Cited by 168Planetary Science and ExplorationAstro and Planetary ScienceGeology and Paleoclimatology Research

Diverse aqueous environments on ancient Mars revealed in the southern highlands

Wray, James J., Murchie, Scott L., Squyres, Steven W., Seelos, Frank P., Tornabene, Livio L.·2009·Geology

Abstract

Research Article| November 01, 2009 Diverse aqueous environments on ancient Mars revealed in the southern highlands James J. Wray; James J. Wray 1Department of Astronomy, Cornell University, Ithaca, New York 14853, USA Search for other works by this author on: GSW Google Scholar Scott L. Murchie; Scott L. Murchie 2Johns Hopkins University/Applied Physics Laboratory, Laurel, Maryland 20723, USA Search for other works by this author on: GSW Google Scholar Steven W. Squyres; Steven W. Squyres 1Department of Astronomy, Cornell University, Ithaca, New York 14853, USA Search for other works by this author on: GSW Google Scholar Frank P. Seelos; Frank P. Seelos 2Johns Hopkins University/Applied Physics Laboratory, Laurel, Maryland 20723, USA Search for other works by this author on: GSW Google Scholar Livio L. Tornabene Livio L. Tornabene 3Lunar and Planetary Laboratory, University of Arizona, Tucson, Arizona 85721, USA Search for other works by this author on: GSW Google Scholar Author and Article Information James J. Wray 1Department of Astronomy, Cornell University, Ithaca, New York 14853, USA Scott L. Murchie 2Johns Hopkins University/Applied Physics Laboratory, Laurel, Maryland 20723, USA Steven W. Squyres 1Department of Astronomy, Cornell University, Ithaca, New York 14853, USA Frank P. Seelos 2Johns Hopkins University/Applied Physics Laboratory, Laurel, Maryland 20723, USA Livio L. Tornabene 3Lunar and Planetary Laboratory, University of Arizona, Tucson, Arizona 85721, USA Publisher: Geological Society of America Received: 20 Apr 2009 Revision Received: 23 Jun 2009 Accepted: 29 Jun 2009 First Online: 02 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2009 Geological Society of America Geology (2009) 37 (11): 1043–1046. https://doi.org/10.1130/G30331A.1 Article history Received: 20 Apr 2009 Revision Received: 23 Jun 2009 Accepted: 29 Jun 2009 First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation James J. Wray, Scott L. Murchie, Steven W. Squyres, Frank P. Seelos, Livio L. Tornabene; Diverse aqueous environments on ancient Mars revealed in the southern highlands. Geology 2009;; 37 (11): 1043–1046. doi: https://doi.org/10.1130/G30331A.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract High-resolution spectral images reveal many new exposures of hydrated minerals across the Noachian southern highlands of Mars. Several different phyllosilicates are observed, with inferred accompanying phases ranging from zeolites to sulfates to chlorides, each in distinct geologic settings. Hydrated sulfates are observed in several locations at mid-latitudes, and likely formed independently from the equatorial sulfates. These assemblages suggest a greater diversity of aqueous environments on ancient Mars than has previously been recognized, and their distribution implies that alteration was widespread during the Noachian Period, not restricted to a few locations. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

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  • Carbonates occur from the north end of the basin to the south, exposed by craters or, in one case, at the eroding edge of a dendritic (fluvial?) feature downslope from the basin wall-incising valleys.

    “They occur from the north end of the basin to the south, Journal of Geophysical Research: Planets 10.1002/2015JE004972 exposed by craters (Figure 4) [see also Wray et al., 2009, Figure DR1C] or, in one case, at the eroding edge of a dendritic (fluvial?)feature downslope from the basin wall-incising valleys (Figure 8).”

    From Orbital evidence for more widespread carbonate-bearing rocks on Mars (2016) · cites this paper as Wray et al., 2009

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References 30 · Cited by 168

Authors
Wray, J. J., Murchie, S. L., Squyres, S. W., Seelos, F. P., & Tornabene, L. L.
Affiliations
  • Cornell University (US)
  • Johns Hopkins University (US)
  • University of Arizona (US)
Venue
Geology
Published
2009-11
Volume
37
Issue
11
Pages
1043-1046
ISSN
  • 0091-7613 (ISSN-L)
  • 1943-2682
OpenAlex
W2041160783
Cited by
168
References
30
Citations by year
2026: 3 · 2025: 7 · 2024: 8 · 2023: 4 · 2022: 7 · 2021: 16 · 2020: 5 · 2019: 8 · 2018: 10 · 2017: 11 · 2016: 10 · 2015: 6 · 2014: 17 · 2013: 9 · 2012: 15
FWCI
7.90
Type
journal article
Language
en
Open access
closed
Locations
Geology (publishedVersion)
Funders
  • National Science Foundation
  • Hertz Foundation
Topics
  • Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Planetary Science and Exploration
  • Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Astro and Planetary Science
  • Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
Keywords
early Mars, aqueous environment, Southern Highlands, water on Mars, Mars Exploration Rover, Mars Express, Mars Global Surveyor, Mars Odyssey, Mars Reconnaissance Orbiter

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