Frasnian-Famennian Event and its response to the sedimentation in Quanzhou of Guangxi Province

HOU Yafei; SONG Bowen; GUO Jungang; KOU Xiaohu; YIN Jiayi; AI Chengzhi; WANG Jiaxuan

2021 Vol. 40, No. 4

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HOU Yafei, SONG Bowen, GUO Jungang, KOU Xiaohu, YIN Jiayi, AI Chengzhi, WANG Jiaxuan. Frasnian-Famennian Event and its response to the sedimentation in Quanzhou of Guangxi Province[J]. Geological Bulletin of China, 2021, 40(4): 499-511.

Citation:

HOU Yafei, SONG Bowen, GUO Jungang, KOU Xiaohu, YIN Jiayi, AI Chengzhi, WANG Jiaxuan. Frasnian-Famennian Event and its response to the sedimentation in Quanzhou of Guangxi Province[J]. Geological Bulletin of China, 2021, 40(4): 499-511.

Frasnian-Famennian Event and its response to the sedimentation in Quanzhou of Guangxi Province

1.
Institute of Geological Survey, China University of Geosciences(Wuhan), Wuhan 430074, Hubei, China
2.
Zhengzhou Institute of Multipurpose Utilization of Mineral Resources, GAGS, Zhengzhou 450006, Henan, China
3.
School of Earth Science, China University of Geosciences(Wuhan), Wuhan 430074, Hubei, China

More Information

Corresponding author: SONG Bowen, bwsong1985@cug.edu.cn

Received Date: 22 October 2019

Revised Date: 04 April 2020

Publish Date: 15 April 2021

Abstract

Abstract

At the turn of Frasnian-Famennian(F-F)in Late Devonian, the environment of earth changed rapidly. As the most developed Devonian sedimentary area in South China, Guangxi has a good record of this event. Based on the study of lithic facies, sedimentary microfacies, and fossils from a series of marine carbonate rocks, siltstone and argillaceous rocks in the Dongshan section, the boundary of F-F was confirmed, and sedimentary records related to the F-F events in this area were revealed to discuss the sea level changes at the turn of F-F. It is suggest that the boundary of F-F can be restricted to the boundary between the 49 layer and 50 layer of the section. It is assumed that two adjacent stepped sea-level rise and fall occurred at the turn of F-F, which is similar to other areas in the world.
- F-F event /
- lithic facies /
- sedimentary microfacies /
- fossils /
- stepped sea-level change

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References

[1]	Buggisch W. The Global Frasnian-Famennian Kellwasser Event[J]. Geologische Rundachau, 1991, 80(1): 49-72. doi: 10.1007/BF01828767 CrossRef Google Scholar
[2]	廖卫华. 华南晚泥盆世弗拉斯期-法门期之交的生物大灭绝及其后的残存和复苏[M]. 合肥: 中国科学技术大学出版社, 2004: 437-456. Google Scholar
[3]	Racki G. Toward understanding Late Devonian global events: few answer, many questions[C]//Over D J, Morrow J R, Wignall P B. Understanding Late Deconian and Permian-Triassic Biotic and Climatic Events: Towards an Integrated Approach. Amsterdam: Elsevier, 2005, 20(5): 5-36. Google Scholar
[4]	Raup V M, Sepkoski J J. Mass Extinctions in the Fossil Record[J]. Science, 1982, 219(4589): 1239-1240. Google Scholar
[5]	季强. 从牙形类研究论华南弗拉阶-法门阶生物灭绝事件[M]. 北京: 地质出版社, 1994: 79-107. Google Scholar
[6]	冯日照, 韦龙明, 何鸿. 桂林地区晚泥盆世沉积相演化特征和海平面变化对F-F生物灭绝事件的影响[C]//华南青年地学学术研讨会论文集, 2006: 35-38. Google Scholar
[7]	殷保安. 广西壮族自治区岩石地层[M]. 武汉: 中国地质大学出版社, 1997: 14-18. Google Scholar
[8]	Chen D Z, Tucker M E. The Frasnian-Famennian mass extinction: insights from high-resolution sequence stratigraphy and cyclostratigraphy in South China[J]. Palaeogeography Palaeoclimatology Palaeoecology, 2003, 193(1): 87-111. doi: 10.1016/S0031-0182(02)00716-2 CrossRef Google Scholar
[9]	杜远生, 龚一鸣, 张哲, 等. 南华海泥盆纪烃源岩的古氧相和缺氧环境模式——以广西中、上泥盆统为例[J]. 古地理学报, 2009, 11(1): 28-36. Google Scholar
[10]	徐冉, 龚一鸣, 谭雪娇, 等. 广西桂林杨堤晚泥盆世弗拉期-法门期之交上、下Kellwasser事件的差异与海洋生产力变化[J]. 地球科学-中国地质大学学报, 2015, 40(2): 357-371. Google Scholar
[11]	Huang C, Song J J, Shen J, et al. The influence of the Late Devonian Kellwasser events on deep-water ecosystems: Evidence from palaeontological and geochemical records from South China[J]. Palaeogeography Palaeoclimatology Palaeoecology, 2018, 504: 60-74. doi: 10.1016/j.palaeo.2018.05.006 CrossRef Google Scholar
[12]	尹家一, 寇晓虎, 郭俊刚, 等. 广西全州地区中——上泥盆统生物地层研究[J]. 地质通报, 2019, 38(6): 930-949. Google Scholar
[13]	Copper P. Reef development at the Frasnian/Famennian mass extinction boundary[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2002, 181(1/3): 27-65. Google Scholar
[14]	龚一鸣, 李保华, 吴诒. 广西弗拉期阶-法门期阶之交碳同位素与分子地层对比研究[J]. 地学前缘, 2002, 93: 151-160. doi: 10.3321/j.issn:1005-2321.2002.03.019 CrossRef Google Scholar
[15]	沈树忠, 张华. 什么引起五次生物大灭绝[J]. 科学通报, 2017, 62(11): 1119-1135. Google Scholar
[16]	Carmichael S K, Waters J A, Königsof P, et al. Paleogeography and paleoenvironments of the Late Devonian Kellwasser event: A review of its sedimentological and geochemical expression[J]. Global and Planetary Change, 2019, 183: 102984. doi: 10.1016/j.gloplacha.2019.102984 CrossRef Google Scholar
[17]	黄家园, 梁昆, 王玉珏, 等. 全球泥盆纪生物礁演化及其影响因素[J]. 地层学杂志, 2019, 43(2): 198-209. Google Scholar
[18]	Qie W, Ma X, Xu H, et al. Devonian integrative stratigraphy and timescale of China[J]. Science China: Earth Sciences, 2019, 62(1): 112-134. doi: 10.1007/s11430-017-9259-9 CrossRef Google Scholar
[19]	Song J, Huang C, Gong Y. Response of Ostracods(Crustacea)to the Devonian F-F event: Evidence from the Yangdi and Nandong sections in Guangxi, South China[J]. Global and Planetary Change, 2019, 173: 109-120. doi: 10.1016/j.gloplacha.2018.12.015 CrossRef Google Scholar
[20]	Xian H, Zhang S, Li H, et al. How did South China connect to and separate from Gondwana? New paleomagnetic constraints from the Middle Devonian red beds in South China[J]. Geophysical Research Letters, 2019, 46: 7371-7378. doi: 10.1029/2019GL083123 CrossRef Google Scholar
[21]	Racki G, Wignall P B. Devonian global changes-Recent advances and challenges in different domains[J]. Global and Planetary Change, 2020, 191: 103200. doi: 10.1016/j.gloplacha.2020.103200 CrossRef Google Scholar
[22]	王玉珏, 梁昆, 陈波, 等. 晚泥盆世F-F大灭绝事件研究进展[J]. 地层学杂志, 2020, 44(3): 277-298. Google Scholar
[23]	赵金科. 广西地质[M]. 北京: 科学出版社, 1958. Google Scholar
[24]	钟铿. 广西的泥盆纪地层[J]. 广西科学, 1994, 1(2): 21-23. Google Scholar
[25]	Hou H F, Ji Q, Wang J X. Preliminary report on Frasnian-Famennian events in South China[C]//McMillan N J, Embry A F, Glass D J. Devonian of the World. Canadian Society of Petroleum Geologists Member, 1988, 14(3): 63-69 Google Scholar
[26]	Ji Q. On the Frasnian-Famennian mass extinction events in south China[J]. Courier Forschungsinstitut Senckenberg, 1989, 117: 275-301. Google Scholar
[27]	Chen D Z, Tucker M E, Jiang M S, et al. Long-distance correlation between tectonic controlled, isolated carbonate platforms by cyclostratigraphy and sequence stratigraphy in the Devonian of South China[J]. Sedimentology, 2001, 48(1): 57-78. doi: 10.1046/j.1365-3091.2001.00351.x CrossRef Google Scholar
[28]	Chen D Z, Tucker M E, Jiang M S, et al. Carbonate sedimentation in a starved pull-apart basin, Middle to late Devonian southern Guilin, South China[J]. Basin Research, 2001, 13(2): 141-167. doi: 10.1046/j.1365-2117.2001.00148.x CrossRef Google Scholar
[29]	马学平, 宗普. 湖南中-晚泥盆世腕足动物组合、海平面升降及古地理演变[J]. 地球科学, 2010, 40(9): 1204-1218. Google Scholar
[30]	陈志明, 杨培基, 潘正莆, 等. 湘、桂中晚泥盆世台槽相沉积特征[J]. 沉积学报, 1983, 1(3): 88-98. Google Scholar
[31]	McGhee G R J. The Late Devonian Mass Extinction[M]. Columbia University Press, New York, 1996: 1-303. Google Scholar
[32]	边春鹏. 滇西保山西邑地区泥盆系沉积特征及沉积古地理研究[D]. 北京: 中国地质大学(北京)硕士学位论文, 2016. Google Scholar
[33]	包洪平, 杨承运. 碳酸盐岩微相分析及其在岩相古地理研究中的意义[J]. 岩相古地理, 1999, 19(6): 59-64. doi: 10.3969/j.issn.1009-3850.1999.06.010 CrossRef Google Scholar
[34]	江大勇, 丁干, 白顺良. 广西六景泥盆纪吉维阶-弗拉斯阶界线层牙形石生物地层[J]. 地层学杂志, 2000, 24(03): 195-200. doi: 10.3969/j.issn.0253-4959.2000.03.005 CrossRef Google Scholar
[35]	王成源, 王志浩. 中国牙形刺生物地层[M]. 杭州: 浙江大学出版社, 2016: 18-22. Google Scholar
[36]	韩迎建. 广西象州中坪马鞍山剖面上泥盆统弗拉阶/法门阶(F/F)界线的研究[J]. 地球学报, 1987, (3): 174-200. Google Scholar
[37]	沈建伟. 广西桂林泥盆纪牙形刺组合序列与海平面变化[J]. 微体古生物学报, 1995, 12(3): 251-273. Google Scholar
[38]	王超勇, 夏文臣. 掌鳞刺属演化及晚泥盆世环境变迁[J]. 广西地质, 2002, 15(2): 21-25. Google Scholar
[39]	张哲, 杜远生, 舒雪松, 等. 鄂东南地区早三叠世风暴沉积序列及其环境意义[J]. 地质科技情报, 2006, 25(2): 29-34. doi: 10.3969/j.issn.1000-7849.2006.02.005 CrossRef Google Scholar
[40]	曾雄伟, 杜远生, 张哲, 等. 广西桂林地区中、上泥盆统风暴岩沉积特征及其地质意义[J]. 地质科技情报, 2007, 26(6): 42-46, 65. doi: 10.3969/j.issn.1000-7849.2007.06.007 CrossRef Google Scholar
[41]	李世毅, 姜迪, 赵莹莹. 安徽巢湖地区石炭纪-早二叠世碳酸盐岩微相与沉积环境[J]. 沉积与特提斯地质, 2015, 35(1): 3-15. doi: 10.3969/j.issn.1009-3850.2015.01.002 CrossRef Google Scholar
[42]	马永生, 刘波, 郭荣涛, 等. 碳酸盐岩微相: 分析、解释及应用[M]. 北京: 地质出版社, 2016. Google Scholar
[43]	周明, 罗平, 董琳, 等. 塔里木盆地柯坪地区奥陶系鹰山组台内滩沉积特征[J]. 沉积学报, 2016, 34(5): 951-962. Google Scholar
[44]	马学平. 湖南中部泥盆纪弗拉-法门阶界线附近的沉积环境[C]//中国古生物学会学术年会, 2001: 24-26. Google Scholar
[45]	李华, 马学平, 韦龙明. 广西菜子岩剖面中上泥盆统界线附近沉积相与海平面变化[J]. 古地理学报, 2009, 11(5): 504-512. Google Scholar
[46]	郭峰. 碳酸盐岩沉积学[M]. 北京: 石油工业出版社, 2011: 121-176. Google Scholar
[47]	桑隆康, 马昌前, 王国庆, 等. 岩石学[M]. 北京: 地质出版社, 2012: 363-384. Google Scholar
[48]	童金南, 殷鸿福. 古生物学[M]. 北京: 高等教育出版社, 2007. Google Scholar
[49]	黄臣军, 刘格云, 刘红光, 等. 标准微相类型在碳酸盐岩微相及沉积环境研究中的应用——以塔西南玉北地区奥陶系为例[J]. 沉积学报, 2017, 35(6): 1166-1176. Google Scholar
[50]	龙建喜, 陈建书, 彭成龙, 等. 贵州水城地区早二叠世包磨山组碳酸盐岩微相特征及沉积环境[J]. 中国岩溶, 2017, 36(3): 313-318. Google Scholar
[51]	张钰莹, 江大勇, 何治亮, 等. 安徽巢湖下三叠统南陵湖组中上段微相及古环境初探[J]. 地层学杂志, 2016, 40(3): 290-296. Google Scholar
[52]	韩毅龙, 姚倩倩. 碳酸盐岩微相与沉积环境浅析[J]. 石化技术, 2016, 23(1): 55-55. doi: 10.3969/j.issn.1006-0235.2016.01.038 CrossRef Google Scholar
[53]	马知恒, 喻美艺, 晏波, 等. 贵州兴义乌沙地区法郎组瓦窑段沉积特征初探[J]. 贵州地质, 2018, 35(1): 37-43. doi: 10.3969/j.issn.1000-5943.2018.01.007 CrossRef Google Scholar
[54]	高计元. 中国南方泥盆系结核泥晶灰岩的成因[J]. 沉积学报, 1988, 6(2): 77-86. Google Scholar
[55]	金若谷. 一种深水沉积标志——"结核泥晶结核"及其成因[J]. 沉积学报, 1989, 7(2): 51-61. Google Scholar
[56]	韩树棻. 安徽沿长江地区下三叠统结核泥晶灰岩成因研究[J]. 地质科学, 1983, (3): 232-238. Google Scholar
[57]	蓝光志, 张廷山, 高卫东. 川西北地区早志留世结核泥晶灰岩的类型、成因及意义[J]. 西南石油学院学报, 1994, 16(3): 1-6. Google Scholar
[58]	董兆雄, 朱晓惠, 侯方浩, 等. 一种特殊结核泥晶灰岩的成因研究[J]. 沉积学报, 2002, 20(1): 20-24. doi: 10.3969/j.issn.1000-0550.2002.01.004 CrossRef Google Scholar
[59]	刘荞菲. 结核泥晶灰岩的分类及成因研究[J]. 四川有色金属, 2015, (2): 26-28, 39. doi: 10.3969/j.issn.1006-4079.2015.02.007 CrossRef Google Scholar
[60]	邝国敦. 广西六景泥盆纪地层、古生物与沉积相[J]. 广西地质, 1984, (创刊号): 46-57. Google Scholar
[61]	龚一鸣, 李保华. 泥盆系弗拉阶-法门阶之交事件沉积和海平面变化[J]. 地球科学-中国地质大学学报, 2001, 26(3): 251-257. doi: 10.3321/j.issn:1000-2383.2001.03.006 CrossRef Google Scholar
[62]	陈建强, 周洪瑞, 王训练. 沉积学及古地理学教程[M]. 北京: 地质出版社, 2004: 144-193. Google Scholar
[63]	冯增昭. 中国沉积学[M]. 北京: 石油工业出版社, 2013: 1118-1227. Google Scholar
[64]	白顺良, 金善燏, 宁宗善, 等. 广西泥盆纪牙形石、竹节石分带及对比[J]. 北京大学学报(自然科学版), 1979, (1): 101-120, 132-133. Google Scholar
[65]	龚一鸣, 吴诒, 杜远生, 等. 华南泥盆纪海平面变化节律及圈层耦合关系[J]. 地质学报, 1997, 71(3): 212-226. Google Scholar
[66]	鲜思远, 陈继荣, 万正权. 四川龙门山甘溪泥盆纪生态地层、层序地层与海平面变化[J]. 沉积与特提斯地质, 1995, 15(6): 2-47. Google Scholar
[67]	龚一鸣, 吴诒, 杜远生. 黔桂泥盆纪层序地层及海平面变化的频幅、速度和相位[J]. 地球科学, 1994, 19(5): 575-586. Google Scholar
[68]	杜远生, 龚一鸣, 刘本培, 等. 华南板块泥盆纪层序地层及海平面变化[J]. 岩相古地理, 1996, 16(6): 14-23. Google Scholar
[69]	Zhang X S, Jeffrey Over D, Ma K Y, et al. Upper Devonian conodont zonation, sea-level changes and bio-events in offshore carbonate facies Lali section, South China[J]. Palaeogeography Palaeoclimatology Palaeoecology, 2019, 531: 109219. doi: 10.1016/j.palaeo.2019.05.041 CrossRef Google Scholar
[70]	Ma X P, Wang H H, Zhang M Q. Devonian event succession and sea level change in South China-With Early and Middle Devonian carbon and oxygen isotopic data[J]. Subcomm Devonian Stratigr Newsl, 2017, 32: 17-24. Google Scholar
[71]	Johnson J G, Klapper G, Sandberg C A. Devonian eustatic fluctuations in Euramerica[J]. Geological Society of America Bulletin, 1985, 96: 567-587. doi: 10.1130/0016-7606(1985)96<567:DEFIE>2.0.CO;2 CrossRef Google Scholar
[72]	Over D J, Ruppel S C. Woodford conodonts and biotratigraphy(Upper Devonian-Carboniferous)in the subsurface of eastern New Mexico and Texas[J]. Stratigraphy, 2011, 8: 271-279. Google Scholar
[73]	Becker R T. Stratigraphische Gliederung und Ammoneen-Faunen im Nehdenium(Oberdevon Ⅱ)von Europa und Nord-Afrika[J]. Courier Forschungsinstitut Senckenberg, 1993, 155: 1-35. Google Scholar
[74]	Becker R T. Anoxia, eustatic changes, and Upper Devonian to lowermost Carboniferous global ammonoid diversity[M]. The Systematics Association Special, 1993: 115-164. Google Scholar
[75]	Becker R T, House M R. Sea-level changes in the Upper Devonian of the Canning Basin, western Australia[J]. Courier Forschungsinstitut Senckenberg, 1997, 199(199): 129-146. Google Scholar