Structural Evolution of Burmese Amber during Petrifaction Based on a Comparison of the Spectral Characteristics of Amber, Copal, and Rosin
Table 1
Infrared peak attributions of the samples.
Group
Saturated or unsaturated
Infrared peak position (cm−1)
Evolution of spectral feature
Burmese ambers
Copal
Rosin
CH2, CH3
Saturated
2925, 2866, 2847, 1458, 1375
2957, 2869, 1464, 1384
1466, 1389
Diminishing absorption intensity from Burmese amber to copal to rosin
ν (CH2−CH3)
Saturated
2731, 2672
2728, 2670
2724, 2667
Decreasing absorption intensity from Burmese amber to copal to rosin. Hydrogen bond cleavage during the formation of amber forms a stable saturated hydrocarbon structure.
C=O
Unsaturated
1719–1724
1720–1726
1710–1722
The peak is split in the spectra of the amber samples.
Unsaturated six-membered ring
Unsaturated
1600
—
—
Weak absorption in spectra of amber samples
Isopropyl
Saturated
1383
1384, 1369
1372, 1386
Diminishing absorption intensity from Burmese amber to copal to rosin
Isopropyl skeleton
Saturated
1162
1164
1161
The absorption intensity of Burmese amber, copal, and rosin is almost the same
Intramolecular hydrogen bonding between carboxylic acids
Saturated
—
—
2651, 2534
No absorption peaks are seen in the spectra of copal and amber.