Progress in the Planktonic Foraminiferal Biostratigraphy of the Neocene
Progress in the Planktonic Foraminiferal Biostratigraphy of the Neocene
复制标题
新新世浮游有孔虫生物地层学研究进展
作者：
F. T. Banner;W. H. Blow
UHH HNT 对浮游有孔虫（特别是 Globigerinacea）作为新近纪生物地层指标的价值的研究现已达到完善阶段，其中在中新世到近现代的区间内可以识别出 23 个区域。这些区域可以在世界环赤道地区的沉积物中找到，而且许多区域也被我们在温带地区直接识别出来。这些区域是通过检查委内瑞拉、哥伦比亚、
UHH HNT research into the value of planktonic foraminifera (particularly the Globigerinacea) as biostratigraphical indexes for the Neogene has now reached the stage of refinement wherein 23 zones may be recognized within the interval from the Miocene to the Recent. These zones may be identified in sediments of the circum-equatorial areas of the world, and many havo also been directly recognized by us in temperate areas. The zones have been established by the examination of the succession of fossil faunas in Venezuela, Colombia,