Articles | Volume 15, issue 1
https://doi.org/10.5194/essd-15-95-2023
https://doi.org/10.5194/essd-15-95-2023
Data description paper
 | 
06 Jan 2023
Data description paper |  | 06 Jan 2023

Gridded pollen-based Holocene regional plant cover in temperate and northern subtropical China suitable for climate modelling

Furong Li, Marie-José Gaillard, Xianyong Cao, Ulrike Herzschuh, Shinya Sugita, Jian Ni, Yan Zhao, Chengbang An, Xiaozhong Huang, Yu Li, Hongyan Liu, Aizhi Sun, and Yifeng Yao

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Cited articles

Birks, H. J. B. and Birks, H. H.: Quaternary palaeoecology, Edward Arnold, London, 289 pp., ISBN 0-7131-2781-3, 1980. 
Blaauw, M. and Christen, J. A.: Flexible paleoclimate age-depth models using an autoregressive gamma process, Bayesian Anal., 6, 457–474, https://doi.org/10.1214/11-BA618, 2011. 
Cao, X., Tian, F., Li, F., Gaillard, M.-J., Rudaya, N., Xu, Q., and Herzschuh, U.: Pollen-based quantitative land-cover reconstruction for northern Asia covering the last 40 ka cal BP, Clim. Past, 15, 1503–1536, https://doi.org/10.5194/cp-15-1503-2019, 2019. 
Cao, X.-Y., Ni, J., Herzschuh, U., Wang, Y.-B., and Zhao, Y.: A late Quaternary pollen dataset from eastern continental Asia for vegetation and climate reconstructions: Set up and evaluation, Rev. Palaeobot. Palynol., 194, 21–37, https://doi.org/10.1016/j.revpalbo.2013.02.003, 2013. 
Chen, F., Chen, J., Holmes, J., Boomer, I., Austin, P., Gates, J. B., Wang, N., Brooks, S. J., and Zhang, J.: Moisture changes over the last millennium in arid central Asia: a review, synthesis and comparison with monsoon region, Quaternary Sci. Rev., 29, 1055–1068, https://doi.org/10.1016/j.quascirev.2010.01.005, 2010. 
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Short summary
The objective of this study is present the first gridded and temporally continuous quantitative plant-cover reconstruction for temperate and northern subtropical China over the last 12 millennia. The reconstructions are based on 94 pollen records and include estimates for 27 plant taxa, 10 plant functional types, and 3 land-cover types. The dataset is suitable for palaeoclimate modelling and the evaluation of simulated past vegetation cover and anthropogenic land-cover change from models.
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