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Early Carboniferous (Late Tournaisian–Early Viséan) ostracods from the Ballagan Formation, central Scotland, UK

MARK WILLIAMS, MICHAEL STEPHENSON, IAN P. WILKINSON, MELANIE J. LENG and C. GILES MILLER
Journal of Micropalaeontology, 24, 77-94, 1 May 2005, https://doi.org/10.1144/jm.24.1.77
MARK WILLIAMS
1British Geological Survey, Keyworth, Nottingham NG12 5GG, UK
2Current address: British Antarctic Survey, Geological Sciences Division, High Cross, Madingley Road, Cambridge CB3 0ET, UK (e-mail: )
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  • For correspondence: mwilli@bas.ac.uk
MICHAEL STEPHENSON
1British Geological Survey, Keyworth, Nottingham NG12 5GG, UK
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IAN P. WILKINSON
1British Geological Survey, Keyworth, Nottingham NG12 5GG, UK
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MELANIE J. LENG
3NERC Isotope Geosciences Laboratory, British Geological Survey, Keyworth, Nottingham NG12 5GG, UK
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C. GILES MILLER
4Natural History Museum, Cromwell Road, South Kensington, London SW7 5BD, UK
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Abstract

The Ballagan Formation (Late Tournaisian–Early Viséan) of central Scotland yields an ostracod fauna of 14 species in ten genera, namely Beyrichiopsis, Cavellina, Glyptolichvinella, Glyptopleura, Knoxiella, Paraparchites, Sansabella, Shemonaella, Silenites and Sulcella. The ostracods, in combination with palynomorphs, are important biostratigraphical indices for correlating the rock sequences, where other means of correlation, especially goniatites, conodonts, foraminifera, brachiopods or corals are absent. Stratigraphical distribution of the ostracods, calibrated with well-established palynomorph biozones, identifies three informally defined intervals: a sub-CM palynomorph Biozone interval with poor ostracod assemblages including Shemonaella scotoburdigalensis; a succeeding interval within the CM palynomorph Biozone where Cavellina coela, Cavellina incurvescens, Sansabella amplectans and the new species Knoxiella monarchella and Paraparchites discus first appear; and, an upper interval, in the upper CM Biozone, marked by the appearance of Sulcella affiliata. At least locally in central Scotland, S. affiliata permits a level of resolution equivalent to a sub-zonal upper division of the CM Biozone. The fauna, flora, sedimentology and stable isotope composition (δ13C and δ18O) of carbonate minerals in the Ballagan Formation suggest the ostracods inhabited brackish, hypersaline and ephemeral aquatic ecologies in a coastal floodplain setting.

KEYWORDS:
  • Carboniferous
  • Tournaisian
  • ostracods
  • biostratigraphy
  • palaeoenvironments
  • © 2005 The Micropalaeontological Society
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Journal of Micropalaeontology: 24 (1)
Journal of Micropalaeontology
Volume 24, Issue 1
May 2005
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Early Carboniferous (Late Tournaisian–Early Viséan) ostracods from the Ballagan Formation, central Scotland, UK

MARK WILLIAMS, MICHAEL STEPHENSON, IAN P. WILKINSON, MELANIE J. LENG and C. GILES MILLER
Journal of Micropalaeontology, 24, 77-94, 1 May 2005, https://doi.org/10.1144/jm.24.1.77
MARK WILLIAMS
1British Geological Survey, Keyworth, Nottingham NG12 5GG, UK
2Current address: British Antarctic Survey, Geological Sciences Division, High Cross, Madingley Road, Cambridge CB3 0ET, UK (e-mail: )
  • Find this author on Google Scholar
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  • Search for this author on this site
  • For correspondence: mwilli@bas.ac.uk
MICHAEL STEPHENSON
1British Geological Survey, Keyworth, Nottingham NG12 5GG, UK
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IAN P. WILKINSON
1British Geological Survey, Keyworth, Nottingham NG12 5GG, UK
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MELANIE J. LENG
3NERC Isotope Geosciences Laboratory, British Geological Survey, Keyworth, Nottingham NG12 5GG, UK
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C. GILES MILLER
4Natural History Museum, Cromwell Road, South Kensington, London SW7 5BD, UK
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Early Carboniferous (Late Tournaisian–Early Viséan) ostracods from the Ballagan Formation, central Scotland, UK

MARK WILLIAMS, MICHAEL STEPHENSON, IAN P. WILKINSON, MELANIE J. LENG and C. GILES MILLER
Journal of Micropalaeontology, 24, 77-94, 1 May 2005, https://doi.org/10.1144/jm.24.1.77
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  • Article
    • Abstract
    • INTRODUCTION
    • KEY SECTIONS AND MATERIAL
    • PALAEOENVIRONMENTAL SETTING
    • BIOSTRATIGRAPHY
    • TAXONOMIC NOTES
    • SYSTEMATIC PALAEONTOLOGY
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