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• W2067366951 abstract "Abstract The hydrogen isotope composition of terrestrial plant leaf wax in sediments is increasingly used as a paleoclimatic indicator. Modern calibration studies suggest that paleoclimatic interpretation of leaf wax δ D values requires consideration of the differences in the apparent fractionation of hydrogen isotopes among different groups of plants. However, it is not common that paleoecological data are used to help interpret leaf wax δ D profiles. Here we assess the relative importance of factors influencing millennial-scale shifts in δ D values of n -alkanoic acids at Steel Lake (Minnesota, USA), an extensively studied site with independent records of vegetation composition, δ D of input water to the lake, and evaporation. The δ D values of the n -C 28 alkanoic acid ( δ D C28 ) vary between −190 and −168‰, and do not correlate with δ D of input water or the extent of evaporation. However, δ D C28 is negatively correlated with the δ 13 C values of the n -C 28 alkanoic acid ( δ 13 C C28 ). The correlation, along with pollen assemblage and carbonate δ 13 C records, suggests that Holocene shifts between forest and grassland and/or in the water use efficiency of C 3 plants influenced the stratigraphic variation in leaf wax δ D. Thus, paleoecological information, such as that inferred from pollen assemblages and carbon isotopes of plant-derived compounds, may aid paleoclimatic interpretation of leaf wax δ D profiles from lake sediments." @default.
• W2067366951 created "2016-06-24" @default.
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• W2067366951 date "2013-03-01" @default.
• W2067366951 modified "2023-09-25" @default.
• W2067366951 title "Influence of terrestrial vegetation on leaf wax δD of Holocene lake sediments" @default.
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• W2067366951 doi "https://doi.org/10.1016/j.orggeochem.2012.12.010" @default.
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