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DOI10.1007/s10533-020-00640-3
Isotope alteration caused by changes in biochemical composition of sedimentary organic matter
Liu X.; Hilfert L.; Barth J.A.C.; van Geldem R.; Friese K.
发表日期2020
ISSN1682563
卷号147期号:3
英文摘要Stable carbon (C) and nitrogen (N) isotope ratios of sedimentary organic matter (OM) can reflect the biogeochemical history of aquatic ecosystems. However, diagenetic processes in sediments may alter isotope records of OM via microbial activity and preferential degradation of isotopically distinct organic components. This study investigated the isotope alteration caused by preferential degradation in surface sediments sampled from a eutrophic reservoir in Germany. Sediments were treated sequentially with hot water extraction, hydrochloric acid hydrolysis, hydrogen peroxide oxidation and di-sodium peroxodisulfate oxidation to chemically simulate preferential degradation pathways of sedimentary OM. Residue and extracts from each extraction step were analyzed using elemental analyzer-isotope ratio mass spectrometry and solid-state 13C nuclear magnetic resonance spectroscopy. Our results show that stable C and N isotope ratios reacted differently to changes in the biochemical composition of sedimentary OM. Preferential degradation of proteins and carbohydrates resulted in a 1.2‰ depletion of 13C, while the isotope composition of 15N remained nearly the same. Sedimentary δ15N values were notably altered when lignins and lipids were oxidized from residual sediments. Throughout the sequential fractionation procedure, δ13C was linearly correlated with the C:N of residual sediments. This finding demonstrates that changes in biochemical composition caused by preferential degradation altered δ13C values of sedimentary OM, while this trend was not observed for δ15N values. Our study identifies the influence of preferential degradation on stable C isotope ratios and provide additional insight into the isotope alteration caused by post-depositional processes. © 2020, Springer Nature Switzerland AG.
英文关键词Biochemical composition; Organic matter; Preferential degradation; Sediment; Stable carbon and nitrogen isotope ratios
学科领域biochemical composition; carbon isotope; hydrochloric acid; isotopic composition; isotopic fractionation; lipid; microbial activity; nitrogen isotope; nuclear magnetic resonance; organic matter; sediment chemistry; Germany
语种英语
scopus关键词biochemical composition; carbon isotope; hydrochloric acid; isotopic composition; isotopic fractionation; lipid; microbial activity; nitrogen isotope; nuclear magnetic resonance; organic matter; sediment chemistry; Germany
来源期刊Biogeochemistry
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/120382
作者单位Department Lake Research, UFZ – Helmholtz Centre for Environmental Research, Brueckstr. 3a, Magdeburg, 39114, Germany; Institute for Chemistry, Otto-von-Guericke – University of Magdeburg, Campus, Magdeburg, 39106, Germany; Department of Geography and Geosciences, GeoZentrum Nordbayern, Friedrich-Alexander University, Erlangen-Nuremberg, Germany; Southern Laboratory of Ocean Science and Engineering (Guangdong, Zhuhai), Zhuhai, 519082, China
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GB/T 7714
Liu X.,Hilfert L.,Barth J.A.C.,et al. Isotope alteration caused by changes in biochemical composition of sedimentary organic matter[J],2020,147(3).
APA Liu X.,Hilfert L.,Barth J.A.C.,van Geldem R.,&Friese K..(2020).Isotope alteration caused by changes in biochemical composition of sedimentary organic matter.Biogeochemistry,147(3).
MLA Liu X.,et al."Isotope alteration caused by changes in biochemical composition of sedimentary organic matter".Biogeochemistry 147.3(2020).
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