Research Overview
                        Thermophile research in the McDermott laboratory involves 
                          two independent research thrusts. One involves the development 
                          of a program that seeks to examine, characterize, and 
                          understand microbial populations inhabiting geothermally 
                          heated soil environments. The discovery, isolation, 
                          and characterization of novel and diverse thermophiles 
                          is a central platform of this particular project. The 
                          second thrust focuses on microbe-arsenic interactions 
                          in geothermal environments. Here, we wish to extend 
                          our general understanding of microbial arsenic redox 
                          biochemistry and physiology, and whether these reactions, 
                          when coupled with other relevant aqueous and solid phase 
                          chemical signatures, can be used as biomarkers of present 
                          or past microbial activity. 
                        Geothermal Soils: 
                        In recent work, we have isolated a novel thermophile, 
                          Thermobaculum terrenum, that appears to be the 
                          only cultured and characterized representative of a 
                          clade (Botero et al. 2004), which was previously comprised 
                          entirely of environmental clones within the phylum Chloroflexi 
                          (formally the Green Non-Sulfur division). In addition, 
                          we have isolated and characterized a proposed novel 
                          species of Geobacillus (species name tepidamans) 
                          (Schaeffer et al, submitted). In other work, we have 
                          employed DNA- and RNA-based molecular techniques to 
                          study population shifts occurring in response to increased 
                          soil temperature resulting from expansion of underlying 
                          geothermal activity (Norris et al. 2002b).
Microbe-Arsenic Interactions. 
                          
                        Work in this thrust seeks to improve our understanding 
                          of how microbes interact with and transform arsenic. 
                          Initial studies were molecular-based examinations of 
                          the microbial communities in arsenite-oxidizing thermal 
                          springs (in collaboration with Bill Inskeep). Subsequent 
                          work with this spring has involved the cultivation and 
                          characterization of different Hydrogenobaculum 
                          isolates (Donahoe-Christiansen et al. 2004). These hydrogenobacula 
                          are also being studied for their contribution to sulfide 
                          and hydrogen oxidation in these springs. This work has 
                          provided training for one postdoc, one MS student, and 
                          three undergraduate interns. 
                         Other microbe-arsenic interaction work has included 
                          a proteomics examination of Sulfolobus global 
                          responses to arsenic (Barry et al. In preparation). 
                          The goal of this particular study was to extend our 
                          knowledge base of microbe-arsenic interactions beyond 
                          its current state, which is largely confined to studies 
                          that focus on ars gene expression. Other arsenic 
                          work includes studies aimed at investigating the potential 
                          contribution of cyanidia to arsenic transformations 
                          in the Yellowstone thermal springs. These evolutionarily 
                          ancient eukaryotic algae are found throughout Yellowstone 
                          and often dominate microbial communities in low pH thermal 
                          springs, pools, and soils.