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首页> 外文期刊>Limnologica >Aquatic hyphomycetes in hyporheic freshwater habitats of southwest India
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Aquatic hyphomycetes in hyporheic freshwater habitats of southwest India

机译:印度西南部淡水淡水生境中的水生真菌

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摘要

The hyporheic zones constitute a major site of storage of organic matter and energy flow in freshwater ecosystems. To complement the studies carried out in North America and Europe, we evaluated the sediment quality and occurrence of aquatic hyphomycetes in coarse particulate organic matter (CPOM; ≥5. mm) and fine particulate matter (FPM; ≤1. mm) in three locations of Kaiga stream and eight locations of Kadra dam of the River Kali in Western Ghats. The pH of sediments of stream and dam was acidic (5.8-6.6) and the average organic carbon of stream sediments was higher than dam sediments (8.6% vs. 3.9%). Among the eight minerals monitored, Fe was highest in all sediments and Ni was below detectable limit in four dam sediments. Spores of aquatic hyphomycetes were directly released from the CPOM fractions of sediments upon bubble chamber incubation, while the FPM fractions produced spores indirectly by colonization of sterile leaf baits followed by bubble chamber incubation. The species richness and diversity in CPOM was higher than FPM in stream as well as dam sediments. The Sorensen's similarity indices between the fungal flora of CPOM in stream (66.7-81.8%) and dam (69.2-88%) locations were generally higher than FPM. The spore output per mg CPOM was between 1215 (dam) and 3384 (stream). The species richness was negatively correlated with Cr (P< 0.01; r= -1.000) of stream sediments, while it was negatively correlated with organic carbon (P< 0.05; r= -0.740) and positively correlated with K (P< 0.05; r= 0.750) of dam sediments. Occurrence and survival of aquatic hyphomycetes in hyporheic habitats of freshwater bodies indicate the importance of such zones as reservoir of fungal inoculum necessary in fundamental functions such as organic matter processing and energy flow. The present study provides baseline data on the sediment quality and fungal composition of stream and dam locations of River Kali of Kaiga region, which will develop as center of industrial activities in future.
机译:泄水带是淡水生态系统中有机物和能量流的主要储藏场所。为了补充在北美和欧洲进行的研究,我们评估了三个地方的粗颗粒有机物(CPOM;≥5.mm)和细颗粒物(FPM;≤1.mm)中沉积物的质量和水生疏水菌的发生。西加特山脉的卡加河和卡里河卡德拉大坝的八个位置。河流和大坝沉积物的pH值为酸性(5.8-6.6),河流沉积物的平均有机碳高于大坝沉积物(8.6%比3.9%)。在监测的八种矿物中,所有沉积物中的Fe含量最高,而四个大坝沉积物中的Ni含量均低于可检测的极限。气泡室温育后,从沉积物的CPOM馏分中直接释放出水生真菌的孢子,而FPM馏分通过无菌叶诱饵定植,然后气泡室温育间接产生孢子。 CPOM中河流和大坝沉积物中的物种丰富度和多样性高于FPM。溪流中的CPOM真菌菌群(66.7-81.8%)和水坝(69.2-88%)位置之间的Sorensen相似性指数通常高于FPM。每mg CPOM的孢子产量在1215(坝)和3384(流)之间。物种丰富度与河流沉积物的Cr呈负相关(P <0.01; r ​​= -1.000),而与有机碳呈负相关(P <0.05; r = -0.740),与K呈正相关(P <0.05; P = 0.05)。 r = 0.750)大坝沉积物。淡水体流产性生境中水生疏水菌的发生和存活表明,这类区域的重要性,如在有机物加工和能量流等基本功能中所必需的真菌接种物库。本研究提供了关于凯加河地区卡里河的沉积物质量和河流和水坝位置的真菌组成的基线数据,这些数据将在未来作为工业活动的中心发展。

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