|Table of Contents|

New advance on Quaternary glacier in Northeast China: remains examination, new discovery and ice epoch model(PDF)

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:
2012年第01期
Page:
55-65
Research Field:
水资源与环境
Publishing date:

Info

Title:
New advance on Quaternary glacier in Northeast China: remains examination, new discovery and ice epoch model
Author(s):
SUN Guang-you1; 2; 3;  WANG Hai-xia4;  FAN Yu5
1. Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun 130012, Jilin, China; 2. School of Environment and Resources, Jilin University, Changchun 130021, Jilin, China; 3. School of Sciences, Harbin University, Harbin 150086, Heilongjiang, China; 4. School of Urban and Environmental Sciences, Northeast Normal University, Changchun 130024, Jilin, China; 5. School of Tourism and Geography Science, Jilin Normal University, Siping 136000, Jilin, China
Keywords:
Quaternary glacier;  remain;  ice epoch model;  environmental evolution;  Changbai Mountains;  Da Hinggan Mountains;  Xiao Hinggan Mountains
PACS:
P343.6
DOI:
-
Abstract:
It is a problem whether Quaternary glacier developed in Northeast China, and the area, property and ice epoch were debatable. Based on the remains examination of Quaternary glacier in Changbai Mountains and Da Hinggan Mountains, Quaternary glaciers were investigated by the methods of the 3S technologies with geographic information science(GIS), remote sensing(RS)and global positioning system(GPS), drilling and mapping, pollen analysis, fineness and osmotic permeability analysis and 14C dating. The remains of Quaternary glacier including glacier valley and boulder clay were discovered in Changbai Mountains and Da Hinggan Mountains; therefore, Quaternary glacier and its ice epoch had been affirmed further in the regions. In Xiao Hinggan Mountains, ice erosion wall discovered for the first time showed that Quaternary glacier developed in the region. There were four ice epochs and three interglacial epochs in Changbai Mountains and Da Hinggan Mountains, respectively, and at least one ice epoch in Xiao Hinggan Mountains. The sequence of ice epoch, which could compare with the international, had been structured in Northeast China. The environmental evolution model of Quaternary glacier was reconstructed: the climate was cold and dry in the early stage of Early Pleistocene; it was worm and wet in the middle of Early Pleistocene; it was cold and wet in the early of Middle Pleistocene; it was cold and a bit wet in the early of Late Pleistocene, worm in the middle, and cold and dry in the late.

References:

[1] 鹿野忠雄.朝鲜东北部山地的冰河地形[J].地理学评论,1937,13:1126-1145. TADAO Kano.North Korea's northeast mountain glacier landform[J].Geography Comment,1937,13:1126-1145.(in Chinese)
[2] 严钦尚.大兴安岭附近的冰川地形[J].地质学报,1952,32(1):1-15. YAN Qin-shang.The glacier landform in Da Hinggan Mountains[J].Journal of Geology,1952,32(1):1-15.(in Chinese)
[3] 杨怀仁.诺敏河流域的冰川地形[J].南京大学学报,1955(1):95-120. YANG Huai-ren.The glacier landform in the Nuomin River Basin[J].Journal of Nanjing University,1955(1):95-120.(in Chinese)
[4] 俞建章,谢宇平,刘 翰.大兴安岭的第四纪冰川[C]∥中国第四纪冰川遗迹调查组.中国第四纪冰川遗迹研究文集.北京:科学出版社,1964:85-100. YU Jian-zhang,XIE Yu-ping,LIU Han.Quaternary glacial of Da Hinggan Mountains[C]∥The Study Group of Quaternary Glacial Relic in China.The Symposium on Quaternary Glacial Relic.Beijing:Science Press,1964:85-100.(in Chinese)
[5] 刘长安,傅景惠,聂景春.白头山一带第四纪冰川遗迹[R].长春:吉林省地质局,1963. LIU Chang-an,FU Jing-hui,NIE Jing-chun.Quaternary glacial relic around Baitou Mountains[R].Changchun:Geology Bureau of Jilin Province,1963.(in Chinese)
[6] 孙建中.吉林省第四纪冰期的划分[J].地质学报,1982,56(2):174-186. SUN Jian-zhong.The Quaternary glacial period division of Jilin Province[J].Aata Geologica Sinica,1982,56(2):174-186.(in Chinese)
[7] 孙建中,王淑英,王雨灼,等.东北末次冰期的古环境[J].中国第四纪研究,1985,6(1):82-89. SUN Jian-zhong,WANG Shu-ying,WANG Yu-zhuo et al.The paleoenvironment of the Last Glaciation of Northeast China[J].Chinese Quaternary Research,1985,6(1):82-89.(in Chinese)
[8] 裘善文.长白山古冰川、冰缘地貌的研究[J].第四纪研究,1990,10(2):137-145. QIU Shan-wen.A study on the Paleo-glacial and periglacial landforms in Changbai Mountains[J].Quaternary Sciences,1990,10(2):137-145.(in Chinese)
[9] 肖荣寰,胡俭彬.东北地貌的区域分异[C]∥中国地理学会地貌与第四纪专业委员会.地貌及第四纪研究进展.北京:科学出版社,1991:267. XIAO Rong-huan,HU Jian-bin.The region differentiation of landforms in Northeast China[C]∥Committees of Landform and Quaternary of Chinese Geographical Society.The Development of Geomorphology and Quaternary Research.Beijing:Science Press,1991:267.(in Chinese)
[10] 施雅风,崔之久,李吉均,等.中国东部第四纪冰川与环境问题[M].北京:科学出版社,1989. SHI Ya-feng,CUI Zhi-jiu,LI Ji-jun,et al.The questions of Quaternary glacial and environment in East China[M].Beijing:Science Press,1989.(in Chinese)
[11] 李吉均.中国第四纪冰川研究的展望[C]∥中国地理学会冰川冻土分会,中国科学院兰州冰川冻土研究所.第四届全国冰川冻土学术会议论文选集.北京:科学出版社,1990:9-14. LI Ji-jun.The outlook on the Quaternary glacial research of China[C]∥Committees of Glacial Frozen Soil of Chinese Geographical Society,Lanzhou Institute of Glaciology and Cryopedology of Chinese Academy of Sciences.The Symposium for the 4th Glacial and Frozen Soil Conference.Beijing:Science Press,1990:9-14.(in Chinese)
[12] 刘嘉麒,王松山.长白山火山与天池的形成时代[J].科学通报,1982,27(21):1312-1315. LIU Jia-qi,WANG Song-shan.The formation age of the Changbai Mountains volcano and Tianchi Lake[J].Chinese Science Bulletin,1982,27(21):1312-1315.(in Chinese)
[13] 孙广友,富德义,宋海远,等.长白山火山期、玄武岩建造及火山地貌的形成[C]∥宋海远.长白山火山研究.延边:延边大学出版社,1990:12-27. SUN Guang-you,FU De-yi,SONG Hai-yuan,et al.The study on volcano epoch and basalt and volcano landform[C]∥SONG Hai-yuan.The Study on Volcano of Changbai Mountains.Yan-bian:Yanbian University Press,1990:12-27.(in Chinese)
[14] 刘忠杰.白头山地区地貌特征及其营力作用[C]∥宋海远.长白山火山研究.延边:延边大学出版社,1990:104-119. LIU Zhong-jie.Landform and effect of the Baitou Mountains[C]∥SONG Hai-yuan.The Study on Volcano of Changbai Mountains.Yanbian:Yanbian University Press,1990:104-119.(in Chinese)
[15] 张 威,牛云博,闫 玲,等.吉林长白山地晚更新世冰川作用[J].科学通报,2008,53(15):1825-1834. ZHANG Wei,NIU Yun-bo,YAN Ling,et al.The Late Plei-stocene glacier in the Changbai Mountains of Jilin Province[J].Chinese Science Bulletin,2008,53(15):1825-1834.(in Chinese)
[16] 孙广友.鸭绿江上游河谷地貌结构与发育史的初步探讨[C]∥宋海远.长白山火山研究.延边:延边大学出版社,1990:94-95. SUN Guang-you.A preliminary research on the landform construction and evolution of the valley upstream of Yalujiang River[C]∥SONG Hai-yuan.The Study on Volcano of Changbai Mountains.Yanbian:Yanbian University Press,1990:94-95.(in Chinese)
[17] 周廷儒.中国第四纪古地理环境的分异[J].地理科学,1983,3(3):191-206. ZHOU Ting-ru.Environment differentiation of the Quaternary geographical in China[J].Scientia Geographica Sinica,1983,3(3):191-206.(in Chinese)
[18] 施雅风,崔之久,李吉均,等.中国冰川与环境[M].北京:科学出版社,2000. SHI Ya-feng,CUI Zhi-jiu,LI Ji-jun,at el.The glacial and environment in China[M].Beijing:Science Press,2000.(in Chinese)
[19] 裘善文,李风华.东北“白土山冰期”沉积物成因与时代的研究[J].冰川冻土,1985,7(3):195-203. QIU Shan-wen,LI Feng-hua.A research on the formation and age of sediments of Baitushan Ice Age in Northeast China[J]. Journal of Glaciology and Geocryology,1985,7(3):195-203.(in Chinese)
[20] 丁锡祉,裘善文,孙广友.大兴安岭北部的冰缘现象[C]∥中国地质学会第四纪冰川与第四纪地质专业委员会.第四纪冰川与第四纪研究(3).北京:地质出版社,1987:184-189. DING Xi-zhi,QIU Shan-wen,SUN Guang-you.The periglacial phenomenon in North Da Hinggan Mountains[C]∥Committee of Quaternary Glacial and Geology of Geological Society of China.Quaternary Glacial and Geology(3).Beijing:Geology Publishing House,1987:184-189.(in Chinese)
[21] 缪振椽,高振操,初本君.对白土山探底第四系的新认识[C]∥中国第四纪研究会.第三届全国第四纪学术会议论文集.北京:科学出版社,1982:251-252. MIAO Zhen-chuan,GAO Zhen-cao,CHU Ben-jun.A new knowledge on Quaternary layers in Baitu Mountain[C]∥Committee of Quaternary Glacial and Geology of Geological Society of China. The Symposium of the 3rd National Quaternary Conference.Beijing:Science Press,1982:251-252.(in Chinese)
[22] 吉林省区域地层表编写组.东北区域地层表:吉林省分册[M].北京:地质出版社,1978. The Group for Region Stratum of Jilin Province.Regional stratum table in Northeast China:Jilin volume[M].Beijing:Geology Publishing House,1978.(in Chinese)
[23] 全国地层委员会.中国的新生界[M].北京:科学出版社,1963. National Commission on Stratum.Cenozoic of China[M].Beijing:Science Press,1963.(in Chinese)
[24] 缪振椽,初本君,高振操.黑龙江省第四纪地层测年[J].地质论评,1984,30(4):357-364. MIAO Zhen-chuan,CHU Ben-jun,GAO Zhen-cao.The Quaternary stratum age of Heilongjiang Province[J].Geological Review,1984,30(4):357-364.(in Chinese)
[25] 列兹尼科夫 A П.沉积岩相与建造[M].王述训译.北京:科学出版社,1961. LIZINIKOV А Π.Phase and construction of deposit rock[M].Translated by WANG Shu-xun.Beijing:Science Press,1961.(in Chinese)
[26] 李文漪.中国第四纪植被与环境[M].北京:科学出版社,1998. LI Wen-yi.Quaternary vegetation and environment in China[M].Beijing:Science Press,1998.(in Chinese)
[27] 施雅风.中国冰川与环境:现在、过去和将来[M].北京:科学出版社,2000. SHI Ya-feng.The glaciers and environment in China:present,past and future[M].Beijing:Science Press,2000.(in Chinese)
[28] 斯米尔诺夫 A M.东北平原地形与水文网的发育[J].中国第四纪研究,1958,1(2):159-162. SMINOV A M.The development of topography and hydrological networks of the Northeast Plain[J].Chinese Quaternary Research,1958,1(2):159-162.(in Chinese)
[29] 孙广友.松辽平原中部第四纪地壳运动与平原发育——兼论松辽分水岭的形成[C]∥东北平原第四纪自然环境形成与演化基金课题组.东北平原第四纪自然环境形成与演化.哈尔滨:哈尔滨地图出版社,1990:44-50. SUN Guang-you.Quaternary crustal movement and plain development in the middle of Songliao Plain—discussing the formation of Songliao watershed[C]∥The Group of Quaternaty Foundation and Natural Environment Evolution in Northeast Plain of China.Quaternary Foundation and Natural Environment Evolution in Northeast Plain of China.Harbin:Harbin Cartographic Press,1990:44-50.(in Chinese)
[30] 夏玉梅,汪佩芳.松嫩平原晚第三纪—更新世孢粉组合及古植被与古气候的研究[J].地理学报,1987,42(2):165-178. XIA Yu-mei,WANG Pei-fang.The paleobotany and paleoclimate in the Songnen Plain:a study on the Late Tertiary-Plei-stocene spore pollen assemblages[J].Acta Geographica Sinica,1987,42(2):165-178.(in Chinese)
[31] 王曼华.我国东北平原晚更新世晚期植物群与古气候指标初探[J].冰川冻土,1987,9(3):229-238. WANG Man-hua.Preliminary study of palaeovegetation and palaeoclimatic index in the later period of the Late Pleistocene in Northeast Plain of China[J].Journal of Glaciology and Geocryology,1987,9(3):229-238.(in Chinese)
[32] 孙建中,张镇洪.松辽第四纪[M].香港:中国评论学术出版社,2007. SUN Jian-zhong,ZHANG Zhen-hong.Quaternary of Songliao[M].Hong Kong:Chinese Academic Commentary Press,2007.(in Chinese)
[33] 姜 鹏.松嫩平原晚更新世猛犸象-披毛犀动物群与环境的研究[C]∥东北平原第四纪自然环境形成与演化基金课题组.东北平原第四纪自然环境形成与演化.哈尔滨:哈尔滨地图出版社,1990:24-29. JIANG Peng.Study on the mammoth-woolly rhinoceros animal group and environment in the Late Pleistocene of the Songnen Plain[C]∥The Group of Quaternaty Foundation and Natural Environment Evolution in Northeast Plain of China.Quaternary Foundation and Natural Environment Evolution in Northeast Plain of China.Harbin:Harbin Cartographic Press,1990:24-29.(in Chinese)
[34] 裴文中.哈尔滨黄山及內蒙扎赉诺尔附近“冰滑”作用的初步研究[J].科学记录,1957,1(1):5. PEI Wen-zhong.The preliminary research on the “ice slip” in the Huangshan of Harbin and Zhalainuoer of Inner Mongolia[J].Science Report,1957,1(1):5.(in Chinese)
[35] 邹春静,徐文铎.中国东北植被生态学研究中的焦点问题[J].应用生态学报,2004,15(10):1711-1721. ZOU Chun-jing,XU Wen-duo.Key problems in ecological research on vegetations in Northeast China[J].Chinese Journal of Applied Ecology,2004,15(10):1711-1721.(in Chinese)
[36] 观 微.大兴安岭首次发现砾质偃松苔原[N].科学时报,2009-09-15(4). GUAN Wei.First discovered pinux pumila growelly tundra in Da Hinggan Mountains[N].Science Times,2009-09-15(4).(in Chinese)
[37] 孙广友.初论三江平原第四纪地壳运动[J].地理科学,1983,3(4):353-360. SUN Guang-you.A limited study for the earth crust movement of Quaternary in Sanjiang Plain[J].Scientia Geographica Sinica,1983,3(4):353-360.(in Chinese)
[38] 孙广友.三江平原地貌结构形成演化与合理开发的初步研究[C]∥孙广友.地理系统探微.长春:吉林科学技术出版社,2008:25-34. SUN Guang-you.The preliminary research on the landform formation and evolution and reasonable development of Sanjiang Plain[C]∥SUN Guang-you.The Small Seeing for Geo-graphy System.Changchun:Jilin Science and Technology Press,2008:25-34.(in Chinese)
[39] 夏玉梅,汪佩芳.三江平原新第三纪—更新世孢粉组合与古气候的探讨[C]∥中国地质学会第四纪冰川与第四纪地质专业委员会.第四纪冰川与第四纪地质论文集.北京:地质出版社,1987:151-168. XIA Yu-mei,WANG Pei-fang.The pollen construction and paleoclimate of Late Pleistocene-Quaternary in Sanjiang Plain[C]∥Committee of Quaternary Glacial and Geology of Geological Society of China.The Symposium on Quaternary Glacial and Geology.Beijing:Geology Publishing House,1987:151-168.(in Chinese)
[40] 曾建平.三江平原第四系划分及下限问题[J].中国第四纪研究,1985,6(1):90-98. ZENG Jian-ping.The lower limit of Quaternary in Sanjiang Plain[J].Chinese Quaternary Research,1985,6(1):90-98.(in Chinese)
[41] 孙洪艳,田明中,武法东,等.大兴安岭南段克什克腾第四纪冰川遗迹的发现及其意义[J].地质学报,2005,79(4):576. SUN Hong-yan,TIAN Ming-zhong,WU Fa-dong,et al.The discovery of Quaternary glacial remains in Keshiketeng of Da Hinggan Mountains and its significance[J].Acta Geologica Sinica,2005,79(4):576.(in Chinese)

Memo

Memo:
-
Last Update: 2012-03-20