Mineralization and carbon turnover in subarctic heath soil as affected by warming and additional litter

Riikka Rinnan; Anders Michelsen; Erland Baath; Sven Evert Jonasson

doi:10.1016/j.soilbio.2007.05.035

Mineralization and carbon turnover in subarctic heath soil as affected by warming and additional litter

Riikka Rinnan, Anders Michelsen, Erland Baath, Sven Evert Jonasson

Terrestrial Ecology

Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › peer review

81 Citationer (Scopus)

Abstract

Udgivelsesdato: December 2007

Originalsprog	Engelsk
Tidsskrift	Soil Biology & Biochemistry
Vol/bind	39
Udgave nummer	12
Sider (fra-til)	3014-3023
ISSN	0038-0717
DOI	https://doi.org/10.1016/j.soilbio.2007.05.035
Status	Udgivet - 2007

Bibliografisk note

Keywords: Arctic; Climate change; Litter; Mineralization; Immobilization; Soil carbon; Bacterial growth; Thymidine; Leucine

Adgang til dokumentet

10.1016/j.soilbio.2007.05.035

Citationsformater

@article{c03e11e0241511de9f0a000ea68e967b,

title = "Mineralization and carbon turnover in subarctic heath soil as affected by warming and additional litter",

abstract = "Arctic soil carbon (C) stocks are threatened by the rapidly advancing global warming. In addition to temperature, increasing amounts of leaf litter fall following from the expansion of deciduous shrubs and trees in northern ecosystems may alter biogeochemical cycling of C and nutrients. Our aim was to assess how factorial warming and litter addition in a long-term field experiment on a subarctic heath affect resource limitation of soil microbial communities (measured by thymidine and leucine incorporation techniques), net growing-season mineralization of nitrogen (N) and phosphorus (P), and carbon turnover (measured as changes in the pools during a growing-season-long field incubation of soil cores in situ). The mainly N limited bacterial communities had shifted slightly towards limitation by C and P in response to seven growing seasons of warming. This and the significantly increased bacterial growth rate under warming may partly explain the observed higher C loss from the warmed soil. This is furthermore consistent with the less dramatic increase in the contents of dissolved organic carbon (DOC) and dissolved organic N (DON) in the warmed soil than in the soil from ambient temperature during the field incubation. The added litter did not affect the carbon content, but it was a source of nutrients to the soil, and it also tended to increase bacterial growth rate and net mineralization of P. The inorganic N pool decreased during the field incubation of soil cores, especially in the separate warming and litter addition treatments, while gross mineralized N was immobilized in the biomass of microbes and plants transplanted into the incubates soil cores, but without any significant effect of the treatments. The effects of warming plus litter addition on bacterial growth rates and of warming on C and N transformations during field incubation suggest that microbial activity is an important control on the carbon balance of arctic soils under climate change.",

author = "Riikka Rinnan and Anders Michelsen and Erland Baath and Jonasson, {Sven Evert}",

note = "Keywords: Arctic; Climate change; Litter; Mineralization; Immobilization; Soil carbon; Bacterial growth; Thymidine; Leucine",

year = "2007",

doi = "10.1016/j.soilbio.2007.05.035",

language = "English",

volume = "39",

pages = "3014--3023",

journal = "Soil Biology & Biochemistry",

issn = "0038-0717",

publisher = "Pergamon Press",

number = "12",

}

TY - JOUR

T1 - Mineralization and carbon turnover in subarctic heath soil as affected by warming and additional litter

AU - Rinnan, Riikka

AU - Michelsen, Anders

AU - Baath, Erland

AU - Jonasson, Sven Evert

N1 - Keywords: Arctic; Climate change; Litter; Mineralization; Immobilization; Soil carbon; Bacterial growth; Thymidine; Leucine

PY - 2007

Y1 - 2007

N2 - Arctic soil carbon (C) stocks are threatened by the rapidly advancing global warming. In addition to temperature, increasing amounts of leaf litter fall following from the expansion of deciduous shrubs and trees in northern ecosystems may alter biogeochemical cycling of C and nutrients. Our aim was to assess how factorial warming and litter addition in a long-term field experiment on a subarctic heath affect resource limitation of soil microbial communities (measured by thymidine and leucine incorporation techniques), net growing-season mineralization of nitrogen (N) and phosphorus (P), and carbon turnover (measured as changes in the pools during a growing-season-long field incubation of soil cores in situ). The mainly N limited bacterial communities had shifted slightly towards limitation by C and P in response to seven growing seasons of warming. This and the significantly increased bacterial growth rate under warming may partly explain the observed higher C loss from the warmed soil. This is furthermore consistent with the less dramatic increase in the contents of dissolved organic carbon (DOC) and dissolved organic N (DON) in the warmed soil than in the soil from ambient temperature during the field incubation. The added litter did not affect the carbon content, but it was a source of nutrients to the soil, and it also tended to increase bacterial growth rate and net mineralization of P. The inorganic N pool decreased during the field incubation of soil cores, especially in the separate warming and litter addition treatments, while gross mineralized N was immobilized in the biomass of microbes and plants transplanted into the incubates soil cores, but without any significant effect of the treatments. The effects of warming plus litter addition on bacterial growth rates and of warming on C and N transformations during field incubation suggest that microbial activity is an important control on the carbon balance of arctic soils under climate change.

AB - Arctic soil carbon (C) stocks are threatened by the rapidly advancing global warming. In addition to temperature, increasing amounts of leaf litter fall following from the expansion of deciduous shrubs and trees in northern ecosystems may alter biogeochemical cycling of C and nutrients. Our aim was to assess how factorial warming and litter addition in a long-term field experiment on a subarctic heath affect resource limitation of soil microbial communities (measured by thymidine and leucine incorporation techniques), net growing-season mineralization of nitrogen (N) and phosphorus (P), and carbon turnover (measured as changes in the pools during a growing-season-long field incubation of soil cores in situ). The mainly N limited bacterial communities had shifted slightly towards limitation by C and P in response to seven growing seasons of warming. This and the significantly increased bacterial growth rate under warming may partly explain the observed higher C loss from the warmed soil. This is furthermore consistent with the less dramatic increase in the contents of dissolved organic carbon (DOC) and dissolved organic N (DON) in the warmed soil than in the soil from ambient temperature during the field incubation. The added litter did not affect the carbon content, but it was a source of nutrients to the soil, and it also tended to increase bacterial growth rate and net mineralization of P. The inorganic N pool decreased during the field incubation of soil cores, especially in the separate warming and litter addition treatments, while gross mineralized N was immobilized in the biomass of microbes and plants transplanted into the incubates soil cores, but without any significant effect of the treatments. The effects of warming plus litter addition on bacterial growth rates and of warming on C and N transformations during field incubation suggest that microbial activity is an important control on the carbon balance of arctic soils under climate change.

U2 - 10.1016/j.soilbio.2007.05.035

DO - 10.1016/j.soilbio.2007.05.035

M3 - Journal article

SN - 0038-0717

VL - 39

SP - 3014

EP - 3023

JO - Soil Biology & Biochemistry

JF - Soil Biology & Biochemistry

IS - 12

ER -