Acidianus manzaensis sp. nov., a Novel Thermoacidophilic Archaeon Growing Autotrophically by the Oxidation of H2 with the Reduction of Fe3+

A novel thermoacidophilic iron-reducing Archaeon, strain NA−1, was isolated from a hot fumarole in Manza, Japan. Strain NA-1 could grow autotrophically using H₂ or S⁰ as an electron donor and Fe³⁺ as an electron acceptor, and also could grow heterotrophically using some organic compounds. Fe³⁺ and O₂ served as electron acceptors for growth. However, S⁰, NO₃ ⁻, NO₂ ⁻, SO₄ ²⁻, Mn⁴⁺, fumarate, and Fe₂O₃ did not serve as electron acceptors. The ranges of growth temperature and pH were 60–90°C (optimum: 80°C) and pH 1.0–5.0 (optimum: pH 1.2–1.5), respectively. Cells were nearly regular cocci with an envelope comprised of the cytoplasmic membrane and a single outer S-layer. The crenarchaeal-specific quinone (cardariellaquinone) was detected, and the genomic DNA G + C content was 29.9 mol%. From 16S rDNA analysis, it was determined that strain NA-1 is closely related to Acidianus ambivalens (93.1%) and Acidianus infernus (93.0%). However, differences revealed by phylogenetic and phenotypic analyses clearly show that strain NA-1 represents a new species, Acidianus manzaensis, sp. nov., making it the first identified thermoacidophilic iron-reducing microorganism (strain NA-1^T = NBRC 100595 = ATCC BAA 1057). Strain NA-1 has been deposited in the culture collections of the National Institute of Technology and Evolution (NBRC 100595) and American Type Culture Collection (ATCC BAA 1057). The 16S rDNA sequence has been deposited at GenBank under accession number AB182498.