The Iberian Pyrite Belt (IPB) is one of the largest deposits of sulphidic minerals on Earth. Río Tinto raises from its core, presenting low a pH and high metal concentration. Several drilling cores were extracted from the IPB's subsurface, and strain T2.3D-1.1 was isolated from a core at 121.8 m depth. We aimed to characterize this subterranean microorganism, revealing its phylogenomic affiliation (Average Nucleotide Identity, digital DNA-DNA Hybridization) and inferring its physiology through genome annotation, backed with physiological experiments to explore its relationship with the Fe biogeochemical cycle. Results determined that the isolate belongs to the (with ANI 99.25 with CN-32). Its genome harbours the necessary genes, including A CAB, to perform the Extracellular Electron Transfer (EET) and reduce acceptors such as Fe, AB to reduce NO to NO, AB to produce H and genes A, ABC and ABC to reduce SO, SO and SO, respectively. A full CRISPR-Cas 1F type system was found as well. T2.3D-1.1 can reduce Fe and promote the oxidation of Fe in the presence of NO under anaerobic conditions. Production of H has been observed under anaerobic conditions with lactate or pyruvate as the electron donor and fumarate as the electron acceptor. Besides Fe and NO, the isolate also grows with Dimethyl Sulfoxide and Trimethyl N-oxide, SO and SO as electron acceptors. It tolerates different concentrations of heavy metals such as 7.5 mM of Pb, 5 mM of Cr and Cu and 1 mM of Cd, Co, Ni and Zn. This array of traits suggests that T2.3D-1.1 could have an important role within the Iberian Pyrite Belt subsurface participating in the iron cycle, through the dissolution of iron minerals and therefore contributing to generate the extreme conditions detected in the Río Tinto basin.