全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...
地球学报  2011 

中全新世云南寻甸地区气候演化与冷干事件的石笋记录

DOI: 10.3975/cagsb.2011.01.12

Keywords: XR1石笋,中全新世,氧碳同位素,西南季风

Full-Text   Cite this paper   Add to My Lib

Abstract:

通过对云南寻甸XR1石笋进行TIMS-U系测年、氧碳同位素和沉积速率变化分析,重建了寻甸地区中全新世季风气候演化模式:(1)8.0~6.0kaBP为温暖湿润期;(2)6.0~5.1kaBP为气候突变期,温湿向冷干转变;(3)5.1~2.1kaBP为气候恢复期,气候从冷干逐渐恢复到中全新世正常的气候水平。XR1石笋还揭示了该地区中全新世出现的四次冷干气候事件:6.0~5.1kaBP冷干事件相当于考古学上的仰韶中期的寒冷期,被Denton称为第二次小冰期;4.7~4.5kaBP气候事件是气候回暖过程中一次短暂的变冷事件;3.1~2.5kaBP间的降温事件在中国历史文献中被称为西周寒冷期,相当于北半球新冰期中的第三次新冰期。2.5~2.1kaBP降温阶段相当于我国近5000年气候变化的第二次冷期。

References

[1]  ZHU Ke-zhen,Preliminary research on climate change over the last 5000 years in China,Journal of Archaeology,1972(01).
[2]  周静;王苏民;吕静.洱海地区一万多年以来气候环境演化的湖泊沉积记录[J].湖泊科学,2003(06)
[3]  Fleitmann D. ;Burns SJ. ;Mudelsee M. ;Neff U. ;Kramers J. ;Mangini A. Matter A.,Holocene forcing of the Indian monsoon recorded in a stalagmite from Southern Oman,Science?,2003, 300(5626).
[4]  DENTON G H;KARLEN W,Holocene climatic variations:their pattern and possible cause,Quaternary Research? ,1973, 3.
[5]  DEMENOCAL P;ORTIZ J;GUIDERSON T;SARNTHEIN M,Coherent high-and-low latitude climate variability during the Holocene warm period,Science,2000(23).
[6]  CRAIG H;GORDON L I;HORIBE Y,Isotopic exchange effects in the evaporation of water,1,low-temperature experimental results,Journal of Geophysical Research,1965.
[7]  王华;洪业汤;朱咏煊;林庆华 冷雪天 毛绪美,红原泥炭腐质化程度记录的全新世气候变化,地质地球化学,2003(02).
[8]  靳桂云;刘东生.华北北部中全新世降温气候事件与古文化变迁[J].科学通报,2001(20)
[9]  曹雯;夏正楷,河南孟津寺河南中全新世湖泊沉积物的易溶盐测定及其古水文意义,北京大学学报(自然科学版),2008(06).
[10]  安芷生;刘晓东.东亚季风气候的历史与变率[J].科学通报,2000(03)
[11]  THOMPSON L G;YAO T;DAVIS M E;HENDERSON K A,.THOMPSON E M,LIN P N,BEER J,SYNAL H A,DAIJ C,.BOLZAN J F Tropical climate instability; the last Glacial cycle from a Qinghai-Tibetan Ice Core [J] 1997(5320) doi:10.1126/science.276.5320.1821
[12]  CAO Wen;XIA Zheng-kai,Paleo-hydrological signification in Mid-Holocene revealed by the analysis soluble salts of Sihenan profile in Menjin,Henan province,Acta Scientiarum Naturalium Universitatis Pekinensis,2008(06).
[13]  AN Zhi-sheng;LIU Xiao-dong,The history and variability of East Asian Monsoon climate,Quaternary Science Reviews,2000(15).
[14]  SANDWEISS D H;MAASCH K A;ANDERSON D G,Transitions in the Mid-Holocene,Science,1998(19).
[15]  QIN Jia-ming;YUAN Dao-xian;LIN Yu-shi,Isotopic record and its environmental interpretation of stalagmites for 44ka BP in Guilin,Acta Geoscientica Sinica,2000(04).
[16]  L(U) Hou-yuan;ZHANG Jian-ping,Neolithic cultural evolution and Holocene climate change in the Guanzhong Basin,Shanxi,China,Quaternary Sciences,2008(06).
[17]  ZHOU Jing;WANG Su-min;L(U) Jing,Climatic and environmental changes from the sediment record of Erhai Lake over the past 10000 years,Journal of Lake Sciences,2003(06).
[18]  ZHANG Zhen-ke;WANG Su-min;WU Rui-jin,Enironment evolution recorded by lake sediments of Erhai and Southwest Monsoon change during the middle Holocence,Bulletin of Science,1998(19).
[19]  ZHANG Mei-liang;LIN Yu-shi;ZHU Xiao-yan;QIN Jia-ming YANG Yan LUO Gui-rong,The records of climatic change from a stalagmite during the late time of the middle Holocence in Ninglang area,Yunnan,Marine Geology and Quaternary Geology,2006(01).
[20]  YU Tong-yuan,Space-time discrepancy of climate change and its influence in Chinese history,Journal of Anhui Institude of Education College,1996(03).
[21]  YANG Huai-ren;XIE Zhi-ren,Sea-level changes along the east coast of china over the last 20,000 years,Oceanologica Et Limnologia Sinica,1984(01).
[22]  WU Wen-xiang;LIU Dong-sheng,5500 a BP climatic event and its implications for the emergence of civilization in Egypt,Mesopotamia and Neolithic cultural development in China,Earth Sciences Frontiers,2002(01).
[23]  WANG Su-min,Climate change and lake environment of Daihai,Beijing:University of science and technology of China press,1990.
[24]  WANG Kai-fa,Preliminarily study on middle and low temperature events during warm period in Holocene,Quaternary Sciences,1990(02).
[25]  WANG Hua;HONG Ye-tang;ZHU Yong-xuan;LIN Qing-hua LENG Xue-tian MAO Xu-mei,The peat humification records of Holocene climate change in Hongyuan region,Geology and Geochemistry,2003(02).
[26]  竺可桢,中国近五千年来气候变迁的初步研究,考古学报,1972(01).
[27]  覃嘉铭;袁道先;林玉石,桂林44 ka BP石笋同位素记录及其环境解译,地球学报,2000(04).
[28]  吕厚远;张建平.关中地区的新石器古文化发展与古环境变化的关系[J].第四纪研究,2008(06)
[29]  李红春;顾德隆;陈文寄;李铁英,利用洞穴石笋的δ18O和δ13C重建3000a以来北京地区古气候和古环境:石花洞研究系列之三,地震地质,1997(01).
[30]  SPINDLER K,The Man in the Ice,New York:Harmony Book,1991.
[31]  LISTER G S;KELTS K;CHEN K Z;JUN Q Y,NIESSEN F,Lake Qinghai,China:closed-basin lake levels and oxygen isotope record for ostracoda since the latest Pleisto-cene,Palaeogeography paleoclimatology paleoecolgy,1991.
[32]  LI Hong-chun;GU De-long;CHEN Wen-ji;LI Tie-ying,Isotope studies of Shihua Cave-III:reconstruction of paleoclimate and paleoenvironment of Beijng during the last 3000 years from δ18O and δ13C records in stalagmite,Seismology and Geology,1997(01).
[33]  JIN Gui-yun;LIU Dong-sheng,Cooling events and cultural transition during middle Holocene in northern part of North China,Bulletin of Science,2001(20).
[34]  HUANG C C;ZHOU J;PANG J L;HAN Y P HOU C H,A regional aridity phase and its possible culture impact during the Holocene Megathermal in the Guanzhong Basin,China,The Holocene,2000(01).
[35]  Gasse F;Arnold M;Fontes J C,A 13000-year climate record from westeru Tibet,Nature? ,1991, 353.
[36]  张振克;王苏民;吴瑞金,全新世中期洱海湖泊沉积记录的环境演化与西南季风变迁,科学通报,1998(19).
[37]  张美良;林玉石;朱晓燕;覃嘉铭 杨琰 罗贵荣.云南宁蒗地区中全新世晚期气候变化的石笋记录[J].海洋地质与第四纪地质,2006(01)
[38]  余同远,中国历史上气候变迁的时空差异性及其影响,安徽教育学院学报,1996(03).
[39]  杨怀仁;谢志仁,中国东部近20,000年来的气候波动与海面升降运动,海洋与湖沼,1984(01).
[40]  吴文祥;刘东生.5500 a BP气候事件在三大文明古国古文明和古文化演化中的作用[J].地学前缘,2002(01)
[41]  王苏民,岱海--湖泊环境与气候变化,合肥:中国科学技术大学出版社,1990.
[42]  王开发,全新世温暖期中低温事件的初步研究,第四纪研究,1990(02).

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133