Hostname: page-component-78c5997874-8bhkd Total loading time: 0 Render date: 2024-11-20T01:21:33.446Z Has data issue: false hasContentIssue false
  • English
  • Français

Stratigraphical palaeontology of the Westphalian of the Ayrshire Coalfield, Scotland

Published online by Cambridge University Press:  03 November 2011

P. J. Brand
P. J. Brand
Affiliation:
Institute of Geological Sciences, Murchison House, West Mains Road, Edinburgh EH9 3LA, Scotland.
Get access Rights & Permissions [Opens in a new window]

Abstract

A brief account of the stratigraphy of the Westphalian (Upper Carboniferous) of the Ayrshire Coalfield is given. Older rocks are found to be overlain by Westphalian strata of differing age in various parts of the coalfield. A correlation of the coal seams known by numerous local names in various areas of the coalfield is shown. The vertical distribution of species of non-marine bivalves is illustrated and the faunas associated with various horizons discussed. The presence of variants of Anthraconaia pulchella Broadhurst at more than one horizon is noted. The lateral distribution of species at given horizons is examined and it is shown that elements of the overall fauna of an horizon may be absent in parts of the coalfield. The occurrence of marine bands in the succession is noted and their distribution discussed. It is suggested that during the Aegiranum Marine Band incursion the northern and north-western parts of the coalfield were nearer a land mass. A new stratigraphical name, the Bogton Marine Band is proposed. The band occurs within the Upper Similis-Pulchra Chronozone.

Keywords

Bogton Marine Bandmarine bandsnon-marine bivalvesspecies distributionstratigraphical palaeontologyWestphalian.
Type
Research Article
Information
Earth and Environmental Science Transactions of The Royal Society of Edinburgh , Volume 73 , Issue 3 , 1983 , pp. 173 - 190
Copyright
Copyright © Royal Society of Edinburgh 1983

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Anderson, E. M. 1925. Economic Geology of the Ayrshire Coalfields. Area II. MEM GEOL SURV G B.Google Scholar
Brand, P. J. 1977. The fauna and distribution of the Queenslie Marine Band (Westphalian) in Scotland. REP INST GEOL SCI 77/18.Google Scholar
Calver, M. A. 1956. Die stratigraphische Verbreitung der nichtmarinen Muscheln in den Penninischen Kohlenfeldern Englands. Z DTSCH GEOL GES 107, 26–39.Google Scholar
Calver, M. A. 1969. Westphalian of Britain. C R 6e CONGR INT STRATIGR GEOL CARBONIF 1, 233–54.Google Scholar
Currie, E. D., Duncan, C. & Muir-Wood, H. M. 1937. The fauna of Skipsey's Marine Band. TRANS GEOL SOC GLASGOW 19, 413–56.CrossRefGoogle Scholar
Davies, A. 1970. Carboniferous rocks of the Sanquhar Outlier. BULL GEOL SURV G B 31, 37–87.Google Scholar
Eagar, R. M. C. 1975. Neuere Arbeiten über das Westfal in Irland. ZENTRALBL GEOL PALAÖNTOL teil 1 Heft 9/10, 291–308.Google Scholar
Eyles, V. A., Simpson, J. B. & MacGregor, A. G. 1930. Economie Geology of the Ayrshire Coalfields. Area III. MEM GEOL SURV G B.Google Scholar
Eyles, V. A., Simpson, J. B. & MacGregor, A. G. 1949. The Geology of Central Ayrshire. MEM GEOL SURV G B.Google Scholar
Leìtch, K., Absalom, R. G. & Henderson, S. M. K. 1937. The basal fauna of the Zone of Anthracomya modiolaris in the Coal Measures of South Ayrshire. TRANS GEOL SOC GLASGOW 19, 404–8.Google Scholar
Lumsden, G. I. 1965. The base of the Coal Measures in the Douglas Coalfield, Lanarkshire. BULL GEOL SURV G B 22, 80–91.Google Scholar
Lumsden, G. I. & Wilson, R. B. 1979. Stratigraphical Classification of the Carboniferous Succession of central Scotland. C. R 8e CONGR INT STRATIGR GEOL CARBONIF 2, 27–36.Google Scholar
MacGregor, A. G. 1960. Divisions of the Carboniferous on Geological Survey Scottish Maps. BULL GEOL SURV G B 16, 127–30.Google Scholar
MacGregor, M. 1930. Scottish Carboniferous Stratigraphy: An introduction to the study of the Carboniferous rocks of Scotland. TRANS GEOL SOC GLASGOW 18, 442–558.Google Scholar
Mykura, W. 1960. The replacement of coal by limestone and the reddening of Coal Measures in the Ayrshire Coalfield. BULL GEOL SURV G B 16, 69–109.Google Scholar
Mykura, W. 1967. The Upper Carboniferous rocks of South West Ayrshire. BULL GEOL SURV G B 26, 23–98.Google Scholar
Ramsbottom, W. H. C., Calver, M. A., Eagar, R. M. C., Hodson, F., Holliday, D. W., Stubblefield, C. J. & Wilson, R. B. 1978. A correlation of Silesian rocks in the British Isles. SPEC REP GEOL SOC LONDON 10.Google Scholar
Richey, J. E., Anderson, E. M. & MacGregor, A. G. 1930. The Geology of North Ayrshire. 2nd edn. MEM GEOL SURV G B.Google Scholar
Richey, J. E., Wilson, G. V. & Anderson, E. M. 1925. Economic Geology of the Ayrshire Coalfields. Area I. MEM GEOL SURV G B.Google Scholar
Simpson, J. B. & MacGregor, A. G. 1932. Economic Geology of the Ayrshire Coalfields. Area IV. MEM GEOL SURV G B.Google Scholar
Smith, D. B., Brunstrom, R. G. W., Manning, P. I., Simpson, S. & Shotton, F. W. 1974. A correlation of Permian rocks in the British Isles. SPEC REP GEOL SOC LONDON 5.Google Scholar
Trueman, A. (Ed). 1954. The Coalfields of Great Britain. London: Edward Arnold.Google Scholar
Trueman, A. E. & Weir, J. 1946–1956. The Carboniferous non-marine Lamellibranchia. PALAEONTOGR SOC MONOGR parts 1–9.Google Scholar
Wagner, R. H. 1966. On the presence of probable Upper Stephanian beds in Ayrshire, Scotland. SCOTT J GEOL 2, 122–3.CrossRefGoogle Scholar
Weir, J. 1956–1968. The Carboniferous non-marine Lamellibranchia. PALAEONTOGR SOC MONOGR Parts 10–13.Google Scholar
Weir, J. & Leitch, D. 1936. The zonal distribution of the non-marine lamellibranchs in the Coal Measures of Scotland. TRANS R SOC EDINB 58, 697–751.Google Scholar