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Disposed plastics in oceans provide a substrate to which microbes can adhere and structure the biofilm, namely the plastisphere. In this study, we showed that the mesoplastic density-based separation, routinely used in quantification assays, is detrimental to studying the microbiome diversity and ecology as it underestimates the real microbial diversity within these samples. Based on SEM and microbiome observations, we propose that chemically fixing samples before density separation preserves cellular diversity (2.32-fold change) and richness (1.12-fold change) that would be naturally lost due to the current methodology. OTUs assigned to Gram-negative bacterial species are the most negatively affected by omitting fixation and polymer composition was not decisive in shifting microbiome composition. Considering our findings, the formaldehyde-fixation step should be incorporated into the current methodology described in most studies as this is crucial to promote a deeper understanding of the microbial community in this ecosystem and biofilm-adhered scattering through aquatic ecosystems. • Formaldehyde prefixation before conserves alpha-diversity of mesoplastic community. • Formaldehyde prefixation before conserves beta-diversity of mesoplastic community. • Gram-negative representatives are naturally lost in saline-float method. • Microscopy and metagenomics data corroborate the use of Formaldehyde prefixation. [ABSTRACT FROM AUTHOR]

Anaerobic digestion has been widely applied for waste treatment, renewable energy generation and biofertilizer production. The biogas potential in Brazil is sizable, but the state of Rio de Janeiro is largely dependent on fossil fuels, and there is a lack of biogas potential assessments in the state. Thus, this study evaluated biomethane, electricity and biofertilizer potentials in the region. Three different scenarios of biomass supply were considered for four major biowaste streams: sewage sludge; cattle manure; sugarcane processing waste; and food waste. Biomethane generation from the assessed sources could reach 0.6–1.3 billion Nm3 year−1, corresponding to 1,768–3,961 GWh year−1 of electricity and 1.6–3.3 million Mg year−1 of biofertilizer. Cattle manure was responsible for 73–84% of the projected biomethane production, presenting an opportunity to reduce the significant emissions from livestock farming. The estimated biofertilizer production could meet the demands of the state, and the produced electricity could offset up to 10% of the demand. The gas grid could facilitate the distribution of upgraded biomethane, and 10–22% of the natural gas demand could be met. The findings of this work highlight the high potential for biogas generation in Rio de Janeiro, which is up to seven times larger than the current production. [ABSTRACT FROM AUTHOR]

Carbonates of the Salitre Formation, Irecê Basin, Brazil, have been the focus of extensive stratigraphic and structural studies for several decades. Besides hosting phosphorites deposits, these rocks are analogues to fractured and certified oil reservoirs, such as those of the Cretaceous pre-salt oil system offshore Brazil. The present study presents an integration of X-Ray Diffraction (XRD), Quantitative Evaluation of Minerals by Scanning Electron Microscopy (QEMScan), Optical Petrography, Cathodoluminescence (CL), and Charge Contrast Imaging (CCI) data that allows a high-resolution characterization of the mineralogy within the carbonate units. In addition, we also present carbon and oxygen stable isotope data to identify possible origins of the associated fluids. The mineral characterization revealed that calcite (50–70%), quartz (20–30%) and dolomite (10–20%) are the main post-sedimentary mineral phases found in veins, vesicle structures and cement of the carbonate units. The mineral phases of veins were formed by the interaction with hydrothermal fluids, which had an important role in the dissolution, karstification, and remobilization of carbonate units. Isotopic analysis shows that δ13C and δ18O are more negative in veins and vesicles when compared to host rock, indicating that there is no effective isotopic exchange between the host rock and the filled structures and that these structures were filled with hydrothermal fluids from an external source. • Hydrothermal processes in carbonate sequences lead to hypogenic carstification. • The carbonate sequences of the Salitre Formation have structures filled with calcite, dolomite and quartz. • Isotopes of carbon and oxygen show that the veins and vesicles have a different signature than the embedding rock. • Fractures and faciological characteristics of carbonate sequences control the pervasive nature of hydrothermal fluids. • Mineralogical characterization shows dolomitization and dolomitic cementation processes. [ABSTRACT FROM AUTHOR]