江西上高龙潭期牙形刺的发现——兼论Galowayinela的时代  

The Discovery of the Longtanian Conodonts from Qibaoshan, Shanggao County,Jiangxi,and Discussion on Gallowayinella Time

作　　者：朱相水[1,2] 林联盛 胡忠[1,2] 

机构地区：[1]江西师范大学环境资源科学系 [2]江西省遥感信息系统中心

出　　处：《江西师范大学学报（自然科学版）》1997年第2期174-177,共4页Journal of Jiangxi Normal University(Natural Science Edition)

摘　　要：江西上高七宝山龙潭组中近年发现了一些牙形刺，为确定该组中产出的Ｇａｌｌｏｗａｙｉｎｅｌａ的地质年代提供了补充依据．按照牙形刺、菊石等动物化石的组合特征及垂直分布。In recent years,some conodonts have been found Longtan Formation at Shanggao county,Jiangxi.It was provided some additional scientific basis for geological time of Longtan Formation and Fusulinida Gallowayinella which yielded in it .In accordance with the association featurs and vertical distribution of the fauna of conodont,ammonoites,and so on,the author believe that the age of Gallowayinella occured in Longtan Formation at Qibaoshan region should be belong to the Longtanian(equal to the Wuchiapingian).

关 键 词：牙形刺 菊石 Gallowayinella 江西 TING 化石 

分 类 号：Q915.725.6[天文地球—古生物学与地层学]