Please use this identifier to cite or link to this item: http://hdl.handle.net/1893/24410
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dc.contributor.authorSchröder, Christianen_UK
dc.contributor.authorBland, Philen_UK
dc.contributor.authorGolombek, Matthewen_UK
dc.contributor.authorAshley, Jamesen_UK
dc.contributor.authorWarner, Nicholasen_UK
dc.contributor.authorGrant, Johnen_UK
dc.date.accessioned2016-12-28T23:19:21Z-
dc.date.available2016-12-28T23:19:21Z-
dc.date.issued2016en_UK
dc.identifier.other13459en_UK
dc.identifier.urihttp://hdl.handle.net/1893/24410-
dc.description.abstractSpacecraft exploring Mars, notably the Mars Exploration Rovers Spirit and Opportunity as well as the Mars Science Laboratory or Curiosity rover, have accumulated evidence for wet and habitable conditions on Early Mars more than 3 billion years ago. Current conditions, by contrast, are cold, extremely arid, and seemingly inhospitable. To evaluate exactly how dry today’s environment is, it is important to understand currently ongoing weathering processes. Here we present chemical weathering rates determined for Mars. We use the oxidation of iron in stony meteorites investigated by the Mars Exploration Rover Opportunity at Meridiani Planum. Their maximum exposure age is constrained by the formation of Victoria crater and their minimum age by erosion of the meteorites. The chemical weathering rates thus derived are ~1 to 4 orders of magnitude slower than that of similar meteorites found in Antarctica where the slowest rates are observed on Earth.en_UK
dc.language.isoenen_UK
dc.publisherSpringer Natureen_UK
dc.relationSchröder C, Bland P, Golombek M, Ashley J, Warner N & Grant J (2016) Amazonian chemical weathering rate derived from stony meteorite finds at Meridiani Planum on Mars. Nature Communications, 7, Art. No.: 13459. https://doi.org/10.1038/ncomms13459en_UK
dc.rightsThis work is licensed under a Creative Commons Attribution 4.0 International License. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in the credit line; if the material is not included under the Creative Commons license, users will need to obtain permission from the license holder to reproduce the material. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/en_UK
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/en_UK
dc.subjectgeochemistryen_UK
dc.subjectmeteoriticsen_UK
dc.titleAmazonian chemical weathering rate derived from stony meteorite finds at Meridiani Planum on Marsen_UK
dc.typeJournal Articleen_UK
dc.identifier.doi10.1038/ncomms13459en_UK
dc.identifier.pmid27834377en_UK
dc.citation.jtitleNature Communicationsen_UK
dc.citation.issn2041-1723en_UK
dc.citation.volume7en_UK
dc.citation.publicationstatusPublisheden_UK
dc.citation.peerreviewedRefereeden_UK
dc.type.statusVoR - Version of Recorden_UK
dc.author.emailchristian.schroeder@stir.ac.uken_UK
dc.citation.date11/11/2016en_UK
dc.contributor.affiliationBiological and Environmental Sciencesen_UK
dc.contributor.affiliationCurtin University Australiaen_UK
dc.contributor.affiliationCalifornia Institute of Technologyen_UK
dc.contributor.affiliationCalifornia Institute of Technologyen_UK
dc.contributor.affiliationState University of New York at Geneseoen_UK
dc.contributor.affiliationSmithsonianen_UK
dc.identifier.isiWOS:000387470500001en_UK
dc.identifier.scopusid2-s2.0-84995370963en_UK
dc.identifier.wtid546968en_UK
dc.contributor.orcid0000-0002-7935-6039en_UK
dc.date.accepted2016-09-26en_UK
dc.date.filedepositdate2016-10-10en_UK
Appears in Collections:Biological and Environmental Sciences Journal Articles

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