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Moldovan, O. T.

Publications and source records attributed to Moldovan, O. T..

2 recordsLinked to original sources

Community-level physiological profiling of carbon substrate metabolization by microbial communities associated to sediments and water in karstic caves from Romania

Cave ecosystems comprise specialized microbial communities that play essential roles in biogeochemical cycles; yet their metabolic capabilities and ecological functions are not yet fully understood. As conventional cultivation techniques offer limited insights into the metabolic capabilities, methods based on direct functionality screening could provide more in-depth knowledge of cave microbial activity. In this study, we utilized the Community-Level Physiological Profiling (CLPP) based on Biolog(R) EcoPlate approach to assessing carbon substrate utilization by microbial communities associated with pool water, sediment, sediment (limon), and moonmilk from five caves in Romania. Principal Component Analysis (PCA) and Generalized Additive Models (GAMs) statistics were employed to infer the patterns of C-substrate metabolization and their environmental drivers. Environmental variables such as sodium (Na) and electrical conductivity (EC) significantly impacted C-utilization capabilities as indicated by both PCA and GAM. The latter analysis elucidated non-linear relationships between variables, such as EC, Na, and Mg, and microbial metabolic diversity indices. However, distinct C utilization patterns were detected among sampled sites and chemical types. Unlike moonmilk samples whose associated microbial communities appeared as exhibiting low C-substrate utilization, the highest activity was shown in cave pool water samples with the associated microbial communities extensively consuming D-galacturonic acid and Tween 80. Conversely, substrates like L-threonine and -ketobutyric acid showed limited utilization across all cave samples. Average Well Color Development (AWCD) and Shannon diversity indices indicated that microbial communities associated to samples from Closani and Muierilor caves demonstrated the highest metabolic diversity. Our findings suggested that metabolic profiling using Biolog(R)EcoPlates method combined with multivariate statistical methods might prove as suitable approach to effectively screen for cave microbial functionality and the probable environmental drivers. Besides, this work distinguishes from similar studies by relying on GAM analysis to predict the environmental factors governing the microbially-mediated organic carbon degradation in subterranean ecosystems.

microbiology↗

Competition-cooperation in the chemoautotrophic ecosystem of Movile Cave - first metagenomic approach on sediments

BackgroundMovile Cave (Dobrogea, SE Romania) hosts a subterranean chemoautotrophically-based ecosystem supported by a sulfidic thermal aquifer analogous to the deep-sea hydrothermal ecosystems. Our current understanding of Movile Cave microbiology has been confined to the thermal water proximity (no more than 2 m distant), with most studies focusing on the water-floating mat, which likely acts as the primary production powerhouse in this sulfidic ecosystem. To gain more insightful information on the functioning of the sulfidic Movile Cave ecosystem, we employed a metagenomics-resolved approach to reveal the microbiome diversity, metabolic potential, and interactions and infer its roles within the food webs in the sediments beyond the sulfidic thermal waters. ResultsA customized bioinformatics pipeline led to the recovery of 106 high-quality metagenome-assembled genomes from 7 cave sediment metagenomes. Assemblies taxonomy spanned 19 bacterial and three archaeal phyla with Acidobacteriota, Chloroflexota, Proteobacteria, Planctomycetota, Ca. Patescibacteria, Thermoproteota, Methylomirabilota, and Ca. Zixibacteria as prevalent phyla. Functional gene analyses allowed prediction of CO2 fixation, methanotrophy, sulfur and ammonia oxidation as possibly occurring in the explored sediments. Species Metabolic Coupling Analysis of metagenome-scale metabolic models revealed the highest competition-cooperation interactions in the sediments collected at the farthest distance from the sulfidic water. As a result of simulated metabolic interactions, autotrophs and methanotrophs were hypothesized as major donors of exchanged metabolites in the sediment communities. Cross-feeding dependencies were assumed only towards currency molecules and inorganic compounds (O2, PO43-, H+, Fe2+, Cu2+) in the sediment nearby sulfidic water, whereas hydrogen sulfide and methanol are predictably traded exclusively among communities dwelling in the distant gallery. ConclusionsThese findings suggest that the primary production potential of the Movile Cave expands way beyond its hydrothermal waters, enhancing our understanding of ecological interactions inside chemolithoautotrophically based subterranean ecosystems and their functioning.

microbiology↗