Discovery of the Norian conodont Mockina slovakensis in Hongyan section of Baoshan area,Yunnan Province and its indication to sedimentary environment
GUO Bao1, DU Yixing1,2, SHI Zhiqiang1,2, JIN Xin1,2
1 Institute of Sedimentary Geology,Chengdu University of Technology,Chengdu 610059,China; 2 State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,Chengdu University of Technology,Chengdu 610059,China
AbstractMockina slovakensis is one of the important species of conodont in Norian period. It plays a significant role in stratigraphy and acts as an indication for certain distinctive sedimentary environments. In this study,a significant abundance of conodont species M. slovakensis was discovered in the limestone deposits located in the lower parts of the Dashuitang Formation in the Hongyan section of Baoshan,Yunnan. Based on the conodont biostratigraphy,the age of the sedimentary strata in this section has been constrained to the late Alaunian of Norian period. Its presence and abundance can provide valuable insights into the paleoenvironmental conditions and depositional settings. M. slovakensis is known for strong adaptability to a diverse living environments,including both shallow and deep oceanic environment,as well as restricted sea to open sea. However,various records indicate that M. slovakensis conodont indicates the restricted depositional environment. Considering the abundance of dominant M. slovakensis found in the Hongyan section of Baoshan,combined with previous studies on the sedimentary environment of the Dashuitang Formation in the Baoshan block,it is reasonable to conclude that the Baoshan area formed a restricted sedimentary basin during the Alaunian stage under a tectonic stretching setting. The results are helpful for understanding the evolution of the sedimentary environment during the Late Triassic period in eastern Tethys.
Fund:Co-funded by the National Nature Science Foundation of China(No.42302131),the Innovative Talent Development Fund of Institute of Sedimentary Geology,Chengdu University of Technology,and the Open Fund of State Key Laboratory of Marine Geology,Tongji University(No. MG201903)
Corresponding Authors:
DU Yixing,born in 1991,is an associate researcher in Institute of Sedimentary Geology,Chengdu University of Technology. He is engaged in research on paleontology and sedimentology. E-mail: yixing.du@outlook.com.
About author: GUO Bao,born in 1999,is a master degree student in Institute of Sedimentary Geology,Chengdu University of Technology. He is engaged in research on paleontology and sedimentology. E-mail: 1539597169@qq.com.
Cite this article:
GUO Bao,DU Yixing,SHI Zhiqiang et al. Discovery of the Norian conodont Mockina slovakensis in Hongyan section of Baoshan area,Yunnan Province and its indication to sedimentary environment[J]. JOPC, 2024, 26(2): 373-386.
GUO Bao,DU Yixing,SHI Zhiqiang et al. Discovery of the Norian conodont Mockina slovakensis in Hongyan section of Baoshan area,Yunnan Province and its indication to sedimentary environment[J]. JOPC, 2024, 26(2): 373-386.
[1] 包佳凤,赵云江,王承平,王伟,杨仕潘,张坤,马进华. 2012. 滇西保山金鸡地区三叠系上统大水塘组震积岩的发现及意义. 沉积学报, 30(3): 490-500. [Bao J F,Zhao Y J,Wang C P,Wang W,Yang S P,Zhang K,Ma J H.2012. The discovery and significance on the seismites of Dashuitang Formation in the Upper Triassic Series in Baoshan Jinji area of western Yunnan. Acta Sedimentologica Sinica, 30(3): 490-500] [2] 包佳凤,赵云江,宋冬虎,孙载波,莫雄,张坤. 2020. 滇西保山地块三叠纪裂谷盆地的演化. 地球科学前沿, 10(4): 261-277. [Bao J F,Zhao Y J,Song D H,Sun Z B,Mo X,Zhang K.2020. The evolution of the Triassic rift basin in the Baoshan Block of western Yunnan. Advances in Geosciences, 10(4): 261-277] [3] 董美玲,董国臣,莫宣学,朱弟成,聂飞,谢许峰,王霞,胡兆初. 2012. 滇西保山地块早古生代花岗岩类的年代学、地球化学及意义. 岩石学报, 28(5): 1453-1464. [Dong M L,Dong G C,Mo X X,Zhu D C,Nie F,Xie X F,Wang X,Hu Z C.2012. Geochronology and geochemistry of the Early Palaeozoic granitoids in Baoshan block,western Yunnan and their implications. Acta Petrologica Sinica, 28(5): 1453-1464] [4] 董致中,王伟. 2006. 云南牙形类动物群: 相关生物地层及生物地理区研究. 昆明: 云南科技出版社,128-146. [Dong Z Z,Wang W.2006. The Cambrian-Triassic Conodont Faunas in Yunnan,China-Correlative Biostratigraphy and the Study of Palaeobiogeographic Province of Conodont. Kunming: Yunnan Science and Technology Press,128-146] [5] 郝子文,饶荣标. 1999. 西南区区域地层. 武汉: 中国地质大学出版社,1-220. [Hao Z W,Rao R B.1999. Regional stratigraphy of southwest China. Wuhan: China University of Geosciences Press,1-220] [6] 胡友恒. 1990. 云南晚三叠世岩相古地理及煤层赋存规律. 煤田地质与勘探, 18(2): 2-11,71-72. [Hu Y H.1990. The occurrence patterns of petrographic facies and palaeogeography and of Late Triassic seams in Yunnan Province. Coal Geology & Exploration, 18(2): 2-11,71-72] [7] 廖世勇,尹福光,孙志明,王冬兵,唐渊,孙洁. 2013. 滇西保山地块东缘晚三叠世何珠次英安斑岩的发现及其地质意义. 地质通报, 32(7): 1006-1013. [Liao S Y,Yin F G,Sun Z M,Wang D B,Tang Y,Sun J.2013. The discovery of Late Triassic subvolcanic dacite porphyry in the eastern margin of the Baoshan terrane,western Yunnan Province and its geodynamic implications. Geological Bulletin of China, 32(7): 1006-1013] [8] 马杏垣. 1982. 论伸展构造. 地球科学, (3): 15-20. [Ma X Y.1982. On extensional tectonics. Earth Science, (3): 15-20] [9] 彭成龙,黄文俊,袁宏. 2014. 滇西姚关上三叠统大水塘组钙屑浊积岩沉积特征及控制因素探讨. 贵州地质, 31(3): 201-205. [Peng C L,Huang W J,Yuan H.2014. Discussion of sedimentary characteristics and controlling factors of calcarenitic turbidite,Dashuitang Formation,Upper Triassic in Yaoguan of western Yunnan. Guizhou Geology, 31(3): 201-205] [10] 王小端,杜怡星,时志强,陈彬. 2019. 云南保山上三叠统诺利阶南梳坝组和大水塘组的牙形石及沉积环境特征. 古生物学报, 58(1): 79-91. [Wang X D,Du Y X,Shi Z Q,Chen B.2019. Characteristics of conodonts and sedimentary environment of Upper Norian Nashuba and Dashuitang Formations in Baoshan,Yunnan Province. Acta Palaeontologica Sinica, 58(1): 79-91] [11] 王义昭,李兴林,段丽兰. 2000. 三江地区南段大地构造与成矿. 北京: 地质出版社,1-123. [Wang Y Z,Li X L,Duan L L.2000. Tectonic and Mineralization of the Southern Section of the Sanjiang Area. Beijing: Geological Publishing House,1-123] [12] 王志浩,董致中. 1985. 云南西南部保山地区晚三叠世 Epigondolella 动物群的发现. 微体古生物学报, 2(2): 125-131. [Wang Z H,Dong Z Z.1985. Discovery of conodont Epigondolella fauna from Late Triassic in Baoshan area,western Yunnan. Acta Micropalaeontologica Sinica, 2(2): 125-131] [13] 吴强旺,金鑫,时志强,周小梅,葛禹. 2020. 云南保山红岩剖面晚三叠世诺利期碳酸盐岩特征及沉积相分析. 矿物岩石, 40(4): 105-115. [Wu Q W,Jin X,Shi Z Q,Zhou X M,Ge Y.2020. Characteristics and sedimentary facies analysis of late Triassic norian carbonate in Hongyan section of Baoshan,Yunnan Province. Mineralogy and Petrology, 40(4): 105-115] [14] 吴强旺,杜怡星,金鑫,时志强. 2022. 滇西巍山地区上三叠统诺利阶三合洞组牙形石年代及沉积相分析. 古生物学报, 61(1): 51-64. [Wu Q W,Du Y X,Jin X,Shi Z Q.2022. Conodont biostratigraphy and sedimentary facies of the Sanhedong Formation(Norian,Upper Triassic)in Weishan,western Yunnan Province. Acta Palaeontologica Sinica, 61(1): 51-64] [15] 燕守勋,王桂梁,邵震杰,孟宪刚. 1996. 鲁西地壳隆升的伸展构造模式. 地质学报, 70(1): 1-9. [Yan S X,Wang G L,Shao Z J,Meng X G.1996. Extensional tectonic model of crustal elevation in western Shandong. Acta Geologica Sinica, 70(1): 1-9] [16] 杨志华. 2016. 滇西保山地区上泥盆统牙形石及其生物地层研究. 中国地质大学(北京)硕士学位论文. [Yang Z H.2016. A study on the Late Devonian conodont and its biostratigraphy of Late Devonian in Baoshan,West Yunnan. Masteral dissertation of China University of Geosciences(Beijing)] [17] 云南省地质矿产局. 1990. 云南省区域地质志. 北京: 地质出版社,1-194. [Yunnan Provincial Bureau of Geology and Mineral Resources. 1990. Regional Geology of Yunnan Province. Beijing: Geological Publishing House,1-194] [18] 张再天. 2016. 滇黔地区拉丁期—卡尼期牙形石生物地层格架及沉积环境演变. 中国地质大学博士学位论文. [Zhang Zai-tian,2016. The Ladinian-Carnian conodont biostratigraphic framework and sedimentary environmental evolution in Yunnan and Guizhou Provinces,South China. Doctoral dissertation of China University of Geosciences] [19] 张远志,张定辉,刘世荣. 1996. 云南省岩石地层. 武汉: 中国地质大学出版社,1-367. [Zhang Y Z,Zhang D H,Liu S R.1996. Rock Formations in Yunnan Province. Wuhan: China University of Geosciences Press,1-367] [20] 曾卫平. 2022. 滇西保山地区晚三叠世诺利晚期牙形石动物群研究. 中国地质大学博士学位论文. [Zeng W P.2022. Late Norian(Late Triassic)Conodont fauna of the Baoshan,western Yunnan. Doctoral dissertation of China University of Geosciences] [21] 赵云江,郑春,黄亮,包佳凤,李冰,王晓林,刘晓燕. 2012. 灾变事件地层斜坡滑塌(带)堆积的特征: 以滇西保山地区上三叠统南梳坝组为例. 地质通报, 31(5): 745-757. [Zhao Y J,Zheng C,Huang L,Bao J F,Li B,Wang X L,Liu X Y.2012. Catastrophic event characteristics of stratigraphic slope slumping accumulation: a case study of the Upper Triassic Nanshuba Formation in Baoshan area,western Yunnan Province. Geological Bulletin of China, 31(5): 745-757] [22] Balini M,Bertinelli A,Di Stefano P,Guaiumi C,Levera M,Mazza M,Muttoni G,Nicora A,Preto N,Rigo M.2010. The late Carnian-Rhaetian succession at Pizzo Mondello(Sicani Mountains). Albertiana, 39: 36-57. [23] Belvedere M,Avanzini M,Mietto P,Rigo M.2008. Norian Dinosaur Footprints from the “Strada delle Gallerie”(Monte Pasubio,NE Italy). Studi Trentini Di Scienza Naturali,Acta Geologica, 83: 267-276. [24] Channell J E T,Kozur H W,Sievers T,Mock R,Aubrecht R,Sykora M.2003. Carnian-Norian biomagnetostratigraphy at Silická Brezová(Slovakia): correlation to other Tethyan sections and to the Newark Basin. Palaeogeography,Palaeoclimatology,Palaeoecology, 191(2): 65-109. [25] Du Y X,Bertinelli A,Jin X,Shi Z Q,Karádi V,Yin H J,Han L,Wu Q W,Rigo M.2020a. Integrated conodont and radiolarian biostratigraphy of the upper Norian in Baoshan Block,southwestern China. Lethaia, 53(4): 533-545. [26] Du Y X,Chiari M,Karádi V,Nicora A,Onoue T,Pálfy J,Roghi G,Tomimatsu Y,Rigo M.2020b. The asynchronous disappearance of conodonts: New constraints from Triassic-Jurassic boundary sections in the Tethys and Panthalassa. Earth-Science Reviews, 203: 103176. [27] Du Y X,Karádi V,Roghi G,Ponton M,Cozzi A,Rigo M.2021. Revision of the conodont Mockina slovakensis and its paleogeographic implications for the Upper Triassic intraplatform basins of the Alps. Journal of Earth Science, 32(3): 657-666. [28] Du Y X,Onoue T,Tomimatsu Y,Wu Q W,Rigo M.2023. Lower Jurassic conodonts from the Inuyama area of Japan: implications for conodont extinction. Frontiers in Ecology and Evolution, 11: 1135789. [29] Huang B C,Yan Y G,Piper J D,Zhang D H,Yi Z Y,Yu S,Zhou T H.2018. Paleomagnetic constraints on the paleogeography of the East Asian blocks during Late Paleozoic and Early Mesozoic times. Earth-Science Reviews, 186: 8-36. [30] Jin X,Du Y X,Bertinelli A,Shi Z Q,Preto N,Zou H,Ogg J G,Han L,Wu Q W,Rigo M.2022. Carbon-isotope excursions in the Norian stage(Upper Triassic)of the Baoshan terrane,western Yunnan,China. Journal of Asian Earth Sciences, 230(4): 105215 [31] Kaya O,Helvaci H,Kozur H,Sadeddin W.2001. Late Norian conodont age for a metacarbonate unit in NW Anatolia,Turkey. Geobios, 34(5): 527-532. [32] Kovács S,Nagy G.1989. Contribution to the age of the Avicula-and Halobia-limestones(Feketehegy Limestone Formation)in Pilis Mts(NE Transdanubian Central Range,Hungary). Annual Report of the Hungarian Geological Institute, 1987: 95-129 [33] Li D P,Chen Y L,Hou K J,Lu Z,Cui D.2015. Detrital zircon record of Paleozoic and Mesozoic meta-sedimentary strata in the eastern part of the Baoshan block: implications of their provenance and the tectonic evolution of the southeastern margin of the Tibetan Plateau. Lithos, 227: 194-204. [34] Li P W,Rui G,Junwen C,Ye G.2004. Paleomagnetic analysis of eastern Tibet: implications for the collisional and amalgamation history of the Three Rivers Region,SW China. Journal of Asian Earth Sciences, 24(3): 291-310. [35] Martini R,Zaninetti L,Villeneuve M,Cornée J J,Krystyn L,Cirilli S,De Wever P,Dumitrica P,Harsolumakso A.2000. Triassic pelagic deposits of Timor: palaeogeographic and sea-level implications. Palaeogeography,Palaeoclimatology,Palaeoecology, 160(1-2): 123-151. [36] Mastandrea A,Ietto F,Neri C,Russo F.1997. Conodont biostratigraphy of the Late Triassic sequence of Monte Cocuzzo(Catena Costiera,Calabria,Italy). Rivista Italiana di Paleontologia e Stratigrafia, 103(2): 173-182. [37] Mazza M,Rigo M,Gullo M.2012. Taxonomy and biostratigraphic record of the Upper Triassic conodonts of the Pizzo Mondello section(western Sicily,Italy),GSSP candidate for the base of the Norian. Rivista Italian di Paleontologia e Stratigrafia, 118: 85-130. [38] Meço S.1999. Conodont biostratigraphy of Triassic Pelagic Strata,Albania. Rivista Italiana di Paleontologia e Stratigrafia, 105(2): 251-266. [39] Metcalfe I.2009. Late Palaeozoic and Mesozoic tectonic and palaeogeographical evolution of SE Asia. Geological Society,London,Special Publications, 315(1): 7-23. [40] Moix P,Kozur H W,Stampfli G M,Mostler H.2007. New paleontological,biostratigraphical and paleogeographic results from the Triassic of the Mersin Mélange,SE Turkey. In: Lucas S G,Spielmann J A(eds). The Global Triassic. Vol. 41. Albuquerque: New Mexico Museum of Natural History and Science Bulletin,282-311. [41] Pálfy J,Demény A,Haas J,Carter E S,Görög Á,Halász D,Oravecz-Scheffer A,Hetényi M,Márton E,Orchard M J,Ozsvárt P,Vetö I,Zajzon N.2007. Triassic-Jurassic boundary events inferred from integrated stratigraphy of the Csövár section,Hungary. Palaeogeography,Palaeoclimatology,Palaeoecology, 244: 11-33. [42] Rigo M,Preto N,Franceschi M,Guaiumi C.2012. Stratigraphy of the Carnian-Norian Calcari con Selce Formation in the Lagonegro Basin,southern Apennines. Rivista Italiana di Paleontologia e Stratigrafia, 118(1): 143-154. [43] Rigo M,Bertinelli A,Concheri G,Gattolin G,Godfrey L,Katz M E,Maron M,Mietto P,Muttoni G,Sprovieri M,Stellin F,Zaffani M.2016. The Pignola-Abriola section(southern Apennines,Italy): a new GSSP candidate for the base of the Rhaetian Stage. Lethaia, 49(3): 287-306. [44] Rigo M,Mazza M,Karádi V,Nicora A.2018. New Upper Triassic conodont biozonation on the Tethyan realm. In: Tanner L H(ed). The Late Triassic World: Earth in a Time of Transition. Topics in Geobiology, 46: 189-235. [45] Roghi G,Mietto P,Vecchia D.1995. Contribution to the conodont biostratigraphy of the Dolomia di Forni(Upper Triassic,Carnia,NE Italy). Memoire di Scienze Geologiche, 47: 125-133 [46] Sone M,Metcalfe I.2008. Parallel Tethyan sutures in mainland Southeast Asia: new insights for Palaeo-Tethys closure and implications for the Indosinian orogeny. Comptes Rendus Geoscience, 340(2-3): 166-179. [47] Trotter J A,Williams I S,Nicora A,Mazza M,Rigo M.2015. Long-term cycles of Triassic climate change: a new δ18O record from conodont apatite. Earth and Planetary Science Letters, 415: 165-174. [48] Wang X D,Ueno K,Mizuno Y,Sugiyama T.2001. Late Paleozoic faunal,climatic,and geographic changes in the Baoshan block as a Gondwana-derived continental fragment in southwest China. Palaeogeography,Palaeoclimatology,Palaeoecology, 170: 197-218. [49] Yamashita D,Kato H,Onoue T,Suzuki N.2018. Integrated Upper Triassic conodont and radiolarian biostratigraphies of the Panthalassa Ocean. Paleontological Research, 22(2): 167-198. [50] Zeng W P,Purnell M A,Jiang H S,Zhang M H.2021. Late Triassic(Norian)conodont apparatuses revealed by conodont clusters from Yunnan Province,southwestern China. Journal of Earth Science, 32(3): 709-724. [51] Zeng W P,Jiang H S,Chen Y,Ogg J,Zhang M H,Dong H X S.2023. Upper Norian conodonts from the Baoshan block,western Yunnan,southwestern China,and implications for conodont turnover. Peer J, 11: e14517. [52] Budai T,Kovács S.1986. A Rezi Dolomite rétegtani helyzete a Keszthelyihegységben. MáFI éviJelentés, 1984: 175-191. [53] Donofrio D A,Brandner R,Poleschinski W.2003. Conodonten der Seefeld-Formation: Ein beitrag zur bio-und lithostratigraphie der Hauptdolomit-Plattform(Obertrias,Westliche Nördliche Kalkalpen,Tirol). Geologisch-Paläontologische Mitteilungen Innsbruck, 26: 91-107. [54] Kozur H.1972. Die conodontengattung metapolygnathus hayashi 1968 und ihr stratigraphischer Wart. Geologisch-Paläontologische Mitteilungen Innsbruck, 2: 1-37.