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Sisma-Ventura, G.

Publications and source records attributed to Sisma-Ventura, G..

4 recordsLinked to original sources

Heterotrophic diazotrophy along a river to lake continuum: lifestyle and contribution to N2 fixation

Heterotrophic diazotrophs are potentially important agents in freshwater ecosystems, yet they remain poorly understood. This study elucidates the contribution of freshwater heterotrophic diazotrophs as free-living or aggregate-associated cells to total N2 fixation along the continuum from the Jordan River to Lake Kinneret, Israel. Heterotrophic diazotrophs accounted for 25%-56% of the total diazotrophs and commonly found as free-living cells or attached to aggregates in the river. N2 fixation by heterotrophic diazotrophs associated with aggregates varied along the river, while accounting for ~50% of N2 fixation in the lake. Non-cyanobacterial diazotrophs dominated the free-living fraction in the river, and cyanobacteria were mostly identified in the lake. The diversity of free-living diazotrophs was sensitive to environmental changes, as the aggregates have likely provided a protected micro-environment. The results reveal the dynamic lifestyle of heterotrophic diazotrophs along a river-lake continuum and highlight their contribution to total N2 fixation and primary production. TeaserFreshwater heterotrophic diazotrophs are more ubiquitous than previously thought, can be found as free-living cells or associated with aggregates, and significantly contribute to primary production.

microbiology↗

Active microbial communities facilitate carbon turnover in brine pools found in the deep Southeastern Mediterranean Sea

Discharge of gas-rich brines fuels productive chemosynthetic ecosystems in the deep sea. In these salty, methanic and sulfidic brines, microbial communities adapt to specific niches along the physicochemical gradients. However, the molecular mechanisms that underpin these adaptations are not fully known. Using metagenomics, we investigated the dense ([~]106 cell ml-1) microbial communities that occupy small deep-sea brine pools found in the Southeastern Mediterranean Sea (1150 m water depth, [~]22{degrees}C, [~]60 PSU salinity, sulfide, methane, ammonia reaching millimolar levels, and oxygen usually depleted), reaching high productivity rates of 685 {micro}g C L-1 d-1 ex-situ. We curated 266 metagenome-assembled genomes of bacteria and archaea from the several pools and adjacent sediment-water interface, highlighting the dominance of a single Sulfurimonas, which likely fuels its autotrophy using sulfide oxidation or inorganic sulfur disproportionation. This lineage may be dominant in its niche due to genome streamlining, limiting its metabolic repertoire, particularly by using a single variant of sulfide: quinone oxidoreductase. These primary producers co-exist with ANME-2c archaea that catalyze the anaerobic oxidation of methane. Other lineages can degrade the necromass aerobically (Halomonas and Alcanivorax), or anaerobically through fermentation of macromolecules (e.g., Caldatribacteriota, Bipolaricaulia, Chloroflexota, etc). These low-abundance organisms likely support the autotrophs, providing energy-rich H2, and vital organics such as vitamin B12.

microbiology↗

Trophic ecology of deep-sea megafauna in the ultra-oligotrophic Southeastern Mediterranean Sea

The trophic ecology of fourteen species of bathybenthic and bathypelagic fishes and six species of bathybenthic decapod crustaceans from the continental slope and rise of the Southeastern Mediterranean Sea (SEMS) was examined using stable isotope analysis. Mean {delta}13C values among fish species varied by more than 4.0{per thousand}, from -20.85{per thousand} (Macroramphosus scolopax) to -16.57{per thousand} (Conger conger and Centrophorus granulosus), and increased as a function of depth (200 - 1400 m). Mean {delta}13C values of the crustaceans showed smaller variation, between -16.38{per thousand} (Polycheles typhlops) and -18.50{per thousand} (Aristeus antennatus). This suggests a shift from pelagic to regenerated benthic carbon sources with depth. Benthic carbon regeneration is further supported by the low benthic-pelagic POM-{delta}13C values, averaging -24.7 {+/-} 1.2{per thousand}, and the mixing model results, presenting very low contribution of epipelagic POM to the bathyal fauna. Mean {delta}15N values of fish and crustacean species ranged 7.91 {+/-} 0.36{per thousand} to 11.36 {+/-} 0.39{per thousand} and 6.15 {+/-} 0.31{per thousand} to 7.69 {+/-} 0.37{per thousand}, respectively, resulting in trophic position estimates, occupying the third and the fourth trophic levels. Thus, despite the proximity to the more productive areas of the shallow shelf, low number of trophic levels (TL~1.0) and narrow isotopic niche breadths (SEAc <1) were observed for bathybenthic crustaceans (TL = 3.62 {+/-} 0.22) and bathypelagic fishes (TL = 4.33 {+/-} 0.34) in the study area - probably due to the ultra-oligotrophic state of the SEMS resulting in limited carbon sources. Our results, which provide the first trophic description of deep-sea megafauna in the SEMS, offer insight into the carbon sources and food web structure of deep-sea ecosystems in oligotrophic marginal seas, and can be further used in ecological modeling and support the sustainable management of marine resources in the deep Levantine Sea.

ecology↗

Diversity, activity and abundance of benthic microbes in the southeastern Mediterranean Sea: A baseline for monitoring

Microbes are key players in marine sediments, yet they are not accessed routinely by monitoring programs. Here, we investigate the spatial and vertical trends in the abundance, activity and diversity of benthic archaea, bacteria and fungi of the southeastern Mediterranean Sea (SEMS), based on [~]150 samples collected by the National Monitoring Program in 2018-2020 in coastal, as well as deep-sea transects across the Israeli exclusive economic zone, using vertical profiles of short sediment cores (0-1, 1-2, 4-5, 9-10 and 19-20 cm below surface). Microbial abundance was usually low (0.01 x108 to 0.21x108 cells gr-1 sediment), while heterotrophic productivity was the highest in the nearshore stations (12{+/-}4 ng C gr-1 sediment h-1), as opposed to 0.5{+/-}0.9 ng C gr-1 sediment h-1 at the offshore sites. Using amplicon sequencing of marker genes, we identified the changes in the diversity of microbes along environmental gradients, in the four dimensions (geographic location, seabed depth, distance from the sediment surface and time). We show high taxonomic diversity of bacteria and archaea (Shannons H 5.0-6.9) and lesser diversity of fungi (Shannons H 0.2-4.8). We use DESeq2 analyses to highlight the role of ammonia-oxidizing Nitrososphaeria in the aerated sediments of the continental slope and deep bathyal plain stations and organotrophic lineages in coastal, shelf, slope, and abyssal plain sediments. Based on taxonomic diversity, we infer the metabolic potential of these communities. Analyses of fungi diversity and guilds suggest the prevalence of the saprotrophic and pathotrophic microfungi Ascomycota (70{+/-}23%) and Basidiomycota (16{+/-}18%) in the SEMS sediments. We provide a comprehensive baseline of benthic microbial populations in the SEMS and pledge for the use of microbial indices in biomonitoring of the marine environment.

microbiology↗