Streptomycetes contributing to atmospheric molecular hydrogen soil uptake are widespread and encode a putative high-affinity [NiFe]-hydrogenase
Uptake of molecular hydrogen (H₂) by soil is a biological reaction responsible for ~80% of the global loss of atmospheric H₂. Indirect evidence obtained over the last decades suggests that free soil hydrogenases with an unusually high affinity for H₂ are carrying out the reaction. This assumption ha...
Saved in:
Published in | Environmental microbiology Vol. 12; no. 3; pp. 821 - 829 |
---|---|
Main Authors | , , , |
Format | Journal Article |
Language | English |
Published |
Oxford, UK
Oxford, UK : Blackwell Publishing Ltd
01.03.2010
Blackwell Publishing Ltd |
Subjects | |
Online Access | Get full text |
Cover
Loading…
Summary: | Uptake of molecular hydrogen (H₂) by soil is a biological reaction responsible for ~80% of the global loss of atmospheric H₂. Indirect evidence obtained over the last decades suggests that free soil hydrogenases with an unusually high affinity for H₂ are carrying out the reaction. This assumption has recently been challenged by the isolation of Streptomyces sp. PCB7, displaying the high-affinity H₂ uptake activity previously attributed to free soil enzymes. While this finding suggests that actinobacteria could be responsible for atmospheric H₂ soil uptake, the ecological importance of H₂-oxidizing streptomycetes remains to be investigated. Here, we show that high-affinity H₂ uptake activity is widespread among the streptomycetes. Among 14 streptomycetes strains isolated from temperate forest and agricultural soils, six exhibited a high-affinity H₂ uptake activity. The gene encoding the large subunit of a putative high-affinity [NiFe]-hydrogenase (hydB-like gene sequence) was detected exclusively in the isolates exhibiting high-affinity H₂ uptake. Catalysed reporter deposition-fluorescence in situ hybridization (CARD-FISH) experiments targeting hydB-like gene transcripts and H₂ uptake assays performed with strain PCB7 suggested that streptomycetes spores catalysed the H₂ uptake activity. Expression of the activity in term of biomass revealed that 10⁶-10⁷ H₂-oxidizing bacteria per gram of soil should be sufficient to explain in situ H₂ uptake by soil. We propose that specialized H₂-oxidizing actinobacteria are responsible for the most important sink term in the atmospheric H₂ budget. |
---|---|
Bibliography: | http://dx.doi.org/10.1111/j.1462-2920.2009.02130.x ArticleID:EMI2130 istex:E46ECBC461529BB03BF9510680E20A568696746E ark:/67375/WNG-TXSM779G-1 ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 ObjectType-Article-2 ObjectType-Feature-1 |
ISSN: | 1462-2912 1462-2920 |
DOI: | 10.1111/j.1462-2920.2009.02130.x |