24 Acidithiobacillus thiooxidans is an acidophilic chemolithoautotrophic bacterium 25 widely used in the mining industry due to its metabolic sulfur-oxidizing capability. The 26 biooxidation of sulfide minerals is enhanced through the attachment of A. thiooxidans 27 cells to the mineral surface. The Type IV pili (TfP) of At. thiooxidans may play an 28 important role in the bacteria attachment, since among other functions, TfP play a 29 key adhesive role in the attachment to and colonization of different surfaces. In this 30 work, we reported for the first time the confirmed mRNA sequences of three TfP 31 proteins from At. thiooxidans, the protein PilY1 and the TfP pilins PilW and PilV. The 32 nucleotide sequences of these TfP proteins show changes of some nucleotide 33 positions with respect to the corresponding annotated sequences. The bioinformatic 34 analyses and 3D-modeling of protein structures sustain their classification as TfP 35 proteins, as structural homologs of the corresponding proteins of P. aeruginosa, 36 results that sustain the role of PilY1, PilW and PilV in pili assembly. Also, that PilY1 37 comprises the conserved Neisseria-PilC (superfamily) domain of the tip-associated 38 adhesin, while PilW of the superfamily of putative TfP assembly proteins and PilV 39 belongs to the superfamily of TfP assembly protein. Also, the analyses suggested 40 the presence of specific functional domains involved in adhesion, energy 41 transduction and signaling functions. The phylogenetic analysis indicated that the 42 PilY1 of Acidithiobacillus genus forms a cohesive group linked with iron-and/or 43 sulfur-oxidizing microorganisms from acid mine drainage or mine tailings. This work 3 44 enriches knowledge regarding colonization, adhesion and biooxidation of inorganic 45 sulfurs by A. thiooxidans. 46 4 47 Introduction 48 Acidithiobacillus thiooxidans is an acidophilic chemolithoautotroph that uses reduced 49 sulfurs as a source of electrons and reducing power, including elemental sulfur (S 0 ), 50 polysulfides (S n 2-) and sulfide minerals, such as pyrite (FeS 2 ), chalcopyrite (CuFeS 2 ) 51 or sphalerite (ZnS). 52 Bacterial attachment to mineral surfaces influences the rate of dissolution of the 53 mineral because of surficial phenomena: Mixed potential decreases, changes in 54 kinetics and mass-transport processes [1]. Accordingly, bacterial attachment is due 55 to self-organization by a bioelectrochemical evolution on the interface. Interfacial 56 studies on charge and mass transfer demonstrate that S 0 biooxidation by At. 57 thiooxidans begins in the early stages of interaction (1 to 24 h) when the biofilm is 58 not constituted, and it is primarily controlled by surficial characteristics that pivoted 59 the bacterial attachment to the hydrophobic S 0 ; such attachment is an energy-60 dependent process in which At. thiooxidans essentially activates or modifies the 61 reactive properties of S 0 [2, 3]. The hydrophobic character of the interface 62 "determines the free energy of the adhesion process" [4]. The Typ...