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Soil Respiration Responses to Prolonged Warming Vary Seasonally in a Subarctic Grassland.

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Title: Soil Respiration Responses to Prolonged Warming Vary Seasonally in a Subarctic Grassland.
Authors: Protti‐Sánchez, Fabrizzio1 (AUTHOR) fabrizzio.protti‐sanchez@uibk.ac.at, Avila, Linsey M.2 (AUTHOR), Meeran, Kathiravan3 (AUTHOR), Ingrisch, Johannes1 (AUTHOR), Sigurðsson, Páll4 (AUTHOR), Larsen, Klaus S.2 (AUTHOR), Sigurdsson, Bjarni D.4 (AUTHOR), Janssens, Ivan5 (AUTHOR), Bahn, Michael1 (AUTHOR) michael.bahn@uibk.ac.at
Source: Global Change Biology. Aug2025, Vol. 31 Issue 8, p1-15. 15p.
Subjects: Soil respiration, Seasonal physiological variations, Temperature effect, Thermal gradient measurment, Seasons, Carbon in soils, Grasslands, Bacterial adaptation
Abstract: Northern ecosystems are warming rapidly, but the effects on soil carbon (C) dynamics are not fully understood. In particular, it is unclear whether warming effects on soil respiration (SR) –the primary source of atmospheric CO2 from terrestrial ecosystems– persist throughout the year or vary seasonally. While both summer and cold‐season processes shape annual soil C fluxes, the long cold season, which dominates high‐latitude regions, has received far less attention. Using a natural geothermal gradient in a subarctic grassland (+0°C to +10°C above ambient soil temperature), we assessed the effects of more than a decade of continuous soil warming on SR. We obtained high‐resolution year‐round soil CO2 fluxes and separated geothermal from biological sources of CO2 following a stable isotope approach. Our findings revealed seasonally variable responses: warming significantly increased SR during the cold season (October–May) but, surprisingly, had no effect during summer (July–September). The lack of a summer warming response likely resulted from warming‐induced soil C depletion and microbial and root adaptations. Overall, prolonged warming altered seasonal C flux dynamics by enhancing the cold‐season contribution to total annual SR. This shift led to a 5.8% rise in annual SR per degree Celsius of warming. Furthermore, the apparent temperature sensitivity of SR (Q10) and the seasonal amplitude of SR declined exponentially with warming intensity, with effects stabilizing beyond +3°C of warming, indicating apparent long‐term thermal acclimation of SR seasonality. Altogether, our findings highlight the importance of considering the seasonality of SR for accurate predictions of soil C dynamics in northern ecosystems under long‐term warming. [ABSTRACT FROM AUTHOR]
Copyright of Global Change Biology is the property of Wiley-Blackwell and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
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  Data: Soil Respiration Responses to Prolonged Warming Vary Seasonally in a Subarctic Grassland.
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  Data: <searchLink fieldCode="AR" term="%22Protti‐Sánchez%2C+Fabrizzio%22">Protti‐Sánchez, Fabrizzio</searchLink><relatesTo>1</relatesTo> (AUTHOR)<i> fabrizzio.protti‐sanchez@uibk.ac.at</i><br /><searchLink fieldCode="AR" term="%22Avila%2C+Linsey+M%2E%22">Avila, Linsey M.</searchLink><relatesTo>2</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Meeran%2C+Kathiravan%22">Meeran, Kathiravan</searchLink><relatesTo>3</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Ingrisch%2C+Johannes%22">Ingrisch, Johannes</searchLink><relatesTo>1</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Sigurðsson%2C+Páll%22">Sigurðsson, Páll</searchLink><relatesTo>4</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Larsen%2C+Klaus+S%2E%22">Larsen, Klaus S.</searchLink><relatesTo>2</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Sigurdsson%2C+Bjarni+D%2E%22">Sigurdsson, Bjarni D.</searchLink><relatesTo>4</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Janssens%2C+Ivan%22">Janssens, Ivan</searchLink><relatesTo>5</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Bahn%2C+Michael%22">Bahn, Michael</searchLink><relatesTo>1</relatesTo> (AUTHOR)<i> michael.bahn@uibk.ac.at</i>
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  Data: <searchLink fieldCode="DE" term="%22Soil+respiration%22">Soil respiration</searchLink><br /><searchLink fieldCode="DE" term="%22Seasonal+physiological+variations%22">Seasonal physiological variations</searchLink><br /><searchLink fieldCode="DE" term="%22Temperature+effect%22">Temperature effect</searchLink><br /><searchLink fieldCode="DE" term="%22Thermal+gradient+measurment%22">Thermal gradient measurment</searchLink><br /><searchLink fieldCode="DE" term="%22Seasons%22">Seasons</searchLink><br /><searchLink fieldCode="DE" term="%22Carbon+in+soils%22">Carbon in soils</searchLink><br /><searchLink fieldCode="DE" term="%22Grasslands%22">Grasslands</searchLink><br /><searchLink fieldCode="DE" term="%22Bacterial+adaptation%22">Bacterial adaptation</searchLink>
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  Data: Northern ecosystems are warming rapidly, but the effects on soil carbon (C) dynamics are not fully understood. In particular, it is unclear whether warming effects on soil respiration (SR) –the primary source of atmospheric CO2 from terrestrial ecosystems– persist throughout the year or vary seasonally. While both summer and cold‐season processes shape annual soil C fluxes, the long cold season, which dominates high‐latitude regions, has received far less attention. Using a natural geothermal gradient in a subarctic grassland (+0°C to +10°C above ambient soil temperature), we assessed the effects of more than a decade of continuous soil warming on SR. We obtained high‐resolution year‐round soil CO2 fluxes and separated geothermal from biological sources of CO2 following a stable isotope approach. Our findings revealed seasonally variable responses: warming significantly increased SR during the cold season (October–May) but, surprisingly, had no effect during summer (July–September). The lack of a summer warming response likely resulted from warming‐induced soil C depletion and microbial and root adaptations. Overall, prolonged warming altered seasonal C flux dynamics by enhancing the cold‐season contribution to total annual SR. This shift led to a 5.8% rise in annual SR per degree Celsius of warming. Furthermore, the apparent temperature sensitivity of SR (Q10) and the seasonal amplitude of SR declined exponentially with warming intensity, with effects stabilizing beyond +3°C of warming, indicating apparent long‐term thermal acclimation of SR seasonality. Altogether, our findings highlight the importance of considering the seasonality of SR for accurate predictions of soil C dynamics in northern ecosystems under long‐term warming. [ABSTRACT FROM AUTHOR]
– Name: AbstractSuppliedCopyright
  Label:
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  Data: <i>Copyright of Global Change Biology is the property of Wiley-Blackwell and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract.</i> (Copyright applies to all Abstracts.)
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      – Type: doi
        Value: 10.1111/gcb.70388
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      – Code: eng
        Text: English
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      Pagination:
        PageCount: 15
        StartPage: 1
    Subjects:
      – SubjectFull: Soil respiration
        Type: general
      – SubjectFull: Seasonal physiological variations
        Type: general
      – SubjectFull: Temperature effect
        Type: general
      – SubjectFull: Thermal gradient measurment
        Type: general
      – SubjectFull: Seasons
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      – SubjectFull: Carbon in soils
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      – SubjectFull: Grasslands
        Type: general
      – SubjectFull: Bacterial adaptation
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      – TitleFull: Soil Respiration Responses to Prolonged Warming Vary Seasonally in a Subarctic Grassland.
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              Text: Aug2025
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