广西坡决二叠纪-三叠纪之交含微生物岩剖面介形虫及其古生态意义OSTRACOD FAUNA AND ITS PALAEOECOLOGICAL SIGNIFICANCE FROM THE PERMIAN-TRIASSIC MICROBIALITES IN POJUE, GUANGXI
万俊雨,袁爱华,叶茜,冯庆来,江海水,陈龑
WAN Junyu,YUAN Aihua,YE Qian,FENG Qinglai,JIANG Haishui,CHEN Yan
摘要(Abstract):
通过对广西坡决二叠纪-三叠纪之交含微生物岩剖面进行系统采样,获得455枚保存相对完好的介形虫标本,鉴定为14属56种。坡决剖面介形虫动物群主要以光滑速足介目为主,特别是土菱介科(Bairdiidae)在动物群中占据绝对优势。在二叠纪末大灭绝之后,介形虫动物群虽遭受重创,但在灾后的微生物岩中仍记录了较为丰富的化石群落,群落的优势度较灭绝前明显上升,其优势种组合的变化可能反映了大灭绝之后古海洋环境从反复波动到逐渐趋于稳定的过程,相比传统的古生态组合具有更高精度的古环境指示意义。
Through systematic sampling of the Permian-Triassic microbialite section from Pojue, Guangxi, South China,455 relatively well-preserved ostracod specimens were obtained and identified as 14 genera and 56 species. The fauna is characterized by smooth-shelled Podocopida, especially the Bairdiidae, which is absolutely dominant. Although the ostracod fauna was severely damaged during the end-Permian mass extinction, some relatively abundant fossil assemblages were still recorded in the post-extinction microbialites, and the dominance of the assemblages increased significantly compared to the pre-extinction assemblages. The changes of the dominant species groups, which may reflect the process from repeated fluctuations to gradual stabilization of the palaeoenvironment after the mass extinction, is a potential highprecision palaeoenvironmental indicator comparing with the traditional palaeoecological assemblages based on family level.
关键词(KeyWords):
介形虫;二叠纪末大灭绝;优势种;古生态;微生物岩
Ostracoda;end-Permian mass extinction;dominant species;palaeoecology;microbialite
基金项目(Foundation): 国家自然科学基金特提斯地球动力系统重大研究计划项目(92055201);国家自然科学基金重点项目(41730320)和国家自然科学基金面上项目(41972033)共同资助~~
作者(Author):
万俊雨,袁爱华,叶茜,冯庆来,江海水,陈龑
WAN Junyu,YUAN Aihua,YE Qian,FENG Qinglai,JIANG Haishui,CHEN Yan
DOI: 10.16087/j.cnki.1000-0674.20230630.001
参考文献(References):
- 王永标,童金南,王家生等,2005.华南二叠纪末大绝灭后的钙质微生物岩及古环境意义.科学通报,50(6):552-558
- 王尚启,1988.中国南方晚古生代介形类的某些集群及其生态探讨.古生物学报,27(1):91-102
- 戎嘉余,詹仁斌,2006.论大灭绝后的幸存类型、复活效应与避难所.地学前缘,13(6):188-198
- 沈树忠,张华,2017.什么引起五次生物大灭绝?科学通报,62(11):1119-1135
- 颜铁增,王尚启,祁玉平,2005.浙江桐庐早二叠世船山组介形类化石.古生物学报,44(2):247-259
- BECKER G,2002.Palaeozoic Ostracoda:the standard classification scheme.Neues Jahrbuch fur Geologie und Palaontologie-Abhandlungen,226(2):165-228
- CHEN Y,YE Q,JIANG H S et al.,2019.Conodonts and carbon isotopes during the Permian-Triassic transition on the Napo Platform,South China.Journal of Earth Science,30(2):244-257
- CRASQUIN S,FOREL M-B,2014.Ostracods (Crustacea) through PermianTriassic events.Earth-Science Reviews,137:52-64
- CRASQUIN S,FOREL M-B,YUAN A H et al.,2018.Species of Hollinella(Palaeocopida:Ostracoda:Crustacea) as stratigraphical indices of the Late Permian-Early Triassic post-extinction interval.Journal of Systematic Palaeontology,16(3):213-224
- CRASQUIN-SOLEAU S,MARCOUX J,ANGIOLINI L et al.,2004.A new ostracode fauna from the Permian-Triassic boundary in Turkey (Taurus,Antalya Nappes).Micropaleontology,50(3):281-295
- DAL CORSO J,MILLS B J W,CHU D L et al.,2020.Permo-Triassic boundary carbon and mercury cycling linked to terrestrial ecosystem collapse.Nature Communications,11(1):2962
- FOREL M-B,2012.Ostracods (Crustacea) associated with microbialites across the Permian-Triassic boundary in Dajiang (Guizhou Province,South China).European Journal of Taxonomy,19:1-34
- FOREL M-B,GR?DINARU E,WANG Y,2018.First report of ostracods(Crustacea) associated with Bithynian (Anisian,Middle Triassic)Tubiphytes-microbial reef in the North Dobrogean Orogen (Romania).Papers in Palaeontology,4(2):211-244
- HAQ B U,2018.Triassic eustatic variations reexamined.GSA Today,28(12):4-9
- HORNE D J,COHEN A,MARTENS K,2002.Taxonomy,morphology and biology of Quaternary and living Ostracoda.The Ostracoda:Applications in Quaternary Research,131:5-36
- KARANOVIC I,BRAND?O S N,2016.The genus Polycope (Polycopidae,Ostracoda) in the North Atlantic and Arctic:taxonomy,distribution,and ecology.Systematics and Biodiversity,14(2):198-223
- KERSHAW S,CRASQUIN S,LI Y et al.,2012.Microbialites and global environmental change across the Permian-Triassic boundary:a synthesis.Geobiology,10(1):25-47
- MOORE R C,1961.Treatise on Invertebrate Paleontology.Part Q.Arthropoda 3.Crustacea Ostracoda.Lawrence:Geological Society of America and University of Kansas Press.1-442
- RONG J Y,ZHAN R B,2006.Re-evaluation of survivors,Lazarus taxa,and refugia from mass extinction.Earth Science Frontiers,13(6):187-198
- SHEN J,ZHANG Y G,YANG H et al.,2022.Early and late phases of the Permian-Triassic mass extinction marked by different atmospheric CO2regimes.Nature Geosciences,15(10):839-844
- SHEN S Z,ZHANG H,2017.What caused the five mass extinctions?Chinese Science Bulletin,62(11):1119-1135
- STANLEY S M,2016.Estimates of the magnitudes of major marine mass extinctions in earth history.Proceedings of the National Academy of Sciences,113(42):E6325-E6334
- WAN J Y,YUAN A H,CRASQUIN S et al.,2019.High-resolution variation in ostracod assemblages from microbialites near the Permian-Triassic boundary at Zuodeng,Guangxi region,South China.Palaeogeography,Palaeoclimatology,Palaeoecology,535:109349
- WANG S Q,1988.Late Paleozoic ostracode associations from South China and their paleoecological significances.Acta Palaeontologica Sinica,27(1):91-102
- WANG Y B,TONG J N,WANG J S et al.,2005.Calcareous microbial rocks and paleoenvironmental significance after the Late Permian mass extinction in South China.Chinese Science Bulletin,50(6):552-558
- YAN T Z,WANG S Q,QI Y P,2005.Ostracodes from the Chuanshan Formation at the Shencun section of Tonglu,Zhejiang.Acta Palaeontologica Sinica,44(2):247-259
- YIN H F,JIANG H S,XIA W C et al.,2014.The end-Permian regression in South China and its implication on mass extinction.Earth-Science Reviews,137:19-33