1984
DOI: 10.2307/3673165
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Stability and Instability of Ecological Systems in New Zealand Mountains

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Cited by 15 publications
(8 citation statements)
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“…The seven treeline types, emerging from the cluster analysis of treeline metrics, aggregate into reasonably well-demarcated regions when mapped back onto the 230 landscape zones across the country. The biogeographic patterning of the seven treeline ecotypes appear to coincide, by and large, with known regional differences among New Zealand's mountain systems (Wardle, 1991;O'Connor, 1984), and their associated Nothofagus forest patterns (Wardle, 1984). This implies a strong spatial structuring of treeline features by abiotic mechanisms that relate, in turn, to strong geographic variation in mountain geology, geomorphology and climate.…”
Section: Discussionmentioning
confidence: 74%
“…The seven treeline types, emerging from the cluster analysis of treeline metrics, aggregate into reasonably well-demarcated regions when mapped back onto the 230 landscape zones across the country. The biogeographic patterning of the seven treeline ecotypes appear to coincide, by and large, with known regional differences among New Zealand's mountain systems (Wardle, 1991;O'Connor, 1984), and their associated Nothofagus forest patterns (Wardle, 1984). This implies a strong spatial structuring of treeline features by abiotic mechanisms that relate, in turn, to strong geographic variation in mountain geology, geomorphology and climate.…”
Section: Discussionmentioning
confidence: 74%
“…Para superar el desequilibrio estacional de pastos se ha deforestado, aún se sigue haciendo, y abriendo claros en masas forestales de no pocas montañas de la Tierra (Mallet, 1978;Bencherifa, 1983;Metailié, 1984;O'Connor, 1984;Tucker, 1987;Mahat et al, 1987). Hay que recordar que el bosque tiene un reciclado lento, estabilizador, mientras que el pasto permite mantener una biomasa animal muy superior al acelerar los ciclos (Montserrat, 1972).…”
Section: Recursos Pascícolas Y Estrategias De Pastoreounclassified
“…Soils age rapidly in the wet climate. Recent soils probably develop through to gleyed or podzolised yellow-brown earths in 1000-2000 years, therefore well-developed soils are unlikely on landforms subject to continual intense erosion or deposition (Archer 1973;Williams et al 1976Williams et al ,1978O'Connor 1980O'Connor , 1984Basher et al 1985).…”
Section: Discussionmentioning
confidence: 99%
“…Within the broad regional patterns (Mark 1969), the distribution of these grasses is largely related to complex gradients in soil nutrient status and climate. Soil nutrient status reflects parent material fertility (e.g., Bell 1973) and the stage of soil development, which is largely dependent on surface stability and surface age (e.g., Williams 1975;Williams et al 1976;O'Connor 1980O'Connor , 1984Sommerville etal. 1982;Basher etal.…”
Section: Introductionmentioning
confidence: 99%