中国上泥盆统阳朔阶牙形类生物地层研究(英文)CONODONT BIOSTRATIGRAPHY OF REGIONAL YANGSHUOAN STAGE(UPPER FAMENNIAN, DEVONIAN) IN CHINA
常君滢,韩淑朋,覃斌贤,郭文,Sven Hartenfels,宋俊俊,梁昆,殷保安,郄文昆
摘要(Abstract):
阳朔阶最早由殷保安于2008年提出,命名源自桂林市阳朔县,用以指代上泥盆统锡矿山阶与邵东阶之间的一个地方阶,大致相当于国际年代地层单位法门阶上部。阳朔阶底界以牙形类Palmatolepis rugosa trachytera的首次出现为定义,顶界则以有孔虫Eoendothyra regularis的首现为标志。阳朔阶典型剖面为广西桂林市铁山剖面,自下而上包括“五指山组”和融县组,形成于孤立碳酸盐岩台地边缘,以浅水相的内碎屑、鲕粒泥粒灰岩、粒泥灰岩和颗粒灰岩为特征,局部夹有少量黑色钙质泥岩。在桂林铁山剖面和邻近的小龙门剖面中共采集牙形样品149件,其中94件样品产丰富的牙形类分子,该牙形动物群以Palmatolepis、Neopolygnathus、Polygnathus、Pseudopolygnathus、Bispathodus、Icriodus、Rhodalepis、Mehlina和Branmehla属分子为特征,自下而上可识别出6个牙形类生物带,包括Pa. marginifera marginifera带、Pa. rugosa trachytera带、Pa. perlobata postera带、Pa. gracilis expansa带、Bi. costatus带和Bi. ultimus ultimus带,为环古特提斯洋地区法门阶地层对比提供了高精度的生物地层格架。基于详细的牙形类生物地层和沉积相分析,在铁山剖面Pa. rugosa trachytera带上部和Pa. gracilis expansa带顶部浅水相碳酸盐岩序列中识别出两次黑色富有机质沉积事件,对应于相对海平面快速上升和海洋贫氧,可能是法门期全球性Annulata和Dasberg事件在华南边缘海区的沉积响应。
关键词(KeyWords): 泥盆系;生物地层;桂林;牙形类;Annulata事件;Dasberg事件
基金项目(Foundation): financially supported by the Strategic Priority Research Program (B) of the Chinese Academy of Sciences (XDA0430202, XDB26000000);; the State Key Laboratory of Palaeobiology and Stratigraphy (Grant No. 20152102);; the Deep-time Digital Earth (DDE) Big Science Program~~
作者(Author): 常君滢,韩淑朋,覃斌贤,郭文,Sven Hartenfels,宋俊俊,梁昆,殷保安,郄文昆
DOI: 10.19839/j.cnki.dcxzz.2024.0003
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