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Rubio-Portillo, E.

Publications and source records attributed to Rubio-Portillo, E..

4 recordsLinked to original sources

Metagenomic insights into microbial mediation of Caulerpa prolifera invasion in a coastal lagoon

Opportunistic seaweeds of the genus Caulerpa have benefited from human-driven environmental change to expand within coastal lagoons, frequently displacing native seagrasses. In the Mar Menor lagoon (southeastern Spain), Caulerpa prolifera has progressively expanded since the 1970s, coinciding with the decline of the native seagrass Cymodocea nodosa. Sediments colonized by Ca. prolifera are characterized by elevated sulfide concentrations, which are toxic to seagrasses. Because sulfide is microbially produced, these sediment communities likely shape the competition between Ca. prolifera and Cy. nodosa. However, their metabolic potential and activity remain poorly understood. Here, we examined the taxonomic composition and functional capabilities of sediment microbial communities using 12 paired metagenomes and metatranscriptomes from areas dominated by either Ca. prolifera or Cy. nodosa. Caulerpa-associated sediments displayed a higher potential for organic matter degradation and sulfate reduction. Several metagenome-assembled genomes (MAGs) encoded enzymes putatively involved in the degradation of pectin-like polysaccharides characteristic of the Caulerpa cell wall. Comparison of metagenomic and metatranscriptomic data further revealed that the most abundant MAGs were not necessarily the most transcriptionally active. This finding challenges the common assumption that ecological importance is primarily determined by abundance and highlights the potential contribution of less abundant microorganisms to biogeochemical cycling. Further, 97 of the 100 most highly expressed genes lacked functional annotation. Recombinant production and functional characterization of the protein encoded by the most highly expressed gene in the analyzed sediments revealed that it is an enzyme able to breakdown endogenous bacterial peptidoglycan. Collectively, these results underscore the importance of integrating metagenomics and metatranscriptomics with experimental validation to achieve a more comprehensive understanding of microbial functional capabilities, an integration that is still uncommon in the microbial ecology field.

microbiology↗

Biological context modulates virus-host dynamics and diversification

Virus-host interactions are fundamental to microbial ecology and evolution, yet they are often studied in simplified systems. To assess the impact of biological complexity, we examined the halophilic bacterium Salinibacter ruber strain M1 and the EM1 virus, a bacteriophage that infects M1, in the presence of additional strains and viruses. In the short term, the presence of a biotic background delayed population-level lysis and reduced EM1 production. In the long term, both M1 and EM1 persisted across all conditions, but their evolutionary trajectories diverged. The virus accumulated many mutations, showed reduced infectivity against its native host, and expanded its host range in the presence of other viruses, highlighting a role of virus-virus interactions in promoting diversification. In contrast, the host accumulated more mutations when evolving with other bacterial strains. Taken together, these findings demonstrate that biological complexity shapes both the ecological dynamics and evolutionary trajectories of virus-host interactions.

microbiology↗

Shifts in marine invertebrate bacterial assemblages associated with tissue necrosis during a heatwave

Marine heatwaves (MHWs) are periods of extremely high seawater temperature that affect marine ecosystems in several ways. Anthozoans (corals and gorgonians) and Porifera (sponges) are usually among the taxa most affected by MHWs. Both are holobiont entities that form complex interactions with a wide range of microbes, which are an essential part of these organisms and play key roles in their health status. Here, we determine microbial community changes suffered in two corals (Cladocora caespitosa and Oculina patagonica), one gorgonian (Leptogorgia sarmentosa), and one sponge (Sarcotragus fasciculatus) during the 2015 MHW. The microbial communities were different among hosts and displayed shifts related to host health status, with a higher abundance in necrosed tissues of Ruegeria species or of potential pathogens like Vibrio. We also carry out a meta-analysis using 93 publicly accessible 16S rRNA gene libraries from O. patagonica, C. caespitosa and L. sarmentosa to establish a Mediterranean core microbiome in these species. We have identified one Ruegeria OTU that maintained a stable and consistent association with these species, which was also related with tissue necrosis in their hosts. Therefore, Ruegeria sp. could play an important and still underexplored role in the health status of its hosts.

microbiology↗

Biophysical and physiological causes of coral reef microbialization

Coral reefs are declining globally as their primary producer communities shift from stony coral to fleshy macroalgae dominance. Previously, we have shown that the rise of fleshy macroalgae produces dissolved organic carbon (DOC) that lead to microbialization and coral death. Here we test the hypothesis that the biophysical cause of bacterial biomass accumulation is a relative decrease in electron acceptors relative to electron donors due to O2 loss from macroalgae. We show that 37 % of photosynthetic O2 produced by reef fleshy macroalgae is lost in the form of gas through ebullition from algae surfaces. O2 loss increases DOC:O2 ratios, decoupling the photosynthetically fixed carbon from oxidative potential for respiration. This biogeochemical environment drives heterotrophic microbes to increase cell-specific DOC consumption and cell sizes, accumulating biomass. In contrast, corals do not lose oxygen and support the growth of smaller and fewer bacteria. In situ biomass and metagenomic analyses of 87 reefs across the Pacific and Caribbean show that on algae-dominated reefs bacteria accumulate organic carbon through a Warburg-like increase in aerobic glycolytic metabolism. Because of its biophysical basis, microbialization is predicted to occur in other marine ecosystems shifting primary producer assemblages, such as planktonic communities in warming and acidifying conditions.

ecology↗