Please use this identifier to cite or link to this item: http://doi.org/10.25358/openscience-6592
Authors: Heidke, Inken
Hartland, Adam
Scholz, Denis
Pearson, Andrew
Hellstrom, John
Breitenbach, Sebastian F. M.
Hoffmann, Thorsten
Title: Lignin oxidation products in soil, dripwater and speleothems from four different sites in New Zealand
Online publication date: 7-Dec-2021
Language: english
Abstract: Lignin oxidation products (LOPs) are widely used as vegetation proxies in climate archives, such as sediment and peat cores. The total LOP concentration, Σ8, provides information on the abundance of vegetation, while the ratios C/V and S/V of the different LOP groups also provide information on the type of vegetation. Recently, LOP analysis has been successfully applied to speleothem archives. However, there are many open questions concerning the transport and microbial degradation of LOPs on their way from the soil into the cave system. These processes could potentially alter the original source-dependent LOP signals, in particular the C/V and S/V ratios, and thus complicate their interpretation in terms of past vegetation changes. We analyzed LOPs in leaf litter and different soil horizons as well as dripwater and flowstone samples from four different cave sites from different vegetation zones in New Zealand using ultrahigh-performance liquid chromatography coupled to high-resolution mass spectrometry. We test whether the original source-dependent LOP signal of the overlying vegetation is preserved and can be recovered from flowstone samples and investigate how the signal is altered by the transport from the soil to the cave. The LOP concentrations range from mg g−1 in the soil to ng g−1 in the flowstones. Our results demonstrate that, from the soil to the flowstone, the C/V and S/V ratios both increase, while the total lignin content, Σ8, strongly decreases. This shows that the LOP signal is strongly influenced by both transport and degradation processes. Nevertheless, the relative LOP signal from the overlying soil at the different cave sites is preserved in the flowstone. We emphasize that for the interpretation of C/V and S/V ratios in terms of past vegetation changes, it is important to compare only samples of the same type (e.g., speleothem, dripwater or soil) and to evaluate only relative variations.
DDC: 540 Chemie
540 Chemistry and allied sciences
550 Geowissenschaften
550 Earth sciences
Institution: Johannes Gutenberg-Universität Mainz
Department: FB 09 Chemie, Pharmazie u. Geowissensch.
Place: Mainz
DOI: http://doi.org/10.25358/openscience-6592
Version: Published version
Publication type: Zeitschriftenaufsatz
License: CC BY
Information on rights of use: https://creativecommons.org/licenses/by/4.0/
Journal: Biogeosciences
18
7
Pages or article number: 2289
2300
Publisher: Copernicus
Publisher place: Katlenburg-Lindau u.a.
Issue date: 2021
ISSN: 1726-4189
Publisher URL: https://doi.org/10.5194/bg-18-2289-2021
Publisher DOI: 10.5194/bg-18-2289-2021
Appears in collections:JGU-Publikationen

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