Temperature sensitivity of surface soil phytoliths: A case study in Northeast China

Abstract

Modern process research on phytoliths, including on the characteristics and spatial distribution of phytoliths assemblages and their relationship with environmental factors, is the basis of the use of phytoliths in paleoenvironmental reconstruction. We collected 54 surface soil samples along the isohyet of 600 mm in Northeast China in order to determine the relationship between modern phytoliths distributions and temperature. These were comprised by 20 samples from Xiaoxing'an Mountains, 32 samples from Songliao Plain, and 2 samples from Liaoxi Hills. The main phytoliths types were elongate and lanceolate, followed by short cell phytoliths, blocky, tabular and cuneiform; the percentages of the other types were all less than 1% and only occurred sporadically. There were significant differences in phytoliths assemblages among Xiaoxing'an Mountains, Songliao Plain, and Liaoxi Hills. Discriminant analysis was conducted using phytoiths assemblages, the samples from these three regions could be separated with a total accuracy of 96.30%. Elongate, lanceolate and pteridophyte‒type on average made up the largest proportion in Xiaoxing'an Mountains and the smallest in Liaoxi Hills, whereas saddle, bilobate and papillae showed the inverse trend; the proportions of blocky, tabular and cuneiform were the largest in Songliao Plain. The percentages of these types abovementioned were significantly different among the three regions. Correlation analysis revealed a significant negative correlation between the percentages of elongate, lanceolate and pteridophyte‒type and mean annual temperature (MAT), while there was a significant positive correlation between the percentages of blocky, tabular, cuneiform, saddle, bilobate, papillae and MAT. There was no significant relationship between rondel, trapeziform sinuate, conduit, carinate, sclereid, silicified stomata and MAT. A phytoliths index (C/W) based on the common phytoliths types in the surface soil samples which had a significant correlation with MAT was built. C/W = (elongate + lanceolate)/(elongate + lanceolate + blocky + tabular + cuneiform + saddle + bilobate). The values of C/W in Northeast China varied from 0.14 to 0.91, with an average of 0.67. The accuracy of the C/W index indicating climatic trends was significantly higher than the previously established Ic (climate index) and Iw (warm index). Overall, our results contribute to an improved understanding on the environmental significance of various phytoliths morphotypes, and provide a modern process foundation for phytoliths–based paleoclimatic reconstruction in the study region.