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Ward, B. B.

Publications and source records attributed to Ward, B. B..

3 recordsLinked to original sources

Origin, age, and metabolisms of dominant anammox bacteria in the global oxygen deficient zones

Anammox bacteria inhabiting oxygen deficient zones (ODZs) are a major functional group mediating fixed nitrogen loss and thus exerting a critical control on the nitrogen budget in the global ocean. However, the diversity, origin, and broad metabolisms of ODZ anammox bacteria remain unknown. Here we report two novel metagenome-assembled genomes of Scalindua, which represent most, if not all, of the anammox bacteria in the global ODZs. Beyond the core anammox metabolism, both organisms contain cyanase and the more dominant one encodes a urease, indicating ODZ anammox bacteria can utilize cyanate and urea in addition to ammonium. The first ODZ Scalindua likely derived from the benthos [~]200 million years ago. Compared to benthic strains of the same clade, ODZ Scalindua uniquely encode genes for urea utilization but lost genes related to growth arrest, flagellum synthesis, and chemotaxis, presumably for adaptation to the anoxic water column.

microbiology↗

Differential substrate affinity and catabolite repression enable preferential use of urea by ammonia-oxidizing bacteria

Four distinct lineages of ammonia-oxidizing microorganisms (AOM) collectively contribute to one of the largest nitrogen fluxes in the global nitrogen budget. AOM possess widely different specific affinities for ammonia, thought to determine their niche differentiation. Nevertheless, ammonia-oxidizing archaea and bacteria (AOA, AOB), and complete ammonia oxidizers (comammox) co-occur in soils, freshwater sediments, and aquifers, suggesting that other factors must drive their coexistence. Here, we show that representatives of four AOM lineages employ distinct regulatory strategies for ammonia or urea utilization, thereby minimizing direct competition for either substrate. The tested AOA and comammox species preferentially used ammonia over urea, while beta-proteobacterial AOB favored urea utilization, repressed ammonia transport in the presence of urea, and showed higher affinity for urea than ammonia, whereas gamma-proteobacterial AOB co-utilized both substrates. Stable isotope tracing, kinetics, and transcriptomics experiments revealed that both assimilation and oxidation of ammonia are transport-dependent. These results reveal novel mechanisms of nitrogen metabolism regulation and transporter-based affinity underlying the contrasting niche adaptation and coexistence patterns among the major AOM lineages.

microbiology↗

Genome-resolved metagenomics reveals abundant nitrate reducers and partitioning of nitrite usage within global oxygen deficient zones

Oxygen deficient zones (ODZs) account for about 30% of total oceanic fixed nitrogen loss via processes including denitrification, a microbially-mediated pathway proceeding stepwise from NO3- to N2. This process may be performed entirely by complete denitrifiers capable of all four steps, but many organisms possess only partial denitrification pathways, either producing or consuming key intermediates such as the greenhouse gas N2O. Marker gene surveys have revealed a diversity of denitrification genes within ODZs, but whether these genes are primarily carried by complete or partial denitrifiers and the identities of denitrifying taxa remain open questions. From 56 metagenomes spanning all three major ODZs, we use genome-resolved metagenomics to reveal the predominance of partial denitrifiers, particularly single-step denitrifiers. We find niche differentiation among nitrogen-cycling organisms, with communities performing each nitrogen transformation distinct in taxonomic identity and motility traits. Our collection of 962 metagenome-assembled genomes presents the largest collection of pelagic ODZ microbes and reveals a clearer picture of the nitrogen cycling community within this environment.

microbiology↗