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Construction and Application of Phytolith-Climate Transfer Function in Peat Surface Deposits of Northeast China
详细信息   
摘要
On the basis of phytolith assemblages from peat surface deposits and some climate indexes, a transfer function of phytolith-climate in Northeast China is established by means of factorial analysis and stepwise regression. Using the function, paleo-climate parameters of Yunshu peat profile were calculated and the paleo-climate evolution is then divided into 7 stages: warm-cold-warm-clod-warm-cold-warm. The reconstructed curves also show that the changes of paleo-annual wind speed might indicate the following changes of paleo-temperature and paleo-precipitation, and the warm and wet climate always corresponds with a stable climate system.

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