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Patterns of biological nitrogen fixation during 60 000 years of forest development on volcanic soils from south central Chile

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Academic year: 2020

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Figure

Table 1. Site codes and substrate ages (after Naranjo & Moreno 2005) for the different ecosystem developmental stages  (numbered 1 to 7, column 2) in the Llaima volcano chronosequence
Figure 2. Changes in basal area of woody  species  present  in  the  seven  ecosystem  developmental stages in the 60 000-year  successional  chronosequence  of  Llaima  volcano in Conguillío National Park, Chile
Figure 3. Tree basal area and total element concentrations of seven  ecosystem developmental stages in the 60 000-year successional  chronosequence of Llaima volcano in Conguillío National Park,  Chile: (a) tree basal area, (b) soil carbon, (c) soil nitrog
Figure 4. (a) Annual rates of BNF (all N-fixing community types) across all the developmental stages (1 to 7) in the chronosequence
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