Non-traditional Fodders from the Halophytic Vegetation of the Deltaic Mediterranean Coastal Desert, Egypt
Mahmoud A. Zahran
Yasser A. El-Amier
The Deltaic Mediterranean coastal desert extends for about 180 km from Abu Qir westward to Port Said. The soil of this coastal belt is generally salt-affected vegetated with different plant communities recognized into zones dominated mainly by halophytes e.g., Arthrocnemum macrostachyum, Halocnemum strobilaceum, Limbarda crithmoides, Aeluropus brevifolius, Sporobolus spicatus, Limoniastrum monopetalum, Zygophyllum aegyptium, Limonium pruinosum, Cressa cretica, Tamarix tetragyna and Bassia indica etc. However, in the sand dune habitat psammophytes predominate e.g., Elymus farctus, Lotus polyphyllos and Thymelaea hirsuta. In the non-saline soil of the most landward zone, non-salt tolerant species predominate e.g., Lygos raetam, Lycium europaeum etc. For the present paper six halophytes have been selected and chemically analysed to determine their nutritive values as fodder producing plants, these are: Arthrocnemum macrostachyum, Halocnemum strobilaceum, Limoniastrum monopetalum, Tamarix tetragyna, Cressa cretica and Bassia indica. The latest species is the only palatable plant, the other five species are not palatable but their vegetative yields may be considered as the main part of the raw materials for fodder production. The results, so far, are promising all studied plants are rich with their carbohydrates and protein contents. The establishment of Bassia indica in the salt affected land of the study area had been successively experimented.
Received: March 08, 2013;
Accepted: March 27, 2013;
Published: July 10, 2013
In Egypt, low meat production is one of the major food problems which is often
exacerbated by the increasing demands due to increasing population. The production
of conventional fodders (alfalfa and clover) is not enough (Zahran
et al., 1999). On the other hand, the natural vegetation of Egypts
deserts comprises considerable number of palatable species and/or species rich
with their nutritive values that may be considered reliable natural resources
for fodder production if their vegetative yields are high enough to maintain
a continuous fodder supply (Zahran and Willis, 2009).
Unfortunately, this cannot be secured in Egypts desert where rainfall
is, generally, scarce and the vegetative yields of these fodder producing plants
are not high enough to meat the requirements of the needed livestock. Apart
from that, it will not be possible to find pure natural vegetation of plants
with high nutritive values only. Usually, unwanted and/or harmful species also
occur in the same area. Thus, the best solution is to widen the desert areas
occupied by the fodder producing plants by propagating them under aridity (drought)
and/or salinity stress of the deserts. Water requirements of these plants are
very small (xerophytes), some of them could be grown with saline water or even
with sea water directly (halophytes).
In Egypts deserts the frequency of the salt affected lands makes their
utilization necessary. This could be achieved by vegetating these lands with
salt tolerant plants of economic values. That is the aim of the present paper.
Six halophytes naturally growing in the deltaic Mediterranean coastal desert
of Egypt had been studied ecologically and their nutritive values as fodder
producing plants were determined shown in Table 2. These plants
are: Arthrocnemum macrostachyum, Halocnemum strobilaceum, Limoniastrum
monopetalum, Tamarix tetragyna, Cressa cretica and Bassia
indica. The establishment of Bassia indica was also experimented
in a salt affected land of the deltaic Mediterranean coast.
MATERIALS AND METHODS
Physiography: The Mediterranean coastal desert of Egypt extends from
Sallum (Libyan border) eastward to Rafah (Palestine border) for about 970 km.
It is the narrow less arid desert of Egypt influenced greatly by the sea.
|| Map of the Nile Delta region showing the study area indicated
It is divided ecologically into three sections: western, middle and eastern.
The western section, the northern coast of the Western Desert (Mariut Coast)
extends from Sallum to Abu Qir for about 550 km, the middle sections (the Deltaic
Coast) runs from Abu Qir to Port Said for about 180 km and the eastern section
(Sinai northern Coast) stretches from Port Said to Rafah for about 240 km (Fig.
The deltaic Mediterranean coast has a width from sea landward (southwards)
for about 15 km. It is characterizied by 3 shallow natural lakes: Manzala (in
the east), Burullus (in the middle) and Idku (in the west). These lakes are
receiving the main bulk of the drainage water from the Nile Delta lands.
The climate of the whole stretch of the Mediterranean coastal desert is, generally,
less arid than the remaining southern parts of Egypt. According to the Bioclimatic
Map of UNESCO/FAO (1963), it belongs to the subdesertic
warm climate. In the deltaic Mediterranean section annual rainfall ranges between
160 mm in Rosetta and 102.3 mm in Damietta. Maximum air temperature in both
coastal cities ranges between 18.1 and 30.2°C and 18.4 and 31.3°C whereas
minimum temperatures range between 11.3, 23, 8.2 and 21.5°C in January and
July respectively. Relative humidity does not vary widely between the two cities
being 76, 74, 83 and 75% in January and July, respectively (Zahran
and Willis, 2009).
Habitats and vegetation types: The deltaic Mediterranean coast, being
directly affected by sea water, is generally, salt affected land divided ecologically
into four main habitats in a landward zonation pattern. The extent and plant
life of these zones vary depending upon: distance from the sea and landform.
These habitats are: 1. sand formation, 2. salt marshes, 3. reed swamps and 4.
potentially cultivated land. The sand formation comprises the low and small
sandy mounds that form low sand bars along the shore-line. In this habitat Zygophyllum
aegyptium predominates with no associated species and with very thin cover.
Also, there are the huge mobile sand dunes of Abu Madi area (up to 60 m high)
which are barren except of a very few plants of Phragmites australis which
may be an indicator of a previously swampy habitat. The partially stabilized
sand dunes are dominated by the pioneer psammophytes: Stipagrostis ciliata
and Elymus farctus with abundant presence of Alhagi graecorum
and Echinops spinosissimus etc. Stabilized sand dunes are dominated by
Asparagus stipularis, Echinops spinosissimus and Thymelaea
hirsuta. In the saline patches of the runnels within the sand dunes, there
are areas dominated by Arthrocnemum macrostachyum, Sporobolus spicatus,
Imperata cylindrica and Cressa cretica etc. The semi-wild Phoenix
dactylifera is also a characteristics feature of the sand dune habitat of
this coastal belt.
The vegetation of the salt marsh habitats is formed of communities dominated
or co-dominated by Arthrocnemum macrostachyum, Cressa cretica
(widespread), Halimione portulacoides, Halocnemum strobilaceum,
Limbarda crithmoides, Juncus acutus, J. rigidus, Aeluropus
brevifolius, Sporobolus spicatus, Limoniastrum monopetalum,
Suaeda vera, Tamarix tetragyna and Zygophyllum aegyptium.
The frequent swampy habitats are usually in low areas of the landward zone where
the water seeping from the lakes and/or drained from cultivated lands accumulate.
Typha domingensis dominates in these swamps with the common presence
of Phragmites australis. In the saline-saturated fringes of these swamps
rushes e.g., Juncus acutus, J. rigidus and sedges, e.g., Carex
extensa, Cyperus laevigatus and Scirpus tuberosus, grow.
Bassia indica predominates on the dry saline banks of these swamps.
The potentially cultivated land occupies the most landward zone of this coastal
belt. Being less saline, this habitat supports the growth of annual weeds. Cakile
maritima is the most abundant weed, common ones include: Amaranthus ascendens,
Launaea angustifolia and Senecio desfontainei.
Field works: Six halophytes have been chosen for the present study,
namely: Arthrocnemum macrostachyum, Halocnemum strobilaceum, Limoniastrum
monopetalum, Tamarix tetragyna, Cressa cretica and Bassia
indica. Samples of the shoot systems of these plants were collected for
chemical analysis. Also, 2 soil samples at 0-20 cm and 20-40 cm depth were collected
from the grounds of the study plants for physical and chemical analysis.
Field experiment: The establishment of Bassia indica in a salt
affected land of the study area was experimented.
Plant analyses: Immediately after collection, the plant samples were washed
several times with distilled water and oven dried in an oven (at 60°C) to
constant dry weight, their fresh and dry weights were determined. After desiccation
the dry samples were ground to fine powder ready for different analysis. Samples
were replicated and each test was repeated twice, the mean values are given
(±) to the standard errors of means. Estimation of succulence and carbohydrates,
were according to Tiku (1975) and Thyumanavan
and Sadasivan (1984), respectively and total protein was calculated by multiplying
the total nitrogen by the factor 6.25, crude fat (Ether extract) (AOAC,
1990) The total digestible nutrient was estimated according to the equation
described by Abu-El-Naga and El-Shazly, 1971). The Digestible
Protein (DP) was calculated according to the regression equation of Demarquilly
and Weiss (1970). Macroelements (Na, K and Ca) were estimated according
to Allen et al. (1974).
Soil analyses: The collected soil samples were air dried, thoroughly
mixed and passed through 2 mm sieve to remove gravels and debris and packed
in plastic bags for physical and chemical analyses. Sieving method was used
to get the weight of sand, silt and clay. Moisture content of the fresh soil
samples were determined by weighting sealed tins before and after drying the
samples in an oven at 105°C to constant weights. Soil chemical properties
were determined following the methods described by Piper (1947)
and Jackson (1962).
Statistical analyses: One-way Analysis of Variance (ANOVA) was applied
to assess the significance of variation in the environmental variables and nutritive
values with equal replication using the COSTAT program. A test (LSD) was applied
to determine the least significance of difference in the salinity tolerance
of B. indica plant.
The study halophytes: Arthrocnemum macrostachyum is a leafless,
jointed succulent shrublet halophyte with flowers in terminal spicate inflorescence.
It is a densely branched, robust plant with decumbent rooting base. Its community
is wide spread in both the coastal and inland deserts of Egypt. Halocnemum
strobilaceum is a richly branched shrub with woody continuous branches,
rudimentary leaves and perfect flowers. It is easily recognized by its numerous
small, decussate green tubercles along the branches, composed of small-rudiments.
Both A. macrostachyum and H. strobilaceum are closely related
halophytes belonging to the Mediterranean, Irano-Turanian and Saharo-Sindian
elements. However, H. strobilaceum is not widespread in the Egyptian
salt marshes. It is absent from the oases of the Western Desert as well as from
the southern section of the Red Sea coastal land.
Limoniastrum monopetalum is a halophytic shrub of whitish-grey aspect.
Leaves narrowly spathulate, as well as stems and branches, densely beset with
white calcareous tubercles. It is an excretive halophyte that seems to be intolerant
to arid climate as it flourishes only in the Mediterranean littoral salt marshes,
absent elsewhere in Egypt. Limoniastrum is a pure Mediterranean element.
Tamarix tetragyna is a woody tall shrub (3-5 m high) with very small
scale-like leaves and large pink flowers. It is an excretive halophyte that
grows in a variety of habitats but it prefers wet salt marshes. T. tetragyna
belongs to the Saharo-Sindian extending to the Mediterranean and Irano-Turanian
regions. In Egypt, this species occurs in both coastal and inland salt marshes.
Cressa cretica is a mat-shaped excretive halophyte with sessile, white
flowers. It is a hairy plant of grey appearance, herbaceous or frutescent, prostrate,
rarely erect. Leaves 3 mm long, crowded, acute. It is one of the Mediterranean
and Palaeotropical elements. In Egypt, C. cretica is very common in both
coastal and inland dry salt marshes. Bassia indica is an annual bushy
richly branched herb, under favourable conditions reaching a height of 2 m.
more or less densely hairy. Leaves on sterile branches linear-lanceolate, 3-4
mm long, on flowering branches very narrow, only a few mm long. B. indica
belongs to the Irano-Turanian and Sudano-Zambezian areas. It may be slightly
extending into Saharo-Sindian regions. Its native home is India and have been
non-intentionally introduced to Egypt (Drar, 1952).
B. indica is usually seen in the waste ground and salt affected lands
throughout Egypt (El-Dingawi, 1990).
Soil properties: The results shown in Table 1 elucidate
that the soil supporting the growth and domination of the study plants are generally
moist, slightly alkaline (pH = 7.4-7.97), sandy to sand-silty in texture with
low amount of clay. Organic carbon contents are generally low (0.12-1.5%), and
calcium carbonate contents are relatively high (56.0-70.0%) in the soil of Limoniastrum
than those of the other species. Total soluble salts are generally high particularly
in the surface layers (up to 11.2% in the soil of Halocnemum), mainly
chlorides and partly sulphates and bicarbonates.
Nutritive values of the study plants: Table 2 contains
the results of the chemical analyses of the shoot samples of the study six species
that elucidate the following facts:
||All species are rich in their carbohydrate contents ranging
between 434.79 mg g-1 DW in Cressa followed by those of
Bassia (331.2 mg g-1 DW), Limoniastrum (320.8
mg g-1 DW), Tamarix (319.7 mg g-1 DW), Arthrocnemum
(300.69 mg g-1 DW) and Halocnemum (143.54 mg g-1
DW). On the other hand, the relatively highest amount of protein had been
also detected in Cressa (14.79%) and the lowest amount was that of
Tamarix (4.43%). In Bassia branches the protein content was
9.25%, whereas in Halocnemum it was 9.44%, in Limoniastrum
was 6.98% and Arthrocnemum was 5.34%
||The amounts of the macro-elements (Na, K and Ca) varied considerably between
the study six species. The highest amount of sodium (34.2 mg g-1
dry weight) was that of Arthrocnemum followed by that of Cressa
(31.6 mg g-1 dry weight), Bassia (28.8 mg g-1
dry weight), Limoniastrum (25.3 mg g-1 dry weight) and
Tamarix (23.7 mg g-1 dry weight). On the other hand, Bassia
contains the relatively highest amount of potassium (23.4 mg g-1
dry weight) and the least was that of Tamarix (10.0 mg g-1
dry weight). The amounts of potassium detected in the other species were:
19.2, 16.3, 15.0 and 11.7 mg g-1 dry weight in Arthrocnemum,
Halocnemum, Cressa and Limoniastrum, respectively. The
relatively highest amount of calcium was detected in Cressa (32.4
mg g-1 dry weight) and the least was that of Bassia (10.2
mg g-1 dry weight). Almost similar amounts of calcium (25.0 and
22.6 mg g-1 dry weight) were detected in Halocnemum and
Arthrocnemum whereas small amounts (15.0 and 14.8 mg g-1
dry weight) were detected in Tamarix and Limoniastrum, respectively
|| Physical and chemical properties of 12 soil samples collected
from the habitats of the study halophytes, deltaic Mediterranean coastal
|MC: Moisture content, OC: Organic carbon, CC: Calcium carbonate,
TS: Total soluble salt, SN: Sample number. Mean of the variables have the
letters which are significantly different according to the LSD-test (p≤0.05)
|| Nutritive values of the shoots of halophytes naturally growing
in the Deltaic Mediterranean coastal desert, Egypt
|FW: Fresh weight, DW: Dry weight, Carb.: Total carbohydrates,
Prot.: Proteins, Suc.: Succulence, EE: Ether extract, DP: Digestible protein,
TDN: Total digestible .nutrients, Mean±standard errors
Establishment experiment: To introduce the six studies halophytes as
non-traditional fodder producing plants, their propagation under salinity and/or
aridity stress should be tested. Bassia indica was the first for such
experiments to be followed by the five remaining plants.
In its natural stands, B. indica usually produce large amounts of seeds
which are short-lived and do not remain viable in the soil more than one year
(Sadek, 1974). However, Hammad (1989)
succeeded to germinate 3-years old B. indica seeds using six concentrations
of sodium chloride solutions (50, 150, 300, 500, 800 and 1000 mM) and found
that the increase in salt concentrations from 500 to 800 mM was associated with
succession decrease in the rate of seed germination. Seeds treated with 1000
mM failed to germinate. Salinity tolerance of B. indica plants was tested
in 80 young seedlings collected from its natural stands of the deltaic Mediteranean
coast. On 10 April 2010 the seedlings were transplanted in 16 pots, 8 were filled
with silty soil and the remainder were filled with sandy soil. Irrigation was
carried out with equal amounts of fresh water (1 L) as control set, 0.5, 2 and
3% NaCl solutions for the second, third and fourth sets, respectively. Application
of NaCl was only once and afterwards all pots were irrigated with fresh water
at 3-days intervals to keep the soil at its field capacity. The experiment
continued for 3 months and the shoots of B. indica were harvested on
July 2010. Plant height and fresh and dry weights were determined. The results
(Table 3) show that B. indica seedlings succeeded to
grow normally after being treated with saline solution as high 3% NaCl. The
results were analyzed statistically (Poole, 1974) and
the correlation coefficients (r) were determined. Positive correlations (0.5
for sand and 0.6 for silty soils) occurred between the measured parameters and
the concentrations of NaCl solutions up to 3%. The relatively highest fresh
and dry weights were recorded in pots filled with silty soil and watered with
3% NaCl solution, the means of fresh and dry weights were 1.14 and 0.24 kg pot-1,
Field establishment experiment of B. indica was conducted in the salt
affected land of the deltaic Mediterranean coast of Egypt. This land which was
dominated by Zygophyllum aegyptium was cleared from its natural vegetation,
prepared and divided into plots (35 plots, 7x7 m each). On 7 February 2011,
a soil profile was dug and soil samples were collected and analyzed. The result
indicate that the soil is alkaline (pH = 8.1, 8.8 and 8.9 in the surface, subsurface
and bottom layers, respectively). The highest amounts of soluble salts (EC =
12 mmohs cm-1) were detected in the surface layer. Salinity decreased
in the middle and bottom layers to 2.5 and 1.85 mmohs cm-1, respectively.
The soil texture varies from sandy to sandy-loam.
On February 10, 2011, seeds of B. indica were sown and seated at 3-4
cm depth in the soil. Plots were irrigated with saline artesian water (total
saline salts = 4851.2 ppm) at weekly intervals. After about 3 weeks, only a
few seeds of B. indica germinated.
|| Salinity tolerance of B. indica plant
Low germination was attributed to the non-viability of most Bassia seeds
and/or deep sowing of seeds in the soil. Thus, sowing was repeated on March
3, 2011 by planting Bassia seeds at less than one cm depth. This time
the germination percentages was high, most of the seeds germinated after 4 days.
Growth of plants continued normally. On May 2011, after irrigation with artesian
water for 11 weeks, a second profile was dug and soil samples were collected
and analyzed. The results revealed that soil salinity (expressed by EC) increased
from 12 to 20 mmohs cm-1 in the surface layer, from 2.5 to 5 mmohs
cm-1 in the second layer and from 1.85 to 3 mmohs cm-1
in the bottom layer. Although associated with high air temperature, such an
increase in soil salinity did not show adverse effects on the growth of B.
indica individuals. At the end of May 2011, the plant cover of the plots
was more than 80%. The plants reached their maximum vegetative growth during
the July-August period, i.e summer forage production. On August 20, 2011, the
height, horizontal extension and fresh weights of 20 representative bushes of
B. indica were determined. The means of these parameters were as follow:
235, 280 cm and 8.5 kg bush-1, respectively. Statistical assessment
of the data obtained from this experiment indicates that there is a positive
correlation between the vegetative yields (forage production) and the other
parameters measured: height of plants and branch extension (r = 0.55). B.
indica plants changed to brownish yellow during September and dried in October.
The newly produced seeds could be collected during December.
The population density of the Egyptian desert is generally, low, hundreds of
square kilometers may be devoid of human habitation. The reverse is true in
the River Nile region which covers only less than 4% of Egypts lands and
in the same time it has very dense population that expected to be hundred millions
by 2020. Thus, areas of desert vacant to-day should be habitated. Land use with
shortage of fresh water in the deserts may limit agriculture and farming. Conventional
crops need lot of fresh water and their cultivation in the deserts will, certainly,
cause quick depletion of the ground water. Thus, trials to introduce non-conventional
crops by growing desert plants capable of living by the least amount of fresh
water or by sea water directly may be the possible and promising way to overcome
such acute population problem.
The forage values of any plant to be good fodder for livestock, apart from
being palatable and non-toxic, it must contain adequate levels of proteins,
fats, carbohydrates, vitamins and mineral nutrients for satisfactory growth
(Heneidy, 1996; Zahran and Willis,
2003). The palatable plant species are always over grazed due to the grazing
pressure of animals particularly in the deserts (El-Shaer,
1981). However, unpalatable and less-palatable halophytes are widely distributed
in the desert throughout Egypt. Factors influencing grazing and nutritive values
of halophytes are: the plant species, ecotypes, stage of growth (Abd
El-Aziz, 1982; El Shaer, 1986), season of use (wet
season versus dry season), environmental factors (El Bassosy,
1983), and location (Gihad and El Shaer, 1994). Halophytic
plants differ in their nutritive value as from one species to another.
The total protein is proposed to be an indicator of the nutritional value of
plants as food for ruminants (Bryant et al., 1983).
In the present study, the selected species contained total protein comparable
with reported by Kadi (1987). Although, lipids are a concentrated
source of energy, they do not constitute a major source of energy from forages
(Chesworth, 1996; Henneidy, 2002).
The lipid content found in the plants of the current work were similar to those
reported by El-Halawany et al. (2008), Kadi
(1987) and Zahran et al. (1999). On the other
hand, the total carbohydrate which provides the plant itself as well as the
animal by energy were, relatively, higher in the study plants than that the
study of El-Shamy (1995) and relatively comparable to
that study of El-Halawany et al. (2008), Kadi
(1987) and Omar (2006). Jeroch et
al. (1999) reported that, the optimal contents of carbohydrates for
producing high quality silage is 8-10%, thus, most of the selected halophytes
may considered as good species for fodder production.
The Digestible Protein (DP) of the study plants, calculated as a percentage
of dry matter, was about 4.51%. With this value their forage qualities is realized
as having a good protein content according to the scale suggested by Boudet
and Riviere (1968). Heneidy (1986) calculated that
the percentage of DP in the forage plants of the Western Desert of Egypt is
about 5.4%. The Total Digestible Nutrient (TDN) is an approximate measure of
the food energy available to animals after digestion (Lofgreen,
1951) and can be used as a measure of energy requirement of animals and
the energy value of feeds. Abdel-Razik et al. (1988)
reported that the annual average of TDN value was 75% DM. In the studied species,
the annual average of TDN is about 57.69% DM which are comparable to those of
clover (56%), barley (64%) and corn (68%) as reported by Soliman
and EL-Shazly (1978). Also the results of the present study show that the
concentration of macroelements (Sodium, Potassium and Calcium) in the selected
species are enough for the requirements of animals which reflects the findings
of Mayland and Hankins (2001).
It is worth to state here that, according to the obtained result, the six halophytes,
namely: Arthrocnemum macrostachyum, Halocnemum strobilaceum, Limoniastrum
monopetalum, Tamarix tetragyna, Cressa cretica and Bassia
indica naturally growing in the salt affected lands of the deltaic Mediterranean
coastal desert of Egypt are of high potentialities as fodder producing plants.
They are rich with their nutritive values and their water requirements are low.
Thus, mass production of their vegetative yields will certainly help to maintain
reasonable quantities of raw materials for fodder industries.
Establishment of B. indica in a piece of salt affected land of the study
coastal desert is actually encouraging. Vegetatively, the plant produced high
amounts of fresh and dry materials and, accordingly, the extension of its cultivation
in such saline non-productive land will, hopefully, change the land to be productive
and secure reasonable amounts of raw materials to establish fodder industries.
The establishment of the other five halophytes and even other xerophytes and
halophytes in Egypts desert
could play the main role for the welfare of Egypts
1: Abd El-Aziz, D.M., 1982. A study of the nutritive value of some range plants in the North-Western coastal desert. Ph.D. Thesis, Faculty of Agriculture, Ain Shams University.
2: Abdel-Razik, M., M.A. Ayyad and S.Z. Heneidy, 1988. Preference of grazing mammals for forage species and their nutritive value in a Mediterranean desert ecosystem (Egypt). J. Arid Environ., 15: 297-300.
3: Abu-El-Naga, M.A. and K. El-Shazly, 1971. The prediction of the nutritive value of animal feeds from chemical analysis. J. Agric. Sci., 77: 25-37.
4: Allen, S.E., H.M. Grimshaw, J.A. Parkinson, C. Quarmby and J.D. Roerts, 1974. Chemical Analysis of Ecological Materials. Blackwell Scientific Publications, Oxford, London, UK., pp: 565.
5: AOAC., 1990. Official Methods of Analysis. 17th Edn., Association of Official Analytical Chemistry, Arlington, Virginia, USA.
6: Boudet, G. and R. Riviere, 1968. Employment praetique analyzes fodder for grazing tropical I'appreciation. Rev. Elev. Med. Vet. Too Countries, 21: 227-266.
7: Bryan, J.P., F.S. Chapin and D.R. Klein, 1983. Carbon nutrient balance of boreal plants in relation to vertebrate herbivory. Okios, 40: 357-368.
Direct Link |
8: Chesworth, J., 1996. The Feeding of Ruminants. In: The Technician of Tropical Agriculture, Et Larose, M. (Ed.). Paris, France, Pages: 263.
9: Drar, M., 1952. A report on Kochia indica Wight in Egypt. Bull. Inst. Deserte Egypt, 2: 45-58.
10: Demarquilly, C. and P. Weiss, 1970. Picture of the nutritional value of forages: Report No. 42. International Live Stok Research Insititute.
11: El-Dingawi, A.A., 1990. Contribution to the studies on Kochia plants and their potentialities in fodder production. Ph.D. Thesis, Faculty of Science, Mansoura University, Egypt.
12: El-Halawany, E.F., I.A. Mashaly and A.M. Abd El-Gawad, 2008. On the ecology and fodder potentiality of some non-conventional forage weeds in the Nile Delta, Egypt. J. Environ. Sci. Mansoura Univ., 35: 143-172.
13: Kadi, H.F.E., 1987. A study of range ecosystems of the Western Mediterranean coastal desert of Egypt. Ph.D. Thesis, Technical University of Berline, West Germany.
14: El-Shamy, M.M., 1995. Studies on some taxa of the genus Acacia in Egypt. Ph.D. Thesis, Faculty of Science, Mansoura University, Egypt.
15: El Bassosy, A.A., 1983. A study of the nutritive value of some range plants from Sallom to Mersa Matrouh. Ph.D. Thesis, Faculty of Agriculture, Ain Shams University, Egypt.
16: El-Shaer, H.M., 1981. A comparative nutrition study on sheep and goats grazing Southern Sinai desert range with supplements. Ph.D. Thesis, Faculty of Agriculture Ain Shams University.
17: El Shaer, H.M., 1986. Seasonal variation of the mineral composition of the natural pasture of Southern Sinai grazed by sheep. Proceedings of the 2nd Egyptian-British Conference on Animal and Poultry Production, August 26-28, 1986, Bangor, Gwynedd, UK -.
18: Gihad, E.A. and H.M. El Shaer, 1994. Nutritive Value of Halophytes. In: Halophytes as a Resources for Livestock and for Rehabilitation of Degraded Lands, Squires, V.R. and A.T. Ayoub (Eds.). Kluwer, Dordrecht, Netherlands, pp: 281-284.
19: Hammad, I.A., 1989. Gene ecological studies on Juncus and Kochia. Ph.D. Thesis, Faculty of Science, Mansoura University, Egypt.
20: Heneidy, H.Z., 1986. A study of the nutrient content and nutritive value of range plants at Omayed, Egypt. M.Sc. Thesis, Faculty of Science, Alex. University.
21: Heneidy, S.Z., 1996. Palatability and nutritive value of some common plant species from the Aqaba Gulf area of Sinai, Egypt. J. Arid Environ., 34: 115-123.
22: Henneidy, S.Z., 2002. Browsing and nutritive value of the most common range species in Matruh area, the coastal Mediterranean region, Egypt. Oecologia Mediterranea, 28: 39-49.
Direct Link |
23: Jackson, M.L., 1962. Soil Chemical Analysis. Prentice-Hall Inc., New York, pp: 498.
24: Jeroch, D., W. Drochner and O. Simon, 1999. Nutrition Nutziere Agricultural. Springer Verlag, Berlin, Germany, Pages: 544.
25: Lofgreen, G.P., 1951. The use of digestible energy in the evaluation of feeds. J. Anim. Sci., 10: 344-351.
26: Mayland, H.F. and J.L. Hankins, 2001. Mineral Imbalances and Animal Health. A Management Puzzle. Station Bull. 73. Idaho Forest, Wildlife and Range Exp. Stn., Moscow.
27: Omar, G., 2006. Plant life of the different habitats in the North Nile Delta of Egypt: Ecology and fodder potentialities. Ph.D Thesis. Mansoura University, Egypt.
28: Piper, C.S., 1947. Soil and Plant Analysis. Interscience Publishers Inc., New York, USA.
29: Poole, R.W., 1974. An Introduction to Quantitative Ecology. McGraw-Hill, New York, USA., ISBN-13: 978-0071354691, Pages: 532.
30: Sadek, L.A., 1974. Autecological studies on Kochia indica Wight. Ph.D. Thesis, Faculty of Science, Alexandria University, Egypt.
31: Soliman, S.M. and K. El-Shazly, 1978. Increasing the productivity per feddan from total digestible nutrients. Alexandria J. Agric. Res., 26: 551-556.
32: Thyumanavan, V. and S. Sadasivan, 1984. Qual Plant Foods Human Nutrition. New Age International Ltd. Publishers, New Delhi, India, pp: 253-257.
33: Tiku, B.L., 1975. Ecophysiological aspects of halophyte zonation in saline sloughs. Plant Soil, 43: 355-369.
CrossRef | Direct Link |
34: UNESCO/FAO, 1963. Bioclimatic Map of the Mediterranean Zone. UNESCO/FAO, Rome, Italy, Pages: 58.
35: Zahran, M.A., B.K. Mohammed and I.A. Mashaly, 1999. Introduction of non-conventional livestock fodders under drought and salinity stress of arid lands. Proceedings of a Workshop on Livestock and Drought: Policies for Coping with Changes, May 24-27, 1999, Cairo, Egypt, pp: 75-79.
36: Zahran, M.A. and A.J. Willis, 2003. Plant Life of the River Nile in Egypt. Mars Publishing, Reyadh, Saudi Arabia.
37: Zahran, M.A. and A.J. Willis, 2009. The Vegetation of Egypt. Springer, New York, USA.