Hydrogen and Carbon Monoxide-Utilizing Kyrpidia Spormannii Species from Pantelleria Island, Italy

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Hydrogen and Carbon Monoxide-Utilizing Kyrpidia Spormannii Species from Pantelleria Island, Italy fmicb-11-00951 May 15, 2020 Time: 16:54 # 1 ORIGINAL RESEARCH published: 19 May 2020 doi: 10.3389/fmicb.2020.00951 Hydrogen and Carbon Monoxide-Utilizing Kyrpidia spormannii Species From Pantelleria Island, Italy Carmen Hogendoorn1, Arjan Pol1, Nunzia Picone1, Geert Cremers1, Theo A. van Alen1, Antonina L. Gagliano2, Mike S. M. Jetten1, Walter D’Alessandro2, Paola Quatrini3 and Huub J. M. Op den Camp1* 1 Department of Microbiology, Institute for Water and Wetland Research, Radboud University, Nijmegen, Netherlands, 2 Istituto Nazionale di Geofisica e Vulcanologia, Palermo, Italy, 3 Department of Biological, Chemical and Pharmaceutical Sciences and Technologies (STEBICEF), University of Palermo, Palermo, Italy Volcanic and geothermal areas are hot and often acidic environments that emit geothermal gasses, including H2, CO and CO2. Geothermal gasses mix with air, creating Edited by: conditions where thermoacidophilic aerobic H2- and CO-oxidizing microorganisms Axel Schippers, could thrive. Here, we describe the isolation of two Kyrpidia spormannii strains, which Federal Institute for Geosciences can grow autotrophically by oxidizing H2 and CO with oxygen. These strains, FAVT5 and and Natural Resources, Germany COOX1, were isolated from the geothermal soils of the Favara Grande on Pantelleria Reviewed by: Philippe Constant, Island, Italy. Extended physiology studies were performed with K. spormannii FAVT5, Institut National de la Recherche and showed that this strain grows optimally at 55◦C and pH 5.0. The highest growth Scientifique (INRS), Canada ± −1 Marianne Quéméneur, rate is obtained using H2 as energy source (mmax 0.19 0.02 h , doubling time UMR7294 Institut Méditerranéen 3.6 h). K. spormannii FAVT5 can additionally grow on a variety of organic substrates, d’Océanographie (MIO), France including some alcohols, volatile fatty acids and amino acids. The genome of each strain *Correspondence: encodes for two O2-tolerant hydrogenases belonging to [NiFe] group 2a hydrogenases Huub J. M. Op den Camp [email protected] and transcriptome studies using K. spormannii FAVT5 showed that both hydrogenases are expressed under H2 limiting conditions. So far no Firmicutes except K. spormannii Specialty section: FAVT5 have been reported to exhibit a high affinity for H2, with a Ks of 327 ± 24 nM. The This article was submitted to Extreme Microbiology, genomes of each strain encode for one putative CO dehydrogenase, belonging to Form a section of the journal II aerobic CO dehydrogenases. The genomic potential and physiological properties of Frontiers in Microbiology these Kyrpidia strains seem to be quite well adapted to thrive in the harsh environmental Received: 21 January 2020 Accepted: 21 April 2020 volcanic conditions. Published: 19 May 2020 Keywords: Kyrpidia spormannii,H2, [NiFe]-hydrogenases, CO, thermoacidophilic, phylogeny Citation: Hogendoorn C, Pol A, Picone N, Cremers G, van Alen TA, Gagliano AL, INTRODUCTION Jetten MSM, D’Alessandro W, Quatrini P and Op den Camp HJM Volcanic and geothermal areas represent the result of the dynamics involving the deeper layers of (2020) Hydrogen and Carbon Monoxide-Utilizing Kyrpidia the earth and resulting in the emission of several gases from volcanic soils. In general, geothermal spormannii Species From Pantelleria gases are mainly composed of H2O and CO2 as the most dominant species, and other minor Island, Italy. Front. Microbiol. 11:951. species as the more reduced gases H2S, CH4,H2, CO, and NH3 (Oppenheimer et al., 2014). The doi: 10.3389/fmicb.2020.00951 abundance of the latter gases, and consequently their impact to the atmosphere, is strictly related to Frontiers in Microbiology| www.frontiersin.org 1 May 2020| Volume 11| Article 951 fmicb-11-00951 May 15, 2020 Time: 16:54 # 2 Hogendoorn et al. H2 and CO-Oxidizing Kyrpidia spormannii the energy of the system, the water-rock interactions, gas- very important because any variation in its amount may indicate gas interactions and also to the gas-biota interactions. In some variations of the hydrothermal system. CO can be oxidized fact, the minor gas species represent the driving forces for under aerobic and anaerobic conditions (Robb and Techtmann, the establishment of an active microbial community (Shock 2018). Anaerobic CO-oxidizing bacteria have been detected in et al., 2010; Lindsay et al., 2019). Commonly, geothermal soils geothermal springs of neutral pH (Brady et al., 2015). In addition, are characterized by high temperatures and often a low pH, anaerobic microbial CO consumption has been observed in acidic which may be caused by the presence of H2S and CS2 in hot spring mud of pH 2.9 (Ikeda et al., 2015). In both cases, the emitted gases and their conversion to sulfuric acid by the microbial population was dominated by Firmicutes. Two sulfide-oxidizing microbes (Chiodini et al., 2001; D’Alessandro distinct classes of CO dehydrogenases (CODH) catalyze CO et al., 2009; Smeulders et al., 2011, 2013; Quatrini and transformation. The active site of the CODH from anaerobes Johnson, 2018). Despite the harsh conditions, these hot and contains a sulfur-coordinated Ni in a [Ni-4Fe-5S] cluster (Robb acidic terrestrial areas harbor distinctive microbial communities and Techtmann, 2018) and can be monofunctional producing (Colman et al., 2019a,b; Lindsay et al., 2019). Analyses of CO2 or bifunctional producing acetyl-CoA and H2. Aerobic soil microbial communities show that at low pH and high CO-oxidizers, or carboxydotrophs, possess heterotrimeric CO temperature, the dominant phyla differ from areas with moderate dehydrogenases with an active site containing a [Mo-Cu] temperature and neutral pH (Strazzulli et al., 2017). Beside cluster in the CoxL subunit. The other components are a temperature and acidity, the available nutrients determine the flavoprotein (CoxM) and an iron-sulfur protein (CoxS). These microbial composition. enzyme complexes catalyze the unidirectional conversion of Gagliano et al.(2016) showed that 99% of the sequences CO to CO2. The aerobic [Mo-Cu]-CO dehydrogenases can be obtained at the FAV1 site at the geothermal soils of the Favara categorized in two groups, Form I and Form II (King and Grande (Pantelleria Island) could be assigned to four main phyla: Weber, 2007). Biochemical analysis showed that Form I has Proteobacteria, Firmicutes, Actinobacteria and Chloroflexi. At highest CO oxidation rates and is responsible for aerobic growth the FAV2 site 98% of the sequences were distributed in on CO. Form II is phylogenetically closer related to Form I only three phyla Proteobacteria, Firmicutes and Actinobacteria. CO dehydrogenase than to other enzymes of the molybdenum Especially Chloroflexi were much less represented than in FAV1. hydroxylases family. So far, no firm evidence is reported for C Apparently sites with low NH4 concentration are dominated by CO oxidation by Form II enzymes, suggesting that Form II CO C a diverse methanotrophic community, whereas high NH4 soils dehydrogenases may also catalyze the oxidation of a different harbor thermo-acidophilic chemolithotrophs, despite CH4 being substrate (Cunliffe, 2011). present. Alphaproteobacterial methanotrophs were isolated from In the upper layer of geothermal soils air is mixed with the C the low NH4 site (Gagliano et al., 2014). Previously, key players geothermal gasses (Gagliano et al., 2016). Since soil porosity in the conversion of H2S, CS2, and CH4 from the Solfatara is higher than in the deeper soil horizon and the uprising geothermal area near Naples, Italy, have been isolated and hydrothermal flux lost part of its energy, this results in conditions characterized (Pol et al., 2007; Smeulders et al., 2011, 2013; where (micro)aerobic H2 and CO-oxidizing bacteria could thrive. van Teeseling et al., 2014). Besides H2S, CS2 and CH4,H2 Here, we used samples of the Favare grande soil to enrich H2- and CO are available and suitable electron donors for novel oxidizing microorganisms. After serial dilution to extinction of chemolithoautotrophs in geothermal soils. In this study, we active enrichments we isolated and characterized two Kyrpidia focused on H2 and CO-utilizing bacteria from the Favara Grande spormannii species capable of using H2 and CO as sole energy geothermal site on Pantelleria Island, Italy. These hot and acidic source. We show that the genomic potential and physiological soils are characterized by H2 (5-168,000 ppm) and CO (1.6- properties of the two Kyrpidia strains seem very suited to thrive 26 ppm) emissions (D’Alessandro et al., 2009) and in situ in harsh volcanic conditions. H2 consumption was already observed (Gagliano et al., 2016). Both H2 and CO have a high potential as electron donor for microbial growth. MATERIALS AND METHODS H2 is an important electron donor in acidic and neutral hot springs (Spear et al., 2005) and can be used in a Geological Setting lithotrophic lifestyle under aerobic or anaerobic conditions. Pantelleria Island is a quiescent volcano located in the Oxidation of H2 is catalyzed by the enzyme hydrogenase, Sicily Channel, and characterized by several hydrothermal which can be classified as [NiFe]-, [FeFe]-, or [Fe]-hydrogenase manifestations as mofettes, fumaroles and passive degassing from depending on the metal ion in the active site (Lubitz et al., geothermal soils. The main exhalative area is Favara Grande, 2014). Hydrogenases are found among many different phyla, where soil temperatures can reach 115◦C at 5 cm of depth such as Proteobacteria, Firmicutes, Cyanobacteria, Chloroflexi, and soil pH may be down to 3. The
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