氨氧化古生物的分布和基因组变异在深层和浅层表面沉积物中
Blandine Trouche1,2, Clemens Schauberger3, Feriel Bouderka4
1Univ Brest, CNRS, Ifremer, UMR6197 Biologie et Ecologie des Ecosystèmes marins Profonds, F-29280, Plouzané, France. blandine.trouche@orange.fr.
ISME communications
|December 22, 2023
概括
深海氨氧化古生物 (AOA) 在沟中显示出基于环境梯度的利基分离. 它们的种群结构是由决定性和随机的过程形成的,这取决于所研究的基因组规模.
科学领域:
- 海洋微生物学 海洋微生物学
- 生物地质化学循环是什么
- 深海生态 深海生态
背景情况:
- 氨氧化古生物 (AOA) 对于海洋沉积物中循环至关重要.
- 对于AOA的利基区分和哈德和深地区的种群结构的理解有限.
研究的目的:
- 研究深海沉积物中AOA的利基区分和种群结构.
- 确定影响沟系统AOA分布和遗传变异性的因素.
主要方法:
- 从阿塔卡马和克拉马德克沟沉积物中重建47个AOA元基因组组装基因组 (MAGs).
- 在氧-氨梯度沿线对AOA分布的分析.
- 使用单核酸变体 (SNVs) 评估人口结构.
主要成果:
- 深海的AOA形成了具有特定分布模式的独特类型.
- 在物种层面上的分布表明了基于利基的生态型.
- 种内结构显示出浴度,沟隔离和沉积物深度的影响.
结论:
- 深海AOA种群表现出确定性利基分区和随机过程.
- 生态利基和选择性压力显著影响了AOA的遗传变异性.
- 浴度和沟地形是构建哈达尔AOA种群的关键因素.
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