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Development of lichenometric dating curves for Highland Scotland

Published online by Cambridge University Press:  03 November 2011

John L. Innes
John L. Innes
Affiliation:
Department of Geography, University of Cambridge, Downing Place, Cambridge, CB2 3EN, England.
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Abstract

The lichens growing on gravestones in 142 Scottish graveyards have been examined. Measurements were restricted to Section Rhizocarpon thalii. These data permit the development of lichenometric growth curves on acidic igneous, basic igneous, sandstone and slate substrates in most areas of Highland Scotland. The colonisation of gravestones, which is extremely erratic, takes place after a minimum of eight years. The ‘great period’ of growth lasts for approximately 20 years after the erection of the gravestone. The lichen factor (growth after 100 years) is correlated with the growth after 25 and 250 years indicating that it is a representative index of the growth rates. Growth rates are non-linear, decreasing with time. Calculated lichen factors for acidic igneous substrates range from 33 to 104 mm. The distributions of different types of gravestones are non-uniform in both time and space, making the comparison of growth rates on different rock types impractical. The results indicate that there may be a gradual decrease in the growth rates from W to E, reflecting the decreasing maritime influence towards the E.

Keywords

acidicbasicgravestoneigneouslichen colonisationlichen growthRhizocarponsandstoneslate.
Type
Research Article
Information
Earth and Environmental Science Transactions of The Royal Society of Edinburgh , Volume 74 , Issue 1 , 1983 , pp. 23 - 32
Copyright
Copyright © Royal Society of Edinburgh 1983

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References

7. References

Benedict, J. B. 1967. Recent glacial history of an alpine area in the Colorado Front Range, U.S.A. I. Establishing a lichen growth curve. J GLACIOL 6, 817–32.CrossRefGoogle Scholar
Beschel, R. E. 1950. Flechten als Altersmasstab rezenter Moränen. Z GLETSCHERKD GLAZIALGEOL 1, 152–61.Google Scholar
Beschel, R. E. 1956. Lichenometrie im Gletschervorfeld. JAHRB VER SCHUTZE ALPENPFLANZ TIERE 22, 164–85.Google Scholar
Beschel, R. E. 1957. A project to use lichens as indicators of climate and time. ARCTIC 10, 60.Google Scholar
Beschel, R. E. 1958. Flechtenvereine der Städte, Städtflechten und ihr Wachstum. BER NATURWISS VER INNSBRUCK 52, 1–158.Google Scholar
Beschel, R. E. 1961. Dating rock surfaces by liehen growth and its application to glaciology and physiography (lichenometry). In Raasch, G. O. (ed.) Geology of the Arctia, Vol. 2, 1044–62. Toronto: University of Toronto Press.CrossRefGoogle Scholar
Calkin, P. E. & Ellis, J. M. 1980. A lichenometric dating curve and its application to Holocene glacier studies in the Central Brooks Range, Alaska. ARCT ALP RES 12, 245–64.CrossRefGoogle Scholar
Carrare, P. E. & Andrews, J. T. 1973. Problems and application of lichenometry to geomorphic studies, San Juan Mountains, Colorado. ARCT ALP RES 5, 373–84.CrossRefGoogle Scholar
cernohorsky, Z. 1977. Rhizocarpon Ram. em. Th.Fr. In Poelt, J. & Vězda, A. (eds) Bestimmungsschlüssel europäischer Flechten. Supplement 1, 217–31. Vaduz: J. Cramer.Google Scholar
Colman, S. M. 1981. Rock-weathering rates as functions of time. QUATERNARY RES 15, 250–64.CrossRefGoogle Scholar
Colman, S. M. & Pierce, K. L. 1980. Weathering rates on andesitic and basaltic stones as a Quaternary age indicator, western United States. PROF PAP U S GEOL SURV 1210.Google Scholar
Faegri, K. 1933, Über die Langenvegetation einiger Gletscher des Jostedalsbre und die dadurch bedingten Pflanzensukzessionen. ARBOK MUS BERGEN 7.Google Scholar
Feuerer, V. T. 1978. Zur Kenntis der Flechtengattung Rhizocarpon in Bayern.BER BAYERISCHEN BOT GES 49, 59–135.Google Scholar
Gregory, K. J. 1976. Lichens and the determination of river channel capacities. EARTH SURF PROCESSES 1, 273–85.CrossRefGoogle Scholar
Innes, J. L. 1982a. Debris flow activity in the Scottish Highlands. Unpublished Ph.D. Thesis, University of Carbridge.Google Scholar
Innes, J. L. 1982b. Lichenometrie use of an aggregated Rhizocarpon ‘species’. BOREAS 11, 53–8.CrossRefGoogle Scholar
Innes, J. L. 1983. The use of an aggregated Rhizocarpon ‘species’ in lichenometry: further observations and implications for lichenometrical dating. BOREAS 12, in press.Google Scholar
Karlén, W. 1979. Glacier variations in the Svartisen area, northern Norway. GEOGR ANN 61A, 11–28.CrossRefGoogle Scholar
King, R. B. 1971. Boulder polygons and stripes in the Cairngorm Mountains, Scotland. J GLACIOL 10, 375–86.CrossRefGoogle Scholar
King, R. B. 1972. Lobes in the Cairngorm Mountains, Scotland. BIUL PERYGLAC 21, 153–67.Google Scholar
Locke, W. W., Andrews, J. T. & Webber, P. J. 1979. A manual for lichenometry. TECH BULL BR GEOMORPHOL RES GROUP 26.Google Scholar
Matthews, J. A. 1974. Families of lichenometrie dating curves from the Storbreen gletschervorfeld, Jotunheimen, Norway. NOR GEOGR TIDSSKR 28, 215–35.CrossRefGoogle Scholar
Matthews, J. A. 1980. Some problems and implications of 14C dates from a podzol buried beneath an end moraine at Haugabreen, southern Norway. GEOGR ANN 62A, 185–208.Google Scholar
Matthews, J. A. 1981. Natural 14C age/depth gradient in a buried soil. NATURWISSENSCHAFTEN 67, 472–4.CrossRefGoogle Scholar
Miller, G. H. & Andrews, J. T. 1972. Quaternary history of Northern Cumberland Peninsula, East Baffin Island, NWT, Canada. Part VI: Preliminary lichen growth curve. BULL GEOL SOC AM 83, 1133–8.CrossRefGoogle Scholar
Mottershead, D. N. & White, I. D. 1972. The lichenometric dating of glacier recession, Tunbergsdal, Southern Norway, GEOGR ANN 54A, 47–52.CrossRefGoogle Scholar
Mottershead, D. N. & White, I. D. 1973. Lichen growth at Tungersdal—a confirmation. GEOGR ANN 55A, 143–5.Google Scholar
Pitman, G. T. K. 1973. A lichenometrical study of snowpatch variation in the Frederiskhåb district, south-west Greenland and its implications for the study of climatic and glacial fluctuations. BULL GRØNLANDS GEOL UNDERS 104, 1–31.CrossRefGoogle Scholar
Porter, S. C. 1981. Lichenometric studies in the Cascade Range of Washington: establishment of Rhizocarpon geographicum growth curves at Mount Rainier. ARCT ALP RES 13, 11–23.CrossRefGoogle Scholar
Sugden, D. E. 1977. Did glaciers really form in the Cairngorms in the 17th-19th centuries? CAIRNGORM CLUB J 97, 187–201.Google Scholar
Topham, P. B. 1977. Colonization, growth, succession and competition. In Seaward, M. R. D. (ed.) Lichen Ecology, 31–68. London: Academic Press.Google Scholar
Trudgill, S. T., Crabtree, R. W. & Walker, P. J. C 1979. The age of exposure of limestone pavements—a pilot lichenometric study in Co. Clare, Eire. TRANS BR CAVE RES ASSOC 6, 10–4.Google Scholar
Ward, R. G. W. 1981. Snow avalanches in Scotland with particular reference to the Cairngorm Mountains. Unpublished Ph.D. Thesis, Aberdeen University.Google Scholar
Worsley, P. 1973. An evaluation of the attempt to date the recession of Tunbergdalsbreen, southern Norway, by liche-nometry. GEOGR ANN 55A, 137–41.CrossRefGoogle Scholar