豫西苗岭统馒头组二段皱饰构造与遗迹化石共生特征<sup>&#x0002A;</sup>

doi:10.7605/gdlxb.2022.06.082

古地理学报 ›› 2022, Vol. 24 ›› Issue (6): 1162-1178. doi: 10.7605/gdlxb.2022.06.082

• 生物古地理学及古生态 • 上一篇下一篇

豫西苗岭统馒头组二段皱饰构造与遗迹化石共生特征^*

李妲^1,2,3, 贺西同¹, 邢智峰^1,2,3, 齐永安^1,2,3, 郑伟^1,2,3, 付建¹

1 河南理工大学资源环境学院,河南焦作 454003;
2 河南省生物遗迹与成矿过程重点实验室,河南焦作 454003;
3 中原经济区煤层气与页岩气协同创新中心,河南焦作 454003

收稿日期:2022-08-05 修回日期:2022-09-26 出版日期:2022-12-01 发布日期:2022-12-05
通讯作者: 邢智峰,1973年生,女,副教授,博士,主要从事沉积学、古生物学、遗迹学等研究工作。ORCID: 0000-0003-2603-640X。E-mail: xingzhifeng925@hpu.edu.cn。
作者简介:李妲,1984年生,女,讲师,博士,主要从事沉积学、古生物学、遗迹学等研究工作. E-mail: lida@hpu.edu.cn。
基金资助:
*国家自然科学基金项目(编号: 41902113),河南省高等学校重点科研项目(编号: 21A170013),河南省科技攻关项目(编号: 202102310336)联合资助

Symbiotic characteristics of wrinkle structure and trace fossils in the Second Member of Miaolingian Mantou Formation in western Henan

LI Da^1,2,3, HE Xitong¹, XING Zhifeng^1,2,3, QI Yong'an^1,2,3, ZHENG Wei^1,2,3, FU Jian¹

1 School of Resources and Environment,Henan Polytechnic University,Henan Jiaozuo 454003, China;
2 Key Laboratory of Biogenic Traces and Sedimentary Minerals of Henan Province,Henan Jiaozuo 454003, China;
3 Central Plains Economic Zone Coalbed Methane and Shale Gas Collaborative Innovation Center,Henan Jiaozuo 454003, China

Received:2022-08-05 Revised:2022-09-26 Online:2022-12-01 Published:2022-12-05
Contact: XING Zhifeng,born in 1973,is an associate professor. She is mainly engaged in researches of sedimentology,paleontology and ichnology. ORCID: 0000-0003-2603-640X.E-mail: xingzhifeng925@hpu.edu.cn.
About author:LI Da,born in 1984,lecturer,is mainly engaged in researches of sedimentology,paleontology and ichnology. E-mail: lida@hpu.edu.cn.
Supported by:
Co-funded by the National Natural Science Foundation of China(No.41902113),Key Research Project of Higher Education Institutions in Henan Province(No.21A170013),and Key Scientific and Technological Projects in Henan Province(No.202102310336)

摘要/Abstract

摘要： 埃迪卡拉纪以来,微生物与后生动物之间呈此消彼长的关系,但在寒武纪苗岭世却出现了微生物成因沉积构造和后生动物扰动构造短暂共存的现象。笔者在豫西馒头组二段下部识别出包括皱饰构造与微生物席裂构造在内的2种微生物成因沉积构造,对皱饰构造与遗迹化石的共生关系进行了分类,建立了席上足辙迹(Monomorphichnus henanensis)与牧食迹(Jinningichnus badaowanensis)、席下水平漫游迹(Planolites montanus)、席下深层泥岩中生物扰动共3种微生物席与后生动物的共生模式和生态演化模型。上述研究表明,具有特殊环境耐受性的“机会主义”动物在食物来源较为宽松的潮坪环境中与微生物席共存,这种微生物席与后生动物短暂而“和谐”的共存关系不仅延续了埃迪卡拉纪双方的部分共生特征,且在以混合底为主导的显生宙生态环境中得到了进一步变化与发展。

关键词: 微生物席, 皱饰构造, 遗迹化石, 控制因素, 寒武系, 豫西

Abstract: Since the Ediacaran period,the microbes and metazoan were interacted,but microbial induced sedimentary structures(MISS)and metazoan bioturbation structures coexisted temporarily in the Cambrian Miaoling age. In this paper,two types of microbially induced sedimentary structures,including wrinkle structures and microbial mat-crack structures,are identified in the lower part of the Second Member of the Mantou Formation in western Henan Province. The symbiotic relationship between MISS and trace fossils was classified,and three models of the symbiotic relationship between the wrinkle structures and metazoans and ecological evolution model of microbial mat and metazoan were established, including the trackways(Monomorphichnus henanensis)and the grazing trace(Jinningichnus badaowanensis)on the microbial mat, Planolites montanus under microbial mat, and the burrows in mudstone substrate. It showed that some organisms with special environmental tolerance coexisted with microbial mats in the tidal environment with relatively sufficient food sources,revealing the short period of harmonious coexistence relationship between microbial mat and metazoans not only continued the partial symbiotic characteristics during the Ediacaran,but also developed in the mixground-dominated Phanerozoic ecological environment.

Key words: microbial mat, wrinkle structure, trace fossils, controlling factors, Cambrian, western Henan Province

中图分类号:

Q911.28

李妲, 贺西同, 邢智峰, 齐永安, 郑伟, 付建. 豫西苗岭统馒头组二段皱饰构造与遗迹化石共生特征^*[J]. 古地理学报, 2022, 24(6): 1162-1178.

LI Da, HE Xitong, XING Zhifeng, QI Yong'an, ZHENG Wei, FU Jian. Symbiotic characteristics of wrinkle structure and trace fossils in the Second Member of Miaolingian Mantou Formation in western Henan[J]. JOPC, 2022, 24(6): 1162-1178.

http://www.gdlxb.cn/CN/Y2022/V24/I6/1162

参考文献

[1] 郭荣涛,郭丽娜,霍荣. 2012. 皱饰构造研究进展综述. 地质科技情报, 31(3): 16-23,30.
[Guo R T,Guo L N,Huo R. 2012. Review on the wrinkle structure. Geological Science and Technology Information, 31(3): 16-23,30]
[2] 李妲,齐永安,代明月,王敏. 2016. 豫西寒武系第二、三统馒头组固底控制的遗迹化石. 古生物学报, 55(2): 170-180.
[Li D,Qi Y A,Dai M Y,Wang M. 2016. Firm-ground trace fossils in the Mantou Formation(Cambrian Series 2 and 3),western Henan,central China. Acta Palaeontologica Sinica, 55(2): 170-180]
[3] 梅冥相. 2011. 陆源碎屑岩中微生物诱发的沉积构造的成因类型及其分类体系. 地质论评, 57(3): 419-436.
[Mei M X. 2011. Genetic types and their classification for the microbial induced sedimentary structure within terrigenous clastic rocks. Geological Review, 57(3): 419-436]
[4] 梅冥相. 2014. 微生物席的特征和属性: 微生席沉积学的理论基础. 古地理学报, 16(3): 285-304.
[Mei M X. 2014. Feature and nature of microbial-mat: theoretical basis of microbial-mat sedimentology. Journal of Palaeogeography(Chinese Edition), 16(3): 285-304]
[5] 齐永安,王敏,李妲,代明月. 2012. 寒武纪底质革命: 从微生物席底到生物扰动混合底. 河南理工大学学报(自然科学版), 31(2): 159-164.
[Qi Y A,Wang M,Li D,Dai M Y. 2012. Cambrian substrate revolution: from matgrounds to bioturbated mixgrounds. Journal of Henan Polytechnic University(Natural Science), 31(2): 159-164]
[6] 齐永安,李小燕,陈白兵,庆国帅. 2019. 豫西宜阳地区寒武系第三统馒头组二段鲕粒滩—微生物丘组合及其成因分析. 河南理工大学学报(自然科学版), 38(2): 34-41.
[Qi Y A,Li X Y,Chen B B,Qing G S. 2019. Analysis on the oolitic shoal-microbial mound combinations and their geneses in the Second Member of Mantou Formation,Cambrian,Series 3,Yiyang area,western Henan. Journal of Henan Polytechnic University(Natural Science), 38(2): 34-41]
[7] 孙大中,陆松年. 1987. 华北地台的元古宙构造演化. 中国地质科学院院报, 16: 55-69.
[Sun D N,Lu S N. 1987. Proterozoic tectonic evolution of the North China Platform. Bulletin of the Chinese Academy of Geosciences, 16: 55-69]
[8] 邢智峰,刘云龙,付玉鑫,齐永安,郑伟. 2020. 豫西鲁山中元古界云梦山组微生物成因沉积构造发育特征及古环境意义. 沉积学报, 38(1): 46-54.
[Xing Z F,Liu Y L,Fu Y X,Qi Y A,Zheng W. 2020. Characteristics of microbially induced sedimentary structures and their paleoenvironmental significance from the Mesoproterozoic Yunmengshan Formation in Lushan area,western Henan. Acta Sedimentologica Sinica, 38(1): 46-54]
[9] 杨式溥,张建平,杨美芳. 2004. 中国遗迹化石. 北京: 科学出版社,353.
[Yang S P,Zhang J P,Yang M F. 2004. Fossils of Chinese Relics. Beijing: Science Press,353]
[10] 赵相宽,史晓颖,王新强,汤冬杰. 2018. 寒武纪早期海洋阶段性氧化驱动早期后生动物多样化进程. 地球科学, 43(11): 3873-3890.
[Zhao X K,Shi X Y,Wang X Q,Tang D J. 2018. Stepwise oxygenation of Early Cambrian ocean drove early metazoan diversification. Earth Science, 43(11): 3873-3890]
[11] 钟怡江,文华国,陈洪德,刘磊,陈安清,王兴龙,王志伟,白璇. 2022. 胞外聚合物在蓝细菌钙化过程中的作用及其地质意义. 沉积学报, 40(1): 88-105.
[Zhong Y J,Wen H G,Chen H D,Liu L,Chen A Q,Wang X L,Wang Z W,Bai X. 2022. The role of extracellular polymeric substances in Cyanobacterial calcification and its geological significance. Acta Sedimentologica Sinica, 40(1): 88-105]
[12] 朱茂旭,史晓宁,杨桂朋,李铁,吕仁燕. 2011. 海洋沉积物中有机质早期成岩矿化路径及其相对贡献. 地球科学进展, 26(4): 395-404.
[Zhu M X,Shi X N,Yang G P,Li T,Lü R Y. 2011. Relative contributions of various early diagenetic pathways to mineralization of organic matter in marine sediments: a review. Advances in Earth Science, 26(4): 395-404]
[13] 朱茂炎,孙智新,杨爱华,袁金良,李国祥,周志强,张俊明. 2021. 中国寒武纪岩石地层划分和对比. 地层学杂志, 45(3): 223-249.
[Zhu M Y,Sun Z X,Yang A H,Yuan J L,Li G X,Zhou Z Q,Zhang J M. 2021 Lithostratigraphic subdivision and correlation of the Cambrian in China. Journal of Stratigraphy, 45(3): 223-249]
[14] Bailey J V,Cocrsetti F A,Bottjer D J,Marenco K N. 2006. Microbially-mediated environmental influences on metazoan colonization of matground ecosystems: evidence from the Lower Cambrian Harkless Formation. Palaios, 21(3): 215-226.
[15] Bayet-Goll A,Daraei M. 2020. Palaeoecological,sedimentological and stratigraphical insights into microbially induced sedimentary structures of the Lower Cambrian successions of Iran. Sedimentology, 67(6): 3199-3235.
[16] Bayet-Goll A,Daraei M,Geyer G,Bahrami N,Bagheri F. 2021. Environmental constraints on the distribution of matground and mixground ecosystems across the Cambrian Series 2-Miaolingian boundary interval in Iran: a case study for the central sector of northern Gondwana. Journal of African Earth Sciences,176: 104120.1-104120.22.
[17] Bosak T,Liang B,Wu T D,Templer S P,Evans A,Vali H,Guerquin-Kern J L,Klepac-Ceraj V,Sim M S,Mui J. 2012. Cyanobacterial diversity and activity in modern conical microbialites. Geobiology, 10: 384-401.
[18] Buatois L A,Mángano M G. 2003. Early colonization of the deep sea: ichnologic evidence of deep-marine benthic ecology from the Early Cambrian of Northwest Argentina. Palaios, 18: 572-581.
[19] Buatois L A,Mángano M G.2011. Ichnology: Organism-substrate Interactions in Space and Time. London:Cambridge University Press,366.
[20] Buatois L A,Mángano M G. 2012. An Early Cambrian shallow-marine ichnofauna from the Puncoviscana Formation of Northwest Argentina: the interplay between sophisticated feeding behaviors,matgrounds and sea-level changes. Journal of Paleontology, 86(1): 7-18.
[21] Buatois L A,Narbonne G M,Mángano M G,Carmona N B,Myrow P. 2014. Ediacaran matground ecology persisted into the earliest Cambrian. Nature Communications, 5: 3544/1-3544/5.
[22] Dornbos S Q,Bottjer D J,Chen J Y. 2004. Evidence for seafloor microbial mats and associated metazoan lifestyles in Lower Cambrian phosphorites of Southwest China. Lethaia, 37: 127-137.
[23] Dornbos S Q,Bottjer D J,Chen J Y. 2005. Paleoecology of benthic metazoans in the Early Cambrian Maotianshan Shale biota and the Middle Cambrian Burgess Shale biota: evidence for the Cambrian substrate revolution. Palaeogeography,Palaeoclimatology,Palaeoecology, 220(1-2): 1-67.
[24] Droser M L,Jensen S,Gehling J G. 2002. Trace fossils and substrates of the terminal Proterozoic-Cambrian transition: implications for the record of early bilaterians and sediment mixing. Proceedings of the National Academy of Sciences, 99(20): 12572-12576.
[25] Fedonkin M A,Simonetta A,Ivantsov A Y. 2007. New data on Kimberella,the Vendian Mollusc-Like Organism(White Sea Region,Russia): palaeoecological and evolutionary implications. In: Vickers-Rich P,Komarower P(eds). the Rise and Fall of the Ediacaran Biota. Geological Society of London Special Publications, 286: 157-179.
[26] Gerdes G,Claes M,Dunajtschik-Piewak K,Riege H,Krumbein W E,Reineck H E. 1993. Contribution of microbial mats to sedimentary surface structures. Facies, 29: 61-74.
[27] Gerdes G,Klenke T,Noffke N. 2000. Microbial signatures in peritidal siliciclastic sediments: a catalogue. Sedimentology, 47(2): 279-308.
[28] Gingras M,Hagadorn J W,Seilacher A,Lalonde S V,Pecoits E,Petrash D,Konhauser K O. 2011. Possible evolution of mobile animals in association with microbial mats. Nature Geoscience, 4: 372-375.
[29] Hagadorn J W,Bottjer D J. 1999. Restriction of a Late Neoproterozoic biotope: suspect-microbial structures and trace fossils at the Vendian Cambrian Transition. Palaios, 14: 73-85.
[30] Hagadorn J W,Dott R H,Damrow D. 2002. Stranded on an Upper Cambrian shoreline: medusae from mentral wisconsin. Geology, 30: 147-150.
[31] Kovalchuk O,Owttrim G W,Konhauser K O,Gingras M K. 2017. Desiccation cracks in siliciclastic deposits: microbial mat-related compared to abiotic sedimentary origin. Sedimentary Geology, 347: 67-78.
[32] Kuwahara V S,Toda T,Hamasaki K,Kikuchi T,Taguchi S. 2000. Variability in the relative penetration of ultraviolet radiation to photosynthetically available radiation in temperate coastal waters,Japan. Journal of Oceanography, 56: 399-408.
[33] Mata S A,Bottjer D J. 2009. The paleoenvironmental distribution of Phanerozoic wrinkle structures. Earth Science Reviews, 96(3): 181-195.
[34] Noffke N,Knoll A,Grotzinger J. 2002. Sedimentary controls on the formation and preservation of microbial mats in siliciclastic deposits: a case study from the upper Neoproterozoic Nama Group,Namibia. Palaios, 17(6): 533-544.
[35] Noffke N,Eriksson K A,Hazen R M,Simpson E L. 2006. A new window into Early Archean life: microbial mats in Earth's oldest siliciclastic tidal deposits(3.2 Ga Moodies Group,South Africa). Geology, 34: 253-256.
[36] Sarkar S,Choudhuri A,Mandal S,Eriksson P G. 2016. Microbial mat-related structures shared by both siliciclastic and carbonate formations. Journal of Palaeogeography, 5(3): 278-291.
[37] Seilacher A,Buatois L A,Mangano M G. 2005. Trace fossils in the Ediacaran-Cambrian transition: behavioural diversification,ecological turnover and environmental shift. Palaeogeography,Palaeoclimatology,Palaeoecology, 227: 323-356.
[38] Seilacher A. 2008. Biomats,biofifilms,and bioglue as preservational agents for arthropod trackways. Palaeogeography,Palaeoclimatology,Palaeoecology, 270: 252-257.
[39] Taylor A M,Goldring R. 1993. Description and analysis of bioturbation and ichnofabric. Journal of the Geological Society, 150(1): 141-148.

选择文件类型/文献管理软件名称

选择包含的内容

豫西苗岭统馒头组二段皱饰构造与遗迹化石共生特征^*

Symbiotic characteristics of wrinkle structure and trace fossils in the Second Member of Miaolingian Mantou Formation in western Henan

RichHTML

PDF

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

[1]	蔡路, 陈华, 杨瑞东, 董艳杰, 梁鹏, 周东东, 高爽, 杨明坤. 黔中石炭系九架炉组含铝岩系中锂分布规律^*[J]. 古地理学报, 2025, 27(2): 383-394.
[2]	谢爽慧, 朱筱敏, 叶蕾, 黄捍东. 湖盆浅水三角洲河道砂体定量表征与控制因素探究及霸县凹陷实例^*[J]. 古地理学报, 2025, 27(2): 446-467.
[3]	郑伟, 和俊淼, 邢智峰, 李妲, 齐永安, 万恩召, 张湘赟. 豫西地区早二叠世—早三叠世植物群演化及其古气候变化^*[J]. 古地理学报, 2025, 27(2): 468-483.
[4]	甯濛, 罗靖茹, 陈家乐, 钟怡江, 文华国. 前寒武系海相白云石胶结物研究现状及展望^*[J]. 古地理学报, 2025, 27(1): 85-108.
[5]	文祖超, 沈玉林, 李壮福, 敬宇鸿, 党志英, 祝玉琳, 孟艳, 李林超. 混合沉积特征精细刻画: 以江苏徐州寒武系馒头组为例^*[J]. 古地理学报, 2024, 26(4): 846-862.
[6]	许旰潇, 齐永安, 何雯逸, 杜耀刚, 刘小梅. 豫北卫辉地区寒武系馒头组含铁鲕粒的特征及形成机制^*[J]. 古地理学报, 2024, 26(4): 863-879.
[7]	孟庆涛, 张训, 杨亮, 高家俊, 刘招君, 胡菲, 邢济麟, 张成铭, 康嘉楠, 崔博, 董秦玮, 张恩威. 陆相拗陷湖盆细粒沉积有机质富集机制研究: 以松辽盆地长岭凹陷青山口组为例^*[J]. 古地理学报, 2024, 26(2): 401-415.
[8]	胡宗全, 高志前, 刘旺威, 卫端. 塔里木盆地东北缘兴地断裂以北地区下寒武统富有机质泥页岩沉积环境与发育机制^*[J]. 古地理学报, 2023, 25(6): 1235-1256.
[9]	彭子霄, 于兴河, 李顺利, 齐荣, 付超, 姜龙燕. 鄂尔多斯盆地东南部本溪组障壁迁移样式及控制因素^*[J]. 古地理学报, 2023, 25(6): 1330-1346.
[10]	王珊, 曹颖辉, 闫磊, 杜德道, 马德波, 张翔, 陈志勇, 周慧, 杨敏, 白莹. 塔里木盆地中下寒武统蒸发岩沉积特征及发育模式^*[J]. 古地理学报, 2023, 25(4): 889-905.
[11]	焦国华, 张卫平, 谢利华, 王军, 周晋科, 汪云海. 准噶尔盆地南部下侏罗统三工河组沉积体系及其控制因素^*[J]. 古地理学报, 2023, 25(3): 628-647.
[12]	毕明威, 孙娇鹏, 陈世悦, 周兆华, 张满郎, 钱爱华. 多尺度河流相致密砂岩储集层表征及控制因素分析:以苏里格气田下石盒子组8段为例^*[J]. 古地理学报, 2023, 25(3): 684-700.
[13]	张小乐, 王怿, 刘建波, 黄璞, 徐洪河. 扬子板块西北缘下泥盆统平驿铺组双壳类遗迹化石^*[J]. 古地理学报, 2023, 25(2): 392-404.
[14]	丁奕, 张立军. 古海洋氧化还原条件的遗迹化石定量表征特征:以华南二叠纪末生物大灭绝事件为例^*[J]. 古地理学报, 2023, 25(2): 405-418.
[15]	许欣, 邢智峰, 郑伟, 齐永安, 李婉颖, 吴盼盼, 张湘赟, 万恩召, 和俊淼, 李妲. 豫西济源地区中下三叠统遗迹网络分析^*[J]. 古地理学报, 2023, 25(2): 419-430.

模态框（Modal）标题

选择文件类型/文献管理软件名称

选择包含的内容

豫西苗岭统馒头组二段皱饰构造与遗迹化石共生特征*

Symbiotic characteristics of wrinkle structure and trace fossils in the Second Member of Miaolingian Mantou Formation in western Henan

RichHTML

PDF

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

豫西苗岭统馒头组二段皱饰构造与遗迹化石共生特征^*