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Seasonal patterns of pollen and the use of pollen as a chronometer in the north‐western Loess Plateau of China

The use of high‐resolution and highly precise age models is essential for quantitative environmental reconstructions. To assess the reliability of pollen as a chronometer in laminated lake sediments, pollen traps and lake cores, statistical methods were used to study seasonal pollen signals. The results showed that (a) the pollen assemblages from air traps and lake/reservoir surface sediment traps in the north‐western Loess Plateau of China displayed distinct seasonal patterns, which were confirmed by nonmetric multidimensional scaling (NMDS); and (b) The pollen assemblages of the dark and light layers in the Zhenhu Lake cores allowed detection of the seasonality of sediment deposition based on the results of the pollen traps. The NMDS method also showed statistically significant differences between the pollen assemblages of the dark and light layers. Furthermore, instrumental monitoring data and characteristic time markers of historical events (1958 and 2011) were used to cross‐check the chronologies obtained by the pollen assemblages, and the results strengthened the credibility and reliability of pollen as a chronometer.