2001
DOI: 10.1016/s0009-2541(00)00415-0
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A hypothesis for the origin of perylene based on its low abundance in sediments of Green Bay, Wisconsin

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Cited by 106 publications
(49 citation statements)
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“…a petroleum reservoir or from hydrocoarbon source rocks. Perylene levels increasing in the depth together with those of alkylated PAH (at open-sea locations but not at fjord locations) may then be hypothetically explained by increased microbial activity due to hydrocarbon fluids (Silliman et al, 2001;Hovland and Judd, 1988).…”
Section: Resultsmentioning
confidence: 99%
“…a petroleum reservoir or from hydrocoarbon source rocks. Perylene levels increasing in the depth together with those of alkylated PAH (at open-sea locations but not at fjord locations) may then be hypothetically explained by increased microbial activity due to hydrocarbon fluids (Silliman et al, 2001;Hovland and Judd, 1988).…”
Section: Resultsmentioning
confidence: 99%
“…Thus, it is not surprising that perylene can be found in most sediments around the world, especially in freshwater lake and nearshore sediments (Ishiwatari and Hanya, 1975;Gschwend et al, 1983;Venkatesan, 1988;Soma et al, 1996;Jiang et al, 2000;Silliman et al, 2001). Occasional high amounts of perylene in sediments might also be attributed to the presence of fossilized gymnosperms that had been decomposed by fungi, since high amounts of perylene have been found in such fossils (Bechtel et al, 2007;Jiang and Liu, 2008).…”
Section: Value Of Perylene In Lake Biwa Sedimentmentioning
confidence: 99%
“…Perylene (C 20 H 12 ) is commonly found with other PAHs (Ishiwatari and Hanya, 1975;Gschwend et al, 1983;Venkatesan, 1988;Soma et al, 1996;Jiang et al, 2000;Silliman et al, 2001) in the natural environment, but its vertical distribution in sediment cores differs from those of other PAHs that originate from combustion (Venkatesan, 1988;Jiang et al, 2000;Silliman et al, 2001). Although the source and mechanism of formation of perylene are not clearly understood, many studies suggest that it has an origin other than combustion, such as in terrestrial or other biota, and that it arises from precursor components under anaerobic conditions (Venkatesan, 1988;Silliman et al, 2001).…”
Section: Introductionmentioning
confidence: 99%
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