
Characterisation of terrestrial acidophilic archaeal ammonia oxidisers and their inhibition and stimulation by organic compounds
Author(s) -
LehtovirtaMorley Laura E.,
Ge Chaorong,
Ross Jenna,
Yao Huaiying,
Nicol Graeme W.,
Prosser James I.
Publication year - 2014
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 - 10.1111/1574-6941.12353
Subject(s) - biology , archaea , microorganism , ammonia , autotroph , candidatus , ecosystem , bacteria , terrestrial ecosystem , phylogenetic diversity , soil microbiology , microbial ecology , botany , ecology , biochemistry , phylogenetics , soil water , 16s ribosomal rna , genetics , gene
Autotrophic ammonia oxidation is performed by two distinct groups of microorganisms: ammonia‐oxidising archaea ( AOA ) and ammonia‐oxidising bacteria ( AOB ). AOA outnumber their bacterial counterparts in many soils, at times by several orders of magnitude, but relatively little is known of their physiology due to the lack of cultivated isolates. Although a number of AOA have been cultivated from soil, N itrososphaera viennensis was the sole terrestrial AOA in pure culture and requires pyruvate for growth in the laboratory. Here, we describe isolation in pure culture and characterisation of two acidophilic terrestrial AOA representing the C andidatus genus N itrosotalea and their responses to organic acids. Interestingly, despite their close phylogenetic relatedness, the two N itrosotalea strains exhibited differences in physiological features, including specific growth rate, temperature preference and to an extent, response to organic compounds. In contrast to N . viennensis , both N itrosotalea isolates were inhibited by pyruvate but their growth yield increased in the presence of oxaloacetate. This study demonstrates physiological diversity within AOA species and between different AOA genera. Different preferences for organic compounds potentially influence the favoured localisation of ammonia oxidisers within the soil and the structure of ammonia‐oxidising communities in terrestrial ecosystems.