华南上泥盆统法门阶哲杜斯贝动物群的埋藏学和居群动力学特征<sup>&#x0002A;</sup>

doi:10.7605/gdlxb.2021.06.077

古地理学报 ›› 2021, Vol. 23 ›› Issue (6): 1210-1224. doi: 10.7605/gdlxb.2021.06.077

• 生物古地理学及古生态 • 上一篇下一篇

华南上泥盆统法门阶哲杜斯贝动物群的埋藏学和居群动力学特征^*

李彤¹, 董琳¹, 袁志伟¹, 凌坤¹, 甯濛², 秦树健¹, 杨润宇¹, 刘威¹, 聂婷¹, 李辰卿¹, 孙元林¹

1 北京大学地球与空间科学学院,北京 100871;
2 成都理工大学沉积地质研究院,四川成都 610059

收稿日期:2021-06-22 修回日期:2021-08-13 出版日期:2021-12-01 发布日期:2021-12-03
作者简介:李彤,女,1995年生,北京大学博士研究生, 研究方向为沉积学和古生物学。E-mail: jessie_li@pku.edu.cn。
基金资助:
*国家自然科学基金项目(编号: 41772015,41672334)资助。

Taphonomic features and population dynamics of the Upper Devonian Famennian Dzieduszyckia fauna in South China

Li Tong¹, Dong Lin¹, Yuan Zhi-Wei¹, Ling Kun¹, Ning Meng², Qin Shu-Jian¹, Yang Run-Yu¹, Liu Wei¹, Nie Ting¹, Li Chen-Qing¹, Sun Yuan-Lin¹

1 School of Earth and Space Science,Peking University,Beijing 100871, China;
2 Institute of Sedimentary Geology,Chengdu University of Technology,Chengdu 610059, China

Received:2021-06-22 Revised:2021-08-13 Online:2021-12-01 Published:2021-12-03
About author:Li Tong,born in 1995,is a candidate for Ph.D. in Peking University. She is engaged in research of sedimentology and paleontology. E-mail: jessie_li@pku.edu.cn.
Supported by:
National Natural Science Foundation of China(Nos. 41772015,41672334)

摘要/Abstract

摘要： 哲杜斯贝是一种以高丰度和低物种分异度为显著特征、在全球广泛独立分布的小嘴贝类。笔者对华南台地相和台间盆地相5个含哲杜斯贝类上泥盆统剖面进行沉积环境和埋藏特征研究,确定华南哲杜斯贝类的原生沉积环境为台地的正常浅水,这与美国和摩洛哥生长在冷泉环境中的哲杜斯贝不同,表明其既可在浅海环境中生长,也可以在冷泉环境中生长,具有较强的生态可塑性。台地相(原地埋藏)的3个哲杜斯贝种群具有以下特征:(1)均呈现出壳体呈层状紧密堆积、集群生长特点,丰度极高,并且有相当数量的个体呈现出由于拥挤生长而导致的壳体生长畸形现象;(2)缺乏其他底栖后生生物,显示了极低的生物多样性;(3)壳体大小—频率分布和生存曲线揭示了3个哲杜斯贝种群都具有非常低的幼年期死亡率特点,同时同一介壳层内哲杜斯贝个体大小均一,表明绝大多数的个体能够达到或接近自然寿命后死亡。上述证据表明,哲杜斯贝具有密集群居生活的习性,其生活在一个独特的、不适合其他后生底栖生物生存的环境。

关键词: Dzieduszyckia(哲杜斯贝), 原地埋藏, 台地相, 台间盆地相, 高丰度, 低物种分异度, 生长畸形

Abstract: Dzieduszyckia is a rhynchonellide brachiopods genus,featured by its bisulcate,strongly costate shell. It is widely accepted that Dzieduszyckia developed in cold-seep environments. This study aims to investigate the primary living environments of Dzieduszyckia in South China and their population features. Comparison of depositional features between coquinas from platform and intra-platform basin indicates that Dzieduszyckia in South China primarily occupied the platform niches,which is different from that in North American and Morocco. It suggests that Dzieduszyckia had a larger ecological plasticity than the modern organisms present in the cold-seep environment. More than one thousand specimens of Dzieduszyckia from three localities were collected in this study. These three populations have an extremely high abundance with high proportions of growth asymmetry,which resulted from squeezing of individuals during growth,suggesting a dense crowed life habit for the brachiopods. The Dzieduszyckia populations barely coexisted with other benthic animals,showing an extremely low diversity in the entire area. Length-frequency distribution and survivorship curve reveal that each of the Dzieduszyckia populations has a low juvenile mortality. The identical shell length in the same natural coquina also supports that the majority of individuals grew up and died naturally. All evidence suggests that Dzieduszyckia takes tight-growth pattern as the survival strategy,living in a unique environment that was not suitable for other benthic organisms.

Key words: Dzieduszyckia, autochthonous burial, platform facies, intraplatform facies, high abundance, low diversity, malformation

中图分类号:

Q915.5

李彤, 董琳, 袁志伟, 凌坤, 甯濛, 秦树健, 杨润宇, 刘威, 聂婷, 李辰卿, 孙元林. 华南上泥盆统法门阶哲杜斯贝动物群的埋藏学和居群动力学特征^*[J]. 古地理学报, 2021, 23(6): 1210-1224.

Li Tong, Dong Lin, Yuan Zhi-Wei, Ling Kun, Ning Meng, Qin Shu-Jian, Yang Run-Yu, Liu Wei, Nie Ting, Li Chen-Qing, Sun Yuan-Lin. Taphonomic features and population dynamics of the Upper Devonian Famennian Dzieduszyckia fauna in South China[J]. JOPC, 2021, 23(6): 1210-1224.

http://www.gdlxb.cn/CN/Y2021/V23/I6/1210

参考文献

[1] 侯鸿飞,季强,吴祥和,熊剑飞,王士涛,高联达,盛怀斌,魏家庸,苏珊·特纳. 1985. 贵州睦化泥盆—石炭系界线. 北京: 地质出版社,226.
[Hou H F,Ji Q,Wu X H,Xiong J F,Wang S T,Gao L D,Sheng H B,Wei J Y,Turner S.1985. Muhua Section of Devonian-Carboniferous Boundary Beds. Beijing: Geological Publishing House,226]
[2] 侯鸿飞,王士涛. 1988. 中国地层7: 中国的泥盆系. 北京:地质出版社, 261-265.
[Hou H F,Wang S T.1988. The Devonian System of China,Stratigraphy of China(No.7). Beijing: Geological Publishing House,261-265]
[3] 阮亦萍. 1981. 广西、贵州泥盆纪和早石炭世早期菊石群. 中国科学院南京地质古生物研究所集刊, 15: 1-152.
[Ruan Y P.1981. Devonian and earliest Carboniferous ammonoids from Guangxi and Guizhou. Memories of Nanjing Institute of Geology and Palaeontology,Academia Sinica, 15: 1-152]
[4] 孙云铸,沈耀庭. 1965. 黔南晚泥盆世后期乌克曼菊石(Wocklumeria)层的菊石群及其地层意义. 中华人民共和国地质部地质科学研究院论文集,乙种, 1: 33-99.
[Sun Y Z,Shen Y T.1965. On the late Upper Devonian ammonite fauna of the Wocklumeria beds of southern Kweichow and its stratigraphical significance. Professional Papers of Chinese Academy of Geological Sciences: Section B, 1: 33-99]
[5] 鲜思远,江宗龙. 1978. 腕足动物门. 见:贵州地层古生物工作队(编著). 西南地区古生物图册(贵州分册)(一):寒武纪—泥盆纪. 北京: 地质出版社,251-337.
[Xian S Y,Jiang Z L.1978. Brachiopoda. In:Stratigraphic and Paleontological Working Team of Guizhou Province(ed). Paleontological Atlas of Western China(Guizhou Province)(Volume 1): Cambrian-Devonian. Beijing: Geological Publishing House,251-337]
[6] 鲜思远,王守德,周希云,熊剑飞,周天荣. 1980. 华南泥盆纪南丹型地层及古生物. 贵阳: 贵州人民出版社,1-161.
[Xian S Y,Wang S D,Zhou X Y,Xiong J F,Zhou T R.1980. Stratigraphy and Paleontology of Nandan-type Devonian in South China. Guiyang: People's Press of Guizhou Province,1-161]
[7] 许寿永. 1984. 湘、鄂二叠纪珊瑚动物群的特征. 古生物学报, 23(5): 605-616.
[Xu S Y.1984. The character of coral fauna in Perian in the Hunan and Hubei Provinces. Acta Palaeontologica Sinica, 23(5): 605-616]
[8] 钟铿,吴诒,殷保安,梁演林,姚肇贵,彭金兰. 1992. 广西的泥盆系. 武汉: 中国地质大学出版社,1-384.
[Zhong K,Wu Y,Yin B A, Liang Y L, Yao Z G,Peng J L.1992. The Devonian System of Guangxi,China. Wuhan: The Press of China University of Geosciences,1-384]
[9] Ager D V,Cossey,S P J,Mullin P R,Walley C D.1976. Brachiopod ecology in mid-Palaezoic sediments near Khenifra,Morocco. Palaeogeography,Palaeoclimatology,Palaeoecology, 20(3): 171-185.
[10] Baliński A,Biernat G.2003. New observations on rhynchonelloid brachiopod Dzieduszyckia from the Famennian of Morocco. Acta Palaeontologica Polonica, 74(5): 463-474.
[11] Biernat G.1967. New data on the genus Dzieduszyckia Siemiradzki,1909(Brachiopoda). Acta Palaeontologica Polonica, 12: 133-155.
[12] Bitner M A.2001. Size-frequency distributions of Miocene micromorphic brachiopods: interpretation tool for population dynamics. Marine Ecology, 23(1): 19-30.
[13] Campbell K A,Bottjer D J.1995. Brachiopods and chemosymbiotic bivalves in Phanerozoic hydrothermal vent and cold seep environments. Geology, 23(4): 321-324.
[14] Campbell K A.2006. Hydrocarbon seep and hydrothermal vent paleoenvironments and paleontology: past developments and future research directions. Palaeogeography,Palaeoclimatology,Palaeoecology, 232(2): 362-407.
[15] Chen D Z,Tucker M E,Jiang M S,Zhu J Q.2001a. Long-distance correlation between tectonic-controlled,isolated carbonate platforms by cyclostratigraphy and sequence stratigraphy in the Devonian of South China. Sedimentology, 48: 57-78.
[16] Chen D Z,Tucker M E,Zhu J Q,Jiang M S.2001b. Carbonate sedimentation in a starved pull-apart basin,Middle to Late Devonian,southern Guilin,South China. Basin Research, 13: 141-167.
[17] Cloud Jr. P E,Boucot A J.1971. Dzieduszyckia in Nevada. Smithsonian Contributions to Paleobiology, 3: 175-180.
[18] Dubé T E.1988. Tectonic significance of Upper Devonian igneous rocks and bedded barite,Roberts Mountain allochthon,Nevada,U.S.A.In: McMillan N S M,Embry A F,Glass D J(eds). Devonian of the World(Vol.Ⅱ,Sedimentation),Canada. Canadian Society of Petroleum Geologists,235-249.
[19] Gischler E,Sandy M,Peckmann J.2003. Ibergirhynchia contraria(F. A. Roemer,1850),an Early Carboniferous seep-related rhynchonellide brachiopod from the Harz Mountains,Germany: a possible successor to Dzieduszyckia?Journal of Paleontology, 77(2): 293-303.
[20] Huang Y,Tong J,Fraiser M L.2018. A Griesbachian(Early Triassic)mollusc fauna from the Sidazhai section,southwest China,with paleoecological insights on the proliferation of genus glaraia(Bivalvia). Journal of Earth Science, 29(4): 794-805.
[21] Lü D,Ma X P.2017. Population statistic of two late Frasnian(Late Devonian)brachiopod faunas from central Hunan of China and its palaeoecological significance. Acta Palaeontologica Sinica, 56(2): 189-200.
[22] Ma X P,Gong Y M,Chen D Z,Racki G,Chen X Q,Liao W H.2016. The Late Devonian Frasnian-Famennian Event in South China: patterns and causes of extinctions,sea level changes,and isotope variations. Palaeogeography,Palaeoclimatology,Palaeoecology, 448: 224-244.
[23] Nie T,Guo W,Sun Y L,Shen B,Yin B A,Tang Z H,Li Y K,Huang X L,Mai C.2016. Age and distribution of the Late Devonian brachiopod genus Dzieduszyckia Siemiradzki,1909 in southern China. Palaeoworld, 25(4): 600-615.
[24] Noll J H,Dutro J T,Beus S S.1984. A new species of the Late Devonian(Famennian)brachiopod Dzieduszyckia from Sonora,Mexico. Journal of Paleontology, 58(6): 1412-1421.
[25] Pan Y,Sha J,Yao X.2012. Taphonomy of Early Cretaceous freshwater bivalve concentrations from the Sihetun area,western Liaoning,NE China. Cretaceous Research, 34: 94-106.
[26] Peckmann J,Campbell K A,Walliser O H,Reitner J.2007. A late Devonian hydrocarbon-seep deposit dominated by dimerelloid brachiopods,Morocco. Palaios, 22(2): 114-122.
[27] Richards R P,Bambach R K.1975. Population dynamics of some Paleozoic brachiopods and their paleoecological significance. Journal of Paleontology, 49(5): 775-798.
[28] Riding R,Liang L.2005. Geobiology of microbial carbonates: metazoan and seawater saturation state influences on secular trends during the Phanerozoic.Palaeogeography,Palaeoclimatology,Palaeoecology, 219(1-2): 101-115.
[29] Sandy M.1995. A review of some Paleozoic and Mesozoic brachiopods as members of cold seep chemosynthetic communities: “unusual” palaeoecology and anomalous palaeobiogeographic patterns explained. Földtani Közlöny Bull Hung Geol Soc, 125: 241-258.
[30] Skawina A.2013. Population dynamics and taphonomy of the Late Triassic(Carnian)freshwater bivalves from Krasiejów(Poland). Palaeogeography,Palaeoclimatology,Palaeoecology, 379-380: 68-80.
[31] Tien C C.1938. Devonian brachiopoda of Hunan. Palaeontologia Sinica,New Series B, 4: 1-192.
[32] Tomašových A.2004. Postmortem durability and population dynamics affecting the fidelity of brachiopod size-frequency distributions. Palaios, 19(5): 477-496.
[33] Tomašových A.2006. Linking taphonomy to community-level abundance: insights into compositional fidelity of the Upper Triassic shell concentrations(Eastern Alps). Palaeogeography,Palaeoclimatology,Palaeoecology, 235(4): 355-381.
[34] Torres M E,Bohrmann G,Dubé T E,Poole F G.2003. Formation of modern and Paleozoic stratiform barite at cold methane seeps on continental margins. Geology, 31(10): 897-900.
[35] Walliser O H,Hassani A,Tahiri A.2000. Mrirt: a key area for the Vanscan Meseta of Morocco,Service Geologique du Maroc. Notes et Memoires, 399: 93-108.
[36] Wang Z,Guo W,Nie T,Ma H,Huang T,Sun Y.2019. Is seawater geochemical composition recorded in marine carbonate?Evidence from iron and manganese contents in Late Devonian carbonate rocks. Acta Geochim, 38(2): 173-189.
[37] Webster M,Gaines R R,Hughes N C.2008. Microstratigraphy,trilobite biostratinomy,and depositional environment of the “Lower Cambrian” Ruin Wash Lagersttte,Pioche Formation,Nevada. Palaeogeography,Palaeoclimatology,Palaeoecology, 264(1-2): 100-122.
[38] Yuan Z,Sun Y,Shen B,Xing C,Liu W,Yang R,Qin S,Baliński A.2019. An in-situ preserved early Carboniferous(Serpukhovian)community in southern Guizhou,China. Rivista Italiana di Paleontologia e Stratigrafia, 125(3): 689-710.
[39] Zuschin M,Harzhauser M,Mandic O.2004. Taphonomy and paleoecology of the Lower Badenian(Middle Miocene)molluscan assemblages at Grund(Lower Austria). Geologica Carpathica, 55(2): 117-128.
[40] Zuschin M,Harzhauser M,Mandic O.2005. Influence of size-sorting on diversity estimates from tempestitic shell beds in the Middle Miocene of Austria. Palaios, 20: 142-158.
[41] Nalivkin D V.1947. Class Brachiopoda. In: Nalivkin D V,Verber V N(eds). Alas Rukovodaâih form Iskopaemyh Faun SSSR(Tom 3),Leningrad: Devonskaaâ sistema,VSEGEI-Gosgeoltehizdat,63-134.
[42] Rozman H S.1962. Stratigraphy and brachiopods of the Famennian stage of Mugodzhars and adjacent areas. Trudy Geologičeskogo Instituta AN SSSR, 50: 1-187.

选择文件类型/文献管理软件名称

选择包含的内容

华南上泥盆统法门阶哲杜斯贝动物群的埋藏学和居群动力学特征^*

Taphonomic features and population dynamics of the Upper Devonian Famennian Dzieduszyckia fauna in South China

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 7

编辑推荐

Metrics

本文评价

[1]	张淑荣, 山显任, 盖志琨. 广西南宁下泥盆统华南鱼类化石新发现及其地层和古地理意义^*[J]. 古地理学报, 2023, 25(2): 341-355.
[2]	山显任, 朱敏, 赵文金, 盖志琨. 湖北武汉地区志留系下红层的古鱼类化石及其生物古地理意义^*[J]. 古地理学报, 2023, 25(2): 327-340.
[3]	董俊彦, 龚一鸣. 层孔虫研究进展与展望^*[J]. 古地理学报, 2019, 21(5): 783-802.
[4]	郭书元, 詹伟, 王强. 河北省白洋淀地区中全新世丽蚌动物群及其生态环境意义[J]. 古地理学报, 2014, 16(3): 335-346.
[5]	路琳琳, 纪友亮. 下扬子地区寒武纪层序格架及古地理演化[J]. 古地理学报, 2013, 15(6): 765-776.
[6]	陈智敏, 孙元林. 具彩色斑纹颅形贝在广西桂林下石炭统黄金组中的发现:兼论颅形贝属的地质地理分布[J]. 古地理学报, 2013, 15(6): 795-808.
[7]	柳永清, 旷红伟, 彭楠, 许欢, 陈军, 徐加林, 刘海, 章朋. 冀西北尚义上侏罗统—下白垩统后城组恐龙足迹新发现及生物古地理意义^*[J]. 古地理学报, 2012, 14(5): 617-627.

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

华南上泥盆统法门阶哲杜斯贝动物群的埋藏学和居群动力学特征*

Taphonomic features and population dynamics of the Upper Devonian Famennian Dzieduszyckia fauna in South China

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 7

编辑推荐

Metrics

本文评价

华南上泥盆统法门阶哲杜斯贝动物群的埋藏学和居群动力学特征^*