Supplementary Figure 5 | Carbonate and phyllosilicate-bearing aeolian bedforms proximal to margin fractured unit. (a) CRISM pixels (blue) for the spectra shown in (d). These pixels cover aeolian bedforms proximal to the margin fractured bedrock shown in Figure S3. (b-c) Enlarged views of carbonate and phyllosilicate-bearing aeolian bedforms where they contact the proximal carbonate and phyllosilicate-bearing margin fractured bedrock described in Figure S3. (d) UMass, TRR3, And TER CRISM spectra from blue pixels shown in (a). The spectral interpretation is the same as described in Figure 4. This aeolian material is therefore interpreted to derive from the proximal margin fractured unit bedrock.