Geology Reference
In-Depth Information
29
a
Fossil
Quercus hispanica
specimen 2
15
56
200
150
100
50
0
-50
ppm
29
b
Fossil
Populus alba
specimen 2
15
56
200
150
100
50
0
-50
ppm
Fig. 3.11
13
C NMR CP-MAS spectra of fossil leaves. (
a
)
Castaneavesca
specimen 2 (
b
)
Populu-
salba
specimen 2
FTIR was used to obtain further structural information. FTIR is particularly
effective for the characterisation of oxygen functionalities and has been applied
previously to fossil algaenan (Blokker et al.
1998
),
Gloeocapsomorphaprisca
microfossils (Derenne et al.
1994
), kerogen (Landais et al.
1993
) and plant fossil
cuticles (Mösle et al.
1998
; Collinson et al.
1998
). In the traditional global mode
analysis (KBr) technique, one of the primary limitations is that the mineral content
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