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The use of stable carbon isotopes as tracers of ecosystem functioning in contrasting wetland ecosystems of Lake Victoria, Kenya

机译:在肯尼亚维多利亚湖湿地生态系统对比中,使用稳定的碳同位素作为生态系统功能的示踪剂

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摘要

Aquatic macrophytes and sediments from two contrasting wetland ecosystems of Lake Victoria, Kenya (Lower Sondu Miriu and Kibos systems) were analyzed for their stable carbon isotopic composition in order to observe patterns in system functioning in these two ecosystems. The aquatic macrophytes had carbon isotope ratios ranging from −8.92 to −29.18 per mil (parts per thousand difference from the reference). For the dominant macrophytes, we observed most 13C enriched values for Cyperus papyrus and most 13C depleted values for Eichhornia crassipes. On transects from the river to the lake, Kibos sediments maintained lower carbon isotope signatures compared to the Lower Sondu Miriu sediments. The possible causes of the observed variation in the δ13C signatures from sediments and aquatic macrophytes in the two-wetland ecosystems are outlined.
机译:分析了肯尼亚维多利亚湖两个相反的湿地生态系统(下桑杜米尔河和基博斯系统)的水生植物和沉积物的稳定碳同位素组成,以便观察这两个生态系统的系统功能模式。水生植物的碳同位素比范围为-8.92至-29.18 / mil(与参考相比千分之几)。对于优势大型植物,我们观察到莎草纸莎草的大多数富集13 C值,凤眼凤梨的大多数13 C耗尽值。在从河到湖的样带上,与下桑杜米留河沉积物相比,基博斯沉积物保持了较低的碳同位素特征。概述了两个湿地生态系统中沉积物和水生植物的δ13C信号变化的可能原因。

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