Phenological stage of tundra vegetation controls bidirectional exchange of BVOCs in a climate change experiment on a subarctic heath

Abstract Traditionally, biogenic volatile organic compound (BVOC) emissions are often considered a unidirectional flux, from the ecosystem to the atmosphere, but recent studies clearly show the potential for bidirectional exchange. Here we aimed to investigate how warming and leaf litter addition af...

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Published in:Global Change Biology
Main Authors: Baggesen, Nanna, Li, Tao, Seco, Roger, Holst, Thomas, Michelsen, Anders, Rinnan, Riikka
Other Authors: Det Frie Forskningsråd, Danmarks Grundforskningsfond, H2020 European Research Council
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2021
Subjects:
Online Access:http://dx.doi.org/10.1111/gcb.15596
https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.15596
https://onlinelibrary.wiley.com/doi/full-xml/10.1111/gcb.15596
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spelling crwiley:10.1111/gcb.15596 2024-06-02T07:54:11+00:00 Phenological stage of tundra vegetation controls bidirectional exchange of BVOCs in a climate change experiment on a subarctic heath Baggesen, Nanna Li, Tao Seco, Roger Holst, Thomas Michelsen, Anders Rinnan, Riikka Det Frie Forskningsråd Danmarks Grundforskningsfond H2020 European Research Council 2021 http://dx.doi.org/10.1111/gcb.15596 https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.15596 https://onlinelibrary.wiley.com/doi/full-xml/10.1111/gcb.15596 en eng Wiley http://creativecommons.org/licenses/by-nc-nd/4.0/ Global Change Biology volume 27, issue 12, page 2928-2944 ISSN 1354-1013 1365-2486 journal-article 2021 crwiley https://doi.org/10.1111/gcb.15596 2024-05-03T10:50:31Z Abstract Traditionally, biogenic volatile organic compound (BVOC) emissions are often considered a unidirectional flux, from the ecosystem to the atmosphere, but recent studies clearly show the potential for bidirectional exchange. Here we aimed to investigate how warming and leaf litter addition affect the bidirectional exchange (flux) of BVOCs in a long‐term field experiment in the Subarctic. We also assessed changes in net BVOC fluxes in relation to the time of day and the influence of different plant phenological stages. The study was conducted in a full factorial experiment with open top chamber warming and annual litter addition treatments in a tundra heath in Abisko, Northern Sweden. After 18 years of treatments, ecosystem‐level net BVOC fluxes were measured in the experimental plots using proton‐transfer‐reaction time‐of‐flight mass spectrometry (PTR–ToF–MS). The warming treatment increased monoterpene and isoprene emissions by ≈50%. Increasing temperature, due to diurnal variations, can both increase BVOC emission and simultaneously, increase ecosystem uptake. For any given treatment, monoterpene, isoprene, and acetone emissions also increased with increasing ambient air temperatures caused by diurnal variability. Acetaldehyde, methanol, and sesquiterpenes decreased likely due to a deposition flux. For litter addition, only a significant indirect effect on isoprene and monoterpene fluxes (decrease by ~50%–75%) was observed. Litter addition may change soil moisture conditions, leading to changes in plant species composition and biomass, which could subsequently result in changes to BVOC emission compositions. Phenological stages significantly affected fluxes of methanol, isoprene and monoterpenes. We suggest that plant phenological stages differ in impacts on BVOC net emissions, but ambient air temperature and photosynthetically active radiation (PAR) also interact and influence BVOC net emissions differently. Our results may also suggest that BVOC fluxes are not only a response to changes in temperature ... Article in Journal/Newspaper Abisko Northern Sweden Subarctic Tundra Wiley Online Library Abisko ENVELOPE(18.829,18.829,68.349,68.349) Global Change Biology 27 12 2928 2944
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract Traditionally, biogenic volatile organic compound (BVOC) emissions are often considered a unidirectional flux, from the ecosystem to the atmosphere, but recent studies clearly show the potential for bidirectional exchange. Here we aimed to investigate how warming and leaf litter addition affect the bidirectional exchange (flux) of BVOCs in a long‐term field experiment in the Subarctic. We also assessed changes in net BVOC fluxes in relation to the time of day and the influence of different plant phenological stages. The study was conducted in a full factorial experiment with open top chamber warming and annual litter addition treatments in a tundra heath in Abisko, Northern Sweden. After 18 years of treatments, ecosystem‐level net BVOC fluxes were measured in the experimental plots using proton‐transfer‐reaction time‐of‐flight mass spectrometry (PTR–ToF–MS). The warming treatment increased monoterpene and isoprene emissions by ≈50%. Increasing temperature, due to diurnal variations, can both increase BVOC emission and simultaneously, increase ecosystem uptake. For any given treatment, monoterpene, isoprene, and acetone emissions also increased with increasing ambient air temperatures caused by diurnal variability. Acetaldehyde, methanol, and sesquiterpenes decreased likely due to a deposition flux. For litter addition, only a significant indirect effect on isoprene and monoterpene fluxes (decrease by ~50%–75%) was observed. Litter addition may change soil moisture conditions, leading to changes in plant species composition and biomass, which could subsequently result in changes to BVOC emission compositions. Phenological stages significantly affected fluxes of methanol, isoprene and monoterpenes. We suggest that plant phenological stages differ in impacts on BVOC net emissions, but ambient air temperature and photosynthetically active radiation (PAR) also interact and influence BVOC net emissions differently. Our results may also suggest that BVOC fluxes are not only a response to changes in temperature ...
author2 Det Frie Forskningsråd
Danmarks Grundforskningsfond
H2020 European Research Council
format Article in Journal/Newspaper
author Baggesen, Nanna
Li, Tao
Seco, Roger
Holst, Thomas
Michelsen, Anders
Rinnan, Riikka
spellingShingle Baggesen, Nanna
Li, Tao
Seco, Roger
Holst, Thomas
Michelsen, Anders
Rinnan, Riikka
Phenological stage of tundra vegetation controls bidirectional exchange of BVOCs in a climate change experiment on a subarctic heath
author_facet Baggesen, Nanna
Li, Tao
Seco, Roger
Holst, Thomas
Michelsen, Anders
Rinnan, Riikka
author_sort Baggesen, Nanna
title Phenological stage of tundra vegetation controls bidirectional exchange of BVOCs in a climate change experiment on a subarctic heath
title_short Phenological stage of tundra vegetation controls bidirectional exchange of BVOCs in a climate change experiment on a subarctic heath
title_full Phenological stage of tundra vegetation controls bidirectional exchange of BVOCs in a climate change experiment on a subarctic heath
title_fullStr Phenological stage of tundra vegetation controls bidirectional exchange of BVOCs in a climate change experiment on a subarctic heath
title_full_unstemmed Phenological stage of tundra vegetation controls bidirectional exchange of BVOCs in a climate change experiment on a subarctic heath
title_sort phenological stage of tundra vegetation controls bidirectional exchange of bvocs in a climate change experiment on a subarctic heath
publisher Wiley
publishDate 2021
url http://dx.doi.org/10.1111/gcb.15596
https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.15596
https://onlinelibrary.wiley.com/doi/full-xml/10.1111/gcb.15596
long_lat ENVELOPE(18.829,18.829,68.349,68.349)
geographic Abisko
geographic_facet Abisko
genre Abisko
Northern Sweden
Subarctic
Tundra
genre_facet Abisko
Northern Sweden
Subarctic
Tundra
op_source Global Change Biology
volume 27, issue 12, page 2928-2944
ISSN 1354-1013 1365-2486
op_rights http://creativecommons.org/licenses/by-nc-nd/4.0/
op_doi https://doi.org/10.1111/gcb.15596
container_title Global Change Biology
container_volume 27
container_issue 12
container_start_page 2928
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