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Upper Paleocene-lower Eocene radiolarian biostratigraphy of the San Francisco de Paula section, western Cuba: Regional and global comparisons

机译:古巴西部圣弗朗西斯科·德·保拉剖面的上古新世-始新世-下新世放射虫生物地层学:区域和全球比较

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In response to a growing need to define the Paleocene/Eocene boundary and record the events which imediately pre- ceded and followed it within a 5 my span, the San francisco de Paula section of western Cuba was evaluated for its potential as a bound- ary stratotype. Radiolarians, reported in previous studies by Cuban geologists as a major component of the faunal assemblages in this section, have been recollected and reanalyzed to determine their stratigraphic utility for recognition of the Paleocene/Eocene boundary in Cuba. On the basis of this and other recent microfossil studies of the San Francisco de Paula section, it is now known that the Paleocene/Eocene boundary in this succession is within an unconformity. Its placement herein is based on the highest occurrence of the Planktonic foraminifera Morozovella velascoensis (Fernandez-Rodriguez et al. 1999, this volume).
机译:为了满足日益增长的定义古新世/始新世边界并记录在5 my span范围内之前和随后发生的事件的需要,对古巴西部的San Paul franca de Paula部分进行了评估,以作为边界层型。古巴地质学家在先前的研究中报告说,放射线虫是本节动物群的主要组成部分,现已对其进行了重新收集和分析,以确定其地层学用途,以识别古巴的古新世/始新世边界。根据对San Francisco de Paula断层的这种微化石研究以及最近的其他微化石研究,现在知道该序列中的古新世/始新世边界是不整合的。它在此处的放置是基于浮游有孔虫veozcoensis的最高发生率(Fernandez-Rodriguez等,1999,此卷)。

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