[1]Berger W H，Labeyrie L D. Abrupt climate change—An introduction[C]//Berger W H，Labeyrie L D,eds. Abrupt Climate Change-Evidence and Implications. Dordrecht：Reidel，1987：3-22.
[2]Heinrich H. Origin and consequences of cyclic ice rafting in the northeast Atlantic Ocean during the past 130 000 years[J]. Quaternary Research,1988，29：143-152.
[3]Broecker W S，Bond G C，Klas M，et al. Origin of the northern Atlantic’s Heinrich events[J].Climate Dynaics，1992，6：265-273.
[4]Dansgaard W，Johnsen S J，Clausen H B，et al. Evidence for general instability of past climate from 1 250 ka ice-core record[J].Nature，1993，364：218-220.
[5]Bond G，Lotti R. Iceberg discharges into the North Atlantic on millennial time scales during the last glaciation[J].Science，1995，267：1 005-1 010.
[6]Oppo D W，McManus J F，Cullen J L. Abrupt climate events 500 000  to 340 000 years ago：Evience from subpolar North Atlantic sediments[J].Science，1998，279：1 335-1 338.
[7]Raymo M E，Ganley K，Carter S，et al. Millennial-scale climate instability during the early Pleistocene epoch[J].Nature，1998，392：699-702.
[8]McManus J F，Oppo D W，Cullen J L. A 0.5 million year record of millennial-scale climate variability in the North Atlantic[J].Science，1999，283：971-975.
[9]Helmke J P，Schulz M，Bauch H A. Sediment-color record from the northeast Atlantic reveals patterns of millennial-scale climate variability during the past 500 000 years[J].Quaternary Research，2002，57：49-57.
[10]Huang Wei,Jian Zhimin,Bühring C.The millennial scale climate fluctuations revealed by the records of color reflectance from ODP Site 1144 in the northern South China Sea[J].Marine Geology and Quaternary Geology，2003，23(3)：5-10. [黄维,翦知湣,Bühring C.南海北部ODP1144孔颜色反射率所揭示的千年尺度气候波动[J]. 海洋地质与第四纪地质，2003,23(3):5-10.]
[11]Bühring C，Sarnthein M，Erlenkeuser H. Toward a high-resolution stable isotope stratigraphy of the last 1.1 M.Y.：Site 1144，South China Sea[C]//Prell W L，Wang P X，Blum P，eds. Proceedings of the Ocean Drilling Program Scientific Results.2004，184：1-29.
[12]Shackleton N J，Hall N J，Pate D. Pliocene stable isotope stratigraphy of site 846[C]//Pisias N G，Mayer L A，Janecek T R，eds. Proceedings of the Ocean Drilling Program Scientific Results，1995，138：337-355.
[13]Tiedemann R，Sarnthein M，Shackleton N J. Astronomic timescale for the Pliocene Atlantic ¹⁸O and dust flux records from Ocean Drilling Program Site 659[J]. Paleoceanography，1994，9：619-638.
[14]Lear C H，Elderfield H，Wilson P A. Cenozoic deep-sea temperatures and global ice volumes from Mg/Ca in benthic foraminiferal calcite[J].Science，2000，287：269-272.
[15]Billups K，Schrag D P. Paleotemperatures and ice volume of the past 27 Myr revisited with paired Mg/Ca and ¹⁸O/¹⁶O measurements on benthic foraminifera[J].Paleoceanograpy， 2002，17：(3-1)-(3-11).
[16]Shackleton N J，Berger A，Peltier W R. An alternative calibration of the lower Pleistocene timescale based on ODP site 677. Transaction of the Royal Society Edinburg[J].Earth Sciences，1990，81：251-261.
[17]Berger W H，Jansen E. Mid-Pleistocene climate shift—The Nansen connection[J].Geophysical Monograph，1994，84：295-311.
[18]Jian Z M，Wang P X，Chen M P，et al. Foraminiferal response to major Pleistocene paleoceanographic changes in the southern South China Sea[J].Paleoceanography，2000，15(2)：229-243.
[19]Zheng F，Li Q Y，Li B H，et al. A millennial scale planktonic foraminifer record of the mid-Pleistocene climate transition from the northern South China Sea[J]. Palaeogeography，Palaeoclimatology，Palaeoecology，2005，223：349-363.
[20]Schulz M，Mudelsee M. REDFIT：Estimating red-noise spectra directly from unevenly spaced paleoclimatic time series[J].Computer & Geoscience，2002，28：421-426.
[21]Wang L J，Sarnthein M，Erlenkeuser H，et al. Holocene variations in Asian monsoon moisture：A bidecadal sediment record from the South China Sea[J]. Geophysical Research Letters，1999，26（18）：2 889-2 892.