6533b7d6fe1ef96bd1266de3
RESEARCH PRODUCT
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subject
chemistry.chemical_classificationgeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesExtraction (chemistry)SpeleothemStalagmite15. Life on land010502 geochemistry & geophysicsMass spectrometry01 natural scienceschemistry.chemical_compoundCavechemistry13. Climate actionEnvironmental chemistrySoil waterLigninOrganic matterEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface Processesdescription
Abstract. Here we present a sensitive method to analyze lignin oxidation products (LOPs) in speleothems and cave drip water to provide a new tool for paleo-vegetation reconstruction. Speleothems are valuable climate archives. However, compared to other terrestrial climate archives, such as lake sediments, speleothems contain very little organic matter. Therefore, very few studies on organic biomarkers in speleothems are available. Our new sensitive method allows us to use LOPs as vegetation biomarkers in speleothems. Our method consists of acid digestion of the speleothem sample followed by solid-phase extraction (SPE) of the organic matter. The extracted polymeric lignin is degraded in a microwave-assisted alkaline CuO oxidation step to yield monomeric LOPs. The LOPs are extracted via SPE and finally analyzed via ultrahigh-performance liquid chromatography (UHPLC) coupled to electrospray ionization (ESI) and high-resolution Orbitrap mass spectrometry (HRMS). The method was applied to stalagmite samples with a sample size of 3–5 g and cave drip water samples with a sample size of 100–200 mL from the Herbstlabyrinth-Advent Cave in Germany. In addition, fresh plant samples, soil water, and powdered lignin samples were analyzed for comparison. The concentration of the sum of eight LOPs (Σ8) was in the range of 20–84 ng g−1 for the stalagmite samples and 230–440 ng L−1 for the cave drip water samples. The limits of quantification for the individual LOPs ranged from 0.3–8.2 ng per sample or 1.5–41.0 ng mL−1 of the final sample solution. Our method represents a new and powerful analytical tool for paleo-vegetation studies and has great potential to identify the pathways of lignin incorporation into speleothems.
| year | journal | country | edition | language |
|---|---|---|---|---|
| 2018-10-04 | Biogeosciences |