豫西潭头盆地上白垩统秋扒组遗迹化石与沉积环境

王长征; 胡斌; 杨凯

豫西潭头盆地上白垩统秋扒组遗迹化石与沉积环境

王长征¹,
胡斌^1,2,
杨凯¹

1.
河南理工大学资源环境学院河南焦作 454000;
2.
河南省生物遗迹与成矿过程重点实验室河南焦作 454000

基金项目: 国家自然科学基金项目(批准号:41272117)资助

详细信息

作者简介:
王长征男 1979年生博士研究生讲师沉积学和遗迹学 E-mail: wangchangzheng@hpu.edu.cn

中图分类号: TE121.3⁺1

计量

文章访问数: 1054
HTML全文浏览量: 2
PDF下载量: 878
被引次数: 0

Ichnofossils and Sedimentary Environments of the Upper Cretaceous Qiupa Formation in Tantou Basin of Western Henan

1.
Institute of Resources and Environment, Henan Polytechnic University, Jiaozuo, Henan 454000;
2.
Key Laboratory of Biogenic Traces and Sedimentaty Minerals of Henan Province, Jiaozuo, Henan 454000

摘要

摘要: 豫西潭头盆地上白垩统秋扒组为一套陆相碎屑岩沉积,岩性主要为褐红色厚层状或块状的粉砂质泥岩夹多层不稳定的砾岩、砂砾岩或砂岩.本次工作在该组中发现了丰富的遗迹化石:Palaeophycus tubularis(管状古藻迹)、Beaconites autarcticus(南极似塔形迹)、Planolites ichnosp.1(漫游迹,未定种1)、Planolites ichnosp.2(漫游迹,未定种2)、Scoyenia gracilis(纤细斯柯茵迹)、Skolithos ichnosp.(石针迹,未定种)和Rhizoliths(根迹).根据遗迹化石的产状及其围岩的沉积特征,建立了Beaconites-Scoyenia遗迹组合和Palaeophycus -Rhizoliths遗迹组合,并提出了遗迹化石组合的沉积环境分布模式;基于岩性特征、沉积构造和遗迹化石组成特征的综合分析,划分出五种沉积序列类型.秋扒组形成于冲积扇、扇三角洲和湖泊沉积环境,自下而上经历了从冲积扇到扇三角洲再到湖泊的沉积环境演化过程.
- 潭头盆地 /
- 陆相沉积 /
- 遗迹化石 /
- 沉积环境
Abstract: The Upper Cretaceous Qiupa Formation in Tantou Basin of the western Henan province is a set of terrestrial clastic deposits. The lithology is mainly made up of thick-bedded or massive red brown silty mudstone in which intercalated beds are instability of graded bedding or massive gravel, sandy gravel or sandstone. Abundant ichnofossils were found in the strata, including Palaeophycus tubularis, Beaconites autarcticus, Planolites ichnosp.1, Planolites ichnosp.2, Scoyenia gracilis, Skolithos ichnosp., and Rhizoliths. According to the outcrop characteristics of these ichnofossils and the sedimentary features of their surrounding rocks, the Beaconites-Scoyenia ichnoassemblage and Palaeophycus-Rhizoliths ichnoassemblage were established and their sedimentary environmental models were proposed. The Beaconites-Scoyenia ichnoassemblage which is consisted of Beaconites antarcticus, Scoyenia gracilis, Planolites ichnosp.2 and Skolithos ichnosp represents the shore and shallow lacustrine sedimentary environments. The Palaeophycus-Rhizoliths ichnoassemblage which is consisted of Palaeophycus tubularis, Planolites ichnosp.1, Beaconites antarcticus and Rhizoliths represents the lacustrine fan-delta plain to fan-delta front sedimentary environments. Based on the comprehensive analysis of the lithology, sedimentary structures, sedimentary sequences and ichnofossil assemblages of the strata, 5 types of depositional sequences are differentiated and the Qiupa Formation is explained to have formed sequentially from the alluvial fan to lacustrine fan delta and then to shore and shallow lake environments.. In addition, the evolution of sedimentary environments represented in the formation is discussed. The research results not only may enrich the ichnofossil database of terrestrial basins in China and offer new data to complete further continental ichnofacies mode, but also offer scientific evidence to explain the palaeobios survival and preserved palaeoenvironments in Tantou basins of western Henan.
- Tantou Basin /
- terrestrial deposit /
- ichnofossil /
- sedimentary environment

HTML全文

参考文献(15)

[1]	周世全,冯祖杰,李占扬. 河南省白垩系—古近系界线划分初探[J]. 地层学杂志,2001,25:235-240 [Zhou Shiquan, Feng Zujie, Li Zhanyang. Study on the Cretaceous-Paleogene boundary of Henan province [J]. Journal of Stratigraphy, 2001, 25: 235-240]
[2]	王德有,冯进城,朱世刚,等. 中国河南恐龙蛋和恐龙化石[M]. 北京:地质出版社,2008:115-116 [Wang Deyou, Feng Jincheng, Zhu Shigang, et al. Dinosaur Eggs and Skeletons from Henan Province in China[M]. Beijing: Geological Publishing House, 2008:115-116]
[3]	江小均,柳永清,姬书安,等. 豫西栾川—潭头盆地含脊椎动物化石地层序列和K/T 界线初步研究[J]. 中国科学(D辑):地球科学,2011,41(5):738-744 [Jiang Xiaojun, Liu Yongqing, Ji Shu'an, et al. Dinosaur-bearing strata and K/T boundary in the Luanchuan-Tantou Basin of western Henan province, China[J]. Science China (Seri. D): Earth Science, 2011,41 (5): 738-744]
[4]	周世全,冯祖杰,张国建. 河南恐龙蛋化石组合类型及其地层时代意义[J]. 现代地质,2001,15(4):362-369 [Zhou Shiquan, Feng Zujie, Zhang Guojian. Oolithias assemblages in Henan province and its age significance[J]. Geoscience, 2001, 15(4): 362-369]
[5]	徐莉. 河南省恐龙化石科学特征及保护研究[D]. 北京:中国地质大学(北京),2007:1-120 [Xu Li. The scientific characters and protection of dinosaurs from Henan province[D]. Beijing: China University of Geosciences, 2007: 1-120]
[6]	张国成,郭卫星,曾玉凤. 河南西峡盆地上白垩统河流及湖泊沉积中的遗迹组构[J]. 古地理学报,2004,6(4):434-441 [Zhang Guocheng, Guo Weixing, Zeng Yufeng. Ichnofabric characteristics of fluvial and lacustrine sediments of the Upper Cretaceous in Xixia Basin, Henan province[J]. Journal of Palaeogeography, 2004, 6(4): 434-441]
[7]	胡斌,齐永安,张国成,等. 中国中—新生代陆相沉积中的遗迹群落[J]. 沉积学报,2002,20(4):574-581 [Hu Bin, Qi Yong'an, Zhang Guocheng, et al. The ichnocoenoses of Mesozoic-Cenozoic terrestrial deposits of China[J]. Acta Sedimentologica Sinica, 2002, 20(4): 574-581]
[8]	王德有. 河南省几个中生代地层问题的讨论[J]. 地质评论,2013,59(4):601-606[Wang Deyou. A discussion on some Mesozoic stratigraphic problems in Henan province[J]. Geological Review, 2013, 59(4): 601-606]
[9]	Lu Junchang, Xu Li, Zhang Xingliao, et al. New dromaeosaurid dinosaur from the Late Cretaceous Qiupa Formation of Luanchuan area, western Henan, China[J]. Geological Bulletin of China, 2007, 26(7): 777-786
[10]	贾松海,吕君昌,徐莉,等. 河南栗川晚白至世秋扒组甲龙类化石的发现及意义[J]. 地质通报,2010,29(4):483-487[Jia Songhai, Lü Junchang, Xu Li, et al. Discovery and significance of ankylosaur specimens from the Late Cretaceous Qiupa Formation in Luanchuan, Henan, China[J]. Geological Bulletin of China, 2010, 29(4): 483-487]
[11]	Lü J, Kobayashi Y, Lee Y, et al. A new vertebrate assemblage from the Late Cretaceous of Luanchuan, Henan Province, China [J]. J Vertbr Paleontol, 2008, 28: 108A
[12]	Keighley D G, Pickerill R K. The ichnotaxa Palaeophycus and Planolites: historical perspectives and recommendations[J]. Ichnos, 1995, 3: 301-309
[13]	Frey R W, Pemberton S G, Fagerstrom J A. Morphological, ethological and environmental significance of the ichnogenera Scoyenia and Ancorichnus[J]. Journal of Paleontology, 1984, 58(2): 511-528
[14]	Buatois L A, Mangano M G. Trace fossils from Carboniferous floodplain deposits in western Argentina: implication for ichnofacies models of continental environments[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2002, 183(1/2): 71-86
[15]	Buatois L A, Mangano M G. Trace fossil analysis of lacustrine facies and basins[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 1998, 140(1/2/3/4): 367-382

[1]	郭沫贞, 吕福亮, 邵大力, 侯福斗, 杨涛涛, 李东. 东爪哇盆地抱球虫灰岩遗迹化石及其沉积环境分析 . 沉积学报, 2021, 39(3): 713-722. doi: 10.14027/j.issn.1000-0550.2020.028
[2]	荆锡贵, 陈政安, 李凤杰, 文胜男, 谢胜军. 龙门山地区中泥盆统养马坝组风暴沉积中的遗迹化石及其环境意义 . 沉积学报, 2019, 37(4): 749-757. doi: 10.14027/j.issn.1000-0550.2018.170
[3]	赵曌, 张立军. 遗迹化石Rhizocorallium中莓状黄铁矿对古环境古生态的指示——以豫西南上泥盆统为例 . 沉积学报, 2017, 35(3): 480-488. doi: 10.14027/j.cnki.cjxb.2017.03.006
[4]	余关美, 时国. 贵阳地区下三叠统安顺组遗迹化石及古环境意义 . 沉积学报, 2016, 34(4): 626-633. doi: 10.14027/j.cnki.cjxb.2016.04.002
[5]	牛永斌, 单婷婷, 董小波, 周硕, 高文秀. 豫西北奥陶系马家沟组遗迹化石及其沉积环境 . 沉积学报, 2015, 33(2): 211-225. doi: 10.14027/j.cnki.cjxb.2015.02.001
[6]	. 柴达木盆地东北缘中新统遗迹化石组合及其沉积环境 . 沉积学报, 2013, 31(3): 413-420.
[7]	胡斌. 豫西济源地区早三叠世和尚沟组湖相遗迹化石及遗迹组构 . 沉积学报, 2009, 27(4): 573-582.
[8]	张喜林. 苏北盆地高邮凹陷古近系戴南组滨浅湖沉积中的遗迹化石 . 沉积学报, 2006, 24(1): 81-89.
[9]	刘志飞, 王成善, 金玮, 伊海生, 郑洪波, 赵西西, 李亚林. 青藏高原沱沱河盆地渐新—中新世沉积环境分析 . 沉积学报, 2005, 23(2): 210-217.
[10]	施振生, 朱筱敏, 王贵文, 钟大康, 张新培. 塔里木盆地塔中地区志留系塔塔埃尔塔格组潮坪沉积中的遗迹化石 . 沉积学报, 2005, 23(1): 91-98.
[11]	张国成, 曾玉凤, Buatois LA, Mangano MG. 济源盆地谭庄组(T_2-3)上段湖相沉积及遗迹化石特征 . 沉积学报, 2005, 23(1): 99-107.
[12]	方国庆, 刘德良. 塔里木盆地西北缘中奥陶统其浪组风暴岩中遗迹化石及其环境意义 . 沉积学报, 2000, 18(1): 68-72.
[13]	杨逢清, 熊伟. 四川省壤塘县金木达晚三叠世深水沉积中的遗迹化石及沉积环境分析 . 沉积学报, 2000, 18(1): 73-79.
[14]	邵磊, 李文厚, 袁明生. 吐鲁番—哈密盆地陆源碎屑沉积环境及物源分析 . 沉积学报, 1999, 17(3): 435-442.
[15]	田军, 龚一鸣, 梁斌, 黄继春. 东昆仑造山带二叠-三叠系遗迹化石及指相意义 . 沉积学报, 1999, 17(3): 361-366.
[16]	赖旭龙. 藏北中侏罗世遗迹化石Tisoa Serres的发现及其环境意义 . 沉积学报, 1998, 16(3): 1-5.
[17]	周志澄, 张瑛. 安徽巢县凤凰山和州组上段Glossifungites遗迹相的成因及其意义 . 沉积学报, 1991, 9(4): 120-127.
[18]	朱莲芳, 马宝林. 塔里木盆地阿克苏—柯坪地区寒武系—奥陶系的沉积环境 . 沉积学报, 1991, 9(2): 55-62.
[19]	沈志达, 曾羽, 梅冥相, 沈建. 康滇古陆东侧早奥陶世遗迹化且合及其指相意义 . 沉积学报, 1990, 8(3): 110-120.
[20]	杨式溥. 青海果洛、玉树地区二叠纪和三叠纪复理石相遗迹化石 . 沉积学报, 1988, 6(1): 1-12.

施引文献

资源附件(0)

访问统计

点击查看大图

计量

文章访问数: 1054
HTML全文浏览量: 2
PDF下载量: 878
被引次数: 0

姓名
邮箱
手机号码
标题
留言内容
验证码

留言板

豫西潭头盆地上白垩统秋扒组遗迹化石与沉积环境

作者简介:
王长征男 1979年生博士研究生讲师沉积学和遗迹学 E-mail: wangchangzheng@hpu.edu.cn

计量

Ichnofossils and Sedimentary Environments of the Upper Cretaceous Qiupa Formation in Tantou Basin of Western Henan

计量

目录

豫西潭头盆地上白垩统秋扒组遗迹化石与沉积环境

1. 河南理工大学资源环境学院河南焦作 454000;

2. 河南省生物遗迹与成矿过程重点实验室河南焦作 454000

作者简介:
王长征男 1979年生博士研究生讲师沉积学和遗迹学 E-mail: wangchangzheng@hpu.edu.cn

English Abstract

Ichnofossils and Sedimentary Environments of the Upper Cretaceous Qiupa Formation in Tantou Basin of Western Henan

1. Institute of Resources and Environment, Henan Polytechnic University, Jiaozuo, Henan 454000;

2. Key Laboratory of Biogenic Traces and Sedimentaty Minerals of Henan Province, Jiaozuo, Henan 454000

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

豫西潭头盆地上白垩统秋扒组遗迹化石与沉积环境

作者简介: 王长征 男 1979年生 博士研究生 讲师 沉积学和遗迹学 E-mail: wangchangzheng@hpu.edu.cn

计量

出版历程

Ichnofossils and Sedimentary Environments of the Upper Cretaceous Qiupa Formation in Tantou Basin of Western Henan

计量

出版历程

目录

豫西潭头盆地上白垩统秋扒组遗迹化石与沉积环境

1. 河南理工大学资源环境学院 河南焦作 454000; 2. 河南省生物遗迹与成矿过程重点实验室 河南焦作 454000

作者简介: 王长征 男 1979年生 博士研究生 讲师 沉积学和遗迹学 E-mail: wangchangzheng@hpu.edu.cn

English Abstract

Ichnofossils and Sedimentary Environments of the Upper Cretaceous Qiupa Formation in Tantou Basin of Western Henan

1. Institute of Resources and Environment, Henan Polytechnic University, Jiaozuo, Henan 454000; 2. Key Laboratory of Biogenic Traces and Sedimentaty Minerals of Henan Province, Jiaozuo, Henan 454000

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
王长征男 1979年生博士研究生讲师沉积学和遗迹学 E-mail: wangchangzheng@hpu.edu.cn

1. 河南理工大学资源环境学院河南焦作 454000;

2. 河南省生物遗迹与成矿过程重点实验室河南焦作 454000

作者简介:
王长征男 1979年生博士研究生讲师沉积学和遗迹学 E-mail: wangchangzheng@hpu.edu.cn

1. Institute of Resources and Environment, Henan Polytechnic University, Jiaozuo, Henan 454000;

2. Key Laboratory of Biogenic Traces and Sedimentaty Minerals of Henan Province, Jiaozuo, Henan 454000