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Trivalent Phosphorus and Phosphines as Components of Biochemistry in Anoxic Environments

机译:三价磷和膦作为缺氧环境中生物化学的组成部分

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Phosphorus is an essential element for all life on Earth, yet trivalent phosphorus (e.g., in phosphines) appears to be almost completely absent from biology. Instead phosphorus is utilized by life almost exclusively as phosphate, apart from a small contingent of other pentavalent phosphorus compounds containing structurally similar chemical groups. In this work, we address four previously stated arguments as to why life does not explore trivalent phosphorus: (1) precedent (lack of confirmed instances of trivalent phosphorus in biochemicals suggests that life does not have the means to exploit this chemistry), (2) thermodynamic limitations (synthesizing trivalent phosphorus compounds is too energetically costly), (3) stability (phosphines are too reactive and readily oxidize in an oxygen (O-2)-rich atmosphere), and (4) toxicity (the trivalent phosphorus compounds are broadly toxic). We argue that the first two of these arguments are invalid, and the third and fourth arguments only apply to the O-2-rich environment of modern Earth. Specifically, both the reactivity and toxicity of phosphines are specific to aerobic life and strictly dependent on O-2-rich environment. We postulate that anaerobic life persisting in anoxic (O-2-free) environments may exploit trivalent phosphorus chemistry much more extensively. We review the production of trivalent phosphorus compounds by anaerobic organisms, including phosphine gas and an alkyl phosphine, phospholane. We suggest that the failure to find more such compounds in modern terrestrial life may be a result of the strong bias of the search for natural products toward aerobic organisms. We postulate that a more thorough identification of metabolites of the anaerobic biosphere could reveal many more trivalent phosphorus compounds. We conclude with a discussion of the implications of our work for the origin and early evolution of life, and suggest that trivalent phosphorus compounds could be valuable markers for both extraterrestrial life and the Shadow Biosphere on Earth.
机译:磷是地球上所有生命必不可少的元素,但是生物学上似乎几乎完全没有三价磷(例如膦中的磷)。取而代之的是,除了一小撮含有结构相似化学基团的其他五价磷化合物之外,磷几乎全部用作磷酸盐。在这项工作中,我们针对生命为什么不探索三价磷提出了前面提到的四个论点:(1)先例(生化试剂中三价磷的确证实例表明,生命没有办法利用这种化学方法),(2 )热力学限制(合成三价磷化合物在能源上太昂贵),(3)稳定性(膦太易反应且在富含氧气(O-2)的气氛中容易氧化)和(4)毒性(三价磷化合物是广泛有毒)。我们认为这些论点中的前两个是无效的,而第三和第四个论点仅适用于现代地球富含O-2的环境。具体而言,膦的反应性和毒性都取决于好氧寿命,并严格取决于富含O-2的环境。我们假设在缺氧(不含O-2-2)的环境中持续存在的厌氧生活可能会更广泛地利用三价磷化学。我们审查了厌氧生物体,包括磷化氢气体和烷基膦,磷烷的三价磷化合物的生产。我们建议未能在现代陆地生活中找到更多此类化合物可能是由于天然产物对有氧生物的强烈偏见造成的。我们推测,对厌氧生物圈代谢产物进行更彻底的鉴定可以发现更多的三价磷化合物。最后,我们讨论了我们的工作对生命起源和早期进化的影响,并提出三价磷化合物可能是地球外生命和地球阴影生物圈的宝贵标志。

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