The authors regret that figure panels 2 d and 4 a (green lines), showing the 10Be concentrations from Dome Fuji, were plotted erroneously in the original version. The correct versions of the figures (green lines) appear below for the reader's convenience. In accordance with the two corrected figure panels, we also correct two statements on page 52 in the early part of the discussion section regarding the 10Be concentrations in the Dome Fuji ice core, as follows: “The Tsambagarav 10Be concentrations exhibit a slight increase around the end of the Dalton Minimum (∼1825), while the Dome Fuji record shows a double-peak structure that extends ∼5 yr beyond the termination of the Dalton Minimum.” And also, “The concentration anomalies observed in the three records are wider than the period traditionally defined as the Maunder Minimum (1645–1715 AD) based on changes in GSNs, all showing an increase prior to 1645 AD and a high degree of variability during the ensuing Maunder Minimum period.” We emphasize that these corrections only pertain to figure panels 2d and 4a as well as the associated description of the Dome Fuji 10Be concentrations, and that they don't affect the overall discussion and conclusions presented in this study.
ASJC Scopus subject areas
- Geochemistry and Petrology
- Earth and Planetary Sciences (miscellaneous)
- Space and Planetary Science