Introduction to papers on the Cambrian–Ordovician Boundary

Abstract The Working Group has the responsibility of recommending a specific level within a suitable stratigraphic section to serve as the global stratotype for the Cambrian–Ordovician Boundary. Commencing in 1974, comprehensive studies culminated in a plenary session in Calgary in 1985 resulting in...

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Published in:Geological Magazine
Main Author: Norford, B. S.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1988
Subjects:
Online Access:http://dx.doi.org/10.1017/s0016756800013005
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800013005
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spelling crcambridgeupr:10.1017/s0016756800013005 2024-09-15T18:19:59+00:00 Introduction to papers on the Cambrian–Ordovician Boundary Norford, B. S. 1988 http://dx.doi.org/10.1017/s0016756800013005 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800013005 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 125, issue 4, page 323-326 ISSN 0016-7568 1469-5081 journal-article 1988 crcambridgeupr https://doi.org/10.1017/s0016756800013005 2024-07-31T04:01:29Z Abstract The Working Group has the responsibility of recommending a specific level within a suitable stratigraphic section to serve as the global stratotype for the Cambrian–Ordovician Boundary. Commencing in 1974, comprehensive studies culminated in a plenary session in Calgary in 1985 resulting in decisions on the ‘golden-spike’ principle of selecting the boundary at a horizon just below the first influx of nematophorous graptolites. Conodonts are to be used as the primary guide for the selection of the specific horizon and the global stratotype section must have potential for studies using paleomagnetism, geochemistry and other non-biological correlation tools. The specific horizon will correspond approximately to the base of the Tremadoc Series of Wales and slightly higher than the base of Canadian Series as used in western North America. The Calgary meeting considered the Broom Point and Green Point sections in Newfoundland, Canada, and the Xiaoyangqiao section at Dayangcha, China, as prime candidates to serve as the global stratotype. A delegation from the Working Group inspected the Dayangcha sections in 1986. For this visit, comprehensive documentation and description of the sequence were prepared and published and are briefly summarized in the present issue. Specific uncertainties remain to be resolved for the Dayangcha and Newfoundland stratigraphic sections before the Working Group will be ready to recommend selection of a global stratotype. Article in Journal/Newspaper Newfoundland Cambridge University Press Geological Magazine 125 4 323 326
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description Abstract The Working Group has the responsibility of recommending a specific level within a suitable stratigraphic section to serve as the global stratotype for the Cambrian–Ordovician Boundary. Commencing in 1974, comprehensive studies culminated in a plenary session in Calgary in 1985 resulting in decisions on the ‘golden-spike’ principle of selecting the boundary at a horizon just below the first influx of nematophorous graptolites. Conodonts are to be used as the primary guide for the selection of the specific horizon and the global stratotype section must have potential for studies using paleomagnetism, geochemistry and other non-biological correlation tools. The specific horizon will correspond approximately to the base of the Tremadoc Series of Wales and slightly higher than the base of Canadian Series as used in western North America. The Calgary meeting considered the Broom Point and Green Point sections in Newfoundland, Canada, and the Xiaoyangqiao section at Dayangcha, China, as prime candidates to serve as the global stratotype. A delegation from the Working Group inspected the Dayangcha sections in 1986. For this visit, comprehensive documentation and description of the sequence were prepared and published and are briefly summarized in the present issue. Specific uncertainties remain to be resolved for the Dayangcha and Newfoundland stratigraphic sections before the Working Group will be ready to recommend selection of a global stratotype.
format Article in Journal/Newspaper
author Norford, B. S.
spellingShingle Norford, B. S.
Introduction to papers on the Cambrian–Ordovician Boundary
author_facet Norford, B. S.
author_sort Norford, B. S.
title Introduction to papers on the Cambrian–Ordovician Boundary
title_short Introduction to papers on the Cambrian–Ordovician Boundary
title_full Introduction to papers on the Cambrian–Ordovician Boundary
title_fullStr Introduction to papers on the Cambrian–Ordovician Boundary
title_full_unstemmed Introduction to papers on the Cambrian–Ordovician Boundary
title_sort introduction to papers on the cambrian–ordovician boundary
publisher Cambridge University Press (CUP)
publishDate 1988
url http://dx.doi.org/10.1017/s0016756800013005
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800013005
genre Newfoundland
genre_facet Newfoundland
op_source Geological Magazine
volume 125, issue 4, page 323-326
ISSN 0016-7568 1469-5081
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op_doi https://doi.org/10.1017/s0016756800013005
container_title Geological Magazine
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container_start_page 323
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