Nicolas Dauphas

ORCID: 0000-0002-1330-2038
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About
Contact & Profiles
Research Areas
  • Astro and Planetary Science
  • Planetary Science and Exploration
  • Geological and Geochemical Analysis
  • Isotope Analysis in Ecology
  • Paleontology and Stratigraphy of Fossils
  • Geology and Paleoclimatology Research
  • Geochemistry and Elemental Analysis
  • High-pressure geophysics and materials
  • Radioactive element chemistry and processing
  • Stellar, planetary, and galactic studies
  • Nuclear Physics and Applications
  • Geomagnetism and Paleomagnetism Studies
  • Astronomical and nuclear sciences
  • Geochemistry and Geologic Mapping
  • earthquake and tectonic studies
  • Space Exploration and Technology
  • Hydrocarbon exploration and reservoir analysis
  • Radioactive contamination and transfer
  • Silicon Effects in Agriculture
  • Methane Hydrates and Related Phenomena
  • Gamma-ray bursts and supernovae
  • Nuclear physics research studies
  • Astrophysics and Star Formation Studies
  • Space Science and Extraterrestrial Life
  • Groundwater and Isotope Geochemistry

Fermi National Accelerator Laboratory
2014-2025

University of Chicago
2016-2025

Nanjing University
2024

National Museum of Nature and Science
2024

Tohoku University
2024

Goddard Space Flight Center
2023

Lunar and Planetary Institute
2023

University of New Mexico
2023

University of Aizu
2023

Johnson Space Center
2023

High‐precision iron isotopic compositions for Fe‐bearing geological reference materials and chondrites with a wide range of matrices (e.g., silicates, oxides, organic‐bearing materials) are reported. This comprehensive data set should serve as studies across biological disciplines both quality assurance inter‐laboratory calibration. Where comparison is available, the most measured in this study were agreement previously published within quoted uncertainties. Recommendations reporting future...

10.1111/j.1751-908x.2010.00085.x article EN Geostandards and Geoanalytical Research 2010-11-08

Magmatic differentiation helps produce the chemical and petrographic diversity of terrestrial rocks. The extent to which magmatic fractionates nonradiogenic isotopes is uncertain for some elements. We report analyses iron in basalts from Kilauea Iki lava lake, Hawaii. isotopic compositions (56Fe/54Fe) late-stagemeltveins are 0.2 permil (per thousand) greater than values olivine cumulates. Olivine phenocrysts up 1.2 per thousand lighter those whole These results demonstrate that fractionate...

10.1126/science.1157166 article EN Science 2008-06-19

Research Article| January 01, 2017 Iron Isotope Systematics Nicolas Dauphas; Dauphas Origins Lab, Department of the Geophysical Sciences and Enrico Fermi Institute, The University Chicago, 5734 South Ellis Avenue, Chicago IL 60637, USA, dauphas@uchicago.edu Search for other works by this author on: GSW Google Scholar Seth G. John; John Southern California, Earth Science, Marine Trace Element Laboratory, 3651 Trousdale Pkwy, Los Angeles, CA 90089, sethjohn@usc.edu Olivier Rouxel IFREMER,...

10.2138/rmg.2017.82.11 article EN Reviews in Mineralogy and Geochemistry 2017-01-01

Isotopic variations usually follow mass-dependent fractionation, meaning that the relative in isotopic ratios scale with difference mass of isotopes involved (e.g., δ 17 O ≈ 0.5×δ 18 O). In detail, however, dependence is not always same, and different natural processes can define distinct slopes three-isotope diagrams. These are subtle, but improvements analytical capabilities now allow precise measurement these effects make it possible to draw inferences about caused them reaction kinetics...

10.1146/annurev-earth-060115-012157 article EN Annual Review of Earth and Planetary Sciences 2016-05-24

Carbonaceous meteorites are thought to be fragments of C-type (carbonaceous) asteroids. Samples the asteroid (162173) Ryugu were retrieved by Hayabusa2 spacecraft. We measured mineralogy and bulk chemical isotopic compositions samples. The samples mainly composed materials similar those carbonaceous chondrite meteorites, particularly CI (Ivuna-type) group. consist predominantly minerals formed in aqueous fluid on a parent planetesimal. primary altered fluids at temperature 37° ± 10°C, about...

10.1126/science.abn7850 article EN Science 2022-06-09

Research Article| January 01, 2017 Non-Traditional Stable Isotopes: Retrospective and Prospective Fang-Zhen Teng; Teng Isotope Laboratory, Department of Earth Space Sciences, University Washington, Seattle WA 98195, USA, fteng@uwashington.edu Search for other works by this author on: GSW Google Scholar Nicolas Dauphas; Dauphas Origins Lab, the Geophysical Sciences Enrico Fermi Institute, The Chicago, Chicago IL 60637, dauphas@uchicago.edu James M. Watkins Oregon, Eugene OR 97403,...

10.2138/rmg.2017.82.1 article EN Reviews in Mineralogy and Geochemistry 2017-01-01

Earth exhibits a dichotomy in elevation and chemical composition between the continents ocean floor. Reconstructing when this arose is important for understanding plate tectonics started how supply of nutrients to oceans changed through time. We measured titanium isotopic shales constrain continental crust exposed weathering found that all ages have uniform composition. This can only be explained if emerged was predominantly felsic (silica-rich) since 3.5 billion years ago, requiring an...

10.1126/science.aan8086 article EN Science 2017-09-21

Abstract An Erratum has been published for this article in Mass Spectrometry Reviews 25: 831–832, 2006 . Although the processes that govern iron isotope variations nature are just beginning to be understood, multiple studies attest of virtue system solve important problems geosciences and biology. In article, we review recent advances geochemistry, cosmochemistry, biochemistry isotopes. Section 2, briefly address question nucleosynthesis Fe 3, describe different methods purifying analyzing...

10.1002/mas.20078 article EN Mass Spectrometry Reviews 2006-02-04

Archean rocks may provide a record of early Earth environments. However, such have often been metamorphosed by high pressure and temperature, which can overprint the signatures their original formation. Here, we show that banded from Isua, Akilia, Innersuartuut, Greenland, are enriched in heavy iron isotopes 0.1 to 0.5 per mil atomic mass unit relative igneous worldwide. The observed enrichments compatible with transport, oxidation, subsequent precipitation ferrous emanating hydrothermal...

10.1126/science.1104639 article EN Science 2004-12-16

10.1016/j.epsl.2012.10.011 article EN Earth and Planetary Science Letters 2012-11-21
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