Author(s): Lin Jingxing
Pages: 16-36
Year: 1983 Issue:  1
Journal: Marine Geology & Quaternary Geology
Keyword:  回回; 同气; 上工; 回叫; 口才; 山口;
Abstract: <正> Quaternary foraminiferal faunas in China fall into five distinct categories according to palaeo-ecologicafeatures,namely:1.Palaeo-Bohai foraminiferal fauna2.Early Pleistocene foraminiferal fauna in Beijing-Shunyi3.Palaeo-epicontinental foraminiferal fauna4.Palaeo-East China Sea foraminiferal fauna5.Palaeo-South China Sea foraminiferal faunaBy correlating world zoogeographical zones of planktonic foraminifera and analysing the diversity in Quaternary foraminifera and ostracoda found in the North China Plain,it is possible to plot a graph of changes inpalaeo-climate since the Quaternary period.Palaeo-ecological studies of Holocene foraminifera on the Fujianseaboard in southern China showed that Holocene foraminifera can be broken down into three climatic phases.The findings of these studies providea a basis for discusssion of the palaeo-geographic variations occurted inthe Palaeo-Bohai,the Palaeo-East China Sea and the Palaeo-South China Sea.On the basis of the distributionof standard foraminifera in time