Aliphatic amines in Antarctic CR2, CM2, and CM1/2 carbonaceous chondrites-Reference-Cited by-同舟云学术

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Aliphatic amines in Antarctic CR2, CM2, and CM1/2 carbonaceous chondrites

Published:2016-09 Issue: Volume:189 Page:296-311
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Aponte José C.,McLain Hannah L.,Dworkin Jason P.,Elsila Jamie E.

Funder

NSF

NASA

NASA Postdoctoral Program at the Goddard Space Flight Center

NASA Astrobiology Institute

Goddard Center for Astrobiology

Simons Foundation

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference76 articles.

1. Carbon isotope fractionation in formation of amino acids by photosynthetic organisms;Abelson;Proc. Natl. Acad. Sci. U.S.A.,1961

2. The origin and evolution of chondrites recorded in the elemental and isotopic compositions of their macromolecular organic matter;Alexander;Geochim. Cosmochim. Acta,2007

3. The provenances of asteroids, and their contributions to the volatile inventories of the terrestrial planets;Alexander;Science,2012

4. The classification of CM and CR chondrites using bulk H, C and N abundances and isotopic compositions;Alexander;Geochim. Cosmochim. Acta,2013

5. On the mechanism and rate of spontaneous decomposition of amino acids;Alexandrova;J. Phys. Chem. B,2011

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