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In Situ Evidence for an Ancient Aqueous Environment at Meridiani Planum, Mars

Title: In Situ Evidence for an Ancient Aqueous Environment at Meridiani Planum, Mars
Authors: Squyres, Steven W.; Grotzinger, John P.; Arvidson, Raymond E.; Bell, James F. III; Calvin, Wendy; Christensen, Philip R.; Clark, Benton C.; Crisp, Jeffrey; Farrand, William H.; Herkenhoff, Ken E.; Johnson, Jeffrey R.; Klingelhofer, Gostar; Knoll, Andrew; McLennan, Scott M.; McSween, Harry Y.; Morris, Richard V.; Rice, John W.; Rieder, Renate; Soderblom, Larry A.
Publisher Information: American Association for the Advancement of Science
Publication Year: 2004
Collection: Harvard University: DASH - Digital Access to Scholarship at Harvard
Description: Sedimentary rocks at Eagle crater in Meridiani Planum are composed of fine-grained siliciclastic materials derived from weathering of basaltic rocks, sulfate minerals (including magnesium sulfate and jarosite) that constitute several tens of percent of the rock by weight, and hematite. Cross-stratification observed in rock outcrops indicates eolian and aqueous transport. Diagenetic features include hematite-rich concretions and crystal-mold vugs. We interpret the rocks to be a mixture of chemical and siliciciastic sediments with a complex diagenetic history. The environmental conditions that they record include episodic inundation by shallow surface water, evaporation, and desiccation. The geologic record at Meridiani Planum suggests that conditions were suitable for biological activity for a period of time in martian history. ; Organismic and Evolutionary Biology
Document Type: other/unknown material
File Description: application/pdf
Language: English
Relation: http://dx.doi.org/10.1126/science.1104559; http://www.ifa.hawaii.edu/%7Emeech/NAIJC/papers/MeridianiPlanum_Science2004_AqueousEnv.pdf; Science
DOI: 10.1126/science.1104559
Availability: http://nrs.harvard.edu/urn-3:HUL.InstRepos:3119538; https://doi.org/10.1126/science.1104559
Accession Number: edsbas.4F2C2705
Database: BASE