Journal of Asian Earth Sciences 156 (2018) 174–179 Contents lists available at ScienceDirect Journal of Asian Earth Sciences journal homepage: www.elsevier.com/locate/jseaes Full length article Peat δ C -recorded wetting trend during the past 8000 years in the celluose southern Altai Mountains, northern Xinjiang, NW China ⁎ ⁎ a,b, c, a,b d c a Dongliang Zhang , Zhaodong Feng , Yunpeng Yang , Bo Lan , Min Ran , Guijin Mu Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, 818 Beijing South Road, Urumqi 830011, China University of Chinese Academy of Sciences, 19A Yuquan Road, Beijing 100049, China College of Environment and Planning, Henan University, Jinming Street, Kaifeng, Henan 475004, China School of Environmental and Chemical Engineering, Chongqing Three Gorges University, Shalong Road, Chongqing 404000, China ARTICLE I NFO ABSTRACT Keywords: There have been large discrepancies in the proposed mechanisms accounting for the wetting trend since Altai Mountains ∼8.0 cal. kyr BP in the Altai Mountains and the surrounding areas. To validate or invalidate the widely reported Holocene wetting trend, we obtained a carbon isotope of cellulose (δ C )-recorded warm-season moisture history celluose Moisture change 13 from a Narenxia (NRX) peat core in the southern Altai Mountains,
Journal of Asian Earth Sciences – Elsevier
Published: May 1, 2018
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