Characterisation of microbial community composition of a Siberian tundra soil by fluorescence in situ hybridisation

The bacterial community composition of the active layer (0–45 cm) of a permafrost-affected tundra soil was analysed by fluorescence in situ hybridisation (FISH). Arctic tundra soils contain large amounts of organic carbon, accumulated in thick soil layers and are known as a major sink of atmospheric...

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Published in:FEMS Microbiology Ecology
Main Authors: Kobabe, Svenja, Wagner, Dirk, Pfeiffer, Eva-Maria
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2004
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/27429/
https://oceanrep.geomar.de/id/eprint/27429/1/2004_Kobabe-etal-Characterization_j.femsec.2004.05.003.pdf
https://doi.org/10.1016/j.femsec.2004.05.003
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spelling ftoceanrep:oai:oceanrep.geomar.de:27429 2023-05-15T15:10:11+02:00 Characterisation of microbial community composition of a Siberian tundra soil by fluorescence in situ hybridisation Kobabe, Svenja Wagner, Dirk Pfeiffer, Eva-Maria 2004 text https://oceanrep.geomar.de/id/eprint/27429/ https://oceanrep.geomar.de/id/eprint/27429/1/2004_Kobabe-etal-Characterization_j.femsec.2004.05.003.pdf https://doi.org/10.1016/j.femsec.2004.05.003 en eng Elsevier https://oceanrep.geomar.de/id/eprint/27429/1/2004_Kobabe-etal-Characterization_j.femsec.2004.05.003.pdf Kobabe, S., Wagner, D. and Pfeiffer, E. M. (2004) Characterisation of microbial community composition of a Siberian tundra soil by fluorescence in situ hybridisation. FEMS Microbiology Ecology, 50 (1). pp. 13-23. DOI 10.1016/j.femsec.2004.05.003 <https://doi.org/10.1016/j.femsec.2004.05.003>. doi:10.1016/j.femsec.2004.05.003 cc_by_nc Article PeerReviewed 2004 ftoceanrep https://doi.org/10.1016/j.femsec.2004.05.003 2023-04-07T15:17:31Z The bacterial community composition of the active layer (0–45 cm) of a permafrost-affected tundra soil was analysed by fluorescence in situ hybridisation (FISH). Arctic tundra soils contain large amounts of organic carbon, accumulated in thick soil layers and are known as a major sink of atmospheric CO2. These soils are totally frozen throughout the year and only a thin active layer is unfrozen and shows biological activity during the short summer. To improve the understanding of how the carbon fluxes in the active layer are controlled, detailed analysis of composition, functionality and interaction of soil microorganisms was done. The FISH analyses of the active layer showed large variations in absolute cell numbers and in the composition of the active microbial community between the different horizons, which is caused by the different environmental conditions (e.g., soil temperature, amount of organic matter, aeration) in this vertically structured ecosystem. Universal protein stain 5-(4,6-dichlorotriazin-2-yl)aminofluorescein (DTAF) showed an exponential decrease of total cell counts from the top to the bottom of the active layer (2.3 × 109–1.2 × 108 cells per gram dry soil). Using FISH, up to 59% of the DTAF-detected cells could be detected in the surface horizon, and up to 84% of these FISH-detected cells could be affiliated to a known phylogenetic group. The amount of FISH-detectable cells decreased with increasing depth and so did the diversity of ascertained phylogenetic groups. Article in Journal/Newspaper Arctic permafrost Tundra OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Arctic FEMS Microbiology Ecology 50 1 13 23
institution Open Polar
collection OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel)
op_collection_id ftoceanrep
language English
description The bacterial community composition of the active layer (0–45 cm) of a permafrost-affected tundra soil was analysed by fluorescence in situ hybridisation (FISH). Arctic tundra soils contain large amounts of organic carbon, accumulated in thick soil layers and are known as a major sink of atmospheric CO2. These soils are totally frozen throughout the year and only a thin active layer is unfrozen and shows biological activity during the short summer. To improve the understanding of how the carbon fluxes in the active layer are controlled, detailed analysis of composition, functionality and interaction of soil microorganisms was done. The FISH analyses of the active layer showed large variations in absolute cell numbers and in the composition of the active microbial community between the different horizons, which is caused by the different environmental conditions (e.g., soil temperature, amount of organic matter, aeration) in this vertically structured ecosystem. Universal protein stain 5-(4,6-dichlorotriazin-2-yl)aminofluorescein (DTAF) showed an exponential decrease of total cell counts from the top to the bottom of the active layer (2.3 × 109–1.2 × 108 cells per gram dry soil). Using FISH, up to 59% of the DTAF-detected cells could be detected in the surface horizon, and up to 84% of these FISH-detected cells could be affiliated to a known phylogenetic group. The amount of FISH-detectable cells decreased with increasing depth and so did the diversity of ascertained phylogenetic groups.
format Article in Journal/Newspaper
author Kobabe, Svenja
Wagner, Dirk
Pfeiffer, Eva-Maria
spellingShingle Kobabe, Svenja
Wagner, Dirk
Pfeiffer, Eva-Maria
Characterisation of microbial community composition of a Siberian tundra soil by fluorescence in situ hybridisation
author_facet Kobabe, Svenja
Wagner, Dirk
Pfeiffer, Eva-Maria
author_sort Kobabe, Svenja
title Characterisation of microbial community composition of a Siberian tundra soil by fluorescence in situ hybridisation
title_short Characterisation of microbial community composition of a Siberian tundra soil by fluorescence in situ hybridisation
title_full Characterisation of microbial community composition of a Siberian tundra soil by fluorescence in situ hybridisation
title_fullStr Characterisation of microbial community composition of a Siberian tundra soil by fluorescence in situ hybridisation
title_full_unstemmed Characterisation of microbial community composition of a Siberian tundra soil by fluorescence in situ hybridisation
title_sort characterisation of microbial community composition of a siberian tundra soil by fluorescence in situ hybridisation
publisher Elsevier
publishDate 2004
url https://oceanrep.geomar.de/id/eprint/27429/
https://oceanrep.geomar.de/id/eprint/27429/1/2004_Kobabe-etal-Characterization_j.femsec.2004.05.003.pdf
https://doi.org/10.1016/j.femsec.2004.05.003
geographic Arctic
geographic_facet Arctic
genre Arctic
permafrost
Tundra
genre_facet Arctic
permafrost
Tundra
op_relation https://oceanrep.geomar.de/id/eprint/27429/1/2004_Kobabe-etal-Characterization_j.femsec.2004.05.003.pdf
Kobabe, S., Wagner, D. and Pfeiffer, E. M. (2004) Characterisation of microbial community composition of a Siberian tundra soil by fluorescence in situ hybridisation. FEMS Microbiology Ecology, 50 (1). pp. 13-23. DOI 10.1016/j.femsec.2004.05.003 <https://doi.org/10.1016/j.femsec.2004.05.003>.
doi:10.1016/j.femsec.2004.05.003
op_rights cc_by_nc
op_doi https://doi.org/10.1016/j.femsec.2004.05.003
container_title FEMS Microbiology Ecology
container_volume 50
container_issue 1
container_start_page 13
op_container_end_page 23
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