Initial Establishment of Saxicolous Lichens Following Recent Glacial Recession in Sverdrup Pass, Ellesmere Island, Canada

Abstract In the recently deglaciated zone of a valley glacier in Central Ellesmere Island the mean period of time before the onset of colonization on bare rock surfaces was estimated to be about 80 years. The first species to establish was Xanthoria elegans , followed by Lecanora crenulata and Umbil...

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Published in:The Lichenologist
Main Authors: Fahselt, Dianne, Maycock, Paul F., Svoboda, Josef
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1988
Subjects:
Online Access:http://dx.doi.org/10.1017/s0024282988000295
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0024282988000295
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spelling crcambridgeupr:10.1017/s0024282988000295 2024-03-03T08:42:01+00:00 Initial Establishment of Saxicolous Lichens Following Recent Glacial Recession in Sverdrup Pass, Ellesmere Island, Canada Fahselt, Dianne Maycock, Paul F. Svoboda, Josef 1988 http://dx.doi.org/10.1017/s0024282988000295 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0024282988000295 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms The Lichenologist volume 20, issue 3, page 253-268 ISSN 0024-2829 1096-1135 Ecology, Evolution, Behavior and Systematics journal-article 1988 crcambridgeupr https://doi.org/10.1017/s0024282988000295 2024-02-08T08:42:59Z Abstract In the recently deglaciated zone of a valley glacier in Central Ellesmere Island the mean period of time before the onset of colonization on bare rock surfaces was estimated to be about 80 years. The first species to establish was Xanthoria elegans , followed by Lecanora crenulata and Umbilicaria virginis approximately 20 years later. Summer temperature appeared to be one factor which affected lichen establishment in recently deglaciated bare areas in the High Arctic. Warmer microsites were identified as preferred locations for thallus establishment; these, therefore, constitute ideal sites for studies of thallus initiation under natural conditions. Following the retreat of a glacier from its most advanced Little Ice Age position, 16 species of saxicolous lichens have become established on bare rock debris in the icefree zone, but in nine transects only five species had a constancy of 80% or more. Lichen diversity in this successional photocommunity was comparable to that in a nearby pre-Little Ice Age landscape with more varied substrata. Article in Journal/Newspaper Arctic Ellesmere Island glacier* Sverdrup Pass Cambridge University Press Arctic Ellesmere Island Canada Bare Rock ENVELOPE(-45.589,-45.589,-60.704,-60.704) Sverdrup Pass ENVELOPE(-80.498,-80.498,79.135,79.135) The Lichenologist 20 3 253 268
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Ecology, Evolution, Behavior and Systematics
spellingShingle Ecology, Evolution, Behavior and Systematics
Fahselt, Dianne
Maycock, Paul F.
Svoboda, Josef
Initial Establishment of Saxicolous Lichens Following Recent Glacial Recession in Sverdrup Pass, Ellesmere Island, Canada
topic_facet Ecology, Evolution, Behavior and Systematics
description Abstract In the recently deglaciated zone of a valley glacier in Central Ellesmere Island the mean period of time before the onset of colonization on bare rock surfaces was estimated to be about 80 years. The first species to establish was Xanthoria elegans , followed by Lecanora crenulata and Umbilicaria virginis approximately 20 years later. Summer temperature appeared to be one factor which affected lichen establishment in recently deglaciated bare areas in the High Arctic. Warmer microsites were identified as preferred locations for thallus establishment; these, therefore, constitute ideal sites for studies of thallus initiation under natural conditions. Following the retreat of a glacier from its most advanced Little Ice Age position, 16 species of saxicolous lichens have become established on bare rock debris in the icefree zone, but in nine transects only five species had a constancy of 80% or more. Lichen diversity in this successional photocommunity was comparable to that in a nearby pre-Little Ice Age landscape with more varied substrata.
format Article in Journal/Newspaper
author Fahselt, Dianne
Maycock, Paul F.
Svoboda, Josef
author_facet Fahselt, Dianne
Maycock, Paul F.
Svoboda, Josef
author_sort Fahselt, Dianne
title Initial Establishment of Saxicolous Lichens Following Recent Glacial Recession in Sverdrup Pass, Ellesmere Island, Canada
title_short Initial Establishment of Saxicolous Lichens Following Recent Glacial Recession in Sverdrup Pass, Ellesmere Island, Canada
title_full Initial Establishment of Saxicolous Lichens Following Recent Glacial Recession in Sverdrup Pass, Ellesmere Island, Canada
title_fullStr Initial Establishment of Saxicolous Lichens Following Recent Glacial Recession in Sverdrup Pass, Ellesmere Island, Canada
title_full_unstemmed Initial Establishment of Saxicolous Lichens Following Recent Glacial Recession in Sverdrup Pass, Ellesmere Island, Canada
title_sort initial establishment of saxicolous lichens following recent glacial recession in sverdrup pass, ellesmere island, canada
publisher Cambridge University Press (CUP)
publishDate 1988
url http://dx.doi.org/10.1017/s0024282988000295
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0024282988000295
long_lat ENVELOPE(-45.589,-45.589,-60.704,-60.704)
ENVELOPE(-80.498,-80.498,79.135,79.135)
geographic Arctic
Ellesmere Island
Canada
Bare Rock
Sverdrup Pass
geographic_facet Arctic
Ellesmere Island
Canada
Bare Rock
Sverdrup Pass
genre Arctic
Ellesmere Island
glacier*
Sverdrup Pass
genre_facet Arctic
Ellesmere Island
glacier*
Sverdrup Pass
op_source The Lichenologist
volume 20, issue 3, page 253-268
ISSN 0024-2829 1096-1135
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0024282988000295
container_title The Lichenologist
container_volume 20
container_issue 3
container_start_page 253
op_container_end_page 268
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