Ammonium loss microbiologically mediated by Fe(III) and Mn(IV) reduction along a coastal lagoon system

Microbial manganese redox cycling drives co-removal of nitrate and ammonium

Manganese (Mn), abundant in the Earth's crust, can act as an oxidant or a reductant for diverse nitrogen biotransformation processes. However, the functional microorganisms and their metabolic pathways, as well as interactions, remain largely elusive. Here, a microbial consortium was enriched from a mixture of freshwater sediments and activated sludge by feeding ammonium, nitrate and Mn(II), which established manganese-driven co-removal of nitrate and ammonium with removal rates of 5.83 and 2.30 mg N L-1 d-1, respectively. The batch tests and metagenomic analyses revealed a nitrate-dependent anaerobic manganese oxidation (NDMO) process mediated by Anaerolineales and Phycisphaerales and a manganese reduction coupled to anaerobic ammonium oxidation (Mnammox) process mediated by Chthonomonadales. Based on identified key genes involved in the nitrogen and manganese metabolic pathways, nitrate was likely reduced to nitrite and nitrogen gas in the NDMO process while ammonium was oxidized to nitrite in the Mnammox process, which in turn fuelled the Anammox process carried out by Candidatus Brocadia. This revealed the microbial interactions of NDMO, Mnammox, and Anammox processes responsible for manganese-driven co-removal of ammonium and nitrate. These findings provide a potential solution for biological nitrogen removal and expand our understanding of the nitrogen and manganese biogeochemical cycles.

Nitrogen loss in coastal sediments driven by anaerobic ammonium oxidation coupled to microbial reduction of Mn(IV)-oxide

Coastal sediments play a central role in regulating the amount of land-derived reactive nitrogen (Nr) entering the ocean, and their importance becomes crucial in vulnerable ecosystems threatened by anthropogenic activities. Sedimentary denitrification has been identified as the main sink of Nr in marine environments, while anaerobic ammonium oxidation with nitrite (anammox) has also been pointed out as a key player in controlling the nitrogen pool in these locations. Collected evidence in the present work indicates that the microbial biota in coastal sediments from Baja California (northwestern Mexico) has the potential to drive anaerobic ammonium oxidation linked to Mn(IV) reduction (manganammox). Unamended sediment showed ammonification, but addition of vernadite (δMnO2 with nano-crystal size ∼15 Å) as terminal electron acceptor fueled simultaneous ammonium oxidation (up to ∼400 μM of ammonium removed) and production of Mn(II) with a ratio ∆[Mn(II)]/∆[NH4+] of 1.8, which is very close to the stoichiometric value of manganammox (1.5). Additional incubations spiked with external ammonium also showed concomitant ammonium oxidation and Mn(II) production, accounting for ∼30 % of the oxidized ammonium. Tracer analysis revealed that the nitrogen loss associated with manganammox was 4.2 ± 0.4 μg 30N2/g-day, which is 17-fold higher than that related to the feammox process (anaerobic ammonium oxidation linked to Fe(III) reduction, 0.24 ± 0.02 μg 30N2/g-day). Taxonomic characterization based on 16S rRNA gene sequencing revealed the existence of several clades belonging to Desulfobacterota as potential microorganisms catalyzing the manganammox process. These findings suggest that manganammox has the potential to be an additional Nr sink in coastal environments, whose contribution to total Nr losses remains to be evaluated.