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    岐口凹陷新近系生物-遗迹相及环境解释

    刘彦博 严德天 王华 卢宗盛 喻建新

    刘彦博, 严德天, 王华, 卢宗盛, 喻建新, 2009. 岐口凹陷新近系生物-遗迹相及环境解释. 地球科学, 34(3): 412-418.
    引用本文: 刘彦博, 严德天, 王华, 卢宗盛, 喻建新, 2009. 岐口凹陷新近系生物-遗迹相及环境解释. 地球科学, 34(3): 412-418.
    LIU Yan-bo, YAN De-tian, WANG Hua, LU Zong-sheng, YU Jian-xin, 2009. Biofacies and Ichnofacies of Neogene in the Qikou Depression and Their Environmental Interpretation. Earth Science, 34(3): 412-418.
    Citation: LIU Yan-bo, YAN De-tian, WANG Hua, LU Zong-sheng, YU Jian-xin, 2009. Biofacies and Ichnofacies of Neogene in the Qikou Depression and Their Environmental Interpretation. Earth Science, 34(3): 412-418.

    岐口凹陷新近系生物-遗迹相及环境解释

    基金项目: 

    国家自然科学基金 40872077

    湖北省自然科学重点基金 2008CDA098

    详细信息
      作者简介:

      刘彦博(1970-)‚男‚副研究员‚主要从事应用沉积学、高等教育管理方面的研究.E-mail: liuyanbo@cug.edu.cn

    • 中图分类号: P588.2;P618

    Biofacies and Ichnofacies of Neogene in the Qikou Depression and Their Environmental Interpretation

    • 摘要: 岐口凹陷新近系包括明化镇组和馆陶组.通过新近系中的孢粉、介形虫和遗迹组构的系统研究, 识别出孢粉53个属种, 并建立了两个孢粉组合, 分别为Magnastites (粗肋孢) -Ulmus (榆粉) -Taxodiaceae pollenites (杉粉) 组合和Polygonaceae-Chenopodiaceae组合; 发现介形虫12个属种, 介形类以金星介科分子为主, 少数湖花介科分子, 以壳形单一、壳壁薄、表面光滑的类型为主, 表现了典型的非海相淡水介形类面貌; 划分出4种遗迹组构类型, 分别为Scoyenia遗迹组构、Skolithos遗迹组构、Palaeophycus遗迹组构和强扰动组构.在此基础上, 探索了生物与环境的关系, 划分了A、B、C、D、E5种生物-遗迹相带, 分别代表泛滥平原、蓄水注地或泛滥平原小型湖、河道及水下分流河道边部、滨浅湖和前三角洲沉积环境.

       

    • 图  1  黄骅坳陷区域构造及研究区位置

      Fig.  1.  The location and tectonic map of Huanghua depression

      图  2  岐口凹陷新近系典型孢粉化石属种

      1.Toroisporis sp.托弟蕨孢(未定种); 2、3.Taxodiaceae pollenites hiatus破隙杉粉; 4、5.Gothenpollenites sp.高腾粉(未定种); 6.Quercoidites minutus小栎粉; 7.Q. henrici亨氏栎粉; 8.Rutaceoidites sp.芸香粉(未定粉); 9.Rhoipites sp.漆树粉(未定种); 10.Trapa菱属; 11.Alnipollenites sp.桤木粉(未定种); 12.Chenopodipollis sp.藜粉(未定种); 13.Campenia sp. 1褶皱藻(未定种1);14.Momipites coryloides拟榛粉; 15.Juglanspollenites sp.胡桃粉(未定种); 16.Liquidambardites sp.枫香粉(未定种); 17.Tricolpites sp.三沟粉(未定种); 18.Campenia sp. 2褶皱藻(未定种2);19.Pterocarya pollenites sp.枫杨粉(未定种); 20.Caryapollenites triangular三角山核桃粉; 21.Salixipollenites sp.柳粉(未定种); 22.Ulmipollenites minor小榆粉; 23、28.Leiosphaeridium sp.光面球藻(未定种); 24、26、27.Pinuspollenites sp. 1双束松粉(未定种1);25.Pinuspollenites sp. 2双束松粉(未定种2).所有化石均放大800倍

      Fig.  2.  The representative genus of Neogene sporopollen in the Qikou depression

      图  3  岐口凹陷新近系典型介形虫属种

      1.Candona planus; 2.Darwinuda exils; 3.Limnocythere sp.1;4.Limnocythere sp.2;5、6.Mediocypris gudavensis; 7.Ilyocypris salebrosa stepanaiys; 8、9.Ilyocypris gudavensis; 10.Mediocypris gudavensis; 11.Ilyocpris subdunschanesis; 12、14.Metacypris datongensis; 13.Cyprinotus chiuhsiensis.所有化石均放大60倍

      Fig.  3.  The representative genus of Neogene ostracod in the Qikou depression

      图  4  岐口凹陷新近系岩心遗迹相特征

      a.Cylindricum(圆柱迹), 港深63-1井, 1 448.9 m; b.Skolithos(石针迹的横断面), 庄浅6井, 1 663.5 m; c.Palaeophycus(丛藻迹), 港92井, 1 731.0 m; d.生物扰动构造, 港深64-1井, 1 560.5 m

      Fig.  4.  Characteristics of Neogene ichnofabrics in the Qikou depression

      图  5  岐口凹陷新近系遗迹组构特点素描

      a.Scoyenia遗迹组构; b.Skolithos遗迹组构; c.Palaeophycus遗迹组构; d.强扰动组构

      Fig.  5.  The sketch map of Neogene ichnofabric characteristics in the Qikou depression

      图  6  岐口凹陷新近系生物相分布的环境模式

      DC.分流河道; VCS.决口扇; LB.分流河道边部; SCH.水下分流河道; SOB.水下分流河道边部; MB.分流河口坝; PDM.前三角洲; OL.浅湖; PL.泛滥平原小型湖

      Fig.  6.  The environment model of Neogene biofacies in the Qikou depression

    • [1] Ekdale, A.A., 1985. Palecology of the marine endobenthos. Palaeogeogr. Palaeocli matol. Palaeoecol. , 50(1): 63-81. doi: 10.1016/S0031-0182(85)80006-7
      [2] Ekdale, A.A., Berger, W.H., 1978. Deep sea ichnofacies: Modern organismtraces on andin Pelagic Carbonates of the western equatorial Pacific. Palaeogeogr. Palaeocli-matol. Palaeoecol. , 23(3-4): 263-278. http://www.onacademic.com/detail/journal_1000035325910010_eb49.html
      [3] Hu, B., Jiang, Z.X., Qi, Y.A., et al., 2006. Trace fossils ofdeeper lacustrine deposits in the Paleogene Shahejie Formation of Jiyang depression, Shandong Province, eastern China. Acta Palaeontologica Sinica, 45(1): 83-94(in Chinese with English abstract). http://europepmc.org/abstract/CBA/606102
      [4] Ji, L.M., Wang, S.F., Xu, J.L., 2006. Acritarch assemblage in Yanchang Formation in eastern Gansu Province and its environmental implications. Earth Science-Journalof China University of Geosciences, 31(6): 798-806(in Chinese with English abtract). doi: 10.1007/s11442-006-0415-5
      [5] Kern, J.P., 1980. Origin of trace fossils in Polish Carpathian flysch. Lethaia, 13(4): 347-362. doi: 10.1111/j.1502-3931.1980.tb01061.x
      [6] Ksiazkiewicz, M., 1975. Bathymetry of the Carpathian flysch basin. Acta Geol. Polonica., 25: 3-17. http://www.researchgate.net/publication/285436259_Bathymetry_of_the_Carpathian_Flysch_Basin
      [7] Li, S.T., 2004. Basin geodynamics background of formation of huge petroleum systems. Earth Science-Journal of China University of Geosciences, 29(5): 505-512(inChinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX200405000.htm
      [8] Lu, Z.S., Hao, C.K., Ma, H.B., et al., 2003. Continental ichnofabric types in the Liaohe oilfield and their environmental interpretation, China. Acta Geologica Sinica, 77(1): 9-15(in Chinese with English abstract). http://www.researchgate.net/publication/286959524_Continental_ichnofabric_types_in_the_Liaohe_Oilfield_and_their_environmental_interpretation_China
      [9] Mi, L.J., Bi, L.G., Gong, S.L., et al., 2004. Direct evidence for development of Bohai paleolake during the Neogene. Marine Geology & Quaternary Geology, 24(2): 37-42(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HYDZ200402006.htm
      [10] Pruss, S.B., Botter, D.J., 2004. Early Triassic trace fossils of the western United States and their implications for prolonged environmental stress from the end Permianmass extinction. Palaios, 19(6): 551-564. doi: 10.1669/0883-1351(2004)019<0551:ETTFOT>2.0.CO;2
      [11] Seilacher, A., 1964. Sedimentological classification and nomenclature of trace fossils. Sedimentology, 3: 253-256. doi: 10.1111/j.1365-3091.1964.tb00464.x
      [12] Seilacher, A., 1967. Bathymetry of trace fossils. Marine Geology, 5(5-6): 413-428. doi: 10.1016/0025-3227(67)90051-5
      [13] Taylor, A.A., Goldring, G.R., 1993. Description and analysis of bioturbation and chnofabric. Jour. of the Geol. Soc. , 150: 141-148. doi: 10.1144/gsjgs.150.1.0141
      [14] Wang, D.F., 1987. Sedimentary facies and sedimentary environments of Tertiary in the Huanghua depression. Geological Publishing House, Beijing (in Chinese).
      [15] Wang, H.F., Hu, B., Zhang, G.L., et al., 2005. Discovery and significance of Paleodictyon of Paleogene in Dongying sag. Xinjiang Petroleum Geology, 26(4): 404-407(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-XJSD200504020.htm
      [16] Wang, K.F., Zhang, Y.L., Jiang, H., et al., 1981. Discovery of pediastrum assemblage from submarine peat bed in the East China Sea and its implication in sea level changes of the latest Pleistocene. Chinese Science Bulletin, 2: 109-112(in Chinese). http://www.cqvip.com/QK/86894X/198106/74888487495756494854484950.html
      [17] Wetzel, A., 1991. Ecologic interpretation of deep sea trace fossil communities. Palaeogeogr. Palaeoclimatol. Palaeoecol. , 85(1-2): 47-69. doi: 10.1016/0031-0182(91)90025-M
      [18] Wetzel, A., Werner, F., 1981. Morphology and ecological significance of Zoophycos in deep sea sediments of NW Africa. Palaeogeogr. Palaeoclimatol. Palaeoecol. , 32(3-4): 185-212. http://earth.unibas.ch/sedi/Publications%20pdf/1981%20Wetzel%20Werner%20Zoophycos%20Palaeo-3%2032.pdf
      [19] Xu, J.L., Zhu, Y.H., 1993. Application of phytoplanktonic microfossils in paleoli mnology. China Ocean Press, Beijing, 117-191(in Chinese).
      [20] Yang, C.Y., 2003. Exploration realm and strategy analysis for Dagang exploration area. China Petroleum Exploration, 8(2): 13-17(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KTSY200302002.htm
      [21] 胡斌, 姜在兴, 齐永安, 等, 2006. 山东济阳坳陷古近系沙河街组深水湖沉积中的遗迹化石. 古生物学报, 45(1): 83-94. doi: 10.3969/j.issn.0001-6616.2006.01.008
      [22] 吉利明, 王少飞, 徐金鲤, 2006. 陇东地区延长组疑源类组合特征及其古环境意义. 地球科学--中国地质大学学报, 31(6): 798-806. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200606007.htm
      [23] 李思田, 2004. 大型油气系统形成的盆地动力学背景. 地球科学--中国地质大学学报, 29(5): 505-512. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200405000.htm
      [24] 卢宗盛, 郝朝坤, 马宏斌, 等, 2003. 辽河油田陆相遗迹组构类型及其环境解释. 地质学报, 77(1): 9-15. doi: 10.3321/j.issn:0001-5717.2003.01.002
      [25] 米立军, 毕力刚, 龚胜利, 等, 2004. 渤海新近纪古湖发育的直接证据. 海洋地质与第四纪地质, 24(2): 37-42. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200402006.htm
      [26] 王德发, 1987. 黄骅坳陷第三系沉积相及沉积环境. 北京: 地质出版社.
      [27] 王海方, 胡斌, 张关龙, 等, 2005. 东营凹陷古近系Paleodictyon遗迹化石的发现及意义. 新疆石油地质, 26(4): 404-407. doi: 10.3969/j.issn.1001-3873.2005.04.018
      [28] 王开发, 张玉兰, 蒋辉, 等, 1981. 东海海底泥炭层盘星藻组合的发现与晚更新世晚期的海平面变化. 科学通报, 2: 109-112. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB198102011.htm
      [29] 徐金鲤, 祝幼华, 1993. 微体浮游植物化石在古湖泊研究中的应用. 北京: 海洋出版社, 117-191.
      [30] 杨池银, 2003. 大港探区勘探领域及对策分析. 中国石油勘探, 8(2): 13-17. doi: 10.3969/j.issn.1672-7703.2003.02.002
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    • 收稿日期:  2008-10-24
    • 刊出日期:  2009-05-25

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