Journal of Micropalaeontology, 24: 77–94. 0262-821X/05 $15.00 2005 The Micropalaeontological Society Early Carboniferous (Late Tournaisian–Early Viséan) ostracods from the Ballagan Formation, central Scotland, UK MARK WILLIAMS1, 2, MICHAEL STEPHENSON1, IAN P. WILKINSON1, MELANIE J. LENG3 & C. GILES MILLER4 1 British 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:
[email protected]. uk). 3NERC Isotope Geosciences Laboratory, British Geological Survey, Keyworth, Nottingham NG12 5GG, UK. 4Natural History Museum, Cromwell Road, South Kensington, London SW7 5BD, UK. 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,