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中国亚热带湖泊湖相沉积物中有机质来源的分子生物标志物。

Molecular biomarkers for sources of organic matter in lacustrine sediments in a subtropical lake in China.

机构信息

School of Geography Science, Nanjing Normal University, 1 Wenyuan Road, Qixia, Nanjing 210046, China.

出版信息

Environ Pollut. 2013 May;176:284-91. doi: 10.1016/j.envpol.2013.01.041. Epub 2013 Feb 27.

Abstract

N-alkanes distributions and stable isotopic compositions (δ(13)C and δ(15)N) in the lacustrine sediments of Shijiu lake were measured to assess whether biological source information was recorded in the molecular biomarker. Results showed regular unimodal n-alkanes distribution in range of C16-C33 with strong predominance of odd-numbered n-alkanes, maximizing at C29. The δ(15)N for SON were uniformly low, ranging from -6.7‰ to 3.8‰ and C/N ratios ranged from 6.6 to 10.0, suggesting that most of organic matter was influenced by terrestrial characteristics of the watershed. The δ(13)C for C27 to C31n-alkanes and for SOC varied from -32.9‰ to -26.6‰ and -23.4‰ to -21.6‰, respectively, falling within the range of corresponding n-alkanes in leaves mainly from C3 land plants. The values of C/N, CPI, OEP, ACL and C27/C31 exhibit similar temporal changes with the primary production, showing enhanced eutrophication resulted from increased anthropogenic activities in Shijiu lake from 1852 to 2010.

摘要

十九湖湖泊沉积物中正构烷烃分布及稳定同位素组成(δ¹³C 和 δ¹⁵N)的研究,旨在评估生物源信息是否记录在分子生物标志物中。结果表明,正构烷烃分布范围为 C16-C33,呈单峰分布,奇数碳优势明显,最大值为 C29。SON 的 δ¹⁵N 普遍较低,范围为-6.7‰至 3.8‰,C/N 比值范围为 6.6 至 10.0,表明大部分有机质受流域陆地特征的影响。C27-C31 正构烷烃和 SOC 的 δ¹³C 分别为-32.9‰至-26.6‰和-23.4‰至-21.6‰,分别落在主要来自 C3 陆地植物的相应正构烷烃的范围内。C/N、CPI、OEP、ACL 和 C27/C31 的值与初级生产力具有相似的时间变化,表明 1852 年至 2010 年,十九湖富营养化程度因人为活动的增加而增强。

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