Biology subjects

Carere, C. R.

Publications and source records attributed to Carere, C. R..

3 recordsLinked to original sources

bioRxiv2026

Reysenbachia aerophila gen. nov., sp. nov., a facultatively anaerobic, hydrogen-oxidizing, thermophilic bacterium isolated from Kuirau Park, Rotorua, New Zealand

A facultatively anaerobic, hydrogen-oxidizing, thermophilic bacterium (strain KUI-RBT) was isolated from a geothermal spring biofilm in Rotorua, New Zealand. Strain KUI-RBT is a motile, straight rod, measuring approximately 0.7 {micro}m by 1.0 to 1.5 {micro}m with a diderm cell wall. Growth of KUI-RBT occurred from 39 to 74 {degrees}C (Topt 64.5 {degrees}C), pH 5.0 to 7.5 (pHopt 6.5), and 0 to 1% (w/v) NaCl (NaClopt 0.4-0.7%, w/v). KUI-RBT utilizes carbon dioxide and various organic carbon substrates as carbon sources and hydrogen as an electron donor. KUI-RBT can use oxygen (0-21%, v/v), elemental sulfur, thiosulfate, sulfite, nitrate, arsenate, and selenate as terminal electron acceptors. Major fatty acids of strain KUI-RBT include C20:1, C18:1, and C18:0 and the primary quinone is MTK-7. The whole genome G+C content is 34.23 mol%. Phylogenetic analyses indicate KUI-RBT to be a member of the family Hydrogenothermaceae, with Sulfurihydrogenibium azorense Az-Fu1T its closest characterised relative (94.51% 16S rRNA gene sequence similarity, 78.01% whole genome ANI, 61.34% whole genome AAI). Based on phylogenetic and phenotypic analyses, we propose KUI-RBT represents a novel genus and species within the family Hydrogenothermaceae, for which we propose the name Reysenbachia aerophila gen. nov., sp. nov. The type strain is KUI-RBT (=KCTC accession =JCM accession). The GenBank accession number for the 16S rRNA gene sequence of strain KUI-RBT is PZ052650. The GenBank accession number for the whole genome of strain KUI-RBT is JBVODP000000000.

microbiology↗

bioRxiv2018

Two Chloroflexi classes independently evolved the ability to persist on atmospheric hydrogen and carbon monoxide

Bacteria within aerated environments often exist within a variety of dormant forms. In these states, bacteria endure adverse environmental conditions such as organic carbon starvation by decreasing metabolic expenditure and using alternative energy sources. In this study, we investigated the energy sources that facilitate the persistence of the environmentally widespread but understudied bacterial phylum Chloroflexi. A transcriptome study revealed that Thermomicrobium roseum (class Chloroflexia) extensively remodels its respiratory chain upon entry into stationary phase due to organic carbon limitation. Whereas primary dehydrogenases associated with heterotrophic respiration were downregulated, putative operons encoding enzymes involved in molecular hydrogen (H2), carbon monoxide (CO), and sulfur compound oxidation were significantly upregulated. Gas chromatography and microsensor experiments were used to show that T. roseum aerobically respires H2 and CO at a range of environmentally relevant concentrations to sub-atmospheric levels. Phylogenetic analysis suggests that the enzymes mediating atmospheric H2 and CO oxidation, namely group 1h [NiFe]-hydrogenases and type I carbon monoxide dehydrogenases, are widely distributed in Chloroflexi genomes and have been acquired on at least two occasions through separate horizontal gene transfer events. Consistently, we confirmed that the sporulating isolate Thermogemmatispora sp. T81 (class Ktedonobacteria) also oxidises atmospheric H2 and CO during persistence. This study provides the first axenic culture evidence that atmospheric CO supports bacterial persistence and reports the third phylum to be experimentally shown to mediate the biogeochemically and ecologically important process of atmospheric H2 oxidation. This adds to the growing body of evidence that atmospheric trace gases serve as dependable energy sources for the survival of dormant microorganisms.

microbiology↗

bioRxiv2018

Microbial biogeography of 1,000 geothermal springs in New Zealand

Geothermal springs are model ecosystems to systematically investigate microbial biogeography as they i) represent discrete, homogenous habitats; ii) are abundantly distributed across multiple geographical scales; iii) span broad geochemical gradients; and iv) have simple community structures with reduced metazoan interactions. Taking advantage of these traits, we undertook the largest known consolidated study of geothermal ecosystems (http://1000springs.org.nz) to determine factors that influence biogeographical patterns. Rigorously standardised methodologies were used to measure microbial communities, 46 physicochemical parameters, and metadata from 1,019 hotspring samples across New Zealand. pH was found to be the primary influence on diversity in springs < 70 {degrees}C with community similarity decreasing with geographic distance. Surprisingly, community composition was dominated by two genera (Venenivibrio and Acidithiobacillus) in both average relative abundance (11.2 and 11.1 %) and prevalence (74.2 and 62.9 % respectively) across physicochemical spectrums of 13.9 - 100.6 {degrees}C and pH < 1 - 9.7. This study provides an unprecedented insight into the ecological conditions that drive community assembly in geothermal springs, and can be used as a foundation to improve the characterisation of global microbial biogeographical processes.

microbiology↗