琵琶湖芦苇带附生藻类和浮游藻类分解尿素的季节变化

O. Mitamura, J. Tachibana, K. Kondo, S. Ueda, Y. Seike
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引用次数: 7

摘要

在浅水近岸地区,经常观察到大量的涌现和淹没的大型植物和相关的附生微生物在淹没的茎上。附生微生物参与了大植带的生物地球化学循环。琵琶湖芦苇群落面积达3公里(含泻湖),占水下大型植物的60%。芦苇一年四季都有大量的基质供附生微生物在芦苇带定植。在沿海地区,这些附生藻类的直立产量通常大于浮游植物。琵琶湖芦苇带是湖泊生态系统生物地球化学动力学研究的重要亚系统。附生微生物对生物地球化学循环的贡献与芦苇茎作为附生基质的有效表面积有关。一些研究者对芦苇茎上附生初生产量的测量进行了研究。一些关于琵瓦湖芦苇带的生物和化学数据已被报道(tananimizu等人,1981年,ÜHTSUKA等人,1996年,MITAMURA & TACHIBANA 1999年,MITO等人,2002年,MITAMURA等人,2005年)。然而,关于芦苇带生物地球化学循环的信息很少。尿素作为浮游植物的重要氮源及其在生物地球化学氮循环中的重要作用,为阐明天然水体中尿素的分布和代谢积累了大量的信息。天然浮游植物对尿素的分解已被证明使用e标记尿素(MITAMURA & SAuo 1986, IRMISCH 1991, MITAMURA et . 1994,1995,2000,2005)。以前的研究人员报告说,浮游植物可能比细菌更有效地分解了远洋水域的尿素。然而,关于附生微生物分解尿素的知识是相当有限的。本研究的目的是研究附生藻类对琵琶湖浅海地区尿素分解的贡献。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Seasonal change in urea decomposition by epiphytic and planktonic algae in a reed zone of Lake Biwa, Japan
A dense biomass of emergent and submerged macrophytes and associated epiphytic microorganisms on submerged stems are often observed in shallow near-shore areas. Epiphytic microorganisms contribute to biogeochemical cycling in macrophyte zones. In Lake Biwa, Phragmites communis covers an area of3 km (including lagoons), which comprises 60% o f submerged macrophytes. Throughout the year, Phragmites has a large substratum for epiphytic microbial colonization in the reed zone. In the littoral zone, the standing crop o f these epiphytic algae is generally larger than that of phytoplankton. The reed zone in Lake Biwa is an important subecosystem for the study ofbiogeochemical dynamics in a lake ecosystem. The contribution of the epiphytic microorganisms to the biogeochemical cycling is related to the available surface area of reed stems as the epiphytic substratum. The measurement of epiphytic primary production on reed stems has been studied by several investigators. Some available biological and chemical data on the reed zones of Lake Biwa has been reported (TANIMIZU et al. 1981, ÜHTSUKA et al. 1996, MITAMURA & TACHIBANA 1999, MITO et al. 2002, MITAMURA et al. 2005). There is, however, little information on the biogeochemical cycling in the reed zone. Much information has been accumulated to elucidate the distribution and metabolism o f urea in natural water bodies because of its significance as an important nitrogen source for phytoplankton and the appreciation o f its ro le in the biogeochemical nitrogen cycle. Urea decomposition by natural phytoplankton has been demonstrated using e labeled urea (MITAMURA & SAuo 1986, IRMISCH 1991, MITAMURA et al. 1994, 1995, 2000, 2005). Previous workers reported that urea in the pelagic waters was presumably decomposed more effectively by phytoplankton than by bacteria. Knowledge of urea decomposition by epiphytic microorganisms, however, is quite limited. The purpose of this study was to provide information on the contribution of epiphytic algae to the urea decomposition in a shallow littoral area of Lake Biwa.
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