铁雪的生物能量为欧洲的生命提供燃料
Nita Sahai1,2,3,4, Doug LaRowe5, John M Senko2,3,4
1School of Polymer Science and Polymer Engineering, The University of Akron, Akron, OH 44325.
概括
像欧罗巴这样的冰冷海洋世界上的生命可能是由"铁雪"维持的. 这个过程中和有害的氧化剂中和,为微生物提供食物,增加检测地球之外的生命的机会.
科学领域:
- 天体生物学和天体地质化学
- 行星科学和海洋世界研究研究
背景情况:
- 像欧罗巴这样的冰冷海洋世界可能存在生命,由光解氧化剂和海底减少剂的氧化还原梯度支持.
- 关键的挑战包括未知的海洋混合和反应性氧物种 (ROS) 对生物分子的破坏.
研究的目的:
- 提出一种新的机制,以维持生命在酸性冰冷的海洋世界,使用酸性矿井排水 (AMD) 坑湖作为一个模拟.
- 研究铁的生态化学循环及其在支持欧洲条件下的微生物生命中的作用.
主要方法:
- 模拟了一个系统,其中表面产生的ROS氧化Fe (II) 到Fe (III) (水氧化物沉,形成"铁雪".
- 在各种pH,温度和H2流量条件下对无氧代谢进行计算的吉布斯能量和最大生物质生产率.
主要成果:
- 铁雪在冰水界面中中和ROS,并为无氧微生物 ("呼吸铁") 提供呼吸基质.
- 降铁剂在大多数条件下表现出更高的生产力;硫酸盐降解剂和甲氧化物在高pH下更受欢迎.
- 铁在代谢氧化还原过程中的作用至关重要,并且在欧洲的生物地球化学模型中经常被忽视.
结论:
- 这种铁雪模型克服了冰冷海洋世界生命的主要障碍,提高了可居住性和潜在的生物标志检测.
- 该模型扩大了对代谢多样性的理解,增加了总初级生产率和可居住的环境.
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