西喀拉期线性凹陷海相沉积物中烃类生物标志物的深度分布

IF 0.7 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
V. S. Sevastyanov, V. S. Fedulov, V. Yu. Fedulova, R. H. Dzhenloda, N. V. Dushenko, S. A. Voropaev
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引用次数: 0

摘要

海洋沉积物的分子和烃组成研究为研究沉积有机质提供了重要的信息。本文研究了西喀拉期线性坳陷沉积盖层中烃类和分子标志物的深度分布。为此,在R/V Akademik Mstislav Keldysh号第89次巡航期间,在7444点和7441点取样了两个沉积物岩心。采用气相色谱-质谱法测定了正构烷烃的分布,确定了海洋沉积物中沉积物有机质生物标志物指数的分布规律。结果表明,7444和7441两个站点的海相沉积物OM主要来源于高等陆生植被。从其Ts/(Ts + Tm)比率可以看出,OM的期限较低。从H31-S/H31-(S + R)和NAR指数来看,研究区有少量的原油烃持续流入,背景点7441的流入量要小得多。CPI25-33、TAR和NAR的分布表明,人为来源的碳氢化合物主要分布在背景点7441 0 ~ 15 cm沉积物的近表层。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Distribution of Hydrocarbon Biomarkers with Depth in Marine Sediments in the Area of the Linear Depression of the West Kara Stage

Studies of molecular and hydrocarbon composition of marine sediments provide important information on sedimentary organic matter (OM). In this work, the distribution of hydrocarbons and molecular markers with depth in the sedimentary cover of the linear depression of the West Kara stage was studied. To do this, two sediment cores were sampled during 89th cruise of the R/V Akademik Mstislav Keldysh at site 7444 and at background site 7441. The distribution of n-alkanes was measured by GC-MS analysis, and the distribution patterns of the biomarker indices of sedimentary OM in the marine sediments with depth were determined. It was shown that higher terrestrial vegetation was the dominant source to the sedimentary OM of marine sediments at sites 7444 and 7441. The OM is of low maturity, as follows from its Ts/(Ts + Tm) ratio. According to the values of H31-S/H31-(S + R) and NAR indices, a small constant inflow of oil hydrocarbons occurs in the study area, and a much lower inflow takes place at background site 7441. The distribution of the CPI25–33, TAR, and NAR suggest that hydrocarbons of anthropogenic origin occur in the near-surface layers of 0–15 cm sediment at background site 7441.

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来源期刊
Geochemistry International
Geochemistry International 地学-地球化学与地球物理
CiteScore
1.60
自引率
12.50%
发文量
89
审稿时长
1 months
期刊介绍: Geochemistry International is a peer reviewed journal that publishes articles on cosmochemistry; geochemistry of magmatic, metamorphic, hydrothermal, and sedimentary processes; isotope geochemistry; organic geochemistry; applied geochemistry; and chemistry of the environment. Geochemistry International provides readers with a unique opportunity to refine their understanding of the geology of the vast territory of the Eurasian continent. The journal welcomes manuscripts from all countries in the English or Russian language.
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