Tree biomass does not correlate with soil carbon stocks in forest-tundra ecotones along a 1100 km latitudinal gradient in Norway

Due to climate warming, forests are expanding to higher elevations and latitudes at the expense of tundra vegetation. While the subsequent increase in aboveground biomass is well-documented, there is much speculation regarding the effects on soil organic carbon (SOC) stocks. To provide insight into...

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Main Authors: Devos, Claire Céline, Ohlson, Mikael, Næsset, Erik, Klanderud, Kari, Bollandsås, Ole Martin
Format: Dataset
Language:unknown
Published: 2023
Subjects:
Online Access:https://zenodo.org/record/8132492
https://doi.org/10.5061/dryad.wm37pvmt3
id ftzenodo:oai:zenodo.org:8132492
record_format openpolar
spelling ftzenodo:oai:zenodo.org:8132492 2023-07-30T04:07:19+02:00 Tree biomass does not correlate with soil carbon stocks in forest-tundra ecotones along a 1100 km latitudinal gradient in Norway Devos, Claire Céline Ohlson, Mikael Næsset, Erik Klanderud, Kari Bollandsås, Ole Martin 2023-07-10 https://zenodo.org/record/8132492 https://doi.org/10.5061/dryad.wm37pvmt3 unknown doi:10.1038/s41598-022-17409-3 https://zenodo.org/communities/dryad https://zenodo.org/record/8132492 https://doi.org/10.5061/dryad.wm37pvmt3 oai:zenodo.org:8132492 info:eu-repo/semantics/openAccess https://creativecommons.org/publicdomain/zero/1.0/legalcode boreal forest Tundra treeline Soil carbon Norway Forest-tundra ecotone info:eu-repo/semantics/other dataset 2023 ftzenodo https://doi.org/10.5061/dryad.wm37pvmt310.1038/s41598-022-17409-3 2023-07-11T23:04:24Z Due to climate warming, forests are expanding to higher elevations and latitudes at the expense of tundra vegetation. While the subsequent increase in aboveground biomass is well-documented, there is much speculation regarding the effects on soil organic carbon (SOC) stocks. To provide insight into the consequences of tree encroachment into treeless tundra, we sampled SOC stocks across 36 forest-tundra ecotones along a 1100 km latitudinal gradient in Norway. Our results show that SOC stocks vary greatly within, as well as among treeline ecotones, and that SOC stocks do not correlate with tree biomass and tree species. SOC stocks do increase with temperature, and vary with slope steepness, slope aspect, and soil parent material. Applying a 'space-for-time substitution' perspective, our findings suggest that tree encroachment into tundra is unlikely to have immediate consequences for SOC stocks. Funding provided by: Norges ForskningsrådCrossref Funder Registry ID: http://dx.doi.org/10.13039/501100005416Award Number: 281066Funding provided by: Norges Miljø- og Biovitenskapelige UniversitetCrossref Funder Registry ID: http://dx.doi.org/10.13039/501100008119Award Number: Dataset Tundra Zenodo Norway
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
topic boreal forest
Tundra
treeline
Soil carbon
Norway
Forest-tundra ecotone
spellingShingle boreal forest
Tundra
treeline
Soil carbon
Norway
Forest-tundra ecotone
Devos, Claire Céline
Ohlson, Mikael
Næsset, Erik
Klanderud, Kari
Bollandsås, Ole Martin
Tree biomass does not correlate with soil carbon stocks in forest-tundra ecotones along a 1100 km latitudinal gradient in Norway
topic_facet boreal forest
Tundra
treeline
Soil carbon
Norway
Forest-tundra ecotone
description Due to climate warming, forests are expanding to higher elevations and latitudes at the expense of tundra vegetation. While the subsequent increase in aboveground biomass is well-documented, there is much speculation regarding the effects on soil organic carbon (SOC) stocks. To provide insight into the consequences of tree encroachment into treeless tundra, we sampled SOC stocks across 36 forest-tundra ecotones along a 1100 km latitudinal gradient in Norway. Our results show that SOC stocks vary greatly within, as well as among treeline ecotones, and that SOC stocks do not correlate with tree biomass and tree species. SOC stocks do increase with temperature, and vary with slope steepness, slope aspect, and soil parent material. Applying a 'space-for-time substitution' perspective, our findings suggest that tree encroachment into tundra is unlikely to have immediate consequences for SOC stocks. Funding provided by: Norges ForskningsrådCrossref Funder Registry ID: http://dx.doi.org/10.13039/501100005416Award Number: 281066Funding provided by: Norges Miljø- og Biovitenskapelige UniversitetCrossref Funder Registry ID: http://dx.doi.org/10.13039/501100008119Award Number:
format Dataset
author Devos, Claire Céline
Ohlson, Mikael
Næsset, Erik
Klanderud, Kari
Bollandsås, Ole Martin
author_facet Devos, Claire Céline
Ohlson, Mikael
Næsset, Erik
Klanderud, Kari
Bollandsås, Ole Martin
author_sort Devos, Claire Céline
title Tree biomass does not correlate with soil carbon stocks in forest-tundra ecotones along a 1100 km latitudinal gradient in Norway
title_short Tree biomass does not correlate with soil carbon stocks in forest-tundra ecotones along a 1100 km latitudinal gradient in Norway
title_full Tree biomass does not correlate with soil carbon stocks in forest-tundra ecotones along a 1100 km latitudinal gradient in Norway
title_fullStr Tree biomass does not correlate with soil carbon stocks in forest-tundra ecotones along a 1100 km latitudinal gradient in Norway
title_full_unstemmed Tree biomass does not correlate with soil carbon stocks in forest-tundra ecotones along a 1100 km latitudinal gradient in Norway
title_sort tree biomass does not correlate with soil carbon stocks in forest-tundra ecotones along a 1100 km latitudinal gradient in norway
publishDate 2023
url https://zenodo.org/record/8132492
https://doi.org/10.5061/dryad.wm37pvmt3
geographic Norway
geographic_facet Norway
genre Tundra
genre_facet Tundra
op_relation doi:10.1038/s41598-022-17409-3
https://zenodo.org/communities/dryad
https://zenodo.org/record/8132492
https://doi.org/10.5061/dryad.wm37pvmt3
oai:zenodo.org:8132492
op_rights info:eu-repo/semantics/openAccess
https://creativecommons.org/publicdomain/zero/1.0/legalcode
op_doi https://doi.org/10.5061/dryad.wm37pvmt310.1038/s41598-022-17409-3
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