Soil organic and phytomass carbon stocks in mountain periglacial settings of Vindelfjällen (Sweden)

We present a detailed soil organic carbon (SOC) and phytomass carbon (C) inventory for a mountain periglacial region in northwest Sweden (altitude range c. 600–1,800 m). We describe plant cover and soil profiles at thirty-nine sites representing the main land cover classes at and above tree line. The mean landscape-level SOC storage for full soil depth is 7.14 kg C m−2, which includes 35 percent of high-alpine ice/snow and bare ground surfaces with negligible SOC stocks. The main SOC hotspots are boreal (maximum stock of 118.5 kg C m−2) and alpine (maximum stock of 79.9 kg C m−2) wetlands. Solifluction lobes in the alpine belt hold above average but highly variable SOC stocks (2.11–19.5 kg C m−2). Permafrost was only encountered in small remnants of collapsing palsas, holding negligible SOC stocks. Mean phytomass C storage is 0.36 kg C m−2, with birch forest storing on average about twenty times more phytomass C (4.41 kg C m−2) compared to the mean for the upland alpine tundra classes (0.20 kg C m−2). Projected increases in ambient temperatures will likely result in an upward shift of the tree line and the alpine vegetation belt with a potential increase in phytomass C and SOC stocks.

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Publication Details

Journal
Arctic Antarctic and Alpine Research
Published
2024-08-09
DOI
https://doi.org/10.1080/15230430.2024.2366333
Primary Topic
Climate change and permafrost
Type
article
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article

Soil organic and phytomass carbon stocks in mountain periglacial settings of Vindelfjällen (Sweden)

Christina Fröjd, Berta González Sánchez, Peter Kuhry
Arctic Antarctic and Alpine Research
Climate change and permafrost
article

Soil organic and phytomass carbon stocks in mountain periglacial settings of Vindelfjällen (Sweden)

Christina Fröjd, Berta González Sánchez, Peter Kuhry
article en

Abstract

We present a detailed soil organic carbon (SOC) and phytomass carbon (C) inventory for a mountain periglacial region in northwest Sweden (altitude range c. 600–1,800 m). We describe plant cover and soil profiles at thirty-nine sites representing the main land cover classes at and above tree line. The mean landscape-level SOC storage for full soil depth is 7.14 kg C m−2, which includes 35 percent of high-alpine ice/snow and bare ground surfaces with negligible SOC stocks. The main SOC hotspots are boreal (maximum stock of 118.5 kg C m−2) and alpine (maximum stock of 79.9 kg C m−2) wetlands. Solifluction lobes in the alpine belt hold above average but highly variable SOC stocks (2.11–19.5 kg C m−2). Permafrost was only encountered in small remnants of collapsing palsas, holding negligible SOC stocks. Mean phytomass C storage is 0.36 kg C m−2, with birch forest storing on average about twenty times more phytomass C (4.41 kg C m−2) compared to the mean for the upland alpine tundra classes (0.20 kg C m−2). Projected increases in ambient temperatures will likely result in an upward shift of the tree line and the alpine vegetation belt with a potential increase in phytomass C and SOC stocks.

Arctic Antarctic and Alpine ResearchVol. 56(1)
Stockholm University (SE), Bolin Centre for Climate Research (SE)
Openalex Percentile: Top 83%
Climate change and permafrost
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Soil organic and phytomass carbon stocks in mountain periglacial settings of Vindelfjällen (Sweden) — Christina Fröjd, Berta González Sánchez, et al. · Arctic Antarctic and Alpine Research (2024) | TGRS Research Map | TGRS