Инд. авторы:	Ishiwatari R., Fujino N., Brincat D., Yamamoto S., Takahara H., Shichi K., Krivonogov S.K.
Заглавие:	A 35 kyr record of organic matter composition and δ13C of n-alkanes in bog sediments close to Lake Baikal: Implications for paleoenvironmental studies
Библ. ссылка:	Ishiwatari R., Fujino N., Brincat D., Yamamoto S., Takahara H., Shichi K., Krivonogov S.K. A 35 kyr record of organic matter composition and δ13C of n-alkanes in bog sediments close to Lake Baikal: Implications for paleoenvironmental studies // Organic Geochemistry. - 2009. - Vol.40. - Iss. 1. - P.51-60. - ISSN 0146-6380.
Внешние системы:	DOI: 10.1016/j.orggeochem.2008.09.007; SCOPUS: 2-s2.0-57449092494;
Реферат:	eng: We characterized the compositions of organic compounds in a Cheremushka bog sediment core (deposited over the last 35 kyr), located at the eastern coast of Lake Baikal, to obtain basic information about the terrestrial organic matter (OM) which contributed to Lake Baikal sediments. The bog sediment was analyzed for the molecular composition of n-alkanes, lignin phenols and n-C24 to C30 alkanoic acids, as well as the carbon isotopic composition of plant wax derived n-C27 to C33 alkanes. Concentrations of lignin phenols [vanillyl (V) plus syringyl (S) phenols] normalized to total organic carbon (TOC) in the Holocene are twice those for the last glacial maximum (LGM), while concentrations of TOC-normalized n-C24 to C30 alkanoic acids do not change markedly in this period. Thus, the ratio of lignin phenols to n-C24 to C30 alkanoic acids increases from the LGM to the Holocene. This result is essentially consistent with pollen analysis indicating an expansion of woody plants in the Holocene and a prevailing herb-abundant environment for the LGM. The δ13C values of n-C27 to C33 alkanes (e.g. -29‰ to -33‰ for C31) indicate the presence of C3-dominant plants throughout the core. The contribution of terrestrial OM to Lake Baikal sediments was estimated using the biomarkers, on the assumption that the OM in the bog sediments is a representative of the terrestrial OM around the lake. Hence, the estimation using lignin phenol or n-C24 to C30 alkanoic acid parameters indicates that 11-24% of the TOC in the Academician Ridge sediments is land-derived for both the Holocene and the LGM, which is similar to the estimates from C/N values of bulk OM. However, the estimates for terrestrial OM using the n-C27 to C33 alkane parameter are generally higher than those using lignin phenol or n-C24 to C30 alkanoic acid parameters. The difference is thought to be associated with the difference in source and behavior of these biomarkers. © 2008 Elsevier Ltd. All rights reserved.
Ключевые слова:	Holocene; Lake Baikal; Last glacial maximums; Molecular compositions; Organic matter compositions; Paleoenvironmental studies; Pollen analyses; Sediment cores; Terrestrial organic matters; Total organic carbons; Woody plants; Arctic engineering; Biogeochemistry; Biological materials; Carboxylic acids; Chemical analysis; Fire hazards; Hydrocarbons; Lakes; Landforms; Lignin; Organic carbon; Organic compounds; Paraffins; Sedimentation; Sedimentology; Wetlands; Phenols; alkane; biomarker; bog; chemical composition; concentration (composition); isotopic composition; Last Glacial Maximum; lignin; organic matter; paleoenvironment; phenol; sediment chemistry; sediment core; Alkanes; Arctic Regions; Carboxylic Acids; Chemical Composition; Fires; Geochemistry; Hydrocarbons; Lakes; Phenols; Sedimentation; Sediments; Swamps; Wetlands; Eurasia; Russian Federation; Carbon isotopic compositions; Lake Baikal;
Издано:	2009
Физ. характеристика:	с.51-60