Patterns of free amino acids in tundra soils reflect mycorrhizal type, shrubification, and warming

The soil nitrogen (N) cycle in cold terrestrial ecosystems is slow and organically bound N is an important source of N for plants in these ecosystems. Many plant species can take up free amino acids from these infertile soils, either directly or indirectly via their mycorrhizal fungi. We hypothesize...

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Published in:Mycorrhiza
Main Authors: Andresen, Louise C., Bodé, Samuel, Björk, Robert G., Michelsen, Anders, Aerts, Rien, Boeckx, Pascal, Cornelissen, J. Hans C., Klanderud, Kari, van Logtestijn, Richard S. P., Rütting, Tobias
Format: Article in Journal/Newspaper
Language:English
Published: 2022
Subjects:
Online Access:https://curis.ku.dk/portal/da/publications/patterns-of-free-amino-acids-in-tundra-soils-reflect-mycorrhizal-type-shrubification-and-warming(3f339f79-9059-4b5e-8a9f-3ead99b18f1d).html
https://doi.org/10.1007/s00572-022-01075-4
https://curis.ku.dk/ws/files/317089116/s00572_022_01075_4.pdf
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spelling ftcopenhagenunip:oai:pure.atira.dk:publications/3f339f79-9059-4b5e-8a9f-3ead99b18f1d 2024-06-09T07:49:51+00:00 Patterns of free amino acids in tundra soils reflect mycorrhizal type, shrubification, and warming Andresen, Louise C. Bodé, Samuel Björk, Robert G. Michelsen, Anders Aerts, Rien Boeckx, Pascal Cornelissen, J. Hans C. Klanderud, Kari van Logtestijn, Richard S. P. Rütting, Tobias 2022 application/pdf https://curis.ku.dk/portal/da/publications/patterns-of-free-amino-acids-in-tundra-soils-reflect-mycorrhizal-type-shrubification-and-warming(3f339f79-9059-4b5e-8a9f-3ead99b18f1d).html https://doi.org/10.1007/s00572-022-01075-4 https://curis.ku.dk/ws/files/317089116/s00572_022_01075_4.pdf eng eng info:eu-repo/semantics/openAccess Andresen , L C , Bodé , S , Björk , R G , Michelsen , A , Aerts , R , Boeckx , P , Cornelissen , J H C , Klanderud , K , van Logtestijn , R S P & Rütting , T 2022 , ' Patterns of free amino acids in tundra soils reflect mycorrhizal type, shrubification, and warming ' , Mycorrhiza , vol. 32 , no. 3-4 , pp. 305-313 . https://doi.org/10.1007/s00572-022-01075-4 Amino acid uptake Ectomycorrhizal plants Ericoid mycorrhiza Global warming Nitrogen cycling Tundra article 2022 ftcopenhagenunip https://doi.org/10.1007/s00572-022-01075-4 2024-05-16T11:29:25Z The soil nitrogen (N) cycle in cold terrestrial ecosystems is slow and organically bound N is an important source of N for plants in these ecosystems. Many plant species can take up free amino acids from these infertile soils, either directly or indirectly via their mycorrhizal fungi. We hypothesized that plant community changes and local plant community differences will alter the soil free amino acid pool and composition; and that long-term warming could enhance this effect. To test this, we studied the composition of extractable free amino acids at five separate heath, meadow, and bog locations in subarctic and alpine Scandinavia, with long-term (13 to 24 years) warming manipulations. The plant communities all included a mixture of ecto-, ericoid-, and arbuscular mycorrhizal plant species. Vegetation dominated by grasses and forbs with arbuscular and non-mycorrhizal associations showed highest soil free amino acid content, distinguishing them from the sites dominated by shrubs with ecto- and ericoid-mycorrhizal associations. Warming increased shrub and decreased moss cover at two sites, and by using redundancy analysis, we found that altered soil free amino acid composition was related to this plant cover change. From this, we conclude that the mycorrhizal type is important in controlling soil N cycling and that expansion of shrubs with ectomycorrhiza (and to some extent ericoid mycorrhiza) can help retain N within the ecosystems by tightening the N cycle. Article in Journal/Newspaper Subarctic Tundra University of Copenhagen: Research Mycorrhiza 32 3-4 305 313
institution Open Polar
collection University of Copenhagen: Research
op_collection_id ftcopenhagenunip
language English
topic Amino acid uptake
Ectomycorrhizal plants
Ericoid mycorrhiza
Global warming
Nitrogen cycling
Tundra
spellingShingle Amino acid uptake
Ectomycorrhizal plants
Ericoid mycorrhiza
Global warming
Nitrogen cycling
Tundra
Andresen, Louise C.
Bodé, Samuel
Björk, Robert G.
Michelsen, Anders
Aerts, Rien
Boeckx, Pascal
Cornelissen, J. Hans C.
Klanderud, Kari
van Logtestijn, Richard S. P.
Rütting, Tobias
Patterns of free amino acids in tundra soils reflect mycorrhizal type, shrubification, and warming
topic_facet Amino acid uptake
Ectomycorrhizal plants
Ericoid mycorrhiza
Global warming
Nitrogen cycling
Tundra
description The soil nitrogen (N) cycle in cold terrestrial ecosystems is slow and organically bound N is an important source of N for plants in these ecosystems. Many plant species can take up free amino acids from these infertile soils, either directly or indirectly via their mycorrhizal fungi. We hypothesized that plant community changes and local plant community differences will alter the soil free amino acid pool and composition; and that long-term warming could enhance this effect. To test this, we studied the composition of extractable free amino acids at five separate heath, meadow, and bog locations in subarctic and alpine Scandinavia, with long-term (13 to 24 years) warming manipulations. The plant communities all included a mixture of ecto-, ericoid-, and arbuscular mycorrhizal plant species. Vegetation dominated by grasses and forbs with arbuscular and non-mycorrhizal associations showed highest soil free amino acid content, distinguishing them from the sites dominated by shrubs with ecto- and ericoid-mycorrhizal associations. Warming increased shrub and decreased moss cover at two sites, and by using redundancy analysis, we found that altered soil free amino acid composition was related to this plant cover change. From this, we conclude that the mycorrhizal type is important in controlling soil N cycling and that expansion of shrubs with ectomycorrhiza (and to some extent ericoid mycorrhiza) can help retain N within the ecosystems by tightening the N cycle.
format Article in Journal/Newspaper
author Andresen, Louise C.
Bodé, Samuel
Björk, Robert G.
Michelsen, Anders
Aerts, Rien
Boeckx, Pascal
Cornelissen, J. Hans C.
Klanderud, Kari
van Logtestijn, Richard S. P.
Rütting, Tobias
author_facet Andresen, Louise C.
Bodé, Samuel
Björk, Robert G.
Michelsen, Anders
Aerts, Rien
Boeckx, Pascal
Cornelissen, J. Hans C.
Klanderud, Kari
van Logtestijn, Richard S. P.
Rütting, Tobias
author_sort Andresen, Louise C.
title Patterns of free amino acids in tundra soils reflect mycorrhizal type, shrubification, and warming
title_short Patterns of free amino acids in tundra soils reflect mycorrhizal type, shrubification, and warming
title_full Patterns of free amino acids in tundra soils reflect mycorrhizal type, shrubification, and warming
title_fullStr Patterns of free amino acids in tundra soils reflect mycorrhizal type, shrubification, and warming
title_full_unstemmed Patterns of free amino acids in tundra soils reflect mycorrhizal type, shrubification, and warming
title_sort patterns of free amino acids in tundra soils reflect mycorrhizal type, shrubification, and warming
publishDate 2022
url https://curis.ku.dk/portal/da/publications/patterns-of-free-amino-acids-in-tundra-soils-reflect-mycorrhizal-type-shrubification-and-warming(3f339f79-9059-4b5e-8a9f-3ead99b18f1d).html
https://doi.org/10.1007/s00572-022-01075-4
https://curis.ku.dk/ws/files/317089116/s00572_022_01075_4.pdf
genre Subarctic
Tundra
genre_facet Subarctic
Tundra
op_source Andresen , L C , Bodé , S , Björk , R G , Michelsen , A , Aerts , R , Boeckx , P , Cornelissen , J H C , Klanderud , K , van Logtestijn , R S P & Rütting , T 2022 , ' Patterns of free amino acids in tundra soils reflect mycorrhizal type, shrubification, and warming ' , Mycorrhiza , vol. 32 , no. 3-4 , pp. 305-313 . https://doi.org/10.1007/s00572-022-01075-4
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1007/s00572-022-01075-4
container_title Mycorrhiza
container_volume 32
container_issue 3-4
container_start_page 305
op_container_end_page 313
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