COMPOSITIONS AND SOURCES OF EXTRACTABLE ORGANIC MATTER IN MESOPOTAMIAN MARSHLAND SURFACE SEDIMENTS OF IRAQ. I: ALIPHATIC LIPIDS

dc.contributor.authorRushdi A.I.
dc.contributor.authorDouabul A.A.
dc.contributor.authorMohammed S.S.
dc.contributor.authorSimoneit B.R.T.
dc.date.accessioned2024-09-10T10:54:47Z
dc.date.available2024-09-10T10:54:47Z
dc.date.issued2006
dc.description.abstractShallow surface sediment samples from the Mesopotamian marshlands of Iraq were collected and analyzed to determine the distribution, concentrations and sources of aliphatic lipid compounds (n-alkanes, n-alkanols, n-alkanoic acids, and methyl n-alkanoates) and molecular markers of petroleum in these wetlands. The sediments were collected using a stainless steel sediment corer, dried, extracted with a dichloromethane/methanol mixture and then analyzed by gas chromatography-mass spectrometry (GC–MS). The aliphatic lipid compounds included n-alkanes, n-alkanoic acids, n-alkanols and methyl n-alkanoates with concentrations ranged from 6.8 to 31.1 μg/g, 4.1 to 5.0 μg/g, 5.9 to 7.7 μg/g and from 0.3 to 5.9 μg/g, respectively. The major sources of aliphatic lipids were natural from waxes of higher plants (24–30%) and microbial residues (42–30%), with a significant contribution from anthropogenic sources (27–30%, petroleum), based on the organic geochemical parameters and indices. Further studies are needed to characterize the rate, accumulation and transformation of various organic matter sources before and after re-flooding of these wetlands.
dc.identifierhttps://www.elibrary.ru/item.asp?id=53181763
dc.identifier.citationEnvironmental Geology, 2006, 50, 6, 857-866
dc.identifier.doi10.1007/s00254-006-0257-6
dc.identifier.issn0943-0105
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/45037
dc.subjectMESOPOTAMIAN MARSHES
dc.subjectUCM
dc.subjectGC-MS
dc.subjectLIPIDS
dc.subjectIRAQ
dc.titleCOMPOSITIONS AND SOURCES OF EXTRACTABLE ORGANIC MATTER IN MESOPOTAMIAN MARSHLAND SURFACE SEDIMENTS OF IRAQ. I: ALIPHATIC LIPIDS
dc.typeСтатья

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