Please use this identifier to cite or link to this item:
http://doi.org/10.25358/openscience-9363
Authors: | Homann, Julia Karbach, Niklas Carolin, Stacy A. James, Daniel H. Hodell, David Breitenbach, Sebastian F. M. Kwiecien, Ola Brenner, Mark Lope, Carlos Peraza Hoffmann, Thorsten |
Title: | Past fire dynamics inferred from polycyclic aromatic hydrocarbons and monosaccharide anhydrides in a stalagmite from the archaeological site of Mayapan, Mexico |
Online publication date: | 8-Aug-2023 |
Year of first publication: | 2023 |
Language: | english |
Abstract: | Speleothems (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. |
DDC: | 540 Chemie 540 Chemistry and allied sciences 550 Geowissenschaften 550 Earth sciences 560 Paläontologie 560 Paleontology 600 Technik 600 Technology (Applied sciences) 620 Ingenieurwissenschaften und Maschinenbau 620 Engineering and allied operations 980 Geschichte Südamerikas 980 General history of South America |
Institution: | Johannes Gutenberg-Universität Mainz |
Department: | FB 09 Chemie, Pharmazie u. Geowissensch. |
Place: | Mainz |
ROR: | https://ror.org/023b0x485 |
DOI: | http://doi.org/10.25358/openscience-9363 |
Version: | Published version |
Publication type: | Zeitschriftenaufsatz |
Document type specification: | Scientific article |
License: | CC BY |
Information on rights of use: | https://creativecommons.org/licenses/by/4.0/ |
Journal: | Biogeosciences 20 15 |
Pages or article number: | 3249 3260 |
Publisher: | Copernicus |
Publisher place: | Katlenburg-Lindau [u.a.] |
Issue date: | 2023 |
ISSN: | 1726-4189 |
Publisher DOI: | 10.5194/bg-20-3249-2023 |
Appears in collections: | DFG-491381577-G |
Files in This Item:
File | Description | Size | Format | ||
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past_fire_dynamics_inferred_f-20230808144256830.pdf | 6.77 MB | Adobe PDF | View/Open | ||
past_fire_dynamics_inferred_f-20230808144417034.pdf | 1.01 MB | Adobe PDF | View/Open |