脂质生物标志物记录了Frasnian-Famennian大规模灭绝事件的海洋微生物社区结构变化
Jian Chen1, Nicholas Hogancamp2, Man Lu1
1Molecular Eco-Geochemistry (MEG) Laboratory, Department of Geological Sciences, The University of Alabama, Tuscaloosa, Alabama, USA.
Geobiology
|July 17, 2023
概括
海洋微生物群落通过增加藻类的生产力而适应了德纪晚期的弗拉斯尼亚-法门尼亚灭绝,这是由土著流入所驱动的. 这表明一个有弹性的生态系统,变化很大程度上局限于灭绝时期.
科学领域:
- 古生物学的古生物学
- 海洋生物学 海洋生物学
- 地质化学 地质化学
背景情况:
- 海洋微生物群落在生态系统功能和弹性方面发挥着至关重要的作用.
- 大规模灭绝事件为进化适应和生态系统恢复提供了洞察力.
- 弗拉斯尼亚-法门尼亚 (F-F) 过渡代表了一个重要的海洋灭绝事件.
研究的目的:
- 为了重建海洋微生物社区结构的变化,在晚代纪F-F过渡期间.
- 调查环境干扰对海洋生态系统的影响.
- 了解大规模灭绝期间海洋生物的适应性和弹性.
主要方法:
- 对来自上代纪新奥尔巴尼页岩的钻井芯的多代理调查.
- 对生物标志物的分析,如阿里尔异oprenoids,hopanes和steranes.
- 土地原生流入和微生物社区动态的重建.
主要成果:
- 在F-F间隔期间,绿色硫细菌和光区域 euxinia (PZE) 的扩张.
- 增加的土壤内流量,以酸盐比率和酸盐/酸盐比率表示.
- 在灭绝过程中,真核微藻生产的主导地位,主要是绿藻,并增加了甲性细菌.
结论:
- 伊利诺伊盆地在F-F灭绝期间经历了藻类生产率和化增加,类似于现代沿海海洋.
- 微生物社区的转移在很大程度上局限于灭绝间隔.
- 晚代纪的海洋微生物生态系统表现出相对稳定性和弹性.
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