在火星的盖尔火山口的30亿年前的泥石中保存的有机物质
Jennifer L Eigenbrode1, Roger E Summons2, Andrew Steele3
1Solar System Exploration Division, NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA. jennifer.l.eigenbrode@nasa.gov.
概括
科学家在35亿年前的火星泥石中发现了保存的有机物质, 这一发现表明硫化有助于有机保存, 提供了古代火星生命的线索.
科学领域:
- 天体生物学
- 星球科学
- 地质化学
背景情况:
- 在火星上寻找有机物和生物标志的研究仍在进行中.
- 之前关于火星有机物质的报道很有限.
- 了解有机保存是评估过去可居住性的关键.
研究的目的:
- 在古代火星沉积岩中检测和描述有机物质.
- 在火星上研究有机化合物的保存机制.
- 评估盖尔火山口可能存在的生物特征.
主要方法:
- 在Curiosity火星车上的样本分析 (SAM) 仪器套件使用现场分析.
- 进化气体分析 (EGA) 检测热解产物
- 气色谱-质谱 (GC-MS) 用于化合物识别.
主要成果:
- 检测各种有机化合物,包括在高温 (500820°C) 上释放的硫,芳香化合物和酸化合物.
- 在35亿年前的穆雷岩层底部的湖泥石中发现有机物质.
- 每克至少50纳米的有机碳含量,有机硫含量约为5%.
结论:
- 在古老的火星湖水环境中保存有机物质.
- 硫化似乎是火星上有机物保存的一个重要机制.
- 检测到的有机化合物为火星的早期碳循环和潜在可居住性提供了洞察力.
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