Ecologia mediterranea 1999-25(2)
Ecologia mediterranea 1999-25(2)
Ecologia mediterranea 1999-25(2)
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Abd EI-Ghani Soil variables affecting the vegetation ofinland western desert ofEgvpt<br />
each), Zygophyllaceae (11.7%), Caryophyllaceae,<br />
Compositae and Leguminosae (10.0% each), while the<br />
other 14 families share 31.7%. Chamaephytes are the<br />
most abundant life form and constituted 40.0% of the<br />
total flora of the study area, followed by therophytes<br />
(33.3%), hemicryptophytes (15.0%) and phanero<br />
phytes (11.7%). The most common perennials re<br />
corded were: Prosopis farcta, Tamarix nilotica,<br />
Fagonia arabica, Zygophyllum coccineum, Salsola<br />
imbricata subsp. imbicata, Cornulaca monacantha,<br />
Alhagi graecorum, Atriplex leucoclada, Randonia af<br />
ricana, Deverra tortuosa and Capparis spinosa var.<br />
aegyptia may be considered as leading dominants and<br />
characteristic species. Each of these species attains a<br />
maximum importance value (IV) of more than 140<br />
(out of 300 for all species in a stand), and a mean of<br />
more than 60. Common but less important perennials<br />
are Phoenix dactylifera, Pulicaria crispa, Anabasis<br />
articulata, Zilla spinosa subsp. spinosa, Stipagrostis<br />
plumosa and Pulicaria incisa. Common annuals in<br />
clude: Trigonella stellata, Zygophyllum simplex, Co<br />
tula cinerea, Eremobium aegyptiacum, Schouwia<br />
thebaica and Paronychia arabica subsp. arabica.<br />
The 144 stands were classified into eight vegeta<br />
tion groups according to TWINSPAN technique (Fig<br />
ure 2). The first level of the dendrogram separates all<br />
the stands into two main groups. The first group com<br />
prises 57 stands found mainly in the northern transect,<br />
and the second comprises 87 stands sampled from<br />
both transects. Table 3 summarises the mean values<br />
and the standard deviations of the measured soil vari<br />
ables in the eight groups derived from TWINSPAN.<br />
Generally, pH shows the least variation among<br />
groups. It can also be noted that whereas levels of<br />
lime and fine materials attain their highest values in<br />
the groups of the northern transect, the organic matter<br />
content reaches its highest levels in those of the south<br />
ern transect.<br />
The identified vegetation groups are named after<br />
the characteristic species as follows: Prosopis farcta<br />
Tamarix nilotica (lower part of the southern transect<br />
in the vicinity of the lowlands of Dakhla Oasis);<br />
Tamarix nilotica-Alhagi graecorum (southern tran<br />
sect, high salinity levels favour the growth of some<br />
halophytic species, e.g. Nitraria retusa and Zygo<br />
phyllum album); Zygophyllum coccineum-Salsola imbricata<br />
subsp. imbricata (in runnels and depressions<br />
of the southern transect); Cornulaca monacantha<br />
Fagonia arabica (larger catchment areas of the north-<br />
178<br />
ern transect, some species of this group do not pene<br />
trate into other groups of the southern transect);<br />
Atriplex leucoclada (lower part of the northern tran<br />
sect); Randonia africana-Deverra tortuosa (the silty<br />
runnels, and occupying a distance of about 20 km of<br />
the middle part of the northern transect); Deverra<br />
tortuosa-Capparis spinosa var. aegyptia (occupying a<br />
distance of about 30 km in the upper stretches of the<br />
middle part of the northern transect); Capparis spi<br />
nosa var. aegyptia-Zilla spinosa subsp. biparmata (in<br />
the low depressions between km 185 and km 198<br />
along the lower part of the northern transect).<br />
The four DCA axes explain 11.7%, 7.0%, 5.3%<br />
and 3.4% of the total variation in the species data, re<br />
spectively. This low percentage of variance explained<br />
by the axes is attributed to the many zero values in the<br />
vegetation data set. Table 4 shows that the eigenvalue<br />
for the first DCA axis was high indicating that it cap<br />
tured the greater proportion of the variation in species<br />
composition among stands, but the species<br />
environment correlation coefficients were low for<br />
DCA axes.<br />
DCA ordination of the perennial species (Figure 3)<br />
shows that species with high positive scores on axis I<br />
are found mainly in stands of the southern transect,<br />
and ordinated close to the right end-point: Prosopis<br />
farcta, Phoenix dactylifera, Nitraria retusa, Sarcocor<br />
nia fruticosa and Imperata cylindrica. The species po<br />
sitioned on the other end of this axis include:<br />
Capparis spinosa var. aegyptia (negative end), De<br />
verra tortuosa, Randonia africana, Ephedra alata and<br />
Helianthemum lippii. These and many other species<br />
are commonly found in the upper and middle parts of<br />
the northern transect. In the centre of axis I there are<br />
many species found throughout the investigated area<br />
with no preference to any geographical aspect (e.g.<br />
Zygophyllum coccineum, Tamarix nilotica, Alhagi<br />
graecorum, Fagonia arabica and Cornulaca monacantha).<br />
Along axis 2, species with high positive<br />
scores include: Atriplex leucoclada and Zilla spinosa<br />
subsp. biparmata. These species are recorded from the<br />
lower part of the northern transect, whereas species on<br />
the other end are of common occurrence in the middle<br />
and upper parts. To compare the classification and<br />
DCA ordination results, the recognised eight<br />
TWINSPAN groups are superimposed. Significance<br />
correlations of soil variables with the first four DCA<br />
axes (results not shown) revealed greater correlations<br />
along axis I than the higher order axes.<br />
ecalogia <strong>mediterranea</strong> <strong>25</strong> (2) - <strong>1999</strong>