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Sakari Tuhkanen (1980)
Climatic parameters and indices in plant geography
R. Develice, W. Burke (1989)
Gradient analysis of forest vegetation in the Maungataniwha Range, western Northland, New ZealandNew Zealand Journal of Botany, 27
C. Thornthwaite, J. Mather (1954)
Climate in Relation to Crops
G. Jane, T. Green (1986)
Etiology of forest dieback areas within the Kaimai Range, North Island, New ZealandNew Zealand Journal of Botany, 24
Rogers Rogers (1989)
Beech and conifer community interactions in Moawhango Ecological Region, North Island, New ZealandN. Z. J. Ecol., 12
P. Haase (1990)
Environmental and floristic gradients in Westland, New Zealand, and the discontinuous distribution of Nothofagus.New Zealand Journal of Botany, 28
P. Froggatt, D. Lowe (1990)
A review of late Quaternary silicic and some other tephra formations from New Zealand: Their stratigraphy, nomenclature, distribution, volume, and ageNew Zealand Journal of Geology and Geophysics, 33
J. Huisman, H. Olff, L. Fresco (1993)
A hierarchical set of models for species response analysisJournal of Vegetation Science, 4
J. Leathwick, N. Mitchell (1992)
Forest pattern, climate and vulcanism in central North Island, New ZealandJournal of Vegetation Science, 3
T. Yee, N. Mitchell (1991)
Generalized additive models in plant ecologyJournal of Vegetation Science, 2
G. Glasby (1991)
A review of the concept of sustainable management as applied to New ZealandJournal of The Royal Society of New Zealand, 21
P. Wardle (1986)
Frequency of cloud cover on New Zealand mountains in relation to subalpine vegetationNew Zealand Journal of Botany, 24
J. Lenihan (1993)
Ecological response surfaces for North American boreal tree species and their use in forest classificationJournal of Vegetation Science, 4
R. Allen, A. Reif, G. Hall (1991)
Elevational distribution of conifer‐broadleaved hardwood forests on South Island, New ZealandJournal of Vegetation Science, 2
N. Mitchell (1991)
The derivation of climate surfaces for New Zealand, and their application to the bioclimatic analysis of the distribution of kauri (Agathis australis)Journal of The Royal Society of New Zealand, 21
Sowell Sowell (1985)
A predictive model relating North American plant formations and climateVegetatio, 60
Zotov Zotov (1938)
Some correlations between vegetation and climate in New ZealandN. Z. J. Sci. Tech., 19
F. Woodward, A. Diament (1991)
Functional Approaches to Predicting the Ecological Effects of Global ChangeFunctional Ecology, 5
P. Froggatt (1981)
Stratigraphy and nature of Taupo Pumice FormationNew Zealand Journal of Geology and Geophysics, 24
H. Connor, E. Edgar (1987)
Name changes in the indigenous New Zealand flora, 1960–1986 and Nomina Nova IV, 1983–1986New Zealand Journal of Botany, 25
M. McGlone, W. Topping (1977)
Aranuian (post-glacial) pollen diagrams from the Tongariro region, North Island, New ZealandNew Zealand Journal of Botany, 15
Thompson Thompson (1946)
Design for a forest surveyN. Z. J. For., 5
I. Prentice, W. Cramer, S. Harrison, R. Leemans, R. Monserud, A. Solomon (1992)
A global biome model based on plant physiology and dominance, soil properties and climateJournal of Biogeography, 19
C. Braak (1986)
Canonical Correspondence Analysis: A New Eigenvector Technique for Multivariate Direct Gradient AnalysisEcology, 67
P. Wardle (1985)
New Zealand timberlines. 3. A synthesisNew Zealand Journal of Botany, 23
P. Wardle (1964)
Facets of the distribution of forest vegetation in New ZealandNew Zealand Journal of Botany, 2
B. Huntley (1990)
European post‐glacial forests: compositional changes in response to climatic changeJournal of Vegetation Science, 1
W. Bond (1989)
The tortoise and the hare: ecology of angiosperm dominance and gymnosperm persistenceBiological Journal of The Linnean Society, 36
Austin Austin, Smith Smith (1989)
A new model for the continuum conceptVegetatio, 83
M. Austin, A. Nicholls, M. Doherty, Jacqui Meyers (1994)
Determining species response functions to an environmental gradient by means of a β‐functionJournal of Vegetation Science, 5
W. Steffen, B. Walker, J. Ingram, G. Koch (1992)
Global change and terrestrial ecosystems. The operational plan.No source information available
M. McGlone (1983)
Holocene pollen diagrams, Lake Rotorua, North Island, New ZealandJournal of The Royal Society of New Zealand, 13
P. Wardle (1963)
Evolution and distribution of the New Zealand flora, as affected by quaternary climatesNew Zealand Journal of Botany, 1
M. Austin, A. Nicholls, C. Margules (1990)
Measurement of the realized qualitative niche: environmental niches of five Eucalyptus speciesEcological Monographs, 60
Connor Connor, Edgar Edgar (1987)
Name changes in the indigenous New Zealand flora, 1960‐1986 and nomina nova IVN. Z. J. Bot., 25
Abstract. A dataset of some 10 000 plots was used to describe the climatic relationships of 33 widespread New Zealand tree species. Estimates of mean annual temperature, temperature seasonality, mean annual solar radiation, and moisture balance were derived from mathematical surfaces fitted to climate station data. Plots were also categorized into five lithological classes and three drainage classes. Generalized additive models were used to examine species/environment relationships. Mean annual temperature and mean annual solar radiation are most strongly correlated with current tree distributions, followed by moisture balance, temperature seasonality, lithology, and drainage. Most broad‐leaved tree species other than Nothofagus spp. reach their greatest levels of occurrence in warm, moist environments with high solar radiation. In contrast, Nothofagus spp. generally reach their greatest levels of occurrence in cooler and/or lower insolation environments, and all have lower levels of occurrence on rhyolitic substrates which have resulted from large‐scale geomorphic disturbance, mostly over the past few thousand years. Although coniferous species have widely differing climatic optima, many are biased towards lithological classes characterized either by large‐scale geomorphic disturbance or harsh edaphic conditions. The relevance of these results to particular synecological questions is briefly discussed. Continuing adjustments in the range of slow‐dispersing Nothofagus spp. are strongly suggested, and the climatic suitability of extensive rhyolitic basins in the central North Island, from which these species are largely absent, is confirmed.
Journal of Vegetation Science – Wiley
Published: Apr 1, 1995
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