Summary account of the Lower Ordovician (Arenig) graptolite biostratigraphy of the Cow Head Group, western Newfoundland

Cj T h e Cow H e a d G r o u p is an al lochthonous sequence of Middle Cambr ian to late Arenig sedimentary brec-cias, l imestones and shales deposi ted in a deep lower slope environment close to a continental margin. Im-bricate thrusting has resulted in repeated exposure of laterally equivalent &qu...

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Main Authors: S. Henry, Williams, Robert K. Stevens
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.555.480
http://2dgf.dk/xpdf/bull35_03-04-259-270.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.555.480 2023-05-15T17:22:43+02:00 Summary account of the Lower Ordovician (Arenig) graptolite biostratigraphy of the Cow Head Group, western Newfoundland S. Henry Williams Robert K. Stevens The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.555.480 http://2dgf.dk/xpdf/bull35_03-04-259-270.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.555.480 http://2dgf.dk/xpdf/bull35_03-04-259-270.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://2dgf.dk/xpdf/bull35_03-04-259-270.pdf text ftciteseerx 2016-01-08T11:45:26Z Cj T h e Cow H e a d G r o u p is an al lochthonous sequence of Middle Cambr ian to late Arenig sedimentary brec-cias, l imestones and shales deposi ted in a deep lower slope environment close to a continental margin. Im-bricate thrusting has resulted in repeated exposure of laterally equivalent "proximal " to "distal " facies which may be correlated using graptolitic control in the interbeds. "Proximal " sections a re characterised by massive, coarse breccias with in terbedded l imestones and green/dark grey shales. M o r e distal ex-posures have fewer and th inner breccias and l imestones, while the green/grey shales a re replaced pro-gressively by red, non-graptolit ic ones. Al though the succession is by no mean unbroken or comple te, it furnishes one of the best and most con-tinuously graptolitic sections through the Arenig. A new zonal scheme is erected for the Cow H e a d G r o u p, which could prove suitable as a new Nor th Amer ican s tandard. Fur the rmore, several l imestones and siliceous shales have yielded exquisitely preserved isolated mater ia l, permit t ing integration of fine growth detail with complete flattened specimens. With the exception of the uppermos t Arenig U. austrodentatus Z o n e, Arenig graptoloids possess a p ro-sicular origin for thl1. The earliest graptoloids with a metasicular origin for the first theca appear in this zone, including Undulograptus, Cryptograptus and Paraglossograptus. This interval, equivalent to Dal of the Australasian scheme, therefore represents a h i ther to unrecorded major evolutionary s tep in graptoli te evolution. Text Newfoundland Unknown Cow Head ENVELOPE(-57.832,-57.832,49.917,49.917)
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description Cj T h e Cow H e a d G r o u p is an al lochthonous sequence of Middle Cambr ian to late Arenig sedimentary brec-cias, l imestones and shales deposi ted in a deep lower slope environment close to a continental margin. Im-bricate thrusting has resulted in repeated exposure of laterally equivalent "proximal " to "distal " facies which may be correlated using graptolitic control in the interbeds. "Proximal " sections a re characterised by massive, coarse breccias with in terbedded l imestones and green/dark grey shales. M o r e distal ex-posures have fewer and th inner breccias and l imestones, while the green/grey shales a re replaced pro-gressively by red, non-graptolit ic ones. Al though the succession is by no mean unbroken or comple te, it furnishes one of the best and most con-tinuously graptolitic sections through the Arenig. A new zonal scheme is erected for the Cow H e a d G r o u p, which could prove suitable as a new Nor th Amer ican s tandard. Fur the rmore, several l imestones and siliceous shales have yielded exquisitely preserved isolated mater ia l, permit t ing integration of fine growth detail with complete flattened specimens. With the exception of the uppermos t Arenig U. austrodentatus Z o n e, Arenig graptoloids possess a p ro-sicular origin for thl1. The earliest graptoloids with a metasicular origin for the first theca appear in this zone, including Undulograptus, Cryptograptus and Paraglossograptus. This interval, equivalent to Dal of the Australasian scheme, therefore represents a h i ther to unrecorded major evolutionary s tep in graptoli te evolution.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author S. Henry
Williams
Robert K. Stevens
spellingShingle S. Henry
Williams
Robert K. Stevens
Summary account of the Lower Ordovician (Arenig) graptolite biostratigraphy of the Cow Head Group, western Newfoundland
author_facet S. Henry
Williams
Robert K. Stevens
author_sort S. Henry
title Summary account of the Lower Ordovician (Arenig) graptolite biostratigraphy of the Cow Head Group, western Newfoundland
title_short Summary account of the Lower Ordovician (Arenig) graptolite biostratigraphy of the Cow Head Group, western Newfoundland
title_full Summary account of the Lower Ordovician (Arenig) graptolite biostratigraphy of the Cow Head Group, western Newfoundland
title_fullStr Summary account of the Lower Ordovician (Arenig) graptolite biostratigraphy of the Cow Head Group, western Newfoundland
title_full_unstemmed Summary account of the Lower Ordovician (Arenig) graptolite biostratigraphy of the Cow Head Group, western Newfoundland
title_sort summary account of the lower ordovician (arenig) graptolite biostratigraphy of the cow head group, western newfoundland
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.555.480
http://2dgf.dk/xpdf/bull35_03-04-259-270.pdf
long_lat ENVELOPE(-57.832,-57.832,49.917,49.917)
geographic Cow Head
geographic_facet Cow Head
genre Newfoundland
genre_facet Newfoundland
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