Articles | Volume 10, issue 1
Clim. Past, 10, 21–39, 2014
https://doi.org/10.5194/cp-10-21-2014
Clim. Past, 10, 21–39, 2014
https://doi.org/10.5194/cp-10-21-2014
Research article
08 Jan 2014
Research article | 08 Jan 2014

Quantitative reconstruction of precipitation changes on the NE Tibetan Plateau since the Last Glacial Maximum – extending the concept of pollen source area to pollen-based climate reconstructions from large lakes

Y. Wang et al.

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Cited articles

Aichner, B., Herzschuh, U., Wilkes, H., Schulz, H., Wang, Y. B., Plessen, B., Mischke, S., Diekmann, B., and Zhang, C. J.: Ecological development of Lake Donggi Cona, north-eastern Tibetan Plateau, since the late glacial on basis of organic geochemical proxies and non-pollen palynomorphs, Palaeogeogr. Palaeocl., 313–314, 140–149, 2012.
An, Z. S., Porter, S. C., Kutzbach, J. E., Wu, X. H., Wang, S. M., Liu, X. D., Li, X. Q., and Zhou, W. J.: Asynchronous Holocene optimum of the East Asian monsoon, Quaternary Sci. Rev., 19, 743–762, 2000.
Anderson, S. T.: The relative pollen productivity and pollen representation of north European trees, and correction factor for tress pollen spectra, Danmarks Geologiske Undersoegelse, Raekke, 2, 1-99 , 1970.
Besag, J. and Clifford, P.: Generalized Monte Carlo significance tests. Biometrika, 76, 633–642, 1989.
Beug, H. J.: Leitfaden der Pollenbestimmung für Mitteleuropa und angrenzende Gebiete, Verlag Dr. Friedrich Pfeil, München (Germany), 2004.
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