Characteristics and sources of chromophoric dissolved organic matter in lakes of the Yungui Plateau.pdf

Characteristics and sources of chromophoric dissolved organic matter in lakes of the Yungui Plateau.pdf

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Characteristics and sources of chromophoric dissolved organic matter in lakes of the Yungui Plateau

Characteristics and sources of chromophoric dissolved organic matter in lakes of the Yungui Plateau, China, differing in trophic state and altitude Yunlin Zhang,a,*,1 Enlou Zhang,a Yan Yin,a Mark A. van Dijk,b Longqing Feng,c Zhiqiang Shi,a Mingliang Liu,a and Boqiang Qina a Taihu Lake Laboratory Ecosystem Research Station, State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing, China bNetherlands Institute of Ecology (NIOO-KNAW), Department of Microbial Ecology, Nieuwersluis, The Netherlands c College of Resource and Environment Science, Nanjing Agricultural University, Nanjing, China Abstract The high-mountain lakes on the Yungui Plateau in China are exposed to high-intensity ultraviolet radiation, and contain low concentrations of chromophoric dissolved organic matter (CDOM). We determined CDOM absorption, fluorescence, composition, and source in 38 lakes on the Yungui Plateau at altitudes of 1516 to 4591 m above sea level. Total nitrogen (TN), total phosphorus (TP), and chlorophyll a (Chl a) concentrations significantly increased with increasing trophic state, and decreased with altitude. The CDOM absorption coefficient aCDOM(280) significantly increased with increasing trophic state, but not with altitude. There were significant and negative correlations between altitude and TN, TP, Chl a concentrations, and aCDOM(280). Parallel factor analysis identified two humic-like and two protein-like fluorescent components. Humic-like component 1 was terrestrially derived and positively correlated to CDOM absorption. Component 2 was similar to a marine humic-like substance originating from biological degradation of phytoplankton. Components 3 and 4 were autochthonous tryptophan- like and tyrosine-like fluorophores. CDOM was, thus, a mixture of material from the catchment and autochthonous material produced by biota in the lake. CDOM fluorescence characteristics of oligotrophic and mesotroph

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