High-resolution paleomagnetic secular variation and relative paleointensity records from the western Canadian Arctic: implication for Holocene stratigraphy and geomagnetic field behaviourThis article is one of a series of papers published in this Special Issue on the theme Polar Climate Stability Network.GEOTOP Contribution 2008-0024.

Author:

Barletta Francesco12345,St-Onge Guillaume12345,Channell James E.T.12345,Rochon André12345,Polyak Leonid12345,Darby Dennis12345

Affiliation:

1. Institut des sciences de la mer de Rimouski (ISMER), 310, allée des Ursulines, Rimouski, QC G5L 3A1, Canada.

2. GEOTOP Research Center, P.O. Box 8888, Succ. Centre-Ville, Montréal, QC H3C 3P8, Canada.

3. Department of Geological Sciences, P.O. Box 112120, University of Florida, Gainesville, FL 32611, USA.

4. Byrd Polar Research Center, Ohio State University, Columbus, OH 43210, USA

5. Department of Ocean, Earth, and Atmospheric Sciences, Old Dominion University, Norfolk, VA 23529, USA.

Abstract

Two piston cores recovered from the Chukchi and the Beaufort seas document Arctic Holocene geomagnetic field behaviour and highlight the potential of secular variation and relative paleointensity as a regional chronostratigraphic tool. Several centennial- to millennial-scale Holocene declination and inclination features can be correlated in both cores, with other high-resolution western North American lacustrine and volcanic paleomagnetic records and with records of changes in Earth’s dipole moment, supporting the geomagnetic origin of these features and implying that they are associated with changes in Earth’s dipole moment.

Publisher

Canadian Science Publishing

Subject

General Earth and Planetary Sciences

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