红原泥炭氧同位素指示的距今6ka温度变化,其总体趋势与金川温度变化及敦德温度变化一致,与格陵兰冰芯记录的温度变化趋势也相似。具体的气候事件具有明显的全球一致性,距今6ka温度变化存在两个明显的“转折点”:即距今4ka左右气温由低温变为高温,距今1.5ka左右气温由高温变为低温。功率谱分析发现红原泥炭氧同位素序列包含1220～1087,752,444,325,213,127～123,88和79a这样的周期。分析表明红原地区气候驱动因子可能主要是太阳活动,同时海洋活动信号也通过海气耦合传递给季风,再由季风携带到红原地区。 The results show that the overall trend of Jinhuchuan temperature and Dundee temperature is consistent with the change of 6ka temperature of the red peat oxygen isotope, and the trend of temperature recorded by Greenland ice core is also similar. Specific climate events have obvious global consistency. There are two obvious “turning points” in temperature change since 6 ka: the temperature changes from low temperature to high temperature about 4 ka, and the temperature changes from high temperature to low temperature about 1.5 ka. Power spectrum analysis revealed that the red peat oxygen isotope sequence contained periods of 1220-1087, 242, 443, 325, 213, 127-123, 88 and 79a. The analysis shows that the climate driving factor in the Red River may be mainly the solar activity, meanwhile the ocean activity signal is also transmitted to the monsoon by the sea-air coupling and then to the Red River region by the monsoon.