刘东生,谭 明,秦小光等.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):41～51L iu Tungsheng,Tan M ing,Q in Xiaoguang et a l.D iscovery ofm icrobedding in speleothem s in China and its significance in thestudy of global change.Q ua ternary S ciences,1997,(1):41～51
[2]
汪永进,孔兴功,邵晓华等.末次盛冰期百年尺度气候变化的南京石笋记录.第四纪研究,2002,22(3):243～251Wang Yongjin,Kong Xinggong,Shao Xiaohua et a.lCentury
[3]
scaleclimatic oscillations during the last glacial maximum recorded in astalagm ite from Nanjing.Quaternary Sciences,2002,22(3):243～251
[4]
谭 明.中国高分辨率记录与全球变化.第四纪研究,2004,24(4):455～462Tan M ing.H ihh
[5]
resolution climatic recorda of China and globalchang.Q ua ternary S ciences,2004,24(4):455～462
[6]
程 海,艾思本,王先锋等.中国南方石笋氧同位素记录的重要意义.第四纪研究,2005,25(2):157～163Cheng Hai,Edwards R L,W ang Xianfeng et a.lOxygen isotoperecords of stalagm ites from Southern China.Q ua ternary S ciences,2005,25(2):157～163
[7]
刘浴辉,胡超涌,黄俊华等.长江中游石笋年层厚度作为东亚夏季风强度代用指标的研究.第四纪研究,2005,25(2):228～234L iu Yuhui,Hu Chaoyong,Huang Junhua et a.lThe research of thelayer thickness of the stalagm ite from the m iddle reaches of theYangtze R iver taken as an p roxy of the East A sian summer monsoonintensity.Q uaterna ry S ciences,2005,25(2):228～234
(6):985～990An Chunlei,Zhang Pingzhong,Dai Zhibo et a .lComparison ofδ18Orecord in W anxiang Cave stalagm ite,Gansu Province of W esternLoess Plateau and those of Southern China staglagm ites.Q ua terna ryS ciences,2006,26(6):985～990
[10]
W ang Y J,Cheng H,Edwards R L et a .lA high2resolution absolute2dated Late Pleistocene monsoon record from Hulu Cave,China.S cience,2001,294:2345～2348
[11]
Yuan D X,Cheng H,Edwards R L et a l.Tim ing,duration,andtransitions of the last interglacial A sian Monsoon.Science,2004,304:575～578
[12]
D rysdale R N,Zanchetta G,Hellstrom J C et a .lStalagm ite evidencefor the p recise tim ing of North A tlantic cold events during the earlylast glacia.lGeology,2007,35(1):77～80
[13]
Kelly M J,Edwards R L,Cheng H et a .lH igh resolutioncharacterization of the A sian Monsoon between 146,000 and 99,000years B
[14]
P1from Dongge Cave,China and global correlation of eventssurrounding Term inationⅡ.Palaeogeography,Pa laeoclim a tology,Palaeoecology,2006,236(1～2):20～38
[15]
North Greenland Ice Core ProjectMembers.H igh2resolution record ofNorthern Hem isphere climate extending into the last interglacialperiod North Greenland Ice Core Project Members.N a ture,2004,431:147～151
[16]
Dansgaard W,Johnsen S J,Clausen H B et a .lEvidence for generalinstability of past climate from a 250
[17]
kyr ice2core record.N ature,1993,364:218～220
[18]
Grootes P M,Stuiver M,W hite J W C et a .lComparison of oxygenisotope records from the GISP2 and GR IP Greenland ice cores.N ature,1993,366:552～554
[19]
Denniston R F,A smerom Y,Polyak V et a l.Synchronous m illennial2scale climatic changes in the Great Basin and the North A tlanticduring the last interglacial.Geology,2007,35(7):619～622
[20]
Cheng Hai,Edwards R L,W ang Yongjin et a .lA penultimate glacialmonsoon record from Hulu Cave and two
[21]
phase glacial term inations.Geology,2006,34(3):217～220
[22]
Sima A,Paul A,Schulz M.The Younger D ryas———An intrinsicfeature of Late Pleistocene climate change at m illennial timescales.Earth and P lanetary S cience L etters,2004,222(3～4):741～750
