Microbiology and Vegetation of Micro-oases and Polar Desert, Haughton Impact Crater, Devon Island, Nunavut, Canada

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منابع مشابه

Hydrocarbons in the Haughton Impact Structure, Devon Island, Nunavut,

CANADA. J. Parnell, G.R. Osinski, P. Lee, M. Baron, M. J. Pearson and M. Feely, Dept. of Geology & Petroleum Geology, University of Aberdeen, Aberdeen AB24 3UE, U.K., [email protected]), Dept. of Geology, University of New Brunswick, Fredericton, New Brunswick E3B 5A3, Canada, SETI Institute, NASA Ames Research Center, Moffett Field, CA 94035-1000, U.S.A., 4 Dept. of Geology, NUI Galway, Rep...

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Heterotrophic microbial colonization of the interior of impact-shocked rocks from Haughton impact structure, Devon Island, Nunavut, Canadian High Arctic

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The Raman Signature of Shocked Carbonates from the Haughton Impact Structure, Devon Island, Canada

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Atmospheric deposition of current use pesticides in the Arctic: snow core records from the Devon Island Ice Cap, Nunavut, Canada.

Current use pesticides (CUPs) have been detected in the Arctic, even though there are no direct sources and their long range atmospheric transport potential is generally lower than that of legacy pesticides. Data on the deposition of CUPs in the Arctic are required to assess the impact of their global usage and emission. In this study, selected CUPs were measured in the layers of a snow pit sam...

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UV-VIS-NIR REFLECTANCE SPECTRA OF SHOCKED CARBONATES FROM THE HAUGHTON IMPACT STRUCTURE, DEVON ISLAND, CANADA: 0.35 – 2.5 μm; IMPLICATIONS FOR CARBONATE IDENTIFICATION ON MARS

Introduction: The identification of carbonates on Mars has remained tentative until very recently [e.g., 1-4, 5, 6]. Given that carbonates are present at or near the surface of Mars and appear to be stable in the present Martian atmosphere, it begs the question, why have we only just found them [7]? Is it because they are simply being masked by overlying material or are there other factors that...

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ژورنال

عنوان ژورنال: Arctic, Antarctic, and Alpine Research

سال: 2001

ISSN: 1523-0430,1938-4246

DOI: 10.1080/15230430.2001.12003435