Paper No. 1
Presentation Time: 3:00 PM

MSA AWARD LECTURE: BIOMINERALIZATION AND FOSSILIZATION OF BACTERIA: WHAT DO WE LEARN FROM FIELD AND EXPERIMENTAL STUDIES


BENZERARA, Karim1, COSMIDIS, Julie2, LI Sr, Jin Hua3, MIOT, Jennyfer1 and COURADEAU, Estelle4, (1)Institut de Mineralogie et de Physique des Milieux Condensés, CNRS & Univ Pierre et Marie Curie, 4 Place Jussieu, Paris, 75005, France, (2)Department of Geological Sciences, University of Colorado, 2200 Colorado Avenue, Boulder, CO 80309, (3)Equipe Géomicrobiologie, Institut de Minéralogie et de Physique des Millieux Condensés, CNRS & Univ. PMC, Tour 23 – Couloir 22/23 – 5e étage – Porte 08, Case courrier 115,4 Place Jussieu, Paris, 75252, France, (4)Equipe Géomicrobiologie, Institut de Minéralogie et de Physique des Millieux Condensés, CNRS & Univ. PMC, Tour 23 – Couloir 22/23 – 5e étage – Porte 08, Case courrier 115,4 Place Jussieu, Paris, 75005, France, karim.benzerara@impmc.upmc.fr

Bacteria can leave fossil traces in the geological record. The search of such traces is key for the study of ancient and/or extraterrestrial life. However, the task is difficult: objects are in the submicrometer size range; morphological criteria of biogenicity are ambiguous for bacteria and microbial-like morphologies can be produced by abiotic processes; phylogenetic diversity which likely impact the fossilization potential of bacteria is very broad and has yet to be analyzed in details.

Here, I will review several approaches that we have been conducting in the recent past. First, I will show how we can use a combination of focused ion beam milling, TEM and synchrotron-based x-ray microscopy to characterize down to the nm-scale some biomorphs in Paleocene phosphorites. While SEM observations provide ambiguous hints, our analyses strongly suggest that these objects are Gram-negative bacteria, with cell walls preserved by incipient biomineralization of Ca-phosphates. In a second approach, we induced biomineralization of diverse bacterial strains in the laboratory. I will show results obtained on anaerobic Fe-oxidizing bacteria and on Ca-phosphate biomineralizing mutant strains affected in their capability to produce a phosphatase enzyme. This improves our understanding of the first steps of fossilization and the ultrastructural details that can be preserved. It moreover provides a source of mineralized cells that are processed through thermal and pressure treatments to simulate the transformations of bacterial structures upon aging. Finally, I will show a study of modern biomineralizing systems in the field, e.g., calcifying microbial communities from a hyperalkaline lake. This allows investigating the link between microbial diversity and fossilization, a key parameter for the study of Precambrian rocks. One lesson is that the use of actualism might be delusive if our knowledge of modern diversity is too limited.