Soil organic carbon and nutrient status in old-growth montane coniferous forest watersheds, Isla Chiloe, Chile
Montane temperate forests of the Cordillera de Piuchué Ecosystem Study, Isla Chiloé, Chile, are unaffected by air pollution, timber exploitation and agricultural clearing, and the current floristic assemblage has been relatively stable for the past 7500 years. The apparent absence of major perturbat...
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Veröffentlicht in: | Plant and soil 1998-04, Vol.201 (2), p.251-258 |
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Zusammenfassung: | Montane temperate forests of the Cordillera de Piuchué Ecosystem Study, Isla Chiloé, Chile, are unaffected by air pollution, timber exploitation and agricultural clearing, and the current floristic assemblage has been relatively stable for the past 7500 years. The apparent absence of major perturbation at this location makes it an appropriate baseline site for ecosystem analysis. We measured soil bulk density, pH, soil organic C (SOC), total N, and NH₄Cl-exchangeable cations (Ca⁺², Mg⁺², K⁺, Na⁺, Al⁺³) in 0-10 and 10-40 cm depth samples from 72 soil profiles representing three vegetation zones: Fitzroya cupressoides Forest, Pilgerodendron uvifera-Tepualia stipularis Forest, and Magellanic Moorland. Fitzroya and Pilgerodendron-Tepualia Forests were indistinguishable for all measured soil characteristics (P > 0.05, Dunn's multiple comparison test on ranked data); these included very high median SOC concentrations (0-10 cm = 49.6%) and correspondingly low bulk density values (0-10 cm = 0.07). Moorland soil median values (0-10 cm) were significantly higher for bulk density (0.12) and lower for SOC (28.5%), but not for total N (Forests = 0.99%, Moorland = 0.95%), resulting in lower median C: N ratios for the moorland (Forests = 44.7; Moorland = 30.3). Across both depths and all three vegetation zones regression analysis indicated that SOC was an excellent predictor (R²= 0.93, P < 0.001) of ∑ (exchangeable Ca⁺² + Mg⁺² + K⁺ + Na⁺).Comparison with other old growth montane environments indicates that the Fitzroya and Pilgerodendron-Tepualia soil profiles are characterized by C:N ratios typical of other relatively unpolluted conifer forest soils (33.0-49.3). Soil profiles of representative polluted montane conifer forests have lower C:N ratios (16.2-23.5).Organic horizons from representative polluted montane conifer forests also retain fewer exchangeable base cations per unit SOC than are retained by organic horizons from the Cordillera de Piuchué forests. |
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ISSN: | 0032-079X 1573-5036 |
DOI: | 10.1023/A:1004375920790 |