在深度高盐无氧盆地中, prokaryotic 生命的团
Paul W J J van der Wielen1, Henk Bolhuis, Sara Borin
1Laboratory of Microbial Ecology, University of Groningen, 9751 NN Haren, Netherlands. paul.van.der.wielen@kiwa.nl
概括
地中海高盐无氧盆地拥有多样化,活跃的微生物群落. 这些极端环境支持了诸如硫酸盐还原和甲基生成之类的关键生态化学过程,挑战了以前的假设.
科学领域:
- 海洋微生物学 海洋微生物学
- 地质化学 地质化学
- 极致生物学的极致生物.
背景情况:
- 地中海的深海高盐无氧盆地 (DHAB) 源自古老的米奥森盐沉积物.
- 这些独特的环境以前被认为可能没有显著的生物地化学活动.
研究的目的:
- 研究地中海DHABs中的生物地化学活动和微生物多样性.
- 描述发现盆地的微生物群落,一个极端的MgCl2-丰富的盐水环境.
主要方法:
- 微生物社区组成和结构的分析.
- 评估现场生物地球化学过程,包括硫酸盐还原和甲基生成.
- 在极端盐水条件下代谢活动概况.
主要成果:
- DHABs是活跃的生物地球化学系统,而不是"死胡同".
- 在现场检测到显著的硫酸盐减少,甲基生成和异质性活性.
- 鉴定出了一个多样化的 prokaryotic 社区,特色是新的,深度分支的 Euryarchaeota 顺序.
- 一个独特的,代谢活跃的微生物社区在发现盆地 (5 M MgCl2) 繁荣发展.
结论:
- 地中海DHAB有充满活力和多样化的微生物生态系统.
- 这些发现扩大了我们对生活在极端高盐环境中的适应能力的理解.
- 鉴定到的微生物群落在这些盆地的独特地质化学中起着至关重要的作用.
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