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首页> 外文期刊>The Mountain Geologist >A New Reference Section for Palynostratigraphic Zonation of Paleocene Rocks in the Rocky Mountain Region
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A New Reference Section for Palynostratigraphic Zonation of Paleocene Rocks in the Rocky Mountain Region

机译:落基山地区古新世岩石古地层划分新的参考剖面

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摘要

A biostratigraphic (palynostratigraphic) zonation of Paleocene rocks was established in the northeastern Wind River Basin near Waltman, Natrona County, Wyoming, in 1978 and subsequently applied extensively by various workers throughout the Rocky Mountain region. Because the original study on which the zonation was based was proprietary, precise details about the locations of the two reference sections and the samples on which the zonation was based were not published and are no longer retrievable. Therefore, it is useful (although not required) to designate formally a new reference section for the Paleocene biozones. Accordingly, exposures of Paleocene and associated strata -within and west of the Castle Gardens Petroglyph Site in Fremont County, Wyoming, in the east-central part of the Wind River Basin, were selected for this purpose. At this location, composite stratigraphic sections encompassing 740 m of strata were measured, described, and sampled. Productive samples yielded characteristic Maastrichtian palynomorphs from the lower part of the sampled interval and diagnostic species of the six palynological biozones zones widely known as PI (lower Paleocene) through P6 (upper Paleocene), through an interval of about 580 m. The Paleocene biozones are present in the same consistent stratigraphic order in the Castle Gardens area as obseived in the 1978 study and subsequent studies throughout the Rocky Mountain region. In accordance with the North American Stratigraphic Code, the historical background is presented; intent to establish the Castle Gardens reference section is declared; the categoiy, rank, and formal names of Liiostratigraphic units within it are specified; and the features of the biozonation are described, including biozone boundaries, ages, and regional relations. Occurrences of biostratigraphically significant palynological species within each biozone in the reference section are tabulated, and presence of these and other species in correlative biozones are discussed. The new reference section in the Castle Gardens area replaces the original reference sections near Waltman and provides a better-documented foundation for Paleocene palynostratigraphy in the Rocky Mountain region.
机译:1978年在怀俄明州纳特罗纳县沃尔特曼附近的东北风河盆地建立了古新世岩石的生物地层(古地层)分区,随后在落基山地区的许多工人中得到了广泛应用。由于基于分区的原始研究是专有的,因此有关两个参考部分的位置以及分区所基于的样本的精确详细信息尚未发布,并且不再可检索。因此,有用的(尽管不是必需的)正式指定古新生物区的新参考部分。因此,为此选择了怀俄明州弗里蒙特县城堡花园岩画遗址内和以西的古新世及其相关地层的暴露。在该位置,测量,描述和采样了包含740 m地层的复合地层剖面。生产性样品从采样间隔的下部和六个古生物学区的诊断物种产生了特征性的马斯特里奇形态,被广泛称为PI(下古新世)至P6(上古新世),间隔约580 m。古新世生物带在城堡花园地区的地层顺序一致,与1978年的研究及随后在整个落基山地区的研究中所观察到的一致。根据北美地层法,介绍了历史背景;宣布建立城堡花园参考部分的意图;指定其中的地层单位的类别,等级和正式名称;描述了生物分区的特征,包括生物分区的边界,年龄和区域关系。将参考部分中每个生物区内生物地层学意义重大的古生物学物种的发生情况制成表格,并讨论了相关生物区内这些物种及其他物种的存在。城堡花园区域中的新参考部分替代了沃尔特曼附近的原始参考部分,并为落基山脉地区的古新世古地层学提供了文献更丰富的基础。

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