Data from: Potential contributions of root decomposition to the nitrogen cycle in arctic forest and tundra

1. Plant contributions to the nitrogen (N) cycle from decomposition are likely to be altered by vegetation shifts associated with climate change. Roots account for the majority of soil organic matter input from vegetation, but little is known about differences between vegetation types in their root...

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Main Authors: Träger, Sabrina, Milbau, Ann, Wilson, Scott D.
Format: Other/Unknown Material
Language:unknown
Published: Zenodo 2018
Subjects:
Online Access:https://doi.org/10.5061/dryad.qg003
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spelling ftzenodo:oai:zenodo.org:4967946 2024-09-15T18:02:12+00:00 Data from: Potential contributions of root decomposition to the nitrogen cycle in arctic forest and tundra Träger, Sabrina Milbau, Ann Wilson, Scott D. 2018-10-16 https://doi.org/10.5061/dryad.qg003 unknown Zenodo https://doi.org/10.1002/ece3.3522 https://zenodo.org/communities/dryad https://doi.org/10.5061/dryad.qg003 oai:zenodo.org:4967946 info:eu-repo/semantics/openAccess Creative Commons Zero v1.0 Universal https://creativecommons.org/publicdomain/zero/1.0/legalcode info:eu-repo/semantics/other 2018 ftzenodo https://doi.org/10.5061/dryad.qg00310.1002/ece3.3522 2024-07-27T02:58:13Z 1. Plant contributions to the nitrogen (N) cycle from decomposition are likely to be altered by vegetation shifts associated with climate change. Roots account for the majority of soil organic matter input from vegetation, but little is known about differences between vegetation types in their root contributions to nutrient cycling. Here, we examine the potential contribution of fine roots to the N cycle in forest and tundra to gain insight into belowground consequences of the widely-observed increase in woody vegetation that accompanies climate change in the Arctic. 2. We combined measurements of root production from minirhizotron images with tissue analysis of roots from differing root diameter and colour classes to obtain potential N input following decomposition. In addition, we tested for changes in N concentration of roots during early stages of decomposition, and investigated whether vegetation type (forest or tundra) affected changes in tissue N concentration during decomposition. For completeness, we also present respective measurements of leaves. 3. The potential N input from roots was two-fold greater in forest than in tundra, mainly due to greater root production in forest. Potential N input varied with root diameter and colour but this variation tended to be similar in forest and tundra. As for roots, the potential N input from leaves was significantly greater in forest than in tundra. Vegetation type had no effect on changes in root or leaf N concentration after one year of decomposition. 4. Our results suggest that shifts in vegetation that accompany climate change in the Arctic will likely increase plant-associated potential N input both belowground and aboveground. In contrast, shifts in vegetation might not alter changes in tissue N concentration during early stages of decomposition. Overall, differences between forest and tundra in potential contribution of decomposing roots to the N cycle reinforce differences between habitats that occur for leaves. Root_Ncycling Other/Unknown Material Climate change Tundra Zenodo
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
description 1. Plant contributions to the nitrogen (N) cycle from decomposition are likely to be altered by vegetation shifts associated with climate change. Roots account for the majority of soil organic matter input from vegetation, but little is known about differences between vegetation types in their root contributions to nutrient cycling. Here, we examine the potential contribution of fine roots to the N cycle in forest and tundra to gain insight into belowground consequences of the widely-observed increase in woody vegetation that accompanies climate change in the Arctic. 2. We combined measurements of root production from minirhizotron images with tissue analysis of roots from differing root diameter and colour classes to obtain potential N input following decomposition. In addition, we tested for changes in N concentration of roots during early stages of decomposition, and investigated whether vegetation type (forest or tundra) affected changes in tissue N concentration during decomposition. For completeness, we also present respective measurements of leaves. 3. The potential N input from roots was two-fold greater in forest than in tundra, mainly due to greater root production in forest. Potential N input varied with root diameter and colour but this variation tended to be similar in forest and tundra. As for roots, the potential N input from leaves was significantly greater in forest than in tundra. Vegetation type had no effect on changes in root or leaf N concentration after one year of decomposition. 4. Our results suggest that shifts in vegetation that accompany climate change in the Arctic will likely increase plant-associated potential N input both belowground and aboveground. In contrast, shifts in vegetation might not alter changes in tissue N concentration during early stages of decomposition. Overall, differences between forest and tundra in potential contribution of decomposing roots to the N cycle reinforce differences between habitats that occur for leaves. Root_Ncycling
format Other/Unknown Material
author Träger, Sabrina
Milbau, Ann
Wilson, Scott D.
spellingShingle Träger, Sabrina
Milbau, Ann
Wilson, Scott D.
Data from: Potential contributions of root decomposition to the nitrogen cycle in arctic forest and tundra
author_facet Träger, Sabrina
Milbau, Ann
Wilson, Scott D.
author_sort Träger, Sabrina
title Data from: Potential contributions of root decomposition to the nitrogen cycle in arctic forest and tundra
title_short Data from: Potential contributions of root decomposition to the nitrogen cycle in arctic forest and tundra
title_full Data from: Potential contributions of root decomposition to the nitrogen cycle in arctic forest and tundra
title_fullStr Data from: Potential contributions of root decomposition to the nitrogen cycle in arctic forest and tundra
title_full_unstemmed Data from: Potential contributions of root decomposition to the nitrogen cycle in arctic forest and tundra
title_sort data from: potential contributions of root decomposition to the nitrogen cycle in arctic forest and tundra
publisher Zenodo
publishDate 2018
url https://doi.org/10.5061/dryad.qg003
genre Climate change
Tundra
genre_facet Climate change
Tundra
op_relation https://doi.org/10.1002/ece3.3522
https://zenodo.org/communities/dryad
https://doi.org/10.5061/dryad.qg003
oai:zenodo.org:4967946
op_rights info:eu-repo/semantics/openAccess
Creative Commons Zero v1.0 Universal
https://creativecommons.org/publicdomain/zero/1.0/legalcode
op_doi https://doi.org/10.5061/dryad.qg00310.1002/ece3.3522
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