Journal of Asian Earth Sciences 155 (2018) 124–133 Contents lists available at ScienceDirect Journal of Asian Earth Sciences journal homepage: www.elsevier.com/locate/jseaes A strengthened East Asian Summer Monsoon during Pliocene warmth: Evidence from ‘red clay’ sediments at Pianguan, northern China a,b, a,b c a a,b Shiling Yang , Zhongli Ding , Shaohua Feng , Wenying Jiang , Xiaofang Huang , a,b Licheng Guo Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China University of Chinese Academy of Sciences, Beijing 100049, China Beijing Geotechnical and Investigation Engineering Institute, Beijing 100083, China ARTICLE I NFO ABSTRACT Keywords: The Pliocene epoch (5.3–2.6 Ma) is the most recent geological interval in which atmospheric CO levels were Red clay similar to those of the present day (∼400 ppmv). This epoch is therefore considered to be the best ancient analog Loess for predicting a future anthropogenic greenhouse world. In order to determine the response of the East Asian Paleosol Summer Monsoon (EASM) rainbelt during Pliocene warmth, a 71.9 m-thick aeolian ‘red clay’ sequence at Paleomagnetism Pianguan was investigated. Rock magnetic experiments suggest that magnetite of pseudo-single domain size is East Asian Summer Monsoon the dominant remanence
Journal of Asian Earth Sciences – Elsevier
Published: Apr 15, 2018
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