Evidence for Amazonian acidic liquid water on Mars-A reinterpretation of MER mission results

Alberto G. Fairén, Dirk Schulze-Makuch, Alexis P. Rodríguez, Wolfgang Fink, Alfonso F. Davila, Esther R. Uceda, Roberto Furfaro, Ricardo Amils, Christopher P. McKay

Research output: Contribution to journalArticle

22 Citations (Scopus)

Abstract

The Mars Exploration Rover (MER) missions have confirmed aqueous activity on Mars. Here we review the analyses of the field-based MER data, and conclude that some weathering processes in Meridiani Planum and Gusev crater are better explained by late diagenetic water-rock interactions than by early diagenesis only. At Meridiani, the discovery of jarosite by MER-1 Opportunity indicates acidic aqueous activity, evaporation, and desiccation of rock materials. MER-based information, placed into the context of published data, point to local and limited aqueous activity during geologically recent times in Meridiani. Pre-Amazonian environmental changes (including important variations in the near-surface groundwater reservoirs, impact cratering, and global dust storms and other pervasive wind-related erosion) are too extreme for pulverulent jarosite to survive over extended time periods, and therefore we argue instead that jarosite deposits must have formed in a climatically more stable period. Any deposits of pre-existent concretionary jarosite surviving up to the Amazonian would not have reached completion in the highly saline and acidic brines occurring at Meridiani. MER-2 Spirit has also revealed evidence for local and limited Amazonian aqueous environmental conditions in Gusev crater, including chemical weathering leading to goethite and hematite precipitation, rock layering, and chemical enhancement of Cl, S, Br, and oxidized iron in rocks and soils. The estimated relative age of the impact crater materials in Gusev indicates that these processes have taken place during the last 2 billion years. We conclude that minor amounts of shallow acidic liquid water have been present on the surface of Mars at local scales during the Amazonian Period.

Original languageEnglish (US)
Pages (from-to)276-287
Number of pages12
JournalPlanetary and Space Science
Volume57
Issue number3
DOIs
StatePublished - Mar 2009

Fingerprint

Mars exploration
mars
Mars
jarosite
liquid
craters
rocks
liquids
water
weathering
crater
wind erosion
deposits
dust storms
brines
cratering
hematite
ground water
rock
drying

Keywords

  • Amazonian
  • Gusev crater
  • Liquid water
  • Mars
  • Mars Exploration Rovers
  • Meridiani Planum

ASJC Scopus subject areas

  • Space and Planetary Science
  • Astronomy and Astrophysics

Cite this

Fairén, A. G., Schulze-Makuch, D., Rodríguez, A. P., Fink, W., Davila, A. F., Uceda, E. R., ... McKay, C. P. (2009). Evidence for Amazonian acidic liquid water on Mars-A reinterpretation of MER mission results. Planetary and Space Science, 57(3), 276-287. https://doi.org/10.1016/j.pss.2008.11.008

Evidence for Amazonian acidic liquid water on Mars-A reinterpretation of MER mission results. / Fairén, Alberto G.; Schulze-Makuch, Dirk; Rodríguez, Alexis P.; Fink, Wolfgang; Davila, Alfonso F.; Uceda, Esther R.; Furfaro, Roberto; Amils, Ricardo; McKay, Christopher P.

In: Planetary and Space Science, Vol. 57, No. 3, 03.2009, p. 276-287.

Research output: Contribution to journalArticle

Fairén, AG, Schulze-Makuch, D, Rodríguez, AP, Fink, W, Davila, AF, Uceda, ER, Furfaro, R, Amils, R & McKay, CP 2009, 'Evidence for Amazonian acidic liquid water on Mars-A reinterpretation of MER mission results', Planetary and Space Science, vol. 57, no. 3, pp. 276-287. https://doi.org/10.1016/j.pss.2008.11.008
Fairén, Alberto G. ; Schulze-Makuch, Dirk ; Rodríguez, Alexis P. ; Fink, Wolfgang ; Davila, Alfonso F. ; Uceda, Esther R. ; Furfaro, Roberto ; Amils, Ricardo ; McKay, Christopher P. / Evidence for Amazonian acidic liquid water on Mars-A reinterpretation of MER mission results. In: Planetary and Space Science. 2009 ; Vol. 57, No. 3. pp. 276-287.
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