An Early-Branching Microbialite Cyanobacterium Forms Intracellular Carbonates

Author:

Couradeau Estelle123,Benzerara Karim1,Gérard Emmanuelle2,Moreira David3,Bernard Sylvain4,Brown Gordon E.56,López-García Purificación3

Affiliation:

1. Institut de Minéralogie et de Physique de la Matière Condensée, CNRS UMR 7590, Université Pierre et Marie Curie, 75005 Paris, France.

2. Institut de Physique du Globe de Paris (IPGP), CNRS UMR 7154, Université Paris Diderot, 75005 Paris, France.

3. Unité d’Ecologie, Systématique et Evolution, CNRS UMR 8079, Université Paris-Sud, 91405 Orsay Cedex, France.

4. Laboratoire de Minéralogie et de Cosmochimie du Museum (LMCM-MNHN), CNRS UMR 7202, 57 rue Cuvier, 75231 Paris Cedex 5, France.

5. Surface and Aqueous Geochemistry Group, Department of Geological and Environmental Sciences, Stanford University, Stanford, CA 94305, USA.

6. Department of Photon Science and Stanford Synchrotron Radiation Lightsource, SLAC National Accelerator Laboratory, 2575 Sand Hill Road, Menlo Park, CA 94025, USA.

Abstract

Keep It Inside Some cyanobacteria form solid-phase calcium carbonate precipitates as a consequence of fixing CO 2 during photosynthesis. Usually, such carbonates form extracellularly near the surface of the cells, sometimes generating structures called stromatolites. In a biofilm growing on carbonate deposits in Lake Alchichica, Mexico, Couradeau et al. (p. 459; see the Perspective by Riding ) discovered one species of cyanobacteria that also precipitates amorphous carbonate particles internally. Because the structure and chemical composition of these carbonates is distinct from those formed extracellularly, there may be cellular control over the mineralization process. These precipitates may influence physiological processes such as cell buoyancy and the sequestration of excess alkalinity generated during photosynthesis.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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