Scientific Highlights and Status of the Mars Science Laboratory Mission, Years 9 Through 12

Abstract We present the scientific highlights and status from years 9-12 of NASA’s Mars Science Laboratory mission, with its Curiosity rover. A thermochemolysis-based sample analysis revealed a variety of organic molecules preserved in clay mineral-rich lake/lake margin deposits of the Glen Torridon region. The stratigraphically higher clay-sulfate mineral transition on Aeolis Mons was found to be associated with a lithological change from lacustrine to dry aeolian depositional environments. Water intermittently returned to the surface after the increase in aridity, including during the deposition of wave ripple strata which indicate a climate capable of sustaining an ice-free lake in the early Hesperian. The overlying Mg sulfate-bearing unit has both poly- and monohydrated Mg sulfates and is also enriched in iron carbonate of a purity consistent with chemical sedimentation and therefore atmospheric sequestration. A channel-incised canyon within Gediz Vallis and distal alluvial deposits recorded numerous fluvial and debris flow events after the deposition, lithification, and erosion of the clay- and sulfate-bearing units. Bright clasts found in Gediz Vallis canyon are composed of native sulfur. The investigation of the modern atmosphere and environment focused on the influence of the crater and mountain topography and captured high-altitude noctilucent and iridescent clouds. Radiation monitoring now spans an 11-year solar cycle. Rover systems and science instruments remain capable of addressing mission scientific objectives. All ten scientific instruments continue to return high-value data despite degradation of the Chemistry and Camera instrument’s high-voltage system, loss of multispectral imaging capability, and loss of active neutron spectroscopy. The mission has mitigated the loss of redundant brakes on two arm joints, additional wheel wear, and highly reduced capability of the redundant flight computer. Efficiency improvements in rover energy utilization and operations staffing have allowed the mission team to maintain a high level of productivity despite declining rover power generation and funding.

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Publication Details

Journal
Space Science Reviews
Published
2026-08-25
DOI
https://doi.org/10.1007/s11214-026-01321-7
Primary Topic
Planetary Science and Exploration
Type
article
Field-Weighted Citation Impact
0.00

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article

Scientific Highlights and Status of the Mars Science Laboratory Mission, Years 9 Through 12

A. A. Fraeman, J. P. Grotzinger, J. A. Berger, A. H. Treiman et al.
Space Science Reviews
Planetary Science and Exploration
article

Scientific Highlights and Status of the Mars Science Laboratory Mission, Years 9 Through 12

A. A. Fraeman, J. P. Grotzinger, J. A. Berger, A. H. Treiman, S. P. Schwenzer, Scott D. Guzewich, Alexandra Holloway, Benjamin M. Tutolo, Amy J. Williams, Olivier Gasnault, J. A. Grant, Ashwin Vasavada, Joel M. Davis, J. Michael Battalio, Jack Quade, Elizabeth B. Rampe, Alex B. Bryk, William E. Dietrich, Reidar Larsen
article en

Abstract

Abstract We present the scientific highlights and status from years 9-12 of NASA’s Mars Science Laboratory mission, with its Curiosity rover. A thermochemolysis-based sample analysis revealed a variety of organic molecules preserved in clay mineral-rich lake/lake margin deposits of the Glen Torridon region. The stratigraphically higher clay-sulfate mineral transition on Aeolis Mons was found to be associated with a lithological change from lacustrine to dry aeolian depositional environments. Water intermittently returned to the surface after the increase in aridity, including during the deposition of wave ripple strata which indicate a climate capable of sustaining an ice-free lake in the early Hesperian. The overlying Mg sulfate-bearing unit has both poly- and monohydrated Mg sulfates and is also enriched in iron carbonate of a purity consistent with chemical sedimentation and therefore atmospheric sequestration. A channel-incised canyon within Gediz Vallis and distal alluvial deposits recorded numerous fluvial and debris flow events after the deposition, lithification, and erosion of the clay- and sulfate-bearing units. Bright clasts found in Gediz Vallis canyon are composed of native sulfur. The investigation of the modern atmosphere and environment focused on the influence of the crater and mountain topography and captured high-altitude noctilucent and iridescent clouds. Radiation monitoring now spans an 11-year solar cycle. Rover systems and science instruments remain capable of addressing mission scientific objectives. All ten scientific instruments continue to return high-value data despite degradation of the Chemistry and Camera instrument’s high-voltage system, loss of multispectral imaging capability, and loss of active neutron spectroscopy. The mission has mitigated the loss of redundant brakes on two arm joints, additional wheel wear, and highly reduced capability of the redundant flight computer. Efficiency improvements in rover energy utilization and operations staffing have allowed the mission team to maintain a high level of productivity despite declining rover power generation and funding.

Space Science ReviewsVol. 222(6)
California Institute of Technology (US), Planetary Science Institute (US), Goddard Space Flight Center (US), Universities Space Research Association (US), Jet Propulsion Laboratory (US), University of Calgary (CA), The Open University (GB), University of Florida (US), National Air and Space Museum (US), Johnson Space Center (US), Institut de Recherche en Astrophysique et Planétologie (FR), Imperial College London (GB), Lunar and Planetary Institute (US), University of California, Berkeley (US)
National Aeronautics and Space Administration
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