Registro Completo |
Biblioteca(s): |
Embrapa Pantanal. |
Data corrente: |
24/05/1996 |
Data da última atualização: |
27/05/1996 |
Autoria: |
PRENTICE, I. C. |
Título: |
Vegetation analysis and order invariant gradient models. |
Ano de publicação: |
1980 |
Fonte/Imprenta: |
Vegetatio, v.42, n.1/3, p.27-34, Oct.1980. |
Idioma: |
Inglês |
Conteúdo: |
An ideal ordination method would have known properties with respect to an explicit, order invariant ecological response model defined in more than one dimension. The Curtis- McIntosh model (each species weakly unimodal) is a good general-purpose model of a single gradient, but no current method is guaranteed to dispose samples from such a gradient along a straight line. There is some theoretical justification for using reciprocal averaging (RA), or local non-metric multidimensional scaling (NMDS) with Kendall's simple similarity coefficient, but the former tends to produce arches rather than straight lines and the latter can produce erratic curves (as illustrated here by applying the method to simulated coenocline data). The non-metric method is nevertheless shown to perform well (a) with high beta- diversity plant distribution data and (b) with simulated coenoplane data, where its performance is better than that of RA. Results with coenoclines and coenoplanes concur with those of Fasham (1977) who tested NMDS with a different coefficient. Local scaling is shown to be preferable to global, and primary tie treatment to secondary, in tests on coenocline and coenoplane data. A possible alternative non-metric approach is mentioned. |
Palavras-Chave: |
Analise de vegetacao; Gradient model; Gradient models; Modelo de gradiente; Order invariant; Vegetation analysis. |
Thesagro: |
Análise; Vegetação. |
Categoria do assunto: |
-- |
Marc: |
LEADER 01828naa a2200217 a 4500 001 1788681 005 1996-05-27 008 1980 bl --- 0-- u #d 100 1 $aPRENTICE, I. C. 245 $aVegetation analysis and order invariant gradient models. 260 $c1980 520 $aAn ideal ordination method would have known properties with respect to an explicit, order invariant ecological response model defined in more than one dimension. The Curtis- McIntosh model (each species weakly unimodal) is a good general-purpose model of a single gradient, but no current method is guaranteed to dispose samples from such a gradient along a straight line. There is some theoretical justification for using reciprocal averaging (RA), or local non-metric multidimensional scaling (NMDS) with Kendall's simple similarity coefficient, but the former tends to produce arches rather than straight lines and the latter can produce erratic curves (as illustrated here by applying the method to simulated coenocline data). The non-metric method is nevertheless shown to perform well (a) with high beta- diversity plant distribution data and (b) with simulated coenoplane data, where its performance is better than that of RA. Results with coenoclines and coenoplanes concur with those of Fasham (1977) who tested NMDS with a different coefficient. Local scaling is shown to be preferable to global, and primary tie treatment to secondary, in tests on coenocline and coenoplane data. A possible alternative non-metric approach is mentioned. 650 $aAnálise 650 $aVegetação 653 $aAnalise de vegetacao 653 $aGradient model 653 $aGradient models 653 $aModelo de gradiente 653 $aOrder invariant 653 $aVegetation analysis 773 $tVegetatio$gv.42, n.1/3, p.27-34, Oct.1980.
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Embrapa Pantanal (CPAP) |
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