Biogeochemical determinants of microbialite formation – Microbialites
Biogeochemical determinants of microbialite formation
MICROBIALITES is an interdisciplinary project at the geology-chemistry-biology interface aiming at understanding the process leading to the formation of modern microbialites, from nano- to macro-scale. We use as models of study microbialites from Lake Alchichica and several other crater lakes in Mexico but will also compare these to other systems.
Goals of the project
The specific goals of the project are:<br /><br />1. Study, at microscale, carbonate precipitation favoured by specific microbial lineages. We will explore the hypothesis that some cyanobacteria favour aragonite formation by locally increasing Ca2+ concentration and alkalinity.<br /><br />2. Study at local scale how microbialite-associated microbial communities globally favour carbonate precipitation. We will explore the hypothesis that the net metabolic balance of microbial activities carried out along night/day cycles promotes carbonate precipitation.<br /><br />3. Study at larger scale which factors determine microbialite formation across ecosystems. We will explore the hypothesis that abiotic parameters and microbial community composition are interdependent and this interaction operates across ecosystems where microbialites form.
To meet our objectives, we combine a variety of methods including genomic, metagenomic and metatranscriptomic analysis of microbial communities, chemical, isotopic and mineralogical analyses as well as high-resolution observation of microbialites and multivariate statistical analyses.
Our first results comprise:
- The identification, genome reconstruction and analysis and metabolic potential inference for Lithoflexus mexicanus, a new potentially biomineralising quasi-clonal species of Chloroflexi identified at different depths in Alchichica microbialites that carries out anoxygenic photosynthesis (Saghaï et al, Genome Biol Evol, 2020)
- The identification of a “core microbiome” shared by microbialite-associated microbial communities from 10 different Mexican lakes (Iniesto et al, Environ Microbiol, in press)
- The alkalinity of Mexican lakes harbouring microbialites correlates with their abundance and massiveness, which allows putting forward a scenario of chemical evolution for these lakes in parallel to that of the abundance, mineral and chemical composition of microbialites (Zeyen et al, submitted).
Near future perspectives:
- Finish the detailed characterization of samples collected during our field trip to Mexico in 2019 (chemistry, mineralogy, isotopes)
- Progress in ongoing comparative metagenomic and metatranscriptomic work
- Initiate comparative analyses with microbialites collected in Sardinia coastal lagoons
- Comparative analysis and building up a synthetic model about microbialite formation
1. Saghaï A, Zivanovic Y, Moreira D, Tavera R, López-García P (2020) A novel microbialite-associated phototrophic Chloroflexi lineage exhibiting a clonal pattern along depth. Genome Biol Evol, 12: 1207–1216
2. Iniesto M, Moreira D, Reboul G, Deschamps P, Benzerara K, Bertolino P, Saghaï A, Tavera R, López-García P. Core microbial communities of lacustrine microbialites sampled along an alkalinity gradient. Environ Microbiol, in press.
3. Integrative analysis of the mineralogical and chemical composition of modern microbialites from ten Mexican lakes: what do we learn about their formation? Nina Zeyen, Karim Benzerara, Olivier Beyssac, Damien Daval, Jérôme Gaillardet, Christophe Thomazo, Rosaluz Tavera, Purificación López-García, David Moreira and Elodie Duprat. Submitted
Séminaires/conférences/communications: 2 international, 7 national
- 5 lectures/courses
- Participation to the documentary ‘Et si la Terre était unique ?’ by L. Lichtenstein partly filmed during our Mexican expedition in 2019 - www.francetvpro.fr/france-5/communiques-de-presse/et-si-la-terre-etait-unique-41196103
Stromatolites and, more generally, microbialites are organosedimentary structures formed under the influence of phylogenetically and functionally diverse microbial communities in interaction with abiotic factors. They are C reservoirs (as biomass and carbonates). Fossil stromatolites represent the oldest undisputed evidence of life on Earth (~3.7 Ga). Yet, the specific identity and functions of associated microorganisms and the local environmental conditions resulting in their formation are poorly understood. We propose an interdisciplinary project at the geology-chemistry-biology interface to decipher the formation process of modern microbialites from the nanoscale to the macroscale. We will combine different types of analyses (‘omics’ methods, (cryo)microscopy, morphology, mineralogy, isotopes) to culture-based carbonatogenesis experiments and natural microbialites from freshwater systems (Mexican crater lakes) to identify common determinants of microbialite formation.
Madame Purificacion Lopez-Garcia (Université Paris-Sud - Laboratoire Ecologie, systématique, évolution)
The author of this summary is the project coordinator, who is responsible for the content of this summary. The ANR declines any responsibility as for its contents.
UPSud ESE Université Paris-Sud - Laboratoire Ecologie, systématique, évolution
IMPMC Institut de Minéralogie, de Physique des Matériaux et de Cosmochimie
I2BC Institut de Biologie Intégrative de la Cellule
BIOGEOSCIENCES Université de Bourgogne
Help of the ANR 575,154 euros
Beginning and duration of the scientific project: January 2019 - 48 Months