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The East Kirkton Limestone, Viséan, of West Lothian, Scotland: introduction and stratigraphy

Published online by Cambridge University Press:  03 November 2011

W. D. I. Rolfe ,
G. P. Durant ,
W. J. Baird ,
C. Chaplin ,
R. L. Paton  and
R. J. Reekie
W. D. I. Rolfe
Affiliation:
National Museums of Scotland, Chambers Street, Edinburgh EH1 1JF, U.K.
G. P. Durant
Affiliation:
Hunterian Museum, University of Glasgow, Glasgow G12 8QQ, U.K.
W. J. Baird
Affiliation:
National Museums of Scotland, Chambers Street, Edinburgh EH1 1JF, U.K.
C. Chaplin
Affiliation:
National Museums of Scotland, Chambers Street, Edinburgh EH1 1JF, U.K.
R. L. Paton
Affiliation:
National Museums of Scotland, Chambers Street, Edinburgh EH1 1JF, U.K.
R. J. Reekie
Affiliation:
National Museums of Scotland, Chambers Street, Edinburgh EH1 1JF, U.K.
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Abstract

A brief history of research into the unusual laminated and spherulitic East Kirkton Limestone (Brigantian, Viséan) is given. It documents the paucity of fossil finds until 1984, when S. P. Wood discovered a previously unsuspected terrestrial biota. Some early finds, such as stromatolites, have since been overlooked, while others were misinterpreted, e.g. a ‘fish-bone’ collected before 1870 proves to be amphibian. A formal lithostratigraphic description is given of the three beds that comprise the c. 15 m sequence in East Kirkton Quarry: the East Kirkton Limestone, overlain by Little Cliff Shale and Geikie Tuff, the latter two being here formally named. Lithological descriptions and a unit-by-unit distribution of major elements of the biota are provided for a measured section comprising 88 units. This is based on bed-by-bed excavations carried out 1985-92, supplemented by nine boreholes. Two 3 m-thick massive limestones lenses are recorded from the quarry and a probable third was proved in a borehole. Brief reports are given on the ‘stromatolites’ (by M. R. Walter), bivalve molluscs (R. M. C. Eagar and R. B. Wilson), ostracods (J. Pollard) and gypsum pseudomorphs.

Keywords

BiotabivalvesBrigantianexcavationsGeikie Tuffgypsumlimestone lenseslithostratigraphyLittle Cliff ShaleostracodsstromatolitesLower Caroniferous
Type
Research Article
Information
Earth and Environmental Science Transactions of The Royal Society of Edinburgh , Volume 84 , Issue 3-4: Volcanism and early terrestrial biotas , 1993 , pp. 177 - 188
Copyright
Copyright © Royal Society of Edinburgh 1993

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References

Cadell, H. M. 1925. The rocks of West Lothian. Edinburgh: Oliver & Boyd.Google Scholar
Casanova, J. 1986. East African Rift stromatolites. In Frostick, L. E. et al. (Eds) Sedimentation in the African Rifts, 201–10. London: GEOL SOC SPEC PUBL 25.Google Scholar
Chisholm, J. I., McAdam, A. D. & Brand, P. J. 1989. Lithostratigraphical classification of Upper Devonian and Lower Carboniferous rocks in the Lothians. BR GEOL SURV SPEC REP WA/89/26.Google Scholar
Cunningham, R. J. H. 1838. On the geology of the Lothians. MEM WERNER NAT HIST SOC EDINBURGH 7, 103–60.Google Scholar
Doody, J. J., McGill, R. A. R., Darby, D. & Smythe, D. K. 1994. Geophysical surveys of the East Kirkton Limestone, Viséan, West Lothian, Scotland. TRANS R SOC EDINBURGH: EARTH SCI 84, 197–202.Google Scholar
Fleming, J. 1825. On the Neptunian formation of siliceous stalactites. EDINB J SCI 2, 307–12.Google Scholar
Francis, E. H. 1991. Carboniferous. In Craig, G. Y. (Ed.) Geology of Scotland (3rd edn), 393–420. London: Geological Society.Google Scholar
Geikie, A. 1861. In Howell, H. H. & Geikie, A. The geology of the neighbourhood of Edinburgh. MEM GEOL SURV UK.Google Scholar
Geikie, A. 1870. Descriptive catalogue of rock specimens collected by the Geological Survey of Scotland, and exhibited in the Edinburgh Museum of Science and Art. Edinburgh: HMSO.Google Scholar
Geikie, J. 1897. Long excursion—Bathgate Hills. PROC GEOL ASSOC LONDON 8, 198–200.CrossRefGoogle Scholar
Hibbert, S. 1834. Additional notices relative to the fresh-water limestones in the vicinity of Edinburgh. EDINB NEW PHIL J 16, 386–8 (=PROC R SOC EDINBURGH 1, 50-3).Google Scholar
Hibbert, S. 1836. On the fresh-water limestone of Burdiehouse. TRANS R SOC EDINBURGH 13, 169–282.CrossRefGoogle Scholar
Lindley, J. & Hutton, W. 1837. The fossil flora of Great Britain, 3. London: James Ridgway & Sons.Google Scholar
Loftus, G. W. F. & Greensmith, J. T. 1988. The lacustrine Burdiehouse Limestone Formation—a key to the deposition of the Dinantian Oil Shales of Scotland. In Fleet, A. J., Kelts, K. & Talbot, M. R. (Eds) Lacustrine petroleum source rocks, 219–34. GEOL SOC SPEC PUBL 40.CrossRefGoogle Scholar
McGill, R. A. R., Hall, A. J., Braithwaite, C. J. R., Fallick, A. E. & Rolfe, W. D. I. 1990. Petrography and geochemistry of a Lower Carboniferous, lacustrine, hot-spring deposit, East Kirkton, Bathgate, Scotland. PROC 12TH NEW ZEALAND GEOTHERMAL WORKSHOP, 203–8.Google Scholar
McGill, R. A. R., Hall, A. J., Fallick, A. E. & Boyce, A. J. 1994. The palaeoenvironment of East Kirkton, West Lothian, Scotland: stable isotope evidence from silicates and sulphides. TRANS R SOC EDINBURGH: EARTH SCI 84, 223–237.Google Scholar
Milner, A. R. 1985. Scottish window on terrestrial life in the lower Carboniferous. NATURE 314, 320–1.CrossRefGoogle Scholar
Milner, A. R., Smithson, T. R., Milner, A. C, Coates, M. I. & Rolfe, W. D. I. 1986. The search for early tetrapods. MODERN GEOLOGY 10, 1–28.Google Scholar
Muir, R. O. & Walton, E. K. 1957. The East Kirkton Limestone. TRANS GEOL SOC GLASGOW 12, 157–68.CrossRefGoogle Scholar
Parnell, J. 1988. Lacustrine petroleum source rocks in the Dinantian Oil Shale Group, Scotland: a review. In Fleet, A. J., Kelts, K. & Talbot, M. R. (Eds) Lacustrine petroleum source rocks, 235–46. London: GEOL SOC SPEC PUBL 40.Google Scholar
Peach, B. N., Clough, C. T., Hinxman, L. W., Grant, Wilson J. A., Crampton, C. B., Maufe, H. B. & Bailey, E. B. 1910. The geology of the neighbourhood of Edinburgh. MEM GEOL SURV SCOTLAND.Google Scholar
Rolfe, W. D. I. 1986. Mr Wood's fossils. DINOSAUR TIMES 12, 1–6.Google Scholar
Rolfe, W. D. I. 1988. Early life on land; the East Kirkton discoveries. EARTH SCI CONSERVATION 25, 22–8.Google Scholar
Rolfe, W. D. I., Durant, G. P., Fallick, A. E., Hall, A. J., Large, D. J., Scott, A. C, Smithson, T. R. & Walkden, G. M. 1990. An early terrestrial biota preserved by Viséan vulcanicity in Scotland. In Lockley, M. G. & Rice, A. (Eds) Volcanism and fossil biotas, 13–24. Boulder, Colorado: GEOL SOC AM SPEC PAP 244.CrossRefGoogle Scholar
Scott, A. C, Brown, R., Galtier, J. & Meyer-Berthaud, B. 1994. Fossil plants from the Viséan of East Kirkton, West Lothian, Scotland. TRANS R SOC EDINBURGH: EARTH SCI 84, 249–60.Google Scholar
Scouler, J. 1831. Description of a fossil crustaceous animal. EDINB J NAT & GEOGR SCI 3, 352–4.Google Scholar
Smith, R. A., Stephenson, D. & Monro, S. K. 1994. The geological setting of the south Bathgate Hills, West Lothian, Scotland. TRANS R SOC EDINBURGH: EARTH SCI 84, 189–196.Google Scholar
Stephenson, D. & Monro, S. K. 1986. Bathgate Hills. In McAdam, A. D. & Clarkson, E. N. K. (Eds) Lothian geology: an excursion guide, 208–16. Edinburgh: Scottish Academic Press.Google Scholar
Walkden, G. M., Irwin, R. W. & Fallick, A. E. 1994. Carbonate spherules and botryoids as lake floor sediments in the East Kirkton Limestone. TRANS R SOC EDINBURGH: EARTH SCI 84, 213–221.Google Scholar
Walter, M. R. (Ed.) 1976. Stromatolites. Amsterdam: Elsevier.Google Scholar
Weir, J. 1960. A monograph of British Carboniferous non-marine Lamellibranchia. PALAEONTOGR SOC MONOGR 10, 273–320.Google Scholar
Wood, S. P., Panchen, A. L. & Smithson, T. R. 1985. A terrestrial fauna from the Scottish lower Carboniferous. NATURE 314, 355–56.CrossRefGoogle Scholar