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- W2005211478 endingPage "326" @default.
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- W2005211478 abstract "Carboniferous (Viséan) coals from Dunbar, East Lothian, Scotland, contain well-preserved miospore and megaspore assemblages suggesting a lycopod-dominated forest ecosystem with some ferns, sphenopsids and pteridosperms. The low rank of the coals and the well defined microflora permit assessment of the palaeoenvironmental significance of lipid biomarkers during the Early Carboniferous. Rock-Eval, petrographic, and lipid analyses indicate a fully terrestrial depositional environment. Although we also present and discuss a wide diversity of other lipid biomarkers (alkanes, hopanoids, steroids), we focus on the terrestrial-derived biomarkers. Combustion-derived PAHs pyrene, fluoranthene, benzo[a]anthracene, chrysene and triphenylene indicate the occurrence of forest fires in the study areas during Early Carboniferous times. Alkyldibenzofurans are considered to derive from lichen-biomass. Retene, cadalene, simonellite, tetrahydroretene and kaurane are poorly specific and can derive from a variety of early Palaeozoic land plants. Abietane, phyllocladane, ent-beyerane and 4β(H)-eudesmane, as well as bisnorsimonellite, diaromatic totarane, diaromatic sempervirane and 2-methylretene, however, as yet had only been reported from conifers, which do not appear in the fossil record until the Late Carboniferous. Within the lower Carboniferous forest ecosystem, arborescent lycopsids and pteridosperms are proposed as alternative sources for these compounds." @default.
- W2005211478 created "2016-06-24" @default.
- W2005211478 creator A5004160583 @default.
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- W2005211478 creator A5039685767 @default.
- W2005211478 creator A5046798101 @default.
- W2005211478 creator A5061922880 @default.
- W2005211478 date "2011-09-01" @default.
- W2005211478 modified "2023-09-30" @default.
- W2005211478 title "Aliphatic and aromatic biomarkers from Carboniferous coal deposits at Dunbar (East Lothian, Scotland): Palaeobotanical and palaeoenvironmental significance" @default.
- W2005211478 cites W132351063 @default.
- W2005211478 cites W1561524330 @default.
- W2005211478 cites W1963674693 @default.
- W2005211478 cites W1963946431 @default.
- W2005211478 cites W1964291746 @default.
- W2005211478 cites W1965575353 @default.
- W2005211478 cites W1967509775 @default.
- W2005211478 cites W1967685912 @default.
- W2005211478 cites W1969368324 @default.
- W2005211478 cites W1969558356 @default.
- W2005211478 cites W1973424875 @default.
- W2005211478 cites W1975826595 @default.
- W2005211478 cites W1977882042 @default.
- W2005211478 cites W1979089141 @default.
- W2005211478 cites W1980959253 @default.
- W2005211478 cites W1986674447 @default.
- W2005211478 cites W1988396197 @default.
- W2005211478 cites W1989971824 @default.
- W2005211478 cites W1991246072 @default.
- W2005211478 cites W1994789946 @default.
- W2005211478 cites W1994845902 @default.
- W2005211478 cites W1995336154 @default.
- W2005211478 cites W1995575035 @default.
- W2005211478 cites W1995596774 @default.
- W2005211478 cites W1998509925 @default.
- W2005211478 cites W2003222613 @default.
- W2005211478 cites W2003990443 @default.
- W2005211478 cites W2004995192 @default.
- W2005211478 cites W2005177176 @default.
- W2005211478 cites W2005353275 @default.
- W2005211478 cites W2007451406 @default.
- W2005211478 cites W2009829591 @default.
- W2005211478 cites W2010320198 @default.
- W2005211478 cites W2014523333 @default.
- W2005211478 cites W2018054530 @default.
- W2005211478 cites W2018976660 @default.
- W2005211478 cites W2022799402 @default.
- W2005211478 cites W2023086177 @default.
- W2005211478 cites W2026630166 @default.
- W2005211478 cites W2026738560 @default.
- W2005211478 cites W2029919752 @default.
- W2005211478 cites W2032247127 @default.
- W2005211478 cites W2032252448 @default.
- W2005211478 cites W2042738358 @default.
- W2005211478 cites W2044417994 @default.
- W2005211478 cites W2045386399 @default.
- W2005211478 cites W2047038378 @default.
- W2005211478 cites W2051534897 @default.
- W2005211478 cites W2053391576 @default.
- W2005211478 cites W2054717068 @default.
- W2005211478 cites W2054778536 @default.
- W2005211478 cites W2055352886 @default.
- W2005211478 cites W2056673581 @default.
- W2005211478 cites W2057595624 @default.
- W2005211478 cites W2061296570 @default.
- W2005211478 cites W2061350756 @default.
- W2005211478 cites W2062333818 @default.
- W2005211478 cites W2064319545 @default.
- W2005211478 cites W2067099347 @default.
- W2005211478 cites W2067308263 @default.
- W2005211478 cites W2067559515 @default.
- W2005211478 cites W2067972129 @default.
- W2005211478 cites W2072887399 @default.
- W2005211478 cites W2073217161 @default.
- W2005211478 cites W2073549439 @default.
- W2005211478 cites W2074988686 @default.
- W2005211478 cites W2075544088 @default.
- W2005211478 cites W2076261307 @default.
- W2005211478 cites W2079258031 @default.
- W2005211478 cites W2080471464 @default.
- W2005211478 cites W2084367469 @default.
- W2005211478 cites W2084728071 @default.
- W2005211478 cites W2085652802 @default.
- W2005211478 cites W2085771800 @default.
- W2005211478 cites W2086714245 @default.
- W2005211478 cites W2088617006 @default.
- W2005211478 cites W2090122760 @default.
- W2005211478 cites W2092005716 @default.
- W2005211478 cites W2092290958 @default.
- W2005211478 cites W2105354089 @default.
- W2005211478 cites W2112702902 @default.
- W2005211478 cites W2125325383 @default.
- W2005211478 cites W2155411703 @default.
- W2005211478 cites W2156118817 @default.
- W2005211478 cites W2162344545 @default.
- W2005211478 cites W2329277471 @default.
- W2005211478 cites W4245131553 @default.
- W2005211478 cites W4249392273 @default.