Ice core record of 10Be over the past millennium from Dome Fuji, Antarctica:: A new proxy record of past solar activity and a powerful tool for stratigraphic dating

The cosmogenic nuclide Be-10 was analyzed by using accelerator mass spectrometry on an ice core drilled at the Dome Fuji station, inland Antarctica, for 700-1900yr CE. The measured concentration of Be-10 in the Dome Fuji ice core and the derived Be-10 flux show similar fluctuations, with both increasing at known solar-activity minima over the last millennium in agreement with earlier observations of Be-10 and C-14. Based on the similar nature of the Be-10 flux to the reconstructed C-14 production rate patterns, a Be-10-C-14 correlation age model for the Dome Fuji ice core was successfully constructed. This age model agrees well with the initial version of the tephrochronology of the core. The Be-10-flux record contains information on variability in the amount of cosmic radiation incident on the atmosphere, which is mainly attributable to high-frequency change in solar activity and low-frequency background intensity adjustment of the geomagnetic field. High-resolution Be-10 analyses of the Dome Fuji ice cores promise to provide potentially important information on the history of cosmic radiation intensity over the past several hundred thousand years. (c) 2008 Elsevier Ltd. All rights reserved.