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- W2372572904 abstract "C and N isotope studies of lakes can give us unique palaeolimnological information on such fundamental features as OM and nutrient sources, nutrient cycling, and water column stability. Lake Taihu is one of the largest freshwater lakes in China. Its east basin supports a dense population of vascular plants,while the west basin is almost free of vascular plants and consists of cyanobacteria. The C and N isotope analysis of sedimentary organic matter (OM) in different areas of Lake Taihu shows that the δ(~(13)C ) and δ(~(15)N) values of sedimentary OM in vascular plants dominated lake areas are generally higher than those in cyanobacteria dominated lake areas. During a transition from oligo-mesotrophy to meso-eutrophy in Lake Taihu, δ(~(13)C) and δ(~(15)N) values of sedimented OM gradually increase whereas TP and TN in sediments of different areas are distinct from one another due to the effect of various factors. δ(~(13)C) and δ(~(15)N) values of OM in sediments appear to be abrupt negative excursions at the stage of eutrophic lake. The results from δ(~(13)C) and δ(~(15)N ) of sedimented OM in the recent 50 years demonstrated that there existed two transitions of the lake environment respectively in 1950s and 1990s, which is coincident with the instrumental data." @default.
- W2372572904 created "2016-06-24" @default.
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- W2372572904 date "2005-01-01" @default.
- W2372572904 modified "2023-09-22" @default.
- W2372572904 title "ENVIRONMENTAL SIGNIFICANCE AND STABLE ISOTOPE SIGNATURES FROM SEDIMENTED ORGANIC MATTER IN LAKE TAIHU" @default.
- W2372572904 hasPublicationYear "2005" @default.
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