Methane flux and high-affinity methanotrophic diversity along the chronosequence of a receding glacier in Greenland

Methane consumption in upland soils represents an important part of the biologically mediated sink of tropospheric methane. The present study focuses on the role of glacier forefields as a potential methane sink. The role of these environments, though increasing in size, has not yet been taken into...

Full description

Bibliographic Details
Published in:Annals of Glaciology
Main Authors: Bárcena, Teresa G., Yde, Jacob C., Finster, Kai W.
Format: Article in Journal/Newspaper
Language:English
Published: 2010
Subjects:
Online Access:https://pure.au.dk/portal/da/publications/methane-flux-and-highaffinity-methanotrophic-diversity-along-the-chronosequence-of-a-receding-glacier-in-greenland(62ea37a7-1294-462b-8b67-db0fe20f592d).html
https://doi.org/10.3189/172756411795932001
http://www.scopus.com/inward/record.url?scp=80052986736&partnerID=8YFLogxK
id ftuniaarhuspubl:oai:pure.atira.dk:publications/62ea37a7-1294-462b-8b67-db0fe20f592d
record_format openpolar
spelling ftuniaarhuspubl:oai:pure.atira.dk:publications/62ea37a7-1294-462b-8b67-db0fe20f592d 2023-05-15T13:29:38+02:00 Methane flux and high-affinity methanotrophic diversity along the chronosequence of a receding glacier in Greenland Bárcena, Teresa G. Yde, Jacob C. Finster, Kai W. 2010-12-01 https://pure.au.dk/portal/da/publications/methane-flux-and-highaffinity-methanotrophic-diversity-along-the-chronosequence-of-a-receding-glacier-in-greenland(62ea37a7-1294-462b-8b67-db0fe20f592d).html https://doi.org/10.3189/172756411795932001 http://www.scopus.com/inward/record.url?scp=80052986736&partnerID=8YFLogxK eng eng info:eu-repo/semantics/restrictedAccess Bárcena , T G , Yde , J C & Finster , K W 2010 , ' Methane flux and high-affinity methanotrophic diversity along the chronosequence of a receding glacier in Greenland ' , Annals of Glaciology , vol. 51 , no. 56 , pp. 23-31 . https://doi.org/10.3189/172756411795932001 article 2010 ftuniaarhuspubl https://doi.org/10.3189/172756411795932001 2023-03-08T23:56:22Z Methane consumption in upland soils represents an important part of the biologically mediated sink of tropospheric methane. The present study focuses on the role of glacier forefields as a potential methane sink. The role of these environments, though increasing in size, has not yet been taken into account in the global methane budget. Net methane fluxes were analysed based on a static chamber method on a proglacial chronosequence from the Mittivakkat valley, southeast Greenland. Methane uptake could be measured in 7of the 12 study sites, with highest rates in the oldest materials from the chronosequence, suggesting that methane oxidation potential may increase during glacier recession (80-150 years). In the chamber located at the glacier front, net methane production was observed, indicating that the microbial community changes after glacial recession from being net methanogenic to becoming net methanotrophic. Diversity analyses based on denaturing gradient gel electrophoresis (DGGE) from the methanotrophic communities responsible for methane uptake at atmospheric levels demonstrate that methanotrophic microbial diversity changes along the chronosequence and show that there is a tendency to a larger diversity in the oldest part of the chronosequence. Sequencing of DNA retrieved from the DGGE revealed a restricted diversity of the methanotrophic community: GenBank accession numbers HM534684-HM534736. Article in Journal/Newspaper Annals of Glaciology glacier Greenland Aarhus University: Research Greenland Annals of Glaciology 51 56 23 31
institution Open Polar
collection Aarhus University: Research
op_collection_id ftuniaarhuspubl
language English
description Methane consumption in upland soils represents an important part of the biologically mediated sink of tropospheric methane. The present study focuses on the role of glacier forefields as a potential methane sink. The role of these environments, though increasing in size, has not yet been taken into account in the global methane budget. Net methane fluxes were analysed based on a static chamber method on a proglacial chronosequence from the Mittivakkat valley, southeast Greenland. Methane uptake could be measured in 7of the 12 study sites, with highest rates in the oldest materials from the chronosequence, suggesting that methane oxidation potential may increase during glacier recession (80-150 years). In the chamber located at the glacier front, net methane production was observed, indicating that the microbial community changes after glacial recession from being net methanogenic to becoming net methanotrophic. Diversity analyses based on denaturing gradient gel electrophoresis (DGGE) from the methanotrophic communities responsible for methane uptake at atmospheric levels demonstrate that methanotrophic microbial diversity changes along the chronosequence and show that there is a tendency to a larger diversity in the oldest part of the chronosequence. Sequencing of DNA retrieved from the DGGE revealed a restricted diversity of the methanotrophic community: GenBank accession numbers HM534684-HM534736.
format Article in Journal/Newspaper
author Bárcena, Teresa G.
Yde, Jacob C.
Finster, Kai W.
spellingShingle Bárcena, Teresa G.
Yde, Jacob C.
Finster, Kai W.
Methane flux and high-affinity methanotrophic diversity along the chronosequence of a receding glacier in Greenland
author_facet Bárcena, Teresa G.
Yde, Jacob C.
Finster, Kai W.
author_sort Bárcena, Teresa G.
title Methane flux and high-affinity methanotrophic diversity along the chronosequence of a receding glacier in Greenland
title_short Methane flux and high-affinity methanotrophic diversity along the chronosequence of a receding glacier in Greenland
title_full Methane flux and high-affinity methanotrophic diversity along the chronosequence of a receding glacier in Greenland
title_fullStr Methane flux and high-affinity methanotrophic diversity along the chronosequence of a receding glacier in Greenland
title_full_unstemmed Methane flux and high-affinity methanotrophic diversity along the chronosequence of a receding glacier in Greenland
title_sort methane flux and high-affinity methanotrophic diversity along the chronosequence of a receding glacier in greenland
publishDate 2010
url https://pure.au.dk/portal/da/publications/methane-flux-and-highaffinity-methanotrophic-diversity-along-the-chronosequence-of-a-receding-glacier-in-greenland(62ea37a7-1294-462b-8b67-db0fe20f592d).html
https://doi.org/10.3189/172756411795932001
http://www.scopus.com/inward/record.url?scp=80052986736&partnerID=8YFLogxK
geographic Greenland
geographic_facet Greenland
genre Annals of Glaciology
glacier
Greenland
genre_facet Annals of Glaciology
glacier
Greenland
op_source Bárcena , T G , Yde , J C & Finster , K W 2010 , ' Methane flux and high-affinity methanotrophic diversity along the chronosequence of a receding glacier in Greenland ' , Annals of Glaciology , vol. 51 , no. 56 , pp. 23-31 . https://doi.org/10.3189/172756411795932001
op_rights info:eu-repo/semantics/restrictedAccess
op_doi https://doi.org/10.3189/172756411795932001
container_title Annals of Glaciology
container_volume 51
container_issue 56
container_start_page 23
op_container_end_page 31
_version_ 1766001608698626048