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Natural product biomarkers as indicators of sources and transport of sedimentary organic matter in a subtropical river.
Jaffé, Rudolf; Rushdi, Ahmed I; Medeiros, Patricia M; Simoneit, Bernd R T.
Afiliação
  • Jaffé R; Environmental Geochemistry Laboratory, Southeast Environmental Research Center and Department of Chemistry and Biochemistry, Florida International University, Miami, 33199, USA.
Chemosphere ; 64(11): 1870-84, 2006 Sep.
Article em En | MEDLINE | ID: mdl-16530807
ABSTRACT
The sources and transformations of sedimentary organic matter along the Harney River, a representative subtropical river of the Florida Everglades, were assessed using a natural product biomarker approach. Sediment samples were collected from the headwaters to the Continental Shelf, with characteristic vegetation dominated by freshwater marsh species, mangrove (middle to lower estuary), and seagrass as the marine end-member. A peat sample was collected inland. All sample extracts were analyzed by GC-MS as underivatized and as silylated compounds. With these total extract analyses, major compound classes can be defined n-alkanols, n-alkanoic acids, methyl alkanoates, methyl alpha- and omega-hydroxyalkanoates, triterpenoids, phytosterols and saccharides, with traces of hydrocarbons. In general, the peat sample extract has a different overall composition compared to the sediment extracts. The major differences include distinct carbon number maxima for the lipid series (e.g., C(max)=28 for n-alkanols) probably from sawgrass and periphyton biomass, and predominance of phytosterols (sitosterol and stigmasterol) from higher plant detritus. In contrast, river sediment extracts contain biomarkers predominantly from mangrove-derived organic matter, such as the triterpenoids taraxerol and myricadiol. Significant amounts of saccharides and omega-hydroxyalkanoates are also found. Generally, compound concentrations decrease downstream due to dilution, and alteration of organic compounds from plant waxes and coastal vegetation is obvious in both peat and sediment samples. This is confirmed by the significant low abundance of n-alkanes and n-alkenoic acids due to biodegradation, oxidation of alpha-tocopherol to homophytanic acid gamma-lactone, and presence of traces of dihydrolacunosic acid, a photochemical alteration product of taraxerol.
Assuntos
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Coleções: 01-internacional Base de dados: MEDLINE Assunto principal: Compostos Orgânicos / Produtos Biológicos / Biomarcadores / Sedimentos Geológicos Idioma: En Ano de publicação: 2006 Tipo de documento: Article
Buscar no Google
Coleções: 01-internacional Base de dados: MEDLINE Assunto principal: Compostos Orgânicos / Produtos Biológicos / Biomarcadores / Sedimentos Geológicos Idioma: En Ano de publicação: 2006 Tipo de documento: Article