The age of CO2 released from soils in contrasting ecosystems during the arctic winter

Iain P Hartley; Mark H Garnett; Martin Sommerkorn; David William Hopkins; Philip A Wookey

doi:10.1016/j.soilbio.2013.03.011

The age of CO₂ released from soils in contrasting ecosystems during the arctic winter

Iain P Hartley, Mark H Garnett, Martin Sommerkorn, David William Hopkins, Philip A Wookey

Research output: Contribution to journal › Article › peer-review

8 Citations (Scopus)

Abstract

In arctic ecosystems, winter soil respiration can contribute substantially to annual CO2 release, yet the source of this C is not clear. We analysed the C-14 content of C released from plant-free plots in mountain birch forest and tundra-heath. Winter-respired CO2 was found to be a similar age (tundra) or older (forest) than C released during the previous autumn. Overall, our study demonstrates that the decomposition of older C can continue during the winter, in these two contrasting arctic ecosystems. (c) 2013 Elsevier Ltd. All rights reserved.

Original language	English
Pages (from-to)	1-4
Number of pages	4
Journal	Soil Biology and Biochemistry
Volume	63
DOIs	https://doi.org/10.1016/j.soilbio.2013.03.011
Publication status	Published - Aug 2013

Keywords

(CO2)-C-14
Passive sampling
Mountain birch
Radiocarbon
Tree-line
Tundra-heath
Winter respiration
TEMPERATURE SENSITIVITY
MOLECULAR-SIEVE
VEGETATION TYPE
ORGANIC-CARBON
CLIMATE-CHANGE
RESPIRATION
DECOMPOSITION
REGION
TUNDRA
STOCKS

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

Access to Document

10.1016/j.soilbio.2013.03.011

Cite this

@article{f2e728e90e544192b65e57aacea59bae,

title = "The age of CO2 released from soils in contrasting ecosystems during the arctic winter",

abstract = "In arctic ecosystems, winter soil respiration can contribute substantially to annual CO2 release, yet the source of this C is not clear. We analysed the C-14 content of C released from plant-free plots in mountain birch forest and tundra-heath. Winter-respired CO2 was found to be a similar age (tundra) or older (forest) than C released during the previous autumn. Overall, our study demonstrates that the decomposition of older C can continue during the winter, in these two contrasting arctic ecosystems. (c) 2013 Elsevier Ltd. All rights reserved.",

keywords = "(CO2)-C-14, Passive sampling, Mountain birch, Radiocarbon, Tree-line, Tundra-heath, Winter respiration, TEMPERATURE SENSITIVITY, MOLECULAR-SIEVE, VEGETATION TYPE, ORGANIC-CARBON, CLIMATE-CHANGE, RESPIRATION, DECOMPOSITION, REGION, TUNDRA, STOCKS",

author = "Hartley, {Iain P} and Garnett, {Mark H} and Martin Sommerkorn and Hopkins, {David William} and Wookey, {Philip A}",

year = "2013",

month = aug,

doi = "10.1016/j.soilbio.2013.03.011",

language = "English",

volume = "63",

pages = "1--4",

journal = "Soil Biology and Biochemistry",

issn = "0038-0717",

publisher = "Elsevier",

}

TY - JOUR

T1 - The age of CO2 released from soils in contrasting ecosystems during the arctic winter

AU - Hartley, Iain P

AU - Garnett, Mark H

AU - Sommerkorn, Martin

AU - Hopkins, David William

AU - Wookey, Philip A

PY - 2013/8

Y1 - 2013/8

N2 - In arctic ecosystems, winter soil respiration can contribute substantially to annual CO2 release, yet the source of this C is not clear. We analysed the C-14 content of C released from plant-free plots in mountain birch forest and tundra-heath. Winter-respired CO2 was found to be a similar age (tundra) or older (forest) than C released during the previous autumn. Overall, our study demonstrates that the decomposition of older C can continue during the winter, in these two contrasting arctic ecosystems. (c) 2013 Elsevier Ltd. All rights reserved.

AB - In arctic ecosystems, winter soil respiration can contribute substantially to annual CO2 release, yet the source of this C is not clear. We analysed the C-14 content of C released from plant-free plots in mountain birch forest and tundra-heath. Winter-respired CO2 was found to be a similar age (tundra) or older (forest) than C released during the previous autumn. Overall, our study demonstrates that the decomposition of older C can continue during the winter, in these two contrasting arctic ecosystems. (c) 2013 Elsevier Ltd. All rights reserved.

KW - (CO2)-C-14

KW - Passive sampling

KW - Mountain birch

KW - Radiocarbon

KW - Tree-line

KW - Tundra-heath

KW - Winter respiration

KW - TEMPERATURE SENSITIVITY

KW - MOLECULAR-SIEVE

KW - VEGETATION TYPE

KW - ORGANIC-CARBON

KW - CLIMATE-CHANGE

KW - RESPIRATION

KW - DECOMPOSITION

KW - REGION

KW - TUNDRA

KW - STOCKS

U2 - 10.1016/j.soilbio.2013.03.011

DO - 10.1016/j.soilbio.2013.03.011

M3 - Article

SN - 0038-0717

VL - 63

SP - 1

EP - 4

JO - Soil Biology and Biochemistry

JF - Soil Biology and Biochemistry

ER -