title: Interaction, at Ambient Temperature and 80 °C, between Minerals and Artificial Seawaters Resembling the Present Ocean Composition and that of 4.0 Billion Years Ago.
abstract: Probably one of the most important roles played by minerals in the origin of life on Earth was to pre-concentrate biomolecules from the prebiotic seas. There are other ways to pre concentrate biomolecules such as wetting/drying cycles and freezing/sublimation. However, adsorption is most important. If the pre-concentration did not occur-because of degradation of the minerals-other roles played by them such as protection against degradation, formation of polymers, or even as primitive cell walls would be seriously compromised. We studied the interaction of two artificial seawaters with kaolinite, bentonite, montmorillonite, goethite, ferrihydrite and quartz. One seawater has a major cation and anion composition similar to that of the oceans of the Earth 4.0 billion years ago (ASW 4.0 Ga). In the other, the major cations and anions are an average of the compositions of the seawaters of today (ASWT). When ASWT, which is rich in Na+and Cl-, interacted with bentonite and montmorrilonite structural collapse occurred on the 001 plane. However, ASW 4.0 Ga, which is rich in Mg2+and SO42-, did not induce this behavior. When ASW 4.0 Ga was reacted with the minerals for 24 h at room temperature and 80 °C, the release of Si and Al to the fluid was below 1 % of the amount in the minerals-meaning that dissolution of the minerals did not occur. In general, minerals adsorbed Mg2+and K+from the ASW 4.0 Ga and these cations could be used for the formation of polymers. Also, when the minerals were mixed with ASW 4.0 Ga at 80 °C and ASWT at room temperature or 80 °C it caused the precipitation of CaSO4∙2H2O and halite, respectively. Finally, further experiments (adsorption, formation of polymers, protection of molecules against degradation, primitive cell wall formation) performed under the conditions described in this paper will probably be more representative of what happened on the prebiotic Earth.
authors: Laboratório de Química Prebiótica, Departamento de Química-CCE, Universidade Estadual de Londrina, Londrina, PR, 86051-990, Brazil.
authors: Cristine E A
authors: CEA
authors: Carneiro
authors: Laboratório de Química Prebiótica, Departamento de Química-CCE, Universidade Estadual de Londrina, Londrina, PR, 86051-990, Brazil.
authors: Antonio C
authors: AC
authors: Stabile
authors: Departamento de Agronomia-CCA, Universidade Estadual de Maringa, Maringá, PR, 87020-900, Brazil.
authors: Frederico P
authors: FP
authors: Gomes
authors: Departamento de Agronomia-CCA, Universidade Estadual de Maringa, Maringá, PR, 87020-900, Brazil.
authors: Antonio C S
authors: ACS
authors: da Costa
authors: Departamento de Ciências Fisiológicas-CCB, Universidade Estadual de Londrina, Londrina, PR, 86051-990, Brazil.
authors: Cássia T B V
authors: CTBV
authors: Zaia
authors: Laboratório de Química Prebiótica, Departamento de Química-CCE, Universidade Estadual de Londrina, Londrina, PR, 86051-990, Brazil. damzaia@uel.br.
authors: Dimas A M
authors: DAM
authors: Zaia
mesh_terms: D000327:Adsorption; D018534:Earth, Planet; D019419:Evolution, Planetary; D008903:Minerals / Q000737:chemistry*; D012623:Seawater / Q000737:chemistry*; D013696:Temperature
chemical_list: D008903:Minerals
keywords: Clay minerals; Iron oxide-hydroxides; Origin of life; Seawater