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在似是而非的早期地球大气条件下,原细胞和益生元化合物的同时形成。

Concomitant formation of protocells and prebiotic compounds under a plausible early Earth atmosphere.

作者信息

Jenewein Christian, Maíz-Sicilia Aurora, Rull Fernando, González-Souto Lorena, García-Ruiz Juan Manuel

机构信息

Laboratory of Crystallographic Studies, Instituto Andaluz de Ciencias de la Tierra, Consejo Superior de Investigaciones Científica, Armilla 18100, Spain.

Espectroscopía Raman e Infrarroja aplicado a Cosmogeoquímica y Astrobiología Research Group, Department of Applied Physics, Universidad de Valladolid, Boecillo 47151, Spain.

出版信息

Proc Natl Acad Sci U S A. 2025 Jan 14;122(2):e2413816122. doi: 10.1073/pnas.2413816122. Epub 2024 Dec 30.

Abstract

Revealing the origin of life and unambiguously detecting fossil remains of the earliest organisms are closely related aspects of the same scientific research. The synthesis of prebiotic molecular building blocks of life and the first compartmentalization into protocells have been considered two events apart in time, space, or both. We conducted lightning experiments in borosilicate reactors filled with a mixture of gases mimicking plausible geochemical conditions of early Earth. In addition to the variety of prebiotic organic molecules synthesized in these experiments, we investigated the micrometer-thick silica-induced organic film that covers the walls of the reactors and floats at the water-gas interface. We found that the film is formed by aggregation of HCN-polymer nanoclusters whenever water is present, either in the liquid or vapor phase. The organic film morphs into micrometer-scale biomorphic vesicular structures hanging from the organic film into the water. We also show that these structures are hollow and may act as microreactors facilitating chemical pathways toward increasing complexity. We propose that these organic biomorphs form through a bubble-driven mechanism and interfacial precipitation of HCN-polymers. The concomitant synthesis of biomorphic poly-HCN protocells and prebiotic molecules under plausible geochemical conditions of early Earth-like planets and moons and opens a different geochemical scenario for the emergence of life. Our results suggest that the coexistence of molecular building blocks of life and submicron biomorphic structures in the oldest rocks on Earth or any other celestial body does not necessarily mean evidence of life.

摘要

揭示生命起源并明确探测到最早生物体的化石遗迹,是同一科学研究中密切相关的两个方面。生命的益生元分子构建块的合成以及最初分隔为原始细胞,一直被认为是在时间、空间或两者上分开的两个事件。我们在硼硅酸盐反应器中进行了闪电实验,反应器中充满了模拟早期地球可能的地球化学条件的气体混合物。除了在这些实验中合成的各种益生元有机分子外,我们还研究了覆盖反应器壁并漂浮在水气界面的微米厚的二氧化硅诱导有机膜。我们发现,只要水以液相或气相存在,该膜就由HCN聚合物纳米团簇的聚集形成。有机膜会变成从有机膜垂入水中的微米级生物形态囊泡结构。我们还表明,这些结构是中空的,可能充当微反应器,促进化学途径向更高复杂性发展。我们提出,这些有机生物形态通过气泡驱动机制和HCN聚合物的界面沉淀形成。在类地行星和卫星早期可能的地球化学条件下,生物形态的聚HCN原始细胞和益生元分子同时合成,为生命的出现开辟了不同的地球化学场景。我们的结果表明,地球上或任何其他天体上最古老岩石中生命的分子构建块和亚微米生物形态结构的共存,不一定意味着有生命的证据。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/520f/11745316/6778c287fbd3/pnas.2413816122fig01.jpg

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