斜度驱动第四纪冰期-间冰期转换——来自中国黄土的证据  

OBLIQUITY PACING OF DEGLACIATIONS IN THE PLEISTOCENE：EVIDENCE FROM THE CHINESE LOESS DEPOSITS

作　　者：李涛 李高军 Li Tao;Li Gaojun(Key Laboratory of Surficial Geochemistry,Ministry of Education School of Earth Sciences and Engineering,Nanjing University,Nanjing 210023,Jiangsu)

机构地区：[1]南京大学地球科学与工程学院,表生地球化学教育部重点实验室,江苏南京210023

出　　处：《第四纪研究》2018年第5期1111-1119,共9页Quaternary Sciences

基　　金：国家自然科学基金项目（批准号：41422205和41730101）资助

摘　　要：第四纪气候冰期-间冰期旋回与地球轨道周期性变化之间的关系是古气候研究的重点。文章利用中国黄土沉积的粒度和次生碳酸盐微量元素记录，在同一剖面中同时获得了冰量信息和地球轨道斜度信息。黄土的平均粒径反映了冬季风的强度从而指示了北半球高纬冰盖的变化，而次生碳酸盐（生物微钙体）的Sr/Ca比值记录了东亚夏季降水的变化，反映了斜度对东亚夏季风的控制作用。通过分析冰消期时粒度快速变化所处的夏季降水指示的斜度变化的相对位置，发现过去1.5 Ma以来的冰消期总在地球轨道处于较高斜度时发生，从而验证了斜度对第四纪冰期-间冰期旋回的驱动作用。Investigating the causal link between Earth＇s orbital parameters and Quaternary glacial-interglacial cycles remains one of the most important branches of paleoclimatic research. This is largely due to the discrepancies between the intensity of summer insolation in the precession band and Pleistocene glacial cycles in the obliquity and eccentricity bands. In this study, we have reconstructed proxy records that document both the Northern Hemisphere ice-sheet volume and the obliquity of Earth from the same loess-paleosol profile on the central Chinese Loess Plateau over the last 1.5 million years, enabling us to explore the potential connections between them. Loess-paleosol samples were collected every 5 cm at Xifeng（35°45＇N, 107°47＇E） and Zhenyuan（35°43＇N, 107°12＇E） sections, which can be well correlated to each other using magnetic susceptibility stratigraphy. Secondary carbonate samples（microcodium） were then picked out from the 〉75 μm fraction of the loess-paleosol samples. Previous studies have suggested that microcodium Sr/Ca ratio can be used as a regional measure of summer precipitation. The reconstructed paleo-precipitation records at Xifeng and Zhenyuan show consistent variations over the last 480 thousand years, confirming the reliability of microcodium Sr/Ca as a summer precipitation proxy. The summer precipitation records show a persistent obliquity cycle of the 41-ka over the last 1.5 million years, which can be attributed to the gradient of boreal summer insolation that modulates the thermal contrast between the Asian continent and surrounding oceans and thus the strength of East Asian summer monsoon. In the loess deposits, the position of terminations in the record can be precisely constrained by rapid shift in grain size and magnetic susceptibility. We find that the mid-points of the terminations are always associated with the peak precipitation. By tuning the summer precipitation to the obliquity periodicity, i.e., matching the peaks and valleys of the precipitation to

关 键 词：中国黄土 生物微钙体 东亚夏季风 斜度 冰消期 

分 类 号：P512.6[天文地球—地质学] P532