贵州西南部三叠系杨柳井组的时代CONODONT-BASED AGE OF THE TRIASSIC YANGLIUJING FORMATION IN SW GUIZHOU,CHINA
陈立德,王成源
摘要(Abstract):
贵州关岭一带的杨柳井组下部产安尼期与拉丁期界线附近的牙形刺Nicoraella kockeli(Tatge),Neogon-dolella constricta cornuta,Neog.constricta postcornuta,Neog.bulgarica,Neog.trammeri及Neog.alpinaalpina等;与匈牙利的Felsoors剖面相似,在该剖面上可以识别出Neogondolella constricta cornuta-Neog.constricta post-cornuta演化关系,据此推断,杨柳井组下部的时代为安尼晚期,杨柳井组上部的时代为拉丁期。牙形刺的发现为确定杨柳井组的时代提供了可靠的化石依据,并为该区安尼—拉丁期地层的划分和对比奠定了基础。
关键词(KeyWords): 牙形刺;生物地层;杨柳井组;安尼阶;拉丁阶;三叠系;关岭;贵州
基金项目(Foundation): 中国地质调查局“关岭生物群研究”项目(No.200113900072)
作者(Author): 陈立德,王成源
参考文献(References):
- 陈楚震,何国雄,陈金华,孙东立,王志浩.2000.海相三叠系.见:中国地层研究二十年(1979-1999).合肥:中国科技大学出版社.241—254
- 陈楚震,黎文本,马其鸿等.1979.西南地区的三叠系.见:西南地碳酸盐生物地层.北京:科学出版社.289—336
- 邓占球,孔磊.1984.黔南、滇东一带中三叠世石珊瑚和海绵.古生物学报,23(4):489—504
- 董卫平.1997.贵州省岩石地层.武汉:中国地质大学出版社.1—306
- 贵州省地质矿产局.1987.贵州省区域地质志.北京:地质出版社.277—321
- 何炎.1984.黔中、黔南中三叠世有孔虫的发现.古生物学报,23(4):420—431
- 王钰,陈楚震,陆麟黄.1963.贵州西南部三叠纪地层.见:黔南地层现场会议全国地层会议学术报告汇编.北京:科学出版社.99—167
- 王红梅,王兴理,李荣西,魏家庸,2005.贵州罗甸边阳关刀剖面三叠纪牙形刺序列及阶的划分.古生物学报,44(4):611—626
- 杨守仁,刘疆,张明发.1995.期贵州西南部"法郎组"牙形石及其时代,地层学杂志,19(3):161—170
- 杨守仁,郝维城,王新平.1999.中国三叠纪不同相区的牙形刺序列.见:八尾昭,江崎洋一,郝维城,王新平编.中国古特提斯生物及地质变迁.北京:北京大学出版社.97-112
- 殷鸿福.1962.贵州西南部三叠系生物地层问题。中国地质,42(2):289—306
- Bureau of Geology and Mineralresouces of Guizhou Province.1987.
- Regional Geology of Guizhou Province.Beijing:GeologicalPublishing House.277—321
- Chen Chu-zhen,He Guo-xiong,Chen Jin-hua,Song Dong-li&Wang Zhi-hao.2000.Marine Triassic.In:Stratigraphic Studiesin China(1979-1999).Hefei:Chinese Sciences and TechnologyUniversity Press.241—254
- Chen Chu-zheng,Li Wen-ben&Ma Qi-hong.1979.Triassic inSouthern China.In:Biostratigraphy of Li mestone in SouthernChina.Beijing:Science Press.289—336
- Deng Zhan-qiu&Kong Lei.1984.Middle Triassic corals and spon-ges fromsouthern Guizhou and eastern Yunnan.Acta Palaeon-tologica Sinica,23(4):489—504
- Dong Wei-ping.1997.Stratigraphy(lithostratic)of Guizhou Prov-ince.Wuhan:Chinese University Press.1—306
- He Yan.1984.Middle Triassic foraminifera fromcentral and centraland southern Guizhou,China.Acta Palaeontologica Sinica,23(4):420—431
- Kovàcs S.1994.Conodont stratigraphical i mportance fromthe Ani-sian/Ladinian boundaryinterval of the Balaton Highland,Hun-gary.Rivista Italianadi Paleontologiae Stratigrafia,99(4):473—514
- Wang Hong-mei,Wang Xing-li,Li Rong-xi&Wei Jia-yong.2005.Triassic conodont succession and stage subdivision of the Guan-dao section,Bianyang,Luodian,Guizhou.Acta PalaeontologicaSinica,44(4):611—626
- Wang Yu,Chen Chu-zhen&Lu Ling-huang.1963.Triassic Stratain Southwest Guizhou.In:On-the-spot meeting in strata ofSouth Guizhou.Beijing:Science Press.99—167
- Yang Shou-ren,Hao Wei-cheng&Wang Xing-ping.1999.Triassicconodont sequences fromdifferent faciesin China.In:Yao Aki-ra,Yoichi Ezaki,Hao Wei-cheng,Wang Xing-ping eds.Bioticand geological development and the Paleo-Tethys in China.Bei-jing:Peking University Press.97—112
- Yang Shou-ren,Liu Jiang&Zhang Ming-fa.1995.Conodonts fromthe“Falang Formation”of southwestern Guizhou andtheir age.Journal of Stratigraphy,19(3):161—170
- Yin Hong-fu.1962.The problems of Triassic biostratigraphyin SWGuizhou.Acta Geologica Sinica,42(2):289—306