Long term drought and warming alter soil bacterial and fungal communities in an upland heathland

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Long term drought and warming alter soil bacterial and fungal communities in an upland heathland. / Seaton, Fiona; Reinsch, Sabine; Goodall, Tim et al.
In: Ecosystems, Vol. 25, No. 6, 09.2022, p. 1279-1294.

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Seaton, F, Reinsch, S, Goodall, T, White, N, Jones, DL, Griffiths, R, Creer, S, Smith, A, Emmett, BA & Robinson, DA 2022, 'Long term drought and warming alter soil bacterial and fungal communities in an upland heathland', Ecosystems, vol. 25, no. 6, pp. 1279-1294. https://doi.org/10.1007/s10021-021-00715-8

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Seaton F, Reinsch S, Goodall T, White N, Jones DL, Griffiths R et al. Long term drought and warming alter soil bacterial and fungal communities in an upland heathland. Ecosystems. 2022 Sept;25(6):1279-1294. Epub 2021 Oct 19. doi: 10.1007/s10021-021-00715-8

Author

Seaton, Fiona ; Reinsch, Sabine ; Goodall, Tim et al. / Long term drought and warming alter soil bacterial and fungal communities in an upland heathland. In: Ecosystems. 2022 ; Vol. 25, No. 6. pp. 1279-1294.

RIS

TY - JOUR

T1 - Long term drought and warming alter soil bacterial and fungal communities in an upland heathland

AU - Seaton, Fiona

AU - Reinsch, Sabine

AU - Goodall, Tim

AU - White, Nicola

AU - Jones, Davey L.

AU - Griffiths, Robert

AU - Creer, Simon

AU - Smith, Andy

AU - Emmett, B. A.

AU - Robinson, D. A.

PY - 2022/9

Y1 - 2022/9

N2 - Abstract: The response of soil microbial communities to a changing climate will impact global biogeochemical cycles, potentially leading to positive and negative feedbacks. However, our understanding of how soil microbial communities respond to climate change and the implications of these changes for future soil function is limited. Here, we assess the response of soil bacterial and fungal communities to long-term experimental climate change in a heathland organo-mineral soil. We analysed microbial communities using Illumina sequencing of the 16S rRNA gene and ITS2 region at two depths, from plots undergoing 4 and 18 years of in situ summer drought or warming. We also assessed the colonisation of Calluna vulgaris roots by ericoid and dark septate endophytic (DSE) fungi using microscopy after 16 years of climate treatment. We found significant changes in both the bacterial and fungal communities in response to drought and warming, likely mediated by changes in soil pH and electrical conductivity. Changes in the microbial communities were more pronounced after a longer period of climate manipulation. Additionally, the subsoil communities of the long-term warmed plots became similar to the topsoil. Ericoid mycorrhizal colonisation decreased with depth while DSEs increased; however, these trends with depth were removed by warming. We largely ascribe the observed changes in microbial communities to shifts in plant cover and subsequent feedback on soil physicochemical properties, especially pH. Our results demonstrate the importance of considering changes in soil microbial responses to climate change across different soil depths and after extended periods of time.

AB - Abstract: The response of soil microbial communities to a changing climate will impact global biogeochemical cycles, potentially leading to positive and negative feedbacks. However, our understanding of how soil microbial communities respond to climate change and the implications of these changes for future soil function is limited. Here, we assess the response of soil bacterial and fungal communities to long-term experimental climate change in a heathland organo-mineral soil. We analysed microbial communities using Illumina sequencing of the 16S rRNA gene and ITS2 region at two depths, from plots undergoing 4 and 18 years of in situ summer drought or warming. We also assessed the colonisation of Calluna vulgaris roots by ericoid and dark septate endophytic (DSE) fungi using microscopy after 16 years of climate treatment. We found significant changes in both the bacterial and fungal communities in response to drought and warming, likely mediated by changes in soil pH and electrical conductivity. Changes in the microbial communities were more pronounced after a longer period of climate manipulation. Additionally, the subsoil communities of the long-term warmed plots became similar to the topsoil. Ericoid mycorrhizal colonisation decreased with depth while DSEs increased; however, these trends with depth were removed by warming. We largely ascribe the observed changes in microbial communities to shifts in plant cover and subsequent feedback on soil physicochemical properties, especially pH. Our results demonstrate the importance of considering changes in soil microbial responses to climate change across different soil depths and after extended periods of time.

KW - Bacteria

KW - Climate change

KW - Drought

KW - Fungi

KW - Heathland

KW - Mycorrhiza

KW - Warming

U2 - 10.1007/s10021-021-00715-8

DO - 10.1007/s10021-021-00715-8

M3 - Article

VL - 25

SP - 1279

EP - 1294

JO - Ecosystems

JF - Ecosystems

SN - 1435-0629

IS - 6

ER -