Post-fire carbon and nitrogen accumulation and succession in Central Siberia

Improved understanding of carbon (C) accumulation after a boreal fire enables more accurate quantification of the C implications caused by potential fire regime shifts. We coupled results from a fire history study with biomass and soil sampling in a remote and little-studied region that represents a...

Full description

Bibliographic Details
Published in:Scientific Reports
Main Authors: Larjavaara, Markku, Berninger, Frank, Palviainen, Marjo, Prokushkin, Anatoly, Wallenius, Tuomo
Other Authors: Department of Forest Sciences, University of Helsinki, Ecosystem processes (INAR Faculty of Agriculture and Forestry), Forest Soil Science, Viikki Tropical Resources Institute (VITRI), Forest Ecology and Management
Format: Article in Journal/Newspaper
Language:English
Published: Nature Research 2017
Subjects:
Online Access:http://hdl.handle.net/10138/228110
_version_ 1831836305512726528
author Larjavaara, Markku
Berninger, Frank
Palviainen, Marjo
Prokushkin, Anatoly
Wallenius, Tuomo
author2 Department of Forest Sciences
University of Helsinki
Ecosystem processes (INAR Faculty of Agriculture and Forestry)
Forest Soil Science
Viikki Tropical Resources Institute (VITRI)
Forest Ecology and Management
author_facet Larjavaara, Markku
Berninger, Frank
Palviainen, Marjo
Prokushkin, Anatoly
Wallenius, Tuomo
author_sort Larjavaara, Markku
collection HELDA – University of Helsinki Open Repository
container_issue 1
container_title Scientific Reports
container_volume 7
description Improved understanding of carbon (C) accumulation after a boreal fire enables more accurate quantification of the C implications caused by potential fire regime shifts. We coupled results from a fire history study with biomass and soil sampling in a remote and little-studied region that represents a vast area of boreal taiga. We used an inventory approach based on predefined plot locations, thus avoiding problems potentially causing bias related to the standard chronosequence approach. The disadvantage of our inventory approach is that more plots are needed to expose trends. Because of this we could not expose clear trends, despite laborious sampling. We found some support for increasing C and nitrogen (N) stored in living trees and dead wood with increasing time since the previous fire or time since the previous stand-replacing fire. Surprisingly, we did not gain support for the well-established paradigm on successional patterns, beginning with angiosperms and leading, if fires are absent, to dominance of Picea. Despite the lack of clear trends in our data, we encourage fire historians and ecosystem scientists to join forces and use even larger data sets to study C accumulation since fire in the complex Eurasian boreal landscapes. Peer reviewed
format Article in Journal/Newspaper
genre taiga
Siberia
genre_facet taiga
Siberia
geographic Norway
geographic_facet Norway
id ftunivhelsihelda:oai:helda.helsinki.fi:10138/228110
institution Open Polar
language English
op_collection_id ftunivhelsihelda
op_relation 10.1038/s41598-017-13039-2
We thank Toivo Haltia, Antti Lavikainen and Aleksey Sadvordaev for their company and help in the field, Markus Saarinen, Riina Jarvela and Marjut Wallner for laboratory work and Olga Shibistova for valuable information on the region, Vladimir L. Gavrikov for advice on allometric equations, Stella Thompson on linguistic editing and Oskar Ofluds Stiftelse, Nordenskiolds Samfundet, the Academy of Finland (ARCTICFIRE project no. 286685), the Russian Science Foundation (RSF 14-24-00113) and Ulla Wallenius for funding.
http://hdl.handle.net/10138/228110
85030792057
000412492400002
op_rights cc_by
info:eu-repo/semantics/openAccess
openAccess
publishDate 2017
publisher Nature Research
record_format openpolar
spelling ftunivhelsihelda:oai:helda.helsinki.fi:10138/228110 2025-05-11T14:25:36+00:00 Post-fire carbon and nitrogen accumulation and succession in Central Siberia Larjavaara, Markku Berninger, Frank Palviainen, Marjo Prokushkin, Anatoly Wallenius, Tuomo Department of Forest Sciences University of Helsinki Ecosystem processes (INAR Faculty of Agriculture and Forestry) Forest Soil Science Viikki Tropical Resources Institute (VITRI) Forest Ecology and Management 2017-10-30T11:40:01Z 11 application/pdf http://hdl.handle.net/10138/228110 eng eng Nature Research 10.1038/s41598-017-13039-2 We thank Toivo Haltia, Antti Lavikainen and Aleksey Sadvordaev for their company and help in the field, Markus Saarinen, Riina Jarvela and Marjut Wallner for laboratory work and Olga Shibistova for valuable information on the region, Vladimir L. Gavrikov for advice on allometric equations, Stella Thompson on linguistic editing and Oskar Ofluds Stiftelse, Nordenskiolds Samfundet, the Academy of Finland (ARCTICFIRE project no. 286685), the Russian Science Foundation (RSF 14-24-00113) and Ulla Wallenius for funding. http://hdl.handle.net/10138/228110 85030792057 000412492400002 cc_by info:eu-repo/semantics/openAccess openAccess SPRUCE WILDFIRE CHRONOSEQUENCE STAND-REPLACING DISTURBANCES CLIMATE-CHANGE IMPACTS SCOTS PINE FORESTS BOREAL FOREST ABOVEGROUND BIOMASS NORWAY SPRUCE BIRCH STEMS GLOBAL CHANGE SILVER BIRCH Forestry Article publishedVersion 2017 ftunivhelsihelda 2025-04-15T00:14:10Z Improved understanding of carbon (C) accumulation after a boreal fire enables more accurate quantification of the C implications caused by potential fire regime shifts. We coupled results from a fire history study with biomass and soil sampling in a remote and little-studied region that represents a vast area of boreal taiga. We used an inventory approach based on predefined plot locations, thus avoiding problems potentially causing bias related to the standard chronosequence approach. The disadvantage of our inventory approach is that more plots are needed to expose trends. Because of this we could not expose clear trends, despite laborious sampling. We found some support for increasing C and nitrogen (N) stored in living trees and dead wood with increasing time since the previous fire or time since the previous stand-replacing fire. Surprisingly, we did not gain support for the well-established paradigm on successional patterns, beginning with angiosperms and leading, if fires are absent, to dominance of Picea. Despite the lack of clear trends in our data, we encourage fire historians and ecosystem scientists to join forces and use even larger data sets to study C accumulation since fire in the complex Eurasian boreal landscapes. Peer reviewed Article in Journal/Newspaper taiga Siberia HELDA – University of Helsinki Open Repository Norway Scientific Reports 7 1
spellingShingle SPRUCE WILDFIRE CHRONOSEQUENCE
STAND-REPLACING DISTURBANCES
CLIMATE-CHANGE IMPACTS
SCOTS PINE FORESTS
BOREAL FOREST
ABOVEGROUND BIOMASS
NORWAY SPRUCE
BIRCH STEMS
GLOBAL CHANGE
SILVER BIRCH
Forestry
Larjavaara, Markku
Berninger, Frank
Palviainen, Marjo
Prokushkin, Anatoly
Wallenius, Tuomo
Post-fire carbon and nitrogen accumulation and succession in Central Siberia
title Post-fire carbon and nitrogen accumulation and succession in Central Siberia
title_full Post-fire carbon and nitrogen accumulation and succession in Central Siberia
title_fullStr Post-fire carbon and nitrogen accumulation and succession in Central Siberia
title_full_unstemmed Post-fire carbon and nitrogen accumulation and succession in Central Siberia
title_short Post-fire carbon and nitrogen accumulation and succession in Central Siberia
title_sort post-fire carbon and nitrogen accumulation and succession in central siberia
topic SPRUCE WILDFIRE CHRONOSEQUENCE
STAND-REPLACING DISTURBANCES
CLIMATE-CHANGE IMPACTS
SCOTS PINE FORESTS
BOREAL FOREST
ABOVEGROUND BIOMASS
NORWAY SPRUCE
BIRCH STEMS
GLOBAL CHANGE
SILVER BIRCH
Forestry
topic_facet SPRUCE WILDFIRE CHRONOSEQUENCE
STAND-REPLACING DISTURBANCES
CLIMATE-CHANGE IMPACTS
SCOTS PINE FORESTS
BOREAL FOREST
ABOVEGROUND BIOMASS
NORWAY SPRUCE
BIRCH STEMS
GLOBAL CHANGE
SILVER BIRCH
Forestry
url http://hdl.handle.net/10138/228110