由于阿拉斯加原的永久土融化,可能存在细菌植物病原体的风险
Dockyu Kim1, Mincheol Kim1, Sungho Woo1
1Division of Life Sciences, Korea Polar Research Institute, Incheon 21990, Republic of Korea.
Ecotoxicology and environmental safety
|December 13, 2024
概括
全球变暖解永久土释放休眠的细菌. 研究人员发现,这些微生物,包括诸如 Pseudomonas 之类的植物病原体,可以重新激活并引起诸如土豆软腐等疾病.
科学领域:
- 微生物学 微生物学
- 环境科学 环境科学
- 植物病理学 植物病理学
背景情况:
- 全球变暖正在导致永久土融化,引发人们对古代微生物释放的担忧.
- 这些释放的微生物,特别是植物病原体的潜在风险尚未得到充分理解.
研究的目的:
- 为了研究模拟永久土解后阿拉斯加原土壤中的微生物变化.
- 评估休眠植物病原菌在永久土解后释放的活性和病原性.
主要方法:
- 在阿拉斯加的原土壤 (活性,过渡和永久结层) 上,在4°C下进行了90天的土壤化实验.
- 细菌的丰富性和社区组成使用殖民地形成单位和16S rRNA基因测序来分析.
- 测试了休眠植物病原体的活性和致病性,重点关注具有蛋白质分解活性的孤立菌株.
主要成果:
- 在解后的过渡层和永久结层中,细菌的丰度显著增加.
- 解引发了细菌社区结构的实质性转变,有利于Fe循环 taxa.
- 伪omonas spp. 这种类型的. 已证实这些单独物质会导致马软腐烂;一些病原体在解后才被检测出来.
结论:
- 永久土是休眠植物病原体的储存库.
- 永久土的解可能会导致这些病原体的复苏.
- 重生病原体对北极生态系统和农业构成潜在风险.
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