Open AccessGenetic characterization of denitrifier communities with contrasting intrinsic functional traits
Author(s) -
Braker Gesche,
Dörsch Peter,
Bakken Lars R.
Publication year - 2012
Publication title -
fems microbiology ecology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.377
H-Index - 155
eISSN - 1574-6941
pISSN - 0168-6496
DOI - 10.1111/j.1574-6941.2011.01237.x
Subject(s) - denitrification , biology , microbial population biology , abundance (ecology) , soil water , community structure , relative species abundance , species richness , ecology , environmental chemistry , bacteria , nitrogen , chemistry , genetics , organic chemistry
Microorganisms capable of denitrification are polyphyletic and exhibit distinct denitrification regulatory phenotypes ( DRP ), and thus, denitrification in soils could be controlled by community composition. In a companion study (Dörsch et al ., 2012) and preceding work, ex situ denitrification assays of three organic soils demonstrated profoundly different functional traits including N 2 O / N 2 ratios. Here, we explored the composition of the underlying denitrifier communities by analyzing the abundance and structure of denitrification genes ( nirK , nirS , and nosZ ). The relative abundance of nosZ (vs. nirK + nirS ) was similar for all communities, and hence, the low N 2 O reductase activity in one of the soils was not because of the lack of organisms with this gene. Similarity in community composition between the soils was generally low for nirK and nirS , but not for nosZ . The community with the most robust denitrification (consistently low N 2 O / N 2 ) had the highest diversity/richness of nosZ and nirK , but not of nirS . Contrary results found for a second soil agreed with impaired denitrification (low overall denitrification activity, high N 2 O / N 2 ). In conclusion, differences in community composition and in the absolute abundance of denitrification genes clearly reflected the functional differences observed in laboratory studies and may shed light on differences in in situ N 2 O emission of the soils.