海洋火山玻璃的改变:微生物活动的纹理证据
1M. R. Fisk, College of Oceanic and Atmospheric Sciences, 104 Ocean Administration Building, Oregon State University, Corvallis, OR 97331-5503, USA. S. J. Giovannoni, Department of Microbiology, 220 Nash Hall, Oregon State University, Corvallis,
概括
深层生物圈,可能占地球生物质的50%,包括海洋地岩石中的广泛细菌. 这种广的息地,虽然很大,但含有不到地球总生物质的1%.
科学领域:
- 地质微生物学的生物.
- 海洋生物学 海洋生物学
- 地表下生物圈研究研究
背景情况:
- 地下生物圈占地球总生物质的很大一部分.
- 有证据表明,海洋地岩石中存在着庞大的微生物生态系统.
- 海洋地是地球最大的已知息地.
研究的目的:
- 为了研究海洋地内的细菌殖民.
- 评估海洋玄武岩中地下生物圈的范围和丰富性.
- 为了支持在海洋上层地中广泛传播微生物生命的假设.
主要方法:
- 来自大西洋,太平洋和印度洋的玄武岩样本的调查.
- 在采集的岩石样本中分析微生物的存在和丰度.
- 估计上层海洋地生态的体积.
主要成果:
- 细菌已经殖民了海洋上层地的很大一部分.
- 海洋地的体积估计为10~18立方米.
- 尽管息地规模很大,但细菌的数量很少,占地球生物质的不到1%.
结论:
- 海洋地是广泛传播的细菌生物圈的所在地.
- 海洋地中的地下生物圈是广泛的,但人口稀少.
- 这一发现突显了地球上最大的微生物息地的独特特征.
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