Search Results - "Holm, Nils G"
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Biogenic Mn-Oxides in Subseafloor Basalts
Published in PloS one (24-06-2015)“…The deep biosphere of the subseafloor basalts is recognized as a major scientific frontier in disciplines like biology, geology, and oceanography. Recently,…”
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Olivine alteration and H2 production in carbonate-rich, low temperature aqueous environments
Published in Planetary and space science (01-06-2014)“…Hydrous alteration of olivine is capable of producing molecular hydrogen (H2) under a wide variety of hydrothermal conditions. Although olivine hydrolysis…”
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3
Serpentinization: Connecting Geochemistry, Ancient Metabolism and Industrial Hydrogenation
Published in Life (Basel, Switzerland) (22-09-2018)“…Rock⁻water⁻carbon interactions germane to serpentinization in hydrothermal vents have occurred for over 4 billion years, ever since there was liquid water on…”
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Distributions of Microbial Activities in Deep Subseafloor Sediments
Published in Science (American Association for the Advancement of Science) (24-12-2004)“…Diverse microbial communities and numerous energy-yielding activities occur in deeply buried sediments of the eastern Pacific Ocean. Distributions of metabolic…”
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Biological Formation of Ethane and Propane in the Deep Marine Subsurface
Published in Proceedings of the National Academy of Sciences - PNAS (03-10-2006)“…Concentrations and isotopic compositions of ethane and propane in cold, deeply buried sediments from the southeastern Pacific are best explained by microbial…”
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Laboratory Studies of Methane and Its Relationship to Prebiotic Chemistry
Published in Astrobiology (01-08-2017)“…To examine how prebiotic chemical evolution took place on Earth prior to the emergence of life, laboratory experiments have been conducted since the 1950s…”
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Borophosphates and silicophosphates as plausible contributors to the emergence of life
Published in Journal of colloid and interface science (01-10-2014)“…[Display omitted] •Inorganic hydrogels as cradle of prebiotic processes.•Enantiomeric enrichment using chiral minerals.•Chiral minerals derived from inorganic…”
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8
Formation of H2 and CH4 by weathering of olivine at temperatures between 30 and 70°C
Published in Geochemical transactions GT (27-06-2011)“…Hydrocarbons such as CH4 are known to be formed through the Fischer-Tropsch or Sabatier type reactions in hydrothermal systems usually at temperatures above…”
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Reduction of nitrogen compounds in oceanic basement and its implications for HCN formation and abiotic organic synthesis
Published in Geochemical transactions GT (22-10-2009)“…Hydrogen cyanide is an excellent organic reagent and is central to most of the reaction pathways leading to abiotic formation of simple organic compounds…”
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Hydrothermal simulation experiments as a tool for studies of the origin of life on Earth and other terrestrial planets: a review
Published in Astrobiology (01-08-2005)“…The potential of life's origin in submarine hydrothermal systems has been evaluated by a number of investigators by conducting high temperature-high pressure…”
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Alkaline fluid circulation in ultramafic rocks and formation of nucleotide constituents: a hypothesis
Published in Geochemical transactions GT (25-07-2006)“…Seawater is constantly circulating through oceanic basement as a low-temperature hydrothermal fluid (<150 degrees C). In cases when ultramafic rocks are…”
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12
Differential Adsorption of Nucleic Acid Bases: Relevance to the Origin of Life
Published in Proceedings of the National Academy of Sciences - PNAS (30-01-2001)“…The adsorption of organic molecules onto the surfaces of inorganic solids has long been considered a process relevant to the origin of life. We have determined…”
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13
Chromite oxidation by manganese oxides in subseafloor basalts and the presence of putative fossilized microorganisms
Published in Geochemical transactions GT (03-06-2011)“…Chromite is a mineral with low solubility and is thus resistant to dissolution. The exception is when manganese oxides are available, since they are the only…”
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14
Characterisation of dissolved organic compounds in hydrothermal fluids by stir bar sorptive extraction - gas chomatography - mass spectrometry. Case study: the Rainbow field (36°N, Mid-Atlantic Ridge)
Published in Geochemical transactions GT (07-11-2012)“…The analysis of the dissolved organic fraction of hydrothermal fluids has been considered a real challenge due to sampling difficulties, complexity of the…”
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A demonstration of an affinity between pyrite and organic matter in a hydrothermal setting
Published in Geochemical transactions GT (07-02-2011)“…One of the key-principles of the iron-sulphur world theory is to bring organic molecules close enough to interact with each other, using the surface of pyrite…”
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16
Isotopic Signatures of Carbon in the ‘Los Pobres’ Graphite Mine, Ronda, Spain
Published in Journal of petrology (01-04-2020)“…Abstract Graphite formation temperatures in the ‘Los Pobres’ mine within the Ronda peridotite, Spain, previously reported to be between 770 and 820 °C, have…”
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17
The evolution of organic matter in space
Published in Philosophical transactions of the Royal Society of London. Series A: Mathematical, physical, and engineering sciences (13-02-2011)“…Carbon, and molecules made from it, have already been observed in the early Universe. During cosmic time, many galaxies undergo intense periods of star…”
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Methane clathrates in the solar system
Published in Astrobiology (01-04-2015)“…We review the reservoirs of methane clathrates that may exist in the different bodies of the Solar System. Methane was formed in the interstellar medium prior…”
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Glasses as sources of condensed phosphates on the early earth
Published in Geochemical transactions GT (06-06-2014)“…Procedures for the analysis of phosphorus in geological material normally aims for the determination of the total amount of P expressed as orthophosphate PO 4…”
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Initial indications of abiotic formation of hydrocarbons in the Rainbow ultramafic hydrothermal system, Mid-Atlantic Ridge
Published in Earth and planetary science letters (30-08-2001)“…In the presence of water, olivine of ultramafic rock is oxidized during the process referred to as `serpentinization'. Water in contact with the olivine is…”
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