Please use this identifier to cite or link to this item: http://doi.org/10.25358/openscience-9363
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dc.contributor.authorHomann, Julia-
dc.contributor.authorKarbach, Niklas-
dc.contributor.authorCarolin, Stacy A.-
dc.contributor.authorJames, Daniel H.-
dc.contributor.authorHodell, David-
dc.contributor.authorBreitenbach, Sebastian F. M.-
dc.contributor.authorKwiecien, Ola-
dc.contributor.authorBrenner, Mark-
dc.contributor.authorLope, Carlos Peraza-
dc.contributor.authorHoffmann, Thorsten-
dc.date.accessioned2023-08-08T12:47:16Z-
dc.date.available2023-08-08T12:47:16Z-
dc.date.issued2023-
dc.identifier.urihttps://openscience.ub.uni-mainz.de/handle/20.500.12030/9381-
dc.description.abstractSpeleothems (cave stalagmites) contain inorganic and organic substances that can be used to infer past changes in local and regional paleoenvironmental conditions. Specific biomarkers can be employed to elucidate the history of past fires, caused by interactions among climate, regional hydrology, vegetation, humans, and fire activity. We conducted a simple solid–liquid extraction on pulverised carbonate samples to prepare them for analysis of 16 polycyclic aromatic hydrocarbons (PAHs) and three monosaccharide anhydrides (MAs). The preparation method requires only small samples (0.5–1.0 g); PAHs and MAs were measured by GC–MS and LC–HILIC–MS, respectively. Detection limits range from 0.05–2.1 ng for PAHs and 0.01–0.1 ng for MAs. We applied the method to 10 samples from a ∼ 400-year-old stalagmite from Cenote Ch'en Mul, at Mayapan (Mexico), the largest Postclassic Maya capital of the Yucatán Peninsula. We found a strong correlation (r = 0.75, p < 0.05) between the major MA (levoglucosan) and non-alkylated PAHs (Σ15). We investigated multiple diagnostic PAH and MA ratios and found that although not all were applicable as paleo-fire proxies, ratios that combine PAHs with MAs are promising tools for identifying different fire regimes and inferring the type of fuel burned. In the 1950s and 1960s, levoglucosan and Σ15 concentrations roughly doubled compared to other times in the last 400 years, suggesting greater fire activity at Mayapan during these two decades. The higher concentrations of fire markers may have been a consequence of land clearance at the site and exploration of the cave by Carnegie Institution archaeologists.en_GB
dc.language.isoengde
dc.rightsCC BY*
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/*
dc.subject.ddc540 Chemiede_DE
dc.subject.ddc540 Chemistry and allied sciencesen_GB
dc.subject.ddc550 Geowissenschaftende_DE
dc.subject.ddc550 Earth sciencesen_GB
dc.subject.ddc560 Paläontologiede_DE
dc.subject.ddc560 Paleontologyen_GB
dc.subject.ddc600 Technikde_DE
dc.subject.ddc600 Technology (Applied sciences)en_GB
dc.subject.ddc620 Ingenieurwissenschaften und Maschinenbaude_DE
dc.subject.ddc620 Engineering and allied operationsen_GB
dc.subject.ddc980 Geschichte Südamerikasde_DE
dc.subject.ddc980 General history of South Americaen_GB
dc.titlePast fire dynamics inferred from polycyclic aromatic hydrocarbons and monosaccharide anhydrides in a stalagmite from the archaeological site of Mayapan, Mexicoen_GB
dc.typeZeitschriftenaufsatzde
dc.identifier.doihttp://doi.org/10.25358/openscience-9363-
jgu.type.contenttypeScientific articlede
jgu.type.dinitypearticleen_GB
jgu.type.versionPublished versionde
jgu.type.resourceTextde
jgu.organisation.departmentFB 09 Chemie, Pharmazie u. Geowissensch.de
jgu.organisation.number7950-
jgu.organisation.nameJohannes Gutenberg-Universität Mainz-
jgu.rights.accessrightsopenAccess-
jgu.journal.titleBiogeosciencesde
jgu.journal.volume20de
jgu.journal.issue15de
jgu.pages.start3249de
jgu.pages.end3260de
jgu.publisher.year2023-
jgu.publisher.nameCopernicusde
jgu.publisher.placeKatlenburg-Lindau [u.a.]de
jgu.publisher.issn1726-4189de
jgu.organisation.placeMainz-
jgu.subject.ddccode540de
jgu.subject.ddccode550de
jgu.subject.ddccode560de
jgu.subject.ddccode600de
jgu.subject.ddccode620de
jgu.subject.ddccode980de
jgu.publisher.doi10.5194/bg-20-3249-2023de
jgu.organisation.rorhttps://ror.org/023b0x485-
jgu.subject.dfgNaturwissenschaftende
Appears in collections:DFG-491381577-G

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