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                <identifier>oai:data.mendeley.com/572tbr9y59.1</identifier>
                <datestamp>2019-12-07T05:58:59Z</datestamp>
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            <metadata><oai_dc:dc xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance">
    <dc:creator>Xie, Shucheng </dc:creator>
    <dc:title>Data for: Distribution of pyrolytic polycyclic aromatic hydrocarbons across Triassic-Jurassic boundary in the Sichuan Basin, southwestern China: Evidence of wildfire occurrence outside the Central Atlantic Magmatic Province</dc:title>
    <dc:publisher>Mendeley Data</dc:publisher>
    <dc:description>1. The elevated concentration of pyrolytic polycyclic aromatic hydrocarbons (PAHs) in Sichuan Basin during Triassic-Jurassic shows multistage wildfire events(TJB, R1,R2 events), including Phenanthrene (Phe), fluoranthene (Fl), pyrene (Py), chrysene (Chry), benzofluoranthene (BFl), benzo[e]pyrene (BPy), indeno[1,2,3-cd] pyrene (InPy), benzo[ghi]perylene (Bpery), and coronene (Cor). 

2.We calculated the parent-PAH-to-(parent-PAH+alkyl-PAH) index (PPAHI) to test variation in PAH sources,  including methylnaphthalene (MeN), methylphenanthrene (MePh), methylfluoranthene (MeFl), methylpyrene (MePy), and other alkyl-PAH homologues present in the aromatic fraction. PPAHI increased during wildfire events.  

3. Ratios of fluoranthene to fluoranthene plus pyrene Fl/(Fl+Py) and indenopyrene to indenopyrene plus benzoperylene InPy/(InPy+Bpery) implies a combustion source.

4.The high content of total oxygenated PAHs, dibenzofuran (DBFs) and its derivatives, occur during wildfire events that indicate soil erosion, possibly due to a loss of rooted vegetation. 


5.The vertical distributions of ratios of total alkanes with carbon numbers &lt;21 to alkanes with carbon numbers &gt;22 (ΣC21-/ΣC22+) reflect a large increase in inputs of organic matter from higher plants during wildfire events.


6.Three episodes of enhanced wildfire frequency in the Sichuan Basin were as a result of regional climate aridification. Also, wildfire events would be a main factor of terrestrial plant change during TJB.</dc:description>
    <dc:subject>Organic Geochemistry</dc:subject>
    <dc:subject>Mass Extinction</dc:subject>
    <dc:subject>Palaeoclimate</dc:subject>
    <dc:contributor>Luo, Genming</dc:contributor>
    <dc:contributor>Algeo, Thomas</dc:contributor>
    <dc:contributor>Li, Liqin</dc:contributor>
    <dc:contributor>Song, Yi</dc:contributor>
    <dc:contributor>Wang, Yongdong</dc:contributor>
    <dc:contributor>Wu, Wenjun</dc:contributor>
    <dc:type>Dataset</dc:type>
    <dc:identifier>doi:10.17632/572tbr9y59.1</dc:identifier>
    <dc:identifier>oai:data.mendeley.com/572tbr9y59.1</dc:identifier>
    <dc:rights>Creative Commons Attribution 4.0 International</dc:rights>
    <dc:rights>http://creativecommons.org/licenses/by/4.0</dc:rights>
    <dc:relation>https://data.mendeley.com/datasets/572tbr9y59</dc:relation>
    <dc:date>2019-12-07T05:58:59Z</dc:date>
    <dc:date>2020-04-01T00:00:00Z</dc:date>
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