Climate change response to astronomical forcing during the Oligocene-Miocene transition in the equat

• 作 者: ZOU ZhuoYan HUANG ChunJu LI Mi
• 机 构: StateKeyLaboratoryofBiogeologyandEnvironmentalGeology,DepartmentofEarthandPlanetarySciences,Departme
• 出 处: 中国科学：地球科学英文版
• 发表日期: 2016年8期
• 关键词: Late Oligocene-Early Miocene ODP Site 926 LIGHTNESS Astronomical time scale Astr
• 基金项目: supported by the National Natural Science Foundation of China （Grant No. 41322013）,the Program of Introducing Talents of Discipline to Universities （Grant No. B14031）,the National Basic Research Progr

The Oligocene-Miocene transition period was characterized by a decrease in global CO2 levels, expansion of polar ice sheet, fall in global sea-level, etc. However, the reasons for, and mechanisms of, this global, extreme-cold climate change event（Mi-1） st