期刊
QUATERNARY INTERNATIONAL
卷 536, 期 -, 页码 52-59出版社
PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.quaint.2019.11.044
关键词
Shallow lake; Sediment core; Subfossil Cladocera; Environmental indices; Shengjin lake
资金
- National Natural Science Foundation of China (NSFC) [41573129]
- National Basic Science and Technology Special Project [2014FY110400]
- National Key Research and Development Program of China [2019YFA0607100]
Shengjin Lake is a typical Yangtze River-connected lake, that is also a national nature reserve and a Wetland of International Importance. In order to evaluate the eco-environmental evolution of Shengjin Lake, a(210)Pb- and Cs-137-dated sediment core collected from the upper part of the lake was analyzed. Based on a biological indicator (subfossil cladoceran) and geochemical indicators (loss on ignition (LOI), total organic carbon (TOC), delta C-13 of bulk sediments (delta C-13(org), total phosphorous (TP) and total nitrogen (TN)), we revealed the changes in the cladoceran assemblages and eco-environmental processes of Shengjin Lake. The results showed that there was a healthy ecological environment with low nutrient levels in Shengjin Lake before the 1980s. However, the increasing levels of the eutrophic species B. longirostris, nutrients (TN and TP) and organic matters (LOI and TOC), and the decreasing delta C-13(org) in recent decades indicated that the trophic state of Shengjin Lake has increased since the 1980s. This corresponded with increasing anthropogenic effects, including land reclamation, chemical fertilizer application, and sluice construction. In addition, the droppings of water birds also promoted increases in nutrient and organic matters levels in Shengjin Lake.
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