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Palaeoecology of the Viséan of East Kirkton, West Lothian, Scotland

Published online by Cambridge University Press:  03 November 2011

E. N. K. Clarkson
Affiliation:
Department of Geology and Geophysics, University of Edinburgh, Edinburgh EH9 3JW, U.K.
A. R. Milner
Affiliation:
Department of Biology, Birkbeck College, University of London, Malet St., London WC1E 7HX, U.K.
M. I. Coates
Affiliation:
Department of Zoology, University of Cambridge, Downing St., Cambridge CB2 3EJ, U.K.

Abstract

The Viséan sequence at East Kirkton was deposited in a shallow lake, set within a richly vegetated landscape formed of volcanic cones a few hundred metres high. There was little volcanic activity, however, while the lake existed, and the many tuff horizons within the sequence were washed in during weathering. The lake may have been generally cool, though of unusual water chemistry, as a result of which the spherulitic East Kirkton Limestone precipitated. At times, however, water temperatures may have risen sharply through localised hot-spring activity; both factors deterred ‘normal’ aquatic life.

The bulk of the preserved biota consists of plants (permineralisations and compressions) and dominantly land-living animals, including the oldest terrestrial tetrapods (amphibians and reptiliomorphs), large terrestrial-aquatic eurypterids, the first harvestman and rare millipedes. All these animals lived close to the lake, in a fire-prone forest dominated by gymnosperms and pteridosperms.

At a late stage in the history of the lake, deposition of spherulitic limestones was replaced by black shales, bearing a ‘standard’ Oil-Shale fish fauna, suggesting that the isolated lake had linked with a larger fish-bearing water body. This is coupled with a shift to a lycopod-dominated flora and may indicate a climatic change to wetter conditions. Finally the lake silted up with tuff, ending an existence of only a few tens of thousands of years.

Type
Research Article
Copyright
Copyright © Royal Society of Edinburgh 1993

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References

Andrews, S. M. 1985. Rhizodont crossopterygian fish from the Dinantian of Foulden, Berwickshire, with a re-evaluation of the group. TRANS R SOC EDINBURGH: EARTH SCI 76, 6795.CrossRefGoogle Scholar
Clack, J. A. 1994. Silvanerpeton miripedes, a new anthracosauroid from the Viséan of East Kirkton, West Lothian, Scotland. TRANS R SOC EDINBURGH: EARTH SCI 84, 369376.Google Scholar
Clarkson, E. N. K. 1985. Palaeoecology of the Dinantian of Foulden, Berwickshire, Scotland. TRANS R SOC EDINBURGH: EARTH SCI 76, 97100.CrossRefGoogle Scholar
Coates, M. I. 1994. Actinopterygian and acanthodian fishes from the Viséan of East Kirkton, West Lothian, Scotland. TRANS R SOC EDINBURGH: EARTH SCI 84, 317327.Google Scholar
Craig, G. Y. 1956. The mode of life of certain Carboniferous animals from West Kirkton Quarry, Bathgate, Scotland. TRANS GEOL SOC EDINBURGH 16, 272–79.CrossRefGoogle Scholar
Denison, R. 1979. Volume 5, Acanthodii. In Schultze, H.-P., (Ed.) Handbook of Palaeoichthyology, Vol. 5. Stuttgart & New York: Gustav Fischer Verlag.Google Scholar
Durant, G. P. 1994. Volcanogenic sediments of the East Kirkton Limestone of West Lothian, Scotland. TRANS R SOC EDINBURGH: EARTH SCI 84, 203207.Google Scholar
Galtier, J. & Scott, A. C. 1991. Stanwoodia, a new genus of probable early gymnosperms from the Dinantian of East Kirkton, Scotland. TRANS R SOC EDINBURGH: EARTH SCI 82, 113–23.CrossRefGoogle Scholar
Galtier, J. & Scott, A. C. 1994. Arborescent gymnosperms from the Viséan of East Kirkton, West Lothian, Scotland. TRANS R SOC EDINBURGH: EARTH SCI 84, 261266.Google Scholar
Jameson, J. 1980. Depositional environments in the Petershill Formation, Bathgate, West Lothian. Unpublished Ph.D. Thesis, University of Edinburgh.Google Scholar
Jameson, J. 1987. Carbonate sedimentation on a mid-basin high: the Petershill Formation, Midland Valley of Scotland. In Miller, J., Adams, A. E. and Wright, V. P. (Eds) European Dinantian Environments. GEOL J SPEC ISS 12, 309–27.Google Scholar
Jeram, A. J. 1994. The scorpions from the Lower Carboniferous of East Kirkton, West Lothian, Scotland, with a revision of the infraorder Mesoscorpionina, TRANS ROY SOC EDINBURGH: EARTH SCI 84, 283299.Google Scholar
Jeram, A. J. & Selden, P. A. 1994. Eurypterids from the Viséan of East Kirkton, West Lothian, Scotland. TRANS R SOC EDINBURGH: EARTH SCI 84, 301308.Google Scholar
Large, D. J. 1987. The East Kirkton Limestone: a hot spring siliceous sinter. Unpublished B.Sc. Thesis, University of Strathclyde, Glasgow.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, 223237.Google Scholar
Milner, A. C. 1994. The aïstopod amphibian from the Viséan of East Kirkton, West Lothian, Scotland. TRANS R SOC EDINBURGH: EARTH SCI 84, 363368.Google Scholar
Milner, A. R. & Sequeira, S. E. K. 1994 The temnospondyl amphibians from the Viséan of East Kirkton, West Lothian, Scotland. TRANS R SOC EDINBURGH: EARTH SCI 84, 331361.Google Scholar
Milner, A. R., Smithson, T. R., Milner, A. C., Coates, M. I. & Rolfe, W. D. I. 1986. The search for early tetrapods. MOD GEOL 10, 128.Google Scholar
Muir, R. O. & Walton, E. K. 1957. The East Kirkton Limestone. TRANS GEOL SOC GLASGOW 12, 157–68.CrossRefGoogle Scholar
Paton, R. L. 1994. Elasmobranch fishes from the Lower Carboniferous of East Kirkton, West Lothian. TRANS R SOC EDINBURGH: EARTH SCI 84, 329330.Google Scholar
Rolfe, W. D. I., Durant, G. P., Fallick, A. E., Hall, A. J. 2, Large, D. J., Scott, A. C., Smithson, T. R. & Walkden, G. M. 1990. An early Viséan biota preserved by Viséan vulcanicity in Scotland. In Lockley, M. G. & Rice, A. (Eds) Volcanism and fossil biotas, Boulder, Colorado. GEOL SOC AM SPEC PAP 244, 1324.Google Scholar
Rolfe, W. D. I., Durant, G. P., Baird, W. J., Chaplin, C., Paton, R. L. & Reekie, R. J. 1994. The East Kirkton Limestone, Viséan, West Lothian, Scotland: introduction and stratigraphy. TRANS R SOC EDINBURGH: EARTH SCI 84, 177188.Google Scholar
Scott, A. C., Brown, R. E., Galtier, J. & Meyer-Berthaud, B. 1994. Fossil plants from the Viséan of East Kirkton, West Lothian, Scotland. TRANS R SOC EDINBURGH: EARTH SCI 84, 249260.Google Scholar
Shear, W. A. 1994 Myriapodous arthropods from the Viséan of East Kirkton, Scotland. TRANS R SOC EDINBURGH: EARTH SCI 84, 309316.Google Scholar
Smithson, T. R. 1989. The earliest known reptile. NATURE 342, 676–78.CrossRefGoogle Scholar
Smithson, T. R. 1994. Eldeceeon rolfei, a new reptiliomorph from the Viséan of East Kirkton, West Lothian, Scotland. TRANS R SOC EDINBURGH: EARTH SCI 84, 377382.Google Scholar
Smithson, T. R. & Rolfe, W. D. I. 1990. Westlothiana gen. nov.; naming the earliest known reptile. SCOTT J GEOL. 26, 137–38.CrossRefGoogle Scholar
Smithson, T. R., Carroil, R. L., Panchen, A. L. & Andrews, S. M. 1994. Westlothiana lizziae from the Viséan of East Kirkton, West Lothian, Scotland, and the amniote stem. TRANS R SOC EDINBURGH: EARTH SCI 84, 383412.Google Scholar
Upton, B. G. J. 1994. Volcanic setting of the East Kirkton sequence, West Lothian, Scotland. TRANS R SOC EDINBURGH: EARTH SCI 84, 209212.Google Scholar
Walkden, G. M., Irwin, J. R. & Fallick, A. E. 1994. Carbonate spherules and bortyoids as lake floor cements in the East Kirkton Limestone of West Lothian, Scotland. TRANS R SOC EDINBURGH: EARTH SCI 84, 213221.Google Scholar