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DOI:10.16418/j.issn.1000-3045.20200316001
中国科学院院刊:2020,35(4):475-483
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第四纪冰冻圈——全球变化长尺度研究
周尚哲1, 赵井东2, 王杰3, 许刘兵1, 崔建新4, 欧先交5, 谢金明3
(1.华南师范大学 广州 510631;2.中国科学院西北生态环境资源研究院 兰州 730000;3.兰州大学 兰州 730000;4.陕西师范大学 西安 710119;5.嘉应学院 梅州 514015)
Quaternary Cryosphere—Study on Global Change in Long Terms
ZHOU Shangzhe1, ZHAO Jingdong2, WANG Jie3, XU Liubing1, CUI Jianxin4, OU Xianjiao5, XIE Jinming3
(1.South China Normal University, Guangzhou 510631, China;2.Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China;3.Lanzhou University, Lanzhou 730000, China;4.Shaanxi Normal University, Xi'an 710119, China;5.Jiaying College, Meizhou 514015, China)
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投稿时间:2020-04-02    
中文摘要: 第四纪是以大冰期为标志的最新地质历史时期。这个大冰期的基本特征是轨道尺度的冰期-间冰期交替及亚轨道尺度的冰阶-间冰阶变化。现在是比较温暖的间冰期,冰川只覆盖陆地面积的10%。而在冰期最盛时,冰川覆盖全球陆地面积的30%,冻土扩展,气候干旱,风沙盛行,海平面降低130-150 m,植被向低纬度收缩10o以上,垂直带谱下移1 000 m以上。冰期天文理论成功解释了冰期-间冰期循环周期问题,但还存在诸多挑战。第四纪也是古人类向现代人发展的时期。古人类诞生于东非,约200万年前曾向欧亚大陆有限扩散,但一直到了末次间冰期才大规模扩散;尤其在随后的末次冰期中,人类更是借助于大陆桥扩散到美洲和澳洲。新仙女木事件后,气候变暖,人类进入细石器时代并逐渐过渡到农业社会。工业革命开始,人类发展深刻影响到了地球的自然进程,导致全球变暖,预示着一个"人类纪"的到来。
中文关键词: 第四纪  冰冻圈演变  人类发展
Abstract:The Quaternary is marked by the Great Ice Age. The basic characteristics of this great ice age are the alternating of glacialinterglacial period in orbital scale and changes of stadial-interstadial in suborbital scale. Present is a relatively warm interglacial period, with glaciers covering only 10% of the land area. At the glacial maximum, glaciers covered about 30% of the global land area, permafrost spread, climate was dry with prevalence of dust, sea level reduced 130-150 m, vegetation contracted to low latitudes more than 10°, and the vertical band spectrum moved down more than 1 000 m. The astronomic theory of ice ages has successfully explained the glacial-interglacial cycles, however, there are still a lot of problems to need studies in detail. Quaternary is also the period of ancient human development. Ancient human was born in East Africa and spread to Eurasia only on a limited scale about 2 Ma ago. The spread on a large scale started during the last interglacial and spread to America and Australia by means of land bridges during Last Glaciation Maximum (LGM). After the younger Dryas, the climate became warm and the human entered the Neolithic Period and gradually transited to the agricultural society. After the Industrial Revolution, human development has been profoundly affecting the natural process of the Earth, leading to global warming, heralding the arrival of an "Anthropocene".
keywords: Quaternary  cryospheric change  human development
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周尚哲 华南师范大学 广州 510631 
赵井东 中国科学院西北生态环境资源研究院 兰州 730000 
王杰 兰州大学 兰州 730000 
许刘兵 华南师范大学 广州 510631 
崔建新 陕西师范大学 西安 710119 
欧先交 嘉应学院 梅州 514015 
谢金明 兰州大学 兰州 730000 
Author NameAffiliation
ZHOU Shangzhe South China Normal University, Guangzhou 510631, China 
ZHAO Jingdong Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China 
WANG Jie Lanzhou University, Lanzhou 730000, China 
XU Liubing South China Normal University, Guangzhou 510631, China 
CUI Jianxin Shaanxi Normal University, Xi'an 710119, China 
OU Xianjiao Jiaying College, Meizhou 514015, China 
XIE Jinming Lanzhou University, Lanzhou 730000, China 
引用文本:
周尚哲,赵井东,王杰,许刘兵,崔建新,欧先交,谢金明.第四纪冰冻圈——全球变化长尺度研究[J].中国科学院院刊,2020,35(4):475-483.
ZHOU Shangzhe,ZHAO Jingdong,WANG Jie,XU Liubing,CUI Jianxin,OU Xianjiao,XIE Jinming.Quaternary Cryosphere—Study on Global Change in Long Terms[J].Bulletin of Chinese Academy of Sciences,2020,35(4):475-483.
 
 
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