Abstract:Compound-specific δ2H composition of leaf-wax n-alkanes are increasingly being used to infer past hydroclimates. However, differences in n-alkane production and apparent fractionation factors (εapp) among different plant groups complicate the relationships between n-alkane and environmental water δ2H. Mid- and long-chain n-alkanes in sedimentary archives (i.e., C23 and C29) are thought to derive from aquatic and terrestrial plants, respectively, and track the isotopic composition of either lake water or precip… Show more
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