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Function of meiobenthos and microorganisms in cellulose breakdown in sediments of wetlands with different origins in Hokkaido

机译:甲鱼和微生物在北海道不同来源的湿地沉积物中纤维素分解中的作用

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摘要

To validate the mechanism of cellulose breakdown in cold climate wetlands, we investigated cellulase activity in sediments collected from 17 wetland sites in Hokkaido, the northern area of Japan. We evaluated cellulase activity by quantitative analysis of glucose released from carboxymethyl cellulose and found that sediments from peat fens demonstrated high activity, followed by sediments from lagoons and estuaries. Sediments from peat fens also contained greater amounts of organic matter, followed by lagoons and estuaries, thereby suggesting a strong positive correlation between organic matter content and cellulase activity. Evaluation of cellulase activity by qualitative cellulose zymographic analysis showed that various cellulases with different molecular sizes were implicated in cellulose breakdown in wetlands. Among them, cellulose breakdown in Meguma Pond (peat fen), Notsuke Gulf (peat fen), and Lake Utonai (lagoon) was potentially due to microorganism cellulase, while that in Lake Chobushi (lagoon) was ascribed to meiobenthos (Oligochaeta species) cellulase. The findings presented herein suggest that the origin and activity level of cellulase vary depending on the type of cold climate wetland.
机译:为了验证寒冷气候湿地中纤维素分解的机理,我们调查了从日本北部北海道的17个湿地站点收集的沉积物中的纤维素酶活性。我们通过定量分析羧甲基纤维素释放的葡萄糖来评估纤维素酶活性,发现泥炭eat的沉积物表现出高活性,其次是泻湖和河口的沉积物。泥炭的沉积物中还含有更多的有机物,其次是泻湖和河口,因此表明有机物含量与纤维素酶活性之间存在很强的正相关性。通过定性纤维素酶谱分析对纤维素酶活性的评估表明,具有不同分子大小的各种纤维素酶与湿地中的纤维素分解有关。其中,Meguma Pond(豌豆粉),Notsuke Gulf(豌豆粉)和Utonai(泻湖)中的纤维素分解可能是由于微生物纤维素酶引起的,而Chobushi湖(泻湖)中的纤维素分解归因于中底苯(Oligochaeta物种)纤维素酶。 。本文提出的发现表明,纤维素酶的起源和活性水平根据寒冷气候湿地的类型而变化。

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