中国东部早第三纪介形虫化石组合及地层对比

张守安

doi:10.11743/ogg19890412

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中国东部早第三纪介形虫化石组合及地层对比
PALEOGENE OSTRACODA ASSEMBLAGES AND STRATIGRAPHIC CORRELATION OF THE MAIN DEPOSITIONAL BASINS IN EAST CHINA
1989年10卷第4期页码：426-438
网络首发：1989-12-25，

纸质出版：1989
DOI： 10.11743/ogg19890412
稿件说明：

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张守安. 中国东部早第三纪介形虫化石组合及地层对比[J]. 石油与天然气地质, 1989,10(4):426-438. DOI： 10.11743/ogg19890412.

Zhang Shouan. PALEOGENE OSTRACODA ASSEMBLAGES AND STRATIGRAPHIC CORRELATION OF THE MAIN DEPOSITIONAL BASINS IN EAST CHINA[J]. 1989, 10(4): 426-438. DOI： 10.11743/ogg19890412.

摘要

我国东部主要盆地早第三纪介形虫

可分为五个组合:上渐新统 Chinocythere unicus-pidata-Dongyingia-Cyprinotus-Cyprois 组合;下、中渐新统 Cyprinotus(Heterocypris)jingheensis-Pinnocypris-Austrocypris-Huabeinia-Chinocythere 组合;上始新统 Cyprinotusigneus-Echinocypris fabaeformis-Limnocythere jiangsuensis 组合;下始新统 Sinocyprisreticulata-Limnocythere weixianensis-Cypris decaryi 组合;上古新统 Sinocypris funing-ensis-Eucypris hengyangensis-Parailyocypris changzhouensis 组合;下古新统 Cypridea(Morinina)xindianensis-Porpocypris-Parailyocypris taizhouensis 组合。归纳为四个发展阶段:(1)中、新生代混生动物群阶段;(2)Sinocypris 动物群阶段;(3)Chinocythere动物群阶段;(4)Dongyingia 动物群阶段。

Abstract

This paper deals with palaeontologic characteristics of the main Paleogenedepositional basins in east China.Five assemblages and four evolution phasesof Ostracrda can be summarised.Five fossil assemblages:Upper Oligocene Chinocythere unicuspinata-Dongyingia-Cyprinotus-Cyprois Assemblage.Lower-Middle Oligocene Cyprinotus(Heterocypris)jingheensis-Pinnocypris-Austrocypris-Huabeinia-Chinocythere Assemblage.Upper Eocene Cyprinotus igneus-Echinocypris fabaeformis-Limnocythere jiang-suensis Assemblage.Lower Eocene Sinocypris reticulata-Limnocythere weixianensis-Cypris decaryi Assemblage.Upper Palaeocene Sinocypris funingensis-Eucypris hengyangensis-Parailyocypris changzhouensis Assemblage.Lower Palaeocene Cypridea(Morinina)xindianensis-Porpocypris-Parailyo-cypris taizhouensis Assemblage.Four major evolution phases:1.Meso-Cenozoic mixed fauna phase;2.Sinocypris fauna phase;3.Chinocythere fauna Phase;4.Dongyingia faunaphase.According to the contrast of Ostracod assemblages

a conclusion can bedrawn that the formation of Palaeogene depositional basins took place earlierin South China than in the North.