The impact of wildfire on microbial C:N:P stoichiometry and the fungal-to-bacterial ratio in permafrost soil

Wildfires thaw near-surface permafrost soils in the boreal forest, making previously frozen organic matter available to microbes. The short-term microbial stoichiometric dynamics following a wildfire are critical to understanding the soil element variations in thawing permafrost. Thus, we selected a...

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Published in:Biogeochemistry
Main Authors: Zhou, Xuan, Sun, Hui, Pumpanen, Jukka, Sietiö, Outi-Maaria, Heinonsalo, Jussi, Köster, Kajar, Berninger, Frank
Other Authors: Ympäristö- ja biotieteiden laitos / Toiminta
Format: Article in Journal/Newspaper
Language:unknown
Published: Springer Nature America, Inc 2018
Subjects:
Online Access:https://erepo.uef.fi/handle/123456789/7203
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spelling ftuniveasternfin:oai:erepo.uef.fi:123456789/7203 2024-06-16T07:42:37+00:00 The impact of wildfire on microbial C:N:P stoichiometry and the fungal-to-bacterial ratio in permafrost soil Zhou, Xuan Sun, Hui Pumpanen, Jukka Sietiö, Outi-Maaria Heinonsalo, Jussi Köster, Kajar Berninger, Frank Ympäristö- ja biotieteiden laitos / Toiminta 2018-12-17T12:52:10Z 1-17 https://erepo.uef.fi/handle/123456789/7203 englanti unknown Springer Nature America, Inc Alankomaat BIOGEOCHEMISTRY http://dx.doi.org/10.1007/s10533-018-0510-6 10.1007/s10533-018-0510-6 0168-2563 1 142 https://erepo.uef.fi/handle/123456789/7203 CC BY 4.0 openAccess © Authors https://creativecommons.org/licenses/by/4.0/ wildfire boreal forest permafrost microbial biomass C:N:P stoichiometry homeostasis fungal-to-bacterial ratio Tieteelliset aikakauslehtiartikkelit A1 article artikkeli 2018 ftuniveasternfin https://doi.org/10.1007/s10533-018-0510-6 2024-05-23T03:07:27Z Wildfires thaw near-surface permafrost soils in the boreal forest, making previously frozen organic matter available to microbes. The short-term microbial stoichiometric dynamics following a wildfire are critical to understanding the soil element variations in thawing permafrost. Thus, we selected a boreal wildfire chronosequence in a region of continuous permafrost, where the last wildfire occurred 3, 25, 46, and > 100 years ago (set as the control) to explore the impact of wildfire on the soil chemistry, soil microbial stoichiometry, and the fungal-to-bacterial gene ratio (F:B ratio). We observed the microbial biomass C:N:P ratio remained constant in distinct age classes indicating that microbes are homeostatic in relation to stoichiometric ratios. The microbial C:N ratios were independent of the shifts in the fungal-to-bacterial ratio when C:N exceeded 12. Wildfire-induced reduction in vegetation biomass positively affected the fungal, but not the bacterial, gene copy number. The decline in microbial biomass C, N, and P following a fire, primarily resulted from a lack of soil available C and nutrients. Wildfire affected neither the microbial biomass nor the F:B ratios at a soil depth of 30 cm. We conclude that microbial stoichiometry does not always respond to changes in the fungal-to-bacterial ratio and that wildfire-induced permafrost thawing does not accelerate microbial respiration. published version peerReviewed Article in Journal/Newspaper permafrost UEF eRepository (University of Eastern Finland) Biogeochemistry 142 1 1 17
institution Open Polar
collection UEF eRepository (University of Eastern Finland)
op_collection_id ftuniveasternfin
language unknown
topic wildfire
boreal forest
permafrost
microbial biomass
C:N:P stoichiometry
homeostasis
fungal-to-bacterial ratio
spellingShingle wildfire
boreal forest
permafrost
microbial biomass
C:N:P stoichiometry
homeostasis
fungal-to-bacterial ratio
Zhou, Xuan
Sun, Hui
Pumpanen, Jukka
Sietiö, Outi-Maaria
Heinonsalo, Jussi
Köster, Kajar
Berninger, Frank
The impact of wildfire on microbial C:N:P stoichiometry and the fungal-to-bacterial ratio in permafrost soil
topic_facet wildfire
boreal forest
permafrost
microbial biomass
C:N:P stoichiometry
homeostasis
fungal-to-bacterial ratio
description Wildfires thaw near-surface permafrost soils in the boreal forest, making previously frozen organic matter available to microbes. The short-term microbial stoichiometric dynamics following a wildfire are critical to understanding the soil element variations in thawing permafrost. Thus, we selected a boreal wildfire chronosequence in a region of continuous permafrost, where the last wildfire occurred 3, 25, 46, and > 100 years ago (set as the control) to explore the impact of wildfire on the soil chemistry, soil microbial stoichiometry, and the fungal-to-bacterial gene ratio (F:B ratio). We observed the microbial biomass C:N:P ratio remained constant in distinct age classes indicating that microbes are homeostatic in relation to stoichiometric ratios. The microbial C:N ratios were independent of the shifts in the fungal-to-bacterial ratio when C:N exceeded 12. Wildfire-induced reduction in vegetation biomass positively affected the fungal, but not the bacterial, gene copy number. The decline in microbial biomass C, N, and P following a fire, primarily resulted from a lack of soil available C and nutrients. Wildfire affected neither the microbial biomass nor the F:B ratios at a soil depth of 30 cm. We conclude that microbial stoichiometry does not always respond to changes in the fungal-to-bacterial ratio and that wildfire-induced permafrost thawing does not accelerate microbial respiration. published version peerReviewed
author2 Ympäristö- ja biotieteiden laitos / Toiminta
format Article in Journal/Newspaper
author Zhou, Xuan
Sun, Hui
Pumpanen, Jukka
Sietiö, Outi-Maaria
Heinonsalo, Jussi
Köster, Kajar
Berninger, Frank
author_facet Zhou, Xuan
Sun, Hui
Pumpanen, Jukka
Sietiö, Outi-Maaria
Heinonsalo, Jussi
Köster, Kajar
Berninger, Frank
author_sort Zhou, Xuan
title The impact of wildfire on microbial C:N:P stoichiometry and the fungal-to-bacterial ratio in permafrost soil
title_short The impact of wildfire on microbial C:N:P stoichiometry and the fungal-to-bacterial ratio in permafrost soil
title_full The impact of wildfire on microbial C:N:P stoichiometry and the fungal-to-bacterial ratio in permafrost soil
title_fullStr The impact of wildfire on microbial C:N:P stoichiometry and the fungal-to-bacterial ratio in permafrost soil
title_full_unstemmed The impact of wildfire on microbial C:N:P stoichiometry and the fungal-to-bacterial ratio in permafrost soil
title_sort impact of wildfire on microbial c:n:p stoichiometry and the fungal-to-bacterial ratio in permafrost soil
publisher Springer Nature America, Inc
publishDate 2018
url https://erepo.uef.fi/handle/123456789/7203
genre permafrost
genre_facet permafrost
op_relation BIOGEOCHEMISTRY
http://dx.doi.org/10.1007/s10533-018-0510-6
10.1007/s10533-018-0510-6
0168-2563
1
142
https://erepo.uef.fi/handle/123456789/7203
op_rights CC BY 4.0
openAccess
© Authors
https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1007/s10533-018-0510-6
container_title Biogeochemistry
container_volume 142
container_issue 1
container_start_page 1
op_container_end_page 17
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