揭示冷生态系统发展阶段的动态病毒景观:对全球海洋生物地质化学的影响
Yuanyuan Wang1, Shanzi Huang1, Jian He1
1School of Marine Sciences, State Key Laboratory for Biocontrol/Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Guangdong Province Key Laboratory of Aquatic Economic Animals/Guangdong Provincial Observation and Research Station for Marine Ranching of the Lingdingyang Bay, Sun Yat-sen University, 135 Xingang Road West, Guangzhou 510275, PR China.
Journal of hazardous materials
|May 14, 2025
概括
这项研究揭示了冷漏的新型病毒多样性,显示了跨漏阶段不同的病毒社区和功能. 病毒在这些独特的生态系统中显著影响微生物生态和生物地化学循环.
科学领域:
- 海洋微生物生态学
- 生物地质化学生物地质化学
- 病毒学 病毒学
背景情况:
- 冷是重要的富含甲的生态系统,影响全球生物地质化学循环.
- 寒流中的病毒群体在很大程度上尚未被探索,这限制了对它们生态作用的理解.
研究的目的:
- 进行首次对冷透生态系统进行全面的病毒基因组分析.
- 描述病毒的多样性,社区结构和不同透发育阶段的功能角色.
- 研究病毒与宿主相互作用及其对生物地化学过程的影响.
主要方法:
- 病毒基因组测序的沉积物从chemoautotrophic,成熟,和海马冷的灭绝阶段.
- 生物信息分析用于识别病毒操作分类单元 (OTU) 和新谱系.
- 在透阶段对病毒社区结构,多样性和辅助代谢基因 (AMG) 档案进行比较分析.
主要成果:
- 发现了4272个病毒OTU,其中77%是新型血统,这表明在冷中病毒新性很高.
- 病毒社区结构和多样性在透阶段的显著变化,在化学自营性阶段达到顶峰.
- 鉴定特定阶段的病毒AMG丰富,包括碳水化合物,氨基酸和硫代谢基因在化学自营阶段,以及成熟阶段的能量代谢/异生菌降解.
- 作为关键宿主,Lytic病毒生活方式和Gammaproteobacteria的占主导地位,在透发展过程中具有动态相互作用.
结论:
- 寒流入的病毒群体拥有独特而多样化的病毒群体,具有重要的功能作用.
- 病毒群体及其代谢功能随着发展阶段的透而演变,影响微生物生态和生物地化学循环.
- 这项研究提供了对冷的病毒生态的基本理解,对海洋科学和生物技术有影响.
相关概念视频
What are Biogeochemical Cycles?
30.8K
The most common elements in organic molecules, carbon, hydrogen, oxygen, nitrogen, sulfur, and phosphorus, are only available in the ecosystem in limited amounts. Therefore, these nutrients must be recycled through both biotic and abiotic components of the ecosystem, in processes generally called biogeochemical cycles.
30.8K
Primary Production
23.5K
The total amount of energy acquired by primary producers in an ecosystem is called gross primary production (GPP). However, of this energy, producers use some for metabolic processes, and some is lost as heat, decreasing the amount of energy available to the next trophic level. The remaining usable amount of energy is called the net primary productivity (NPP). In terrestrial ecosystems, NPP is driven by climate, while light penetration and nutrient availability drive NPP in aquatic ecosystems.
23.5K
The Sulfur Cycle
43.4K
Sulfur, an important element in the chemical makeup of proteins, is recycled through the atmosphere and aquatic and terrestrial environments. Found in the atmosphere as sulfur dioxide (SO2), sulfur is released by decaying organisms, weathered rocks, geothermal vents, volcanos, and burning fossil fuels. It is deposited into the ecosystem, cycled through the biotic community, and either released back into the atmosphere as gas or deposited in marine sediment for long-term storage and eventual...
43.4K
What is an Ecosystem?
39.0K
Overview
39.0K
Global Climate Change
24.0K
Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
24.0K


