Biomineralization process in magnetotactic bacteria and calcareous sponges

Event date and time: 22/05/2019 12:30 pm

Event location: Seminar Room – NIMP

This event was posted by Admin

GENERAL SEMINAR – Dr. Jacques Werckmann, State University of Rio de Janeiro, Brazil.

Over 60 different minerals are known to be produced by organisms in a process called biomineralization. In biomineralization, organisms passively or actively, but selectively, accumulate chemical elements from the environment and transform them into mineral structures inside or outside the cell [1]. Biomineralization processes play crucial roles in ecosystems as many of these organisms participate in the geochemical cycles of major elements necessary to life. About two billion years ago, after the great collapse of life, which was anoxic, due to the release of oxygen by the activity of cyano bacteria, magnetotactic bacteria appeared. There are the first organism which syntheses crystal, magnetite or greitgite. 0.5 billion years ago appeared sponges which are the first multicellular organism.  Many sponges have internal skeletons of spongin and/or spicules of calcium carbonate or silicon dioxide. In general, the formation of minerals are under precise biological control and is mediated by a mineralization process, which is known as biologically controlled mineralization. This phenomenon will be illustrated by the presentation of two processes of biomineralization, that of magnetite in the case of magnetotactic bacteria [2] and spicules of calcite in the case of sponges of the calcareous species [3].
[1] Weiner, S. & Dove, P. M. An overview of biomineralization processes and the problem of the vital effect. Rev. in Mineral. Geochem. 54, 1–29 (2003).
[2] J. Werckmann et al., Localized iron accumulation precedes nucleation and growth of magnetite crystals in magnetotactic bacteria, Sci. Rep. 7 (2017
[3] A.L. Rossi et al., Long-range crystalline order in spicules from the calcareous sponge Paraleucilla magna (Porifera, Calcarea), Acta Biomater. 10 (2014).
Acknowledgements: CNPQ, FAPERJ Brazil and LIA-CNRS France


Back to top

Copyright © 2019 National Institute of Materials Physics. All Rights Reserved