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。
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-CyproisAssemblage.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 decaryiAssemblage.Upper Palaeocene Sinocypris funingensis-Eucypris hengyangensis-Parailyocyprischangzhouensis 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.
出处
《石油与天然气地质》
EI
CAS
CSCD
北大核心
1989年第4期426-437,共12页
Oil & Gas Geology