His primary areas of study are Hydrothermal circulation, Abiogenesis, Environmental chemistry, Olivine and Geochemistry. He works mostly in the field of Hydrothermal circulation, limiting it down to concerns involving Carbon and, occasionally, Inorganic chemistry. His studies in Environmental chemistry integrate themes in fields like Seawater and Psychrophile, Bacteria.
His study looks at the relationship between Seawater and topics such as Sulfide, which overlap with Hydrothermal vent and Mineralogy. His Olivine research includes themes of Ultramafic rock, Methane, Lost City Hydrothermal Field and Peridotite. In his research, Thomas M. McCollom performs multidisciplinary study on Geochemistry and Oceanic crust.
Thomas M. McCollom mainly investigates Geochemistry, Hydrothermal circulation, Mineralogy, Methane and Mars Exploration Program. His work on Ultramafic rock and Crust as part of general Geochemistry research is often related to Coast Range Ophiolite and Oceanic crust, thus linking different fields of science. His Hydrothermal circulation research is multidisciplinary, incorporating perspectives in Seawater, Deep sea, Inorganic chemistry and Environmental chemistry.
When carried out as part of a general Mineralogy research project, his work on Olivine is frequently linked to work in Table, therefore connecting diverse disciplines of study. His Methane research focuses on Abiogenesis and how it relates to Carbon, Earth and Lost City Hydrothermal Field. His Mars Exploration Program study integrates concerns from other disciplines, such as Volcano and Sulfate.
The scientist’s investigation covers issues in Geochemistry, Mars Exploration Program, Environmental science, Environmental chemistry and Olivine. His work on Jarosite and Diagenesis as part of general Geochemistry study is frequently linked to Biogeosciences, therefore connecting diverse disciplines of science. Thomas M. McCollom focuses mostly in the field of Mars Exploration Program, narrowing it down to topics relating to Sulfate and, in certain cases, Thiosulfate and Sulfide.
His research in Environmental chemistry intersects with topics in Ecology, Methane and Abiotic component. He has researched Olivine in several fields, including Magnetite and Reaction rate. His work on Hydrothermal vent is typically connected to Earth as part of general Hydrothermal circulation study, connecting several disciplines of science.
Thomas M. McCollom mainly focuses on Methane, Mineralogy, Environmental chemistry, Magnetite and Olivine. In his study, Abiogenesis, Carbon monoxide dehydrogenase, Catalysis, Carbon fixation and Awaruite is inextricably linked to Hydrogen, which falls within the broad field of Methane. His Environmental chemistry study combines topics in areas such as Anaerobic oxidation of methane, Organic chemistry, Archaea and Ultramafic rock.
The concepts of his Olivine study are interwoven with issues in Total inorganic carbon, Abiotic component and Abiotic synthesis. His study looks at the relationship between Hydrogen production and fields such as Reaction rate, as well as how they intersect with chemical problems. His study ties his expertise on Analytical chemistry together with the subject of Hydrothermal circulation.
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Geochemical constraints on chemolithoautotrophic metabolism by microorganisms in seafloor hydrothermal systems
Thomas M. McCollom;Everett L. Shock.
Geochimica et Cosmochimica Acta (1997)
Abiotic Synthesis of Organic Compounds in Deep-Sea Hydrothermal Environments
Thomas M McCollom;Jeffrey S Seewald.
Chemical Reviews (2007)
Lipid synthesis under hydrothermal conditions by Fischer-Tropsch-type reactions.
Thomas M. McCollom;Gilles Ritter;Bernd R. T. Simoneit.
Origins of Life and Evolution of Biospheres (1999)
Thermodynamic constraints on hydrogen generation during serpentinization of ultramafic rocks
Thomas M. McCollom;Wolfgang Bach.
Geochimica et Cosmochimica Acta (2009)
A reassessment of the potential for reduction of dissolved CO 2 to hydrocarbons during serpentinization of olivine
Thomas M McCollom;Jeffrey S Seewald.
Geochimica et Cosmochimica Acta (2001)
Hydrogen and bioenergetics in the Yellowstone geothermal ecosystem.
John R. Spear;Jeffrey J. Walker;Thomas M. McCollom;Norman R. Pace.
Proceedings of the National Academy of Sciences of the United States of America (2005)
Carbon isotope composition of organic compounds produced by abiotic synthesis under hydrothermal conditions
Thomas M. McCollom;Jeffrey S. Seewald.
Earth and Planetary Science Letters (2006)
Isolation and Characterization of Novel Psychrophilic, Neutrophilic, Fe-Oxidizing, Chemolithoautotrophic α- and γ-Proteobacteria from the Deep Sea
Katrina J. Edwards;Daniel R. Rogers;Carl O. Wirsen;Thomas M. McCollom.
Applied and Environmental Microbiology (2003)
Geomicrobiology in oceanography: microbe–mineral interactions at and below the seafloor
Katrina J. Edwards;Wolfgang Bach;Thomas M. McCollom.
Trends in Microbiology (2005)
Iron partitioning and hydrogen generation during serpentinization of abyssal peridotites from 15°N on the Mid-Atlantic Ridge
Frieder Klein;Wolfgang Bach;Niels Jöns;Thomas M McCollom.
Geochimica et Cosmochimica Acta (2009)
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