ࡱ> "$!s jbjb kk] i &((((((,}`TT&&&& Ghյ&The YD record: timing of the Antarctic Cold Reversal and the atmospheric CO2 increase with respect to the YD event (Blunier et al., 1997), as deduced from the CH4 synchronization, the isotopics records of the GRIP, Byrd and Vostok ice cores, together with the CO2 record from Byrd. Raynaud, D., et al. (2000). The ice record of greenhouse gases: a view in the context of future changes. Quaternary Science Reviews 19: 9-17. Blunier, T., et al. (1997). Timing of temperature variations during the last deglaciation in Antarctica and the atmospheric CO2 increase with respect to the Younger Dryas event. Geophys. Res. Lett. 24: 2683-2686. KL`stv5OJPJQJnH >*OJPJQJnH OJPJQJnH H* $0d$d/ =!"#$% [4@4NormalCJOJPJQJmH <A@<Default Paragraph Font t{"RW`gnrKeith Alverson>pingguo:Desktop Folder:qsr overhead catptions:bipolardryas.txt@  @p@GTimes New Roman5Symbol3 Arial5 Geneva3Times"qh I I$0RThe YD record: timing of the Antarctic Cold Reversal and the atmospheric CO2 increase with respect to the YD event (Blunier et Keith AlversonKeith Alverson Oh+'0$<HX p|   'The YD record: timing of the Antarctic Cold Reversal and the atmospheric CO2 increase with respect to the YD event (Blunier et he Keith AlversonteitNormallKeith Alversont1itMicrosoft Word 8.0n@@z@NƝ ՜.+,0l hp  L'PAGESr The YD record: timing of the Antarctic Cold Reversal and the atmospheric CO2 increase with respect to the YD event (Blunier et Title  #Root Entry Fy.%1Table WordDocumentSummaryInformation(DocumentSummaryInformation8CompObjXObjectPooly.y. FMicrosoft Word DocumentNB6WWord.Document.8