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. 2007 Jan 4;99(2):333–343. doi: 10.1093/aob/mcl263

Table 3.

Gaussian models for the two gypsovags occurring in gypsum and calcareous soils at both sites. The P-value of the corresponding analysis of deviance and the mean value of each variable in each class are indicated

Variable Salvia lavandulifolia
Rosmarinus officinalis
Gy/Caa Siteb Interaction termc Gy/Caa Siteb Interaction termc
Ash 0·037 ns ns 0·007 ns ns
Ca = 6·36; Gy = 7·23 Ca = 5·43; Gy = 6·04
Ca 0·001 ns ns 0·019 ns 0·020
Ca = 1·50; Gy = 1·94 Ca = 1·20; Gy = 1·43 Z-Ca = 1·17; Z-Gy = 1·64; M-Ca = 1·22; M-Gy = 1·22
C 0·001 0·001 ns 0·032 ns 0·011
Ca = 56·37; Gy = 54·94 Z = 54·7; M = 56·6 Ca = 56·35; Gy = 55·96 Z-Ca = 56·21; Z-Gy = 56·30; M-Ca = 56·49; M-Gy = 55·62
C/N 0·0001 ns ns ns ns ns
Ca = 37·53; Gy = 31·31
Mg 0·003 0·003 0·003 0·001 ns ns
Ca = 3·03; Gy = 3·28 Z = 2·34; M = 3·97 Z-Ca = 3·04; Z-Gy = 1·64; M-Ca = 3·01; M-Gy = 4·92 Ca = 1·69; Gy = 2·77
N 0·0001 ns ns ns ns ns
Ca = 15·08; Gy = 17·64
Na ns 0·0001 ns ns ns ns
Z = 0·52; M = 0·35
P 0·006 0·003 0·003 0·004 ns ns
Ca = 0·85; Gy = 1·03 Z = 1·03; M = 0·85 Z-Ca = 0·85; Z-Gy = 1·21; M-Ca = 0·85; M-Gy = 0·84 Ca = 0·85; Gy = 0·68
K ns 0·005 ns 0·017 ns ns
Z = 6·80; M = 4·22 Ca = 10·04; Gy = 8·05
S 0·001 ns ns ns ns ns
Ca = 0·05; Gy = 0·11

aCa = calcareous soil, Gy = gypsum soil.

bM = Madrid (central Spain, Middle Tajo Basin); Z = Zaragoza (north-east Spain, Middle Ebro Basin).

cZ-Ca = calcareous soils in Zaragoza; Z-Gy = gypsum soils in Zaragoza; Ca-M = calcareous soils in Madrid; Gy-M = gypsum soils in Madrid.

ns indicates that predictors do not explain a significant fraction of deviance. See text for details on statistics. n = 5.