Please use this identifier to cite or link to this item: https://cir.cenieh.es/handle/20.500.12136/2887
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dc.contributor.authorBogdan, Diana Felicia-
dc.contributor.authorBaricz, Andreea Ionela-
dc.contributor.authorChiciudean, Iulia-
dc.contributor.authorBulzu, Paul Adrian-
dc.contributor.authorCristea, Adorján-
dc.contributor.authorNăstase-Bucur, Ruxandra-
dc.contributor.authorLevei, Erika-
dc.contributor.authorCadar, Oana-
dc.contributor.authorSitar, Cristian-
dc.contributor.authorBanciu, Horia Leonard-
dc.contributor.authorMoldovan, Oana Teodora-
dc.date.accessioned2023-02-15T13:58:21Z-
dc.date.issued2023-02-
dc.identifier.citationFrontiers in Microbiology, 2023, 14, 962452.es_ES
dc.identifier.issn1664-302X-
dc.identifier.urihttps://cir.cenieh.es/handle/20.500.12136/2887-
dc.description.abstractIntroduction: Karst caves are characterized by relatively constant temperature, lack of light, high humidity, and low nutrients availability. The diversity and functionality of the microorganisms dwelling in caves micro-habitats are yet underexplored. Therefore, in-depth investigations of these ecosystems aid in enlarging our understanding of the microbial interactions and microbially driven biogeochemical cycles. Here, we aimed at evaluating the diversity, abundance, distribution, and organic substrate preferences of microbial communities from Peștera cu Apă din Valea Leșului (Leșu Cave) located in the Apuseni Mountains (North-Western Romania). Materials and Methods: To achieve this goal, we employed 16S rRNA gene amplicon sequencing and community-level physiological profiling (CLPP) paralleled by the assessment of environmental parameters of cave sediments and water. Results and Discussion: Pseudomonadota (synonym Proteobacteria) was the most prevalent phylum detected across all samples whereas the abundance detected at order level varied among sites and between water and sediment samples. Despite the general similarity at the phylum-level in Leșu Cave across the sampled area, the results obtained in this study suggest that specific sites drive bacterial community at the order-level, perhaps sustaining the enrichment of unique bacterial populations due to microenvironmental conditions. For most of the dominant orders the distribution pattern showed a positive correlation with C-sources such as putrescine, γ-amino butyric acid, and D-malic acid, while particular cases were positively correlated with polymers (Tween 40, Tween 80 and α-cyclodextrin), carbohydrates (α-D-lactose, i-erythritol, D-mannitol) and most of the carboxylic and ketonic acids. Physicochemical analysis reveals that sediments are geochemically distinct, with increased concentration of Ca, Fe, Al, Mg, Na and K, whereas water showed low nitrate concentration. Our PCA indicated the clustering of different dominant orders with Mg, As, P, Fe, and Cr. This information serves as a starting point for further studies in elucidating the links between the taxonomic and functional diversity of subterranean microbial communities.es_ES
dc.description.sponsorshipThis work was supported by a grant of the Ministry of Research, Innovation and Digitization, CNCS/CCCDI – UEFISCDI, project number 2/2019 (DARKFOOD), within PNCDI III. DFB has received financial support through the project: Entrepreneurship for innovation through doctoral and postdoctoral research, POCU/380/6/13/123886 co-financed by the European Social Fund, through the Operational Program for Human Capital 2014-2020. P-AB was supported by the research grant 20-23718Y (Grant Agency of the Czech Republic).es_ES
dc.language.isoenes_ES
dc.publisherFrontiers Mediaes_ES
dc.rightsinfo:eu-repo/semantics/openAccesses_ES
dc.rightsAttribution 4.0 International (CC BY 4.0)*
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/*
dc.subjectMicrobial communitieses_ES
dc.subjectCave ecosystemses_ES
dc.subjectAmplicon sequencinges_ES
dc.subjectKarst cavees_ES
dc.subjectCommunity-level physiological profileses_ES
dc.titleDiversity, distribution and organic substrates preferences of microbial communities of a low anthropic activity cave in North-Western Romaniaes_ES
dc.typeArticlees_ES
dc.identifier.doi10.3389/fmicb.2023.962452-
dc.relation.publisherversionhttps://doi.org/10.3389/fmicb.2023.962452es_ES
dc.date.available2023-02-15T13:58:21Z-
Appears in Collections:Geocronología y Geología



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