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Babbin, A. R.

Publications and source records attributed to Babbin, A. R..

5 recordsLinked to original sources

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↗

Sinking diatom aggregates provide carbon to drive microscale denitrification in a bulk oxygenated ocean

Sinking marine particles drive the biological gravitational pump that naturally sequesters carbon dioxide from the atmosphere. Ubiquitous throughout the ocean, these particles are largely composed of phytoplankton that aggregate together or are repackaged by zooplankton into pellets that sink to the deep. Despite their small size, the compartmentalized nature of these particles promotes intense localized metabolic activity by the bacteria lucky enough to colonize them. Due to their sheer numbers, these microscale interactions can change the chemistry of the bulk ocean and impact global biogeochemical budgets. As soon as phytoplankton-derived particles are exported from the surface ocean, the fate of the carbon depends on the lability and availability of the carbon, the diffusive supply of oxidants from the bulk, and the development of microbial communities throughout the aggregate. Here we show with a model experimental system that aggregates composed of marine diatoms -- important primary producers substantially contributing to global carbon export -- can support active denitrification even among bulk oxygenated water ill-conducive to anaerobic metabolisms. We further show the primary nitrite maximum could be formed, in part, due to dissimilatory reduction of nitrate and nitrite occurring at anoxic microsites within such particles. Particle-based denitrification and other anaerobic metabolisms can change the global budget of elemental cycles important for life and climate across the oceans.

microbiology↗

Nitrite accumulation and the associated anammox bacteria niche partitioning in marine sediments

By consuming ammonium and nitrite, anammox bacteria form an important functional guild in nitrogen cycling in many environments including marine sediments. Recent studies have shown that anammox bacteria can consume most of the upwardly diffusing ammonium from deep anoxic sediments; however, their impact on the other important substrate nitrite has not been well characterized. Here we show niche partitioning of two anammox families emerges in a 2.4-m long mostly anoxic sediment core retrieved from the Nordic Seas. We document high abundances (~106 cells g-1) of anammox bacteria in most investigated sediment layers, with two distinct anammox abundance maxima in two nitrite consumption zones. Between the two anammox abundance maxima, nitrite accumulates as observed in other marine sediment sites and aquatic environments, indicating anammox bacteria play a fundamental role in modulating the nitrite distribution. Anammox bacteria in the upper nitrite consumption zone are dominated by the Candidatus Bathyanammoxibiaceae family, while Ca. Scalinduaceae family dominate at the lower zone. A high-quality representative Ca. Bathyanammoxibiaceae genome is recovered, which, comparing to Ca. Scalindua sediminis, the representative of Scalinduaceae in marine sediments, has fewer high-affinity ammonium transporters and lacks the capacity to access alternative substrates or energy sources such as urea and cyanate. These features may restrict Ca. Bathyanammoxibiaceae to conditions of higher ammonium concentrations or fluxes, and therefore drive the observed niche partitioning. These findings improve our understanding about nitrogen cycling in marine sediments by revealing the association between nitrite accumulation and niche partitioning of anammox bacteria.

microbiology↗

Porous marine snow differentially benefits chemotactic, motile, and non-motile bacteria

Particulate organic carbon settling through the marine water column is a key process that regulates global climate by sequestering atmospheric carbon. The initial colonization of marine particles by heterotrophic bacteria represents the first step in recycling this carbon back to inorganic constituents - setting the magnitude of vertical carbon transport to the abyss. Here, we demonstrate experimentally that bacterial motility is required for particle colonization and chemotaxis specifically benefits at higher settling velocities. We further explore the role of particle microstructure on the colonization efficiency of bacteria with different motility traits. We highlight that non-motile cells benefit disproportionally from the porous microstructure and are relatively enriched in the particle wake due to the efficient particle colonization of chemotactic and motile cells. Our results imply that although the chemotactic and motile bacteria benefit from the high nutrient availability when colonizing the particles, scavenging of these cells benefits the often oligotrophic, non-motile cells common among the planktonic community. Significance statementBacteria in the ocean rely on ephemeral nutrient patches from sinking marine particles, but attaching to these structures is challenging as particle settling rates often exceed bacterial swimming velocities and the numerically dominant marine bacteria are non-motile - posing an interesting paradox about the prominence of particle foraging. Here, we quantify the importance of chemotaxis and motility for the efficient colonization of marine particles and find that although chemotaxis provides a clear advantage, motility is the basic requirement for particle colonization. We expand this analysis to consider highly heterogeneous particle structures and find a disproportionate benefit for non-motile cells by facilitating a direct encounter with the particle surface and enriching non-motile microbes in the nutrient-rich particle plume.

microbiology↗

Aerobic Bacteria Produce Nitric Oxide via Denitrification and Trigger Algal Population Collapse

Microbial interactions govern marine biogeochemistry. These interactions are generally considered to rely on exchange of organic molecules. Here we report on a novel inorganic route of microbial communication, showing that algal-bacterial interactions are mediated through inorganic nitrogen exchange. Under oxygen-rich conditions, aerobic bacteria reduce algal-secreted nitrite to nitric oxide (NO) through denitrification, a well-studied anaerobic respiration mechanism. Bacteria secrete NO, triggering a cascade in algae akin to programmed cell death. During death, algae further generate NO, thereby propagating the signal in the algal population. Eventually, the algal population collapses, similar to the sudden demise of oceanic algal blooms. Our study suggests that the exchange of denitrification intermediates, particularly in oxygenated environments, is an overlooked yet ecologically significant route of microbial communication within and across kingdoms. One Sentence SummaryAerobic bacteria activate denitrification in oxygenated conditions and produce nitric oxide that kills their algal partners

microbiology↗