Carrie L. Thomas , Boris Jansen , E. Emiel van Loon , Guido L.B. Wiesenberg
{"title":"Evaluating the applicability of the VERHIB model to a 2600-year peat sequence from Central Germany","authors":"Carrie L. Thomas , Boris Jansen , E. Emiel van Loon , Guido L.B. Wiesenberg","doi":"10.1016/j.apgeochem.2025.106338","DOIUrl":null,"url":null,"abstract":"<div><div>Plant-derived biomarkers have been used extensively for source identification of organic matter in soil, peat, and sediments. These are chemical components, primarily of leaf waxes, that are naturally more resistant to degradation than most organic molecules and can be preserved in depositional archives for hundreds to thousands of years. However, using biomarkers for vegetation reconstruction can be complicated because individual compounds or compound classes do not necessarily indicate specific plant sources. The composition across multiple compounds must be holistically evaluated to develop accurate reconstructions. The VERHIB model was developed to enable a range of <em>n</em>-alkane and <em>n</em>-alkanol data to be evaluated simultaneously and estimate past vegetation development using the biomarker signature of leaves and roots from present-day specimens of the plant species of interest compared to the preserved, mixed signature of a soil or peat core. In this study, we have applied the VERHIB model to data gathered from the Beerberg peatland in Central Germany. A previous study characterized plant macrofossils, pollen, <em>n</em>-alkane, <em>n</em>-alkanol, and <em>n</em>-fatty acid composition in the Beerberg peat. We have collected modern plant samples from the peatland and measured their biomarker composition to use as input for the model. Despite many overlapping biomarker signatures across plant species and parts, our results show that the model could recreate a reasonable vegetation development pattern for most of the peat core if <em>n</em>-fatty acid data were included alongside <em>n</em>-alkane data. The model had difficulty recreating the transition from poor fen vegetation to <em>Sphagnum</em> bog, which was evident in the plant macrofossil records, so further calibration is needed. This was the first attempt at considering <em>n</em>-fatty acid data in a reconstruction using the VERHIB model; previous reconstructions only included <em>n</em>-alkanes or a combination of <em>n</em>-alkanes and <em>n</em>-alkanols. Our study shows that <em>n</em>-fatty acids are a valuable compound class to add to the VERHIB model and provides recommendations for future development.</div></div>","PeriodicalId":8064,"journal":{"name":"Applied Geochemistry","volume":"184 ","pages":"Article 106338"},"PeriodicalIF":3.1000,"publicationDate":"2025-03-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Applied Geochemistry","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0883292725000617","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 0
Abstract
Plant-derived biomarkers have been used extensively for source identification of organic matter in soil, peat, and sediments. These are chemical components, primarily of leaf waxes, that are naturally more resistant to degradation than most organic molecules and can be preserved in depositional archives for hundreds to thousands of years. However, using biomarkers for vegetation reconstruction can be complicated because individual compounds or compound classes do not necessarily indicate specific plant sources. The composition across multiple compounds must be holistically evaluated to develop accurate reconstructions. The VERHIB model was developed to enable a range of n-alkane and n-alkanol data to be evaluated simultaneously and estimate past vegetation development using the biomarker signature of leaves and roots from present-day specimens of the plant species of interest compared to the preserved, mixed signature of a soil or peat core. In this study, we have applied the VERHIB model to data gathered from the Beerberg peatland in Central Germany. A previous study characterized plant macrofossils, pollen, n-alkane, n-alkanol, and n-fatty acid composition in the Beerberg peat. We have collected modern plant samples from the peatland and measured their biomarker composition to use as input for the model. Despite many overlapping biomarker signatures across plant species and parts, our results show that the model could recreate a reasonable vegetation development pattern for most of the peat core if n-fatty acid data were included alongside n-alkane data. The model had difficulty recreating the transition from poor fen vegetation to Sphagnum bog, which was evident in the plant macrofossil records, so further calibration is needed. This was the first attempt at considering n-fatty acid data in a reconstruction using the VERHIB model; previous reconstructions only included n-alkanes or a combination of n-alkanes and n-alkanols. Our study shows that n-fatty acids are a valuable compound class to add to the VERHIB model and provides recommendations for future development.
期刊介绍:
Applied Geochemistry is an international journal devoted to publication of original research papers, rapid research communications and selected review papers in geochemistry and urban geochemistry which have some practical application to an aspect of human endeavour, such as the preservation of the environment, health, waste disposal and the search for resources. Papers on applications of inorganic, organic and isotope geochemistry and geochemical processes are therefore welcome provided they meet the main criterion. Spatial and temporal monitoring case studies are only of interest to our international readership if they present new ideas of broad application.
Topics covered include: (1) Environmental geochemistry (including natural and anthropogenic aspects, and protection and remediation strategies); (2) Hydrogeochemistry (surface and groundwater); (3) Medical (urban) geochemistry; (4) The search for energy resources (in particular unconventional oil and gas or emerging metal resources); (5) Energy exploitation (in particular geothermal energy and CCS); (6) Upgrading of energy and mineral resources where there is a direct geochemical application; and (7) Waste disposal, including nuclear waste disposal.