Blunier T, Chappellaz J, Scwander J, et al. 1998. Asynchrony of Antarctic and Greenland climate changes during the last glacial period. Nature, 394:739～743.
[4]
Bond G C, Broecker W S, Jonnsen S J, et al. 1993. Correlations between climate records from North Atlantic sediments and Greenland ice. Nature, 365:143～147.
[5]
Broecker W S. 1994. Massive iceberg discharges as triggers for global climate change. Nature, 372: 421～ 424.
[6]
Dansgaard W, Clausen H B, Gundestrup N, et al. 1982. A new Greenland deep ice core. Science, 218:1273～1277.
[7]
Dorale J A, Edward R L, Ito E, et al. 1998. Climate and vegetation history of the midcontinent from 75 to 25 ka:A speleothem record from Crevice Cave, Missouri, USA. Science, 282: 1871～1874.
[8]
Frumkin A, Ford D C, Schwarcz H P, et al. 1999. Continental oxygen isotopic of the last 170,000 years in Jerusalem. Quaternary Research, 51:317～327.
[9]
Guo Z T, Peng S Z, Liu T S. 2001. Millennial-scale oscillations of loess weathering over the last glacial period. PAGES, 9(2): 9.
[10]
Hendy C H, Wilson A T. 1968. Paleoclimatic data from speleothems.Nature, 219:48～ 51.
[11]
Johnsen S J, Clausen H B, Dansgaard W. 1992. Irregular glacial interstadials recorded in a new Greenland ice core. Nature, 359:311～313.
[12]
Lang C, Leuenberger M, Schwander J, et al. 1999. 16℃ rapid temperature variation in central Greenland 70,000 years ago. Science,286: 934～937.
[13]
Ninkovich D, Shackleton N J, Abdel-Monem A A, et al. 1978. K-Ar age of the Pleistocene eruption of Toba, north Sumatra. Nature,276:574～577.
[14]
Porter S C, An Z S. 1995. Correlation between climate events in the North Atlantic and China during the last glaciation. Nature, 375:305～308.
[15]
Schulz H, Rad U, Erlenkeuser H. 1998. Correlation between Arabian Sea and Greenland climate oscillations of the past 110,000 years.Nature, 393: 54～57.
[16]
Wu J Y, Wang Y J, Cheng H, et al. 2002. A high resolution stalagmite O-C isotope record from Nanjing and its rapid response to climatic events. Chinese Science Bulletin, 47(2):139～142.
[17]
Wei K Q, Lin R F. 1994. The influence of the monsoon climate on the isotopic compositions of precipitation in China. Geochimica, 23(1): 33 ～ 41 (in Chinese with English abstract).
[18]
Zielinski G A, Mayewski P A, Meeker L D, et al. 1996. Potential atmospheric impact of the Toba mega-eruption 71000 years ago.Geophvsical Research Letter, 23(8): 837～840.
Alley R B, Meese D A, Shuman C A, et al. 1993. Abrupt increase in Greenland snow accumulation at the end of the Younger Dryas event. Nature, 362:527～529.
[23]
Behl R J, Kennett J P. 1996. Evidence for brief interstadial events in the Santa Barbara Basin, NE Pacific during the past 60 Kyr. Nature, 379:243～246.
[24]
Blunier T, Brook E J. 2001. Timing of millennial-scale climate change in Antarctica and Greenland during the last glacial period. Science, 291:109～112.
[25]
Bond G C, Lotti R. 1995. Iceberg discharges into the North Atlantic on millennial time scales during the last glaciation. Nature, 267:1005～1010.
[26]
Chesner C A, Rose W I, Deino A, et al. 1991. Eruption history of Earth\'s largest Quaternary caldera (Toba, Indonisla) clarified.Geology, 19: 200～203.
[27]
Dansgaard W, Johnsen S J, Clausen H B, et al. 1993. Evidence for general instability of past climate from a 250-Kyr ice-core record.Nature, 364:218～220.
[28]
Dorale J A, Gonzalez L A, Reagan M K, et al. 1992. A high resolution record of Holocene climate change in speleothem calcite from Cold Water Cave, northeast Iowa. Science, 258: 1626～1630.
[29]
Edwards R L, Chen J H, Wasserburg G J. 1986/87. 238U-234U 230Th-232Th systematics and the precise measurement of time over the past 500,000 years. Earth and Planetary Science Letters, 81:175～192.
[30]
Grimm E C, Jacobson G L, Watts J W A, et al. 1993. A 50,000 year record of climate oscillations from Florida and its temporal correlation with the Heinrich events. Science, 261:198～200.
[31]
Guiot J, de Beaaulieu J L, Cheddadi R D, et al. 1993. The climate in Western Europe during the last glacial/interglacial cycle derived from pollen and insect remains. PALEO3, 103: 73～93.
[32]
Heinrich H. 1988. Origin and consequences of cyclic ice rafting in the northeast Atlantic Ocean during the past 130,000 years. Quaternary Research, 29:142 ～ 152.
[33]
Hendy C H. 1971. The isotopic geochemistry of spelethems--I.The calculation of the effects of different models of formation on the isotopic composition of speleothems and their applicability as palaeoclimatic indicators. Geochimica et Cosmochimica Acta, 35:801～824.
[34]
Leuschner D C, Sirocko F. 2000. The low-latitude monsoon climate during Dansgaard-Oeschger cycles and Heinrich Events. Quaternary Science Reviews, 19: 243 ～ 254.
[35]
Li W X, Lundberg J, Dickin A P, et al. 1989. High-precision massspectrometric uranium-series dating of cave deposits and implications for palaeoclimate studies. Nature, 339: 534～ 536.
[36]
McCrea J M. 1950. The isotopic chemistry of carbonates and a paleotemperature-scale. Journal of Chemical Physics, 18: 849～861.
[37]
Meese D A, Gow A J, Alley R B, et al. 1997. The Greenland ice sheet project 2 depth-age scale methods and results. Journal of Geophysical Research, 102 ( c 12 ): 26411 ～ 26423.
[38]
O\'Nell J R, Clayton R N, Mayeda T K. 1969. Oxygen isotope fractionation in divalent metal carbonates. The Journal of Chemical Physics, 51:5547～5559.
[39]
Phillips F M, Campbell A\'R, Smith G I, et al. 1994. Interstadial climatic cycles: a link between western North America and Greenland. Geology, 22 : 1115～1118.
[40]
Rose W I, Chesner C A. 1987. Dispersal of ash in the great Toba eruption, 75ka. Geology, 15:913～917.
[41]
Rose W I, Chesner C A. 1990. Worldwide dispersal of ash and gases from earth\'s largest known eruption: Toba, Sumatra, 75 ka.PALEO3, 89:269～275.
[42]
Wang Y J, Wu J Y, Wu J Q, et al. 2001. Correlation between highresolution climate records from a Nanjing stalagmite and GRIP ice core during the last glaciation. Science in China (Series D), 44(1):14～23.
[43]
Zheng S H, Hou F G, Ni B L. 1983. The studies of hydrogen and oxygen stable isotopes in a atmospheric precipitation in China.Chinese Science Bulletin, 13:801～806 (in Chinese).
