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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>

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