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Prell W L, Kutzbach J E. Sensitivity of the Indian monsoonto forcing parameters and implications for its evolution.Nature, 1992, 360(10): 647-652.
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Herzschuh U, Kramer A, Mischke S, et al. Quantitativeclimate and vegetation trends since the late glacial on thenortheastern Tibetan Plateau deduced from Koucha Lakepollen spectra. Quaternary Research, 2009, 71(4):162-171.
[8]
Herzschuh U, Birks H B, Mischke S, et al. A modern pollen-climate calibration set based on lake sediments fromthe Tibetan Plateau and its application to a Late Quaternarypollen record from the Qilian Mountains. Journal ofBiogeography, 2010, 37(1): 752-766.
[9]
Wischnewski J, Mischke S, Wang Yongbo, et al. Reconstructingclimate variability on the northeastern Tibetanplateau since the last Lateglacial: A multi-proxy, dual-siteapproach comparing terrestrial and aquatic signals. QuaternaryScience Reviews, 2011, 30(4): 82-97.
[10]
Tang L Y, Shen C M, Li C H, et al. Pollen-inferred vegetationand environmental changes in the central Tibetan Plateausince 8200 yr BP. Sci China Ser D: Earth Sci, 2009,doi: 10.1007/s11430-009-0080-5.
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Shen C M, Liu K M, Tang L Y, et al. Quantitative relationshipsbetween modern pollen rain and climate in theTibetan Plateau. Review of Palaeobotany and Palynology,2006, 140(5): 61-77.
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Lu H Y, Wu N Q, Liu K M, et al. Modern pollen distributionsin Qinghai-Tibetan Plateau and the development oftransfer functions for reconstructing Holocene environmentalchanges. Quaternary Science Reviews, 2011, 30(3): 947-966.
Campo E V, Cour P, Hang S X. Holocene environmentalchanges in Bangong Co basin (Western Tibet). Part 2:The pollen record. Palaeogeography, Palaeoclimatology,Palaeoecology,1996, 120(5): 49-63.
[20]
Campo E V, Gasse F. Pollen and diatom-inferred climaticand hydrological changes in Sumxi Co basin(wesetern Tibet)since 13000yrB.P. Quaternary Research,1993, 39(1):300-313.
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Xu Q H, Li Y C, Bunting M J, et al. The effects of trainingset selection on the relationship between pollen assemblagesand climate parameters: Implications. Palaeogeography,Palaeoclimatology, Palaeoecology, 2010, doi:10.1016/j.palaeo.2010.02.024.
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[26]
Dykoski C A, Edwards R L, Cheng H, et al. A high-resolution,absolute-dated Holocene and deglacial Asian monsoonrecord from Dongge Cave, China. Earth and PlanetaryScience Letters, 2005, 233(6): 71- 86.
Herzschuh U, Kramer A, Mischke S, et al. Quantitativeclimate and vegetation trends since the late glacial on thenortheastern Tibetan Plateau deduced from Koucha Lakepollen spectra. Quaternary Research, 2009, 71(4):162-171.
[32]
Shen C M, Liu K M, Tang L Y, et al. Quantitative relationshipsbetween modern pollen rain and climate in theTibetan Plateau. Review of Palaeobotany and Palynology,2006, 140(5): 61-77.
[33]
Lu H Y, Wu N Q, Liu K M, et al. Modern pollen distributionsin Qinghai-Tibetan Plateau and the development oftransfer functions for reconstructing Holocene environmentalchanges. Quaternary Science Reviews, 2011, 30(3): 947-966.
Campo E V, Cour P, Hang S X. Holocene environmentalchanges in Bangong Co basin (Western Tibet). Part 2:The pollen record. Palaeogeography, Palaeoclimatology,Palaeoecology,1996, 120(5): 49-63.
[41]
Campo E V, Gasse F. Pollen and diatom-inferred climaticand hydrological changes in Sumxi Co basin(wesetern Tibet)since 13000yrB.P. Quaternary Research,1993, 39(1):300-313.
[42]
Xu Q H, Li Y C, Bunting M J, et al. The effects of trainingset selection on the relationship between pollen assemblagesand climate parameters: Implications. Palaeogeography,Palaeoclimatology, Palaeoecology, 2010, doi:10.1016/j.palaeo.2010.02.024.
Gasse F, Arnold M, Fontes J C, et al. A 13000 year climaterecord from western Tibet. Nature, 1991, 353(4):742-745.
[48]
Dykoski C A, Edwards R L, Cheng H, et al. A high-resolution,absolute-dated Holocene and deglacial Asian monsoonrecord from Dongge Cave, China. Earth and PlanetaryScience Letters, 2005, 233(6): 71- 86.
Kutzbach J E, Guetter P J, Ruddiman W F, et al. The sensitivityof climate to late Cenozoic uplift in southern Asiaand the American west: Numerical experiments. Journalof Geophysical Research, 1989, 94(3): 18393-18407.
[52]
An Z S, Kutzbach J E, Prell W L, et al. Evolution ofAsian monsoons and phased uplift of the Himalayan-Tibetanplateau since late Miocene times. Nature, 2001, 411(18): 62-66.
[53]
Prell W L, Kutzbach J E. Sensitivity of the Indian monsoonto forcing parameters and implications for its evolution.Nature, 1992, 360(10): 647-652.
[54]
Bradley R S, Alverson T R, Pedersen F. Challenges of achanging earth: Past perspectives, future concerns//AlersonK R. Bradley T S, Pedersen F. Paleoclimate, GlobalChange and the Future. Berlin: Springer Verlag, 2003:163-167.
[55]
COHMAP Members. Climatic changes of the last 18,000years: Observation and model simulations. Science, 1988,241(6): 1043-1052.
[56]
Herzschuh U, Birks H B, Mischke S, et al. A modern pollen-climate calibration set based on lake sediments fromthe Tibetan Plateau and its application to a Late Quaternarypollen record from the Qilian Mountains. Journal ofBiogeography, 2010, 37(1): 752-766.
[57]
Wischnewski J, Mischke S, Wang Yongbo, et al. Reconstructingclimate variability on the northeastern Tibetanplateau since the last Lateglacial: A multi-proxy, dual-siteapproach comparing terrestrial and aquatic signals. QuaternaryScience Reviews, 2011, 30(4): 82-97.
[58]
Tang L Y, Shen C M, Li C H, et al. Pollen-inferred vegetationand environmental changes in the central Tibetan Plateausince 8200 yr BP. Sci China Ser D: Earth Sci, 2009,doi: 10.1007/s11430-009-0080-5.
[59]
唐领余, 沈才明, Liu K M, 等. 南亚古季风的演变:西藏新的高分辨率古气候记录. 科学通报, 1999, 44(18):2004-2007.
