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Milucka, J.

Publications and source records attributed to Milucka, J..

5 recordsLinked to original sources

Occurrence and temporal dynamics of denitrifying protist endosymbionts in the wastewater microbiome

Effective wastewater treatment is of critical importance for preserving public health and protecting natural environments. Key processes in wastewater treatment, such as denitrification, are performed by a diverse community of prokaryotic and eukaryotic microbes. However, the diversity of the microbiome and the potential role of the different microbial taxa in some wastewater treatment plant setups is not fully understood. We aimed to investigate the presence and diversity of denitrifying bacteria of the candidate family Azoamicaceae that form obligate symbioses with protists in wastewater treatment plants. Our analyses showed that denitrifying endosymbionts belonging to the Ca. Azoamicus genus are present in 20-50% of wastewater treatment plants worldwide. Time-resolved amplicon data from four Danish wastewater treatment plants showed high temporal fluctuations in the abundance and composition of the denitrifying endosymbiont community. Fifteen high-quality metagenome-assembled genomes of denitrifying endosymbionts, four of which were circular, were recovered. Genome annotation showed that a newly described, globally widespread species, Ca. Azoamicus parvus, lacked a nitrous oxide reductase, suggesting that its denitrification pathway is incomplete. This observation further expands the diversity of metabolic potentials found in denitrifying endosymbionts and indicates that the contribution of microbial eukaryote holobionts to the wastewater ecosystem dynamics of nitrogen removal and greenhouse gas production may have been underestimated and needs further study.

microbiology↗

Genetic potential for aerobic respiration and denitrification in globally distributed respiratory endosymbionts

The endosymbiont Candidatus Azoamicus ciliaticola generates ATP for its eukaryotic host, an anaerobic ciliate of the Plagiopylea class, fulfilling a function analogous to mitochondria in other eukaryotic cells. The discovery of this respiratory endosymbiosis has major implications for both evolutionary history and ecology of microbial eukaryotes. However, with only a single species described, knowledge of its environmental distribution and diversity is limited. Here we report four new complete, circular metagenome assembled genomes (cMAGs) representing respiratory endosymbionts inhabiting groundwater in California, Ohio, and Germany. These cMAGs form two lineages comprising a monophyletic clade within the uncharacterized gammaproteobacterial order UBA6186, enabling evolutionary analysis of their key protein complexes. Strikingly, all four novel cMAGs encode a cytochrome cbb3 oxidase, which indicates the capacity for both aerobic and anaerobic respiration. Accordingly, we detect these respiratory endosymbionts in diverse habitats worldwide, thus significantly expanding the ecological scope of this respiratory symbiosis.

microbiology↗

Microplastics reduce the efficiency of the biological carbon pump by decreasing the settling velocity and carbon content of marine snow

Plastics are pervasive in marine ecosystems and ubiquitous in both shallow and deep oceans. Microfibers, amongst other microscopic plastics, accumulate in deep sea sediments at concentrations up to four orders of magnitude higher than in surface waters. This is at odds with the fact that most microfibers are positively buoyant; therefore, it is hypothesized that settling aggregates are vectors for downward transport of microfibers in the ocean. However, little is known about the impact of microfibers on carbon export. We formed diatom aggregates with differing concentrations of microfibers using roller tanks and observed that microfiber addition stimulated aggregate formation, but decreased their structural cohesion and caused them to break apart more readily, resulting in smaller average sizes. Incorporation of positively buoyant microfibers into settling aggregates reduced their size-specific sinking velocities proportional to the microfiber concentration. Slower sinking may extend aggregate retention time in the upper ocean, thereby increasing the time available for organic matter remineralization in the upper water column. Here, we show that microfiber concentrations typical of those in the English Channel and Atlantic Ocean decrease potential export flux by 15-50%. Present day microfiber concentrations in surface waters may therefore be substantially reducing the efficiency of the biological carbon pump relative to the pre-plastic era.

biochemistry↗

Anaerobic metabolism of Foraminifera thriving below the seafloor

Foraminifera are single-celled eukaryotes (protists) of large ecological importance, as well as environmental and paleoenvironmental indicators and biostratigraphic tools. In addition, they are capable of surviving in anoxic marine environments where they represent a major component of the benthic community. However, the cellular adaptations of Foraminifera to the anoxic environment remain poorly constrained. We sampled an oxic-anoxic transition zone in marine sediments from the Namibian shelf, where the genera Bolivina and Stainforthia dominated the Foraminifera community, and use metatranscriptomics to characterize Foraminifera metabolism across the different geochemical conditions. The relative abundance of Foraminifera gene expression in anoxic sediment depths increased an order of magnitude, which was confirmed in a ten-day incubation experiment where the development of anoxia coincided with a 27-fold increase in the relative abundance of Foraminifera protein encoding transcripts. This indicates that many Foraminifera were not only surviving, but thriving under the anoxic conditions. The anaerobic energy metabolism of these active Foraminifera was characterized by fermentation of sugars and amino acids, dissimilatory nitrate reduction, fumarate reduction, and dephosphorylation of creatine phosphate. This was co-expressed alongside genes involved in production of reticulopodia, phagocytosis, calcification, and clathrin-mediated-endocytosis (CME). Thus, Foraminifera may use CME under anoxic conditions to utilize dissolved organic matter as a carbon and energy source, in addition to ingestion of prey cells via phagocytosis. These mechanisms help explain how some Foraminifera can thrive under anoxia, which would help to explain their ecological success documented in the fossil record since the Cambrian period more than 500 million years ago.

microbiology↗

Dark aerobic sulfide oxidation by anoxygenic phototrophs in the anoxic waters of Lake Cadagno

SUMMARYAnoxygenic phototrophic sulfide oxidation by green and purple sulfur bacteria (PSB) plays a key role in sulfide removal from anoxic shallow sediments and stratified waters. Although some PSB can also oxidize sulfide with nitrate and oxygen, little is known about the prevalence of this chemolithotrophic lifestyle in the environment. In this study, we investigated the role of these phototrophs in light-independent sulfide removal in the chemocline of Lake Cadagno. Our temporally resolved, high-resolution chemical profiles indicated that dark sulfide oxidation was coupled to high oxygen consumption rates of ~9 M O2{middle dot}h-1. Single-cell analyses of lake water incubated with 13CO2 in the dark revealed that Chr. okenii was to a large extent responsible for aerobic sulfide oxidation and it accounted for up to 40 % of total dark carbon fixation. The genome of Chr. okenii reconstructed from the Lake Cadagno metagenome confirms its capacity for microaerophilic growth and provides further insights into its metabolic capabilities. Moreover, our genomic and single-cell data indicated that other PSB grow microaerobically in these apparently anoxic waters. Altogether, our observations suggest that aerobic respiration may not only play an underappreciated role in anoxic environments, but also that organisms typically considered strict anaerobes may be involved.\n\nORIGINALITY-SIGNIFICANCE STATEMENTThis study reveals that dark aerobic sulfide oxidation within an anoxic layer dominated by anoxygenic phototrophic bacteria in the stratified water column of Lake Cadagno is to a large extent carried out by the anoxygenic phototrophic bacterium Chromatium okenii. Our findings imply that aerobic metabolisms may be more prevalent in anoxic zones than previously thought. We also present an environmental metagenome-assembled genome of Chr. okenii which is the first genome sequence for the genus Chromatium and reveals new interesting physiological features of this environmentally relevant organism, including its capacity for aerobic respiration.

microbiology↗