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. Author manuscript; available in PMC: 2020 May 21.
Published in final edited form as: Meteorit Planet Sci. 2018 Oct 14;54(1):142–156. doi: 10.1111/maps.13202

Figure 2.

Figure 2.

GC-MS chromatograms of derivatized aldehyde and ketone standards, the serpentine mineral analogue blank, and the Murchison meteorite extract, and a GC-IRMS chromatogram of carbonyl compounds in the Murchison sample measured for δ13C. GC-MS peaks in the upper three chromatograms represent PFBHA derivatives, containing the characteristic ion of m/z= 181.0. The lower GC-MS chromatogram is a total ion chromatogram (TIC). The GC-IRMS chromatogram shows the m/z= 44 (12CO2 peak) measured during carbon compound-specific isotope analysis. Peak R represents unreacted PFBHA derivatization reagent. The identities of the labeled peaks are presented in Table 1.