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1. The Bay of Bengal exposes abundant photosynthetic picoplankton and newfound diversity along salinity‐driven gradients

   https://doi.org/10.1111/1462-2920.16431  

   Strauss, Jan; Choi, Chang_Jae; Grone, Jonathan; Wittmers, Fabian; Jimenez, Valeria; Makareviciute‐Fichtner, Kriste; Bachy, Charles; Jaeger, Gualtiero_Spiro; Poirier, Camille; Eckmann, Charlotte; et al (June 2023, Environmental Microbiology)

   Abstract The Bay of Bengal (BoB) is a 2,600,000 km²expanse in the Indian Ocean upon which many humans rely. However, the primary producers underpinning food chains here remain poorly characterized. We examined phytoplankton abundance and diversity along strong BoB latitudinal and vertical salinity gradients—which have low temperature variation (27–29°C) between the surface and subsurface chlorophyll maximum (SCM). In surface waters,Prochlorococcusaveraged 11.7 ± 4.4 × 10⁴ cells ml⁻¹, predominantly HLII, whereas LLII and ‘rare’ ecotypes, HLVI and LLVII, dominated in the SCM.Synechococcusaveraged 8.4 ± 2.3 × 10⁴ cells ml⁻¹in the surface, declined rapidly with depth, and population structure of dominant Clade II differed between surface and SCM; Clade X was notable at both depths. Across all sites,OstreococcusClade OII dominated SCM eukaryotes whereas communities differentiated strongly moving from Arabian Sea‐influenced high salinity (southerly; prasinophytes) to freshwater‐influenced low salinity (northerly; stramenopiles, specifically, diatoms, pelagophytes, and dictyochophytes, plus the prasinophyteMicromonas) surface waters. Eukaryotic phytoplankton peaked in the south (1.9 × 10⁴ cells ml⁻¹, surface) where a novelOstreococcuswas revealed, named hereOstreococcus bengalensis. We expose dominance of a single picoeukaryote and hitherto ‘rare’ picocyanobacteria at depth in this complex ecosystem where studies suggest picoplankton are replacing larger phytoplankton due to climate change. 

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2. High‐frequency sampling captures variability in phytoplankton population‐specific periodicity, growth, and productivity

   https://doi.org/10.1002/lno.12683  

   Hynes, Annette_M; Winter, Jordan; Berthiaume, Chris_T; Shimabukuro, Eric; Cain, Kelsy; White, Angelicque; Armbrust, E_Virginia; Ribalet, François (September 2024, Limnology and Oceanography)

   Abstract The Hawaii Ocean Time‐series (HOT) at Station ALOHA (22.75°N, 158°W) in the North Pacific Subtropical Gyre (NPSG) serves as a critical vantage point for observing plankton biomass production and its ecological implications. However, the HOT program's near‐monthly sampling frequency does not capture shorter time scale variability in phytoplankton populations. To address this gap, we deployed the SeaFlow flow cytometer for continuous monitoring during HOT cruises from 2014 to 2021. This approach allowed us to examine variations in the surface abundance and cell carbon content of specific phytoplankton groups: the cyanobacteriaProchlorococcus,Synechococcus, andCrocosphaeraas well as a range of small eukaryotic phytoplankton ( 5 μm). Our data showed that daily to monthly variability inProchlorococcusandSynechococcusabundance matches seasonal and interannual variability, while small eukaryotic phytoplankton andCrocosphaerashowed the highest seasonal and interannual fluctuations. The study also found that eukaryotic phytoplankton andCrocosphaerahad higher median cellular growth rates (0.076 and , respectively) compared toProchlorococcusandSynechococcus(0.037 and , respectively). These variances in abundance and growth rates indicate that shifts in the community structure significantly impact primary productivity in the NPSG. Our results underscore the importance of daily to monthly phytoplankton dynamics in ecosystem function and carbon cycling. 

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3. Production and cross-feeding of nitrite within Prochlorococcus populations

   https://doi.org/10.1128/mbio.01236-23  

   Berube, Paul M.; O'Keefe, Tyler J.; Rasmussen, Anna; LeMaster, Trent; Chisholm, Sallie W. (July 2023, mBio)

   Dubilier, Nicole (Ed.)

   ABSTRACT Prochlorococcusis an abundant photosynthetic bacterium in the open ocean, where nitrogen (N) often limits phytoplankton growth. In the low-light-adapted LLI clade ofProchlorococcus, nearly all cells can assimilate nitrite (NO₂⁻), with a subset capable of assimilating nitrate (NO₃⁻). LLI cells are maximally abundant near the primary NO₂⁻maximum layer, an oceanographic feature that may, in part, be due to incomplete assimilatory NO₃⁻reduction and subsequent NO₂⁻release by phytoplankton. We hypothesized that someProchlorococcusexhibit incomplete assimilatory NO₃⁻reduction and examined NO₂⁻accumulation in cultures of threeProchlorococcusstrains (MIT0915, MIT0917, and SB) and twoSynechococcusstrains (WH8102 and WH7803). Only MIT0917 and SB accumulated external NO₂⁻during growth on NO₃⁻. Approximately 20–30% of the NO₃⁻transported into the cell by MIT0917 was released as NO₂⁻, with the rest assimilated into biomass. We further observed that co-cultures using NO₃⁻as the sole N source could be established for MIT0917 andProchlorococcusstrain MIT1214 that can assimilate NO₂⁻but not NO₃⁻. In these co-cultures, the NO₂⁻released by MIT0917 is efficiently consumed by its partner strain, MIT1214. Our findings highlight the potential for emergent metabolic partnerships that are mediated by the production and consumption of N cycle intermediates withinProchlorococcuspopulations. IMPORTANCEEarth’s biogeochemical cycles are substantially driven by microorganisms and their interactions. Given that N often limits marine photosynthesis, we investigated the potential for N cross-feeding within populations ofProchlorococcus, the numerically dominant photosynthetic cell in the subtropical open ocean. In laboratory cultures, someProchlorococcuscells release extracellular NO₂⁻during growth on NO₃⁻. In the wild,Prochlorococcuspopulations are composed of multiple functional types, including those that cannot use NO₃⁻but can still assimilate NO₂⁻. We show that metabolic dependencies arise whenProchlorococcusstrains with complementary NO₂⁻production and consumption phenotypes are grown together on NO₃⁻. These findings demonstrate the potential for emergent metabolic partnerships, possibly modulating ocean nutrient gradients, that are mediated by cross-feeding of N cycle intermediates. 

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4. Selective Uptake of Pelagic Microbial Community Members by Caribbean Reef Corals

   https://doi.org/10.1128/AEM.03175-20  

   Hoadley, Kenneth D.; Hamilton, Maria; Poirier, Camille L.; Choi, Chang Jae; Yung, Cheuk-Man; Worden, Alexandra Z. (April 2021, Applied and Environmental Microbiology)

   Johnson, Karyn N. (Ed.)

   ABSTRACT Coral reefs are possible sinks for microbes; however, the removal mechanisms at play are not well understood. Here, we characterize pelagic microbial groups at the CARMABI reef (Curaçao) and examine microbial consumption by three coral species: Madracis mirabilis , Porites astreoides , and Stephanocoenia intersepta . Flow cytometry analyses of water samples collected from a depth of 10 m identified 6 microbial groups: Prochlorococcus , three groups of Synechococcus , photosynthetic eukaryotes, and heterotrophic bacteria. Minimum growth rates (μ) for Prochlorococcus , all Synechococcus groups, and photosynthetic eukaryotes were 0.55, 0.29, and 0.45 μ day −1 , respectively, and suggest relatively high rates of productivity despite low nutrient conditions on the reef. During a series of 5-h incubations with reef corals performed just after sunset or prior to sunrise, reductions in the abundance of photosynthetic picoeukaryotes, Prochlorococcus and Synechococcus cells, were observed. Of the three Synechococcus groups, one decreased significantly during incubations with each coral and the other two only with M. mirabilis. Removal of carbon from the water column is based on coral consumption rates of phytoplankton and averaged between 138 ng h −1 and 387 ng h −1 , depending on the coral species. A lack of coral-dependent reduction in heterotrophic bacteria, differences in Synechococcus reductions, and diurnal variation in reductions of Synechococcus and Prochlorococcus , coinciding with peak cell division, point to selective feeding by corals. Our study indicates that bentho-pelagic coupling via selective grazing of microbial groups influences carbon flow and supports heterogeneity of microbial communities overlying coral reefs. IMPORTANCE We identify interactions between coral grazing behavior and the growth rates and cell abundances of pelagic microbial groups found surrounding a Caribbean reef. During incubation experiments with three reef corals, reductions in microbial cell abundance differed according to coral species and suggest specific coral or microbial mechanisms are at play. Peaks in removal rates of Prochlorococcus and Synechococcus cyanobacteria appear highest during postsunset incubations and coincide with microbial cell division. Grazing rates and effort vary across coral species and picoplankton groups, possibly influencing overall microbial composition and abundance over coral reefs. For reef corals, use of such a numerically abundant source of nutrition may be advantageous, especially under environmentally stressful conditions when symbioses with dinoflagellate algae break down. 

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5. Plasticity in the grazing ecophysiology of Florenciella (Dichtyochophyceae), a mixotrophic nanoflagellate that consumes Prochlorococcus and other bacteria

   https://doi.org/10.1002/lno.11585  

   Li, Qian; Edwards, Kyle F.; Schvarcz, Christopher R.; Selph, Karen E.; Steward, Grieg F. (August 2020, Limnology and Oceanography)

   Abstract Mixotrophic nanoflagellates can account for more than half of the bacterivory in the sunlit ocean, yet very little is known about their ecophysiology. Here, we characterize the grazing ecology of an open‐ocean mixotroph in the genusFlorenciella(class Dictyochophyceae). Members of this class were indirectly implicated as major consumers ofProchlorococcusandSynechococcusin the oligotrophic North Pacific Subtropical Gyre, but their phagotrophic capabilities have never been investigated. Our studies showed thatFlorenciellareadily consumedProchlorococcus,Synechococcus, and heterotrophic bacteria, and that the ingested prey relieved nutrient limitations on growth.Florenciellagrew faster (3 d⁻¹) in nitrogen‐deplete medium given sufficient liveSynechococcus, than in nitrogen‐replete K medium (2 d⁻¹), but it did not grow in continuous darkness. Grazing rates were substantially higher under nutrient limitation and showed a hint of diel variability, with rates tending to be highest near the end of the light period. An apparent trade‐off between the maximum clearance rate (5 nLFlorenciella⁻¹h⁻¹) and the maximum ingestion rate (up to ∼ 10 prey cellsFlorenciella⁻¹h⁻¹) across experiments suggests that grazing behavior may also vary in response to prey concentration. If the observed grazing rates are representative of other open‐ocean mixotrophs, their collective activity could account for a significant fraction of the daily cyanobacterial mortality. This study provides essential parameters for understanding the grazing ecology of a common marine mixotroph and the first characterization of mixotrophic nanoflagellate functional responses when feeding on unicellular cyanobacteria, the dominant marine primary producers in the oligotrophic ocean. 

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