RESUMO
Vanishing of white matter (VWM) is a hereditary heterogeneous brain disorder that most often affects children. However, the onset of the disease varies from childhood to adulthood. VWM is caused by mutations in one of the five genes encoding subunits of the eukaryotic initiation factor eIF2B. In the current study, we aimed to determine the genetic cause of VWM in a large consanguineous Iranian family with three affected members. Next-generation sequencing was conducted on the proband to determine the underlying cause of VWM. The identified variant was validated by PCR-Sanger sequencing in the patient and was also segregated in his parents and two other affected members of the pedigree. The potential functional effects of this mutation within EIF2B5 were predicted by in silico analysis. We have also reviewed all EIF2B5 disease-causing variants and available clinical features of each patient reported in HGMD Professional 2022.2. A novel homozygous variant c.746T>G [p.Ile249Ser] was detected in EIF2B5 which was co-segregated with the disease in all affected family members in an autosomal recessive manner. All employed in silico prediction tools and 3D structure analysis for the novel mutation also supported the pathogenicity of this variant. Our study not only expanded the spectrum of the pathogenic variants in EIF2B5 but also presented a literature review on EIF2B5-related conditions that provide a comprehensive picture of the genetic nature of this gene and phenotypic variability in patients.
Assuntos
Leucoencefalopatias , Criança , Humanos , Adolescente , Adulto Jovem , Irã (Geográfico) , Consanguinidade , Leucoencefalopatias/genética , Mutação de Sentido Incorreto , Mutação , Fator de Iniciação 2B em Eucariotos/genéticaRESUMO
Contributions of fungal and oomycete communities to freshwater carbon cycling have received increasing attention in the past years. It has been shown that fungi and oomycetes constitute key players in the organic matter cycling of freshwater ecosystems. Therefore, studying their interactions with dissolved organic matter is crucial for understanding the aquatic carbon cycle. Therefore, we studied the consumption rates of various carbon sources using 17 fungal and 8 oomycete strains recovered from various freshwater ecosystems using EcoPlate™ and FF MicroPlate™ approaches. Furthermore, phylogenetic relationships between strains were determined via single and multigene phylogenetic analyses of the internal transcribed spacer regions. Our results indicated that the studied fungal and oomycete strains could be distinguished based on their carbon utilization patterns, as indicated by their phylogenetic distance. Thereby, some carbon sources had a higher discriminative strength to categorize the studied strains and thus were applied in a polyphasic approach. We concluded that studying the catabolic potential enables a better understanding of taxonomic relationships and ecological roles of fungal vs. oomycete strains.
RESUMO
Permafrost, a vast storage reservoir of frozen organic matter, is rapidly thawing due to climate change, releasing previously preserved carbon into the environment. This phenomenon has significant consequences for microbial communities, including fungi, inhabiting permafrost-associated regions. In this review, we delve into the intricate interplay between permafrost thawing and fungal diversity and functionality with an emphasis on thermokarst lakes. We explore how the release of organic carbon from thawing permafrost alters the composition and activities of fungal communities, emphasizing the potential for shifts in taxonomic diversity and functional gene expression. We discuss the formation of thermokarst lakes, as an example of permafrost thaw-induced ecological disruptions and their impact on fungal communities. Furthermore, we analyze the repercussions of these changes, including effects on nutrient cycling, plant productivity, and greenhouse gas (GHG) emissions. By elucidating the multifaceted relationship between permafrost thaw and aquatic fungi, this review provides valuable insights into the ecological consequences of ongoing climate change in permafrost-affected regions.