Reconstructing lake evaporation history and the isotopic composition of precipitation by a coupled 未18O-未2H biomarker approach
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文摘

2H biomarker record was established for a lake sediment archive.

16 ka 18Osugar and 2Hn-alkane biomarker records follow similar trends.

18O/2H differences are explained by evaporative isotopic enrichment of lake water.

Reconstructed d-excess of lake water serves as proxy for evaporative losses.

A coupled 18O–2H approach allows a model-based reconstruction of 18O/2Hprec.

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