2015
DOI: 10.1038/nature14856
|View full text |Cite
|
Sign up to set email alerts
|

Cyanate as an energy source for nitrifiers

Abstract: Ammonia-and nitrite-oxidizers are collectively responsible for the aerobic oxidation of ammonia via nitrite to nitrate and play essential roles for the global biogeochemical nitrogen cycle. The physiology of these nitrifying microbes has been intensively studied since the first experiments of Sergei Winogradsky more than a century ago. Urea and ammonia are the only recognized energy sources that promote the aerobic growth of ammonia-oxidizing bacteria and archaea. Here we report the aerobic growth of a pure cu… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
1
1

Citation Types

4
221
2
4

Year Published

2016
2016
2018
2018

Publication Types

Select...
4
3

Relationship

0
7

Authors

Journals

citations
Cited by 221 publications
(231 citation statements)
references
References 42 publications
4
221
2
4
Order By: Relevance
“…Comparative genomics indicate that the genes required for F 420 biosynthesis are also distributed in the Thaumarchaeota, Aigarchaeota, Geoarchaeota, Bathyarchaeota, and Lokiarchaeota (138)(139)(140)(141)(142). The absorbance spectra of single cells of the ammonia-and cyanate-oxidizing thaumarchaeon Nitrososphaera gargensis are also consistent with the presence of F 420 (143,144). It is unclear whether F 420 is pro- duced by Crenarchaeota; while the cofactor was reported to be present at low levels in representatives of the Sulfolobus and Thermoplasma (20), the genomes of these organisms suggest that in fact they lack the capacity to synthesize this deazaflavin by any currently understood biosynthetic mechanism.…”
Section: Distributionmentioning
confidence: 55%
“…Comparative genomics indicate that the genes required for F 420 biosynthesis are also distributed in the Thaumarchaeota, Aigarchaeota, Geoarchaeota, Bathyarchaeota, and Lokiarchaeota (138)(139)(140)(141)(142). The absorbance spectra of single cells of the ammonia-and cyanate-oxidizing thaumarchaeon Nitrososphaera gargensis are also consistent with the presence of F 420 (143,144). It is unclear whether F 420 is pro- duced by Crenarchaeota; while the cofactor was reported to be present at low levels in representatives of the Sulfolobus and Thermoplasma (20), the genomes of these organisms suggest that in fact they lack the capacity to synthesize this deazaflavin by any currently understood biosynthetic mechanism.…”
Section: Distributionmentioning
confidence: 55%
“…Genomic analysis of several Thaumarchaea species revealed the presence of genes related to transport, production and degradation of urea (Palatinszky et al, 2015). Urea can be used by Thaumarchaeota members as source of ammonia, as shown by biochemical assays of cultivated species (Lehtovirta-Morley et al, 2016), and as carbon source, as inferred from 14 C-labeled urea incorporation of prokaryotic communities of Artic waters (Alonso-Saez et al, 2012).…”
Section: Resultsmentioning
confidence: 99%
“…Cyanate lyase decomposes cyanate to CO 2 and ammonia in a reaction dependent of bicarbonate (Johnson and Anderson, 1987). Its activity was described in N. moscoviensis and its proposed biological roles include nitrogen assimilation, cyanate detoxification and energy acquisition (Anderson et al, 1990;Palatinszky et al, 2015). The cya gene was localized downstream from two genes encoding for proteins of the formate/nitrite transporter family (TPM av 513-904) (Supplementary Figure S9).…”
Section: Resultsmentioning
confidence: 99%
See 2 more Smart Citations