熊尚发,刘东生,丁仲礼. 末次间冰期末次冰期转换时期斋堂黄土记录中的气候回返事件[J]. 科学通报,1998,43(17):1873-1876.[Xiong Shangfa, Liu Tungsheng, Ding Zhongli. A climatic reversal at the last interglacial to last glacial transition recorded in the loess section at Zhaitang[J]. Chinese Science Bulletin, 1999, 44(6): 571-575.]
[2]
管清玉,潘保田,高红山,等. 三门峡王官与武威沙沟黄土记录中的末次间冰期向末次冰期转换期的暖性回返事件[J]. 兰州大学学报:自然科学版,2005,41(4):1-5.[Guan Qingyu, Pan Baotian, Gao Hongshan, et al. A warm-return event during the transition of last interglacial-glacial cycle[J]. Journal of Lanzhou University Natural Sciences, 2005, 41(4): 1-5.]
[3]
吴帅男,陈仕涛,段福才. 北半球72 ka BP气候突变事件及其与Toba火山的关系[J]. 地球科学进展,2012,27(1):35-41.[Wu Shuainan, Chen Shitao, Duan Fucai. The relation between the 72 ka BP Event and the Toba super-eruption[J]. Advances in Earth Science, 2012, 27(1): 35-41.]
[4]
吴江滢,汪永进,邵晓华,等. 晚更新世东亚季风气候不稳定性的洞穴石笋同位素证据[J]. 地质学报,2002,76(3):413-419.[Wu Jiangying, Wang Yongjin, Shao Xiaohua, et al. Instability of the Late Pleistocene east Asian monsoon climate—Evidence from the variation of the stable isotope composition of a cave stalagmite[J]. Acta Geologica Sinica, 2002, 76(3): 413-419.]
[5]
杨勋林,张平中,陈发虎,等. 近50 a来青藏高原东部高海拔洞穴现代石笋氧同位素组成及其含义[J]. 科学通报,2007,52(6):698-706.[Yang Xunlin, Zhang Pingzhong, Chen Fahu, et al. Modern stalagmite oxygen isotopic composition and its implications of climatic change from a high-elevation cave in the eastern Qinghai-Tibet Plateau over the past 50 years[J]. Chinese Science Bulletin, 2007, 52(6): 698-706.]
[6]
杨勋林,张平中,袁道先,等. 黄龙洞年轻石笋的210Pb测年研究[J]. 地质论评,2010,56(4):543-548.[Yang Xunlin, Zhang Pingzhong, Yuan Daoxian, et al. 210Pb dating of young stalagmite from Huanglong Cave[J]. Geological Review, 2010, 56(4): 543-548.]
[7]
张月明,杨勋林,黄帆,等. 重庆丰都高分辨率石笋δ13C记录与AD1250-1750a季风气候变化[J]. 西南大学学报:自然科学版,2013,35(3):117-123.[Zhang Yueming, Yang Xunlin, Huang Fan, et al. A high—resolution stalagmite δ13C record from Shuiming Cave over the past 500 years[J]. Journal of Southwest University Natural Science Edition, 2013, 35(3): 117-123.]
[8]
黄俊华,胡超涌,周群峰,等. 长江中游和尚洞石笋的高分辨率同位素、微量元素记录及古气候研究[J]. 沉积学报,2002,20(3):442-446.[Huang Junhua, Hu Chaoyong, Zhou Qunfeng, et al. Study on high-resolution carbon, oxygen isotope and trace element records and paleoclimate from Heshang Cave, the middle reach of the Yangtsz River[J]. Acta Sedimentologica Sinica, 2002, 20(3): 442-446.]
[9]
姚春彦,马东升,丁海峰,等. 新疆阿克苏地区早寒武世碳酸盐岩沉积环境微量元素和碳同位素证据[J]. 地球化学,2011,40(1):63-71.[Yao Chunyan, Ma Dongsheng Ding Haifeng, et al. Reconstruction of the Early Cambrian carbonate sedimentary environment in Akesu area of Xinjiang, China: Evidence from trace elements and carbon isotope excursion[J]. Geochimica, 2011, 40(1): 63-71.]
[10]
赵兴媛,季宏兵,朱先芳,等. 黔中小流域水体悬浮物与沉积物微量元素地球化学特征及物源指示[J]. 地球化学,2012,41(3):250-265.[Zhao Xingyuan, Ji Hongbing, Zhu Xianfang, et al. Geochemical characteristics of trace elements in suspended matters and sediments in a small watershed of the central Guizhou Province and their provenance implications[J]. Geochimica, 2012, 41(3): 250-265.]
[11]
李彬,袁道先,林玉石,等. 洞穴次生化学沉积物中Mg、Sr、Ca及其比值的环境指代意义[J]. 中国岩溶,2000,19(2):115-122.[Li Bin, Yuan Daoxian, Lin Yushi, et al. The ratios of Mg/Ca, Mg/Sr in the speleothems and their environmental significance in Guilin area[J]. Carsologica Sinica, 2000, 19(2): 115-122.]
[12]
王建力,何潇,李清,等. 重庆新崖洞4.5ka以来气候变化的石笋微量元素记录及环境意义[J]. 地理科学,2010,30(6):910-915.[Wang Jianli, He Xiao, Li Qing, et al. Climate change since 4.5 ka BP recorded by trace elements in a stalagmite from Xinya Cave in Chongqing[J]. Scientia Geographica Sinica, 2010, 30(6): 910-915.]
[13]
Roberts M S, Smart P L, Baker A. Annual trace element variations in a Holocene speleothem[J]. Earth and Planetary Science Letters, 1998, 154(14): 237-246.
[14]
Johnson K R, Hu C Y, Belshaw N S, et al. Seasonal trace-element and stable-isotope variations in a Chinese speleothem: The potential for high resolution paleomonsoon reconstruction[J]. Earth and Planetary Science Letters, 2006, 244(1/2): 394-407.
[15]
马志邦,李红春,夏明,等. 距今3ka来京东地区的古温度变化:石笋Mg/Sr记录[J].科学通报,2002,47(23):1829-1834.[Ma Zhibang, Li Hongchun, Xia Ming, et al. Paleotemperature changes over the past 3000 years in eastern Beijing, China: A reconstruction based on Mg/Sr records in a stalagmite[J]. Chinese Science Bulletin, 2002, 47(23): 1829-1834.]
[16]
周厚云,王悦,黄柳苑,等. 氧同位素阶段5c~d时期川东北石笋MgSr和Ba记录及其意义[J]. 科学通报,2011,56(33):2791-2796.[Zhou Houyun, Wang Yue, Huang Liuyuan, et al. Speleothem Mg, Sr and Barecords during the MIS 5c-d, and implications for paleoclimate change in NE Sichuan, Central China[J]. Chinese Science Bulletin, 2011, 56(33): 2791-2796.]
[17]
李清,王建力,李红春,等. 重庆地区石笋记录中Mg/Ca比值及古气候意义[J]. 中国岩溶2008,27(2):145-150.[Li Qing, Wang Jianli, Li Hongchun, et al. Climatic significance of the Mg/Ca ratio from speleothems in Chongqing[J]. Carsologica Sinica, 2008, 27(2): 145-150.]
[18]
Shen C C, Edwards R L, Cheng Hai, et al. Uranium and thorium isotopic and concentration measurements by magnetic sector inductively coupled plasma mass spectrometry[J]. Chemical Geology, 2002, 185(3/4): 165-178.
[19]
Cheng Hai, Adkins J, Edwards R L, et al. U-Th dating of deep-sea corals[J]. Geochimica et Cosmochimica Acta, 2000, 64(14): 2401-2416.
[20]
郑立娜,周厚云,朱照宇. 洞穴次生碳酸盐沉积的Mg/Ca与Sr/Ca比值研究进展—兼论洞穴次生沉积物Mg/Ca与Sr/Ca的影响机制[J]. 中国岩溶,2010,29(2):212-218.[Zheng Lina, Zhou Houyun, Zhu Zhaoyu. Progress of study on Mg/Ca and Sr/Ca ratios of speleothem in caves[J]. Carsologica Sinica, 2010, 29(2): 212-218.]
[21]
GascoyneM , Ford D C. Uranium-series ages of speleothem from northwest England: correlation with Quaternary climate[J]. Philosophical Transactions of the Royal Society of London. Series B: Biological Sciences, 1983, 301(1104): 143-164.
[22]
Fairchild I J, Borsato A, Tooth A F, et al. Controls on trace element (Sr-Mg) compositions of carbonate cave waters: implications for speleothem climatic records[J]. Chemical Geology, 2000, 166(3/4): 255-269.
[23]
Holland H D, Kirsipu T V, Huebner J S, et al. On some aspects of the chemical evolution of cave waters[J]. The Journal of Geology, 1964, 72(1): 36-67.
[24]
Zhou Houyun, Feng Yuexing, Zhao Jianxin, et al. Deglacial variations of Sr and 87Sr/86Sr ratio recorded by a stalagmite from Central China and their association with past climate and environment[J]. Chemical Geology, 2009, 268(3/4): 233-247.
[25]
Treble P, Shelley J M G, Chappell J. Comparison of high-resolution sub-annual records of trace elements in a modern(1911-1992) speleothem with instrumental climate data from southwest Australia[J]. Earth and Planetary Science Letters, 2003, 216(1/2): 141-153.
[26]
Berger A. Long-term variations of caloric insolation resulting from the Earth's orbital elements[J]. Quaternary Research, 1978, 9(2):139-167.
[27]
Dansgaard W, Johnson S J, Clausen H B,et al. Evidence for general instability of past climate from a 250-kyr ice-core record[J]. Nature, 1993, 364(6434): 218-220.
[28]
Zhao M, Beveridge N A S, Shackleton N J, et al. Molecular stratigraphy of cores off Northwest Africa: Sea surface temperature history over the last 80 ka[J]. Paleoceanography, 1995, 10(3): 661-675.
[29]
Hellstrom J C, McCulloch M T.Multi-proxy constraints on the climatic significance of trace element records from a New Zealand speleothem[J]. Earth and Planetary Science Letters, 2000, 179(2): 287-297.
[30]
Burton E A, Walter L M. The effects of PCO2 and temperature on magnesium incorporation in calcite in seawater and MgCl2-CaCl2 solution[J]. Geochimica et Cosmochimica Acta, 1991, 55(3): 777-785.
[31]
杨勋林,陈发虎,袁道先,等. 高分辨率石笋记录的三峡库区小冰期气候变化[J]. 地理科学,2013,33(5):629-633.[Yang Xunlin, Chen Fahu, Yuan Daoxian, et al. Climate change during little ice age with high-resolution stalagmite record in the Three-Gorges Reservoir Area[J]. Scientia Geographica Sinica, 2013, 33(5): 629-633.]
[32]
刘敬华,张平中,程海,等. 黄土高原西缘在AD 1875~2003 期间石笋氧同位素记录的季风降水变化与海气系统的联系[J]. 科学通报,2008,53(22):2801-2808.[Liu Jinghua, Zhang Pingzhong, Cheng Hai, et al. Asian summer monsoon precipitation recorded by stalagmite oxygen isotopic composition in the western Loess Plateau during AD1875-2003 and its linkage with ocean-atmosphere system[J]. Chinese Science Bulletin, 2008, 53(22): 2801-2808.]
[33]
安春雷,张平中,代志波,等. 中国黄土高原西缘甘肃万象洞MIS5石笋δ18O记录与南方地区石笋记录的对比研究[J]. 第四纪研究,2006,26(6):985-990.[An Chunlei, Zhang Pingzhong, Dai Zhibo, et al. Comparison of δ18O record during MIS 5 in Wanxiang Cave Stalagmite, Gansu province of western loess plateau and those of southern China Stalagmites[J]. Quaternary Sciences, 2006, 26(6): 985-990.]
[34]
Song S R, Chen C H, Lee M Y, et al. Newly discovered eastern dispersal of the Youngest Toba Tuff[J]. Marine Geology, 2000, 167(3/4): 303-312.
[35]
Clemens S C, Prell W L, Sun Y B. Orbital-scale timing and mechanisms driving Late Pleistocene Indo-Asian summer monsoons: Reinterpreting cave speleothem δ18O[J]. Paleoceanography, 2010, 25(4): PA4207, doi:10.1029/2010PA001926.
