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A note on the biostratigraphy of Paleocene-Eocene larger foraminifera from western Cuba

机译:古巴西部古新世-始新世较大有孔虫的生物地层学注释

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摘要

Larger foraminifera were collected from various Paleocene and Eocene localities in western Cuba. Included was a mea- sured section at San Francisco de Paula in Ciudad de la Habana Province in the Apolo and Capdevila Formations. This section spans the Paleocene/Eocene boundary and has been the focus of intensive biostratigraphic work. In this study, the stratigraphic occurrences of the Larger formainifera were correlated to biozoonations based on planktonic formainifera, calcareous nannofossils, radiolaria, and smaller benthic foraminifera already identified at San Francisco de Paula.
机译:从古巴西部的古新世和始新世地区收集到较大的有孔虫。其中包括在阿波罗岩层和卡普德维拉岩层的哈瓦那城省旧金山保拉测量区。该部分跨越了古新世/始新世的边界,一直是密集的生物地层学工作的重点。在这项研究中,大型浮游动物的地层发生与基于浮游性浮游动物,钙质纳米化石,放射虫和较小的底栖有孔虫的生物活动有关。

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