Note to users. If you're seeing this message, it means that your browser cannot find this page's style/presentation instructions -- or possibly that you are using a browser that does not support current Web standards. Find out more about why this message is appearing, and what you can do to make your experience of our site the best it can be.
The Observatoire pour la Minéralogie, l'Eau, les Glaces,et l'Activité (OMEGA) imaging spectrometer observed thenorthern circumpolar regions of Mars at a resolution of a fewkilometers. An extended region at 240°E, 85°N, withan area of 60 kilometers by 200 kilometers, exhibits absorptionsat wavelengths of 1.45, 1.75, 1.94, 2.22, 2.26, and 2.48 micrometers.These signatures can be unambiguously attributed to calcium-richsulfates, most likely gypsum. This region corresponds to thedark longitudinal dunes of Olympia Planitia. These observationsreveal that water alteration played a major role in the formationof the constituting minerals of northern circumpolar terrains.
Institut d'Astrophysique Spatiale (IAS), Bâtiment 121, 91405 Orsay Campus, France.
* To whom correspondence should be addressed. E-mail: yves.langevin{at}ias.u-psud.fr
David A. Paige (11 March 2005) Science307 (5715), 1575.
[DOI: 10.1126/science.1110530] |Abstract »|Full Text »|PDF »
NEWS OF THE WEEK
Richard A. Kerr (18 February 2005) Science307 (5712), 1025a.
[DOI: 10.1126/science.307.5712.1025a] |Summary »|Full Text »|PDF »
THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
Detection of Perchlorate and the Soluble Chemistry of Martian Soil at the Phoenix Lander Site.
M. H. Hecht, S. P. Kounaves, R. C. Quinn, S. J. West, S. M. M. Young, D. W. Ming, D. C. Catling, B. C. Clark, W. V. Boynton, J. Hoffman, et al. (2009)
Science
325, 64-67
|Abstract »|Full Text »|PDF »
Continental-scale salt tectonics on Mars and the origin of Valles Marineris and associated outflow channels.
D. R. Montgomery, S. M. Som, M. P. A. Jackson, B. C. Schreiber, A. R. Gillespie, and J. B. Adams (2009)
Geological Society of America Bulletin
121, 117-133
|Abstract »|Full Text »|PDF »
High-pressure behavior of gypsum: A single-crystal X-ray study.
P. Comodi, S. Nazzareni, P. F. Zanazzi, and S. Speziale (2008)
American Mineralogist
93, 1530-1537
|Abstract »|Full Text »|PDF »
Eukaryote-Dominated Biofilms in Extreme Environments: Overlooked Sources of Information in the Geologic Record.
S. S. Brake and S. T. Hasiotis (2008)
Palaios
23, 121-123
|Full Text »|PDF »
Meter-Scale Morphology of the North Polar Region of Mars.
K. E. Herkenhoff, S. Byrne, P. S. Russell, K. E. Fishbaugh, and A. S. McEwen (2007)
Science
317, 1711-1715
|Abstract »|Full Text »|PDF »
Crystal molds on Mars: Melting of a possible new mineral species to create Martian chaotic terrain.
A. Aubrey, H. J. Cleaves, J. H. Chalmers, A. M. Skelley, R. A. Mathies, F. J. Grunthaner, P. Ehrenfreund, and J. L. Bada (2006)
Geology
34, 357-360
|Abstract »|Full Text »|PDF »
Global mineralogical and aqueous mars history derived from OMEGA/Mars Express data..
J.-P. Bibring, Y. Langevin, J. F. Mustard, F. Poulet, R. Arvidson, A. Gendrin, B. Gondet, N. Mangold, P. Pinet, F. Forget, et al. (2006)
Science
312, 400-404
|Abstract »|Full Text »|PDF »
Spectral Reflectance and Morphologic Correlations in Eastern Terra Meridiani, Mars.
R. E. Arvidson, F. Poulet, J.-P. Bibring, M. Wolff, A. Gendrin, R. V. Morris, J. J. Freeman, Y. Langevin, N. Mangold, and G. Bellucci (2005)
Science
307, 1591-1594
|Abstract »|Full Text »|PDF »
Sulfates in Martian Layered Terrains: The OMEGA/Mars Express View.
A. Gendrin, N. Mangold, J.-P. Bibring, Y. Langevin, B. Gondet, F. Poulet, G. Bonello, C. Quantin, J. Mustard, R. Arvidson, et al. (2005)
Science
307, 1587-1591
|Abstract »|Full Text »|PDF »
Mars Surface Diversity as Revealed by the OMEGA/Mars Express Observations.
J.-P. Bibring, Y. Langevin, A. Gendrin, B. Gondet, F. Poulet, M. Berthe, A. Soufflot, R. Arvidson, N. Mangold, J. Mustard, et al. (2005)
Science
307, 1576-1581
|Abstract »|Full Text »|PDF »