The organic matter of the recent sediments of Lake Beloe, West Siberia (from data of pyrolytic studies)

被引：19

作者：

Melenevskii, V. N. ^{[1
]}

Leonova, G. A. ^{[1
]}

Konyshev, A. S. ^{[1
]}

机构：

[1] Russian Acad Sci, Siberian Branch, AA Trofimuk Inst Petr Geol & Geophys, Novosibirsk 630090, Russia

来源：

RUSSIAN GEOLOGY AND GEOPHYSICS | 2011年 / 52卷 / 06期

关键词：

recent sediments; diagenesis; organic matter; pyrolysis; biomarker hydrocarbons; ROCK-EVAL PYROLYSIS; MARINE SILICEOUS ROCKS; MOLECULAR MECHANICS; HORONOBE HOKKAIDO; LATE MIOCENE; DIAGENESIS; SOIL; GEOCHEMISTRY; HYDROCARBONS; CUTICLES;

D O I：

10.1016/j.rgg.2011.05.002

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

Study of the Holocene sediments of Lake Beloe (West Siberia) in the depth range 0-137 cm gave an insight into the transformation of organic matter (OM) at the early stages of diagenesis. Analysis of OM was performed by pyrolytic methods (Rock Eval and pyrolysis + chromato-mass spectrometry). It showed that the macromolecular aliphatic structure of the kerogen and the precursors of sterane and hopane geomoleculessterenes and hopenesform at the early stages of diagenesis. We suggest that macrophytes and bacteria are the main sources of OM for the lacustrine sediments. (C) 2011, V. S. Sobolev IGM, Siberian Branch of the RAS. Published by Elsevier B. V. All rights reserved.

引用

页码：583 / 592

页数：10

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