地球科学进展 ›› 2010, Vol. 25 ›› Issue (9): 966 -973. doi: 10.11867/j.issn.1001-8166.2010.09.0966

研究论文 上一篇    下一篇

华南泥盆纪 Chondrites 的特征及其对古氧相的示踪
马会珍 1,张立军 2,龚一鸣 2,3   
  1. 1.贵州省地质调查院,贵州贵阳 550005; 2.中国地质大学生物地质与环境地质教育部重点实验室, 湖北武汉 430074;
    3.河南理工大学生物遗迹与沉积矿产河南省重点实验室,河南焦作454003
  • 收稿日期:2010-01-25 修回日期:2010-06-22 出版日期:2010-09-10
  • 通讯作者: 马会珍 E-mail:hbdzhmhzh@163.com
  • 基金资助:

    国家自然科学基金项目“动藻迹(Zoophycos)的地球生物学研究”(编号:40872001)资助

Chondrites from the Devonian Neritic Cruziana Ichnofacies as Indicators of Palaeo-oxygenation Facies in South China

Ma Huizhen 1, Zhang Lijun 2, Gong Yiming 2, 3   

  1. 1.Guizhou Academy of Geologic Survey, Guiyang 550005,China; 
    2. Key Laboratory of Biogeology and Environmental Geology of Ministry of Education, China University of Geosciences, Wuhan 430074, China; 3. Key Laboratory of Biogenic Traces & Sedimentary Minerals of Henan Province, Henan Polytechnic University, Jiaozuo 454003, China
  • Received:2010-01-25 Revised:2010-06-22 Online:2010-09-10 Published:2010-09-10

系统描述了发育于广西六景、贵州独山、贵阳乌当泥盆纪3个浅海沉积区Cruziana遗迹相Chondrites的产出特征,结合华南泥盆纪其他5个浅海沉积区Cruziana遗迹相的Chondrites资料,对Chondtites的寄主岩系颜色分级、遗迹组构、潜穴直径、遗迹属种的综合研究表明,只有寄主岩系为深灰色—黑色,岩性为灰岩、泥灰岩,潜穴直径小于1 mm,无其他遗迹化石共生时,Chondrites才是贫氧环境标志性遗迹化石的新认识,而个体粗大的Chondrites常发育在常氧环境中。

Chondrites widely occurred in the Devonian neritic Cruziana ichnofacies from the Liujing, Dushan and Wudang sections in South China. Colors of host strata, ichnofabrics and burrow size as well as taxonomy of Chondrites have been studied from 8 selected marine regions in South China. Our data indicated that only those small Chondrites (burrow size <1 mm) preserved in dark, dark grey limestones, mudstones and marls can be viewed as evidence of dysaerobic environments, and that large and strong Chondrites can be found in strata deposited in oxic facies.

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[1] Savrda C E, Bottjer D J. The exaeroxic zone, a new oxygen—Deficient marine biofacies[J]. Nature, 1987, 327: 54-56.
[2] Rhoads D C, Morse J W. Evolutionary and ecologic significance of oxygen-deficient marine basins[J].Lethaia,1971, 4: 413-428.[3] Seilacher A.Bathymetry of trace fossils[J].Marine Geology,1967, 5: 413-428.
[4] Bromley R G, Ekdale A A. Chondrites: A trace fossil indicator of anoxia in sediments[J].Science, 1984, 224: 872-874.
[5] Bromley R G, Ekdale A A. Composite ichnofabrics and tiering of burrows[J]. Geological Magazine, 1986, 123 (1): 59-65.
[6] Ekdale A A, Mason T R. Characteristic trace fossil associations in oxygen-poor sedimentary environments[J].Geology, 1988, 16:720-723.
[7] Ekdale A A,Bromley R G. Analysis of composite ichnofabrics:An example in uppermost Cretaceous chalk of Denmark[J]. Palaios,1991,6:232-249.
[8] Savrda C E, Bottjer D J. Trace fossils model for reconstructingoxygenation histories ofancient marine bottom waters: Application to upper cretaceous Niobrara formation,Colorado[J].Palaeogeography Palaeoclimatology Palaeoecology,1989,74: 49-74.
[9] Savrda C E, Bottjer D J. Oxygen-related biofacies in marine strata: Overview and update[C]//Tyson R V, Pearson T H, eds.Modern and Ancient Continental Shelf Anoxia. Geological Society, London: Special Publication, 1991, 58: 201-219.
[10] Wetzel A. Ecologic interpretation of deep-sea trace fossil communities[J].Palaeogeography, Palaeoclimatology, Palaeoecology,1991, 85: 47-69.
[11] Gong Yiming, Droser M L.Periodic anxic shelf in the early-middle Ordovician transition:Ichnosedimentologyic evidence from west and central ATAH, USA[J].Journal of Palaeogeography,2002, 4(4):81-89[龚一鸣,Droser M L.早、中奥陶世之交陆架周期性缺氧:来自美国犹他州的遗迹沉积学证据[J].古地理学报,2002, 4(4):81-89.]
[12] Gong Yiming.Indicator facies significance and tiering dist ribution of Chondrites[J].Acta Palaeontologica Sinica,2004,43(1): 94-102.[龚一鸣.遗迹化石 Chondrites 的指相意义和阶层分布[J].古生物学报,2004,43(1): 94-102.]
[13] Savrda C E, Bottjer D J. Trace fossil model for reconstruction of paleooxygenation in bottomwaters[J].Geology,1986, 14: 3-6.[14] Yan Jiaxin, Zhang Haiqing. Paleo-oxygenation facies—A new research filed in sedimentary[J].Geological Science and Technology Information, 1996, 35(3):7-13.[颜佳新,张海清.古氧相——一个新的沉积学研究领域[J].地质科技情报,1996, 35(3):7-13.] [15] Yan Jiaxin, Chen Beiyue, Li Sitian,et al. Oxygen-related facies and sequence stratigraphy in the Qixia formation of the Hubei-Hunan-Guangxi region[J].Gelogical Review,1997, 43(2): 193-199.[颜佳新,陈北岳,李思田,等.鄂湘桂地区栖霞组古氧相分析与层序地层和海平面变化[J].地质论评,1997, 43(2): 193-199.]
[16] Jin Huijuan, Li Yuci, Fang Guoqing.Oxygen-dependent ichnocoenose in paleo-pelagic substrates[J].Acta Sedimentologica Sinica,2003, 23(1): 75-80.[晋慧娟,李育慈,方国庆.古代深海底质氧控的遗迹化石群落[J].沉积学报,2003, 23(1): 75-80.]
[17] Pruss S B, Botter D J. Early triassic trace fossils of western united states and their implications for prolonged environmental stress from the end-permian mass extinction[J].Palaios,2004, 19: 551-564.
[18] Watanabe S, Tada R, Ikehara K, et al. Sediment fabrics, oxygenation history, and circulation modes of Japan sea during the late Quaternary[J].Palaios,2007,247:50-64.
[19] Christopher D,Stanley A, Pickerill R K. Systematic ichnology of the late ordovician Georgian bay formation of southern Ontario,eastern Canada[J].Life Sciences Contributions (Royal Ontario Museum), 1998,162: 1-56.
[20] Young F G. Early Cambrian and older trace fossils from the southern Cordililera of Canada[J].Canadian Journal Earth Sciences,1972,9: 1-17.
[21] Droser M L, Bottjer D J. Trends in depth and extent of bioturbation in cambrian carbonate marine environments,western United states[J]. Geology, 1988,16: 233-236.
[22] Archer A W, Maples C G. Trace fossil distribution across a marine to nonmarine gradient in the Pennsylvanian of southwestern Indiana[J].Paleont,1984, 58: 448-466.
[23] McCann T, Pickerill R K. Flysch trace fossils from the cretaceous kodiak formation of Alaska[J].Paleont, 1988,62(3): 330-348.[24] Wignall P B. Black shales[M]. Oxford: Clarendon Press,1994.
[25] Yang Shipu. Early Devonian t race fossils f rom Liujing, Guangxi and their palaeoecological significance[J].Regional Geology of China, 1983,5:12-22.[杨式溥.广西横县六景早泥盆世遗迹化石极其古生态学意义[J].中国区域地质,1983,5:12-22.]
[26] Wang Yue, Shen Jianwei, Zhou Zhicheng. Ichnofacies and sequence stratigraphy of the lower devonian in the south Guizhou[J].Acta Micropalaeontologica Sinica,1997:14 (2): 203-213.[王约,沈建伟,周志澄. 黔南独山下、中泥盆统遗迹相与层序地层学研究[J]. 微体古生物学报,1997:14 (2): 203-213.]
[27] Chengdu Institute of Geology and Mineral Resources Chinese Academy of Gelogical Sciences.Devonian Stratigraphy, Paeontology and Sdementary Fcies of Longmenshan[M].Beijing: Geological PublishingHouse,1988:1-159.[中国地质科学院地质研究所,成都地质矿产研究所.四川龙门山地区泥盆纪地层古生物及沉积相[M].北京:地质出版社,1988:1-159]
[28] Wang Daren, Lin Zuwei, Zhang Xinping. Palaeoecology of the trilobite ichnocoenosis from the middle Devonian Yuntaiguan Formation in the western Hunan[J].Acta Palaeontologica Sinica,1988,1(1):48-58.[王大任,林祖蔚,张新平.湘西中泥盆世云台观组三叶虫遗迹群落的古生态[J].古生物学报,1988,1(1):48-58.]
[29] Gong Yiming. Trace fossils of early-middle devonian clastic formation in southwesten Hunan and their relation to sedimentary enviroments[J].Sedimentory Facies and Palaeogeography, 1989,6(5):26-32.[龚一鸣.湘西南早一中泥盆世碎屑岩地层遗迹化石与沉积环境的关系[J]. 岩相古地理文集,1989,6(5):26-32.]
[30] Zhang Xinping, Qing Shangkang. Upper Devonian trace fossils from Xinhua, Hunan and their sedimentary environments[J]. Petroleumand Gas Geology,1988, 9(3):252-260.[张新平,卿上康.湖南新化上泥盆统的遗迹化石及其沉积环境[J].石油与天然气地质,1988,9(3):252-260.]
[31] Yang Shipu, Hu Changming, Sun Chuanfang. Discovery of Late Devonian t race fossils from Guodingshan district, Hanyang, China and its significance[J].Earth Science—Journal of China University of Geosciences,1987, 12(1):1-8. [杨式溥,胡昌铭,孙传芳.汉阳锅顶山地区晚泥盆世遗迹化石的发现及其意义[J].地球科学——中国地质大学学报,1987,12(1):1-8.]
[32] Yang Shipu,Zhang Jianping,Yang Meifang, et al.Trace Fossil s of China[M].Beijing: Science Press,2004.[杨式溥, 张建平, 杨美芳,等.中国遗迹化石[M]. 北京:科学出版社,2004.]

[1] 赵文金,朱敏. 云南的早期脊椎动物化石研究[J]. 地球科学进展, 2003, 18(6): 863-869.
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