Assessing the impact of long-term changes in climate and atmospheric deposition on a shallow alpine lake from southeast Tibet

被引:25
|
作者
Kang, Wengang [1 ]
Chen, Guangjie [1 ]
Wang, Jiaoyuan [1 ]
Huang, Linpei [1 ]
Wang, Lei [1 ]
Li, Rui [1 ]
Hu, Kui [1 ,2 ]
Liu, Yuanyuan [1 ]
Tao, Jianshuang [1 ]
Blais, Jules M. [3 ]
Smol, John P. [4 ]
机构
[1] Yunnan Normal Univ, Yunnan Key Lab Plateau Geog Proc & Environm Chang, Sch Tourism & Geog, Kunming 650500, Yunnan, Peoples R China
[2] North Dakota State Univ, Dept Biol Sci, Fargo, ND 58108 USA
[3] Univ Ottawa, Dept Biol, Ottawa, ON K1N 6N5, Canada
[4] Queens Univ, PEARL, Dept Biol, Kingston, ON K7L 3N6, Canada
基金
中国国家自然科学基金;
关键词
Atmospheric deposition; Climate warming; Catchment erosion; Lake-water TOC; Nitrogen stable isotope; Algae; ANTHROPOGENIC NITROGEN DEPOSITION; ASIAN MONSOON; ICE-CORE; NUTRIENT LIMITATION; REACTIVE NITROGEN; MOUNTAIN LAKES; PHYTOPLANKTON; SEDIMENTS; HOLOCENE; TRENDS;
D O I
10.1016/j.scitotenv.2018.09.066
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Regional warming and atmospheric nitrogen deposition have been widely recorded to impact remote catchments and alpine lakes; however, their independent roles and interactions have rarely been identified. Here, we combined down-core analyses of sedimentary mercury (Hg) and aluminum (Al) with multiple proxies (i.e. nitrogen stable isotope, chlorophyll a pigments, diatoms) for a radiometrically-dated sediment core of an alpine lake in southeast Tibet to track the atmospheric deposition of pollutants, and to examine possible effects of climate and catchment forcing over the past three centuries. The sediment data revealed that airborne deposition of Hg was recorded from the similar to 1860s, with an accelerating increase in anthropogenic Hg flux since the similar to 1960s. A synchronous decrease in reconstructed lake-water TOC indicated that acid deposition may have affected lake-water carbon concentrations and impaired catchment export of decomposed organic matter (OM). A moderate depletion of bulk sediment delta N-15 started from the similar to 1820s, but was followed by an enriching trend after the similar to 1970s. This positive shift of delta N-15 was associated with elevated sedimentOMand decreased catchment runoff of clastic materials (as inferred by Al). Sediment OM content displayed an accelerating increase from the similar to 1960s, with an increased input of autochthonous sources (i.e. lower bulk sediment C: N ratios), such as algae (as inferred by sedimentary chlorophyll a pigments). Meanwhile, climate warming and decreased lake-water TOC enhanced the production of algae, which was characterized by a more enriched delta N-15 signal than that of allochthonousOM. Furthermore, atmospheric acid deposition was significantly related to diatom assemblage changes, with an increase in acidophilous taxa. Our sediment evidence revealed the dominating impact of climate and catchment processes on lake-water chemistry and algal shifts in the context of atmospheric nitrogen deposition, and highlighted an increasing link of external forcing with in-lake processes in enriching sediment delta N-15 signal over the last few decades. (C) 2018 Elsevier B.V. All rights reserved.
引用
收藏
页码:713 / 724
页数:12
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