δ13C analysis of bulk organic matter in speleothems using liquid chromatography–isotope ratio mass spectrometry
Author:
Publisher
Elsevier BV
Subject
Geochemistry and Petrology
Reference5 articles.
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3. Rapid and precise δ13C measurement of dissolved inorganic carbon in natural waters using liquid chromatography coupled to an isotope-ratio mass spectrometer;Brandes;Limnology and Oceanography: Methods,2009
4. Dead carbon in stalagmites: carbonate bedrock palaeodissolution vs. ageing of soil organic matter. Implications for 13C variations in speleothems;Genty;Geochimica et Cosmochimica Acta,2001
5. Causes of colour and fluorescence in speleothems;van Beynen;Chemical Geology,2001
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2. Application of microbial membrane tetraether lipids in speleothems;Frontiers in Ecology and Evolution;2023-05-02
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4. Liquid Chromatography coupled to Isotope Ratio Mass Spectrometry (LC-IRMS): A review;TrAC Trends in Analytical Chemistry;2022-02
5. Lignin oxidation products as a potential proxy for vegetation and environmental changes in speleothems and cave drip water – a first record from the Herbstlabyrinth, central Germany;Climate of the Past;2019-06-14
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