Sequences of psychrophilic fungi amplified from glacier-preserved ascolichens

Ribosomal DNA sequences were amplified from subfossils of the ascolichen Umbilicaria cylindrica (L.) Delise ex Duby collected at the ablating edges of Greenland glaciers. Surprisingly, phylogenetic analysis indicated that the amplified rDNA sequences were not closely related to those of the lichen-f...

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Published in:Canadian Journal of Botany
Main Authors: DePriest, Paula T, Ivanova, Natalia V, Fahselt, Dianne, Alstrup, Vagn, Gargas, Andrea
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 2000
Subjects:
Online Access:http://dx.doi.org/10.1139/b00-120
http://www.nrcresearchpress.com/doi/pdf/10.1139/b00-120
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spelling crcansciencepubl:10.1139/b00-120 2024-09-15T18:07:45+00:00 Sequences of psychrophilic fungi amplified from glacier-preserved ascolichens DePriest, Paula T Ivanova, Natalia V Fahselt, Dianne Alstrup, Vagn Gargas, Andrea 2000 http://dx.doi.org/10.1139/b00-120 http://www.nrcresearchpress.com/doi/pdf/10.1139/b00-120 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Botany volume 78, issue 11, page 1450-1459 ISSN 0008-4026 journal-article 2000 crcansciencepubl https://doi.org/10.1139/b00-120 2024-08-01T04:10:00Z Ribosomal DNA sequences were amplified from subfossils of the ascolichen Umbilicaria cylindrica (L.) Delise ex Duby collected at the ablating edges of Greenland glaciers. Surprisingly, phylogenetic analysis indicated that the amplified rDNA sequences were not closely related to those of the lichen-forming fungus but rather represented two groups of psychrophilic basidiomycetes (orders Cystofilobasidiales and Sporidiales) and one group of ascomycetes (order Leotiales). Two of these groups, the Sporidiales and the Leotiales, include other fungi previously detected in DNA extracted from the grass clothing of the Tyrolean Iceman desiccated and frozen for over 3000 years and also in 2000- and 4000-year-old ice core samples from northern Greenland. Large subunit ribosomal DNA sequences representing the group Cystofilobasidiales were nearly identical to those of the basidioyeast saprobe Mrakia frigida. The adjacent internal transcribed spacer sequence was more than 98% similar to those from three samples of U. cylindrica from different sites that had been subjected to ice burial for various lengths of time, suggesting they also were Mrakia sequences. Although ancient contamination of multiple U. cylindrica specimens with fungi such as Mrakia cannot be ruled out, it is more probable that saprobic colonization of the subfossil tissues by psychrophilic fungi proceeded during recent ice melt.Key words: ancient DNA, small subunit ribosomal DNA, 18S ribosomal DNA, phylogenetic analysis, psychrophilic fungi, lichen-forming fungi. Article in Journal/Newspaper glacier Greenland ice core Canadian Science Publishing Canadian Journal of Botany 78 11 1450 1459
institution Open Polar
collection Canadian Science Publishing
op_collection_id crcansciencepubl
language English
description Ribosomal DNA sequences were amplified from subfossils of the ascolichen Umbilicaria cylindrica (L.) Delise ex Duby collected at the ablating edges of Greenland glaciers. Surprisingly, phylogenetic analysis indicated that the amplified rDNA sequences were not closely related to those of the lichen-forming fungus but rather represented two groups of psychrophilic basidiomycetes (orders Cystofilobasidiales and Sporidiales) and one group of ascomycetes (order Leotiales). Two of these groups, the Sporidiales and the Leotiales, include other fungi previously detected in DNA extracted from the grass clothing of the Tyrolean Iceman desiccated and frozen for over 3000 years and also in 2000- and 4000-year-old ice core samples from northern Greenland. Large subunit ribosomal DNA sequences representing the group Cystofilobasidiales were nearly identical to those of the basidioyeast saprobe Mrakia frigida. The adjacent internal transcribed spacer sequence was more than 98% similar to those from three samples of U. cylindrica from different sites that had been subjected to ice burial for various lengths of time, suggesting they also were Mrakia sequences. Although ancient contamination of multiple U. cylindrica specimens with fungi such as Mrakia cannot be ruled out, it is more probable that saprobic colonization of the subfossil tissues by psychrophilic fungi proceeded during recent ice melt.Key words: ancient DNA, small subunit ribosomal DNA, 18S ribosomal DNA, phylogenetic analysis, psychrophilic fungi, lichen-forming fungi.
format Article in Journal/Newspaper
author DePriest, Paula T
Ivanova, Natalia V
Fahselt, Dianne
Alstrup, Vagn
Gargas, Andrea
spellingShingle DePriest, Paula T
Ivanova, Natalia V
Fahselt, Dianne
Alstrup, Vagn
Gargas, Andrea
Sequences of psychrophilic fungi amplified from glacier-preserved ascolichens
author_facet DePriest, Paula T
Ivanova, Natalia V
Fahselt, Dianne
Alstrup, Vagn
Gargas, Andrea
author_sort DePriest, Paula T
title Sequences of psychrophilic fungi amplified from glacier-preserved ascolichens
title_short Sequences of psychrophilic fungi amplified from glacier-preserved ascolichens
title_full Sequences of psychrophilic fungi amplified from glacier-preserved ascolichens
title_fullStr Sequences of psychrophilic fungi amplified from glacier-preserved ascolichens
title_full_unstemmed Sequences of psychrophilic fungi amplified from glacier-preserved ascolichens
title_sort sequences of psychrophilic fungi amplified from glacier-preserved ascolichens
publisher Canadian Science Publishing
publishDate 2000
url http://dx.doi.org/10.1139/b00-120
http://www.nrcresearchpress.com/doi/pdf/10.1139/b00-120
genre glacier
Greenland
ice core
genre_facet glacier
Greenland
ice core
op_source Canadian Journal of Botany
volume 78, issue 11, page 1450-1459
ISSN 0008-4026
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/b00-120
container_title Canadian Journal of Botany
container_volume 78
container_issue 11
container_start_page 1450
op_container_end_page 1459
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