Fig. 6From: FTIR microspectroscopy of carbonaceous matter in ~ 3.5 Ga seafloor hydrothermal deposits in the North Pole area, Western AustraliaExamples of Raman spectra of the carbonaceous clots. The spectra marked as CH2, CH2 only, and no CH2 were obtained from sample 96NP452 (CH2: both aliphatic CH2 and CH3 bonds were observed in micro-FTIR measurements; CH2 only: CH2 bond was observed but CH3 was not; no CH2: neither CH2 nor CH3 were observed). Spot numbers (#3, #12, and #13) corresponding to Table 1 are also shown. The band around 464 cm−1 is due to the quartz matrix of the silica veinsBack to article page