Please use this identifier to cite or link to this item: http://repositorio.unicamp.br/jspui/handle/REPOSIP/323901
Type: Artigo
Title: Adenine Interaction With And Adsorption On Fe-zsm-5 Zeolites: A Prebiotic Chemistry Study Using Different Techniques
Author: Anizelli P.R.
Baú J.P.T.
Valezi D.F.
Canton L.C.
Carneiro C.E.A.
Di Mauro E.
Da Costa A.C.S.
Galante D.
Braga A.H.
Rodrigues F.
Coronas J.
Casado-Coterillo C.
Zaia C.T.B.V.
Zaia D.A.M.
Abstract: Most adsorption experiments are performed under conditions that did not exist on Earth before the life arose on it. Because adsorption is the first step for all other processes (protection against degradation and polymerization), it is important that it is performed under conditions that existed on prebiotic Earth. In this paper, we use an artificial seawater (seawater 4.0 Ga), which contains major cations and anions that could present on the oceans of the prebiotic Earth. In addition, zeolites, with substituted Fe in the framework, and adenine were probably common substances on the prebiotic Earth. Thus, study the interaction between them is an important issue in prebiotic chemistry. There are two main findings described in this paper. Firstly, zeolites with different Si/Fe ratios adsorbed adenine differently. Secondly, XAFS showed that, after treatments with seawater 4.0 Ga and adenine, an increase in the complexity of the system occurred. In general, salts of seawater 4.0 Ga did not affect the adsorption of adenine onto zeolites and adenine adsorbed less onto zeolites with iron isomorphically substituted. The C=C and NH2 groups of adenine interacted with the zeolites. Gypsum, formed from aqueous species dissolved in seawater 4.0 Ga, precipitated onto zeolites. EPR spectra of zeolites showed lines caused by Fe framework and Fe3+ species. TG curves of zeolites showed events caused by loss of water weakly bound to zeolite (in the 30-140 °C range), water bounded to iron species or cations from seawater 4.0 Ga or located in the cavities of zeolites (157-268 °C) and degradation of adenine adsorbed onto zeolites (360-600 °C). Mass loss follows almost the same order as the amount of adenine adsorbed onto zeolites. The XAFS spectrum showed that Fe3+ could be substituted into the framework of the Fe7-ZSM-5 zeolite. © 2016 Elsevier Inc. All rights reserved.
Subject: Adsorption
Iron Zeolites
Nucleic Acid Base
Prebiotic Chemistry
Seawater
Editor: Elsevier
Rights: fechado
Identifier DOI: 10.1016/j.micromeso.2016.02.004
Address: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84959419775&doi=10.1016%2fj.micromeso.2016.02.004&partnerID=40&md5=a6f18d3e5ea8d7237ea1f3f0964b59dd
Date Issue: 2016
Appears in Collections:Unicamp - Artigos e Outros Documentos

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