会议专题

VEGETATION AND CLIMATE CHANGES IN CENTRAL ASIA DURING OVER THE LAST 28,000 YRS: A HIGH-RESOLUTION POLLEN RECORD FROM VALIKHANOV SECTION, KAZAKHSTAN

A high-resolution pollen-based bioclimatic reconstruction from Valikhanov section in Kazakhstan, supported by 6 AMS dates reveals vegetation and climate change history during last glaciations and Holocene.The vegetation probably was Artemisia arid steppe during ~28,000 - ~18,000 14C yr BP., then turned to be Artemisia steppe during ~18,000 - ~ 10,000 14C yr BP, an Atermisia-Chenopodiaceae desert steppe during ~10,000 - ~5,000 14C yr BP and a Chenopodiaceae-Artemisia steppe after ~5,000 14C yr BP in this region.Climate is cold and slightly wet during 28,000-10,000 14C yr BP., dry and mild during 10,000-5,000 14C yr BP., wet after ~5,000 14C yr BP in this region.Climate in the Central Asian domain was constantly wetter than that in the East Asian domain during MIS2.The Central Asian domain experienced a wetter climate in late Holocene whereas the East Asian domain expereinced a wetter climate in early Holocene.Climate in the Central Asian domain was constantly wetter than that in the East Asian domain during MIS2.The Central Asian domain experienced a wetter climate in late Holocene whereas the East Asian domain expereinced a wetter climate in early Holocene.

pollen MIS2 Holocene Central Asia climate

CHANGQING HUANG KAM-BIU LIU ZHAODONG FENG MING RAN

MOE Key Laboratory of West Chinas Environmental System,Lanzhou University,Lanzhou,Gansu,China Depart Department of Oceanography and Coastal Sciences,School of the Coast and Environment,Louisiana State MOE Key Laboratory of West Chinas Environmental System,Lanzhou University,Lanzhou,Gansu,China

国际会议

2011 3rd International Conference on Computer Technology and Development(2011第三届计算机技术与发展国际会议 ICCTD2011)

成都

英文

787-791

2011-11-25(万方平台首次上网日期,不代表论文的发表时间)