Shen Bei-Bei, Wu Jing-Lu, Zeng Hai-Ao, Zhang Yong-Dong, Jin Miao
State Key Laboratory of Lake and Environmental Sciences, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China.
University of Chinese Academy of Sciences, Beijing 100049, China.
Huan Jing Ke Xue. 2017 Sep 8;38(9):3682-3688. doi: 10.13227/j.hjkx.201702062.
Concentrations and distribution of -alkanes (-C to -C) in Lake Wanghu sediment core were analyzed to investigate the environmental changes in the lake during the past~100 years. Relatively higher concentrations of mid-and long-chain -alkanes with a strong odd-over-even carbon number predominance indicated organic matter contributions dominated by aquatic macrophytes and terrestrial plants. The lower values of 2-C/(-C+-C) highlighted a type of landscape dominated by woody plants. The environmental changes that have been happening over the past 100 years in Lake Wanghu can be divided into three stages, based on the organic matter sources inferred from the changes in -alkane parameters in the sediments. Before the 1950s, higher values of terrigenous/aquatic ratio (TAR) and high-/low-molecular weight n-alkanes (H/L) indicated vascular, plant-derived sediments deposited during a low-nutrient, clear-water phase with frequent water exchange between the lake and the Yangtze River. Between the 1950s and 1980s, decrease in values of H/L and TAR, and increase in the proportion of mid-and short-chain -alkanes indicated a shift towards mid-and shorter-chain components likely associated with the increasing contribution of macrophytes and algae. Lower 2-C/(-C+-C) values indicated a relatively low algal abundance. In that stage, the lake trophic state increased slightly with the decreasing influence of the Yangtze River flow. After the 1980s,H/L and TAR values increased and then decreased, total -alkane concentrations and 2-C/(-C+-C) increased significantly, especially after 2000s, suggesting the main contributor to high organic matter input most likely shifted to algae because of the eutrophication caused by anthropogenic activities.
分析了望湖沉积物岩芯中C23 - C33正构烷烃的浓度和分布,以研究该湖泊过去约100年的环境变化。中长链正构烷烃浓度相对较高,且具有很强的碳数奇偶优势,表明水生植物和陆生植物对有机质的贡献占主导。2-甲基十七烷/(十七烷+十九烷)的较低值突出了以木本植物为主导的景观类型。根据沉积物中正构烷烃参数变化推断的有机质来源,望湖在过去100年发生的环境变化可分为三个阶段。20世纪50年代之前,陆源/水生比值(TAR)和高分子量/低分子量正构烷烃(H/L)的较高值表明,在湖泊与长江之间频繁进行水交换的低营养、清水阶段,有维管束植物来源的沉积物沉积。20世纪50年代至80年代,H/L和TAR值下降,中短链正构烷烃比例增加,表明向中短链组分转变,这可能与大型植物和藻类贡献增加有关。较低的2-甲基十七烷/(十七烷+十九烷)值表明藻类丰度相对较低。在那个阶段,随着长江水流影响的减弱,湖泊营养状态略有增加。20世纪80年代之后,H/L和TAR值先升高后降低,总正构烷烃浓度和2-甲基十七烷/(十七烷+十九烷)显著增加,特别是在21世纪之后,这表明由于人为活动导致的富营养化,高有机质输入的主要贡献者很可能转向了藻类。