Fig. 4From: Amino acid compositions in heated carbonaceous chondrites and their compound-specific nitrogen isotopic ratiosComparison of the δ15N values (‰) of amino acids. Comparison of the δ15N values (‰) of amino acids obtained from this study and previous measurements on CM chondrites: ALH 83100, Murchison, LEW 90500 and LON 94101(Elsila et al. 2012; Engel and Macko 1997), CR chondrites: GRA 95229, LAP 02342, EET 92042, and QUE 99177 (Elsila et al. 2012; Pizzarello and Holmes 2009), and terrestrial materials (Burton et al. 2012b and references therein)Back to article page