Unknown

Dataset Information

0

Dual nitrogen and oxygen isotope fractionation during anaerobic ammonium oxidation by anammox bacteria.


ABSTRACT: Natural abundance of stable nitrogen (N) and oxygen (O) isotopes are invaluable biogeochemical tracers for assessing the N transformations in the environment. To fully exploit these tracers, the N and O isotope effects (15? and 18?) associated with the respective nitrogen transformation processes must be known. However, the N and O isotope effects of anaerobic ammonium oxidation (anammox), one of the major fixed N sinks and NO3- producers, are not well known. Here, we report the dual N and O isotope effects associated with anammox by three different anammox bacteria including "Ca. Scalindua japonica", a putative marine species, which were measured in continuous enrichment culture experiments. All three anammox species yielded similar N isotope effects of NH4+ oxidation to N2 (15?NH4?N2) ranging from 30.9‰ to 32.7‰ and inverse kinetic isotope effects of NO2- oxidation to NO3- (15?NO2?NO3?=?-45.3‰ to -30.1‰). In contrast, 15?NO2?N2 (NO2- reduction to N2) were significantly different among three species, which is probably because individual anammox bacteria species might possess different types of nitrite reductase. We also report the combined O isotope effects for NO2- oxidation (18ENO2?NO3) by anammox bacteria. These obtained dual N and O isotopic effects could provide significant insights into the contribution of anammox bacteria to the fixed N loss and NO2- reoxidation (N recycling) in various natural environments.

SUBMITTER: Kobayashi K 

PROVIDER: S-EPMC6775995 | biostudies-literature | 2019 Oct

REPOSITORIES: biostudies-literature

altmetric image

Publications

Dual nitrogen and oxygen isotope fractionation during anaerobic ammonium oxidation by anammox bacteria.

Kobayashi Kanae K   Makabe Akiko A   Yano Midori M   Oshiki Mamoru M   Kindaichi Tomonori T   Casciotti Karen L KL   Okabe Satoshi S  

The ISME journal 20190528 10


Natural abundance of stable nitrogen (N) and oxygen (O) isotopes are invaluable biogeochemical tracers for assessing the N transformations in the environment. To fully exploit these tracers, the N and O isotope effects (<sup>15</sup>ε and <sup>18</sup>ε) associated with the respective nitrogen transformation processes must be known. However, the N and O isotope effects of anaerobic ammonium oxidation (anammox), one of the major fixed N sinks and NO<sub>3</sub><sup>-</sup> producers, are not well  ...[more]

Similar Datasets

| S-EPMC3697569 | biostudies-literature
| PRJNA454513 | ENA
| S-EPMC4070702 | biostudies-literature
| S-EPMC7188810 | biostudies-literature
| S-EPMC3839690 | biostudies-literature
| S-EPMC3082692 | biostudies-literature
| PRJNA526389 | ENA
| S-EPMC3666723 | biostudies-literature