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从巴基斯坦 Murree 下喜马拉雅的碎屑沉积岩中分离出的溶磷外生和内生细菌。

Phosphate solubilizing epilithic and endolithic bacteria isolated from clastic sedimentary rocks, Murree lower Himalaya, Pakistan.

机构信息

Department of Microbiology, Faculty of Biological Sciences, Quaid-I-Azam University, Islamabad, 45320, Pakistan.

Environmental Engineering, Guangdong Technion Israel Institute of Technology, Shantou, Guangdong, China.

出版信息

Arch Microbiol. 2022 May 18;204(6):332. doi: 10.1007/s00203-022-02946-2.

Abstract

Rock microbes are capable to solubilize phosphate present in the rocks.. In this study, we focused on the isolation of phosphate solubilizing bacteria from rocks of Murree, Pakistan. Both endolithic and epilithic bacteria were screened for phosphate solubilization. Three bacterial strains were selected based on halozone formation inNational Botanical Research Institute for phosphate) medium supplemented with TCP (tribasic calcium phosphate). The solubilization index for these bacteria was recorded as 4.29, 4.03 and 3.99. The pH of the medium dropped from 7.0 to 4.0 after 5 days with continuous shaking at 150 rpm, which facilitate the phosphate solubilization. The strains P26, P4 and N27 were identified as Pseudomonas putida strain (KT004381), Pseudomonas grimontii (KT223621) and Alcaligenes faecalis (KT004385). Strain P26 showed maximum phosphate solubilization (367.54 µg/ml), while P4 and N27 showed 321.88 and 291.36 µg/ml after 3 days of incubation. Such inorganic phosphate solubilization could be attributed to the organic acids production by bacteria. The presence of organic acids is determined by high-performance liquid chromatography. Three different types of acids, gluconic, oxalic and malic acid were the dominant acids found in the culture medium. It may be assumed that these bacteria can play a role in weathering of rocks as well. PSB is likely to serve as an efficient biofertilizer, especially in areas deficient in P to increase the overall performance of crops.

摘要

岩石微生物能够溶解岩石中的磷酸盐。在这项研究中,我们专注于从巴基斯坦穆雷的岩石中分离出具有磷酸盐溶解能力的细菌。我们筛选了内生菌和外生菌以检测其磷酸盐溶解能力。根据在添加 TCP(磷酸三钙)的 National Botanical Research Institute 磷酸盐培养基中形成的 halo 区,选择了 3 株细菌。这些细菌的溶磷指数记录为 4.29、4.03 和 3.99。在 150rpm 连续摇晃 5 天后,培养基的 pH 值从 7.0 降至 4.0,这有利于磷酸盐的溶解。菌株 P26、P4 和 N27 被鉴定为恶臭假单胞菌(KT004381)、居泉假单胞菌(KT223621)和粪产碱杆菌(KT004385)。菌株 P26 表现出最大的磷酸盐溶解能力(367.54µg/ml),而 P4 和 N27 在孵育 3 天后分别显示出 321.88µg/ml 和 291.36µg/ml。这种无机磷酸盐的溶解可能归因于细菌产生的有机酸。有机酸的存在通过高效液相色谱法确定。在培养基中发现了三种不同类型的酸,葡萄糖酸、草酸和苹果酸,它们是主要的酸。可以假设这些细菌也可以在岩石风化中发挥作用。PSB 很可能作为一种有效的生物肥料,特别是在缺乏 P 的地区,以提高作物的整体性能。

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