English   español  
Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/91881
logo share SHARE logo core CORE   Add this article to your Mendeley library MendeleyBASE

Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL
Exportar a otros formatos:


Microbial and inorganic control on the composition of clay from volcanic glass alteration experiments

AuthorsCuadros, Javier; Afsin, B.; Jadubansa, P.; Ardakani, M.; Ascaso, Carmen ; Wierzchos, Jacek
KeywordsMicrobial control on clay generation
Mechanism of clay formation
Glass alteration
Issue Date2013
PublisherMineralogical Society of America
CitationAmerican Mineralogist 98: 319- 334 (2013)
AbstractBiological activity plays a substantial role in the geochemistry of the Earth’s surface. Particularly interesting are effects on clay formation because clays are abundant and have high surface-to-volume ratio, resulting in clays making up a large fraction of the overall mineral-fluid interface and having an effective control of mineral reactions. Thus, biological control on clay composition would affect element budget globally and the mineralogy of subsequent diagenetic processes. Biological acceleration of clay production would result in enhanced clay control of mineral reactions and faster organic C sequestration, by adsorption on clay minerals, with implications for the C and related cycles. We investigated the combined effect of microbial activity and water chemistry on the composition of neoformed clay by reacting volcanic glass with natural waters covering a large composition range (fresh water from a lake and a spring, seawater, and hypersaline water). The microbes (bacteria, fungi, and algae) were totally or partially identified using molecular and microscopy techniques. The solid alteration products were analyzed using cryo-SEM to investigate the mineral-microbe interface and TEM-AEM to study the composition of the neoformed clay. The solution chemistry was also investigated. We found that clay composition was controlled mainly by glass chemistry, rather than biological activity, through a mechanism of in situ transformation. The resulting clay was Al-rich (dioctahedral composition). In one case (inorganic experiment, freshwater lake), the specific inorganic conditions of pH and Mg and Si concentration promoted formation of Mg-rich (trioctahedral clay). Microbes, however, did influence clay composition by confining glass grains in biofilms where water chemistry is significantly different from the bulk solution. Alteration in such conditions generated significant amounts of trioctahedral, Mg-rich clay in the hypersaline water experiment, whereas it favored production of dioctahedral, Al-rich clay in the freshwater lake experiment. It is thus demonstrated that biofilms can exert an effective control on clay mineralogy
Publisher version (URL)http://dx.doi.org/10.2138/am.2013.4272
Identifiersdoi: 10.2138/am.2013.4272
issn: 0003-004X
Appears in Collections:(MNCN) Artículos
Files in This Item:
File Description SizeFormat 
accesoRestringido.pdf15,38 kBAdobe PDFThumbnail
Show full item record
Review this work

Related articles:

WARNING: Items in Digital.CSIC are protected by copyright, with all rights reserved, unless otherwise indicated.