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Cited by 19Origins and Evolution of LifeClay minerals and soil interactionsAnalytical Chemistry and Chromatography

Chiral interactions of histidine in a hydrated vermiculite clay

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Fraser, Donald G., Greenwell, H. Christopher, Skipper, Neal T., Smalley, Martin V., Wilkinson, Michael A., Demé, Bruno, Heenan, R. K.·2011·Phys. Chem. Chem. Phys.
DOI 10.1039/c0cp01387k
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Abstract

Recent work shows a correlation between chiral asymmetry in non-terrestrial amino acids extracted from the Murchison meteorite and the presence of hydrous mineral phases in the meteorite [D. P. Glavin and J. P. Dworkin, Proc. Natl. Acad. Sci. U. S. A., 2009, 106, 5487-5492]. This highlights the need for sensitive experimental tests of the interactions of amino acids with clay minerals together with high level computational work. We present here the results of in situ neutron scattering experiments designed to follow amino acid adsorption on an exchanged, 1-dimensionally ordered n-propyl ammonium vermiculite clay. The vermiculite gel has a (001) d-spacing of order 5 nm at the temperature and concentration of the experiments and the d-spacing responds sensitively to changes in concentration, temperature and electronic environment. The data show that isothermal addition of D-histidine or L-histidine solutions of the same concentration leads to an anti-osmotic swelling, and shifts in the d-spacing that are different for each enantiomer. This chiral specificity, measured in situ, in real time in the neutron beam, is of interest for the question of whether clays could have played an important role in the origin of biohomochirality.

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  • Supposedly enantiospecific adsorptions with allophane, hydrotalcite-like compound, montmorillonite, and vermiculite likely belong to this category.

    “Supposedly enantiospecific adsorptions of amino acids with allophane, 274 hydrotalcite-like compound, 275 montmorillonite, 276 and vermiculite 277,278 also likely belong to this category.”

    From Possible chemical and physical scenarios towards biological homochirality (2022) · cites this paper as [278]

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Authors
Fraser, D. G., Greenwell, H. C., Skipper, N. T., Smalley, M. V., Wilkinson, M. A., Demé, B., & Heenan, R. K.
Affiliations
  • University of Oxford (GB)
  • University College London (GB)
  • University of York (GB)
  • Institut Laue-Langevin (FR)
  • Rutherford Appleton Laboratory (GB)
Corresponding author
Fraser, Donald G.
ORCID
Venue
Phys. Chem. Chem. Phys.
Publisher
Royal Society of Chemistry (RSC)
Published
2011
Volume
13
Issue
3
Pages
825-830
ISSN
  • 1463-9076 (ISSN-L)
  • 1463-9084
DOI
10.1039/c0cp01387k
OpenAlex
W2953011479
Cited by
19
References
0
Citations by year
2022: 4 · 2020: 3 · 2018: 2 · 2017: 1 · 2016: 1 · 2015: 2 · 2014: 2 · 2012: 4
FWCI
0.71
Type
journal article
Language
en
Open access
Locations
  • Physical Chemistry Chemical Physics (publishedVersion)
  • PubMed (publishedVersion)
  • arXiv (Cornell University) (submittedVersion)
  • Durham Research Online (Durham University) (submittedVersion)
  • Science and Technology Facilities Council (submittedVersion)
  • Durham Research Online (Durham University) (submittedVersion, cc-by)
  • arXiv (Cornell University)
Topics
  • Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Origins and Evolution of Life
  • Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Clay minerals and soil interactions
  • Physical Sciences › Chemistry › Analytical Chemistry › Analytical Chemistry and Chromatography
Keywords
histidine, vermiculite, chiral interactions, amino acid adsorption, chiral recognition, osmotic swelling, clay mineral hydration, Murchison meteorite, in situ neutron scattering, clay-water interaction
MeSH terms
Adsorption, Aluminum Silicates, Crystallization, Histidine, Stereoisomerism, Water, Neutron Diffraction

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