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The power of paired proximity science observations: Co-located data from SHERLOC and PIXL on Mars

  • Joseph Razzell Hollis
  • , Kelsey R. Moore
  • , Sunanda Sharma
  • , Luther Beegle
  • , John P. Grotzinger
  • , Abigail Allwood
  • , William Abbey
  • , Rohit Bhartia
  • , Adrian J. Brown
  • , Benton Clark
  • , Edward Cloutis
  • , Andrea Corpolongo
  • , Jesper Henneke
  • , Keyron Hickman-Lewis
  • , Joel A. Hurowitz
  • , Michael W.M. Jones
  • , Yang Liu
  • , Jesús Martinez-Frías
  • , Ashley Murphy
  • , David A.K. Pedersen
  • Svetlana Shkolyar, Sandra Siljeström, Andrew Steele, Mike Tice, Alan Treiman, Kyle Uckert, Scott VanBommel, Anastasia Yanchilina
  • Jet Propulsion Laboratory, California Institute of Technology
  • The Natural History Museum, London
  • California Institute of Technology
  • Photon Systems Inc.
  • Plancius Research
  • Space Science Institute
  • University of Winnipeg
  • University of Cincinnati
  • Technical University of Denmark
  • University of Bologna
  • Queensland University of Technology
  • CSIC
  • Planetary Science Institute
  • University of Maryland, College Park
  • NASA Goddard Space Flight Center
  • RISE Research Institutes of Sweden
  • Carnegie Institution of Washington
  • Texas A&M University
  • Universities Space Research Association
  • Washington University St. Louis
  • Impossible Sensing

Research output: Contribution to journalArticlepeer-review

37 Scopus citations

Abstract

We present a synthesis of PIXL elemental data and SHERLOC Raman spectra collected on two targets investigated by the Perseverance rover during the first year of its exploration of Jezero Crater, Mars. The Bellegarde target (in the Máaz formation) and Dourbes target (in the Séítah formation) exhibit distinctive mineralogies that are an ideal case study for in situ analysis by SHERLOC and PIXL. Each instrument alone produces valuable data about the chemistry and spatial distribution of mineral phases at the sub-millimeter scale. However, combining data from both instruments provides a more robust interpretation that overcomes the limitations of either instrument, for example: 1) Detection of correlated calcium and sulfur in Bellegarde by PIXL is corroborated by the co-located detection of calcium sulfate by SHERLOC. 2) Detection of sodium and chlorine in Dourbes is consistent with either chloride or oxychlorine salts, but SHERLOC does not detect perchlorate or chlorate. 3) A Raman peak at 1120 cm−1 in Dourbes could be sulfate or pyroxene, but elemental abundances from PIXL at that location are a better match to pyroxene. This study emphasizes the importance of analyzing co-located data from both instruments together, to obtain a more complete picture of sub-millimeter-scale mineralogy measured in situ in Jezero crater, Mars, by the Perseverance rover.

Original languageEnglish
Article number115179
JournalIcarus
Volume387
DOIs
StatePublished - Nov 15 2022

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