High microbial activity on glaciers: importance to the global carbon cycle

Abstract Cryoconite holes, which can cover 0.1–10% of the surface area of glaciers, are small, water‐filled depressions (typically <1 m in diameter and usually <0.5 m deep) that form on the surface of glaciers when solar‐heated inorganic and organic debris melts into the ice. Recent studies sh...

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Published in:Global Change Biology
Main Authors: ANESIO, ALEXANDRE M., HODSON, ANDREW J., FRITZ, ANDREAS, PSENNER, ROLAND, SATTLER, BIRGIT
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2009
Subjects:
Online Access:http://dx.doi.org/10.1111/j.1365-2486.2008.01758.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1365-2486.2008.01758.x
https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1365-2486.2008.01758.x
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spelling crwiley:10.1111/j.1365-2486.2008.01758.x 2024-06-23T07:47:52+00:00 High microbial activity on glaciers: importance to the global carbon cycle ANESIO, ALEXANDRE M. HODSON, ANDREW J. FRITZ, ANDREAS PSENNER, ROLAND SATTLER, BIRGIT 2009 http://dx.doi.org/10.1111/j.1365-2486.2008.01758.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1365-2486.2008.01758.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1365-2486.2008.01758.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Global Change Biology volume 15, issue 4, page 955-960 ISSN 1354-1013 1365-2486 journal-article 2009 crwiley https://doi.org/10.1111/j.1365-2486.2008.01758.x 2024-06-13T04:21:20Z Abstract Cryoconite holes, which can cover 0.1–10% of the surface area of glaciers, are small, water‐filled depressions (typically <1 m in diameter and usually <0.5 m deep) that form on the surface of glaciers when solar‐heated inorganic and organic debris melts into the ice. Recent studies show that cryoconites are colonized by a diverse range of microorganisms, including viruses, bacteria and algae. Whether microbial communities on the surface of glaciers are actively influencing biogeochemical cycles or are just present in a dormant state has been a matter of debate for long time. Here, we report primary production and community respiration of cryoconite holes upon glaciers in Svalbard, Greenland and the European Alps. Microbial activity in cryoconite holes is high despite maximum temperatures seldom exceeding 0.1 °C. In situ primary production and respiration in cryoconites during the summer is often comparable with that found in soils in warmer and nutrient richer regions. Considering only glacier areas outside Antarctica and a conservative average cryoconite distribution on glacial surfaces, we found that on a global basis cryoconite holes have the potential to fix as much as 64 Gg of carbon per year (i.e. 98 Gg of photosynthesis minus 34 Gg of community respiration). Most lakes and rivers are generally considered as heterotrophic systems, but our results suggest that glaciers, which contain 75% of the freshwater of the planet, are largely autotrophic systems. Article in Journal/Newspaper Antarc* Antarctica glacier glacier Greenland Svalbard Wiley Online Library Greenland Svalbard Global Change Biology 15 4 955 960
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract Cryoconite holes, which can cover 0.1–10% of the surface area of glaciers, are small, water‐filled depressions (typically <1 m in diameter and usually <0.5 m deep) that form on the surface of glaciers when solar‐heated inorganic and organic debris melts into the ice. Recent studies show that cryoconites are colonized by a diverse range of microorganisms, including viruses, bacteria and algae. Whether microbial communities on the surface of glaciers are actively influencing biogeochemical cycles or are just present in a dormant state has been a matter of debate for long time. Here, we report primary production and community respiration of cryoconite holes upon glaciers in Svalbard, Greenland and the European Alps. Microbial activity in cryoconite holes is high despite maximum temperatures seldom exceeding 0.1 °C. In situ primary production and respiration in cryoconites during the summer is often comparable with that found in soils in warmer and nutrient richer regions. Considering only glacier areas outside Antarctica and a conservative average cryoconite distribution on glacial surfaces, we found that on a global basis cryoconite holes have the potential to fix as much as 64 Gg of carbon per year (i.e. 98 Gg of photosynthesis minus 34 Gg of community respiration). Most lakes and rivers are generally considered as heterotrophic systems, but our results suggest that glaciers, which contain 75% of the freshwater of the planet, are largely autotrophic systems.
format Article in Journal/Newspaper
author ANESIO, ALEXANDRE M.
HODSON, ANDREW J.
FRITZ, ANDREAS
PSENNER, ROLAND
SATTLER, BIRGIT
spellingShingle ANESIO, ALEXANDRE M.
HODSON, ANDREW J.
FRITZ, ANDREAS
PSENNER, ROLAND
SATTLER, BIRGIT
High microbial activity on glaciers: importance to the global carbon cycle
author_facet ANESIO, ALEXANDRE M.
HODSON, ANDREW J.
FRITZ, ANDREAS
PSENNER, ROLAND
SATTLER, BIRGIT
author_sort ANESIO, ALEXANDRE M.
title High microbial activity on glaciers: importance to the global carbon cycle
title_short High microbial activity on glaciers: importance to the global carbon cycle
title_full High microbial activity on glaciers: importance to the global carbon cycle
title_fullStr High microbial activity on glaciers: importance to the global carbon cycle
title_full_unstemmed High microbial activity on glaciers: importance to the global carbon cycle
title_sort high microbial activity on glaciers: importance to the global carbon cycle
publisher Wiley
publishDate 2009
url http://dx.doi.org/10.1111/j.1365-2486.2008.01758.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1365-2486.2008.01758.x
https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1365-2486.2008.01758.x
geographic Greenland
Svalbard
geographic_facet Greenland
Svalbard
genre Antarc*
Antarctica
glacier
glacier
Greenland
Svalbard
genre_facet Antarc*
Antarctica
glacier
glacier
Greenland
Svalbard
op_source Global Change Biology
volume 15, issue 4, page 955-960
ISSN 1354-1013 1365-2486
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1111/j.1365-2486.2008.01758.x
container_title Global Change Biology
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