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Abstract

A total of 237 surface soil pollen samples were collected from less disturbed zonal communities, and a new surface pollen data set has been established in northern China. Pollen—climate parameter transfer functions using weighted-averaging regression and calibration partial least squares (WA-PLS) model as a tool to reconstruct past climate changes from pollen data, were tested with this new surface pollen data set. The results of cross-validation showed that the method worked very well with precipitation (R = 0.94, R ² _jack = 0.89, RMSEP_jack = 69 mm, the safe dynamic range of the reconstruction was 40 mm~800 mm) and worked well with temperature (T _ann: R = 0.84, R ² _jack = 0.71, RMSEP_jack = 2.0°C, the safe dynamic range of the reconstruction was −4°C~13°C; MT_wa: R = 0.79, R ² _jack = 0.63, RMSEP_jack = 2.5°C, and the safe dynamic range of the reconstruction was 8°C~26°C), indicating that the surface pollen data set and WA-PLS reconstruction technique in this paper have strong potential for palaeoclimatic reconstruction.

Keywords

Surface pollen data set northern China transfer functions WA-PLS models cross-validation palaeoclimate reconstruction.

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A transfer-function model developed from an extensive surface-pollen data set in northern China and its potential for palaeoclimate reconstructions

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