Publications

4359

A novel strictly anaerobic, moderately halophilic and mesophilic bacterium, designated strain SOL3f37T, was isolated from a hydrocarbon-polluted soil surrounding a deep petroleum environment located in south Tunisia. Cells of strain SOL3f37T stained Gram-positive and were motile, straight and spore-forming. Strain SOL3f37T had a typical Gram-positive-type cell-wall structure, unlike the thick, multilayered cell wall of its closest relative Clostridiisalibacter paucivorans. The major fatty acids were iso-C15 : 0 (41 %), iso-C14 : 0 3-OH and/or iso-C15 : 0 dimethyl acetal (21.6 %), iso-C13 : 0 (4.4 %), anteiso-C15 : 0 (3.9 %) and iso-C15 : 1 (2.8 %). Strain SOL3f37T grew between 20 and 48 °C (optimum 40 °C) and at pH 6.2–8.1 (optimum pH 6.9). Strain SOL3f37T required at least 0.5 g NaCl l−1 and grew in the presence of NaCl concentrations up to 150 g l−1 (optimum 40 g l−1). Yeast extract (2 g l−1) was required for degradation of pyruvate, fumarate, fructose, glucose and mannitol. Also, strain SOL3f37T grew heterotrophically on yeast extract, peptone and bio-Trypticase, but was unable to grow on Casamino acids. Sulfate, thiosulfate, sulfite, elemental sulfur, fumarate, nitrate and nitrite were not reduced. The DNA G+C content was 30.7 mol%. Phylogenetic analysis based on 16S rRNA gene sequences revealed that strain SOL3f37T was a member of the family Clostridiaceae in the order Clostridiales; strain SOL3f37T was related to members of various genera of the family Clostridiaceae. It exhibited highest 16S rRNA gene sequence similarity (93.4 %) with Clostridiisalibacter paucivorans 37HS60T, 91.8 % with Thermohalobacter berrensis CTT3T and 91.7 % with Caloranaerobacter azorensis MV1087T. On the basis of genotypic, phenotypic and phylogenetic data, it is suggested that strain SOL3f37T represents a novel species in a new genus. The name Sporosalibacterium faouarense gen. nov., sp. nov. is proposed, with SOL3f37T (=DSM 21485T =JCM 15487T) as the type strain of Sporosalibacterium faouarense.

Abstract Marine pelagic redoxclines are areas of enhanced biogeochemical cycling inhabited by distinct functional groups of prokaryotes. In this study, the diversity and abundance of archaeal and bacterial nitrifying populations throughout a pelagic redoxcline in the central Baltic Sea were examined using a suite of molecular methods. 16S rRNA/rRNA gene as well as bacterial and archaeal amoA mRNA/amoA gene fingerprints and clone libraries revealed that the putative nitrifying assemblages consisted solely of one crenarchaeotal subcluster, named GD2, which was closely related to Candidatus Nitrosopumilus maritimus. Neither distinct differences between transcript- and gene-based fingerprints nor pronounced differences in the crenarchaeotal composition throughout the whole redoxcline were detected. The abundance of this GD2 subgroup, as determined by the oligonucleotide probe Cren537 and the newly developed and more specific probe Cren679 showed that GD2 and total crenarchaeotal cell numbers were nearly identical throughout the redoxcline. The highest GD2 abundance (2.3 × 105 cells ml−1) occurred in the suboxic zone, accounting for around 26% of total prokaryotic cells. Below the chemocline, GD2 abundance was relatively stable (1.5–1.9 × 105 cells ml−1). Archaeal amoA expression was detected only in the putative nitrification zone and formed a narrow band in the suboxic layer, where ammonium, oxygen, nitrate, nitrite and phosphate concentrations were below 5 μmol l−1. To our knowledge this is the first study to show the dominance of only one crenarchaeotal nitrifying key cluster in a natural habitat. The metabolic properties and survival mechanisms present in this cluster inside and outside the nitrification zone remain to be determined.