Bond G,Heinrich H,Broecker W,et al.Evidence for Massive Discharges of Icebergs into the North-Atlantic Ocean During the Last Glacial Period[J].Nature,1992,360(6401):245-249.
[2]
Wang Y J,Cheng H,Edwards R L,et al.A High-Resolution Absolute-Dated Late Pleistocene Monsoon Record from Hulu Cave,China[J].Science,2001,294(5550):2345-2348.
[3]
Liu Z,Otto-Bliesner B L,He F,et al.Transient Simulation of Last Deglaciation with a New Mechanism for Bolling-Allerod Warming[J].Science,2009,325(5938):310-314.
[4]
Taylor K C,Lamorey G W,Doyle G A,et al.The `flickering switch' of late Pleistocene climate change[J].Nature,1993,361(6411):432-436.
Guo Z T,Ruddiman W F,Hao Q Z,et al.Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China[J].Nature,2002,416(6877):159-163.
Stevens T, Armitage S J, Lu H Y,et al.Sedimentation and diagenesis of Chinese loess: Implications for the preservation of continuous, high-resolution climate records[J].Geology,2006,34(10):849-852.
[13]
Zhu R X,Zhang R,Deng C L,et al.Are Chinese loess deposits essentially continuous?[J].Geophysical Research Letters,2007,34 L17306. DOI:10.1029/2007GL030591.
安芷生,Porter S C,Kukla G,等.最近13万年黄土高原季风变迁的磁化率证据[J].科学通报,1990,(7):529~532.
[16]
Fang X M,Ono Y,Fukusawa H,et al.Asian summer monsoon instability during the past 60 000 years:magnetic susceptibility and pedogenic evidence from the western Chinese Loess Plateau[J].Earth and Planetary Science Letters,1999,168(3-4):219-232.
[17]
Sun Y B,Chen J,Clemens S C,et al.East Asian monsoon variability over the last seven glacial cycles recorded by a loess sequence from the northwestern Chinese Loess Plateau[J].Geochem.Geophys.Geosyst.,2006, 7(12):DOI:10.1029/2006gc001287.
Dansgaard W,Johnsen S J,Clausen H B,et al.Evidence for general instability of past climate from a 250-kyr ice-core record[J].Nature,1993,364(6434):218-220.
于学峰,周卫健,Franzen L G,等.青藏高原东部全新世冬夏季风变化的高分辨率泥炭记录[J].中国科学(D辑-地球科学),2006,36(2):182~187.
[22]
Berger A.Long-term variations of daily insolation and Quaternary climatic changes[J].Journal of the Atmospheric Sciences,1978,35(12):2362-2367.
[23]
Zhou W J,Head M J,An Z S,et al.Terrestrial evidence for a spatial structure of tropical-polar interconnections during the Younger Dryas episode[J].Earth and Planetary Science Letters,2001,191(3-4):231-239.
[24]
Zhou W J,Yu X F,Jull A J T,et al.High-resolution evidence from southern China of an early Holocene optimum and a mid-Holocene dry event during the past 18 000 years[J].Quaternary Research,2004,62(1):39-48.
[25]
An Z S,Kutzbach J E,Prell W L,et al.Evolution of Asian monsoons and phased uplift of the Himalaya-Tibetan plateau since Late Miocene times[J].Nature,2001,411(6833):62-66.
Porter S C,An Z S.Correlation between climate events in the North Atlantic and China during the last glaciation[J].Nature,1995,375:305-308.
[28]
Reimer P J, Baillie M G L, Bard E, et al. IntCal 09 and Marine 09 radiocarbon age calibration curves,0-50 000 yeats cal BP[J].Radiocarbon,2009,51(4):1111-1150.
Wang Y,Cheng H,Edwards R L,et al.The Holocene Asian Monsoon: Links to Solar Changes and North Atlantic Climate[J].Science,2005,308(5723):854-857.
[32]
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(2):142-152.
[33]
Bond G,Kromer B,Beer J,et al.Persistent Solar Influence on North Atlantic Climate During the Holocene[J].Science,2001,294(5549):2130-2136.
[34]
Porter S C,Zhou W J.Synchronism of Holocene East Asian monsoon variations and North Atlantic drift-ice tracers[J].Quaternary Research,2006,65(3):443-449.
