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A geochemical study of long-chain n-aldehydes in Washington coastal sediments
Affiliation:1. Department of Biology, Faculty of Science, Razi University, Kermanshah, Iran;2. Transplant Research Center, Namazi Hospital, Shiraz University of Medical Sciences, Shiraz, Iran;3. Department of Immunology, Prof. Alborzi Clinical Microbiology Research Center, Shiraz University of Medical Sciences, Shiraz, Iran;4. Université Paris-Sud 11, Villejuif 94807, France;5. Inserm, U1197, Hôpital Paul Brousse, Villejuif 94807, France;1. Consortium for Fossil Fuel Science, Department of Chemical and Materials Engineering, University of Kentucky, Lexington, KY 40508, United States;2. Department of Earth and Environmental Sciences, University of Kentucky, Lexington, KY 40508, United States;3. Department of Mining Engineering, University of Kentucky, Lexington, KY 40508, United States;1. Institute of Chemistry, UFRGS, Av. Bento Gonçalves 9500, CEP 91501-970 Porto Alegre, RS, Brazil;2. Department of Geology, UFRGS, Av. Bento Gonçalves 9500, CEP 91501-970 Porto Alegre, RS, Brazil
Abstract:A series of n-aldehydes, C20 to C32, with strong even-to-odd carbon preference was identified in the mixture of solvent extractable lipids isolated from various Washington coastal sediments. A limited survey of the lipid composition of surface waxes of foliage and cuticular waxes of pollen from several major plant species indigenous to the Pacific Northwest revealed that similar series of n-aldehydes are intrinsic to regional vegetation. Debris from such plants, discharged at the mouth of the Columbia River, represents a “preformed” source of the n-aldehyde series accumulating in sediments from the Washington coastal region. Although the evidence suggests n-aldehydes are largely introduced erosionally to this region as a chemical component of land-derived debris and are not formed in situ in the coastal sediments, further study is warranted to establish the postdepositional stability of this series of compounds relative to other lipids of higher plantwax origin. Despite but few literature reports of the occurrence of these geochemicals, long-chain n-aldehydes are very likely common in many sediments from environments that receive an input of detrital organic matter from higher plants.
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