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species in all soils, but is highest in the south. Increasing b5ca/b6ca ratios to
the north indicate a decreasing degree of condensation.
The profile pattern of
15 N (Fig. 4.14.4) contrasts with
the chemical analysis of SOM, if only aerobic decomposition processes are
δ
13 C and
δ
Fig. 4.14.3. Composition of SOM in soils of the forest tundra, northern taiga and central taiga
with respect to lignin-derived phenols, microbial-derived amino sugars and pyrogenic C (for details,
see Methods).
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