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The 2004 Mars Exploration Rover Mission Evidence for Water and Prospects for Life. Dr. John Grotzinger Hot Science - Cool Talks Volume 38.
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The 2004 Mars ExplorationRover Mission Evidence for Water and Prospects for Life Dr. John Grotzinger Hot Science - Cool Talks Volume 38 Produced by and for the Hot Science – Cool Talks Outreach Lecture Series of the Environmental Science Institute. We request that the use of any of these materials include an acknowledgement of Dr. John Grotzinger, and the Hot Science – Cool Talks Outreach Lecture Series of the Environmental Science Institute of the University of Texas at Austin. We hope you find these materials educational and enjoyable.
The 2004 Mars ExplorationRover Mission: Evidence for Water andProspects for Life John Grotzingeron behalf of MER Athena Science Team
Mars Science Strategy Mars Science Strategy: Follow the Water! Common Thread LIFE CLIMATE GEOLOGY HUMAN
The Athena Science Payload The Athena Science Payload Remote Sensing Package Pancam Mast Assembly (PMA) Pancam Mini-TES Magnetic Properties Experiment In-Situ Package Instrument Deployment Device (IDD) Microscopic Imager Alpha Particle X-Ray Spectrometer Mössbauer Spectrometer Rock Abrasion Tool
The Team The Team
Mars Pathfinder Mars Pathfinder
Wrap it up and cram it in…… Wrap it up and cram it in…
The Three Challenging Mission Phases The Three Challenging Mission Phases Launch & Cruise Entry, Descent & Landing Egress & Surface Operations
Meridiani Gusev Opportunity at Meridiani Planum 2000 km
Hematite: Mineralogic Beacon Hematite Distribution Map from Tes Data 5oN 0 6oS 10oW 0 2oE 0% 15% hematite (Figure based on Christensen et al., (2001) JGR, v. 106(E10), Plate 2, p.23,877.)
Hole in One Eagle Crater
Backshell and Parachute Backshell and Parachute
You are here You are here
Short-Timescale Temperature Excursions 1 Red = hot Purple = cold Red to purple is 2 K (degrees Kelvin) 0.8 0.6 Height Above Surface (km) 0.4 0.2 0 21 22 23 24 25 26 27 28 29 Minutes past 1000 hours (sol 12) • Largest temperature variations confined to lowest 100 meters or so • Appears that temperature perturbations propagate upward
Dust Devils Dust Devils
Opportunity: View from Lander Spirit: View from Lander 5 metres 5 metres
Mössbauer Spectrum of El Capitan Mössbauer Spectrum of El Capitan: Meridiani Planum Jarosite: (K, Na, X+1)Fe3(SO4) (OH)6
Rio Tinto, Spain Andy Knoll
Spherules Spherules 5 mm
Sediment Bedforms Sediment Bedforms (e.g. Ripples)
Ancient Terrestrial Ripples Ancient Terrestrial Ripples: 1.4 Billion Years Old
Ripple Cross-Bedding in 3-D Ripple Cross-Bedding in 3D
Bedforms in Flowing Water Bedforms in Flowing Water Antidunes 2.0 Upper Plane Beds 1.0 Lower Plane Beds Dunes 0.6 Mean flow velocity (m sec-1) Ripples No Sediment Movement 0.2 V. Fine Sand V. Coarse Sand 0.5 1.0 2.0 0.1 Median grain diameter (mm) Southard and Bouchwal,1990
Current Ripples in Water Current Ripples in Water 6 hours of ripple migration Image is 60x40 cm Flume experiments by Dave Rubin and Jon Nelson, USGS
Current Ripples in Cross Section Simulation by Dave Rubin, USGS
Festoon Cross-Bedding on Earth Festoon Cross-Bedding on Earth
Festoon Cross-Bedding on Mars Festoon Cross-Bedding on Mars
Burns formation Burns formation (Endurance crater) 2.0 m
Burns Stratigraphy 7 Burns Stratigraphy Interdune/Playa Festoon Cross-lamination Wavy Bedding Translatent Strata Lower Unit 6 Whatanga Contact Zone of Recrystallization Capillary Fringe of Water Table? 5 Eolian Sand Sheet Translatent Strata Low-Angle Strata Lower Unit 4 3 Wellington Contact Deflation Surface Water Table Controlled? 2 Eolian Dune Field Cross-Bedded Sandstone Lower Unit 1 m
Modern Sand Dunes on Mars Modern Sand Dunes on Mars ~ 50 cm
Interdune Surface Interdune Surface
Interdune Deflation Surface Interdune Deflation Surface
Modern Mars Analog Modern Mars Analog: Um Asamin
Modern Interdune Depression Modern Interdune Depression
Endurance Chemostratigraphy ~ 50 cm
Ratio to surface rock average Depth in crater
Changes Down Section: Texture Ontario Diamond Jenness
Meridiani environment appears to have been acidic, hypersaline, and only intermittently wet. • Life exists at such extremes on Earth. • But Meridiani data suggest potential challenges to origin as well as persistence of life. Rio Tinto Extremophiles Andy Knoll
The Good News • Evidence of any life that might have existed might well be preserved in chemical sediments and concretions. • Chemical and textural details of Meridiani salts and iron oxides likely to reveal much about environmental history. • All this favors Meridiani Planum as a target for sample return. Andy Knoll
Summary • Rovers have: • Operated for over 1200 days • Returned over 100,000 images • Analyzed dozens of rocks and soils
Summary • Evidence for water: • Mössbauer detection of jarosite • Crystal molds, concretions, diagenesis • Festoon ripple cross-bedding • Stratigraphic succession of environments