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Rio Tinto

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Encyclopedia of Astrobiology

Chemical Formula

$$ 4\bullet {\mathrm{FeS}}_2\ \left(\mathrm{pyrite}\right)+3\bullet {\mathrm{O}}_2+10\bullet {\mathrm{H}}_2\mathrm{O}\to 4\bullet \left[\mathrm{FeOOH}\right]\ \left(\mathrm{ferruginous}\ \mathrm{sediments}\right)+2\bullet {{\mathrm{SO}}_4}^{2-}+16\bullet {\mathrm{H}}^{+} $$
(1)
$$ {\mathrm{Fe}}^{3+}+{\mathrm{H}}_2\mathrm{O}\leftrightarrow \mathrm{Fe}{\left(\mathrm{OH}\right)}^{2+}+{\mathrm{H}}^{+}\, \left(\mathrm{chemical}\ \mathrm{buffer}\ \mathrm{controlled}\ \mathrm{by}\ {\mathrm{Fe}}^{3+}\right) $$
(2)

Definition

Río Tinto is a 100-km-long acidic fluvial system (Fig. 1) emplaced in the IPB (Leistel et al. 1998) considered as a chemical environmental analog of Mars (Fernández-Remolar et al. 2005). Since the paleolithic (Mayoral et al. 2021), the Rio Tinto basin has been populated by different cultures and civilizations (chalcolithic, bronze, and iron), which have mined the rich metallic ore bodies for copper, silver, and gold for millennia. The fluvial system is...

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Abbreviations

IPB:

Iberian Pyrite Belt

IPBSL:

Iberian Pyrite Belt Subsurface Life

MARTE:

Mars Analog and Research Technology Experiment

References and Further Reading

  • Amils R, Fernandez Remolar D (2020) Rio Tinto: an extreme acidic environmental model of Astrobiological interest. In: Seckbach J, Stan-Lotter H (eds) Extremophiles as astrobiological models. Wiley, pp 21–44

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  • Ehlmann BL, Edwards CS (2014) Mineralogy of the Martian surface. Annu Rev Earth Planet Sci 42(1):291–315

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  • Essalhi M et al (2011) A case study of the internal structures of gossans and weathering processes in the Iberian Pyrite Belt using magnetic fabrics and paleomagnetic dating. Mineral Deposita 46(8):981–999

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  • Fernández-Remolar DC, Knoll AH (2008) Fossilization potential of iron-bearing minerals in acidic environments of Rio Tinto, Spain: implications for Mars exploration. Icarus 194:72–85

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  • Fernández-Remolar D, Rodríguez N, Gómez F, Amils R (2003) The geological record of an acidic environment driven by iron hydrochemistry: the Tinto River system. J Geophys Res 108(E7). https://doi.org/10.1029/2002JE001918

  • Fernández-Remolar DC, Morris RV, Gruener JE, Amils R, Knoll AH (2005) The Rio Tinto Basin, Spain: mineralogy, sedimentary geobiology, and implications for interpretation of outcrop rocks at Meridiani Planum, Mars. Earth Planet Sci Lett 240(1):149–167

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  • Fernández-Remolar DC, Banerjee N, Gómez-Ortiz D, Izawa M, Amils R (2018) A mineralogical archive of the biogeochemical sulfur cycle preserved in the subsurface of the Río Tinto system. Am Mineral 103:394–411

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  • Fernandez-Remolar DC et al. accepted. The molecular record of metabolic activity in the subsurface of the Rio Tinto Mars analog. Astrobiology

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  • Gómez F, Fernández-Remolar D, González-Toril EF, Amils R (2004) The Tinto River, an extreme Gaian environment. In: Margulis L, Miller J, Boston P, Schneider S, Crist E (eds) Scientist on Gaia 2000. MIT Press, Boston, pp 321–334

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  • Gómez-Ortiz D et al (2014) Identification of the subsurface sulfide bodies responsible for acidity in Río Tinto source water, Spain. Earth Planet Sci Lett 391:36–41

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  • Mayoral E et al (2021) Tracking late Pleistocene Neandertals on the Iberian coast. Sci Rep 11(1):4103

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Correspondence to David C. Fernandez-Remolar .

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Fernandez-Remolar, D.C. (2022). Rio Tinto. In: Gargaud, M., et al. Encyclopedia of Astrobiology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-27833-4_1379-3

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  • DOI: https://doi.org/10.1007/978-3-642-27833-4_1379-3

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  • Print ISBN: 978-3-642-27833-4

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Chapter history

  1. Latest

    Rio Tinto
    Published:
    27 November 2021

    DOI: https://doi.org/10.1007/978-3-642-27833-4_1379-3

  2. Original

    Rio Tinto
    Published:
    16 April 2015

    DOI: https://doi.org/10.1007/978-3-642-27833-4_1379-2