摘要
In light of the U-series dating results, 900 annual laminae, 320 C and O isotopes data and gray level data of stalagmite NH33 from the Nuanhe Cave, δ13C and gray level sequence of the stalagmite in recent 1 000 years in the Holocene Optimun(8 638±60~7 748±53)a B.P. are established. Paleo-environments interpreted by the stalagmite-series can be divided into three climate-stages, that is well fitted with the pollen record at the same time. Some non-climate factors are also contained in stalagmite δ13C, which is led by changes in dissolved CaCO3 of the wall rock affected mainly by water seepage rate. Making regression analysis on the stalagmite δ13C and gray level data can effectively avoid the non-climate factors led by the hydrodynamic conditions.