IMPLICATIONS OF GLACIERS ON JAPANESE MOUNTAINS FOR THE LOW MOUNTAIN GLACIERS IN EASTERN CHINA
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摘要: 日本列岛冰川作用的启动时间大致控制在末次冰期范围内,包含末次冰期早期(MIS4)、末次冰期中期(MIS3b)和末次冰期晚期(MIS2)及全新世几个阶段,冰期规模呈现依次递减的变化规律。结合影响冰川发育的地形(海拔高度)和气候条件:充沛的降水、活跃的新构造运动和适宜的地理位置等因素同步响应,体现出冰川发育的优越性与特殊性。因此,日本列岛冰川作用在东亚季风区启动时间最早,消退时间最晚,冰川发育环境最优,冰进期大致控制于几次寒冷降温事件。与同纬度大陆区的我国东部山地的对比,中国东部发育"低海拔型"山地冰川的结论值得商榷。Abstract: The research of timing and extent of the late Quaternary glaciation in the Japanese islands show that the glacial sequences, dated as the early stage (MIS4), middle stage (MIS3b),late stage(MIS2) and the Holocene (MIS1), are all constrained within the last glacial cycle, and the glacial extent decreases with time. According to the topography (altitude) and climate affected the glacier development, abundant precipitation, active tectonic movement and the suitable geographic position provide the necessary conditions for the glacier development on the Japanese mountains. In the east Asia monsoon region, they are initiated the earlist,but, the retreated the latest. The glacial advances are mainly controlled by several cold events. Compared with the mountains in the same latitude in eastern China, the existance of the low altitude glacial action in eastern China is doubtful.
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[1] 韩同林, 劳雄, 郭克毅. 河北, 内蒙古中低山区发现罕见的冰臼群[J]. 地质论评, 1999, 45(5):456-462. [HAN Tonglin, LAO Xiong, Guo Keyi. Rare moulin swarms discovered in the medium-low mountains areas in Hebei and Inner Mongolia[J]. Geological Review, 1999, 45(5):456-462.]
[2] 吕洪波, 任晓辉, 杨超.赤峰等地第四纪大陆冰川的地貌证据[J].地质论评, 2006, 52(3):379-385. [LU Hongbo, REN Xiaohui, YANG Chao. Landform evidences of Quaternary continental glaciation in Chifeng and the vicinity area, North of China[J]. Geological Review, 2006, 52(3):379-385.]
[3] 赵松龄.中国东部低海拔型古冰川遗迹[M]. 北京:海洋出版社, 2010:14-19.[ZHAO Songling. Glacial remains of lower altitude mountains in the Eastern China[M]. Beijing, China:China Ocean Press, 2010:14 -19.]
[4] Chen A D, Tian M Z, Zhao Z Z. et al. Macroscopic and microscopic evidence of Quaternary glacial features and ESR dating in the Daweishan Mountain area, Hunan, eastern China[J]. Quaternary International, 2014, 333:62-68.
[5] 徐兴永, 肖尚斌, 李萍. 崂山古冰川遗迹的地质证据[J]. 石油大学学报:自然科学版, 2005, 29(4):5-9. [XU Xingyong, XIAO Shangbin, LI ping. Geologic proof on paleo-glaciation remains in Laoshan Mountain[J]. Journal of the University of Petroleum, China, 2005, 29(4):5-9.]
[6] 张建伟, 郭秀岩, 申卫星, 等. 泰山地区第四纪冰川探讨[J].山东国土资源, 2011, 27(4):12-14. [ZHANG Weijian, GUO xiuyan, SHEN Weixing, et al. Study on Quaternary Glaciers in Mountain Tai[J]. Land resources Shandong, 2011, 27(4):12-14.]
[7] 施雅风. 中国东部中低山地有无发育第四纪冰川的可能性[J]. 地质论评, 2011, 57(1):44-49. [Shi Yafeng. Is it any possible for the low mountains of Eastern China to develop Quaternary glacier[J]. Geological Review, 2011, 57(1):44-49.]
[8] 阎恒凯. 关于日本的冰川问题[J]. 辽宁师范大学(自然科学版), 1980, 3:12-17.[YAN Hengkai. Glacial problem about Japan[J]. Journal of Liaoning Normal University(Natural Science Edition), 1980, 3:12-17.] [9] Ono Y, Aoki T, Hasengawa H. et al. Mountain glaciation in Japan and Taiwan at the global Last Glacial Maximum[J]. Quaternary International, 2005, 138/139:79-92.
[10] 橋本誠二, 熊野純男. 北部日高山脈の氷蝕地形. 地质学雑誌, 1955, 61:208-217.[HASHIMOTO S, KUMANO S. Zur Gletschertopographieim Hidaka-Gebirge, Hokkaido, Japan[J]. The Geological society of Japan, 1955 , 61:208-217.]
[11] Yanagida M. Age of the Shikotsu pumice fall-1 deposit[J]. The Quaternary Research, 1994, 33:205-207.
[12] 岩崎正吾, 平川一臣, 澤柿教伸. 日高山脈エサオマントツタベツ川流域における第四紀後期の氷河作用とその編年[J]. 地学雑誌, 2000, 109(1):37-55. [Iwasaki S, Hi-rakawa K, Sawagaki T, et al. Late Quaternary glaci-ation in the Esaoman-Tottabetsu Valley, Hidaka Range, Hokkaido, Japan[J]. Journalof Geography, 2000, 109(1):37-55.]
[13] Machida H, Arai F. Atlas of tephra in and around Japan(revised edition)[M]. University of Tokyo Press, 2004, 336.
[14] Ono Y. Last glacial paleoclimate reconstructed from glacial and periglacial landforms in Japan[J]. Geographical Review, 1984, 57B:87-100.
[15] Ono Y, Naruse T. Snowline elevation and eolian dust flux in the Japanese islands during isotope stages 2and4[J]. Quaternary International, 1997, 37:45-54.
[16] Ono Y, Shulmeister J, Lehmkuhl F, et al. Timing and causes of glacial advances across the PEP-2 Transect(East-Asia to Antarctica)during the last glaciation cycle[J]. Quaternary International, 2004, 118/119.
[17] Ehlers J, Gibbard P L. Quaternary glaciations extent and chronology[M]. Amsterdam, Holland:Elsevier, 2011:217-223.
[18] 李吉均. 中国东部山地第四纪冰期气候问题[J]. 地理学报, 1983, 38(4):438-442. [LI Jijun. Climatic problems of quaternary glaciation in the eastern China Mountains[J]. Acta Geographica Sinica, 1983, 38(4):438-442.]
[19] 長谷川裕彦. 北アルプス西南部,打込谷の氷河地形と氷河前進期[J]. 地理学評論, 1992, 65A:320-338.[Hasegawa H.Glacial and periglacial landforms around Mt. Kasaga-take, northern Japanese Alps[J]. Geographical Review of Japan, 1992 , 65(4):320-338.]
[20] 青木賢人. モレ-ン構成砾の風化皮膜の厚さから推定した中央アルプス北部における氷河前進期[J]. 地理学評論, 1994, 67A(9):601-618. [Aoki T. Chronological study of glacial advances based on the weathering-rind thickness of morainic gravels in the northern part of the central Japan Alps[J]. Geographical Review of Japan, 1994, 67A(9):601-618.]
[21] Kondoa R, Tsukamoto S, Tachibanaa H, et al. Age of glacial and periglacial landforms in northern Hokkaido, Japan, using SOL dating of fine grain quartz[J]. Quaternary Geochronology, 2007, (2):260-265.
[22] Aoki T. Younger Dryas glacial advances in Japan dated with in situ produced cosmogenic radionuclides[J]. Transactions, 2003, 24(1):27-39.
[23] 施雅风. 对崔之久和张威《末次冰期冰川规模与冰川"异时"?"同时"问题的讨论》一文的商榷[J]. 冰川冻土, 2003, 25(5):536.[SHI Yafeng. Discussion about the glacier extent and advance/retreat asynchrony during the Last Glaciation[J]. Journal of Glaciology and Geocryology, 2003 , 25(5):536.]
[24] 崔之久, 杨健夫, 刘耕年, 等. 季风的发展与冰川的消失:从台湾高山末次冰期冰川发育特征说起[J]. 冰川冻土, 2000, 22(1):7-13. [CUI Zhijiu, YANG Jianfu, LIU Gengnian, et al. Monsoon development and glacier disappearance:from the point of view of glacier revolution features during Last Glaciation in Xueshan, Taiwan[J]. Journal of Glaciology and Geocryology, 2000, 22(1):7-14.]
[25] 张威, 于治龙, 李媛媛, 等. 亚洲中纬度地区第四纪冰川作用差异性探讨[J]. 干旱区地理, 2013, 68(7):407-418. [ZHANG Wei, YU Zhilong, Li Yuanyuan, et al. Discussion on difference of Quaternary glaciation in the mid-latitude regions of Asia[J]. Arid Land Geography, 2014, 37(3):407-418.]
[26] Zhang W, Liu L, Chen Y X, et al. Late glacial 10Be ages for glacial landforms in the upper region of the Taibai glaciation in the Qinling Mountain range, China[J]. Journal of Asian Earth Sciences, 2016, 115:383-392.
[27] 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 Yunbo, YAN Ling, et al. Late Pleistocene glaciations of Changbai Mountains in northeastern China[J]. Chinese Science Bulletin, 2008, 53:2672-2684.]
[28] 张威, 闫玲, 崔之久, 等. 东亚沿海山地末次冰期冰川与环境[J]. 地理学报, 2009, 64(1):33-41. [ZHANG Wei, YAN Ling, CUI Zhijiu, et al. Glacial environment during the Last Glacial Cycle in the mountains of East Asia[J]. Acta Geographica Sinica, 2009, 64(1):33-41.]
[29] 沈兴艳, 万世明. 日本海第四纪沉积记录及其海陆联系的研究进展[J].海洋地质与第四纪地质, 2015, 35(6):139-151. [SHEN Xingyan, WAN Shiming. Research progress of Quaternary depositional records of the Japan Sea and implicatons for the linkages to the Asian continent[J]. Marine Geology&Quaternary Geology, 2015, 35(6):139-151.]
[30] 姜大膀, 梁潇云. 末次盛冰期东亚气候的成因监测[J]. 第四纪研究, 2008, 28(3):491-501. [JIANG Dabang, LIANG Xiaoyun. Attribut on of East Asian climate at the Last Glacial maximum[J]. Quaternary Sciences, 2008, 28(3):491-501.]
[31] 张威,刘锐,刘亮. 东亚季风影响区末次冰期冰川作用的控制性因素[J]. 地理科学进展, 2015, 34(7):871-882. [ZHANG Wei, LIU Rui, LIU Liang. Control factors on glaciation during the last glacial period in the East Asia monsoon area[J]. Progress in Geography, 2015, 34(7):871-882.]
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