在解永久土中处理碳的基因组中心视图
Ben J Woodcroft1, Caitlin M Singleton1, Joel A Boyd1
1Australian Centre for Ecogenomics, School of Chemistry and Molecular Biosciences, University of Queensland, Brisbane, Queensland, Australia.
Nature
|July 18, 2018
概括
全球变暖正在融化永久土, 这项研究揭示了碳循环中的微生物, 对于预测这些敏感生态系统未来的温室气体排放至关重要.
科学领域:
- 微生物生态学
- 生物地质化学
- 气候变化科学
背景情况:
- 全球气温上升加快永久土的融化,释放大量储存的碳.
- 了解微生物群落对于预测永久土融化的碳排放至关重要.
研究的目的:
- 在融化永久土中使用元基因组学来描述微生物群落.
- 确定与碳降解和温室气体产生有关的关键微生物系.
主要方法:
- 在融化梯度上对214个永久土样本进行基因组测序.
- 1,529个基因组组合基因组 (MAG) 的组合.
- 用于将微生物种群与生物地化学过程联系起来.
主要成果:
- 从代表性不足的族群中恢复众多的基因组,增强基因组代表性.
- 鉴定真菌酸分解的细菌途径.
- 特定微生物系与温室气体产生的相关性和新型的合成关系.
结论:
- 这项研究将特定的微生物系与永久土解过程中的碳处理联系起来.
- 这些发现为预测气候变化对永久土碳循环的影响提供了关键数据.
- 这项研究提高了我们对北极地区温室气体排放中的微生物作用的理解.
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