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Volumn 279, Issue 5349, 1998, Pages 366-369

Isotopic evidence for a terrestrial source of organic compounds found in martian meteorites Allan Hills 84001 and Elephant Moraine 79001

Author keywords

[No Author keywords available]

Indexed keywords

HYDROCARBON;

EID: 0032536042     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.279.5349.366     Document Type: Article
Times cited : (127)

References (40)
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    • note
    • 14C in carbonates from these two meteorites to have decayed to a level about 0.9% of the modern value.
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    • 14C analysis by AMS. The AMS measurements on these graphite targets were made at the University of Arizona AMS Facility (34). Blanks run at each temperature step showed 3 ± 1 μg of modern C for each extraction step (35). For our samples, each combustion step yielded between 9 and 79 μg of C, with an average sample size of ∼30 μg.
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    • note
    • The blank levels we determined for a series of combustion steps gave 3 μg (75° to 200°C), 2.5 μg (200° to 400°C), and 5.6 μg (400° to 600°C) of modern carbon. Other studies on blanks in our laboratory for combustions using this line give a mean blank of 3 ± 1 μg of carbon.
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    • note
    • We are grateful to the Meteorite Working Group for provision of the samples. We wish to thank A. L. Hatheway, D. Biddulph, L. R. Hewitt, and T. E. Lange for technical assistance, and K. Hutchins, G. S. Burr, D. J. Donahue, and C. J. Eastoe for many useful scientific discussions. This work was partly supported by NASA grant NAGW-3614 and NSF grant EAR 95-08413.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.