Abstract
Abstract Several recent studies confirmed that 10Be records obtained from lake and marine sediments show significant climatic signals [1] , [2] , [3] , [4] . We have recently investigated 10Be and 9Be in sedimentary core materials obtained from the East Sea [5] . The results indicate that a combination of the 10Be and 9Be data provides significant information to enhance our understanding of marine environmental changes for the East Sea during the last two glacial–interglacial periods. The range of the 10Be concentrations of the sediments is consistent with previously published 10Be concentrations from the other regions [2] , [3] , [4] . The 10Be records from the East Sea tend to show significant global climate change during the warm periods of Holocene and Eemian. The results of our study deliver a new and deeper insight into marine environmental changes and paleoclimate records in the deep sea areas surrounding Korea.
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