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Non-Enzymatic, Template-Free Polymerization of 3',5' Cyclic Guanosine Monophosphate on Mineral Surfaces

  1. 1.
    SYSNO ASEP0554850
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleNon-Enzymatic, Template-Free Polymerization of 3',5' Cyclic Guanosine Monophosphate on Mineral Surfaces
    Author(s) Šponer, Judit E. (BFU-R) RID, ORCID
    Šponer, Jiří (BFU-R) RID, ORCID
    Výravský, J. (CZ)
    Šedo, O. (CZ)
    Zdráhal, Z. (CZ)
    Costanzo, G. (IT)
    Di Mauro, E. (IT)
    Wunnava, S. (DE)
    Braun, D. (DE)
    Matyášek, Roman (BFU-R) ORCID
    Kovařík, Aleš (BFU-R) RID, ORCID
    Number of authors11
    Source TitleCHEMSYSTEMSCHEM. - : Wiley
    Roč. 3, č. 6 (2021)
    Number of pages10 s.
    Publication formOnline - E
    Languageeng - English
    CountryUS - United States
    Keywordslong prebiotic oligomers ; origin ; oligonucleotides ; crystal ; life
    Subject RIVCE - Biochemistry
    OECD categoryBiochemistry and molecular biology
    R&D ProjectsGA19-03442S GA ČR - Czech Science Foundation (CSF)
    Method of publishingLimited access
    Institutional supportBFU-R - RVO:68081707
    UT WOS000671941700001
    DOI10.1002/syst.202100017
    AnnotationPrevious studies on the polymerization of 3',5' cyclic guanosine monophosphate (cGMP) demonstrated the potential of the compound in the abiotic generation of the first oligonucleotide sequences on the early Earth. These experiments were conducted under idealized laboratory conditions, which logically raises the question whether the same chemistry could take place in the harsh environment present on our planet in its earliest days. In the current study, we focus on the mineralogical context of this chemistry and show that numerous, but not all, common minerals assumed to be present on the early Earth could host the polymerization of H-form 3',5' cGMP. In particular, we have found that quartz varieties are especially suitable for this purpose, similar to andalusite, amphibole or micas. On the contrary, olivine, calcite, and serpentine-group minerals interfere with the studied polymerization chemistry. Our results show that crystallization on mineral surfaces, which is mainly a diffusion controlled process, determines the ability of 3',5' cGMP to polymerize. The observation that numerous amorphous and crystalline SiO2 forms are compatible with the oligomerization chemistry suggests that the process could commonly occur in a wide range of primordial environments allowing for crystallization of the cyclic monomers from a dropping solution.
    WorkplaceInstitute of Biophysics
    ContactJana Poláková, polakova@ibp.cz, Tel.: 541 517 244
    Year of Publishing2022
    Electronic addresshttps://chemistry-europe.onlinelibrary.wiley.com/doi/10.1002/syst.202100017
Number of the records: 1  

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