Towards an Integrated Geomagnetic Polarity Reversal Timescale for the Pleistocene

Tiffany Rivera, Michael Storey, Klaudia Kuiper, Heiko Palike

    Publikation: KonferencebidragKonferenceabstrakt til konferenceForskning

    Resumé

    The development of the geomagnetic polarity timescale (GPTS) in the mid 20th century led to the greater understanding of seafloor spreading and plate tectonics (Heirtzler et al., 1968). Over 40 years later, the GPTS continues to be refined, particularly in terms of integrating multiple dating techniques to improve precision of such events, or to resolve the duration of geomagnetic transitions. Recent advancements in integrating astronomical and 40Ar/39Ar dating techniques, and improving upon the precision of neutron fluence monitors, necessitate re-evaluation of the accuracy and precision of various geologic events. Here, we review the ages of three Pleistocene geomagnetic polarity reversals: the Matuyama-Brunhes (ca. 0.78 Ma), the Cobb Mountain (ca. 1.2 Ma), and the Reunion (ca. 2.1 Ma) events. High-precision astronomically calibrated 40Ar/39Ar ages have been obtained via a Noblesse multi-collector noble gas mass spectrometer on volcanic and other datable materials related to each event. The ages were derived by single- or multi-crystal total fusion and/or step heating experiments, using the astronomically calibrated Fish Canyon sanidine and/or the astronomically tuned A1 sanidine as monitor minerals. Each of these ages is then compared to independent astronomical ages for the events in order to define tie-points for constructing a Pleistocene a multi-chronometer GPTS. Although only three reversals are addressed here, the methodology applied shows promise to refining short-lived excursions to enable further understanding of the wavering magnetic field.

    The research leading to these results has received funding from the European Community's Seventh Framework Programme [FP7/2007-2013] under grant agreement no. 215458.
    OriginalsprogEngelsk
    Publikationsdato2011
    StatusUdgivet - 2011
    BegivenhedAGU Fall Meeting 2011 - San Francisco, USA
    Varighed: 9 sep. 20119 sep. 2011
    http://sites.agu.org/fallmeeting/

    Konference

    KonferenceAGU Fall Meeting 2011
    LandUSA
    BySan Francisco
    Periode09/09/201109/09/2011
    Internetadresse

    Citer dette

    Rivera, T., Storey, M., Kuiper, K., & Palike, H. (2011). Towards an Integrated Geomagnetic Polarity Reversal Timescale for the Pleistocene. Abstract fra AGU Fall Meeting 2011, San Francisco, USA.
    Rivera, Tiffany ; Storey, Michael ; Kuiper, Klaudia ; Palike, Heiko. / Towards an Integrated Geomagnetic Polarity Reversal Timescale for the Pleistocene. Abstract fra AGU Fall Meeting 2011, San Francisco, USA.
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    Rivera, T, Storey, M, Kuiper, K & Palike, H 2011, 'Towards an Integrated Geomagnetic Polarity Reversal Timescale for the Pleistocene' AGU Fall Meeting 2011, San Francisco, USA, 09/09/2011 - 09/09/2011, .

    Towards an Integrated Geomagnetic Polarity Reversal Timescale for the Pleistocene. / Rivera, Tiffany; Storey, Michael; Kuiper, Klaudia; Palike, Heiko.

    2011. Abstract fra AGU Fall Meeting 2011, San Francisco, USA.

    Publikation: KonferencebidragKonferenceabstrakt til konferenceForskning

    TY - ABST

    T1 - Towards an Integrated Geomagnetic Polarity Reversal Timescale for the Pleistocene

    AU - Rivera, Tiffany

    AU - Storey, Michael

    AU - Kuiper, Klaudia

    AU - Palike, Heiko

    PY - 2011

    Y1 - 2011

    N2 - The development of the geomagnetic polarity timescale (GPTS) in the mid 20th century led to the greater understanding of seafloor spreading and plate tectonics (Heirtzler et al., 1968). Over 40 years later, the GPTS continues to be refined, particularly in terms of integrating multiple dating techniques to improve precision of such events, or to resolve the duration of geomagnetic transitions. Recent advancements in integrating astronomical and 40Ar/39Ar dating techniques, and improving upon the precision of neutron fluence monitors, necessitate re-evaluation of the accuracy and precision of various geologic events. Here, we review the ages of three Pleistocene geomagnetic polarity reversals: the Matuyama-Brunhes (ca. 0.78 Ma), the Cobb Mountain (ca. 1.2 Ma), and the Reunion (ca. 2.1 Ma) events. High-precision astronomically calibrated 40Ar/39Ar ages have been obtained via a Noblesse multi-collector noble gas mass spectrometer on volcanic and other datable materials related to each event. The ages were derived by single- or multi-crystal total fusion and/or step heating experiments, using the astronomically calibrated Fish Canyon sanidine and/or the astronomically tuned A1 sanidine as monitor minerals. Each of these ages is then compared to independent astronomical ages for the events in order to define tie-points for constructing a Pleistocene a multi-chronometer GPTS. Although only three reversals are addressed here, the methodology applied shows promise to refining short-lived excursions to enable further understanding of the wavering magnetic field.The research leading to these results has received funding from the European Community's Seventh Framework Programme [FP7/2007-2013] under grant agreement no. 215458.

    AB - The development of the geomagnetic polarity timescale (GPTS) in the mid 20th century led to the greater understanding of seafloor spreading and plate tectonics (Heirtzler et al., 1968). Over 40 years later, the GPTS continues to be refined, particularly in terms of integrating multiple dating techniques to improve precision of such events, or to resolve the duration of geomagnetic transitions. Recent advancements in integrating astronomical and 40Ar/39Ar dating techniques, and improving upon the precision of neutron fluence monitors, necessitate re-evaluation of the accuracy and precision of various geologic events. Here, we review the ages of three Pleistocene geomagnetic polarity reversals: the Matuyama-Brunhes (ca. 0.78 Ma), the Cobb Mountain (ca. 1.2 Ma), and the Reunion (ca. 2.1 Ma) events. High-precision astronomically calibrated 40Ar/39Ar ages have been obtained via a Noblesse multi-collector noble gas mass spectrometer on volcanic and other datable materials related to each event. The ages were derived by single- or multi-crystal total fusion and/or step heating experiments, using the astronomically calibrated Fish Canyon sanidine and/or the astronomically tuned A1 sanidine as monitor minerals. Each of these ages is then compared to independent astronomical ages for the events in order to define tie-points for constructing a Pleistocene a multi-chronometer GPTS. Although only three reversals are addressed here, the methodology applied shows promise to refining short-lived excursions to enable further understanding of the wavering magnetic field.The research leading to these results has received funding from the European Community's Seventh Framework Programme [FP7/2007-2013] under grant agreement no. 215458.

    M3 - Conference abstract for conference

    ER -

    Rivera T, Storey M, Kuiper K, Palike H. Towards an Integrated Geomagnetic Polarity Reversal Timescale for the Pleistocene. 2011. Abstract fra AGU Fall Meeting 2011, San Francisco, USA.