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Abstract The bulk of knowledge on marine ciliates is from shallow and/or sunlit waters. We studied ciliate diversity and distribution across epi‐ and mesopelagic oceanic waters, using DNA metabarcoding and phylogeny‐based metrics. We analyzed sequences of the 18S rRNA gene (V4 region) from 369 samples collected at 12 depths (0–1000 m) at the Bermuda Atlantic Time‐series Study site of the Sargasso Sea (North Atlantic) monthly for 3 years. The comprehensive depth and temporal resolutions analyzed led to three main findings. First, there was a gradual but significant decrease in alpha‐diversity (based on Faith's phylogenetic diversity index) from surface to 1000‐m waters. Second, multivariate analyses of beta‐diversity (based on UniFrac distances) indicate that ciliate assemblages change significantly from photic to aphotic waters, with a switch from Oligotrichea to Oligohymenophorea prevalence. Third, phylogenetic placement of sequence variants and clade‐level correlations (EPA‐ng and GAPPA algorithms) show Oligotrichea, Litostomatea, Prostomatea, and Phyllopharyngea as anti‐correlated with depth, while Oligohymenophorea (especially Apostomatia) have a direct relationship with depth. Two enigmatic environmental clades include either prevalent variants widely distributed in aphotic layers (the Oligohymenophorea OLIGO5) or subclades differentially distributed in photic versus aphotic waters (the Discotrichidae NASSO1). These results settle contradictory relationships between ciliate alpha‐diversity and depth reported before, suggest functional changes in ciliate assemblages from photic to aphotic waters (with the prevalence of algivory and mixotrophy vs. omnivory and parasitism, respectively), and indicate that contemporary taxon distributions in the vertical profile have been strongly influenced by evolutionary processes. Integration of DNA sequences with organismal data (microscopy, functional experiments) and development of databases that link these sources of information remain as major tasks to better understand ciliate diversity, ecological roles, and evolution in the ocean. 

Eutrophication and hypoxia markedly alter trophic dynamics and nutrient cycling in estuarine water columns, but little is known about the microbial communities that drive and interact with these changes. Here we studied microbial plankton (bacteria, archaea, protists and micro-metazoans) in a large temperate estuary where bottom hypoxia occurs every summer due to warmer temperatures, stratification, and oxidation of organic matter fueled by nutrient enrichment. We used high-throughput sequencing of the 16S and 18S rRNA genes (V4 region) and quantified multiple abiotic and biotic factors in surface and bottom waters during the summer of 2019. The conditions associated with the intensification of hypoxia in bottom waters as the summer progressed were linked to significant changes in the diversity, community structure and potential functioning of microbial communities. Under maximum hypoxia (dissolved oxygen concentration: 0.9-3.1 mg l -1 ), there were increased proportions of ammonia-oxidizing archaea (AOA), bacterivorous and parasitic protists, and copepod nauplii. Sequence proportions of AOA ( Nitrosopumilus) and nitrite-oxidizing bacteria ( Nitrospinaceae) were significantly correlated with the concentration of oxidized N species (nitrite plus nitrate, which peaked at 14.4 µM) and the proportions of nauplii DNA sequences and biomass. Our data support a tight coupling of biogeochemical and food web processes, with rapid oxidation of ammonia and accumulation of oxidized N species as hypoxia intensifies during the summer. 

Ciliates are abundant microplankton that are widely distributed in the ocean. In this paper, the distribution patterns of ciliate diversity in the South China Sea (SCS) were analyzed by compiling community data from previous publications. Based on morphological identification, a total of 592 ciliate species have been recorded in the SCS. The ciliate communities in intertidal, neritic and oceanic water areas were compared in terms of taxonomy, motility and feeding habit composition, respectively. Significant community variation was revealed among the three areas, but the difference between the intertidal area and the other two areas was more significant than that between neritic and oceanic areas. The distributions of ciliates within each of the three areas were also analyzed. In the intertidal water, the community was not significantly different among sites but did differ among habitat types. In neritic and oceanic areas, the spatial variation of communities among different sites was clearly observed. Comparison of communities by taxonomic and ecological traits (motility and feeding habit) indicated that these traits similarly revealed the geographical pattern of ciliates on a large scale in the SCS, but to distinguish the community variation on a local scale, taxonomic traits has higher resolution than ecological traits. In addition, we assessed the relative influences of environmental and spatial factors on assembly of ciliate communities in the SCS and found that environmental selection is the major process structuring the taxonomic composition in intertidal water, while spatial processes played significant roles in influencing the taxonomic composition in neritic and oceanic water. Among ecological traits, environmental selection had the most important impact on distributions. 

Abstract Schmidingerella arcuata is an ecologically important tintinnid ciliate that has long served as a model species in plankton trophic ecology. We present a partial micronuclear genome and macronuclear transcriptome resource for S. arcuata, acquired using single-cell techniques, and we report on pilot analyses including functional annotation and genome architecture. Our analysis shows major fragmentation, elimination, and scrambling in the micronuclear genome of S. arcuata. This work introduces a new nonmodel genome resource for the study of ciliate ecology and genomic biology and provides a detailed functional counterpart to ecological research on S. arcuata. 

During the last decade, high-throughput metabarcoding became routine for analyzing protistan diversity and distributions in nature. Amid a multitude of exciting findings, scientists have also identified and addressed technical and biological limitations, although problems still exist for inference of meaningful taxonomic and ecological knowledge based on short DNA sequences. Given the extensive use of this approach, it is critical to settle our understanding on its strengths and weaknesses and to synthesize up-to-date methodological and conceptual trends. This article summarizes key scientific and technical findings, and identifies current and future directions in protist research that uses metabarcoding.