The Pilbara Drilling Project 2004
Two crucial intervals in geologic time were chosen for drilling purposes. The Early Archaean at 3.5 Ga (Dresser Formation, Warrawoona Group), which was dominated by ocean floor hydrothermal processes and/or shallow evaporitic environment and associated forms of life (thermophilic, photosynthetic ?), and the late Archaean at 2.7 Ga (Tumbiana Formation, Fortescue Group) right before the rise in atmospheric oxygen, when methanotrophic life must have been diversifying.
The important issues to be addressed concern:
1) the origin and conditions of formation of the deposits;
2) the composition and temperature of hydrothermal fluids and Archaean seawater and the origins of the carbonaceous material (biogenic vs chemical);
3) the significance of stromatolites and putative microfossils
4) characterizing the metabolisms of early microbial ecosystems (methanotrophs, sulfato-reducers, photosynthesizers ?) and their impact on early Earth environments and atmosphere;
5) the redox and chemical evolution of the Archaean atmosphere;
6) the study of the microbial diversity associated with drilling fluids, and the central and outer parts of cores to address the issue of potential microbial contamination.
The Pilbara Drilling Project was initiated current 2003 as part of a cross-disciplinary research project at the frontier between Microbiology and Earth Sciences entitled 'Modern and Archaean Deep Biosphere: A dual approach based on drill core samples' and supported by the French interdisciplinary program GEOMEX (Geomicrobiology of Extreme Environments, Lopez-Garcia and Philippot, PI).
Institut de Physique du Globe de Paris - Mise à jour 11/2024
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