MOE Laboratory for Earth Surface Processes, College of Urban & Environmental Sciences, Peking University, Beijing 100871, China; Stockbridge School of Agriculture, University of Massachusetts, Amherst, MA 01003, USA.
MOE Laboratory for Earth Surface Processes, College of Urban & Environmental Sciences, Peking University, Beijing 100871, China.
Sci Total Environ. 2017 Mar 1;581-582:874-884. doi: 10.1016/j.scitotenv.2017.01.037. Epub 2017 Jan 12.
The sources of sediment organic matter (SOM) could be explained by various indicators. To test their biases and associations, the present study determined multiple indicators for SOM source apportionment, including elemental analysis (carbon and nitrogen, and their stable isotope δC and δN), n-alkanes compositions as well as derivative indicators (e.g., terrigenous to aquatic ratio), and carbon isotopes of n-alkane in Lake Chaohu, a eutrophic lake. The spatial variation of anthropogenic effects could be revealed by SOM elemental variations. The n-alkanes of all samples had a bimodal distribution with the 1st peak at n-alkane with 17 carbons (C17) and the 2nd predominant peak at C29. The parity advantage index of n-alkanes indicated that the sediments had mixed characteristics of both endogenous and terrigenous sources. Some n-alkanes indicators also revealed eutrophication characteristics of dominant algae in Lake Chaohu. SOM received a mixed contribution of plankton (I), low-latitude terrestrial high-grade plants (II) and microbial material (III) as indicated by isotopic compositions of long-chain n-alkane. Multiport element model (MEM) showed the contribution of self-generated sources of organic matter in Lake Chaohu is >50%, indicating the historic serious eutrophication in Lake Chaohu. The main sources of SOM in the eastern part of the lake were algae and terrestrial input, with little input from microbes, and the contribution from algae decreased from west to east. The multiple indicators' judgment by MEM and principle component analysis (PCA) was of ecological significance and proposed because they offered scientific tools for disclosing the historic variations of SOM as well as their sources.
沉积物有机质(SOM)的来源可以用各种指标来解释。为了检验它们的偏差和关联,本研究确定了 SOM 源分配的多个指标,包括元素分析(碳和氮及其稳定同位素 δC 和 δN)、正烷烃组成以及衍生指标(如陆源与水生比)和巢湖沉积物中正烷烃的碳同位素。通过 SOM 元素变化可以揭示人为影响的空间变化。所有样品的正烷烃均呈双峰分布,第一个峰在 17 个碳原子(C17)的正烷烃,第二个主要峰在 C29。正烷烃的奇偶优势指数表明,沉积物具有内源和陆源混合特征。一些正烷烃指标也揭示了巢湖优势藻类的富营养化特征。根据长链正烷烃的同位素组成,SOM 受到浮游生物(I)、低纬度陆地高等植物(II)和微生物物质(III)的混合贡献。多端口元素模型(MEM)显示,巢湖自身有机质的来源贡献>50%,表明巢湖历史上严重富营养化。湖泊东部 SOM 的主要来源是藻类和陆地输入,微生物输入较少,藻类的贡献从西向东减少。MEM 和主成分分析(PCA)的多种指标判断具有生态意义,并提出了这些指标,因为它们为揭示 SOM 的历史变化及其来源提供了科学工具。