World's Best Scientists 2026 revealed!

D-Index & Metrics

Earth Science

D-Index
31
Citations
5976
World Ranking
8837
National Ranking
81

Best Publications

  • Geochemistry of high H2 and CH4 vent fluids issuing from ultramafic rocks at the Rainbow hydrothermal field (36°14'N, MAR)

    J.L Charlou;J.P Donval;Y Fouquet;P Jean-Baptiste

  • Distributions of Microbial Activities in Deep Subseafloor Sediments

    Steven D'Hondt;Bo Barker Jørgensen;D. Jay Miller;Anja Batzke

  • Initial indications of abiotic formation of hydrocarbons in the Rainbow ultramafic hydrothermal system, Mid-Atlantic Ridge

    Unknown

  • The internal structure of an active sea-floor massive sulphide deposit

    S. E. Humphris;Peter Herzig;D. J. Miller;J .C. Alt

  • Abiotic synthesis of amino acids under hydrothermal conditions and the origin of life: a perpetual phenomenon?

    Unknown

  • Biological formation of ethane and propane in the deep marine subsurface.

    Kai-Uwe Hinrichs;John M. Hayes;Wolfgang Bach;Arthur J. Spivack

  • Hydrocarbons and oxidized organic compounds in hydrothermal fluids from Rainbow and Lost City ultramafic-hosted vents

    Cécile Konn;Jean-Luc Charlou;Jean-Pierre Donval;Nils Holm

  • Serpentinization and the Formation of H2 and CH4 on Celestial Bodies (Planets, Moons, Comets)

    Nils G. Holm;C. Oze;O. Mousis;J. H. Waite

  • The Production of Methane, Hydrogen, and Organic Compounds in Ultramafic-Hosted Hydrothermal Vents of the Mid-Atlantic Ridge

    Cecile Konn;Jean-Luc Charlou;N. G. Holm;O. Mousis

  • Hydrothermal simulation experiments as a tool for studies of the origin of life on Earth and other terrestrial planets: a review.

    Unknown

  • Formation of H2 and CH4 by weathering of olivine at temperatures between 30 and 70°C.

    Anna Neubeck;Nguyen Thanh Duc;David Bastviken;Patrick Crill

  • Chapter 1 Why are hydrothermal systems proposed as plausible environments for the origin of life

    Unknown

  • Alkaline fluid circulation in ultramafic rocks and formation of nucleotide constituents: a hypothesis.

    Unknown

  • Reduction of nitrogen compounds in oceanic basement and its implications for HCN formation and abiotic organic synthesis

    Nils G Holm;Anna Neubeck

  • Serpentinization: Connecting Geochemistry, Ancient Metabolism and Industrial Hydrogenation

    Martina Preiner;Joana C. Xavier;Filipa L. Sousa;Verena Zimorski

  • Olivine alteration and H2 production in carbonate-rich, low temperature aqueous environments

    Anna Neubeck;Nguyen Thanh Duc;Helge Hellevang;Christopher Oze

  • What determines the volume of the oceans

    James F. Kasting;Nils G. Holm

  • Why are Hydrothermal Systems Proposed as Plausible Environments for the Origin of Life

    Unknown

  • Links Between Hydrothermal Environments, Pyrophosphate, Na +, and Early Evolution

    Unknown

  • The 13C12C ratios of siderite and organic matter of a modern metalliferous hydrothermal sediment and their implications for banded iron formations

    Unknown

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