Home > Research > Publications & Outputs > Diminished soil functions occur under simulated...

Links

Text available via DOI:

View graph of relations

Diminished soil functions occur under simulated climate change in a sup-alpine pasture, but heterotrophic temperature sensitivity indicates microbial resilience

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Published

Standard

Diminished soil functions occur under simulated climate change in a sup-alpine pasture, but heterotrophic temperature sensitivity indicates microbial resilience. / Mills, Robert T. E.; Gavazov, Konstantin S.; Spiegelberger, Thomas et al.
In: Science of the Total Environment, Vol. 473-474, 01.03.2014, p. 465-472.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Harvard

APA

Vancouver

Mills RTE, Gavazov KS, Spiegelberger T, Johnson D, Buttler A. Diminished soil functions occur under simulated climate change in a sup-alpine pasture, but heterotrophic temperature sensitivity indicates microbial resilience. Science of the Total Environment. 2014 Mar 1;473-474:465-472. doi: 10.1016/j.scitotenv.2013.12.071

Author

Mills, Robert T. E. ; Gavazov, Konstantin S. ; Spiegelberger, Thomas et al. / Diminished soil functions occur under simulated climate change in a sup-alpine pasture, but heterotrophic temperature sensitivity indicates microbial resilience. In: Science of the Total Environment. 2014 ; Vol. 473-474. pp. 465-472.

Bibtex

@article{f2915ef55ac44665a63711ee04805895,
title = "Diminished soil functions occur under simulated climate change in a sup-alpine pasture, but heterotrophic temperature sensitivity indicates microbial resilience",
abstract = "The pressure of climate change is disproportionately high in mountainous regions, and small changes may push ecosystem processes beyond sensitivity thresholds, creating new dynamics of carbon and nutrient cycling. Given that the rate of organic matter decomposition is strongly dependent upon temperature and soil moisture, the sensitivity of soil respiration to both metrics is highly relevant when considering soil atmosphere feedbacks under a changing climate. To assess the effects of changing climate in a mountain pasture system, we transplanted turfs along an elevation gradient, monitored in situ soil respiration, incubated collected top-soils to determine legacy effects on temperature sensitivity, and analysed soil organic matter (SOM) to detect changes in quality and quantity of SOM fractions. In situ transplantation down-slope reduced soil moisture and increased soil temperature, with concurrent reductions in soil respiration. Soil moisture acted as an overriding constraint to soil respiration, and significantly reduced the sensitivity to temperature. Under controlled laboratory conditions, removal of the moisture constraint to heterotrophic respiration led to a significant respiration-temperature response. However, despite lower respiration rates down-slope, the response function was comparable among sites, and therefore unaffected by antecedent conditions. We found shifts in the SOM quality, especially of the light fraction, indicating changes to the dynamics of decomposition of recently deposited material. Our findings highlighted the resilience of the microbial community to severe climatic perturbations, but also that soil moisture stress during the growing season can significantly reduce soil function in addition to direct effects on plant productivity. This demonstrated the sensitivity of subalpine pastures under climate change, and possible implications for sustainable use given reductions in organic matter turnover and consequent feedbacks to nutrient cycling. (C) 2013 Elsevier B.V. All rights reserved.",
keywords = "Mountain grasslands, Climate warming, Soil moisture, Altitudinal gradient, Soil respiration, Density fractionation, ORGANIC-MATTER, NITROGEN MINERALIZATION, GRASSLAND SOIL, RESPIRATION, CARBON, MOISTURE, DECOMPOSITION, GRADIENT, BIOMASS, DEPENDENCE",
author = "Mills, {Robert T. E.} and Gavazov, {Konstantin S.} and Thomas Spiegelberger and David Johnson and Alexandre Buttler",
year = "2014",
month = mar,
day = "1",
doi = "10.1016/j.scitotenv.2013.12.071",
language = "English",
volume = "473-474",
pages = "465--472",
journal = "Science of the Total Environment",
issn = "0048-9697",
publisher = "Elsevier Science B.V.",

}

RIS

TY - JOUR

T1 - Diminished soil functions occur under simulated climate change in a sup-alpine pasture, but heterotrophic temperature sensitivity indicates microbial resilience

AU - Mills, Robert T. E.

AU - Gavazov, Konstantin S.

AU - Spiegelberger, Thomas

AU - Johnson, David

AU - Buttler, Alexandre

PY - 2014/3/1

Y1 - 2014/3/1

N2 - The pressure of climate change is disproportionately high in mountainous regions, and small changes may push ecosystem processes beyond sensitivity thresholds, creating new dynamics of carbon and nutrient cycling. Given that the rate of organic matter decomposition is strongly dependent upon temperature and soil moisture, the sensitivity of soil respiration to both metrics is highly relevant when considering soil atmosphere feedbacks under a changing climate. To assess the effects of changing climate in a mountain pasture system, we transplanted turfs along an elevation gradient, monitored in situ soil respiration, incubated collected top-soils to determine legacy effects on temperature sensitivity, and analysed soil organic matter (SOM) to detect changes in quality and quantity of SOM fractions. In situ transplantation down-slope reduced soil moisture and increased soil temperature, with concurrent reductions in soil respiration. Soil moisture acted as an overriding constraint to soil respiration, and significantly reduced the sensitivity to temperature. Under controlled laboratory conditions, removal of the moisture constraint to heterotrophic respiration led to a significant respiration-temperature response. However, despite lower respiration rates down-slope, the response function was comparable among sites, and therefore unaffected by antecedent conditions. We found shifts in the SOM quality, especially of the light fraction, indicating changes to the dynamics of decomposition of recently deposited material. Our findings highlighted the resilience of the microbial community to severe climatic perturbations, but also that soil moisture stress during the growing season can significantly reduce soil function in addition to direct effects on plant productivity. This demonstrated the sensitivity of subalpine pastures under climate change, and possible implications for sustainable use given reductions in organic matter turnover and consequent feedbacks to nutrient cycling. (C) 2013 Elsevier B.V. All rights reserved.

AB - The pressure of climate change is disproportionately high in mountainous regions, and small changes may push ecosystem processes beyond sensitivity thresholds, creating new dynamics of carbon and nutrient cycling. Given that the rate of organic matter decomposition is strongly dependent upon temperature and soil moisture, the sensitivity of soil respiration to both metrics is highly relevant when considering soil atmosphere feedbacks under a changing climate. To assess the effects of changing climate in a mountain pasture system, we transplanted turfs along an elevation gradient, monitored in situ soil respiration, incubated collected top-soils to determine legacy effects on temperature sensitivity, and analysed soil organic matter (SOM) to detect changes in quality and quantity of SOM fractions. In situ transplantation down-slope reduced soil moisture and increased soil temperature, with concurrent reductions in soil respiration. Soil moisture acted as an overriding constraint to soil respiration, and significantly reduced the sensitivity to temperature. Under controlled laboratory conditions, removal of the moisture constraint to heterotrophic respiration led to a significant respiration-temperature response. However, despite lower respiration rates down-slope, the response function was comparable among sites, and therefore unaffected by antecedent conditions. We found shifts in the SOM quality, especially of the light fraction, indicating changes to the dynamics of decomposition of recently deposited material. Our findings highlighted the resilience of the microbial community to severe climatic perturbations, but also that soil moisture stress during the growing season can significantly reduce soil function in addition to direct effects on plant productivity. This demonstrated the sensitivity of subalpine pastures under climate change, and possible implications for sustainable use given reductions in organic matter turnover and consequent feedbacks to nutrient cycling. (C) 2013 Elsevier B.V. All rights reserved.

KW - Mountain grasslands

KW - Climate warming

KW - Soil moisture

KW - Altitudinal gradient

KW - Soil respiration

KW - Density fractionation

KW - ORGANIC-MATTER

KW - NITROGEN MINERALIZATION

KW - GRASSLAND SOIL

KW - RESPIRATION

KW - CARBON

KW - MOISTURE

KW - DECOMPOSITION

KW - GRADIENT

KW - BIOMASS

KW - DEPENDENCE

U2 - 10.1016/j.scitotenv.2013.12.071

DO - 10.1016/j.scitotenv.2013.12.071

M3 - Journal article

VL - 473-474

SP - 465

EP - 472

JO - Science of the Total Environment

JF - Science of the Total Environment

SN - 0048-9697

ER -