Content of Pigments in the Bottom Sediments in a Small Valley Channel Reservoir

IF 0.8 4区 生物学 Q4 MARINE & FRESHWATER BIOLOGY
L. E. Sigareva, N. A. Timofeeva, V. V. Zakonnov
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Abstract

This paper presents the first data on the content of plant pigments in the bottom sediments of the Uvod Reservoir (Volga basin, Russia), unique in its hydrological regime, which support the hypothesis of more intensive carbon accumulation in small water bodies. It is established that the average concentration of chlorophyll a and its transformation products at the stations is 62.6 ± 10.0 μg/g of dry sediment, 35.2 ± 4.5 mg/(m2 mm) of wet sediment, and 0.73 ± 0.09 mg/g of organic matter of sediments. The ratio of organic carbon to the pigment concentration varies within 400–6000, depending on the type of bottom sediments, which significantly exceeds the values known for macrophytes and phytoplankton. Despite the features of hydrodynamics and geomorphology of the reservoir, the spatial distribution of sedimentary pigments is consistent with the structure of the bottom sediment complex, which is typical for water bodies of different types. A decrease in differences between the pigment concentrations in the sandy and silty biotopes of the Uvod Reservoir compared to the Upper Volga is noted. The average concentration of chlorophyll a with pheopigments (58.5 ± 6.7 μg/g of dry sediment), calculated considering the areas of bottom sediments of different types, in the Uvod Reservoir is 2.3 times higher than in the Gorky Reservoir (25.3 ± 1.5 μg/g), from which water inflows through the Volga–Uvod Canal. According to the content of sedimentary pigments, the trophic state of the reservoir is mesotrophic. Features of eutrophication in the Uvod Reservoir are more distinctly expressed than in the Gorky Reservoir.

Abstract Image

小河谷水库底泥中的色素含量
摘要 本文首次提出了乌沃德水库(俄罗斯伏尔加河流域)底层沉积物中植物色素含量的数据,这些数据支持了小水体中碳积累更为密集的假说。研究表明,各站叶绿素 a 及其转化产物的平均浓度为干沉积物 62.6 ± 10.0 微克/克,湿沉积物 35.2 ± 4.5 毫克/(平方米毫米),沉积物有机物 0.73 ± 0.09 毫克/克。有机碳与色素浓度的比值在 400-6000 之间变化,具体取决于底层沉积物的类型,这大大超过了大型植物和浮游植物的已知值。尽管水库的水动力和地貌有其特点,但沉积色素的空间分布与底层沉积物复合体的结构是一致的,这在不同类型的水体中很典型。与上伏尔加河相比,乌沃德水库沙质和淤泥质生物群落的色素浓度差异有所缩小。根据不同类型底层沉积物的面积计算,乌沃德水库中叶绿素 a 的平均浓度(58.5 ± 6.7 微克/克干沉积物)比高尔基水库(25.3 ± 1.5 微克/克)高出 2.3 倍,而高尔基水库的水是通过伏尔加河-乌沃德运河流入的。根据沉积色素的含量,水库的营养状态属于中营养状态。乌沃德水库的富营养化特征比高尔基水库更为明显。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Inland Water Biology
Inland Water Biology 生物-海洋与淡水生物学
CiteScore
1.30
自引率
55.60%
发文量
87
审稿时长
6-12 weeks
期刊介绍: Inland Water Biology publishes thematic reviews and original papers devoted to flora and fauna in waterbodies, biodiversity of hydrobionts, biology, morphology, systematics, ecology, ethology, ecological physiology and biochemistry of aquatic organisms, patterns of biological cycle, structure and functioning of aquatic ecosystems, anthropogenic and uncontrolled natural impacts on aquatic organisms and ecosystems, invasion of nonindigenous species into ecosystems and their ecology, methods of hydrobiological and ichthyological studies.
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