[l] Reille M，Andifeu V.Late Pleistocene and Holocene in the Lourdes basin，Western Pyrenees，France：New pollen analytical land chronological data. Vegetation History and Archaeobotany，1995，4(1)：l-21．
[2] Levesque A J，Mayle F E，Walker I K，et al.A previously unrecognized late-glacial cold event in eastern North American.Nature,1993,361：623-626．
[3] Walker M J，Harkness D D． Radiocarbon dating the Devensian Lateglacial in Britain: new evidence from Llanilid,South Wales.Journal of Quaternary Science，1990，5：135-144.
[4] Lehman S J，Keigwin L D.Sudden changes in North Atlantic circulation during the late deglaciation，l992，356；757-762．
[5] Koc Karpuz N,Jansen E. A high-resolution diatom record of the last deglaciation from the SE Norwegian Sea:documentation of rapid climatic changes.Paleoceanography，l992，7(4)：499-520.
[6] Kromer B,Becker B. German oak and pine ¹⁴C calibration,7200 BC to 9600 BC. Radiocabon,1993,35：125-135．
[7] Goslar T，Kuc M，Ralsh-Jasiewiczowa K,et al.High resolution lacustrine record of the late glacial/Holocene transition in central Europe. Quaternary Science Review,1993，12:287-294．
[8] Hohnsen S J，Clausen H B，Dansgaard W,et al. Irregular glacial intrstadials recorded in a new Greenland ice core.Nature，l992，356：311-313．
[9] Taylor K C，Lamorey G W，Doyle G A，et al.The flickering switch of late Pleistocene climate chang.Nature，1993，361：432-436.
[l0] Alley R B，Meese D A,Shuman C A，et al.Abrupt increase in Greenland snow accumulation at the end of Younger Dryas event. Nature,1993，362：527-529．
[11] Edwards R L，Beck J W，Burr G S，et al．A large drop in atmosphere ¹⁴C/¹²C and reduced melting in the Younger Dryas,documented with ²³⁰Th ages of coral. Science,1993，260：962-968．
[12] Mitchell G F．The Shell Guide to Reading the Irish Landscape. Dublin: Country House,1986．1-228．
[13] Thop P．A moutain ice field of Loch Lomond Stadial age，west Granpians，Scotland.Boreas，1986,15:83-97．
[14] Huang Chun Chang，Environmental Changes in Western Ireland（Ph D Thesis of National University of Ireland，Dublin）.Xi'an：Shanxi Normal University Press，1994.
[15] Audrieu V,Huang C C,O'Connell M,et al. Late glacial vegetation and environment in Ireland: First results from four western sites. Quaternary Science Review,1994,12(8):681-705.
[16] von Grafenstein U,Erlenkeuser H,Kleinmann A,et al. High-frequency climatic oscillation during the late deglaciation as revealed by oxygen-istope records of benthic organism(Ammersee,southern Germany).Journal of Paleoliminology,1994,11:349-357．
[17] Atkinson T C,Briffa K R,Coope G R. Seansonal temperatures in Britain during the past 22 000 years,reconstructed using beetle remains. Nature,1987，325：587-592．
[18] Lowe J J,Coope G R．High resoution stratigraphy of the late glacial-interglacial transition and inferred climatic gradients.In:Funnell B.Palaeoclimate of the last Glacial/interglacial cycle.Special publication, 1994,2:47-52.
[19] Peteet D M. Younger Dryas in North America: modeling,data analysis and re-evaluation. In: Berger W. Abrupt Climatic Change. Dordrecht: Reidel, 1987．185-193．
[20] Mott R J，Grant D R, Stea R, et al．Late glacial climate oscillation in Atlantic Canada equivalent to the Allerod-Younger Dryas event. Nature,1986，323：247-250.
[21] Bond G，Broecker W，Johensen S，et al. Correlaion between climate records from North Atlantic sediment and Greenland ice.Nature,1993，365：143-147．
[22] Koc Karpuz N,Jansen E,Haflidason H.Palaeoceanographic reconstruction of surface ocean condition in the Greenland,Iceland and Norwegian Seas through the last 14 ka based on diatoms.Quaternary Science Review.1993,12：115-140．
[23] 汪品先，卞云华，李保华．等．西太平详边缘海的“新仙女木”事件．中国科学(D)，1996，26(5)：432-460.
[24] Fairbanks R G. A 17000-year glacioeustatic sea level record：influence of glacial melting rate on the Younger Dryas event.Nature，1989，342：637-642．
[25] Dansgaard W，White J W，Johnsen S J，et al．The abrupt termination of the Younger Dryas climate event.Nature，1989，339：532-533．
[26] Thompson L，Mosley-Thompson E，Henderson K，et al.Late glacial stage and post-Younger Dryas events.Global Biogeochemical Cycles，1995，269：46-50．
[27] Epstein S. The isotopic climatic records in the Allerod-Bolling-Younger Dryas and post-Younger Dryas events.Global Biogeochemical Cycles,l995，4：557-563．
[28] Broecker W，White J W，Johnsen S J,et al. Late glacial stage and Holocene tropical ice core records from Huascaran, Peru.Science,1989,341：318-321.
[29] Rind D，Peteet D, Broecher W, et al．The impact of cold North Atlantic Sea surface temperature on climate:implications for the Younger Dryas cooling(11-10 ka).Climate Dynamics,1986,1:3-33.
[30] Harvey L D．Modeling the Younger Dryas.Quaternary Science,1989,8：137-149．
[31] Genthon C，Barnola J M，Raynaud D．et al．Vostok ice core: climatic response to CO₂ and orbiatal forcing change over the last climatic cycle.Nature,1987，329：414-418.