Archaeal dominated ammonia-oxidizing communities in Icelandic grassland soils are moderately affected by long-term N fertilization and geothermal heating

The contribution of ammonia-oxidizing bacteria and archaea (AOB and AOA, respectively) to the net oxidation of ammonia varies greatly between terrestrial environments. To better understand, predict and possibly manage terrestrial nitrogen turnover, we need to develop a conceptual understanding of am...

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Main Authors: Daebeler, Anne, Abell, Guy C. J., Bodelier, Paul L. E., Bodrossy, Levente, Frampton, Dion M. F., Hefting, Mariet M., Laanbroek, Hendrikus J.
Format: Online
Language:English
Published: Frontiers Media S.A. 2012
Online Access:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3463987/
id pubmed-3463987
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spelling pubmed-34639872012-10-11 Archaeal dominated ammonia-oxidizing communities in Icelandic grassland soils are moderately affected by long-term N fertilization and geothermal heating Daebeler, Anne Abell, Guy C. J. Bodelier, Paul L. E. Bodrossy, Levente Frampton, Dion M. F. Hefting, Mariet M. Laanbroek, Hendrikus J. Microbiology The contribution of ammonia-oxidizing bacteria and archaea (AOB and AOA, respectively) to the net oxidation of ammonia varies greatly between terrestrial environments. To better understand, predict and possibly manage terrestrial nitrogen turnover, we need to develop a conceptual understanding of ammonia oxidation as a function of environmental conditions including the ecophysiology of associated organisms. We examined the discrete and combined effects of mineral nitrogen deposition and geothermal heating on ammonia-oxidizing communities by sampling soils from a long-term fertilization site along a temperature gradient in Icelandic grasslands. Microarray, clone library and quantitative PCR analyses of the ammonia monooxygenase subunit A (amoA) gene accompanied by physico-chemical measurements of the soil properties were conducted. In contrast to most other terrestrial environments, the ammonia-oxidizing communities consisted almost exclusively of archaea. Their bacterial counterparts proved to be undetectable by quantitative polymerase chain reaction suggesting AOB are only of minor relevance for ammonia oxidation in these soils. Our results show that fertilization and local, geothermal warming affected detectable ammonia-oxidizing communities, but not soil chemistry: only a subset of the detected AOA phylotypes was present in higher temperature soils and AOA abundance was increased in the fertilized soils, while soil physio-chemical properties remained unchanged. Differences in distribution and structure of AOA communities were best explained by soil pH and clay content irrespective of temperature or fertilizer treatment in these grassland soils, suggesting that these factors have a greater potential for ecological niche-differentiation of AOA in soil than temperature and N fertilization. Frontiers Media S.A. 2012-10-04 /pmc/articles/PMC3463987/ /pubmed/23060870 http://dx.doi.org/10.3389/fmicb.2012.00352 Text en Copyright © 2012 Daebeler, Abell, Bodelier, Bodrossy, Frampton, Hefting and Laanbroek. http://www.frontiersin.org/licenseagreement This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in other forums, provided the original authors and source are credited and subject to any copyright notices concerning any third-party graphics etc.
repository_type Open Access Journal
institution_category Foreign Institution
institution US National Center for Biotechnology Information
building NCBI PubMed
collection Online Access
language English
format Online
author Daebeler, Anne
Abell, Guy C. J.
Bodelier, Paul L. E.
Bodrossy, Levente
Frampton, Dion M. F.
Hefting, Mariet M.
Laanbroek, Hendrikus J.
spellingShingle Daebeler, Anne
Abell, Guy C. J.
Bodelier, Paul L. E.
Bodrossy, Levente
Frampton, Dion M. F.
Hefting, Mariet M.
Laanbroek, Hendrikus J.
Archaeal dominated ammonia-oxidizing communities in Icelandic grassland soils are moderately affected by long-term N fertilization and geothermal heating
author_facet Daebeler, Anne
Abell, Guy C. J.
Bodelier, Paul L. E.
Bodrossy, Levente
Frampton, Dion M. F.
Hefting, Mariet M.
Laanbroek, Hendrikus J.
author_sort Daebeler, Anne
title Archaeal dominated ammonia-oxidizing communities in Icelandic grassland soils are moderately affected by long-term N fertilization and geothermal heating
title_short Archaeal dominated ammonia-oxidizing communities in Icelandic grassland soils are moderately affected by long-term N fertilization and geothermal heating
title_full Archaeal dominated ammonia-oxidizing communities in Icelandic grassland soils are moderately affected by long-term N fertilization and geothermal heating
title_fullStr Archaeal dominated ammonia-oxidizing communities in Icelandic grassland soils are moderately affected by long-term N fertilization and geothermal heating
title_full_unstemmed Archaeal dominated ammonia-oxidizing communities in Icelandic grassland soils are moderately affected by long-term N fertilization and geothermal heating
title_sort archaeal dominated ammonia-oxidizing communities in icelandic grassland soils are moderately affected by long-term n fertilization and geothermal heating
description The contribution of ammonia-oxidizing bacteria and archaea (AOB and AOA, respectively) to the net oxidation of ammonia varies greatly between terrestrial environments. To better understand, predict and possibly manage terrestrial nitrogen turnover, we need to develop a conceptual understanding of ammonia oxidation as a function of environmental conditions including the ecophysiology of associated organisms. We examined the discrete and combined effects of mineral nitrogen deposition and geothermal heating on ammonia-oxidizing communities by sampling soils from a long-term fertilization site along a temperature gradient in Icelandic grasslands. Microarray, clone library and quantitative PCR analyses of the ammonia monooxygenase subunit A (amoA) gene accompanied by physico-chemical measurements of the soil properties were conducted. In contrast to most other terrestrial environments, the ammonia-oxidizing communities consisted almost exclusively of archaea. Their bacterial counterparts proved to be undetectable by quantitative polymerase chain reaction suggesting AOB are only of minor relevance for ammonia oxidation in these soils. Our results show that fertilization and local, geothermal warming affected detectable ammonia-oxidizing communities, but not soil chemistry: only a subset of the detected AOA phylotypes was present in higher temperature soils and AOA abundance was increased in the fertilized soils, while soil physio-chemical properties remained unchanged. Differences in distribution and structure of AOA communities were best explained by soil pH and clay content irrespective of temperature or fertilizer treatment in these grassland soils, suggesting that these factors have a greater potential for ecological niche-differentiation of AOA in soil than temperature and N fertilization.
publisher Frontiers Media S.A.
publishDate 2012
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3463987/
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