Source: Litter decomposition, climate, and litter quality. Link. |
Nutrients: Mn and N
Manganese and Nitrogen control forest decomposition, but in an unexpected way. Mn is an
essential component of ligninolytic enzymes important for degrading litter in
the later stages of decomposition. But high available N can limit decomposition. The most
efficient degraders of lignin and humic acids are wood-rotting or
litter-decomposing white-rot fungi (Hintikka 1970; Hatakka 2001). For several of the lignin-degrading white-rot fungi, high
concentrations of low-molecular weight N compounds suppress the synthesis of
the lignin-degrading enzymes (Keyser et al. 1978; Eriksson et al. 1990;
Carreiro et al. 2000).
Further, N has repeatedly been reported to react with
remains of degrading lignin to form recalcitrant condensation products. Such
products form chemically (Vahtras 1982; Stevenson 1982) rather than biologically. Spaccini (1999) suggested that such bonds
create a hydrophobic surface thereby resisting decomposition. The higher the
concentrations of lignin and N in a litter material the more likely it seems
that such covalent bonds will be formed. Using 106 sets of foliar litter
comprising 21 tree species (both coniferous and deciduous) representing a wide
range in chemical composition, Berg (2000) found a highly significant negative
relationship between limit values and initial N concentrations in litter.
Many examples exist in which addition of N to a N-deficient
system slows down decomposition, especially where organic matter with high
lignin content is present (Verhoef and Brussaard, 1990; Carreiro et al., 2000).
Nitrogen and other fertilizers may negatively influence specific groups of
organisms, particularly microbes. Any
shift in microbial composition can have a negative effect on other soil fauna. As a result, decomposition and mineralization
may decrease. Additionally, plants can compete successfully with decomposers
for nutrients. (Neher 2003.)
What about pH?
In a review of 58 studies, Wardle (1998) found that temporal variability in soil carbon (C) was related most closely to soil N content in forests and soil pH in arable and grassland ecosystems. (Neher 2003.)
But a study by Parn et al adding ash to a pine forest to
increase soil pH did not observe increased decomposition. A large meta-review noted that 22-85% of
treatment trials have failed to affect decomposition: “This analysis shows that
Ca additions are not universally beneficial and provides insight into when Ca
additions to forest soils are likely to be most effective." (Evaluating the
effects of liming and wood-ash treatment on forest ecosystems through
systematic meta-analysis. Carolyn Reid, Shaun A. Watmough)
Decomposition Rate and Ecosystem Integrity
This WSU website has a great review of pine forest decomposition.
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