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Transition of the Bacterial Community and Culturable Chitinolytic Bacteria in Chitin-treated Upland Soil: From Streptomyces to Methionine-auxotrophic Lysobacter and Other Genera

机译:甲壳素治疗的高地土壤中细菌群落和培养型胰酸钠细菌的过渡:从链霉菌对甲硫氨酸 - 营养营养粘膜和其他属的影响

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摘要

Chitin amendment is an agricultural management strategy for controlling soil-borne plant disease. We previously reported an exponential decrease in chitin added to incubated upland soil. We herein investigated the transition of the bacterial community structure in chitin-degrading soil samples over time and the characteristics of chitinolytic bacteria in order to elucidate changes in the chitinolytic bacterial community structure during chitin degradation. The addition of chitin to soil immediately increased the population of bacteria in the genus Streptomyces, which is the main decomposer of chitin in soil environments. Lysobacter, Pseudoxanthomonas, Cellulosimicrobium, Streptosporangium, and Nonomuraea populations increased over time with decreases in that of Streptomyces. We isolated 104 strains of chitinolytic bacteria, among which six strains were classified as Lysobacter, from chitin-treated soils. These results suggested the involvement of Lysobacter as well as Streptomyces as chitin decomposers in the degradation of chitin added to soil. Lysobacter isolates required yeast extract or casamino acid for significant growth on minimal agar medium supplemented with glucose. Further nutritional analyses demonstrated that the six chitinolytic Lysobacter isolates required methionine (Met) to grow, but not cysteine or homocysteine, indicating Met auxotrophy. Met auxotrophy was also observed in two of the five type strains of Lysobacter spp. tested, and these Met auxotrophs used d-Met as well as l-Met. The addition of Met to incubated upland soil increased the population of Lysobacter. Met may be a factor increasing the population of Lysobacter in chitin-treated upland soil.
机译:壳粉修正案是控制土壤植物疾病的农业管理战略。我们以前报道了甲壳素的指数下降,添加到培养的旱地土壤中。我们在本文中研究了细菌群落结构在几丁质降解土样中随着时间的推移和依甲酸钠细菌的特征在甲壳素降解过程中阐明了几丁质细菌群落结构的特征。甲壳素对土壤的添加立即增加了链霉菌属的细菌群体,这是土壤环境中甲壳素的主要分解。随着时间的推移,粘膜术,假瘤,纤维素粒子,链孢菌,链孢菌素和非牙科血管囊肿随着时间的推移而增加。我们孤立104株依赖甲壳素溶解细菌,其中六种菌株被归类为粘附杆菌,从甲壳素处理的土壤中被归类为粘膜。这些结果表明,粘附杆菌以及链霉菌的参与作为依甲酸丁蛋白的降解中的甲壳素分解。粘结术分离所需的酵母提取物或CasaminoAc氨基酸,用于含有葡萄糖的最小琼脂培养基上的显着生长。进一步的营养分析表明,六甲基氨基溶解粘膜分离物中所需的蛋氨酸(MET)生长,但不是半胱氨酸或同型胱内硬化,表明营养营养营养学。在五种类型的溶血杆菌菌株中也观察到患有侧卵体。经过测试,这些符合型营养丰富使用D-Met以及L-Met。添加满足以孵育的旱地土壤增加了粘附杆菌的群体。满足可能是增加甲壳素处理过的高地土壤中粘膜杆菌群的因素。

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