人口生态学和生物地球化学影响ssDNA和dsDNA病毒沿着永久土融化梯度
Gareth Trubl1,2, Simon Roux3, Mikayla A Borton4
1Department of Microbiology, The Ohio State University, Columbus, OH, USA. trubl1@llnl.gov.
Nature communications
|December 11, 2025
概括
气候变化正在加速永久土的融化,释放出古老的碳. 病毒在处理这种碳中发挥着关键作用,随着永久土的解,它们的活动增加,影响全球碳循环.
科学领域:
- 环境微生物学环境微生物学
- 病毒学 病毒学
- 气候科学是气候科学.
背景情况:
- 由于气候变化导致的永久土融化释放出大量的碳储量.
- 病毒在永久土碳循环中的作用基本上是未知的.
- 土壤病毒在技术上很难检测和表征.
研究的目的:
- 调查病毒对解永久土中的碳循环的贡献.
- 在永久土环境中描述病毒种群及其功能基因.
- 评估永久土融化对病毒多样性和功能的影响.
主要方法:
- 在永久土融梯度中应用优化的维丰富工作流.
- 病毒种群的识别和表征 (病毒操作分类学单位 - vOTU).
- 病毒辅助代谢基因 (AMG) 的宿主预测和基因组分析.
主要成果:
- 发现了9,963个新的病毒种群 (vOTU),与其他土壤相比,其新性为99.9%.
- 预测38%的vOTU在各种细菌和古生物学类的宿主.
- 确定了811个涉及碳处理的假定AMG,包括与碳储存相关的糖化酸和基因.
结论:
- 病毒在永久土解过程中对碳处理做出了重大贡献.
- 随着永久土的解,病毒的功能多样性增加,影响微生物代谢.
- 病毒是决定气候变化下的土壤碳命运的关键参与者.
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