Silurian conodont biostratigraphy of the east-central Appalachian Basin (eastern USA): Re-examination of the C.T. Helfrich Collection

IF 1.5 3区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
A. Bancroft, B. Cramer
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引用次数: 6

Abstract

collection of conodonts from middle to upper Silurian (uppermost Llandovery–Pridoli series) strata in the Appa­ lachian Basin was produced by Charles T. Helfrich during the 1970’s. Most of the work was completed as part of his Ph.D. dissertation (Helfrich 1972) and published in a series of papers (Helfrich 1975, 1978, 1980) that laid the foundation for Silurian conodont biostratigraphy in the Appalachian Basin. In total, more than 15,000 spe­ cimens were recovered from six sections in the West Virgi nia, Virginia, and Maryland tri­state area, with which he established the conodont biozonation for the Silurian succession of the east­central Appalachian Mountains. Helfrich’s work was carried out at the dawn of a major transition in conodont systematics, from form taxonomy to multi­element taxonomy, and relied on the original Silurian conodont biozonation of Walliser (1964) to establish a biostratigraphic zonation for the Appalachian Basin consisting of eight zones for uppermost Llandovery through Pridoli strata. Most reported specimens were identified as form species, typically with tentative multi­ element species designations in open nomenclature. Silur­ ian conodont taxonomy and biostratigraphy have advanced tremendously in the intervening decades (e.g., Barrick & Klapper 1976; Bischoff 1986; Aldridge & Schönlaub 1989; Kleffner 1989, 1995; Nowlan 1995; Jeppsson 1997; Männik 1998, 2007; Corradini & Serpagli 1999; Jeppsson & Aldridge 2000; Calner & Jeppsson 2003; Murphy et al. 2004; Jeppsson et al. 2006; Carls et al. 2007; Slavík 2014; Corradini et al. 2015; Männik et al. 2015; Mathieson et al. 2016; Waid & Cramer 2017a, b), however, no modern systematic revision to the conodont biozonation of the uppermost Llandovery to Pridoli interval of the east­ central Appalachian Basin has been undertaken. Herein, we provide a modern and revised conodont biozonation for the central axis portion of the Appalachian Basin based upon the conodont collection of C.T. Helfrich (Helfrich 1972, 1975, 1980) that was re­examined by the authors at the University of Iowa from 2015–2018. The Helfrich collection is housed at the Museum of Geosciences at Virginia Tech (Virginia Polytechnic Institute and State University).
美国东部阿巴拉契亚盆地中东部志留系牙形石生物地层学:C.T. helrich Collection的再检验
Charles T.Helfrich于20世纪70年代在阿巴拉契亚盆地收集了志留系中上部(Llandovery-Pridoli系列最上部)的牙形刺。大部分工作是作为他的博士论文(Helfrich 1972)的一部分完成的,并发表在一系列论文中(Helfrich1975、1978、1980),为阿巴拉契亚盆地志留系牙形石生物地层学奠定了基础。在西弗吉尼亚州、弗吉尼亚州和马里兰州三州地区的六个地区,总共发现了15000多个牙形石,他据此建立了阿巴拉契亚山脉中东部志留纪序列的牙形石生物分带。Helfrich的工作是在牙形刺分类学从形态分类学到多元分类学的重大转变之初进行的,并依靠Walliser(1964)的原始志留纪牙形刺生物分带建立了阿巴拉契亚盆地的生物地层分带,该分带由最上层Llandovery至Pridoli地层的八个带组成。大多数报告的标本被鉴定为形态物种,通常在开放命名法中有暂定的多元素物种名称。志留纪牙形石分类学和生物地层学在这几十年里取得了巨大进步(例如,Barrick&Klapper 1976;Bischoff 1986;Aldridge&Schönlaub 1989;Kleffner 19891995;Nowlan 1995;Jeppsson 1997;Männik 19982007;Corradini&Serpagli 1999;Jeppsson&Aldridge 2000;Calner&Jeppsson 2003;Murphy等人2004;Jeppson等人2006;Carls等人2007;Slavík 2014;Corradii等人2015;Mánnik等人2015;Mathieson等人2016;Waid&Cramer 2017a,b),尚未对阿巴拉契亚盆地中东部最上部Llandovery至Pridoli区间的牙形石生物分带进行现代系统修订。在此,我们根据C.T.Helfrich(Helfrich 1972、1975、1980)的牙形刺集合,提供了阿巴拉契亚盆地中轴线部分的现代和修订的牙形齿生物分带,该集合由作者在爱荷华大学于2015年至2018年重新审查。Helfrich收藏在弗吉尼亚理工大学地球科学博物馆(弗吉尼亚理工学院和州立大学)。
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来源期刊
Bulletin of Geosciences
Bulletin of Geosciences 地学-地球科学综合
CiteScore
3.10
自引率
5.30%
发文量
18
审稿时长
>12 weeks
期刊介绍: The Bulletin of Geosciences is an international journal publishing original research papers, review articles, and short contributions concerning palaeoenvironmental geology, including palaeontology, stratigraphy, sedimentology, palaeogeography, palaeoecology, palaeoclimatology, geochemistry, mineralogy, geophysics, and related fields. All papers are subject to international peer review, and acceptance is based on quality alone.
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