凤山组叠层石主要由致密泥晶、微亮晶构成,内部可见白云石、生物碎屑、黄铁矿颗粒;在柱状叠层石中可见大量保存精美的葛万菌(Girvanella)、胞网菌(Bacinella)等钙化微生物化石。凤山组大型柱状叠层石的建造者是以蓝细菌为主导的光合作用微生物席。特殊不规则网状物中的钙化丝状体及零星分散的黄铁矿颗粒,指示在大型柱状叠层石形成过程中微生物席内部存在复杂的微生物新陈代谢活动。仙人洞剖面凤山组大型柱状叠层石的发现既为寒武系叠层石研究提供典型实例,也为显生宙第一幕蓝细菌钙化作用发生期提供重要的岩石记录。
The Xianrendong Section of Western Shandong Area is rich in Cambrian outcropping and sedimentation.Based on field observation and lab analysis,the sedimentary characteristics of stromatolites were studied under the framework of sequence stratigraphy.Some investigations showed that the large columnar stromatolites in Fengshan Formation are locally concentrated macroscopically,clear border of the column,fine lamination,and rounded cross-sections,its relatively large column diameter represents a special type of Cambrian stromatolites in North China Platform.The stromatolites in Fengshan Formation are mainly composed of dense micrite and microspar and dolomite,bioclastics and pyrite particles can be seen inside.Besides,a large number of well-preserved calcified microorganism fossils such as Girvanellaand Bacinellacan be found in the main body of stromatolites,which demonstrated the large columnar stromatolites in Xianrendong Section of Cambrian Fengshan Formation were constructed by photosynthetic microbial mats led by cyanobacteria.And calcified filaments in a particularly irregular network and scattered pyrite particles indicate that there are complex microbial metabolic activities in the mat during the formation of large columnar stromatolites.Therefore,the discovery of large columnar stromatolites in Xianrendong Section of Fengshan Formation provides a typical example for the study of Cambrian stromatolites and an important rock record for the first episode of phanerozoic cyanobacteria calcification.
The Xianrendong Section of Western Shandong Area is rich in Cambrian outcropping and sedimentation.Based on field observation and lab analysis,the sedimentary characteristics of stromatolites were studied under the framework of sequence stratigraphy.Some investigations showed that the large columnar stromatolites in Fengshan Formation are locally concentrated macroscopically,clear border of the column,fine lamination,and rounded cross-sections,its relatively large column diameter represents a special type of Cambrian stromatolites in North China Platform.The stromatolites in Fengshan Formation are mainly composed of dense micrite and microspar and dolomite,bioclastics and pyrite particles can be seen inside.Besides,a large number of well-preserved calcified microorganism fossils such as Girvanellaand Bacinellacan be found in the main body of stromatolites,which demonstrated the large columnar stromatolites in Xianrendong Section of Cambrian Fengshan Formation were constructed by photosynthetic microbial mats led by cyanobacteria.And calcified filaments in a particularly irregular network and scattered pyrite particles indicate that there are complex microbial metabolic activities in the mat during the formation of large columnar stromatolites.Therefore,the discovery of large columnar stromatolites in Xianrendong Section of Fengshan Formation provides a typical example for the study of Cambrian stromatolites and an important rock record for the first episode of phanerozoic cyanobacteria calcification.
引文
[1]KALKOWSKY E.Oolith und stromatolith in norddeutschen Buntsandstein[J].Zeitschrift der Deutschen Geologischen Gesellschaft,1908,60:68-125.
[2]SEMIKHATOV M A,GEBELEIN C D,CLOUD P,et al.Stromatolite morphogenesis-progress and problems[J].Canadian Journal of Earth Sciences,1979,16(5):992-1015.
[3]AWRAMIK S M.The history and significance of stromatolites[M]//Early Organic Evolution.Berlin:Springer Berlin Heidelberg,1992:435-449.
[4]RIDING R.Microbial carbonates:the geological record of calcified bacterial-algal mats and biofilms[J].Sedimentology,2000,47(Supp.1):179-214.
[5]梅冥相.微生物碳酸盐岩分类体系的修订:对灰岩成因结构分类体系的补充[J].地学前缘,2007,14(5):222-234.MEI Mingxiang.Revised classification of microbial carbonates:complementing the classification of limestones[J].Earth Science Frontiers,2007,14(5):222-234.
[6]陈旭,阮亦萍,布科A J.中国古生代气候演变[M].北京:科学出版社,2001:14-20.CHEN Xu,RUAN Yiping,BOUCOT A J.Paleozoic climate evolution in China[M].Beijing:Science Press,2001:14-20.
[7]陈荣坤,孟祥化.华北地台早古生代沉积建造及台地演化[J].沉积与特提斯地质,1993,13(4):46-55.CHEN Rongkun,MENG Xianghua.Early Palaeozoic sedimentary suites and the evolution of the North China Platform[J].Sedimentary Geology and Tethyan Geology,1993,13(4):46-55.
[8]RIDING R.Cyanobacterial calcification,carbon dioxide concentrating mechanisms,and Proterozoic-Cambrian changes in atmospheric composition[J].Geobiology,2006,4(4):299-316.
[9]RIDING R.Microbialites,stromatolites and thrombolites[M]//REITNER J,THIEL V.Encyclopedia of Geobiology.Netherlands:Springer,2011:635-654.
[10]高振西,熊永先,高平.中国北部震旦纪地层(英文)[J].中国地质学会志,1934(1):267-318.GAO Zhenxi,XIONG Yongxian,GAO Ping.Preliminary notes on Sinian stratigraphy of North China[J].Bulletin of the Geological Society of China,1934(1):267-318.
[11]杨杰.山西五台山南台之南变质石灰岩内之椎管状化石[J].地质论评,1936,1(2):213.YANG Jie.Vertebral tubular fossil in metamorphic limestone on the south of Wutai Mountain,Shanxi[J].Geological Review,1936,1(2):213.
[12]曹瑞骥,袁训来.叠层石[M].合肥:中国科学技术大学出版社,2006:45-53.CAO Ruiji,YUAN Xunlai.Stromatolite[M].Hefei:Press of University of Science and Technology of China,2006:45-53.
[13]梅冥相,刘丽,胡媛.北京西郊寒武系凤山组叠层石生物层[J].地质学报,2015,89(2):440-460.MEI Mingxiang,LIU Li,HU Yuan.Stromatolitic bostrome of the Cambrian Fengshan Formation at the Xiaweidian Section in the wstern sburb of Beijing,North China[J].Acta Geologica Sinica,2015,89(2):440-460.
[14]梅冥相,张瑞,李屹尧,等.华北地台东北缘寒武系芙蓉统叠层石生物丘中的钙化蓝细菌[J].岩石学报,2017,33(4):1073-1093.MEI Mingxiang,ZHANG Rui,LI Yiyao,et al.Calcified cyanobacterias within the stromatolotic bioherm for the Cambrian Furongian Series in the northeastern margin of the North-China Platform[J].Acta Petrologica Sinica,2017,33(4):1073-1093.
[15]CHEN J,LEE J H,WOO J.Formative mechanisms,depositional processes,and geological implications of Furongian(Late Cambrian)Reefs in the North China Platform[J].Palaeogeography Palaeoclimatology Palaeoecology,2014,414(9):246-259.
[16]LEE J H,CHEN J,CHOUGH S K.Paleoenvironmental implications of an extensive maceriate microbialite bed in the Furongian Chaomidian Formation,Shandong Province,China[J].Palaeogeography Palaeoclimatology Palaeoecology,2010,297(4):621-632.
[17]韩作振,陈吉涛,张晓蕾,等.鲁西寒武系第三统张夏组附枝菌与附枝菌微生物灰岩特征研究[J].地质学报,2009,83(8):1097-1103.HAN Zuozhen,CHEN Jitao,ZHANG Xiaolei,et al.Characteristics of Epiphytonand Epiphyton microbialites in the Zhangxia Formation(Third Series of Cambrian),Shandong Province[J].Acta Geologica Sinica,2009,83(8):1097-1103.
[18]彭善池.全球寒武系四统划分框架正式确立[J].地层学杂志,2006,30(2):147-148.PENG Shanchi.The framework of the global Cambrian quaternary division was formally established[J].Journal of Stratigraphy,2006,30(2):147-148.
[19]卢衍豪,朱兆玲,钱义元,等.中国寒武纪地层对比表及说明书[M]//中国科学院南京地质古生物研究所.中国各纪地层对比表及说明书.北京:科学出版社,1982:28-54.LU Yanhao,ZHU Zhaoling,QIAN Yiyuan,et al.Stratigraphical correlation tables and their directions for the Cambrian in China[M]//Institute of Palaeontology and Geology of China Academy of Science.Stratigraphical correlation tables and their directions for Each Periods.Beijing:Science Press,1982:28-54.
[20]肖恩照,隋明园,覃英伦,等.河北涞源祁家峪剖面寒武系层序地层划分[J].大庆石油地质与开发,2017,36(6):20-29.XIAO Enzhao,SUI Mingyuan,QIN Yinglun,et al.Cambrian sequence stratigraphic division for Qijiayu Section in Hebei Laiyuan[J].Petroleum Geology and Oilfield Development in Daqing,2017,36(6):20-29.
[21]肖恩照,覃英伦,MUHAMMAD RIAZ,等.吕梁山东北缘寒武系层序地层划分:以文水苍尔会剖面为例[J].东北石油大学学报,2017,41(5):43-53.XIAO Enzhao,QIN Yinglun,MUHAMMAD RIAZ,et al.Sequence stratigraphy division of Cambrian in the northeast area of Lyuliang Mountain:a case study of the Cangerhui Section in Wenshui City[J].Journal of Northeast Petroleum University,2017,41(5):43-53.
[22]GOLDHAMMER R K,DUNN P A,HARDIE L A.Depositional cycles,composite sea-level changes,cycle stacking patterns,and the hierarchy of stratigraphic forcing:examples from Alpine Triassic platform carbonates[J].Geological Society of America Bulletin,1990,102(5):535-562.
[23]梅冥相.从正常海退与强迫型海退的辨别进行层序界面对比:层序地层学进展之一[J].古地理学报,2010,12(5):549-564.MEI Mingxiang.Correlation of sequence boundaries according to discerning between normal and forced regressions:the first advance in sequence stratigraphy[J].Journal of Palaeogeography,2010,12(5):549-564.
[24]孟祥化,乔秀夫,葛铭.华北古浅海碳酸盐风暴沉积和丁家滩相序模式[J].沉积学报,1986,4(2):1-18.MENG Xianghua,QIAO Xiufu,GE Ming.Storm deposits of the paleoepicontinental sea and the Dingjiatan Model in the Cambrian of the North China Platform[J].Acta Sedimentologia Sinica,1986,4(2):1-18.
[25]CHEN J T.Origin of the Furongian limestone breccias in the North China Platform[J].Science China Earth Sciences,2015,58(5):770-775.
[26]VAIL P,MITCHUM R,THOMPSON III S.Seismic stratigraphy and global changes of sea level:art 3.Relative changes of sea level from coastal onlap:ection 2.Application of seismic reflection configuration to stratigraphic interpretation[M].[S.l.]:Seismic Stratigraphy-Applications to Hydrocarbon Exploration,1977:63-81.
[27]CUMINGS E R.Reefs or bioherms[J].Geological Society of America Bulletin,1932,43(1):331-352.
[28]COULSON K P,BRAND L R.Lithistid sponge-microbial reef-building communities construct laminated,Upper Cambrian(Furongian)'stromatolites[J].Palaios,2016,31(7):358-370.
[29]WOODS,ADAM D.Microbial ooids and cortoids from the Lower Triassic(Spathian)virgin limestone,Nevada USA:evidence for an Early Triassic microbial bloom in shallow depositional environments[J].Global and Planetary Change,2013,105:91-101.
[30]齐永安,张喜洋,代明月,等.豫西寒武系微生物岩中的葛万菌化石及其微观结构[J].古生物学报,2017,56(2):154-167.QI Yong'an,ZHANG Xiyang,DAI Mingyue,et al.Girvanellafossils and their microstructure from Cambrian microbialites of Western Henan[J].Acta Palaeontologica Sinica,2017,56(2):154-167.
[31]RIDING R.Calcified plectonema(blue-green algae),a recent example of Girvanellafrom Aldabra Atoll[J].Palaeontology,1977,20:33-46.
[32]LEE J H,RIDING R,CHERNS L.Xinellar:a new mat-forming calcified cyanobacterium from the Middle-Late Ordovician of North China[J].Papers in Palaeontology,2016,2(3):439-449.
[33]SCHLAGINTWET F,BOVER-ARNAL T.Remarks on Bacinella Radoicic,1959(type species B.irregularis)and its representatives[J].Facies,2010,56(4):635-673.
[34]LUO C,REITNER J.'Stromatolites'built by sponges and microbes-a new type of Phanerozoic bioconstruction[J].Lethaia,2016,49(4):555-570.
[35]WANG L,SHI X,JIANG G.Pyrite morphology and redox fluctuations recorded in the Ediacaran Doushantuo Formation[J].Palaeogeography Palaeoclimatology Palaeoecology,2012,333(2):218-227.
[36]VISSCHER P T,REID R P.Microscale observations of sulfate reduction:correlation of microbial activity with lithified[J].Geology,2000,28(10):919-922.
[37]朱士兴,黄学光.13亿年前叠层石的生长节律和地—日—月动力学(英文)[J].微体古生物学报,2003(1):23-30.ZHU Shixing,HUANG Xueguang.The earth-sun-moon dynamics from growth rhythms of 1 300Ma stromatolites[J].Acta Micropalaeontologica Sinica,2003(1):23-30.
[38]梅冥相,孟庆芬.现代叠层石的多样化构成:认识古代叠层石形成的关键和窗口[J].古地理学报,2016,18(2):127-146.MEI Mingxiang,MENG Qingfen.Composition diversity of modern stromatolites:a key and window for further understanding of the formation of ancient stromatolites[J].Journal of Palaeogeography,2016,18(2):127-146.
[39]王皓,肖恩照.山西灵丘刁泉剖面寒武系第三统张夏组核形石[J].东北石油大学学报,2018,42(5):44-53.WANG Hao,XIAO Enzhao.Oncolites in Cambrian Series 3at Diaoquan Section in Lingqiu,Shanxi[J].Journal of Northeast Petroleum University,2018,42(5):44-53.
[40]梅冥相,RIAZ M,刘丽,等.辽东半岛复州湾剖面寒武系第二统光合作用生物膜建造的核形石[J].古地理学报,2019,21(1):31-48.MEI Mingxiang,RIAZ M,LIU Li,et al.Oncoids built by photosynthetic biofilms:an example from the Series 2of Cambrian at Fuzhouwan Section in Liaodong Peninsula[J].Journal of Palaeogeography,2019,21(1):31-48.
[2]SEMIKHATOV M A,GEBELEIN C D,CLOUD P,et al.Stromatolite morphogenesis-progress and problems[J].Canadian Journal of Earth Sciences,1979,16(5):992-1015.
[3]AWRAMIK S M.The history and significance of stromatolites[M]//Early Organic Evolution.Berlin:Springer Berlin Heidelberg,1992:435-449.
[4]RIDING R.Microbial carbonates:the geological record of calcified bacterial-algal mats and biofilms[J].Sedimentology,2000,47(Supp.1):179-214.
[5]梅冥相.微生物碳酸盐岩分类体系的修订:对灰岩成因结构分类体系的补充[J].地学前缘,2007,14(5):222-234.MEI Mingxiang.Revised classification of microbial carbonates:complementing the classification of limestones[J].Earth Science Frontiers,2007,14(5):222-234.
[6]陈旭,阮亦萍,布科A J.中国古生代气候演变[M].北京:科学出版社,2001:14-20.CHEN Xu,RUAN Yiping,BOUCOT A J.Paleozoic climate evolution in China[M].Beijing:Science Press,2001:14-20.
[7]陈荣坤,孟祥化.华北地台早古生代沉积建造及台地演化[J].沉积与特提斯地质,1993,13(4):46-55.CHEN Rongkun,MENG Xianghua.Early Palaeozoic sedimentary suites and the evolution of the North China Platform[J].Sedimentary Geology and Tethyan Geology,1993,13(4):46-55.
[8]RIDING R.Cyanobacterial calcification,carbon dioxide concentrating mechanisms,and Proterozoic-Cambrian changes in atmospheric composition[J].Geobiology,2006,4(4):299-316.
[9]RIDING R.Microbialites,stromatolites and thrombolites[M]//REITNER J,THIEL V.Encyclopedia of Geobiology.Netherlands:Springer,2011:635-654.
[10]高振西,熊永先,高平.中国北部震旦纪地层(英文)[J].中国地质学会志,1934(1):267-318.GAO Zhenxi,XIONG Yongxian,GAO Ping.Preliminary notes on Sinian stratigraphy of North China[J].Bulletin of the Geological Society of China,1934(1):267-318.
[11]杨杰.山西五台山南台之南变质石灰岩内之椎管状化石[J].地质论评,1936,1(2):213.YANG Jie.Vertebral tubular fossil in metamorphic limestone on the south of Wutai Mountain,Shanxi[J].Geological Review,1936,1(2):213.
[12]曹瑞骥,袁训来.叠层石[M].合肥:中国科学技术大学出版社,2006:45-53.CAO Ruiji,YUAN Xunlai.Stromatolite[M].Hefei:Press of University of Science and Technology of China,2006:45-53.
[13]梅冥相,刘丽,胡媛.北京西郊寒武系凤山组叠层石生物层[J].地质学报,2015,89(2):440-460.MEI Mingxiang,LIU Li,HU Yuan.Stromatolitic bostrome of the Cambrian Fengshan Formation at the Xiaweidian Section in the wstern sburb of Beijing,North China[J].Acta Geologica Sinica,2015,89(2):440-460.
[14]梅冥相,张瑞,李屹尧,等.华北地台东北缘寒武系芙蓉统叠层石生物丘中的钙化蓝细菌[J].岩石学报,2017,33(4):1073-1093.MEI Mingxiang,ZHANG Rui,LI Yiyao,et al.Calcified cyanobacterias within the stromatolotic bioherm for the Cambrian Furongian Series in the northeastern margin of the North-China Platform[J].Acta Petrologica Sinica,2017,33(4):1073-1093.
[15]CHEN J,LEE J H,WOO J.Formative mechanisms,depositional processes,and geological implications of Furongian(Late Cambrian)Reefs in the North China Platform[J].Palaeogeography Palaeoclimatology Palaeoecology,2014,414(9):246-259.
[16]LEE J H,CHEN J,CHOUGH S K.Paleoenvironmental implications of an extensive maceriate microbialite bed in the Furongian Chaomidian Formation,Shandong Province,China[J].Palaeogeography Palaeoclimatology Palaeoecology,2010,297(4):621-632.
[17]韩作振,陈吉涛,张晓蕾,等.鲁西寒武系第三统张夏组附枝菌与附枝菌微生物灰岩特征研究[J].地质学报,2009,83(8):1097-1103.HAN Zuozhen,CHEN Jitao,ZHANG Xiaolei,et al.Characteristics of Epiphytonand Epiphyton microbialites in the Zhangxia Formation(Third Series of Cambrian),Shandong Province[J].Acta Geologica Sinica,2009,83(8):1097-1103.
[18]彭善池.全球寒武系四统划分框架正式确立[J].地层学杂志,2006,30(2):147-148.PENG Shanchi.The framework of the global Cambrian quaternary division was formally established[J].Journal of Stratigraphy,2006,30(2):147-148.
[19]卢衍豪,朱兆玲,钱义元,等.中国寒武纪地层对比表及说明书[M]//中国科学院南京地质古生物研究所.中国各纪地层对比表及说明书.北京:科学出版社,1982:28-54.LU Yanhao,ZHU Zhaoling,QIAN Yiyuan,et al.Stratigraphical correlation tables and their directions for the Cambrian in China[M]//Institute of Palaeontology and Geology of China Academy of Science.Stratigraphical correlation tables and their directions for Each Periods.Beijing:Science Press,1982:28-54.
[20]肖恩照,隋明园,覃英伦,等.河北涞源祁家峪剖面寒武系层序地层划分[J].大庆石油地质与开发,2017,36(6):20-29.XIAO Enzhao,SUI Mingyuan,QIN Yinglun,et al.Cambrian sequence stratigraphic division for Qijiayu Section in Hebei Laiyuan[J].Petroleum Geology and Oilfield Development in Daqing,2017,36(6):20-29.
[21]肖恩照,覃英伦,MUHAMMAD RIAZ,等.吕梁山东北缘寒武系层序地层划分:以文水苍尔会剖面为例[J].东北石油大学学报,2017,41(5):43-53.XIAO Enzhao,QIN Yinglun,MUHAMMAD RIAZ,et al.Sequence stratigraphy division of Cambrian in the northeast area of Lyuliang Mountain:a case study of the Cangerhui Section in Wenshui City[J].Journal of Northeast Petroleum University,2017,41(5):43-53.
[22]GOLDHAMMER R K,DUNN P A,HARDIE L A.Depositional cycles,composite sea-level changes,cycle stacking patterns,and the hierarchy of stratigraphic forcing:examples from Alpine Triassic platform carbonates[J].Geological Society of America Bulletin,1990,102(5):535-562.
[23]梅冥相.从正常海退与强迫型海退的辨别进行层序界面对比:层序地层学进展之一[J].古地理学报,2010,12(5):549-564.MEI Mingxiang.Correlation of sequence boundaries according to discerning between normal and forced regressions:the first advance in sequence stratigraphy[J].Journal of Palaeogeography,2010,12(5):549-564.
[24]孟祥化,乔秀夫,葛铭.华北古浅海碳酸盐风暴沉积和丁家滩相序模式[J].沉积学报,1986,4(2):1-18.MENG Xianghua,QIAO Xiufu,GE Ming.Storm deposits of the paleoepicontinental sea and the Dingjiatan Model in the Cambrian of the North China Platform[J].Acta Sedimentologia Sinica,1986,4(2):1-18.
[25]CHEN J T.Origin of the Furongian limestone breccias in the North China Platform[J].Science China Earth Sciences,2015,58(5):770-775.
[26]VAIL P,MITCHUM R,THOMPSON III S.Seismic stratigraphy and global changes of sea level:art 3.Relative changes of sea level from coastal onlap:ection 2.Application of seismic reflection configuration to stratigraphic interpretation[M].[S.l.]:Seismic Stratigraphy-Applications to Hydrocarbon Exploration,1977:63-81.
[27]CUMINGS E R.Reefs or bioherms[J].Geological Society of America Bulletin,1932,43(1):331-352.
[28]COULSON K P,BRAND L R.Lithistid sponge-microbial reef-building communities construct laminated,Upper Cambrian(Furongian)'stromatolites[J].Palaios,2016,31(7):358-370.
[29]WOODS,ADAM D.Microbial ooids and cortoids from the Lower Triassic(Spathian)virgin limestone,Nevada USA:evidence for an Early Triassic microbial bloom in shallow depositional environments[J].Global and Planetary Change,2013,105:91-101.
[30]齐永安,张喜洋,代明月,等.豫西寒武系微生物岩中的葛万菌化石及其微观结构[J].古生物学报,2017,56(2):154-167.QI Yong'an,ZHANG Xiyang,DAI Mingyue,et al.Girvanellafossils and their microstructure from Cambrian microbialites of Western Henan[J].Acta Palaeontologica Sinica,2017,56(2):154-167.
[31]RIDING R.Calcified plectonema(blue-green algae),a recent example of Girvanellafrom Aldabra Atoll[J].Palaeontology,1977,20:33-46.
[32]LEE J H,RIDING R,CHERNS L.Xinellar:a new mat-forming calcified cyanobacterium from the Middle-Late Ordovician of North China[J].Papers in Palaeontology,2016,2(3):439-449.
[33]SCHLAGINTWET F,BOVER-ARNAL T.Remarks on Bacinella Radoicic,1959(type species B.irregularis)and its representatives[J].Facies,2010,56(4):635-673.
[34]LUO C,REITNER J.'Stromatolites'built by sponges and microbes-a new type of Phanerozoic bioconstruction[J].Lethaia,2016,49(4):555-570.
[35]WANG L,SHI X,JIANG G.Pyrite morphology and redox fluctuations recorded in the Ediacaran Doushantuo Formation[J].Palaeogeography Palaeoclimatology Palaeoecology,2012,333(2):218-227.
[36]VISSCHER P T,REID R P.Microscale observations of sulfate reduction:correlation of microbial activity with lithified[J].Geology,2000,28(10):919-922.
[37]朱士兴,黄学光.13亿年前叠层石的生长节律和地—日—月动力学(英文)[J].微体古生物学报,2003(1):23-30.ZHU Shixing,HUANG Xueguang.The earth-sun-moon dynamics from growth rhythms of 1 300Ma stromatolites[J].Acta Micropalaeontologica Sinica,2003(1):23-30.
[38]梅冥相,孟庆芬.现代叠层石的多样化构成:认识古代叠层石形成的关键和窗口[J].古地理学报,2016,18(2):127-146.MEI Mingxiang,MENG Qingfen.Composition diversity of modern stromatolites:a key and window for further understanding of the formation of ancient stromatolites[J].Journal of Palaeogeography,2016,18(2):127-146.
[39]王皓,肖恩照.山西灵丘刁泉剖面寒武系第三统张夏组核形石[J].东北石油大学学报,2018,42(5):44-53.WANG Hao,XIAO Enzhao.Oncolites in Cambrian Series 3at Diaoquan Section in Lingqiu,Shanxi[J].Journal of Northeast Petroleum University,2018,42(5):44-53.
[40]梅冥相,RIAZ M,刘丽,等.辽东半岛复州湾剖面寒武系第二统光合作用生物膜建造的核形石[J].古地理学报,2019,21(1):31-48.MEI Mingxiang,RIAZ M,LIU Li,et al.Oncoids built by photosynthetic biofilms:an example from the Series 2of Cambrian at Fuzhouwan Section in Liaodong Peninsula[J].Journal of Palaeogeography,2019,21(1):31-48.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |