Community structure, ecophysiology, and regulation of new, acid-tolerant denitrifiers as cause of high N2O emissions from cryoturbated peat circles of acidic tundra soils
Denitrification is the main source of N2O emissions from cryoturbated peat circles in the Eastern European Arctic tundra. These permafrost-affected bare peat circles lack vegetation, have a high amount of available nitrate, and a low carbon to nitrogen ratio. Together with a soil moisture of ~ 70%,...
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Hannover : Institutionelles Repositorium der Leibniz Universität Hannover
2021
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ftunivhannover:oai:www.repo.uni-hannover.de:123456789/11134 2023-07-16T03:57:10+02:00 Community structure, ecophysiology, and regulation of new, acid-tolerant denitrifiers as cause of high N2O emissions from cryoturbated peat circles of acidic tundra soils Hetz, Stefanie Alexandra 2021 https://www.repo.uni-hannover.de/handle/123456789/11134 https://doi.org/10.15488/11052 eng eng Hannover : Institutionelles Repositorium der Leibniz Universität Hannover http://dx.doi.org/10.15488/11052 https://www.repo.uni-hannover.de/handle/123456789/11134 Es gilt deutsches Urheberrecht. Das Dokument darf zum eigenen Gebrauch kostenfrei genutzt, aber nicht im Internet bereitgestellt oder an Außenstehende weitergegeben werden. frei zugänglich Denitrification N2O Tundra Permafrost Peat Soil Denitrifikation Torfboden ddc:570 status-type:publishedVersion doc-type:DoctoralThesis doc-type:Text 2021 ftunivhannover https://doi.org/10.15488/11052 2023-06-28T10:38:50Z Denitrification is the main source of N2O emissions from cryoturbated peat circles in the Eastern European Arctic tundra. These permafrost-affected bare peat circles lack vegetation, have a high amount of available nitrate, and a low carbon to nitrogen ratio. Together with a soil moisture of ~ 70%, these are optimum conditions for denitrification and associated microorganisms. An acidic in situ pH of these peat circles is hypothesized to be a major controlling factor influencing denitrification and triggering the release of N2O as emitted end product of denitrification, as the final enzymatic step of denitrification is impaired by a low pH. This thesis aimed to test if the ecophysiology of new and acid-tolerant denitrifiers affects the emissions of N2O from cryoturbated peat circles. Microcosm experiments with soil from bare peat circles and surrounding vegetated peat plateau were conducted to test denitrification potentials of both soils. Additionally, the influence of pH on denitrification was tested. Nitrate reduction and associated production of gaseous N-products by denitrification were detected in both soils. In peat circle soil microcosms, independent of pH, the released end product was N2. Though nitrate reduction was slower at pH 4. In peat plateau microcosms N 2 was as well the emitted main end product at pH 6, whereas at pH 4 N2O was emitted. Therefore, data indicate the potential for denitrification in both soil types, as well as complete denitrification potential at acidic pH in peat circles. Microcosms experiments supplemented with labeled acetate were conducted to reveal the active, organic acid utilizing archaeal and bacterial community of denitrifiers based on 16S rRNA stable isotope probing coupled to Illumina MiSeq amplicon sequencing. Results suggest Burkholderiaceae as key nitrate reducers and acetate assimilators. This is supported by a new species within the Burkholderiaceae (Caballeronia) isolated from peat circle soil that encodes diverse nitrate and nitrite reductases. Potential key ... Doctoral or Postdoctoral Thesis Arctic Peat Peat plateau permafrost Tundra Institutional Repository of Leibniz Universität Hannover Arctic |
institution |
Open Polar |
collection |
Institutional Repository of Leibniz Universität Hannover |
op_collection_id |
ftunivhannover |
language |
English |
topic |
Denitrification N2O Tundra Permafrost Peat Soil Denitrifikation Torfboden ddc:570 |
spellingShingle |
Denitrification N2O Tundra Permafrost Peat Soil Denitrifikation Torfboden ddc:570 Hetz, Stefanie Alexandra Community structure, ecophysiology, and regulation of new, acid-tolerant denitrifiers as cause of high N2O emissions from cryoturbated peat circles of acidic tundra soils |
topic_facet |
Denitrification N2O Tundra Permafrost Peat Soil Denitrifikation Torfboden ddc:570 |
description |
Denitrification is the main source of N2O emissions from cryoturbated peat circles in the Eastern European Arctic tundra. These permafrost-affected bare peat circles lack vegetation, have a high amount of available nitrate, and a low carbon to nitrogen ratio. Together with a soil moisture of ~ 70%, these are optimum conditions for denitrification and associated microorganisms. An acidic in situ pH of these peat circles is hypothesized to be a major controlling factor influencing denitrification and triggering the release of N2O as emitted end product of denitrification, as the final enzymatic step of denitrification is impaired by a low pH. This thesis aimed to test if the ecophysiology of new and acid-tolerant denitrifiers affects the emissions of N2O from cryoturbated peat circles. Microcosm experiments with soil from bare peat circles and surrounding vegetated peat plateau were conducted to test denitrification potentials of both soils. Additionally, the influence of pH on denitrification was tested. Nitrate reduction and associated production of gaseous N-products by denitrification were detected in both soils. In peat circle soil microcosms, independent of pH, the released end product was N2. Though nitrate reduction was slower at pH 4. In peat plateau microcosms N 2 was as well the emitted main end product at pH 6, whereas at pH 4 N2O was emitted. Therefore, data indicate the potential for denitrification in both soil types, as well as complete denitrification potential at acidic pH in peat circles. Microcosms experiments supplemented with labeled acetate were conducted to reveal the active, organic acid utilizing archaeal and bacterial community of denitrifiers based on 16S rRNA stable isotope probing coupled to Illumina MiSeq amplicon sequencing. Results suggest Burkholderiaceae as key nitrate reducers and acetate assimilators. This is supported by a new species within the Burkholderiaceae (Caballeronia) isolated from peat circle soil that encodes diverse nitrate and nitrite reductases. Potential key ... |
format |
Doctoral or Postdoctoral Thesis |
author |
Hetz, Stefanie Alexandra |
author_facet |
Hetz, Stefanie Alexandra |
author_sort |
Hetz, Stefanie Alexandra |
title |
Community structure, ecophysiology, and regulation of new, acid-tolerant denitrifiers as cause of high N2O emissions from cryoturbated peat circles of acidic tundra soils |
title_short |
Community structure, ecophysiology, and regulation of new, acid-tolerant denitrifiers as cause of high N2O emissions from cryoturbated peat circles of acidic tundra soils |
title_full |
Community structure, ecophysiology, and regulation of new, acid-tolerant denitrifiers as cause of high N2O emissions from cryoturbated peat circles of acidic tundra soils |
title_fullStr |
Community structure, ecophysiology, and regulation of new, acid-tolerant denitrifiers as cause of high N2O emissions from cryoturbated peat circles of acidic tundra soils |
title_full_unstemmed |
Community structure, ecophysiology, and regulation of new, acid-tolerant denitrifiers as cause of high N2O emissions from cryoturbated peat circles of acidic tundra soils |
title_sort |
community structure, ecophysiology, and regulation of new, acid-tolerant denitrifiers as cause of high n2o emissions from cryoturbated peat circles of acidic tundra soils |
publisher |
Hannover : Institutionelles Repositorium der Leibniz Universität Hannover |
publishDate |
2021 |
url |
https://www.repo.uni-hannover.de/handle/123456789/11134 https://doi.org/10.15488/11052 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Peat Peat plateau permafrost Tundra |
genre_facet |
Arctic Peat Peat plateau permafrost Tundra |
op_relation |
http://dx.doi.org/10.15488/11052 https://www.repo.uni-hannover.de/handle/123456789/11134 |
op_rights |
Es gilt deutsches Urheberrecht. Das Dokument darf zum eigenen Gebrauch kostenfrei genutzt, aber nicht im Internet bereitgestellt oder an Außenstehende weitergegeben werden. frei zugänglich |
op_doi |
https://doi.org/10.15488/11052 |
_version_ |
1771543674977517568 |