[meteorite-list] Nanobacteria-Like Calcite Single Crystals At The Surface of Tataouine Meteorite
From: Ron Baalke <baalke_at_meteoritecentral.com>
Date: Thu Apr 22 10:22:34 2004 Message-ID: <200306051641.JAA01520_at_zagami.jpl.nasa.gov> http://www.pnas.org/cgi/content/abstract/0832464100v1 Proc. Natl. Acad. Sci. USA, 10.1073/pnas.0832464100 Geology Nanobacteria-like calcite single crystals at the surface of the Tataouine meteorite Karim Benzerara *, Nicolas Menguy *, François Guyot *, Christian Dominici , and Philippe Gillet *Laboratoire de Minéralogie-Cristallographie, Unité Mixte de Recherche 7590 Centre National de la Recherche Scientifique and Institut de Physique du Globe de Paris, 4 Place Jussieu, 75252 Paris Cedex, France; Laboratoire CP2M Faculté des Sciences et Techniques de Saint Jerôme, Université d'Aix-Marseille, III, F-13397 Marseille Cedex 20, France; and Laboratoire des Sciences de la Terre, Ecole Normale Supérieure Lyon, 46 Allée d'Italie, 69007 Lyon Cedex, France Communicated by Russell J. Hemley, Carnegie Institution, Washington, DC, April 24, 2003 (received for review March 8, 2003) Nanobacteria-like objects evidenced at the surface of the orthopyroxenes of the Tataouine meteorite in South Tunisia have been studied by scanning and transmission electron microscopies. A method of micromanipulation has been developed to ensure that exactly the same objects were studied by both methods. We have shown that the nanobacteria-like objects are spatially correlated with filaments of microorganisms that colonized the surface of the meteoritic pyroxene during its 70 years of residence in the aridic Tataouine soil. Depressions of a few micrometers in depth are observed in the pyroxene below the carbonates, indicating preferential dissolution of the pyroxene and calcite precipitation at these locations. The nanobacteria-like small rods that constitute calcium carbonate rosettes are well crystallized calcite single crystals surrounded by a thin amorphous layer of carbonate composition that smoothes the crystal edges and induces rounded shapes. Those morphologies are unusual for calcite single crystals observed in natural samples. A survey of recent literature suggests that the intervention of organic compounds derived from biological activity is likely in their formation. To whom correspondence should be addressed. E-mail: benzerar_at_lmcp.jussieu.fr. Received on Thu 05 Jun 2003 12:41:18 PM PDT |
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