沿海细菌和原生体同化病毒碳和
Joaquín Martínez Martínez1,2, David Talmy3, Jeffrey A Kimbrel4
1Bigelow Laboratory for Ocean Sciences, 60 Bigelow Drive, East Boothbay, ME, 04544, United States.
The ISME journal
|November 13, 2024
概括
病毒吞食,即微生物消耗病毒,显著增加了病毒的碳和循环. 这种微生物消耗对于理解水生生态系统中的营养循环至关重要.
科学领域:
- 微生物生态学 微生物生态学
- 生物地质化学生物地质化学
- 水生微生物学 水生微生物学
背景情况:
- 自由病毒是丰富的,但它们的消费 (virovory) 是很差量化.
- 这种知识差距限制了资源理论在生物地化学模型中的整合.
研究的目的:
- 量化病毒碳 (C) 和 (N) 流入原体和细菌的数量.
- 为了比较由于非生物与生物因素引起的病毒损失.
主要方法:
- 用同位素标记的病毒在微观实验中与自然微生物群落进行微观实验.
- 采用单细胞分辨率同位素测量和流细胞计.
- 量化病毒C和N流量和病毒去除率.
主要成果:
- 原生体可以通过资源实验满足显著的C和N需求.
- 病毒C和N被纳入细菌生物质中.
- 与单独的非生物过程相比,细菌和原生体每日病毒去除率增加了33%~85%.
- 生物过程导致了83%91%的病毒去除,而非生物过程在一周内达到50%.
结论:
- 提供了病毒C和N转移回微生物循环的直接证据.
- 突出了源泉在水层C和N循环中的全球重要作用.
- 强调需要进一步研究以改进生物地球化学模型.
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