Table of Contents
Section I: Geology, Hydrology, and Paleontology1. The geological framework of the R�o Tinto: The largest accumulation of sulfides in the Earth crust
2. Sedimentology and geobiology of R�o Tinto
3. Hydrogeological and hydrogeochemical characteristics of the source of the R�o Tinto
4. Paleontology of R�o Tinto
Section II. Microbial and Eukaryotic Diversity
5. Prokaryotic diversity along the R�o Tinto
6. Microbial biodiversity in the anoxic sediments of R�o Tinto
7. Acidophilic cyanobacteria in the Tinto basin
8. Cyanobacteria in the deep subsurface of the Iberian Pyrite Belt
9. Eukaryotic diversity along the Tinto basin
10. Fungal diversity in the Tinto basin
11. Vegetation associated to an extreme acidic river with high metal content, R�o Tinto
12. R�o Tinto virology
Section III. R�o Tinto as a Mars Terrestrial Analogue
13. Mineralogical and geochemical characterization of R�o Tinto using combined spectroscopic methods: implications for exploration of Mars
14. Methanogenesis in a Mars terrestrial analogue
15. From R�o Tinto to Mars: Investigating potential microbial metabolisms and their signatures
16. Technology developments for the characterization of the deep subsurface of the Iberian Pyrite Belt and Mars
Section IV. Geomicrobiology: Fundamentals and Applications
17. Origin of R�o Tinto, anaerobic oxidation of iron in the deep subsurface of the Iberian Pyrite Belt
18. Biogeochemical cycles operating in the deep subsurface of the Iberian Pyrite Belt
19. Retrotranscriptomic analysis of the Tinto basin to understand polyextremicity
20. Biotechnological applications of the biodiversity existing in the Tinto basin
21. Vitamin B12 in the deep subsurface of the Iberian Pyrite Belt

