A SURVEY OF RESEARCHES ON PALEOCLIMATIC CHANGE UP TO 200 000 A BP IN CHINA AND SOME SUGGESTIONS
Received date: 1997-04-28
Revised date: 1997-09-15
Online published: 1998-04-01
Global change is one of the key problems that human faces, and the understanding on the past global change, especially on the paleoclimatic change up to 200 000 a BP, is the key to forecasting future climatic change. Based on the studies on the loess, the lake deposits, the ice cores, the marine sediments and the cave sediments, some important results have been got in China. But there are still so medeficiency, i. e. low resolution records, lack of systematical information in some areas and comprehensive mechanism studies etc. Considering these deficiency and the special regional superiority in China, we should give more effective studies on some important areas and periods in order to understand further the influence of the uplift of Qinghai-Xizang plateau on the East Asia's climate, the evolution of the East Asia monsoon and so on.
Key words： Paleoclimate study; Sediment; Ice core; China.
Li Bin，Yuan Daoxian . A SURVEY OF RESEARCHES ON PALEOCLIMATIC CHANGE UP TO 200 000 A BP IN CHINA AND SOME SUGGESTIONS[J]. Advances in Earth Science, 1998 , 13(2) : 192 -197 . DOI: 10.11867/j.issn.1001-8166.1998.02.0192
[1] 吴世迎, 房泽成, 陈成业, 等. 中太平洋西部 L2011岩心氧同位素地层学研究. 科学通报, 1982, (9): 553～556.
[2] 顾兆炎, 刘东生, 陈明阳, 等. 中国南海沉积物中有孔虫的氧同位素研究. 第四纪研究, 1991, (1): 55～63.
[3] 陈承惠, 蓝东兆, 于永芬, 等. 台湾海峡西部海域第四纪地层. 第四纪研究, 1990, (4): 301～307.
[4] Yue-Gau Chen, Tsung-Kwei Liu. Sea level changes in the last several thousand years, Penghu Islands, Taiwan Strait.Quaternary Research, 1996, (45): 254～262.
[5] 王兆荣. 中国渤海五万年来的古气候. 见: 地幔演化与成岩成矿同位素地球化学. 北京: 地震出版社, 1993. 220～221.
[6] Broecker W S, Andree M, Klas M, et al. New evidence from the south China sea for an abrupt termination of the last glacial period. Nature, 1988, (333):156～158.
[7] 刘东生, 文启忠, 安芷生, 等. 黄土与环境. 北京: 科学出版社, 1985. 1～481.
[8] An Z, Kukla G J, Porter S C, et al. Magnetic susceptibility evidence of monsoon variation on the loess plateau of central China during the last 130 000 years.Quaternary Research, 1991, 36:29～36.
[9] An Z, Porter S C, Zhou W, et al. Episode of Strengthened summer monsoon climate of Younger Dryas age on the loess plateau of central China. Quaternary Research, 1993, 39: 45～54.
[10] Marker B A, Thompson R. Paleorainfall reconstruction from pedogenic magnetics usceptility variations in the chinese loess and paleosols. Quaternary Research, 1995, 44:383～391.
[11] Xiao J, Porter S C, An Z, et al. Grain size of quartz as an indicator of winter monsoon strength on the loess plateau of central China during the last 130 000 yr. Quaternary Research, 1995, 43:22～29.
[12] 文启中, 刁桂仪, 贾蓉芬, 等. 黄土剖面中古环境变化的地球化学记录. 第四纪研究, 1995, (3) : 223～230.
[13] 万国江. 云贵高原湖泊现代沉积地球化学过程及环境信息的辨识与提取. 见: 国家自然科学基金重点项目简介(三). 北京: 科学出版社, 1996. 145～146.
[14] Campo E V,Cour P,Hang S.Holocene environmental changes in Bangong Co basin (western Tibet),Part2: The pollen record. Paleography Paleoclimatology Paleoecology, 1996, 120: 49～63.
[15] 王瑜, 孙湘君. 内蒙古察尔素泥炭剖面全新世古环境变迁的初步研究. 科学通报, 1997, 42: 514～518.
[16] Jarvis D I. Pollenevidence of changing Holocene monsoon climate in Sichun province, China. Quaternary Research,1993, 39: 325～337.
[17] 汪训一. 桂林洞穴沉积物的氧、碳同位素特征. 中国岩溶, 1985, (2): 149～159.
[18] 陈跃, 黄培华, 朱洪山. 北京周口店地区洞穴第四纪石笋的同位素古温度研究. 科学通报, 1986, 20: 1 576～1 577.
[19] 李平, 彭子诚, 洪阿实, 等. 福建宁化天鹅洞石笋年代和古温度. 见: 谢云鹤, 杨明德主编. 人类活动与岩溶环境. 北京: 北京科学技术出版社, 1994. 133～139.
[20] Li B,Y uan D,Qin J,et al.A high resolution record of climate change in a stalagmite from Panlong cave of Guilin since 3 6 000 years BP.Climate Change:
The Karst Record, USA.Karst water Institute Special Publication2,1996.93～96.
[21] Qin J. Studies on oxygen isotope thermometry of cave sediment and paleoclimatic record. 中国岩溶, 1996, 15(1～2): 174～182.
[22] 沈冠军, Gahleb B, 金林红. 热电离质谱法测定贵州邓家洞石笋铀系年代及其古气候意义. 中国岩溶, 1997, 16(1) : 11～18.
[23] 刘东生, 谭明, 覃小光, 等. 洞穴碳酸钙微层理在中国的首次发现及其对全球变化研究的意义. 第四纪研究, 1997,(1): 41～51.
[24] Thompson L G, Mosley-Thompson E, Davis M E, et al. Holocene-late Pleistocene climate ice core records from Qinghai-Tibetan plateau. Science,1989,246:474～477.
[25] 卫克勤, 林瑞芬. 祁连山敦德冰心氧同位素剖面的古气候信息探究. 地球化学, 1994, 23: 311～320.
[26] 孙鸿烈. 青藏高原研究的新进展. 地球科学进展, 1996, 11(6): 536～542.
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