
Обосновывается метод определения основных климатических показателей по групповым спорово-пыльцевым спектрам. Расчетные показатели сравниваются с фактическими данными палинологического обследования обширных участков территории Тюменской области.The article grounds a method of determining basic climatic indices after group palynospectres. Calculated indices being correlated with findings of palynological survey through vast areas of Tyumen Oblast.
СПОРОВО-ПЫЛЬЦЕВЫЕ СПЕКТРЫ,ФУНКЦИОНАЛЬНЫЕ ТИПЫ РАСТИТЕЛЬНОСТИ,РЕКОНСТРУКЦИЯ КЛИМАТА,ГОЛОЦЕН,ДЕФОРМАЦИОННАЯ МОДЕЛЬ,ЗАПАДНАЯ СИБИРЬ
СПОРОВО-ПЫЛЬЦЕВЫЕ СПЕКТРЫ,ФУНКЦИОНАЛЬНЫЕ ТИПЫ РАСТИТЕЛЬНОСТИ,РЕКОНСТРУКЦИЯ КЛИМАТА,ГОЛОЦЕН,ДЕФОРМАЦИОННАЯ МОДЕЛЬ,ЗАПАДНАЯ СИБИРЬ
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