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《Journal of Glaciology and Geocryology》 2003-01
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The Quaternary Glaciations and Glacier Properties in the Tanggula Range

JIAO Ke-qin, SHEN Yong-ping (Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou Gansu 730000, China)  
The occurrence and development of the Quaternary glaciers in the Tanggula Range was closely related to the amplitude and time of mountain uplift and climatic conditions. The evolution process of the glaciers in the range did not completely accord with that in other regions of the Tibetan Plateau, and the number of glaciations was not completely the same. Since the mid-Pleistocene epoch, three Pleistocene glaciations (i.e., the Kunlun Ice Age, the Penultimate Ice Age and Last Ice Age) and two Holocene glaciations (i.e., the Neoglaciation and the Little Ice Age) have occurred in the Tanggula Range. The Kunlun Ice Age occurred in the early mid-Pleistocene epoch (0^80~0^60 Ma BP), which was not only the earliest ice age, but also the largest glaciation in this range. The glaciers developed over the main ridge connected together, forming a huge ice cap with piedmont glaciers, of which the size was 16~18 times larger than that at present. The Penultimate Ice Age occurred in the late mid-Pleistocene (0^30~0^135 Ma BP), when the size of glaciers, still large ice cap with piedmont glaciers, was smaller than that in the preceding ice age but was 13~15 times larger than that at present. The Last Ice Age occurred in the late period of the late Pleistocene, which can be divided into the earlier ice age (75^0~58^0 ka BP) and the latter ice age (32^0~15^0 ka BP, with the largest scale of glaciers during 23^0~16^0 ka BP). Up to now, however, the glacial vestiges of the earlier ice age have not been found in field investigation and in the research of the Quaternary glaciers yet. Therefore, this paper discusses the latter ice age of the Last Ice Age (i.e., Last Glacial Maximum) only. During the latter ice age of the Last Ice Age, the scale of glaciers, mainly in the form of ice cap and valley glaciers, was 10 times larger than that at present. The Neoglaciation occurred after the high-temperature period of the Holocene epoch ({} 14C dating ({5 805}±173) a BP), when the {} 14C age was ({3 540}±160) a BP, and the scale of glaciers was slightly larger than that at present. The Little Ice Age occurred during the 1500s~1800s, and the scale of glaciers was close to that at present.;The scale of glaciers in the Tanggula Range has become smaller and smaller since the Kunlun Ice Age, because of the drying process in the hinterland of the Tibetan Plateau due to the uplift of the plateau. The evolution course of glacial climate type was monsoon maritime →transitional monsoon maritime-continental→monsoon continental→continental.
【Fund】: 中国科学院寒区旱区环境与工程研究所知识创新工程项目 (CACX2 10 0 17;CACX2 10 0 91);; 中国科学院知识创新重大项目(KZCX1 -10-0 6 )资助
【CateGory Index】: P343.6
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