Growth rates of Rhizocarpon geographicum lichens: a review with new data from Iceland

Abstract This paper reviews evidence from previous growth‐rate studies on lichens of the yellow‐green species of Subgenus Rhizocarpon —the family most commonly used in lichenometric dating. New data are presented from Rhizocarpon section Rhizocarpon thalli growing on a moraine in southern Iceland ov...

Full description

Bibliographic Details
Published in:Journal of Quaternary Science
Main Authors: Bradwell, Tom, Armstrong, Richard A.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2006
Subjects:
Online Access:http://dx.doi.org/10.1002/jqs.1058
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.1058
https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.1058
id crwiley:10.1002/jqs.1058
record_format openpolar
spelling crwiley:10.1002/jqs.1058 2024-06-02T08:08:33+00:00 Growth rates of Rhizocarpon geographicum lichens: a review with new data from Iceland Bradwell, Tom Armstrong, Richard A. 2006 http://dx.doi.org/10.1002/jqs.1058 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.1058 https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.1058 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Journal of Quaternary Science volume 22, issue 4, page 311-320 ISSN 0267-8179 1099-1417 journal-article 2006 crwiley https://doi.org/10.1002/jqs.1058 2024-05-03T11:25:21Z Abstract This paper reviews evidence from previous growth‐rate studies on lichens of the yellow‐green species of Subgenus Rhizocarpon —the family most commonly used in lichenometric dating. New data are presented from Rhizocarpon section Rhizocarpon thalli growing on a moraine in southern Iceland over a period of 4.33 yr. Measurements of 38 lichen thalli, between 2001 and 2005, show that diametral growth rate (DGR, mm yr −1 ) is a function of thallus size. Growth rates increase rapidly in small thalli (<10 mm diameter), remain high (ca. 0.8 mm yr −1 ) and then decrease gradually in larger thalli (>50 mm diameter). Mean DGR in southern Iceland, between 2001 and 2005, was 0.64 mm yr −1 (SD = 0.24). The resultant growth‐rate curve is parabolic and is best described by a third‐order polynomial function. The striking similarity between these findings in Iceland and those of Armstrong ( 1983 ) in Wales implies that the shape of the growth‐rate curve may be characteristic of Rhizocarpon geographicum lichens. The difference between the absolute growth rate in southern Iceland and Wales (ca. 66% faster) is probably a function of climate and micro‐environment between the two sites. These findings have implications for previous lichenometric‐dating studies, namely, that those studies which assume constant lichen growth rates over many decades are probably unreliable. © British Geological Survey/Natural Environment Research Council copyright 2006. Reproduced with the permission of BGS/NERC. Published by John Wiley & Sons, Ltd. Article in Journal/Newspaper Iceland Wiley Online Library Journal of Quaternary Science 22 4 311 320
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract This paper reviews evidence from previous growth‐rate studies on lichens of the yellow‐green species of Subgenus Rhizocarpon —the family most commonly used in lichenometric dating. New data are presented from Rhizocarpon section Rhizocarpon thalli growing on a moraine in southern Iceland over a period of 4.33 yr. Measurements of 38 lichen thalli, between 2001 and 2005, show that diametral growth rate (DGR, mm yr −1 ) is a function of thallus size. Growth rates increase rapidly in small thalli (<10 mm diameter), remain high (ca. 0.8 mm yr −1 ) and then decrease gradually in larger thalli (>50 mm diameter). Mean DGR in southern Iceland, between 2001 and 2005, was 0.64 mm yr −1 (SD = 0.24). The resultant growth‐rate curve is parabolic and is best described by a third‐order polynomial function. The striking similarity between these findings in Iceland and those of Armstrong ( 1983 ) in Wales implies that the shape of the growth‐rate curve may be characteristic of Rhizocarpon geographicum lichens. The difference between the absolute growth rate in southern Iceland and Wales (ca. 66% faster) is probably a function of climate and micro‐environment between the two sites. These findings have implications for previous lichenometric‐dating studies, namely, that those studies which assume constant lichen growth rates over many decades are probably unreliable. © British Geological Survey/Natural Environment Research Council copyright 2006. Reproduced with the permission of BGS/NERC. Published by John Wiley & Sons, Ltd.
format Article in Journal/Newspaper
author Bradwell, Tom
Armstrong, Richard A.
spellingShingle Bradwell, Tom
Armstrong, Richard A.
Growth rates of Rhizocarpon geographicum lichens: a review with new data from Iceland
author_facet Bradwell, Tom
Armstrong, Richard A.
author_sort Bradwell, Tom
title Growth rates of Rhizocarpon geographicum lichens: a review with new data from Iceland
title_short Growth rates of Rhizocarpon geographicum lichens: a review with new data from Iceland
title_full Growth rates of Rhizocarpon geographicum lichens: a review with new data from Iceland
title_fullStr Growth rates of Rhizocarpon geographicum lichens: a review with new data from Iceland
title_full_unstemmed Growth rates of Rhizocarpon geographicum lichens: a review with new data from Iceland
title_sort growth rates of rhizocarpon geographicum lichens: a review with new data from iceland
publisher Wiley
publishDate 2006
url http://dx.doi.org/10.1002/jqs.1058
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.1058
https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.1058
genre Iceland
genre_facet Iceland
op_source Journal of Quaternary Science
volume 22, issue 4, page 311-320
ISSN 0267-8179 1099-1417
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/jqs.1058
container_title Journal of Quaternary Science
container_volume 22
container_issue 4
container_start_page 311
op_container_end_page 320
_version_ 1800753839732686848