在海洋地表沉积物中的现存生物量中,Archaea的显著贡献
Julius S Lipp1, Yuki Morono, Fumio Inagaki
1Organic Geochemistry Group, Department of Geosciences and MARUM Center for Marine Environmental Sciences, University of Bremen, PO Box 330 440, 28334 Bremen, Germany.
Nature
|July 22, 2008
概括
古代生物占据了深海地下生物圈的主导地位,至少占活微生物生物质的87%. 这一发现重新塑造了我们对这些广,尚未探索的海洋息地的全球碳储存的理解.
科学领域:
- 微生物学 微生物学
- 地质化学 地质化学
- 海洋学 海洋学 海洋学
背景情况:
- 深海地下有着庞大的微生物细胞生态系统,估计储存的细胞碳的范围很广.
- 以前使用培养独立技术的研究尚未澄清这种环境中古生物学和细菌的相对丰富性.
研究的目的:
- 为了确定深海地下沉积物中占主导地位的微生物领域 (古生物或细菌).
- 为了提供一个更准确的估计全球细胞碳储存在海洋地下生物圈.
主要方法:
- 分析完整的极膜脂质作为地下沉积物 (>1米深) 中活细胞的生物标志物.
- 修改的定量聚合酶连锁反应和槽斑杂交的应用.
- 脂质度与总有机碳的相关性.
主要成果:
- 在地下沉积物中,至少有87%的完整的极膜脂质可以归因于古生物膜,这表明古生物是生物质的主要组成部分.
- 发现脂质度与总有机碳成比例.
- 在全球海洋地下地表生物圈中,细胞碳的修订估计为90 Pg.
结论:
- 古代生物占深海地下生物质的很大一部分.
- 以前的方法可能低估了考古生物质.
- 海底是全球生物质预算的关键组成部分.
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