[1] Jensen K.Some west Baltic pollen diagrams[J].Quartar,1938,1:124-139 [2] Bond G,Broecker W,Johnsen S,et al.Correlations between climate records from North Atlantic sediments and Greenland ice[J].Nature,1993,365:143-147. [3] Leverington D W,Mann J D,Teller J T.Changes in the bathymetry and volume of glacial Lake Agassiz between 9200 and 7700 C-14 yr BP[J].Quaternary Research,2002,57(2):244-252. [4] Manabe S,Stouffer R J.Century-scale effects of increased atmospheric CO2 on the ocean atmosphere system[J].Nature,1993,364:215-218. [5] Stocker T F,Schmittner A.Influence of CO2 emission rates on the stability of the thermohaline circulation[J].Nature,1997,388:862-865. [6] Taylor K C,Lamorey G W,Doyle G A,et al.The flickering switch of late Pleistocene climatic change[J].Nature,1993,361:432-436. [7] Stuiver M,Grootes P M.GISP2 oxygen isotope ratios[J].Quaternary Research,2000,53(3):277-284. [8] Mayewski P A,Meeker L D,Whitlow S,et al.Changes in atmospheric circulation and ocean ice cover over the North Atlantic during the last 41,000 years[J].Science,1994,263:1747-1751. [9] Brook E J,Sowers T,Orchardo J.Rapid variations in atmospheric methane concentration during the past 110,000 years[J].Science,1996,273:1087-1091. [10] Hughen K A,Overpeck J T,Peterson L C,et al.Rapid climate changes in the tropical Atlantic region during the last deglaciation[J].Nature,1996,380:51-54. [11] Yu Z.Ecosystem response to Late glacial and early Holocene climate oscillations in the Great Lakes region of North America[J].Quaternary Science Reviews,2000,19:1723-1747. [12] Shuman B,Thompson W,Bartlein P,et al.The anatomy of a climatic oscillation:vegetation change in eastern North America during the Younger Dryas chronozone[J].Quaternary Science Reviews,2002,21:1777-1791 [13] Hammarlund D,Edwards T W D,Bjorck D,et al.Climate and environment during the Younger Dryas (GS-1) as reflected by composite stable isotope records of lacustrine carbonates at Torreberga,southern Sweden[J].Quaternary Science,1999,14:17-28. [14] Broecker W S.Does the Trigger for abrupt climate change reside in the ocean or in the atmosphere[J].Science,2003,300:1519-1522. [15] Wang Youqing,Yao Tandong.Progresses in the studies of abrupt in ice cores during the Last Glacial-Interglacial cycle[J].Journal of Glaciology and Geocryology,2000,24(5):550-558.[王有清,姚檀栋.冰芯记录中末次间冰期-冰期旋回气候突变事件的研究进展[J].冰川冻土,2000,24(5):550-558] [16] Yi SH,Saito Y.Latest Pleistocene climate variation of the East Asian monsoon from pollen records of two East China regions[J].Quaternary International,2004,121:75-87. [17] Zhou Weijian,Li Xiaoqiang,Dong Guangrong,et al.High resolution turfy record in desert/loess transition area during Younger Dryas period[J].Science in China(Series D),1996,26(2):118-124.[周卫健,李小强,董光荣,等.新仙女木期沙漠/黄土过渡带高分辨率泥炭记录[J].中国科学:(D辑),1996,26(2):118-124.] [18] Gasse F,Arnold M,Fontes J C,et al.A 13,000-year climate record from western Tibet[J].Nature,1991,353:742-745. [19] Yang Zhihong,Yao Tandong.Younger Dryas event recorded in Guliya ice core[J].Chinese Science Bulletin,1997,42(18):1975-1978.[杨志红,姚檀栋.古里雅冰芯中的新仙女木期事件记录[J].科学通报,1997,42(18):1975-1978. [20] Zhong Wei.The Younger Dryas cooling event reflected by carbonate isotopic data from Bosten Lake sediment during late deglaciation[J].Marine Geology Quaternary Geology.1998,18(3):87-94[钟巍.博斯腾湖末次冰消期新仙女木事件的碳酸盐同位素记录[J].海洋地质与第四纪地质,1998,18(3):87-94.] [21] Li Yuanfang,Zhang Qingsong,Li Bingyuan.Stracod fauna and environmental changes during the past 17000 years in the western Tibet[J].Acta Geographica Sinica,1994,49(1):46-54.[李元芳,张青松,李炳元.青藏高原西北17000年以来的介形类及环境演变[J].地理学报,1994,49(1):46-54.] [22] Liu Xingqi,Shen Jie,Wang Sumin,et al.Pollen record and the evolution of palaeoclimatology over 16 ka in Qinghai Lake[J].Chinese Science Bulletin,2002,47(17):1351-1354.[刘兴起,沈吉,王苏民,等.青海湖16 ka以来的花粉记录及其古气候古环境演化[J].科学通报,2002,47(17):1351-1354.] [23] Wang Sumin,Jie Lei,Yang Xiangdong,et al.Younger Dryas records from sediment of Dalainuoer Lake,Inner-Mongolia[J].Chinese Science Bulletin,1994,39(4):348-351.[王苏民,吉磊,羊向东,等.内蒙古达赉诺尔湖泊沉积物中的新仙女木事件记录[J].科学通报,1994,39(4):348-351.] [24] An Z,Porter S,Zhou W.Episode of strengthened summer monsoon climate of Younger Dryas age on the loess plateau of central of China[J].Quaternary Research,1993,62:413-461. [25] Wang Pinxian,Li Baohua.The Younger Dryas event of western Pacific[J].Science in China(Series D),1996,26(5):452-460.[汪品先,李保华.西太平洋边缘海的"新仙女木"事件[J].中国科学(D辑),1996,26(5):452-460] [26] Lemcke G,Sturm M.δ18O and trace element measurements as proxy for the reconstruction of climate changes at Lake Van (Turkey):preliminary results[M]//Third Millennium BC Climate Change and Old World Collapse,NATO ASI Ser,Ser.1.,49,1996:653-678. [27] Abell P I,Plug I.The Pleistocene/Holocene transition in South Africa:evidence for the Younger Dryas event[J].Global and Planetary Change,2000,26:173-179. [28] Scott L,Thackeray J F.Multivariate analysis of Late Plesitocene and Holocene pollen spectra from Wonderkrater,Transvaal,South Africa[J].Suid-Afrikaanse Tydskrif vir Wetenskap.1987,83:93-98. [29] Coetzee J A.Pollen analytical studies in East and Central Africa[J].Palaeoecol.Afr.,1967,3:1-146. [30] Roberts N,Taieb M,Barker P,et al.Timing of the Younger Dryas event in East Africa from lake level changes[J].Nature,1993,366:146-148. [31] Maley J,Brenac P.Vegetation dynamics,palaeoenvironments and climatic changes in the forests of western Cameroon during the last 28,000 years B P[J].Review of Palaeobotany and Palynology,1998,99(2):157-187. [32] Stager J C,Mayewski P A,Meeker L D.Cooling cycles,Heinrich event 1,and the desiccation of Lake Victoria[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2002,183(1/2):169-178. [33] Gasse F.Diatom-inferred salinity and carbonate oxygen isotopes in Holocene waterbodies of the western Sahara and Sahel (Africa)[J].Quaternary Science Reviews,2002,21(7):737-767. [34] Clapperton C M,Hall M,Mothes P,et al.A Younger Dryas icecap in the Ecuadorian Andes[J].Quaternary Research,1997,47:13-28. [35] Van't Veer R,Islebe GA,Hooghiemstra H.Climatic change during the Younger Dryas chron in northern South America:a test of the evidence[J].Quaternary Science Reviews,2000,19(17/18):1821-1835. [36] Hajdas I,Bonani G,Moreno P I,et al.Precise radiocarbon dating of Late-Glacial cooling in mid-latitude South America[J].Quaternary Research,2003,59(1):70-78. [37] Cwynar L C,Levesque A J,Mayle F E,et al.Wisconsinan Late-glacial environmental change in New Brunswick:a regional synthesis[J].Journal of Quaternary Science,1994,9(2):161-164. [38] Moreno P I,Jacobson G L,Lowell T V,et al.Interhemispheric climate links revealed by a late-glacial cooling episode in southern Chile[J].Nature,2001,409:804-808. [39] Strelin J A,Malagnino E C.Late-glacial history of Lago Argentino,Argentina,and age of the Puerto Bandera moraines[J].Quaternary Research,2000,54(3):339-347. [40] Thompson L G,Thompson E M,Henderson K A.Ice-core palaeoclimate records in tropical South America since the Last Glacial Maximum[J].Journal of Quaternary Science,2000,15(4):377-394. [41] Heine.K,Heine J T.Late Glacial climatic fluctuations in Ecuador:Glacier retreat during the Younger Dryas Time[J].Arctic and Alpine Researc,1996,28(4):496-501. [42] Bennett K D,Haberle S G,Lumley S H.The Last Glacial-Holocene Transition in Southern Chile[J].Science,2000,290:325-328 [43] Glasser N F,Harrison S,Winchester V,et al.Late Pleistocene and Holocene palaeoclimate and glacier fluctuations in Patagonia[J].Global and Planetary Change,2004,43(1/2):79-101. [44] Denton G H,Hendy C H.Younger Dryas age advance of Franz-Josef Glacier in the Southern Alps of New Zealand[J].Science,1994,264:1434-1437. [45] Andres M S,Bernasconi S M,McKenzie J A,et al.Southern Ocean deglacial record supports global Younger Dryas[J] ,Earth Planet Science Letters,2003,216 (4):515-524. [46] Newnham R M,Lowe D J.Fine-resolution pollen record of late-glacial climate reversal from New Zealand[J].Geology,2000,28 (8):759-762. [47] Singer C,Shulmeister J,McLea B.Evidence against a significant Younger Dryas cooling event in New Zealand[J].Science,1998,281:812-814. [48] Matt S,Glone M,Chris S M.Late-glacial and Holocene vegetation and climatic history of the Cass Basin,central South Island,New Zealand[J].Quaternary Research,2004,62(3):267-279. [49] Turney C S M,McGlone M S,Wilmshurst J M.Asynchronous climate change between New Zealand and the North Atlantic during the last deglaciation[J].Geology,2003,31(3):223-226. [50] Sowers T,Bender M.Climate records covering the last deglaciation[J].Science,1995,269:210-214. [51] Broecker W S,Kennett J P,Flower B P,et al.routing of meltwater from the Laurentide Ice Sheet during the Younger Dryas cold episode[J].Nature,1989,341:318-321. [52] Stocker T F.The seesaw effect[J].Science,1998,282:61-62. [53] Steig E J,Brook E J,White J W C,et al.Synchronous climate changes in Antarctica and the North Atlantic[J].Science,1998,282:92-95. [54] Morgan V,Delmotte M,Van O,et al.Relative timing of deglacial climate events in Antarctica and Greenland[J].Science,2002,297:1862-1864. [55] Bond G,Showers W,Cheseby M,et al.A pervasive millennial-scale cycle in North Atlantic Holocene and Glacial climates[J].Science,1997,278:1257-1266. [56] Berger W H.The Younger Dryas cold spell-quest for causes[J].Palaeogeography,Palaeoclimatology,Palaeoecology,1990,89:219-237. [57] Teller J T,Leverington D W,Mann J D.Freshwater outbursts to the oceans from glacial Lake Agassiz and their role in climate change during the last deglaciation[J].Quaternary Science Reviews,2002,21(8-9):879-887. [58] Rahmstorf S.Bifurcations of the Atlantic thermohaline circulation in response to changes in the hydrological cycle[J].Nature,1995,378:145-149. [59] Broecker W S,Denton G H.the role of ocean-atmosphere reorganizations in glacial cycles[J].Geochimica et Cosmochimica Acta,1989,53(10):2465-2501. [60] Boyle E A,Keigwin L.North Atlantic thermohaline circulation during the past 20,000 years linked to high-latitude surface temperature[J].Nature,1987,330:35-40. [61] Andrew J W,Oleg A S,Peter U C,et al.Mitrovica meltwater pulse 1A from Antarctica as a trigger of the B lling-Aller d warm interval[J].Science,2003,299:1709-1713. [62] Seidov D,Haupt B J,Barron E J,et al.Ocean bi-polar seesaw and climate:Southern versus northern meltwater impacts[M]//AGU Geophysical Monograph 126:The Oceans and Rapid Climate Change:Past,Present,and Future.Washington,DC:American Geophysical Union,2001:147-168 [63] Alley R B,Clark P U.The deglaciation of the northern hemisphere:A global perspective[J].Annual Review of Earth and Planetary Sciences.1999,27,149-182. [64] Clark P U,Mitrovica J X,Milneet G A,et al.Sea-Level Fingerprinting as a Direct Test for the Source of Global Meltwater Pulse 1A[J].Science,2002,295:2438-2441. [65] Clark P U,Marshall S J,Clarke G K C,et al.Freshwater Forcing of Abrupt Climate Change During the Last Glaciation[J].Science,2001,293,283-287. [66] Kanfoush S L,Hodell D A,Charles C D,et al.Millennial-scale instability of the Antarctic Ice Sheet during the Last Glaciation[J].Science,2000,288,1815-1819. [67] Zhou W J,Donahue D J,Porter S C,et al.Variability of monsoon climate in East Asia at the end of the Last Glaciation[J].Quaternary Research,1996,46(3):219-229. [68] Rasmussen T L,Thomsen E.The role of the North Atlantic Drift in the millennial timescale glacial climate fluctuations[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2004,210(1):101-116. [69] Jouzel J,Vaikmae R,Petit J R,et al.The 2-step shape and timing of the last deglaciation in Antarctica[J].Climate Dynamics,1995,11(3):151-161. [70] Bard E,Rostek F,Sonzogni C.Interhemispheric synchrony of the last deglaciation inferred from alkenone palaeothermometry[J].Nature,1997,385,707-710. [71] Hughen K A,Overpeck J A,Lehman S J.Deglacial changes in ocean circulation from an extended radiocarbon calibration[J].Nature,1998,391:65-68. [72] Bjorck S,Kromer B,Johnsen S,et al.Synchronized terrestrial atmospheric deglacial records around the North Atlantic[J].Science,1996,274:1155-1160. [73] Broecker W S,Peng T H.Tracers in the Sea[M].Eldigio,Palisades,NY,1982. [74] Goslar T,Wohlfarth B,Bjorck S,et al.Variations of atmospheric C-14 concentrations over the Allerd-Younger Dryas transition[J].Climate Dynamics,1999,15(1):29-42. [75] Broecker W S.Paleocean circulation during the last deglaciation:a bipolar seesaw?[J].Paleoceanography 1998,13(2):119-12. [76] Hoyt D V,Schatten K H.The Role of the Sun in Climate Change[M].Oxford:Oxford University Press,,1997:1-279. [77] Van Geel B,Raspopov O M,Renssen H,et al.The role of solar forcing upon climate change[J].Quaternary Science Reviews.1999,18(3):331-338. [78] Hastenrath S.On the meridional heat transports in the world ocean[J].Journal of Physical Oceanography,1982,12:922-927. [79] Renssen H,van Geel B,van der Plicht J,et al.Reduced solar activity as a trigger for the start of the Younger Dryas?[J].Quaternary International,2000,68:373-383. [80] Broecker W S,Henderson G M.The sequence of events surrounding Termination II and their implications for the cause of glacial-interglacial CO2 changes[J].Paleoceanography,1998,13:352-364. [81] Shackleton N.The 100,000 year ice age cycle identified and found to lag temperature,dioxide and orbital eccentricity[J].Science,2000,289:1897-1902. [82] Cane M.clement A.Mechanisms of global climate change at millennial time scales[M]//AGU Geophysical Monograph 112.Washington DC:American Geophysical Union,1999:373-383. |