The identified results of 121 surface sediment spore-pollen samples in Shennongjia and meteorological data base of 30 years(January,1971―December,2000)of 7 meteorological stations around Dajiuhu, Shennongjia are used in this study.Selecting 55 species of common spore-pollen with the method of space fitting and stepwise regression we construct the pollen climate factor transfer function of annual mean tem- perature:T=7.649-2.33097X Abies -0.10873X Betula -0.17352X Compositae -0.13176X Cruciferae +0.13356XEuphorbiaceae -0.83069X Campanulaceae +1.96494XPyrrosia+0.38411XPteris+2.77741XSelaginella+0.04439XMonolites.We had reconstructed annual mean temperature series by use of the sporo-pollen samples concentra-tion percentage in peat section with 297 cm thickness in Dajiuhu since 15.753 kaBP.The temperature series reflect well the character of climatic change since the late glacial,which indicates extreme cold climate event of the Oldest Dryas,the Older Dryas,the Younger Dryas and the 8.2 kaBP,the same to the climate fluctuations of Bolling Warm Period and Allerod Warm Period,and the character of temperature change fluctuating frequently at the transition age from the late glacial to the Holocene.The reconstructed temperature also indicate Holocene Optimum,late Holocene warm-dry climate,and the character of climatic change in Dajiuhu in the last 1 ka.The conclusion is that the sporo-pollen samples have important climatic significance to surface sediment and the section of Dajiuhu,Shennongjia and important reference value to studying climatic change during the last glaciation by the temperature transfer function and reconstructed temperature series. The identified results of 121 surface sediment spore-pollen samples in Shennongjia and meteorological data base of 30 years (January, 1971-December, 2000) of 7 meteorological stations around Dajihu, Shennongjia are used in this study. Select 55 species of common spore- pollen with the method of space fitting and stepwise regression we construct the pollen climate factor transfer function of annual mean temperture: T = 7.649-2.33097X Abies -0.10873X Betula -0.17352X Compositae -0.13176X Cruciferae + 0.13356XEuphorbiaceae -0.83069X Campanulaceae + 1.96494X Pyrrosia + 0.38411XPteris + 2.77741X Selaginella + 0.04439XMonolites.We had reconstructed annual mean temperature series by use of the sporo-pollen samples concentra- tion percentage in peat section with 297 cm thickness in Dajihuhu since 15.753 kaBP.The temperature series reflectances well the character of climatic change since the late glacial, which indicates extreme cold climate event of the Oldest Dryas, the Older Dryas, the Younger Dryas and the 8.2 kaBP, the same to the climate fluctuations of Bolling Warm Period and Allerod Warm Period, and the character of temperature change fluctuating frequently at the transition age from the late glacial to the Holocene. recon reconcted temperature also indicate Holocene Optimum, late Holocene warm-dry climate, and the character of climatic change in Dajihuhu in the last 1 ka. the conclusion is that the sporo-pollen samples have important climatic significance to surface sediment and the section of Dajihuhu, Shennongjia and important reference value to studying climatic change during the last glaciation by the temperature transfer function and reconstructed temperature series.