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1. Patchy Blooms and Multifarious Ecotypes of Labyrinthulomycetes Protists and Their Implication in Vertical Carbon Export in the Pelagic Eastern Indian Ocean

   https://doi.org/10.1128/spectrum.00144-22  

   Xie, Ningdong; Bai, Mohan; Liu, Lu; Li, Jiaqian; He, Yaodong; Collier, Jackie L.; Hunt, Dana E.; Johnson, Zackary I.; Jiao, Nianzhi; Wang, Guangyi (June 2022, Microbiology Spectrum)

   dos Santos, Adriana Lopes (Ed.)

   ABSTRACT Labyrinthulomycetes protists are an important heterotrophic component of microeukaryotes in the world’s oceans, but their distribution patterns and ecological roles are poorly understood in pelagic waters. This study employed flow cytometry and high-throughput sequencing to characterize the abundance, diversity, and community structure of Labyrinthulomycetes in the pelagic Eastern Indian Ocean. The total Labyrinthulomycetes abundance varied much more among stations than did the abundance of prokaryotic plankton, reaching over 1,000 cells mL −1 at a few “bloom” stations. The total Labyrinthulomycetes abundance did not decline with depth throughout the whole water column (5 to 2,000 m) like the abundance of prokaryotic plankton did, and the Labyrinthulomycetes average projected biomass over all samples was higher than that of the prokaryotic plankton. However, Labyrinthulomycetes diversity showed obvious vertical variations, with richness, Shannon diversity, and evenness greatest in the upper epipelagic, lower epipelagic, and deep waters, respectively. Many abundant phylotypes were detected across multiple water layers, which aligned with the constant vertical Labyrinthulomycetes biomass, suggesting potential sinking and contribution to the biological pump. Hierarchical clustering revealed distinct ecotypes partitioning by vertical distribution patterns, suggesting their differential roles in the carbon cycle and storage processes. Particularly, most phylotypes showed patchy distributions (occurring in only few samples) as previously found in the coastal waters, but they were less associated with the Labyrinthulomycetes blooms than the prevalent phylotypes. Overall, this study revealed distinct patterns of Labyrinthulomycetes ecotypes and shed light on their importance in the pelagic ocean carbon cycling and sequestration relative to that of the prokaryotic plankton. IMPORTANCE While prokaryotic heterotrophic plankton are well accepted as major players in oceanic carbon cycling, the ecological distributions and functions of their microeukaryotic counterparts in the pelagic ocean remain largely unknown. This study focused on an important group of heterotrophic (mainly osmotrophic) protistan microbes, the Labyrinthulomycetes, whose biomass can surpass that of the prokaryotic plankton in many marine ecosystems, including the bathypelagic ocean. We found patchy horizontal but persistent vertical abundance profiles of the Labyrinthulomycetes protists in the pelagic waters of the Eastern Indian Ocean, which were distinct from the spatial patterns of the prokaryotic plankton. Moreover, multiple Labyrinthulomycetes ecotypes with distinct vertical patterns were detected and, based on the physiologic, metabolic, and genomic understanding of their cultivated relatives, were inferred to play multifaceted key roles in the carbon cycle and sequestration, particularly as contributors to the vertical carbon export from the surface to the dark ocean, i.e., the biological pump. 

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2. Contrasting diversity patterns of prokaryotes and protists over time and depth at the San-Pedro Ocean Time series

   https://doi.org/10.1038/s43705-022-00121-8  

   Yeh, Yi-Chun; Fuhrman, Jed A. (April 2022, ISME Communications)

   Abstract Community dynamics are central in microbial ecology, yet we lack studies comparing diversity patterns among marine protists and prokaryotes over depth and multiple years. Here, we characterized microbes at the San-Pedro Ocean Time series (2005–2018), using SSU rRNA gene sequencing from two size fractions (0.2–1 and 1–80 μm), with a universal primer set that amplifies from both prokaryotes and eukaryotes, allowing direct comparisons of diversity patterns in a single set of analyses. The 16S + 18S rRNA gene composition in the small size fraction was mostly prokaryotic (>92%) as expected, but the large size fraction unexpectedly contained 46–93% prokaryotic 16S rRNA genes. Prokaryotes and protists showed opposite vertical diversity patterns; prokaryotic diversity peaked at mid-depth, protistan diversity at the surface. Temporal beta-diversity patterns indicated prokaryote communities were much more stable than protists. Although the prokaryotic communities changed monthly, the average community stayed remarkably steady over 14 years, showing high resilience. Additionally, particle-associated prokaryotes were more diverse than smaller free-living ones, especially at deeper depths, contributed unexpectedly by abundant and diverse SAR11 clade II. Eukaryotic diversity was strongly correlated with the diversity of particle-associated prokaryotes but not free-living ones, reflecting that physical associations result in the strongest interactions, including symbioses, parasitism, and decomposer relationships. 

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3. Sinking Trichodesmium fixes nitrogen in the dark ocean

   https://doi.org/10.1038/s41396-022-01289-6  

   Benavides, Mar; Bonnet, Sophie; Le Moigne, Frédéric A. C.; Armin, Gabrielle; Inomura, Keisuke; Hallstrøm, Søren; Riemann, Lasse; Berman-Frank, Ilana; Poletti, Emilie; Garel, Marc; et al (July 2022, The ISME Journal)

   Abstract The photosynthetic cyanobacterium Trichodesmium is widely distributed in the surface low latitude ocean where it contributes significantly to N2 fixation and primary productivity. Previous studies found nifH genes and intact Trichodesmium colonies in the sunlight-deprived meso- and bathypelagic layers of the ocean (200–4000 m depth). Yet, the ability of Trichodesmium to fix N2 in the dark ocean has not been explored. We performed 15N2 incubations in sediment traps at 170, 270 and 1000 m at two locations in the South Pacific. Sinking Trichodesmium colonies fixed N2 at similar rates than previously observed in the surface ocean (36–214 fmol N cell−1 d−1). This activity accounted for 40 ± 28% of the bulk N2 fixation rates measured in the traps, indicating that other diazotrophs were also active in the mesopelagic zone. Accordingly, cDNA nifH amplicon sequencing revealed that while Trichodesmium accounted for most of the expressed nifH genes in the traps, other diazotrophs such as Chlorobium and Deltaproteobacteria were also active. Laboratory experiments simulating mesopelagic conditions confirmed that increasing hydrostatic pressure and decreasing temperature reduced but did not completely inhibit N2 fixation in Trichodesmium. Finally, using a cell metabolism model we predict that Trichodesmium uses photosynthesis-derived stored carbon to sustain N2 fixation while sinking into the mesopelagic. We conclude that sinking Trichodesmium provides ammonium, dissolved organic matter and biomass to mesopelagic prokaryotes. 

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4. Housekeeping in the Hydrosphere: Microbial Cooking, Cleaning, and Control under Stress

   https://doi.org/10.3390/life11020152  

   Biddanda, Bopaiah; Dila, Deborah; Weinke, Anthony; Mancuso, Jasmine; Villar-Argaiz, Manuel; Medina-Sánchez, Juan Manuel; González-Olalla, Juan Manuel; Carrillo, Presentación (February 2021, Life)

   Who’s cooking, who’s cleaning, and who’s got the remote control within the waters blanketing Earth? Anatomically tiny, numerically dominant microbes are the crucial “homemakers” of the watery household. Phytoplankton’s culinary abilities enable them to create food by absorbing sunlight to fix carbon and release oxygen, making microbial autotrophs top-chefs in the aquatic kitchen. However, they are not the only bioengineers that balance this complex household. Ubiquitous heterotrophic microbes including prokaryotic bacteria and archaea (both “bacteria” henceforth), eukaryotic protists, and viruses, recycle organic matter and make inorganic nutrients available to primary producers. Grazing protists compete with viruses for bacterial biomass, whereas mixotrophic protists produce new organic matter as well as consume microbial biomass. When viruses press remote-control buttons, by modifying host genomes or lysing them, the outcome can reverberate throughout the microbial community and beyond. Despite recognition of the vital role of microbes in biosphere housekeeping, impacts of anthropogenic stressors and climate change on their biodiversity, evolution, and ecological function remain poorly understood. How trillions of the smallest organisms in Earth’s largest ecosystem respond will be hugely consequential. By making the study of ecology personal, the “housekeeping” perspective can provide better insights into changing ecosystem structure and function at all scales. 

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5. Interactions and Community Structure of Fungi and Prokaryotes in Salt and Brackish Marsh Ecosystems

   https://doi.org/10.1002/edn3.70199  

   Thompson, Madeleine_A; Peng, Xuefeng (October 2025, Environmental DNA)

   ABSTRACT Microbial communities play a fundamental role in biogeochemical cycling within salt and brackish marsh ecosystems, yet fungal‐prokaryotic interactions in these environments remain poorly understood. This study employed metabarcoding of the 16S and 28S rRNA genes to investigate prokaryotic and fungal communities across four locations in sediments and surface waters of the North Inlet salt marsh and Winyah Bay brackish marsh (South Carolina, USA) over four time points from 2020 to 2021. Co‐occurrence network analyses were used to identify potential microbial interactions and their ecological implications. Distinct fungal and prokaryotic communities were observed between the two marsh types. From the 16S prokaryotic primer set, Proteobacteria, Bacteroidota, and Cyanobacteriota dominated both marshes. Early diverging fungi and Actinomycetota (bacteria) were prevalent in the brackish marsh, whereas salt marsh communities were primarily composed of Dikarya fungi (Ascomycota and Basidiomycota) and Desulfobacteria. Network analyses revealed contrasting interactions between surface water and sediment. In brackish marsh sediments, fungi and prokaryotes exhibited nearly exclusively negative connections, suggesting strong resource competition. In contrast, Dikarya fungi in brackish marsh surface water displayed numerous positive connections with bacteria, suggesting potential cross‐feeding interactions. In the salt marsh, fungi and prokaryotes exhibited potential cooperative and competitive/antagonistic interactions. Ascomycota were positively connected with Desulfobacteria, suggesting a role in complex organic matter degradation. Conversely, negative connections between Chytridiomycota (early diverging fungi) and Cyanobacteriota (bacteria) implied parasitic interactions. These findings highlight the dynamic nature of fungal‐prokaryotic interactions in coastal ecosystems. By analyzing potential microbial relationships in salt and brackish marshes, this study provides new insights into the ecological roles of fungi in estuarine environments, particularly their contributions to nutrient cycling and organic matter decomposition. Understanding these interactions is crucial for generating hypotheses and predicting microbial responses to environmental changes—such as shifts in salinity and nutrient availability—and their potential impacts on marsh ecosystem functioning. 

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