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Mid-Brunhes Event : ウィキペディア英語版 | Mid-Brunhes Event The Mid-Brunhes Event (MBE) is a climatic shift evident in a number of marine sediment and Antarctic ice cores. It corresponds to an increase in amplitude of glacial-interglacial cycles.〔EPICA community members (2004) Nature, 365, 143-147.〕 The MBE roughly corresponds to the transition between MIS 12 and MIS 11 (Termination V) about 430 kyr ago. It is characterized by a further increase of ice-volume variations with, from then to the present day, four large-amplitude 100-kyr-dominated glacial–interglacial cycles. == References ==
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Mid-Brunhes Event」の詳細全文を読む
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