Long-term ecological consequences of forest fires in the continuous permafrost zone of Siberia ...

Abstract Wildfires are an important factor in controlling forest ecosystem dynamics across the circumpolar boreal zone. An improved understanding of their direct and indirect, short- to long-term impacts on vegetation cover and permafrost–vegetation coupling is particularly important to predict chan...

Full description

Bibliographic Details
Main Authors: Kirdyanov, AV, Saurer, M, Siegwolf, R, Knorre, AA, Prokushkin, AS, Churakova, OV, Fonti, MV, Büntgen, U
Format: Article in Journal/Newspaper
Language:English
Published: IOP Publishing 2020
Subjects:
Online Access:https://dx.doi.org/10.17863/cam.50177
https://www.repository.cam.ac.uk/handle/1810/303100
id ftdatacite:10.17863/cam.50177
record_format openpolar
spelling ftdatacite:10.17863/cam.50177 2024-02-27T08:44:26+00:00 Long-term ecological consequences of forest fires in the continuous permafrost zone of Siberia ... Kirdyanov, AV Saurer, M Siegwolf, R Knorre, AA Prokushkin, AS Churakova, OV Fonti, MV Büntgen, U 2020 https://dx.doi.org/10.17863/cam.50177 https://www.repository.cam.ac.uk/handle/1810/303100 en eng IOP Publishing open.access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 active soil layer boreal forest permafrost Siberia stable isotopes tree rings wildfire CreativeWork Other article 2020 ftdatacite https://doi.org/10.17863/cam.50177 2024-02-01T14:52:52Z Abstract Wildfires are an important factor in controlling forest ecosystem dynamics across the circumpolar boreal zone. An improved understanding of their direct and indirect, short- to long-term impacts on vegetation cover and permafrost–vegetation coupling is particularly important to predict changes in carbon, nutrient and water cycles under projected climate warming. Here, we apply dendrochronological techniques on a multi-parameter dataset to reconstruct the effect of wildfires on tree growth and seasonal permafrost thaw depth in Central Siberia. Based on annually-resolved and absolutely dated information from 19 Gmelin larch (Larix gmelinii (Rupr.) Rupr.) trees and active soil layer thickness measurements, we find substantial stand-level die-off, as well as the removal of ground vegetation and the organic layer following a major wildfire in 1896. Reduced stem growth coincides with increased δ 13 C in the cellulose of the surviving trees during the first decade after the wildfire, when stomatal ... Article in Journal/Newspaper permafrost Siberia DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic active soil layer
boreal forest
permafrost
Siberia
stable isotopes
tree rings
wildfire
spellingShingle active soil layer
boreal forest
permafrost
Siberia
stable isotopes
tree rings
wildfire
Kirdyanov, AV
Saurer, M
Siegwolf, R
Knorre, AA
Prokushkin, AS
Churakova, OV
Fonti, MV
Büntgen, U
Long-term ecological consequences of forest fires in the continuous permafrost zone of Siberia ...
topic_facet active soil layer
boreal forest
permafrost
Siberia
stable isotopes
tree rings
wildfire
description Abstract Wildfires are an important factor in controlling forest ecosystem dynamics across the circumpolar boreal zone. An improved understanding of their direct and indirect, short- to long-term impacts on vegetation cover and permafrost–vegetation coupling is particularly important to predict changes in carbon, nutrient and water cycles under projected climate warming. Here, we apply dendrochronological techniques on a multi-parameter dataset to reconstruct the effect of wildfires on tree growth and seasonal permafrost thaw depth in Central Siberia. Based on annually-resolved and absolutely dated information from 19 Gmelin larch (Larix gmelinii (Rupr.) Rupr.) trees and active soil layer thickness measurements, we find substantial stand-level die-off, as well as the removal of ground vegetation and the organic layer following a major wildfire in 1896. Reduced stem growth coincides with increased δ 13 C in the cellulose of the surviving trees during the first decade after the wildfire, when stomatal ...
format Article in Journal/Newspaper
author Kirdyanov, AV
Saurer, M
Siegwolf, R
Knorre, AA
Prokushkin, AS
Churakova, OV
Fonti, MV
Büntgen, U
author_facet Kirdyanov, AV
Saurer, M
Siegwolf, R
Knorre, AA
Prokushkin, AS
Churakova, OV
Fonti, MV
Büntgen, U
author_sort Kirdyanov, AV
title Long-term ecological consequences of forest fires in the continuous permafrost zone of Siberia ...
title_short Long-term ecological consequences of forest fires in the continuous permafrost zone of Siberia ...
title_full Long-term ecological consequences of forest fires in the continuous permafrost zone of Siberia ...
title_fullStr Long-term ecological consequences of forest fires in the continuous permafrost zone of Siberia ...
title_full_unstemmed Long-term ecological consequences of forest fires in the continuous permafrost zone of Siberia ...
title_sort long-term ecological consequences of forest fires in the continuous permafrost zone of siberia ...
publisher IOP Publishing
publishDate 2020
url https://dx.doi.org/10.17863/cam.50177
https://www.repository.cam.ac.uk/handle/1810/303100
genre permafrost
Siberia
genre_facet permafrost
Siberia
op_rights open.access
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
http://purl.org/coar/access_right/c_abf2
op_doi https://doi.org/10.17863/cam.50177
_version_ 1792052865783562240