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. 2018 Aug 6;115(34):8535–8540. doi: 10.1073/pnas.1808101115

Fig. 2.

Fig. 2.

NanoSIMS images showing the distribution of 12C14N, 16O, 56Fe16O, and 28Si secondary ion species in Murchison and Orgueil IOM acid maceration residues. White and cyan arrows indicate higher 56Fe16O and 28Si intensities, respectively.