乔治亚州斯screen和Burke县5个岩心下第三系沉积物的花粉生物地层学

Professional Paper Pub Date : 1900-01-01 DOI:10.3133/pp1603h
N. Frederiksen
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引用次数: 0

摘要

在佐治亚州斯克雷文和伯克县的5个测试孔(Millhaven, Girard, Thompson Oak, Millers Pond和McBean)中,对17个具有生物地层学意义的下第三系样品进行了花粉分类。埃伦顿组10个生物地层学上有用的样品,其最早和最晚的可能年龄分别为早古新世晚期和晚古新世晚期,但大部分或全部样品可能是早古新世晚期或晚古新世早期。斯纳普组的一个较好的样品年龄不超过古新世最早晚期,也不低于古新世中晚期。4个产样的花粉年代测定不太好,但可能的年代一般在始新世早期晚期到中始新世中期。三提石灰岩的两个样品的花粉年代在始新世晚期至中始新世(或更年轻?)之间。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Pollen biostratigraphy of Lower Tertiary sediments from five cores from Screven and Burke Counties, Georgia
Seventeen biostratigraphically useful lower Tertiary samples were examined for their pollen taxa from five test holes (Millhaven, Girard, Thompson Oak, Millers Pond, and McBean) in Screven and Burke Counties, Georgia. Ten biostratigraphically useful samples from the Ellenton Formation have earliest and latest possible ages of late early Paleocene and late Paleocene, respectively, but most or all of the samples are probably late early or early late Paleocene. One good sample from the Snapp Formation is no older than earliest late Paleocene and no younger than middle late Paleocene. Four productive samples from the Congaree Formation are not very well dated using pollen, but possible ages are generally from late early to middle middle Eocene. Two samples from the Santee Limestone are poorly dated from pollen within the late early Eocene to middle Eocene (or younger?) interval.
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