Amino acid compositions in heated carbonaceous chondrites and their compound-specific nitrogen isotopic ratios-Reference-Cited by-同舟云学术

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Amino acid compositions in heated carbonaceous chondrites and their compound-specific nitrogen isotopic ratios

Published:2016-01-21 Issue:1 Volume:68 Page:
ISSN:1880-5981
Container-title:Earth, Planets and Space
language:en
Short-container-title:Earth Planet Sp

Author:

Chan Queenie Hoi Shan,Chikaraishi Yoshito,Takano Yoshinori,Ogawa Nanako O.,Ohkouchi Naohiko

Funder

Japan Society for the Promotion of Science

National Aeronautics and Space Administration

Publisher

Springer Science and Business Media LLC

Subject

Space and Planetary Science,Geology

Link

http://link.springer.com/content/pdf/10.1186/s40623-016-0382-8.pdf

Reference70 articles.

1. Anders E, Ebihara M (1982) Solar-system abundances of the elements. Geochim Cosmochim Acta 46(11):2363–2380

2. Bada JL, Miller SL, Zhao M (1995) The stability of amino acids at submarine hydrothermal vent temperatures. Origins Evol Biospheres 25(1):111–118

3. Bland PA, Collins GS, Davison TM, Abreu NM, Ciesla FJ, Muxworthy AR, Moore J (2014) Pressure–temperature evolution of primordial solar system solids during impact-induced compaction. Nat Commun 5(5):1–13

4. Botta O, Bada JL (2002) Extraterrestrial organic compounds in meteorites. Surv Geophys 23:411–467

5. Brand W, Tegtmeyer A, Hilkert A (1994) Compound-specific isotope analysis: extending toward 15N14N and 18O16O. Org Geochem 21(6):585–594

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