Authigenic 10Be/9Be ratio signatures of the cosmogenic nuclide production linked to geomagnetic dipole moment variation since the Brunhes/Matuyama boundary

Type Article
Date 2016-11
Language English
Author(s) Simon QuentinORCID1, 2, Thouveny Nicolas1, Bourles Didier L.1, Valet Jean-Pierre2, Bassinot Franck3, 4, Menabreaz Lucie1, Guillou Valery1, Choy Sandrine1, 2, Beaufort Luc1
Affiliation(s) 1 : Aix Marseille Univ, CNRS, IRD, Coll France,CEREGE UM34, Aix En Provence, France.
2 : Univ Paris Diderot, Sorbonne Paris Cite, IPGP, CNRS,UMR 7154, Paris, France.
3 : CEA CNRS UVSQ, LSCE IPSL, LSCE, UMR 8212, Paris, France.
4 : Univ Paris Saclay, Paris, France.
Source Journal Of Geophysical Research-solid Earth (2169-9313) (Amer Geophysical Union), 2016-11 , Vol. 121 , N. 11 , P. 7716-7741
DOI 10.1002/2016JB013335
WOS© Times Cited 58
Abstract Geomagnetic dipole moment variations associated with polarity reversals and excursions are expressed by large changes of the cosmogenic nuclide beryllium-10 (10Be) production rates. Authigenic 10Be/9Be ratios (proxy of atmospheric 10Be production) from oceanic cores therefore complete the classical information derived from relative paleointensity (RPI) records. This study presents new authigenic 10Be/9Be ratio results obtained from cores MD05-2920 and MD05-2930 collected in the west equatorial Pacific Ocean. Be ratios from cores MD05-2920, MD05-2930 and MD90-0961 have been stacked and averaged. Variations of the authigenic 10Be/9Be ratio are analyzed and compared with the geomagnetic dipole low series reported from global RPI stacks. The largest 10Be overproduction episodes are related to dipole field collapses (below a threshold of 2 × 1022 Am2) associated with the Brunhes/Matuyama reversal, the Laschamp (41 ka) excursion, and the Iceland Basin event (190 ka). Other significant 10Be production peaks are correlated to geomagnetic excursions reported in literature. The record was then calibrated by using absolute dipole moment values drawn from the Geomagia and Pint paleointensity value databases. The 10Be-derived geomagnetic dipole moment record, independent from sedimentary paleomagnetic data, covers the Brunhes-Matuyama transition and the whole Brunhes Chron. It provides new and complementary data on the amplitude and timing of millennial-scale geomagnetic dipole moment variations and particularly on dipole moment collapses triggering polarity instabilities.
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Simon Quentin, Thouveny Nicolas, Bourles Didier L., Valet Jean-Pierre, Bassinot Franck, Menabreaz Lucie, Guillou Valery, Choy Sandrine, Beaufort Luc (2016). Authigenic 10Be/9Be ratio signatures of the cosmogenic nuclide production linked to geomagnetic dipole moment variation since the Brunhes/Matuyama boundary. Journal Of Geophysical Research-solid Earth, 121(11), 7716-7741. Publisher's official version : https://doi.org/10.1002/2016JB013335 , Open Access version : https://archimer.ifremer.fr/doc/00358/46910/