VEGETATION OF THE BISKRA REGION.

A glance over the list of plants which grow naturally in the vicinity

of Biskra[30] shows that many are the same as occur farther south,

with many unlike these, having affinities outside of the desert

proper; also, the number of plants as well as species is greater at

Biskra than farther south. This would be expected from the greater

rainfall and more diverse topography.

The flora of the Biskra oasis, according to the authors referred to

above, consists of 175 or more species. Of cultivated plants there

are 25 or more species, the most conspicuous being the date. The

other species are mostly the same as have already been noted at

other Algerian oases, except that both the peach and the apricot

are wanting at Biskra, although cultivated at Laghouat, Ghardaia,

etc. On the outskirts of the town the fairly extensive flood-plain is

given over mainly to the cultivation of grain, barley predominating.

The hills and mountains, and the bajada at their base, as well as

certain oueds with water relations, exposure, and soils different

from those of the oasis, have also a very different flora, which, for

the most part, is desertic in character. For purposes of comparison,

some of the leading characteristics of the plants growing in a

half-dozen localities will be given.

As stated above, to the southwest of Biskra there runs a range

of hills, Ed Delouatt, to the south and the north of which may be

found interesting plants and plant conditions. On the south side

the slope (bajada) descends gradually to the great reg, and near

the base of the range, in the vicinity of the place where tradition

says a Roman town formerly existed, there is a wide, sandy plain,

reaching from the Oued Melah, which pierces Ed Delouatt hills,

nearly or quite to the western extension of the oasis. There are

no large dunes here, but sand billows about a meter in height and

sand hillocks diminutive in size. Between these the plain is fairly

level. Over this whole tract there seemed to be only one species

(_Euphorbia guyoniana_), but this was fairly abundant. (Fig. 65.) As

at Ghardaia and elsewhere, this species grows in small colonies

because of its suckering habit, and acts to a small degree as a

sand-binder, each group being situated on a sandy hillock. It will

be remembered that this species at Ghardaia, as well as at a certain

bordj east of that place, had roots which were somewhat fleshy as

well as roots which were fibrous, on one and the same plant. I was

interested to learn whether similar conditions should obtain at

Biskra, since it had been learned, in the case of two species of

_Opuntia_ in the Tucson region, that a different habit followed

certain differences in habitat. Several specimens of _Euphorbia_

were removed with care from the soil and in no case was it found

that the roots were fleshy, but in every instance they were entirely

fibrous. It is supposed that the reason for the variation in behavior

may possibly be traced to differences in the water relation, as

was found to be the case of the variation in cactus roots cited,

but no experiments have been made on _Euphorbia_ to prove this.[31]

There is a variety of habitats on the opposite (north) side of the

hills, ranging from the large dune (which reaches the summit to the

west of the pass through which the oued passes and which must be 100

to 150 meters above the oued) to the flood-plain, with water very

near the surface, during rainy season at least. There are rocky

slopes, also, and sandy slopes apart from the dunes referred to,

as well as a fine clay with sand admixture on the flood-plain. In

all of these habitats, except the large dune, the vegetation is

actually or relatively abundant. (See fig. 67.) Among the rocks

are small shrubs or half-shrubs, and also on the plain below. Here

one may find, among other species, _Echiochilon fruticosum_,

_Helianthemum_ sp., _Atractylis serratuloides_, _Gymnocarpos

fruticosum_, _Thymelæa microphylla_, _Nitraria tridentata_, and

_Acanthyllis tragacanthoides_. On the sandy slope was growing a very

numerous population of liliaceous forms, mainly, perhaps wholly,

_Asphodelus fistulosus_ (fig. 72).

It has been noted that the oued which pierces Ed Delouatt is made

up of the confluence of all of the small oueds lying between the

Bou Rhezal Mountains to the north of Biskra and the hills lying

directly north as well as those (Ed Delouatt) to the southwest. The

united oueds reach the base of the hills nearly 1 kilometer east

of the pass, and turning abruptly follow the base the remainder

of the distance. At the place where the oued touches the range

the soil is moist nearly to the surface of the plain (reg) and for

several meters back from the oued. Here, then, the water relations

of the plants are such as to favor, probably most of the year,

the growth of mesophytes (?) or even of hydrophytes, but for some

reason there is not much vegetation there; whether large species

have been removed as for fuel, have been destroyed by animals, or

never existed, was not learned. The most interesting plant found

was the well-known parasite _Phelypæa violacea_, which grows,

according to Mobius, on a salsolaceous host.[32] Only a few specimens

were seen at the time of the second visit to Biskra, in March,

and they were just appearing above the ground. (See figs. 69, 70,

and 71.) When removed from the soil the longest specimen was found

to have penetrated over 59 cm.; it was 6.5 cm. in diameter at a

point 50 cm. from the tip. The plants were exceedingly heavy, being

gorged with sap, and appeared to be able to absorb moisture from

the wet soil through the white and delicate epidermis of the entire

portion submerged. If this is the case the parasitical relation

is of especial interest, as the species is wholly dependent on its

host for organized foods, but not for water—a condition opposite

that found in such semi-parasites as the mistletoes, which obtain

water and unorganized foods in solution from the host, but which,

save for the fact of attachment, are otherwise independent of it.

To the northeast of Ed Delouatt hills and north of Biskra, but

immediately adjoining the town, is an irregular group of low,

rounded hills, mostly very arid, which support a scant vegetation

of typical desert plants. These hills, without a name, are eroded

to a degree and have shallow washes leading from them in every

direction. The soil appears to be thin, except in the washes, where

it has accumulated to the depth of a meter or more. On the rounded

summits it is rather fine, but in the washes there is much gravel

and larger stones. Here one finds the greatest range in exposure,

and probably also an accompanying difference in the temperature of

the air and soil.

In considering the vegetation of the hills it must be remembered

that no plants suitable for forage or large enough for fuel would be

left untouched, as the biotic factor is quite as much in evidence in

modifying the Biskra flora as that of the other regions visited. As

the plants are at present, however, and for whatever definitive

causes, there is a considerable variation in numbers and apparently

also in kinds. An examination of different parts of the hills

by which various exposures as well as other conditions are seen

bears out the hypothesis. On the southern slopes, particularly

the upper portions, the plant covering is especially poor. The

population of an area 16 by 16 meters in the upper south slope

included 134 perennials and numerous annuals. Of the species,

_Haloxylon scoparium_ was the most numerous; there were also

_Dæmia cordata_, _Thymelæa microphylla_, and _Fagonia sinaica_

(figs. 78 and 80). All of these species were small, so that from

superficial examination the area appeared fairly barren (fig. 73).

When one crosses the hills to the north, so that northern and

northwestern exposures are seen, a striking difference is immediately

apparent. The northern slopes are much richer in perennials than

the opposite facing. The population of an area of the size before

taken shows this observation to be correct. On a square 16 by 16

meters, with north exposure, 536 living perennials and numerous

annuals were found, with _Haloxylon scoparium_ again the dominant

species. The species second in number was _Ferula vesceritensis_,

which is to be found chiefly on the north exposure (figs. 74, 75,

and 77). There were also a few specimens of _Acanthyllis numidica_,

and many annuals, which, unlike those on the south facing, were

not in flower.

On the lower slopes, in the small and open gulches and the lower

portions of the washes and their flood-plains, the plants were most

numerous and include a variety of forms, with _Peganum harmala_

the most conspicuous and most numerous.

The roots of several species growing on the hills were studied

with the following as perhaps the leading results: The root-system

of _Haloxylon scoparium_, as has already been seen to be the case

with an allied species in the country of the M’Zab, may be said

to be a modification of the generalized type. One specimen, partly

exposed by erosion in a wash, had a tap-root over 113 cm. in length

(fig. 76). As this root was 4 mm. in diameter where left, and was

8 mm. in diameter at the crown, it may have penetrated much beyond

the point where it was left, provided the soil conditions continued

favorable. The main root gave off two large laterals, of which one

left the parent root 8 cm. and the other 18 cm. beneath the surface

of the ground, but there were also numerous filamentous roots about

2 cm. in length, which were borne in tufts. (See fig. 79.) These

resembled the deciduous rootlets found on many perennials in the

Tucson region and doubtless function quite as they, namely, they

are organized at the beginning of the rainy season, operate to

increase the water-absorbing area of the plant quickly and greatly,

and die as soon as unbearably arid conditions set in.

In the same wash, where the soil was deep with an admixture of

small stones and pebbles, the roots of other species were also

examined. One of these was _Peganum harmala_, whose roots were

examined at Ghardaia. The root-systems of the plant in the two

regions were similar in being generalized. A main root was found

extending downward over 61 cm. and it gave off three good-sized

laterals, arising from 15 to 27 cm. beneath the surface. The

uppermost lateral took a horizontal course. Figure 82 gives a fairly

good idea of the general character of the root-system of the species.

There were many specimens of _Plantago albicans_ growing in the

same habitat as _Haloxylon_ and _Peganum_. Its root-system was

also studied with the following results: The tap-root is strongly

developed. In one instance the slender main root was found to go

straight down over 71 cm. Numerous laterals were borne between 8

and 20 cm. beneath the surface of the ground. The species has an

interesting habit of propagating vegetatively by means of fleshy

stolons. An examination of the stolons showed them to be of very

unequal age, some having been lately formed, while others had been

organized in previous years and were no longer living. Many specimens

were examined to learn the probable service of the fleshiness of its

stolons, and the conclusion was that this factor probably enables

the species to pass over periods of excessive drought.

Running across country are the Bou Rhezal Mountains, of which

the north and south faces were examined in one or two places, on

each side somewhat in detail. The south face is precipitous and

has little vegetation, but there are many plants on the opposite

face, especially near the base, where the soil conditions are

relatively favorable (fig. 84). Among the perennials were found a

few specimens of _Rhus oxyacantha_ and _Zizyphus lotus_, which,

although dwarfed, were the largest plants seen away from the

oasis, being about 1.5 meters high. In another gulch were found the

following species: _Acanthyllis tragacanthoides_, _Dæmia cordata_,

_Ferula vesceritensis_, _Haloxylon scoparium_, and other plants

unknown. Toward the upper portions of the gulches _Haloxylon_ was

seen to be especially abundant, but in the bed of the washes and on

their flood-plains _Peganum_ grows in large numbers (fig. 83). In

the most favorable places on the northern slope in March the annuals

were the most abundant observed in the vicinity of Biskra, although

even there they failed to completely conceal the ground. Where the

situation was less favorable as regards soil and water conditions

(for example, on the side of the gulches, on the summit of ridges,

and the like) there were almost no annuals and those present were

relatively small.

In this brief account of some of the most striking features of

the Biskra flora it should be noted that several habitats are

omitted as not being pertinent to the points in view. Especially,

nothing has been said regarding the flora of the salt flats along

the Oued el Hamman or that of the dunes, since the influences here

are largely edaphic, while the present interest lies mainly in the

relation between plants and climate; and the flora of the oasis

has been largely neglected for similar reasons.

Not only is there in certain regards a larger number of plants

in the Biskra region than had been previously seen in southern

Algeria, but there are certain types, mostly new, which point to

more favorable conditions of plant life. These are such forms as

have a water-storage habit, like _Asphodelus_, _Ferula_, _Plantago_,

and _Phelypæa_, which, although not wholly absent farther south,

appear to be much more numerous near Biskra. The presence of bulbous

plants is well known as being one of the floral characteristics

of the High Plateau, and it is also known that similar forms are

not to be found where the arid conditions are the most severe,

which probably accounts for the facts noted. It may be pointed

out also that plants at Biskra exhibit exposure preference where

soil conditions appear to be parallel. This condition is not so

marked farther in the desert as at Ghardaia, for example, where,

provided there is sufficient depth of soil, apparently any species

may be found on any exposure. In other words, exposure preference

implies a certain amount of water as well as sufficient soil.

So far as shown by observations of the root-systems carried out on

similar species growing in the Biskra region and at Ghardaia, the

essential root characters of plants growing in the two regions are

the same. The single exception to this so far noted is that of the

roots of _Euphorbia guyoniana_, which, contrary to the expectation,

are apparently wholly fibrous at Biskra, although they are in

part fleshy farther south, where the soil conditions are surely

more arid. At Biskra, also, the only plant observed with typical

generalized root-systems (_Peganum_) does not grow where the soil is

shallowest, but where it is relatively deep. So far as seen, also,

plants growing where the soil is shallow have either a generalized

root-system or a root-system approaching this type, even if the

branching is only relatively deep.

=GENERAL SUMMARY AND CONCLUSIONS.=

Botanical features of the Algerian Sahara · 第 77 / 87 题