PDF下载 分享
[1]杨 亮,陈 琳,黄嘉仪,等.南岭东部水源洞过去700年石笋氧同位素变化与气候意义[J].地球化学,2016,45(02):164-172.
 YANG Liang,CHEN Lin,HUANG Jia-yi,et al.δ18O record of a 700-years-old speleothem from the Shuiyuan Cave in eastern Nanling Mountain and its paleoclimatic implications[J].Geochimica,2016,45(02):164-172.
点击复制

南岭东部水源洞过去700年石笋氧同位素变化与气候意义

参考文献/References:

[1] 迟宝泉, 周厚云, 赵建新, 韦刚健, 关华政, 俸月星, 朱照宇, 周国庆, 闫峻. 54~46 ka川东北石笋的氧同位素记录及其气候环境意义探讨[J]. 地球化学, 2007, 36(4): 337-343.
Chi Bao-quan, Zhou Hou-yun, Zhao Jian-xin, Wei Gang-jian, Guan Hua-zheng, Feng Yue-xing, Zhu Zhao-yu, Zhou Guo-qing, Yan Jun. δ18o variation during 54-46 ka recorded by a stalagmite from Northeast Sichuan, Central China and its relationship with summer monsoon evolution [J]. Geochimica, 2007, 36(4): 337-343 (in Chinese with English abstract).
[2] 张美良, 程海, 林玉石, 覃嘉铭, 张会领, 涂琳玲, 王华, 冯玉梅. 贵州荔波1.5万年以来石笋高分辨率古气候环境记录[J]. 地球化学, 2004, 33(1): 65-74.
Zhang Mei-liang, Cheng Hai, Lin Yu-shi, Qin Jia-ming, Zhang Hui-ling, Tu Lin-ling, Wang Hua, Feng Yu-mei. High resolu-tion paleoclimatic environment records from a stalagmite of Dongge Cave since 15000 a in Libo, Guizhou Province, China [J]. Geochimica, 2004, 33(1): 65-74 (in Chinese with English abstract).
[3] 杨琰, 袁道先, 程海, 覃嘉铭, 张美良, 林玉石, 朱晓燕. 文石-方解石石笋U/Th体系的封闭性判断及意义[J]. 地球化学, 2008, 37(2): 97-106.
Yang Yan, Yuan Dao-Xian, Cheng Hai, Qin Jia-ming, Zhang Mei-liang, Lin Yu-shi, Zhu Xiao-yan. Discrimination of close U/Th system in aragonite-calcite stalagmites and their signi-ficance [J]. Geochimica, 2008, 37(2): 97-106 (in Chinese with English abstract).
[4] 殷建军, 林玉石, 唐伟. 洞穴文石石笋古气候环境变化研究进展、存在问题及研究方向[J]. 中国岩溶, 2014, 33(4): 387-395.
Yin Jian-jun, Lin Yu-shi, TANG Wei. Aragonite stalagmite use in paleoclimate and environmental change research: Progress, disadvantages and further research directions [J]. Carsol Si-nica, 2014, 33(4): 387-395 (in Chinese with English ab-stract).
[5] Zhang P Z, Cheng H, Edwards R L, Chen F H, Wang Y J, Yang X L, Liu J, Tan M, Wang X F, Liu J H, An C L, Dai Z B, Zhou J, Zhang D Z, Jia J H, Jin L Y, Johnson K R. A test of climate, sun, and culture relationships from an 1810-year Chinese cave record [J]. Science, 2008, 322(5903): 940-942.
[6] 章程, 袁道先. 洞穴滴石石笋与陆地古环境记录研究进展[J]. 地球科学进展, 2001, 16(3): 374-381.
Zhang Cheng, Yuan Dao-xian. Study on continental paleoen-vironmental proxy based on speleothems (drop stones) [J]. Adv Earth Sci, 2001, 16(3): 374-381 (in Chinese with English abstract).
[7] 覃嘉铭, 林玉石, 张美良, 王华, 冯玉梅, 涂琳玲. 末次冰期东亚季风气候的变迁: 贵州都匀七星洞石笋的δ18O记录[J]. 中国岩溶, 2003, 22(3): 167-173.
Qin Jia-ming, Lin Yu-shi, Zhang Mei-liang, Wang Hua, Feng Yu-mei, Tu Lin-ling. Change of the East-Asian monsoon climate during the Last Glaciation: δ18O records of stalagmites in Qixing cave, Duyun City, Guizhou Province [J]. Carsol Sinica, 2003, 22(3): 167-173 (in Chinese with English abstract).
[8] 张会领, 覃嘉铭, 张美良, 王华. 洞穴化学沉积物的古环境记录研究进展[J]. 中国岩溶, 2004, 23(2): 144-153.
Zhang Hui-ling, Qin Jia-ming, Zhang Mei-liang, Wang Hua. Progress in paleoenvironment record study form cave sed-ments [J]. Carsol Sinica, 2004, 23(2): 144-153 (in Chinese with English abstract).
[9] 谭明. 环流效应: 中国季风区石笋氧同位素短尺度变化的气候意义——古气候记录与现代气候研究的一次对话[J]. 第四纪研究, 2009, 29(5): 851-862.
Tan Ming. Circulation effect: Climatic significance of the short term variability of the oxygen isotopes in stalagmites from monsoonal China — Dialogue between paleoclimate records and modern climate research [J]. Quater Sci, 2009, 29(5): 851-862 (in Chinese with English abstract).
[10] 谭明, 刘东生, 秦小光, 钟华, 李铁英, 赵树森, 李红春, 吕金波, 鲁向阳. 北京石花洞全新世石笋微生长层与稳定同位素气候意义初步研究[J]. 中国岩溶, 1997, 16(1): 1-10.
Tan Ming, Liu Dong-sheng, Qin Xiao-guang, Zhong Hua, Li Tie-ying, Zhao Shu-sen, Li Hong-chun, Lü Jin-bo, Lu Xiang-yang. Preliminary study on the date from microbanding and stable isotopes of stalagmites of Beijing Shihua Cave [J]. Carsol Sinica, 1997, 16(1): 1-10 (in Chinese with English abstract).
[11] Wang Y J, Cheng H, Edwards R L, An Z S, Wu J Y, Shen C C, Dorale J A. A high-resolution absolute-dated late Pleistocene monsoon record from Hulu Cave, China [J]. Science, 2001, 294(5550): 2345-2348.
[12] Wang Y, Cheng H, Edwards R L, He Y Q, Kong X G, An Z S, Wu J Y, Kelly M J, Dykoski C A, Li X D. The Holocene Asian monsoon: Links to solar changes and North Atlantic climate [J]. Science, 2005, 308(5723): 854-857.
[13] Paulsen D E, Li H C, Ku T L. Climate variability in central China over the last 1270 years revealed by high-resolution stalagmite records [J]. Quater Sci Rev, 2003, 22(5): 691-701.
[14] Yuan D X, Cheng H, Edwards R L, Dykoski C A, Kelly M J, Zhang M L, Qin J M, Lin Y S, Wang Y J, Wu J Y, Dorale J A, An Z S, Cai Y J. Timing, duration, and transitions of the last interglacial Asian monsoon [J]. Science, 2004, 304(5670): 575-578.
[15] Hu C, Henderson G M, Huang J, Xie S C, Sun Y, Johnson K R. Quantification of Holocene Asian monsoon rainfall from spatially separated cave records [J]. Earth Planet Sci Lett, 2008, 266(3): 221-232.
[16] Zhang R, Schwarcz H P, Ford D C, Schroeder F S, Beddows P A. An absolute paleotemperature record from 10 to 6 ka in-ferred from fluid inclusion D/H ratios of a stalagmite from Vancouver Island, British Columbia, Canada [J]. Geochim Cosmochim Acta, 2008, 72(4): 1014-1026.
[17] Cheng H, Edwards R L, Broecker W S, Denton G H, Kong X G, Wang Y J, Zhang R, Wang X F. Ice age terminations [J]. Science, 2009, 326(5950): 248-252.
[18] Tan L C, Cai Y J, Cheng H, An Z S, Edwards R L. Summer monsoon precipitation variations in central China over the past 750 years derived from a high-resolution absolute-dated stalagmite [J]. Palaeogeogr Palaeoclimatol Palaeoecol, 2009, 280(3): 432-439.
[19] Pausata F S R, Battisti D S, Nisancioglu K H, Bitz C M. Chinese stalagmite δ18O controlled by changes in the Indian monsoon during a simulated Heinrich event [J]. Nat Geosci, 2011, 4(7): 474-480.
[20] Liu Y H, Henderson G M, Hu C Y, Mason A J, Charnley N, Johnson K R, Xie S C. Links between the East Asian monsoon and North Atlantic climate during the 8,200 year event [J]. Nat Geosci, 2013, 6(2): 117-120.
[21] Maher B A. Holocene variability of the East Asian summer monsoon from Chinese cave records: A re-assessment [J]. Holocene, 2008, 18(6): 861-866.
[22] Maher B A, Thompson R. Oxygen isotopes from Chinese caves: Records not of monsoon rainfall but of circulation re-gime [J]. J Quater Sci, 2012, 27(6): 615-624.
[23] Liu J B, Chen J H, Zhang X J, Li Y, Rao Z G, Chen F H. Ho-locene East Asian summer monsoon records in northern China and their inconsistency with Chinese stalagmite δ18O records [J]. Earth Sci Rev, 2015, 148: 194-208.
[24] Johnson K R, Hu C Y, Belshaw N S, Henderson G M. Seasonal trace-element and stable-isotope variations in a Chinese speleothem: The potential for high-resolution paleomonsoon reconstruction [J]. Earth Planet Sci Lett, 2006, 244(1): 394-407.
[25] Clemens S C, Prell W L, Sun Y. Orbital-scale timing and me-chanisms driving Late Pleistocene Indo-Asian summer mon-soons: Reinterpreting cave speleothem δ18O [J]. Paleoceano-graphy, 2010, 25(4): PA4207, DOI: 10.1029/ 2010PA001926.
[26] [26] Dayem K E, Molnar P, Battisti D S, Roe G H. Lessons learned from oxygen isotopes in modern precipitation applied to interpretation of speleothem records of paleoclimate from eastern Asia [J]. Earth Planet Sci Lett, 2010, 295(1): 219-230.
[27] Shen C C, Wu C C, Cheng H, Edwards R L, Hsieh Y T, Gallet S, Chang C C, Li T Y, Lam D D, Kano A, Hori M, Sp?tl C. High-precision and high-resolution carbonate 230Th dating by MC-ICP-MS with SEM protocols [J]. Geochim Cosmochim Acta, 2012, 99: 71-86.
[28] Hendy C H. The isotopic geochemistry of speleothems — I. The calculation of the effects of different modes of formation on the isotopic composition of speleothems and their applicability as palaeoclimatic indicators [J]. Geochim Cosmochim Acta, 1971, 35(8): 801-824.
[29] Schwarcz H P. Geochronology and isotopic geochemistry of speleathems [J]. Handbook Environ Isotop Geochem, 1986, 2: 271-303.
[30] Fairchild I J, Smith C L, Baker A, Fuller L, Sp?tl C, Mattey D, McDermott F, EIMF. Modification and preservation of envi-ronmental signals in speleothems [J]. Earth Sci Rev, 2006, 75(1/4): 105-153.
[31] Dorale J A, Liu Z. Limitations of Hendy test criteria in judging the paleoclimatic suitability of speleothems and the need for replication [J]. J Cave Karst Stud, 2009, 71(1): 73-80.
[32] Kennett D J, Breitenbach S F M, Aquino V V, Asmerom Y, Awe J, Baldini J U L, Bartlein P, Culleton B J, Ebert C, Jazwa C, Macri M J, Marwan N, Polyak V, Prufer K M, Ridley H E, Sodemann H, Winterhalder B, Haug G H. Development and disintegration of Maya political systems in response to climate change [J]. Science, 2012, 338(6108): 788-791.
[33] Lachniet M S, Bernal J P, Asmerom Y, Polyak V, Piperno D. A 2400 yr Mesoamerican rainfall reconstruction links climate and cultural change [J]. Geology, 2012, 40(3): 259-262.
[34] Zhang H L, Yu K F, Zhao J X, Feng Y X, Lin Y S, Zhou W, Liu G H. East Asian summer monsoon variations in the past 12.5 ka: High-resolution δ18O record from a precisely dated aragonite stalagmite in central China [J]. J Asian Earth Sci, 2013, 73: 162-175.
[35] Shi F, Yang B, Von Gunten L. Preliminary multiproxy surface air temperature field reconstruction for China over the past millennium [J]. Sci China Earth Sci, 2012, 55(12): 2058-2067.
[36] Ge Q, Zheng J, Fang X, Man Z, Zhang X, Zhang P, Wang W C. Winter half-year temperature reconstruction for themiddle and lower reaches of the Yellow River and Yangtze River, China, during the past 2000 years [J]. Holocene, 2003, 13: 933-940.
[37] Zhou G T, Zheng Y F. An experimental study of oxygen iso-tope fractionation between inorganically precipitated aragonite and water at low temperatures [J]. Geochim Cosmochim Acta, 2003, 67: 387-399.
[38] Qian W, Hu Q, Zhu Y, Lee D K. Centennial-scale dry-wet variations in East Asia [J]. Clim Dyn, 2003, 21: 77-89.
[39] 周秀骥, 赵平, 刘舸, 周天军. 中世纪暖期、小冰期与现代东亚夏季风环流和降水年代-百年尺度变化特征分析[J]. 科学通报, 2011, 56(25): 2060-2067.
Zhou Xiuji, Zhao Ping, Liu Ke, Zhou Tianjun. Years-hundred scale analysis of summer monsoon circulation and precipitation changes bewteen Medieval warm period, the little ice age and the modern time [J]. Chinese Sci Bull, 2011, 56(25): 2060-2067 (in Chinese).
[40] Qian W, Lin X. Regional trends in recent precipitation indices in China [J]. Meteorol Atmos Phys, 2005, 90(3/4): 193-207.
[41] Hong Y T, Hong B, Lin Q H, Zhu Y X, Shibata Y, Hirota M, Uchida M, Leng X T, Jiang H B, Xu H, Wang H, Yi L. Corre-lation between Indian Ocean summer monsoon and North Atlantic climate during the Holocene [J]. Earth Planet Sci Lett, 2003, 211(3): 371-380.

相似文献/References:

[1]谢小敏,胡文瑄,王小林,等.新疆柯坪地区寒武纪-奥陶纪碳酸盐岩沉积旋回的碳氧同位素研究[J].地球化学,2009,38(01):75.
 XIE Xiao-min,HU Wen-xuan,WANG Xiao-lin,et al.Sedimentary sequences in Keping area, Xinjiang: Constraints from carbon and oxygen isotope compositions of Cambrian to Ordovician carbonate rocks[J].Geochimica,2009,38(02):75.
[2]魏菊英,郑淑蕙,莫志超.冀东滦县一带前震旦纪含铁石英岩中磁铁矿的氧同位素组成[J].地球化学,1979,08(03):195.
[3]于津生,张鸿斌,虞福基,等.西藏东部大气降水氧同位素组成特征[J].地球化学,1980,09(02):113.
[4]虞福基,刘德平.微升量水氧、氢同位素连续分析法及其在矿物包裹体中的应用[J].地球化学,1982,11(03):291.
[5]于津生,虞福基,刘德平.中国东部大气降水氢、氧同位素组成[J].地球化学,1987,16(01):22.
[6]王可法,陈锦石.燕山地区铁岭组稳定同位素组成特征及其地质意义[J].地球化学,1993,22(01):10.
[7]袁超,于津生.青岛花岗岩类复式岩基的古化石热水体系研究[J].地球化学,1994,23(01):50.
[8]卫克勤,林瑞芬.祁连山敦德冰芯氧同位素剖面的古气候信息探究[J].地球化学,1994,23(04):311.
[9]郑永飞.云母族矿物的氧同位素分馏[J].地球化学,1994,23(04):321.
[10]卫克勤,林瑞芬.内陆封闭湖泊自生碳酸盐氧同位素剖面的古气候意义[J].地球化学,1995,24(03):215.

备注/Memo

收稿日期(Received): 2015-06-17; 改回日期(Revised): 2015-11-15; 接受日期(Accepted): 2015-12-07
基金项目: 国家自然科学基金(41271212); 教育部博士点基金(20120101110050); 广东省自然科学基金重点项目(9251064004000001)
作者简介: 杨亮(1990-), 男, 硕士研究生, 研究方向为第四纪地质与全球气候变化。E-mail: yang10135@163.com
* 通讯作者(Corresponding author): ZHOU Hou-yun, E-mail: hyzhou@gig.ac.cn, Tel: +86-20-85211380

更新日期/Last Update: 2016-03-30