Limnology and Oceanography

Hydrodynamics is a strong regulator of phytoplankton cell densities and population connectivity. However, the extent to which hydrodynamics, specifically dilution and advection, dictates the internal physiological state and overall bloom dynamics remains poorly understood. We conducted an integrated study of the harmful diatom Pseudo-nitzschia australis in two neighboring coastal bays with similar abiotic conditions but contrasting bloom trajectories. Using a combination of field observations, transcriptomics, domoic acid (DA) measurements, and hydrodynamic simulations, we show that a three-fold difference in dilution rates alone explains a 25-day shift in bloom timing and an order-of-magnitude difference in cell densities. Transcriptomic profiling revealed distinct metabolic and stress-associated gene modules that synchronized with hydrodynamically-mediated nutrient depletion rate, linking residence times to cellular mortality. Furthermore, directional connectivity between the bays may explain population-level toxin heterogeneity, as advection of older cells, releasing DA outside the cells, may have decreased the proportion of intracellular DA in the destination bay. Our results illustrate that hydrodynamics do not merely modulate population transport; they structure the full physiological life cycle of a bloom, from initiation to nutrient-driven demise. This highlights the necessity of considering hydrodynamics as a primary explanation for bloom dynamics with cascading effects on bloom onset, cell density, nutrient consumption, cell physiology and mortality.

Intertidal mudflats hosting diatom-dominated microphytobenthic communities experience strong variability in environmental conditions, which can lead to cellular oxidative stress. These constraints can, in some cases, affect diatom metabolism and photosynthetic performance in the short term, potentially compromising their survival and even leading to cell death. This study investigates pigment, isoprostanoid, and photophysiological changes in a diatom assemblage originating from a natural microphytobenthic biofilm under different durations of helium-oxygen bubbling cold atmospheric plasma experimental treatments, mimicking complex oxidative conditions of the environment. To this end, 2-min and 5-min treatments were applied to the diatom assemblage, and metabolic parameters were monitored over time up to +180 min after plasma treatment cessation. Despite physicochemical changes and slight perturbations in metabolite profiles induced by plasma treatments, photosynthetic capacities of the diatoms remained largely preserved. The duration-dependent effects of plasma treatments induced selective and mostly reversible changes, primarily characterized by an increase in the relative proportions of pheopigments and a decrease in the relative proportions of {beta}-carotenes following the 5-min treatment. A transient decrease in the relative proportions of the isoprostanoids 10-F4t-neuroP and 5-F2t-IsoP was also observed. By exposing natural diatom assemblage to plasma-generated oxidative conditions, this study provides novel insights into how marine microbiome respond to oxidative perturbations, contributing to our understanding of diatom success in fluctuating intertidal environments.

Oligotrophic subtropical waters are some of the ocean's largest continuous ecosystems, yet their protist diversity and community succession remain poorly understood. We examined the protist community in the surface waters of the Gulf of Aqaba at near-daily resolution from March 2024 to July 2025 using an Imaging FlowCytobot. The record revealed a clear seasonal succession. Total cell density increased nearly threefold during winter mixing, driven mainly by an increase in cells smaller than 5 microns. Cells were generally larger during summer, making total biovolume similar in summer and winter. Biovolume reached its highest sustained values during the spring bloom. Despite its low cell density, the summer community was dynamic, with sudden appearances of euglenophytes, flagellates and dinoflagellates at high densities. Coccolithophores and cryptophytes increased during winter, followed by diatoms and ciliates in spring. We also provide a dataset of 31,700 annotated IFCB images.

The picocyanobacterium Prochlorococcus is a fundamental contributor to ocean primary productivity. While its free-living population has been extensively studied, primarily using flow cytometric analyses, the size and distribution of its particle-associated population is not well understood. Using filter fractionated samples from cruises in the Pacific Ocean, Atlantic Ocean, and Mediterranean Sea, we generated metagenomic data using internal standards, yielding absolute genome equivalent counts of Prochlorococcus cells in different size fractions. We used these data to model a relationship between relative and absolute genome equivalent counts, yielding a correction factor that we validated using published datasets. We then applied the correction factor to size-fractionated global metagenomic data from the TARA Oceans Project, which has widespread Prochlorococcus cells in size fractions >1.6 m throughout the transects, to calculate the fraction of the total Prochlorococcus population in large size fractions. The ''particle-associated'' population fraction increased with net primary productivity. Dissolved inorganic carbon was also directly correlated with increased particle association, which, combined with other evidence, could indicate an association with upwelling. We also examined the relationship between particle-associated population and carbon export at 150 m by incorporating published estimates of carbon flux based on TARA optical scattering data. This study highlights the potential importance of particle-associated Prochlorococcus to carbon flux in marine ecosystems and offers a way to convert relative to absolute genome equivalents of microorganisms in archival metagenomic datasets.

Inshore coastal waters are almost invariably supersaturated with respect to methane and are thereby sources of methane to the atmosphere. We investigated floating algal mats and surface waters of four contrasting inshore habitats and quantified methane concentrations, sea-to-air emissions, and microbial community composition of surface waters over a seasonal cycle to determine the potential for in-situ microbial methane production in shallow oxygen-saturated surface waters with floating algal biomass. 16S rDNA sequencing indicated that Archaea belonging to the genera Methanocorpusculum, Methanosarcina, Candidatus Methanomethylophilus, and some genera from order Methanobacteriales occurred in the floating algal mats. qPCR of the genes encoding the methyl coenzyme M reductase mcrA revealed the highest expression levels during the warmest sampling periods supporting active methane production directly in surface water. Co-occurrence of the Archaea sequences and sequences belonging to the cyanobacterium strain Nodularia PCC 9350 suggests a structural relationship. Our study underscores the significant, yet underexplored impact of methane production on the surface in aggregates of floating algal material. While Nodularia and methanogens can exist independently in surface waters, their co-occurrence in algal mats reveals where the layered mat structure creates distinct microenvironments that facilitate direct metabolic exchange and provide physical stability for both groups, thereby potentially enhancing methane production in these shallow coastal systems.

Marine diatoms contribute to about 20% of global primary production. We present the first basin-scale, multiyear assessment of diatom communities in the North Pacific, combining taxonomically high-resolution RuBisCO large subunit gene (rbcL) metabarcoding with concurrent environmental measurements. Using a nine-year time series of daily samples resolved at the species level via ~500 bp rbcL fragments, we performed multivariate analyses across biogeographic provinces, identifying significant correlations between community structure and environmental drivers such as temperature and macronutrient availability. We report the prevalence of a previously overlooked centric diatom species in the North Pacific, Eunotogramma lunatum, which appears to be near-dominant even in subarctic high-nitrate, low-chlorophyll waters where pennate diatoms are typically favored. These results demonstrate the power of rbcL for large-scale ocean monitoring and provide a critical baseline for future studies of diatom population dynamics, climate change impacts, and ecosystem resilience in a key marine region.

Hydrostatic pressure is a defining feature of the deep ocean, yet how it structures microbial activity across the subseafloor biosphere is poorly understood. Here, we assess pressure effects on anabolic activity in seafloor and subseafloor communities across a margin-to-hadal-to-abyssal transect of the Puerto Rico Trench region (493-8,385 m water depth). Community-level responses to pressure reverse with burial, revealing a previously unrecognized shift toward piezophily in resident subseafloor communities down to 20 meters below seafloor (mbsf). In pressure-incubation experiments, atmospheric pressure yielded higher proportions of active cells in surficial sediments, whereas in situ pressure yielded higher proportions in the subseafloor. Pressure also structured active-community composition; in trench-axis sediments extending to 8.35 mbsf, JS1/Atribacterota populations belonging to geographically widespread hadal lineages exhibited a physiological response to in situ pressure, indicative of subseafloor piezophily. These findings suggest that hydrostatic pressure acts as an ecological filter after burial, favoring piezophilic traits that may support microbial persistence in the deep subseafloor biosphere.

Eutrophication and warming in Lake Erie create two microbial threats: cyanobacterial harmful algal blooms (cHABs) that can produce toxins, and seasonal hypoxia driven by microbial respiration. These phenomena are often studied separately, with cHABs research focused on the Western basin and hypoxia on the Central basin. We conducted lakewide microbial sampling at three time points in 2024 (May, August, and September), integrating physicochemical data, cyanotoxin quantification, amplicon sequencing, and flow cytometry. We demonstrate that cyanobacteria form spatially and seasonally distinct "cohorts" that act as hubs structuring abundant, diverse, and active communities across all basins. These cohorts display distinct relationships with heterotrophic communities, with colonial, bloom-forming cohorts (i.e., C1: Microcystis, C2: Pseudanabaena) associated with higher richness and evenness, the picocyanobacterium C3: Cyanobium with increased heterotrophic abundance, and C2: Pseudanabaena additionally associated with increased numbers of metabolically active cells. Neither temperature nor nutrient concentrations consistently explained these patterns, although total phosphorus correlated with bloom-forming C1 and C2 cohorts. The cohorts also formed structured "consortia" with heterotrophic taxa, with each cyanobacterial group associated with consistent sets of heterotrophic partners. Together, these results are consistent with a model in which cyanobacterial abundance increases heterotrophic growth and respiration, suggesting a lakewide pathway linking cHABs to oxygen demand and hypoxia. IMPORTANCECyanobacterial harmful algal blooms and hypoxia are two microbial processes shaping water quality in Lake Erie, yet they are typically studied separately and at basin-specific scales. We link cyanobacterial abundance to heterotrophic metabolism at a lakewide scale. We show that cyanobacterial abundance is associated with heterotrophic diversity, abundance, and metabolic activity, with contrasting patterns across cyanobacterial functional groups. These relationships were not explained by temperature nor consistently by nutrients, although cyanobacterial distribution in the Central basin is likely linked to nutrient availability as a result of upwellings and basin-wide gyres. Bloom-forming and picocyanobacterial cohorts play fundamentally different roles in structuring microbial diversity and biomass, with implications for how bloom management influences ecosystem metabolism. By identifying cyanobacteria as a major predictor of microbial biomass and activity, this work reveals a spatially-explicit pathway connecting cyanobacterial primary production to oxygen demand, suggesting that managing blooms may regulate oxygen depletion.

Eutrophication-driven hypoxia and harmful algal blooms are an expanding threat to water quality in estuaries. Engineered aeration is a technology used in freshwater and, to a lesser extent, estuarine systems to mitigate both hypoxia and algal blooms. However, the efficacy of engineered aeration has not been well studied within estuarine ecosystems and very little is known about the impact of aeration on microbial communities in either estuarine or freshwater environments. Here we present a time series investigation of microbial community response to aeration and cessation of aeration in a eutrophic estuary. Samples for 16S rRNA gene analysis were collected over about a month-long period during which time the aerators transitioned from being "on" to "off" to "on" again. Cessation of aeration selected for the dominance of a eukaryotic algae similar to Heterosigma akashiwo. After the resumption of aeration, H. akashiwo dominance decreased rapidly. Cessation of aeration also shifted the structure of the entire microbial community, where diversity decreased and the structure of microbial communities at the surface diverged from those from the bottom of the water column. These changes did not occur at non-aerated control sites. Distinct groups of taxa responded to the disruption in a successional pattern through time, with most taxa never returning to their pre-aeration-cessation abundance during the observational period. These findings demonstrate the complex community response to anthropogenic interventions and provide support for bloom suppression through aeration.

Epipelic diatoms continuously adjust their position within sediments, yet how individual motility contributes to the spatial organization and temporal dynamics of collective aggregation and how this behaviour responds to environmental conditions remain poorly understood. We resuspended a natural assemblage dominated by Pleurosigma strigosum and Gyrosigma balticum in filtered seawater and monitored aggregation dynamics over 72 h under a dark control condition or under 24 h exposure to a nominal initial H2O2 concentration of 400 umol L-1, followed by a 48 h post-exposure period. Time-lapse imaging and quantitative image analysis revealed rapid aggregation and continuous remodeling into dynamic, spatially complex multicellular networks. In the control, aggregate number declined from 11,767 to 3,237 and surface coverage from 24.4% to 10.3%, with pronounced temporal fluctuations. Under H2O2, aggregation followed a distinct, less variable trajectory, with fewer aggregates and persistent differences following the cessation of H2O2 exposure. These observations suggest that dynamic aggregation behaviour may contribute to biofilm organization and resilience, while not distinguishing active regulation from emergent cell-cell-matrix interactions.

The decline in fishery yields in Japan's enclosed coastal seas has been accompanied by a reduction in phytoplankton biomass, suggesting a widespread decrease in ecosystem productivity. Oligotrophication in Mikawa Bay has caused substantial declines in phytoplankton biomass and Manila clam (Ruditapes philippinarum) production. To assess whether external nutrient enhancement could stimulate phytoplankton growth, a controlled demonstration experiment using treated effluent from two sewage treatment plants (WWTPs) was conducted (spanning fiscal years 2022 to 2024) based on analysis using a three-dimensional non-hydrostatic model. Although effluent DIP and nitrogen concentrations were increased, model results showed that WWTP-derived nutrients represent only a minor portion of the total nutrient budget. Field observations revealed limited increases in surface water phosphorus, strong seasonal variability, and only temporary rises in chlorophyll-a and clam harvests. Monthly TP data demonstrated that seasonal DIP pulses, especially spring phosphorus bursts, dominate nutrient dynamics and overshadow external loading effects. Laboratory experiments further showed that phosphate is efficiently fixed by Fe(III) under oxidizing conditions and rapidly released during reductive dissolution of [FeOOH-HPO4]2- complexes, confirming iron as the principal regulator of internal P cycling. Because current numerical models omit iron-driven internal cycling, they cannot accurately predict bioavailable P or ecosystem responses. Overall, the study indicates that localized nutrient enhancement is insufficient to counter long-term oligotrophication, and effective management must integrate nitrogen limitation, internal Fe and P cycling, oceanic exchange, and seasonal variability in Ise and Mikawa Bays.

Accelerated retreat of the Greenland Ice Sheets is increasing freshwater discharge to coastal fjords and promoting transitions from marine-terminating glacier (MTG) regimes to land-terminating (LTG) ones. These changes strongly affect the physical and chemical features of the water column, which in turn impact the structure and functioning of fjord ecosystems. We used high-throughput imaging and DNA metabarcoding approaches to investigate seasonal (spring vs summer) differences in the structure of pelagic microbial communities in two contrasting fjord systems (MTG vs LTG) in southwest Greenland, with focus on the bacterial and heterotrophic protist components, which to date remain understudied in Greenland fjords. Our analyses revealed a marked seasonal restructuring in the microbial communities, especially in the surface layers. In spring, heterotrophic community composition in both fjords manifested a strong link with the diatom spring bloom, being dominated by typical phytoplankton-associated and copiotroph bacterial groups that can utilize algal-derived organic matter, and protists grazing on phytoplankton. In summer, heterotroph communities strongly diverged between the two fjords, most likely caused by the differential impact of MTG vs LTG glaciers on water column structure and chemistry. There was a marked increase in pico- and nano-sized heterotrophs, parasitic protists (dinoflagellate Syndiniales), and bacterial groups indicative of low-nutrient environments. In addition, bacterial, phytoplankton and heterotrophic protist communities become more strongly coupled, either through stronger interactions and/or stronger environmental filtering acting on all groups simultaneously. These observations are indicative of a shift from resource-replete systems in spring to more resourced-depleted systems in summer. However, this shift was less pronounced in the MTG fjord, where subglacial upwelling enabled the persistence of diatom bloom related communities into summer. Finally, we uncovered the presence of a unique, ice melange associated inner fjord microbial community, which shows similarities with both supraglacial and sea-ice associated communities, in the inner part of the MTG impacted fjord.

Nitrogen source and availability can modulate thermal stress responses in marine macroalgae, yet the transcriptional mechanisms underpinning these effects in green seaweeds remain poorly understood. We tested how three N sources (ammonium, nitrate, urea) at low (5 M) and high (100 M) concentrations influence the thermal physiology and gene expression of Codium cylindricum. Thermal performance curves were constructed for growth, photosynthesis, and pigment content across a 5-29 {degrees}C gradient, coupled with transcriptomic analysis at three key temperatures. At high concentrations, ammonium reduced maximum growth rate by 25% and lowered the thermal optimum relative to nitrate and urea, while nitrate supported the broadest thermal performance. Urea constrained thermal breadth regardless of concentration. These responses were linked to differential expression of Nitrogen assimilation genes. Ammonium suppressed nitrate transporter genes (NRT) and nitrite transporter (FNT), and drove pigment accumulation with rising temperature despite reduced growth, suggesting resource reallocation from growth to photoprotection. In contrast, nitrate upregulated photosystem and phosphorylation-related genes. Our findings demonstrate that Nitrogen source and concentration jointly determine the thermal threshold of C. cylindricum, with high ammonium reducing both maximum growth and the temperature at which it is achieved. This highlights how shifting coastal nutrient regimes may alter macroalgal resilience under ocean warming.

Dark waters harbour two-thirds of the ocean's bacterial and archaeal cells, yet the energy sources sustaining microbial life at these depths remain poorly understood. Here we integrate hydrographic profiles with metagenomic analyses and ex situ activity measurements to investigate whether carbon monoxide (CO) and molecular hydrogen (H2) are viable energy sources for epipelagic and mesopelagic microbial populations in the Mariana Trench region. Both gases were detected from 5 to 9,371 m, with concentrations generally higher in the photic zone but anomalously high in several deeper waters. Metagenomic analyses indicate a shift from phototrophic towards lithotrophic energy acquisition with depth. Microbial populations encoding CO dehydrogenases increased from 6.1% at 5 m to 45% at 1,000 m, while those encoding uptake hydrogenases were much less abundant, but increased from 0.34% to 0.63%. Ex situ incubations revealed that in situ cell-specific CO oxidation rates declined with depth, whereas corresponding H2 oxidation rates were significantly higher at 1,000 m than at the surface. At 1,000 m, cell-specific H2 oxidation rates were approximately 4,500-fold higher than those of CO. These contrasting trends suggest that CO oxidation is a widespread auxiliary energy-acquisition strategy, whereas H2 oxidation may sustain hydrogenotrophic growth in dark waters. Together, our results suggest H2 and CO are readily available to pelagic microbial populations and are biologically oxidised in the dark zone, supporting microbial energy acquisition and oceanic biogeochemical cycling.

Tidal flats cover less than 1% of the surface of our planet, but they provide important ecosystem functions and services, like carbon sequestration and nutrient (re-)mineralization, primary, sec-ondary, and food production, and habitats for a variety of species. Despite their importance, they are threatened by environmental stressors and anthropogenic impacts. Hence, a better under-standing of the interaction between macrozoobenthos, their metabolic activity, and their contri-bution to carbon and nitrogen cycling is important. Therefore, we conducted in-situ pulse-chase tracer experiments at a Pacific oyster (Magallana gigas) reef in the Eastern Scheldt (Southwest Dutch Delta, Netherlands) in summer and autumn 2020. During these experiments, we provided the submerged benthic community with 13C and 15N-enriched bacterioplankton and incubated it in seawater enriched in 1% deuterium oxide (2H2O) for one tidal cycle (~9 h), before the benthic community was kept at in situ conditions for another 14 d. Our aim was (1) to assess seasonal variations in 13C and 15N processing by macrozoobenthos, (2) to evaluate potential life-stage de-pendent differences in 2H uptake - a proxy for metabolic activity, and (3) to identify the macro-zoobenthos taxon which had the highest metabolic turnover rate (MTR). In summer, most bacte-rioplankton-derived 13C- and 15N was taken up by sponges (Halichondria panicea), limpets (Crepidula fornicata), and clams (Ruditapes philippinarum), whereas in autumn, H. panicea, C. fornicata and the sponge Hymeniacidon perlevis dominated 13C and 15N incorporation. Statisti-cally significant differences in 2H uptake between life stages (juvenile/ small vs. adult) was de-tected in Malacostraca (i.e., Rhithropanopeus harrisii), but not in Polychaeta or Bivalvia. There-fore, this difference between taxonomic classes might be linked to mold-intermolt periods. Sea-sonal differences in MTR of H. panicea and M. gigas (i.e., the species with the highest MTRs in summer and autumn) might be linked to seasonal environmental variability, such as temperature and food availability.

Marine microbial communities vary seasonally and spatially, shaped by physiochemical gradients and biotic interactions. Spatiotemporal variability of seawater microbiomes in tropical coastal regions is comparatively understudied, especially in Southeast Asia with high pressures from development and anthropogenic activities. Here, we examined the microspatial and temporal variability of bacterioplankton in the Singapore Strait, which is a tropical system in Southeast Asia influenced by monsoons. By applying total community amplicon sequencing to three particle size fractions reflecting microspatial habitats of seawater (0.22-1 {micro}m ''free-living'', 1-10 {micro}m ''large cells and small aggregates'' and 10-150 {micro}m ''particle-associated''), we show that the seawater microbial community was structured by their microspatial habitats, monsoon seasons and physiochemical variables. Monsoon-driven alternation of water masses originating from the South China Sea to the East and from off the Sumatran coast to the West resulted in a distinct community during the Southwest monsoon across all three size fractions. Total DNA (biomass) was lowest in the 10-150 {micro}m fraction, but these particle-associated sequences had the highest diversity and were surprisingly enriched with picocyanobacterial and some pathogenic taxa, potentially reflecting aggregate formation and/or host-derived particle association. This fraction also exhibited greater temporal variability than the two smaller fractions, which could be related to a more heterogenous environment in particle microhabitats. Overall, this study demonstrated compositional variability in the bacterioplankton across space and time in an equatorial region influenced by monsoons.

A diverse array of photosynthetic phytoplankton drives primary production in equatorial surface waters. Among these, the cyanobacterium Prochlorococcus is an important contributor to net primary production in these typically iron-limited, high-nutrient and low-chlorophyll (HNLC) regions. Here, we explore the diversity of these organisms, in part, through targeted enrichment of Prochlorococcus cells using field-based high-speed cell sorting techniques. We demonstrate that the genomes of Prochlorococcus belonging to the low-light adapted LLI clade, and isolated from the surface of the Equatorial Pacific Ocean, are depleted in functions related to the assimilation of urea, nitrite, and amino acids. These are the first examples of LLI Prochlorococcus that have lost the ability to use nitrite, a trait considered to be a core feature of this clade. All new equatorial cultures of LLI Prochlorococcus appear to use a distinct isoform of protoporphyrinogen IX oxidase (HemG), for the biosynthesis of a chlorophyll precursor, that does not require the use of iron-containing heme. In contrast, the heme-dependent HemJ isoform is typically used by Prochlorococcus found outside equatorial HNLC waters. Together, these findings suggest that low-light adapted Prochlorococcus in the equatorial ocean possess accessory gene content that reflects adaptation to the generally iron-limited but nitrogen-replete conditions of surface waters.

The Deep Chlorophyll Maximum (DCM) is likely the most important feature organizing the marine epipelagic environment. Within this layer, opposing gradients of light and nutrients create a stratified habitat that supports high phytoplankton biomass and a substantial fraction of oceanic primary production. Despite its ecological importance, most studies treat the DCM as a single depth, overlooking its fine-scale heterogeneity. Here we investigated prokaryotic community organization across the DCM in the northwestern Mediterranean Sea through high-resolution sampling of four profiles collected over two days. Free-living (0.2-3 {micro}m) and particle-associated (3-20 {micro}m) communities were characterized using 16S rRNA gene amplicon sequencing. Prokaryotic communities changed progressively along the vertical gradient, revealing the DCM as a microbial coenocline with continuous community turnover. Fuzzy clustering identified distinct assemblages associated with environmental transitions from warm surface waters to the chlorophyll maximum, the nitrite peak below the DCM, and deeper nitrate-rich layers. In both the free-living and particle-associated fractions, most ASVs remained consistently associated with the same depth-defined clusters across all samplings, indicating stable niche partitioning over short timescales. However, these temporally stable ASVs accounted for a substantially smaller fraction of community sequences in particle-associated communities, suggesting higher dynamism, likely driven by particle-mediated transport. Nevertheless, phylogenetic analyses revealed that closely related ASVs tended to occupy similar depth niches, indicating that habitat preferences are phylogenetically conserved in both size fractions. Our results demonstrate prokaryotic niche partitioning over scales of only a few meters within the DCM, highlighting the importance of fine-scale sampling for understanding microbial community structure and responses to ocean change.

The cyanobacterium Trichodesmium is important in ocean nitrogen (N) and carbon (C) biogeochemistry through fixation of N2 gas and CO2 into NH3, amino acids, and carbohydrates. These essential compounds then fuel primary productivity, bacterial and grazing communities, and upper trophic levels. In the oligotrophic surface oceans, they are one of few taxa capable of utilizing both atmospheric C and N. Trichodesmium fall into 2 diazotrophic phylogenomic clades named "Thieb" and "Tery" after the most well characterized botanical species, Trichodesmium thiebautii and Trichodesmium erythraeum. Thieb is commonly the most abundant clade in all major ocean regions and paradoxically, is also the least characterized in terms of morphology, genomics, and ecophysiology due to underrepresentation in culture collections. In this study, 25 novel strains of Thieb were enriched in culture from the Sargasso Sea, phenotypically characterized, and whole genome sequenced. Cultures were found to belong to four well-supported subclades (i.e., ThiebA, ThiebB, ThiebC, and ThiebD). Trichodesmium subclades were found to have environmentally relevant differences in colony shape, gene content, cell dimensions, and inferred temperature range. Specifically, ThiebD and ThiebC had the largest biovolumes whereas ThiebA and ThiebB had the smallest. Importantly ThiebB also became relatively more abundant only in bulk seawater metagenomes collected at high temperature (>28{degrees}C). This finding indicates that as ocean warming continues, there may be shifts in Trichodesmium community structure towards smaller cells, which would affect overall C+N standing stocks.

Mesophotic coral ecosystems are commonly interpreted as thin biological veneers over relict shallow-water reef structures, but their capacity to generate late Holocene carbonate deposits remains poorly quantified. Here we combine diver excavations, rubble-bed thickness surveys, radiocarbon age-depth modelling, sediment grain-size analyses, coral-rubble assemblages, trace-element geochemistry, and modern Alveopora allingi growth measurements from two 40-65 m deep coral-rubble fields in the northern Gulf of Eilat/Aqaba, Red Sea. Rubble deposits are at least 1.0-1.5 m thick and accumulated at mean rates of 2.21 {+/-} 0.52 mm yr-1 at the Dekel site and 1.33 {+/-} 0.13 mm yr-1 at the IUI site, implying persistent carbonate accumulation over centuries to >1 kyr. Age-depth models indicate quasi-continuous deposition despite pronounced faunal changes, including a shift from A. allingi-dominated rubble to upper layers enriched in Euphyllia paradivisa at Dekel. The dominant modern rubble-forming coral, A. allingi, extends at 3.04 {+/-} 0.87 mm yr-1 and has skeletal density of 1.17 {+/-} 0.27 g cm-3. First-order cover-based accretion estimates at present coral cover fall well below the radiocarbon-derived rates, indicating that long-term mesophotic rubble accumulation integrates historical cover, secondary calcification and sediment retention rather than present live coral cover alone. These data demonstrate that mesophotic rubble fields can act as active carbonate factories and palaeoecological archives, challenging the assumption that modern mesophotic habitats are geomorphologically passive.