Abstract
Numerous field studies have shown that leaf wax n-alkane δD values (δDn-alkane) can be used as a proxy for paleoelevation reconstruction. However, the lack of systematic global analysis of δDn-alkane values with respect to altitude limits the reliability of δDn-alkane values for paleoaltimetry at the global scale. In this study, we analyzed the variation of δDn-alkane values with altitude in terrestrial higher plants based upon our compiled global δDn-alkane database. The general decrease in δDn-alkane values with altitude corresponds to the variation in precipitation δD (δDprec) with altitude, suggesting that the δDn-alkane values effectively reflect δDprec values. When eliminating the effect of latitude at the global scale, the global δDn-alkane-altitude lapse rate for all species was −1.01±0.10‰ (100 m)−1, while these lapse rates were −1.03±0.13‰ and −0.47±0.13‰ (100 m)−1 for dicots and monocots, respectively. Our study reveals that it is reliable to use δDn-alkane values to gain information about paleoelevation at the global scale, and the global δDn-alkane-altitude lapse rates provide an alternative to reconstruct paleoelevation at some δDn-alkane-uninvestigated areas.
Published Version
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