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    Search for Supernova-Produced Fe60 in a Marine Sediment

    C. Fitoussi1, G. M. Raisbeck1, K. Knie2,5, G. Korschinek2, T. Faestermann2, S. Goriely3, D. Lunney1, M. Poutivtsev2, G. Rugel2 et al.

    C. Waelbroeck4 and A. Wallner5

    • 1Centre de Spectrométrie Nucléaire et de Spectrométrie de Masse (CSNSM) IN2P3/CNRS, Université Paris Sud, Bâtiment 108, 91405 Orsay, France
    • 2Fakultät für Physik, Technische Universität München, James-Franck-Straße 1, 85747 Garching, Germany
    • 3Institut d’Astronomie et d’Astrophysique, C.P. 226, Université Libre de Bruxelles, Boulevard Du Triomphe, B-1050 Brussels, Belgium
    • 4Laboratoire des Sciences du Climat et de l’Environnement, Domaine du CNRS, 91198 Gif-sur-Yvette, France
    • 5VERA Laboratory, Fakultät für Physik, Universität Wien, Währinger Straße 17, A-1090 Vienna, Austria

    Phys. Rev. Lett. 101, 121101 – Published 19 September, 2008

    DOI: https://doi.org/10.1103/PhysRevLett.101.121101

    Abstract

    An Fe60 peak in a deep-sea FeMn crust has been interpreted as due to the signature left by the ejecta of a supernova explosion close to the solar system 2.8±0.4  Myr ago [Knie et al., Phys. Rev. Lett. 93, 171103 (2004)]. In an attempt to confirm this interpretation with better time resolution and obtain a more direct flux estimate, we measured Fe60 concentrations along a dated marine sediment. We find no Fe60 peak at the expected level from 1.7 to 3.2 Myr ago. Possible causes for the discrepancy are discussed.

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