Nature Communications (Jan 2021)

Jarosite formation in deep Antarctic ice provides a window into acidic, water-limited weathering on Mars

  • Giovanni Baccolo,
  • Barbara Delmonte,
  • P. B. Niles,
  • Giannantonio Cibin,
  • Elena Di Stefano,
  • Dariush Hampai,
  • Lindsay Keller,
  • Valter Maggi,
  • Augusto Marcelli,
  • Joseph Michalski,
  • Christopher Snead,
  • Massimo Frezzotti

DOI
https://doi.org/10.1038/s41467-020-20705-z
Journal volume & issue
Vol. 12, no. 1
pp. 1 – 8

Abstract

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The authors report in-situ formation of jarosite witin the Talos Dome ice core (East Antarctica) and show that this ferric-potassium sulfate mineral is present in ice deeper than 1000 meters and progressively increases with depth. This has implications for the presence and formation mechanisms of jarosite observed on Mars.