摘要
1963—1964年,在陕西蓝田第四纪地层内发现了猿人化石,吴汝康(1964、1966)命名为蓝田猿人。化石采自两个不同的地点:头盖骨、上颌骨及3颗牙齿产于公王岭(34°11′06″N,109°29′22″E),下颌骨则采自陈家窝(34°14′05″,109°15′07″E)。
On the basis of work on the Lantian Quaternary Stratigraphy and the application of sedimento-, bio-, magneto-, and astroclimatostratigraphy, Gongwangling fauna is middle Matuyama reversed epoch in age (i.e.0.96-1.4 m.y.B.P.), and Chenjiawo fauna is early Brunhes normal epoch in age.In fact, there exist relations among these disciplines mentioned above, and more and more scientists of insight have realized that multidisciplinary and interdisciplinary studies, such as climatostratigraphy, should be given serious consideration.A synthetical or comprehensive study of cosmos, earth, and life science is very important: for the develop ment of Quaternary Stratigraphy.
出处
《地层学杂志》
CSCD
北大核心
1990年第1期76-80,共5页
Journal of Stratigraphy
