Acritarchs from the Lower Palaeozoic succession on the south County Wexford coast, Ireland: new age constraints for the Cullenstown Formation and the Cahore and Ribband Groups

Abstract Lower Palaeozoic sediments crop out on the southern coast of County Wexford, Ireland, comprising three distinctive lithostratigraphical units: from west to east the Cahore Group, the Blackhall Formation of the Ribband Group and the Cullenstown Formation. The three units are largely devoid o...

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Published in:Geological Journal
Main Authors: Brück, P. M., Vanguestaine, M.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2004
Subjects:
Online Access:http://dx.doi.org/10.1002/gj.966
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spelling crwiley:10.1002/gj.966 2024-06-02T08:10:45+00:00 Acritarchs from the Lower Palaeozoic succession on the south County Wexford coast, Ireland: new age constraints for the Cullenstown Formation and the Cahore and Ribband Groups Brück, P. M. Vanguestaine, M. 2004 http://dx.doi.org/10.1002/gj.966 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fgj.966 https://onlinelibrary.wiley.com/doi/pdf/10.1002/gj.966 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Geological Journal volume 39, issue 2, page 199-224 ISSN 0072-1050 1099-1034 journal-article 2004 crwiley https://doi.org/10.1002/gj.966 2024-05-03T11:34:57Z Abstract Lower Palaeozoic sediments crop out on the southern coast of County Wexford, Ireland, comprising three distinctive lithostratigraphical units: from west to east the Cahore Group, the Blackhall Formation of the Ribband Group and the Cullenstown Formation. The three units are largely devoid of macrofossils and thus their ages have to date been uncertain and, in the case of the Cullenstown Formation, speculative. In the Cahore Group, a diverse assemblage of acritarchs composed of seventeen species has been recorded indicating a middle Early Cambrian age. This is similar to the age of the lithologically identical Bray Group to the north, in County Wicklow. In the Ribband Group, two very distinct assemblages have been noted. Both are poorly preserved, but diagnostic species have been determined giving a biostratigrapical range of early Mid‐Cambrian to Llanvirn. Palynomorphs have been recorded for the first time from the Cullenstown Formation allowing comparison with eastern Newfoundland where a similar, less diverse assemblage has been recorded. The age indicated is latest Mid‐Cambrian to early Late Cambrian. Overall, despite generally poor preservation of the organic matter, some 45 acritarch species have been distinguished, among which one new combination is proposed: Retisphaeridium postae instead of Cymatiosphaera postae . Copyright © 2004 John Wiley & Sons, Ltd. Article in Journal/Newspaper Newfoundland Wiley Online Library Bray ENVELOPE(-114.067,-114.067,-74.833,-74.833) Geological Journal 39 2 199 224
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language English
description Abstract Lower Palaeozoic sediments crop out on the southern coast of County Wexford, Ireland, comprising three distinctive lithostratigraphical units: from west to east the Cahore Group, the Blackhall Formation of the Ribband Group and the Cullenstown Formation. The three units are largely devoid of macrofossils and thus their ages have to date been uncertain and, in the case of the Cullenstown Formation, speculative. In the Cahore Group, a diverse assemblage of acritarchs composed of seventeen species has been recorded indicating a middle Early Cambrian age. This is similar to the age of the lithologically identical Bray Group to the north, in County Wicklow. In the Ribband Group, two very distinct assemblages have been noted. Both are poorly preserved, but diagnostic species have been determined giving a biostratigrapical range of early Mid‐Cambrian to Llanvirn. Palynomorphs have been recorded for the first time from the Cullenstown Formation allowing comparison with eastern Newfoundland where a similar, less diverse assemblage has been recorded. The age indicated is latest Mid‐Cambrian to early Late Cambrian. Overall, despite generally poor preservation of the organic matter, some 45 acritarch species have been distinguished, among which one new combination is proposed: Retisphaeridium postae instead of Cymatiosphaera postae . Copyright © 2004 John Wiley & Sons, Ltd.
format Article in Journal/Newspaper
author Brück, P. M.
Vanguestaine, M.
spellingShingle Brück, P. M.
Vanguestaine, M.
Acritarchs from the Lower Palaeozoic succession on the south County Wexford coast, Ireland: new age constraints for the Cullenstown Formation and the Cahore and Ribband Groups
author_facet Brück, P. M.
Vanguestaine, M.
author_sort Brück, P. M.
title Acritarchs from the Lower Palaeozoic succession on the south County Wexford coast, Ireland: new age constraints for the Cullenstown Formation and the Cahore and Ribband Groups
title_short Acritarchs from the Lower Palaeozoic succession on the south County Wexford coast, Ireland: new age constraints for the Cullenstown Formation and the Cahore and Ribband Groups
title_full Acritarchs from the Lower Palaeozoic succession on the south County Wexford coast, Ireland: new age constraints for the Cullenstown Formation and the Cahore and Ribband Groups
title_fullStr Acritarchs from the Lower Palaeozoic succession on the south County Wexford coast, Ireland: new age constraints for the Cullenstown Formation and the Cahore and Ribband Groups
title_full_unstemmed Acritarchs from the Lower Palaeozoic succession on the south County Wexford coast, Ireland: new age constraints for the Cullenstown Formation and the Cahore and Ribband Groups
title_sort acritarchs from the lower palaeozoic succession on the south county wexford coast, ireland: new age constraints for the cullenstown formation and the cahore and ribband groups
publisher Wiley
publishDate 2004
url http://dx.doi.org/10.1002/gj.966
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fgj.966
https://onlinelibrary.wiley.com/doi/pdf/10.1002/gj.966
long_lat ENVELOPE(-114.067,-114.067,-74.833,-74.833)
geographic Bray
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genre Newfoundland
genre_facet Newfoundland
op_source Geological Journal
volume 39, issue 2, page 199-224
ISSN 0072-1050 1099-1034
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op_doi https://doi.org/10.1002/gj.966
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