Composition of organic compounds in bottom sediments of lakes in the taiga and steppe zones in Siberia

The paper presents chromatographic–mass spectrometric data on the individual composition of organic compounds in sapropel-like deposits of lakes in the steppe, forest–steppe, and three taiga natural climatic zones (NCZ) in Khakassia and western Siberia. Data on the individual composition of n -alkan...

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Veröffentlicht in:Geochemistry international 2017-12, Vol.55 (12), p.1090-1104
Hauptverfasser: Serebrennikova, O. V., Strel’nikova, E. B., Russkikh, I. V.
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Strel’nikova, E. B.
Russkikh, I. V.
description The paper presents chromatographic–mass spectrometric data on the individual composition of organic compounds in sapropel-like deposits of lakes in the steppe, forest–steppe, and three taiga natural climatic zones (NCZ) in Khakassia and western Siberia. Data on the individual composition of n -alkanes, carboxylic acids and their esters, thiophenes, phytol, phytone, steroids, and di- and triterpenoids and on their distribution in the sediments show systematic variations in the composition of the organic matter (OM) with increasing ambient temperature and the aridity of the climate. The concentrations of all groups of the compounds in lacustrine sediments decrease southward, and simultaneously esters with long (up to С 20 ) alkyl substituents appear. The concentrations of oxygen-bearing compounds increase among the acyclic structures and triterpenoids, as also do the concentrations of structures ketonic substituents among the steroids. The dominance of the carboxylic acids and their esters by high molecular weight homologues gives way to the dominance of palmic acid and its derivatives. Among n -alkanes, the dominance of С 27 and С 29 hydrocarbons typical of terrestrial plants gives way to a higher percentage of homologues С 21 –С 25 (macrophytes) and С 31 (herbaceous plants). Among the tocopheroles, the concentration of the oxidized form of α-tocopherol (acetate) increases.
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The concentrations of oxygen-bearing compounds increase among the acyclic structures and triterpenoids, as also do the concentrations of structures ketonic substituents among the steroids. The dominance of the carboxylic acids and their esters by high molecular weight homologues gives way to the dominance of palmic acid and its derivatives. Among n -alkanes, the dominance of С 27 and С 29 hydrocarbons typical of terrestrial plants gives way to a higher percentage of homologues С 21 –С 25 (macrophytes) and С 31 (herbaceous plants). 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V.</au><au>Strel’nikova, E. B.</au><au>Russkikh, I. V.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Composition of organic compounds in bottom sediments of lakes in the taiga and steppe zones in Siberia</atitle><jtitle>Geochemistry international</jtitle><stitle>Geochem. Int</stitle><date>2017-12-01</date><risdate>2017</risdate><volume>55</volume><issue>12</issue><spage>1090</spage><epage>1104</epage><pages>1090-1104</pages><issn>0016-7029</issn><eissn>1556-1968</eissn><abstract>The paper presents chromatographic–mass spectrometric data on the individual composition of organic compounds in sapropel-like deposits of lakes in the steppe, forest–steppe, and three taiga natural climatic zones (NCZ) in Khakassia and western Siberia. Data on the individual composition of n -alkanes, carboxylic acids and their esters, thiophenes, phytol, phytone, steroids, and di- and triterpenoids and on their distribution in the sediments show systematic variations in the composition of the organic matter (OM) with increasing ambient temperature and the aridity of the climate. The concentrations of all groups of the compounds in lacustrine sediments decrease southward, and simultaneously esters with long (up to С 20 ) alkyl substituents appear. The concentrations of oxygen-bearing compounds increase among the acyclic structures and triterpenoids, as also do the concentrations of structures ketonic substituents among the steroids. The dominance of the carboxylic acids and their esters by high molecular weight homologues gives way to the dominance of palmic acid and its derivatives. Among n -alkanes, the dominance of С 27 and С 29 hydrocarbons typical of terrestrial plants gives way to a higher percentage of homologues С 21 –С 25 (macrophytes) and С 31 (herbaceous plants). Among the tocopheroles, the concentration of the oxidized form of α-tocopherol (acetate) increases.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S0016702917090087</doi><tpages>15</tpages></addata></record>
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subjects Acetates
Acetic acid
Acids
Alkanes
Ambient temperature
Aquatic plants
Aridity
Bottom sediments
Carboxylic acids
Climatic zones
Composition
Dominance
Earth and Environmental Science
Earth Sciences
Esters
Geochemistry
Homology
Hydrocarbons
Lacustrine sedimentation
Lakes
Macrophytes
Molecular weight
Organic compounds
Organic matter
Palmic acid
Phytol
Sapropels
Sediment
Sediments
Spectrometry
Steppes
Steroid hormones
Steroids
Structures
Taiga
Thiophenes
Tocopherol
Triterpenoids
title Composition of organic compounds in bottom sediments of lakes in the taiga and steppe zones in Siberia
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