{"title":"Silurian conodont biostratigraphy of the east-central Appalachian Basin (eastern USA): Re-examination of the C.T. Helfrich Collection","authors":"A. Bancroft, B. Cramer","doi":"10.3140/bull.geosci.1748","DOIUrl":null,"url":null,"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).","PeriodicalId":9332,"journal":{"name":"Bulletin of Geosciences","volume":"1 1","pages":"1-22"},"PeriodicalIF":1.5000,"publicationDate":"2020-03-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"6","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Bulletin of Geosciences","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.3140/bull.geosci.1748","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
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).
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.