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Showing 1–6 of 6 results
Advanced filters: Author: Laurent Remusat Clear advanced filters
  • The insoluble organic matter in primitive carbonaceous chondrites has a systematic large enrichment in deuterium and several hypotheses have been proposed to explain this. Here, the authors demonstrate that irradiation from the protosun could quantitatively explain the deuteration.

    • Boris Laurent
    • Mathieu Roskosz
    • Jean-Marc Lefebvre
    ResearchOpen Access
    Nature Communications
    Volume: 6, P: 1-6
  • A new study of samples from the Ryugu asteroid reveal a greater diversity of macromolecular organic matter than that found in related carbonaceous meteorites. Researchers find distinct populations of alkyl-aromatic grains, and organic carbonate is found with coarse-grained clay minerals

    • Bradley De Gregorio
    • George D. Cody
    • Yuichi Tsuda
    ResearchOpen Access
    Nature Communications
    Volume: 15, P: 1-11
  • Through platinum metal-silicate partitioning coefficient measurements, the authors here show that platinum partitioning into metal is lowered at high pressure–temperature conditions. This finding implies that the Earth’s mantle was likely enriched in platinum immediately following the core-mantle differentiation.

    • Terry-Ann Suer
    • Julien Siebert
    • Guillaume Fiquet
    ResearchOpen Access
    Nature Communications
    Volume: 12, P: 1-10
  • Many major mass extinction events have been associated with large volcanic eruption events, with the argument that large volumes of volcanic degassing could trigger past global climate changes. Here, the authors find that during the end-Triassic extinction event volcanic pulses emitted large amounts of CO2 comparable to projected anthropogenic emissions for the 21st century in the future 2 °C warming scenario.

    • Manfredo Capriolo
    • Andrea Marzoli
    • Csaba Szabó
    ResearchOpen Access
    Nature Communications
    Volume: 11, P: 1-11
  • Laboratory analyses on six carbonaceous chondrites suggest the presence of two water sources with different deuterium (D) enrichment levels in the protoplanetary disk: a D-poor inner reservoir and a D-rich water component transferred inward from the outer disk.

    • Laurette Piani
    • Hisayoshi Yurimoto
    • Laurent Remusat
    Research
    Nature Astronomy
    Volume: 2, P: 317-323