Cited by 89Origins and Evolution of LifeGeochemistry and Elemental AnalysisGeological and Geochemical Analysis

Alkaline fluid circulation in ultramafic rocks and formation of nucleotide constituents: a hypothesis

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Holm, Nils G, Dumont, Marion, Ivarsson, Magnus, Konn, Cécile·2006·Geochemical Transactions

Abstract

Seawater is constantly circulating through oceanic basement as a low-temperature hydrothermal fluid (<150 degrees C). In cases when ultramafic rocks are exposed to the fluids, for instance during the initial phase of subduction, ferromagnesian minerals are altered in contact with the water, leading to high pH and formation of secondary magnesium hydroxide, among other--brucite, that may scavenge borate and phosphate from seawater. The high pH may promote abiotic formation of pentoses, particularly ribose. Pentoses are stabilized by borate, since cyclic pentoses form a less reactive complex with borate. Analyses have shown that borate occupies the 2' and 3' positions of ribose, thus leaving the 5' position available for reactions like phosphorylation. The purine coding elements (adenine, in particular) of RNA may be formed in the same general hydrothermal environments of the seafloor.

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  • Phosphate was possibly concentrated at hydrothermal vents via brucite-driven precipitation processes.

    “Phosphate was possibly concentrated at hydrothermal vents, however, via the mineral brucite—Mg(OH)2—driven precipitation processes that Holm et al. [68] suggest to have involved sepentinization.”

    From Early bioenergetic evolution (2013) · cites this paper as [68]

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References 64 · Cited by 89

Research works printed but not linked: 2

  1. Berndt ME Allen DE Seyfried WE Jr Reduction of CO2 during serpentinization of olivine at 300°C and 500 bar Geology 1996 24 351 354 10.1130/0091-7613(1996)024<0351:ROCDSO>2.3.CO;2 · DOI · Paper page
  2. D'Hondt SL Jørgensen BB Miller DJ Aiello IW Bekins B Blake R Cragg BA Cypionka H Dickens GR Ferdelman T Ford K Gettemy GL Guèrin G Hinrichs K-U Holm NG House C Inagaki F Meister P Mitterer RM Naehr T Niitsuma S Parkes RJ Schippers A Skilbeck CG Smith DC Spivack AJ Teske A Wiegel J Naranjo Padilla C Solis Acosta JS Controls on Microbial Communities in Deeply Buried Sediments, Eastern Equatorial Pacific and Peru Margin Proceedings of the Ocean Drilling Program, Initial Reports 201 2003 College Station: Ocean Drilling Program

Authors
Holm, N. G., Dumont, M., Ivarsson, M., & Konn, C.
Affiliations
Stockholm University (SE)
Corresponding author
Holm, Nils G
Venue
Geochemical Transactions
Published
2006-07-25
Volume
7
Issue
1
Pages
7-7
ISSN
1467-4866 (ISSN-L)
OpenAlex
W2159082941
Cited by
89
References
64
Citations by year
2025: 3 · 2023: 3 · 2022: 1 · 2021: 8 · 2020: 6 · 2019: 3 · 2018: 4 · 2017: 3 · 2016: 2 · 2015: 7 · 2014: 6 · 2013: 11 · 2012: 4
FWCI
3.26
Type
journal article
Language
en
Open access
Licence
cc-by
Locations
  • Geochemical Transactions (publishedVersion, cc-by)
  • PubMed (publishedVersion)
  • DOAJ (DOAJ: Directory of Open Access Journals) (submittedVersion)
Funders
Vetenskapsrådet
Topics
  • Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Origins and Evolution of Life
  • Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
  • Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
Keywords
alkaline hydrothermal fluids, ultramafic rocks, ribose, borate, brucite, magnesium hydroxide, phosphate scavenging, purine nucleobases, adenine, subduction, oceanic basement

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