Rm. Hazen et al., Selective adsorption of L- and D-amino acids on calcite: Implications for biochemical homochirality, P NAS US, 98(10), 2001, pp. 5487-5490
Citations number
28
Categorie Soggetti
Multidisciplinary
Journal title
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA
The emergence of biochemical homochirality was a key step in the origin of
life, yet prebiotic mechanisms for chiral separation are not well constrain
ed. Here we demonstrate a geochemically plausible scenario for chiral separ
ation of amino acids by adsorption on mineral surfaces. Crystals of the com
mon rock-forming mineral calcite (CaCO3), when immersed in a racemic aspart
ic acid solution, display significant adsorption and chiral selectivity of
D- and L-enantiomers on pairs of mirror-related crystal-growth surfaces. Th
is selective adsorption is greater on crystals with terraced surface textur
es, which indicates that D- and L-aspartic acid concentrate along step-like
linear growth features. Thus, selective adsorption of linear arrays of D-
and L-amino acids on calcite, with subsequent condensation polymerization,
represents a plausible geochemical mechanism for the production of homochir
al polypeptides on the prebiotic Earth.