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Living roots magnify the response of soil organic carbon decomposition to temperature in temperate grassland
Journal article   Open access   Peer reviewed

Living roots magnify the response of soil organic carbon decomposition to temperature in temperate grassland

Paul W. Hill, Mark H. Garnett, John Farrar, Zafar Iqbal, Muhammad Khalid, Nawaf Soleman and Davey L. Jones
Global change biology, Vol.21(3), pp.1368-1375
2015
PMCID: PMC4365897
PMID: 25351704
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Published160.60 kBDownloadView
Open Access

Abstract

Biodiversity & Conservation Ecology Environmental Sciences Environmental Sciences & Ecology Life Sciences & Biomedicine Science & Technology
Increasing atmospheric carbon dioxide (CO2) concentration is both a strong driver of primary productivity and widely believed to be the principal cause of recent increases in global temperature. Soils are the largest store of the world's terrestrial C. Consequently, many investigations have attempted to mechanistically understand how microbial mineralisation of soil organic carbon (SOC) to CO2 will be affected by projected increases in temperature. Most have attempted this in the absence of plants as the flux of CO2 from root and rhizomicrobial respiration in intact plant-soil systems confounds interpretation of measurements. We compared the effect of a small increase in temperature on respiration from soils without recent plant C with the effect on intact grass swards. We found that for 48weeks, before acclimation occurred, an experimental 3 degrees C increase in sward temperature gave rise to a 50% increase in below ground respiration (ca. 0.4kg Cm-2; Q(10)=3.5), whereas mineralisation of older SOC without plants increased with a Q(10) of only 1.7 when subject to increases in ambient soil temperature. Subsequent C-14 dating of respired CO2 indicated that the presence of plants in swards more than doubled the effect of warming on the rate of mineralisation of SOC with an estimated mean C age of ca. 8years or older relative to incubated soils without recent plant inputs. These results not only illustrate the formidable complexity of mechanisms controlling C fluxes in soils but also suggest that the dual biological and physical effects of CO2 on primary productivity and global temperature have the potential to synergistically increase the mineralisation of existing soil C.

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UN Sustainable Development Goals (SDGs)

This output has contributed to the advancement of the following goals:

#2 Zero Hunger
#13 Climate Action
#14 Life Below Water
#15 Life on Land

Source: InCites

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Collaboration types
Domestic collaboration
International collaboration
Citation topics
3 Agriculture, Environment & Ecology
3.45 Soil Science
3.45.112 Soil Carbon Dynamics
Web Of Science research areas
Biodiversity Conservation
Ecology
Environmental Sciences
ESI research areas
Environment/Ecology
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