“…The work of Jonsson et al (2009Jonsson et al ( , 2010, who studied the adsorption of L-glutamate and L-aspartate on the surface of rutile (a-TiO 2 , pH PZC ¼ 5.4) in NaCl solutions using potentiometric titrations and batch adsorption experiments over a wide range of pH, ligandto-solid ratio, and ionic strength, illustrates the need for such integrated studies. Not only did they find that adsorption depends strongly on ionic strength and glutamate concentration, but the extended triple-layer surface complexation model of all the experimental results also indicated the existence of at least two surface glutamate complexes.…”
Crystalline surfaces of common rock-forming minerals are likely to have played several important roles in life's geochemical origins. Transition metal sulfides and oxides promote a variety of organic reactions, including nitrogen reduction, hydroformylation, amination, and Fischer-Tropsch-type synthesis. Fine-grained clay minerals and hydroxides facilitate lipid self-organization and condensation polymerization reactions, notably of RNA monomers. Surfaces of common rock-forming oxides, silicates, and carbonates select and concentrate specific amino acids, sugars, and other molecular species, while potentially enhancing their thermal stabilities. Chiral surfaces of these minerals also have been shown to separate left-and right-handed molecules. Thus, mineral surfaces may have contributed centrally to the linked prebiotic problems of containment and organization by promoting the transition from a dilute prebiotic "soup" to highly ordered local domains of key biomolecules.
“…The work of Jonsson et al (2009Jonsson et al ( , 2010, who studied the adsorption of L-glutamate and L-aspartate on the surface of rutile (a-TiO 2 , pH PZC ¼ 5.4) in NaCl solutions using potentiometric titrations and batch adsorption experiments over a wide range of pH, ligandto-solid ratio, and ionic strength, illustrates the need for such integrated studies. Not only did they find that adsorption depends strongly on ionic strength and glutamate concentration, but the extended triple-layer surface complexation model of all the experimental results also indicated the existence of at least two surface glutamate complexes.…”
Crystalline surfaces of common rock-forming minerals are likely to have played several important roles in life's geochemical origins. Transition metal sulfides and oxides promote a variety of organic reactions, including nitrogen reduction, hydroformylation, amination, and Fischer-Tropsch-type synthesis. Fine-grained clay minerals and hydroxides facilitate lipid self-organization and condensation polymerization reactions, notably of RNA monomers. Surfaces of common rock-forming oxides, silicates, and carbonates select and concentrate specific amino acids, sugars, and other molecular species, while potentially enhancing their thermal stabilities. Chiral surfaces of these minerals also have been shown to separate left-and right-handed molecules. Thus, mineral surfaces may have contributed centrally to the linked prebiotic problems of containment and organization by promoting the transition from a dilute prebiotic "soup" to highly ordered local domains of key biomolecules.
“…Chang (1988) surveyed the potential of mineral surfaces to adsorb dilute monomers, and concluded that it was unlikely that this was the case. However, there are also more recent experiments that suggest that some amino acids are adsorbed very strongly to some mineral surfaces, especially under appropriate conditions of pH and ionic strength Jonsson et al, 2009Jonsson et al, , 2010Hazen and Sverjensky, 2010). Understanding the possible contributions of mineral surfaces to peptide oligomerization is thus central to several models for the origin of life (Orgel, 1998;Zaia, 2004).…”
Section: Introductionmentioning
confidence: 99%
“…Glycine is also one of the most chemically stable a-amino acids (Abelson, 1959;Vallentyne, 1964;Hare and Mitterer, 1969;Andersson and Holm, 2000;Snider and Wolfenden, 2000;Li and Brill, 2003a,b) and therefore the conclusions reached may be true of many amino acids . However, it is also clear that some amino acids, for example those with multiple negative or positive charges, such as aspartic and glutamic acids and lysine may form innersphere complexes with oppositely charged mineral surface sites mediated via their ionizable side chains Jonsson et al, 2009Jonsson et al, , 2010, which may be bound considerably more strongly than those formed by simple zwitterions like glycine. There may thus be significant differences between peptides composed of more complex charged amino acids and oligoglycines.…”
“…More recently, a series of studies by Hazen and collaborators have addressed the issue of chemistry at geological interfaces, proposing that crystal surfaces of Hadean eon-relevant minerals provide an effective substrate upon which the concentration of prebiotic molecules could have been achieved [17][18][19][20][21][22][23][24] . These works have demonstrated the pivotal role played by mineralwater interfaces in both concentration and catalysis processes.…”
This review introduces its readers to a ‘stochastic approach’ to origins of life research, from the viewpoints of both prebiotic chemistry and geology. The idea of a “primordial soup” has been subject to extensive criticism from thermodynamic, biochemical and geochemical perspectives, yet recent advancements have made clearer the plausibility of this theory. Herein, we review the theoretical and experimental approaches which have previously been explored, among these modelling, laboratory‐confined and geologically motivated experimentation. Of these, we consider organo‐mineral interactions, uniting aspects of prebiotic chemistry and geology, to be an especially promising way forward. However, we aim here to advance current approaches by advocating a methodology involving chemical systems and their stochastic reactivity on heterogeneous geological surfaces. This models the origins of life as a continuity of chemical reactions in an analogue to the early Earth (Hadean) environment.
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