Research Article| March 01, 2006 A penultimate glacial monsoon record from Hulu Cave and two-phase glacial terminations Hai Cheng; Hai Cheng 1Department of Geology and Geophysics, University of Minnesota, Minneapolis, Minnesota 55455, USA, and College of Geography Science, Nanjing Normal University, Nanjing 210097, China Search for other works by this author on: GSW Google Scholar R. Lawrence Edwards; R. Lawrence Edwards 2Department of Geology and Geophysics, University of Minnesota, Minneapolis, Minnesota 55455, USA Search for other works by this author on: GSW Google Scholar Yongjin Wang; Yongjin Wang 3College of Geography Science, Nanjing Normal University, Nanjing 210097, China Search for other works by this author on: GSW Google Scholar Xinggong Kong; Xinggong Kong 3College of Geography Science, Nanjing Normal University, Nanjing 210097, China Search for other works by this author on: GSW Google Scholar Yanfang Ming; Yanfang Ming 3College of Geography Science, Nanjing Normal University, Nanjing 210097, China Search for other works by this author on: GSW Google Scholar Megan J. Kelly; Megan J. Kelly 4Department of Geology and Geophysics, University of Minnesota, Minneapolis, Minnesota 55455, USA Search for other works by this author on: GSW Google Scholar Xianfeng Wang; Xianfeng Wang 4Department of Geology and Geophysics, University of Minnesota, Minneapolis, Minnesota 55455, USA Search for other works by this author on: GSW Google Scholar Christina D. Gallup; Christina D. Gallup 5Department of Geological Sciences and Large Lakes Observatory, University of Minnesota Duluth, Duluth, Minnesota 55812, USA Search for other works by this author on: GSW Google Scholar Weiguo Liu Weiguo Liu 6Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710054, China Search for other works by this author on: GSW Google Scholar Author and Article Information Hai Cheng 1Department of Geology and Geophysics, University of Minnesota, Minneapolis, Minnesota 55455, USA, and College of Geography Science, Nanjing Normal University, Nanjing 210097, China R. Lawrence Edwards 2Department of Geology and Geophysics, University of Minnesota, Minneapolis, Minnesota 55455, USA Yongjin Wang 3College of Geography Science, Nanjing Normal University, Nanjing 210097, China Xinggong Kong 3College of Geography Science, Nanjing Normal University, Nanjing 210097, China Yanfang Ming 3College of Geography Science, Nanjing Normal University, Nanjing 210097, China Megan J. Kelly 4Department of Geology and Geophysics, University of Minnesota, Minneapolis, Minnesota 55455, USA Xianfeng Wang 4Department of Geology and Geophysics, University of Minnesota, Minneapolis, Minnesota 55455, USA Christina D. Gallup 5Department of Geological Sciences and Large Lakes Observatory, University of Minnesota Duluth, Duluth, Minnesota 55812, USA Weiguo Liu 6Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710054, China Publisher: Geological Society of America Received: 10 Oct 2005 Revision Received: 14 Nov 2005 Accepted: 16 Nov 2005 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (2006) 34 (3): 217–220. https://doi.org/10.1130/G22289.1 Article history Received: 10 Oct 2005 Revision Received: 14 Nov 2005 Accepted: 16 Nov 2005 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Hai Cheng, R. Lawrence Edwards, Yongjin Wang, Xinggong Kong, Yanfang Ming, Megan J. Kelly, Xianfeng Wang, Christina D. Gallup, Weiguo Liu; A penultimate glacial monsoon record from Hulu Cave and two-phase glacial terminations. Geology 2006;; 34 (3): 217–220. doi: https://doi.org/10.1130/G22289.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Oxygen isotope records of three stalagmites from Hulu Cave, China, extend the previous high-resolution absolute-dated Hulu Asian Monsoon record from the last to the penultimate glacial and deglacial periods. The penultimate glacial monsoon broadly follows orbitally induced insolation variations and is punctuated by at least 16 millennial-scale events. We confirm a Weak Monsoon Interval between 135.5 ± 1.0 and 129.0 ± 1.0 ka, prior to the abrupt increase in monsoon intensity at Asian Monsoon Termination II. Based on correlations with both marine ice-rafted debris and atmospheric CH4 records, we demonstrate that most of marine Termination II, the full rise in Antarctic temperature and atmospheric CO2, and much of the rise in CH4 occurred within the Weak Monsoon Interval, when the high northern latitudes were probably cold. From these relationships and similar relationships observed for Termination I, we identify a two-phase glacial termination process that was probably driven by orbital forcing in both hemispheres, affecting the atmospheric hydrological cycle, and combined with ice sheet dynamics. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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