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An automated apparatus for he simulation of prebiotic wet-dry cycles under strictly anaerobic conditions

机译:在严格厌氧条件下对益生元湿干循环进行模拟的自动化装置

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Prebiotic chemical evolution on the early Earth may have been driven in part by fluctuating environments, for example wet-dry and temperature cycling in volcanic rock pools. Here, we describe the setup, operating principle and test applications of a newly developed 'wet-dry apparatus' (WDA) designed to simulate such fluctuating environments. The WDA allows adjusting the duration of the cycles, the temperature during the wet and dry phases and the organic and mineral components, which are all key parameters in wet-dry simulations. The WDA's most important features, however, are (i) that it is automated, which means that long-time experiments are possible without the need for an operator and (ii) that the virtual absence of free oxygen in the early Earth's atmosphere at ground level can be simulated. Rigorously oxygen-free conditions were achieved by passing 99.999% nitrogen gas through two alkaline pyrogallol solutions in series, prior to entering the WDA. We used three chemical systems to test the WDA: (i) the amino acid glycine in the presence and absence of clay minerals, (ii) linoleic acid (an oxygen-sensitive amphiphile) with and without the mineral olivine, and (iii) alkaline pyrogallol solution. We observed that clay minerals greatly accelerated the decomposition of glycine under wet-dry conditions. Glycine peptides were formed as minor products. In the course of the glycine experiments, we developed a reliable gas chromatographic method to quantify the cyclic dipeptide 2,5-diketopiperazine. The decomposition of linoleic acid in wet-dry cycles was promoted by both air and olivine. And finally, the extremely oxygen-sensitive pyrogallol solution was used as a colour indicator for residual oxygen in the WDA. The simulation facility in our laboratory currently consists of eight identical WDAs and a surrounding infrastructure. It can be made available to others who wish to perform cyclic wet-dry experiments.
机译:早期地球上的益生元化学进化可能已经通过波动环境部分地驱动,例如在火山岩池中的湿干燥和温度循环。在这里,我们描述了新开发的“湿干设备”(WDA)的设置,操作原理和测试应用,该设计用于模拟这种波动环境。 WDA允许调节循环的持续时间,湿和干阶段的温度和有机和矿物成分,这是湿干模拟中的所有关键参数。然而,WDA最重要的特征是(i)它是自动化的,这意味着长期实验是可能的,而无需操作员和(ii)即将在地球上的早期地球大气层中的虚拟缺乏自由氧气可以模拟水平。通过在进入WDA之前通过串联通过两种碱性吡糖醇溶液通过含有99.999%的氮气来实现严格的无氧条件。我们使用了三种化学系统来测试WDA:(i)在存在和不存在粘土矿物质中的氨基酸甘氨酸,(ii)亚油酸(氧敏感两种),具有和不含矿物橄榄石,(III)碱性Pyrogallol解决方案。我们观察到粘土矿物质大大加速了湿干燥条件下甘氨酸的分解。甘氨酸肽形成为次要产品。在甘氨酸实验过程中,我们开发了可靠的气相色谱法,用于量化环二肽2,5-二酮哌嗪。空气和橄榄石促进了湿干循环中亚油酸的分解。最后,使用极其氧敏感的吡糖醇溶液用作WDA中残留氧的颜色指示剂。我们实验室的仿真设施目前包括八个相同的WDA和周围基础设施。它可以向希望进行循环湿干实验的人提供。

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