Articles | Volume 12, issue 1
Earth Syst. Sci. Data, 12, 119–135, 2020
https://doi.org/10.5194/essd-12-119-2020

Special issue: Paleoclimate data synthesis and analysis of associated uncertainty...

Earth Syst. Sci. Data, 12, 119–135, 2020
https://doi.org/10.5194/essd-12-119-2020

Data description paper 22 Jan 2020

Data description paper | 22 Jan 2020

A taxonomically harmonized and temporally standardized fossil pollen dataset from Siberia covering the last 40 kyr

Xianyong Cao et al.

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Cited articles

Anderson, P., Minyuk, P., Lozhkin, A., Cherepanova, M., Borkhodoev, V., and Finney, B.: A multiproxy record of Holocene environmental changes from the northern Kuril Islands (Russian Far East), J. Paleolimnol., 54, 379–393, https:/dor.org/10.1007/s10933-015-9858-y, 2015. 
Anderson, P. M. and Lozhkin, A. V.: LateQuaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database), North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia, 2002. 
Anderson, P. M. and Lozhkin, A. V.: Late Quaternary vegetation of Chukotka (Northeast Russia), implications for Glacial and Holocene environments of Beringia, Quaternary Sci. Rev., 107, 112–128, https://doi.org/10.1016/j.quascirev.2014.10.016, 2015. 
Anderson, P. M., Lozhkin, A. V., Belaya, B. V., and Stetsenko, T. V.: New data about the stratigraphy of late Quaternary deposits of northern Priokhot'ye in: Environmental changes in Beringia during the Quaternary, edited by: Simakov, K. V., North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan, 69–87, 1998a (in Russian). 
Anderson, P. M., Lozhkin, A. V. and Belaya, B. V.: Younger Dryas in western Beringia (northeastern Siberia), in: Environmental changes in Beringia during the Quaternary, North East Interdisciplinary Research Institute, edited by: Simakov, K. V., Far East Branch, Russian Academy of Sciences, Magadan, 28–44, 1998b (in Russian). 
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Pollen percentages in spectra cannot be utilized to indicate past plant abundance directly because of the different pollen productivities among plants. In this paper, we applied relative pollen productivity estimates (PPEs) to calibrate plant abundances during the last 40 kyr using pollen counts from 203 pollen spectra in northern Asia. Results indicate the vegetation are generally stable during the Holocene and that climate change is the primary factor.