<?xml version="1.0" encoding="UTF-8"?><!DOCTYPE article  PUBLIC "-//NLM//DTD Journal Publishing DTD v3.0 20080202//EN" "http://dtd.nlm.nih.gov/publishing/3.0/journalpublishing3.dtd"><article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" dtd-version="3.0" xml:lang="en" article-type="research article"><front><journal-meta><journal-id journal-id-type="publisher-id">AJPS</journal-id><journal-title-group><journal-title>American Journal of Plant Sciences</journal-title></journal-title-group><issn pub-type="epub">2158-2742</issn><publisher><publisher-name>Scientific Research Publishing</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.4236/ajps.2019.109107</article-id><article-id pub-id-type="publisher-id">AJPS-94921</article-id><article-categories><subj-group subj-group-type="heading"><subject>Articles</subject></subj-group><subj-group subj-group-type="Discipline-v2"><subject>Biomedical&amp;Life Sciences</subject></subj-group></article-categories><title-group><article-title>
 
 
  Fodder Halophytes for Saline Lands of Kyzylkum Desert
 
</article-title></title-group><contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Lola</surname><given-names>S. Ortiqova</given-names></name><xref ref-type="aff" rid="aff1"><sub>1</sub></xref><xref ref-type="corresp" rid="cor1"><sup>*</sup></xref></contrib></contrib-group><aff id="aff1"><label>1</label><addr-line>Djizak State Pedagogical Institute, Djizak, Uzbekistan</addr-line></aff><pub-date pub-type="epub"><day>06</day><month>09</month><year>2019</year></pub-date><volume>10</volume><issue>09</issue><fpage>1517</fpage><lpage>1526</lpage><history><date date-type="received"><day>29,</day>	<month>July</month>	<year>2019</year></date><date date-type="rev-recd"><day>7,</day>	<month>September</month>	<year>2019</year>	</date><date date-type="accepted"><day>10,</day>	<month>September</month>	<year>2019</year></date></history><permissions><copyright-statement>&#169; Copyright  2014 by authors and Scientific Research Publishing Inc. </copyright-statement><copyright-year>2014</copyright-year><license><license-p>This work is licensed under the Creative Commons Attribution International License (CC BY). http://creativecommons.org/licenses/by/4.0/</license-p></license></permissions><abstract><p>
 
 
   The article is devoted to the economic and biological characteristics of promising desert semi-shrub halophytes (Kochia prostrate, Salsola orientalis, Ceratoides ewersmaniana, Halothamhus subaphyllus, Camphorosma lessingii) to improve saline lands of the Kyzylkum desert. 
 
</p></abstract><kwd-group><kwd>Kyzylkum</kwd><kwd> Desert</kwd><kwd> Pastures</kwd><kwd> Saline Lands</kwd><kwd> Karakul</kwd></kwd-group></article-meta></front><body><sec id="s1"><title>1. Introduction</title><p>The Kyzylkum desert, often known geographically Botanical references as the Kyzylkum district [<xref ref-type="bibr" rid="scirp.94921-ref1">1</xref>] [<xref ref-type="bibr" rid="scirp.94921-ref2">2</xref>] [<xref ref-type="bibr" rid="scirp.94921-ref3">3</xref>] , is a large footprint and economic importance of the region of Karakul breeding in Central Asia.</p><p>The Kyzylkum desert occupies a large part of the flat territory of Uzbekistan and southern Kazakhstan with altitudes of 100 - 300 (700) m near the sea and is located between the rivers Amudarya, Syrdarya, lower and middle reaches of Zaravshan.</p><p>Kyzylkum at the current level of development of productive forces in agricultural production is the largest pasture region of Karakul within Uzbekistan, Kazakhstan and the Republic of Karakalpakstan. It is dominated by pastures year-round use, accounting for almost 80% of the total area of the district [<xref ref-type="bibr" rid="scirp.94921-ref2">2</xref>] .</p><p>This huge desert area is diverse in geological and geomorphologic against powerful sand formations (ridges, hills, dunes), relict mountain areas (Bukantau, Aristantau, Aktau, Kazakhtau, Djetimtau, Sangruntau, Kokchatau, etc.), plains, pits of depression (Ayakagitma, Karakata, Mingbulak, Beshbulak, etc.).</p><p>In geomorphology of Kyzylkum there are also alluvial low plains, and the relief of the Aral part was formed under the influence of the Aral Sea—along the Eastern shore is characterized by the deposition of loose and fixed Sands.</p><p>The sands of Kyzylkum are the product of centuries—old destruction of sediments that compose the plateau itself. They have a characteristic reddish color (the Uzbek term “Kyzylkum” literally means “red sand”), which owes its name to the entire Kyzylkum desert.</p><p>Believe it is appropriate to briefly elaborate on the General characteristics Ayakagitma and Karatin troughs—the area of the present study.</p><p>Ayakagitma and Karatin basin is located on the administrative boundaries of Gijduvan, Shafirkan, Karmana districts of Bukhara and Navoi regions of Uzbekistan. Common footprint is only one Ayakagitma basin of about 20 km<sup>2</sup> [<xref ref-type="bibr" rid="scirp.94921-ref4">4</xref>] .</p><p>The geomorphological structure of the Ayakagitma depression is quite complex and variegated. It is a saucer-like surface, in some years, sometimes accumulated a small amount of precipitation. This is salt marsh of Bashagitma; there are other small areas of wet salt marshes, often populated by representatives of most supplies of salt-resistant halophytes, or no vegetation.</p><p>The outskirt of this relatively large basin is a terraced formation and wide gentle slopes with uneven terrain. The banks of the depression are often precipitous; they are quite clearly visible outputs of various tertiary rocks—green and red clay, sandstones, marls. In some places, alluvial and proluvial formations are well traced. Separate arrays of cavities, especially near the count, Akmurt, Yavshan-Tepe marked area of aeolian sandy sediment in the form of bumps and ridges.</p><p>The soil cover Ayakagitma basin is quite diverse. From 6 types (grey-brown, desert-sandy, takir, meadow, bog, and salt marshes), 9 subtypes and 31 kinds of soils are characteristic of arid areas in Ayakagitma depression found in almost all of these types and options.</p><p>On elevated areas gray-brown and desert-sandy soils of different mechanical composition prevail; in depressions and moist places with close groundwater— saline soils, meadow, meadow-marsh soils [<xref ref-type="bibr" rid="scirp.94921-ref5">5</xref>] .</p><p>Similar or nearly similar structure of geomorphology is inherent in Karakatin basin. Research Institute of Karakul and desert ecology (Uzbekistan) began to systematically deal with the study of feed halophytes since 1982 under the scientific guidance of Professor Z. Sh. Shamsutdinova [<xref ref-type="bibr" rid="scirp.94921-ref6">6</xref>] [<xref ref-type="bibr" rid="scirp.94921-ref7">7</xref>] [<xref ref-type="bibr" rid="scirp.94921-ref8">8</xref>] [<xref ref-type="bibr" rid="scirp.94921-ref9">9</xref>] [<xref ref-type="bibr" rid="scirp.94921-ref10">10</xref>] .</p><p>The main purpose of the research of this institution, as a scientific staff of Karakul, was and is the development of scientific and technological foundations of phytomelioration of pastures including saline lands of Uzbekistan.</p><p>To achieve this goal, the research program consisted of the following main tasks:</p><p>Collection and creation of the gene pool of fodder halophytes; testing and evaluation of fodder halophytes in saline desert conditions; study of palatability and nutritional value of promising halophyte species; development of agrotechnical methods of cultivation of fodder halophytes in the conditions of culture; identify the specifics of the water regime of promising fodder halophytes in terms of culture.</p><p>Field studies conducted on pastures latitudinal economy “Madaniyat” of Kanimex district of Navoi region. The experimental site is located 150 km North-West of the city of Navoi at an altitude of 130 m.n.u.m., the farm specializes in the production of Karakul products.</p><p>The natural conditions of the research area are sharply continental and arid. The annual amount of atmospheric precipitation for a long period, averages 120 mm, ranging from 38.2 to 264.5 mm. the main period of precipitation—autumn, winter and earlier spring (XI-IV). The average annual temperature is 14.8˚C; the average monthly July 32.4˚C, absolutely maximum—45˚C - 48.3˚C; minimum (January, December)—15˚C - 19˚C.</p><p>The soils of the experimental field (state farm “Madaniyat”, array “Kizil kesek”) are quite saline from the surface (<xref ref-type="table" rid="table1">Table 1</xref>); at a depth of 28 - 62 cm the salt content is significantly reduced; even lower (62 - 100 cm) the content of the dense residue is 1.2% (<xref ref-type="table" rid="table1">Table 1</xref>).</p><p>Among 87 samples comprised of 9 Botanical families, one and perennial halophytes in a culture of the Kyzylkum desert in such important biological parameters as survival, the dynamics of annual growth and amount of biomass on prospects objects in the feed, biomeliorative relations were perennial shrubs (Kohia prostrate, Salsola orientalis, Ceratoides eversmaniana, Halonamnus sufaphyllis), etc.</p><p>More detailed results of the research are reflected in the press [<xref ref-type="bibr" rid="scirp.94921-ref11">11</xref>] - [<xref ref-type="bibr" rid="scirp.94921-ref18">18</xref>] .</p><p>The main purpose of this report is the economic and biological characteristics of promising phytomeliorants from the number of semi-shrub halophytes used to improve the saline pastures of Kyzylkum.</p><p>Below you will find the botanical characteristics of some plants.</p><table-wrap id="table1" ><label><xref ref-type="table" rid="table1">Table 1</xref></label><caption><title> The composition of the aqueous extract of the soil of experimental plot, Kanimex region, “state farm Madaniyat”, array &quot;Kizil kesek”, Mg/eq. Analytical chemist—Lee. P.M</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  rowspan="2"  >Horizon, cm</th><th align="center" valign="middle"  rowspan="2"  >Dense residue, %</th><th align="center" valign="middle"  colspan="4"  >Anions</th><th align="center" valign="middle"  colspan="4"  >Cations</th></tr></thead><tr><td align="center" valign="middle" >СО<sup>3</sup><sub> </sub></td><td align="center" valign="middle" >НСО<sub>3 </sub></td><td align="center" valign="middle" >Cl</td><td align="center" valign="middle" >S O 4 2 <sup> </sup></td><td align="center" valign="middle" >Ca</td><td align="center" valign="middle" >Mg</td><td align="center" valign="middle" >Na</td><td align="center" valign="middle" >K</td></tr><tr><td align="center" valign="middle" >0 - 2</td><td align="center" valign="middle" >13.62</td><td align="center" valign="middle" >0.0012 0.04</td><td align="center" valign="middle" >0.04.09 0.72</td><td align="center" valign="middle" >0.1932 5.448</td><td align="center" valign="middle" >89.09 18.54</td><td align="center" valign="middle" >0.0360 1.79</td><td align="center" valign="middle" >0.1403 11.53</td><td align="center" valign="middle" >40.600 17.72</td><td align="center" valign="middle" >0.0380 0.972</td></tr><tr><td align="center" valign="middle" >2 - 28</td><td align="center" valign="middle" >9.23</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >0.0171 0.28</td><td align="center" valign="middle" >0.4781 13.482</td><td align="center" valign="middle" >5.9669 12.42</td><td align="center" valign="middle" >0.0500 2.49</td><td align="center" valign="middle" >0.1757 14.45</td><td align="center" valign="middle" >2.7750 12.06</td><td align="center" valign="middle" >0.0153 0.39</td></tr><tr><td align="center" valign="middle" >28 - 62</td><td align="center" valign="middle" >6.78</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >0.0145 0.23</td><td align="center" valign="middle" >0.2072 5.84</td><td align="center" valign="middle" >0.4013 8.35</td><td align="center" valign="middle" >0.0300 1.40</td><td align="center" valign="middle" >0.0683 5.61</td><td align="center" valign="middle" >0.1635 7.09</td><td align="center" valign="middle" >0.008 0.22</td></tr><tr><td align="center" valign="middle" >62 - 100</td><td align="center" valign="middle" >1.24</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >0.0136 0.22</td><td align="center" valign="middle" >0.1673 4.71</td><td align="center" valign="middle" >0.7029 14.63</td><td align="center" valign="middle" >0.9380 1.89</td><td align="center" valign="middle" >0.0964 7.92</td><td align="center" valign="middle" >0.2220 9.65</td><td align="center" valign="middle" >0.0037 0.09</td></tr><tr><td align="center" valign="middle" >Subsoil water</td><td align="center" valign="middle" >12.4</td><td align="center" valign="middle" >0.0288 0.96</td><td align="center" valign="middle" >0.0329 0.54</td><td align="center" valign="middle" >0.3885 10.0</td><td align="center" valign="middle" >0.4057 8.45</td><td align="center" valign="middle" >0.0420 2.08</td><td align="center" valign="middle" >0.0372 3.65</td><td align="center" valign="middle" >0.3182 13.8</td><td align="center" valign="middle" >0.0747 1.91</td></tr></tbody></table></table-wrap></sec><sec id="s2"><title>2. Cochia prostrata (L.) Schrad.</title><p>Botanical characteristics. Xerophilous shrub: 30 - 75 cm, from the family Chenopodiaceae. There are three ecotypes: sandy, rocky, clay.</p><p>Sand (Cochia) is characterized by ascending branches, covered with hairs, with filiform-linear, fibrous leaves. Inflorescence paniculate, with flowers collected in clumps.</p><p>Seeds: round-oval, smooth, brownish, 1.2 - 2.0 mm long and 1.0 and 1.5 mm wide, in the center on both sides dented. Weight of 1000 seeds: 0.9 - 1.2 g.</p><p>The root system of ecotypes of Izena well developed both horizontally and in depth of the soil. In the foothill semi-desert penetrates to a depth of 6.0 m, sandy desert—4.5 - 5.2 m, gypsum desert—3.5 m [<xref ref-type="bibr" rid="scirp.94921-ref19">19</xref>] .</p><p>Stony (Cochia) has a greenish color and a weak descent of shoots and leaves. Its typical growing conditions—crushed and stony soils of foothills and mountains; gray earth of different mechanical composition. It is a valuable plant for the creation of hayfields and pasture agrophytocenoses in the desert and semi-desert.</p><p>Clay (Cochia) istands out light yellow, sometimes reddening shoots with a slight omission. It grows on clay loamy soils, in the mountains of Pamir-Alai, Tien Shan and on saline soils of the Northern subzone of deserts and semi-deserts of the arid zone.</p><p>The ecotypes of Cochia vegetate in conditions of culture of the Kyzylkum desert from early spring till late autumn (<xref ref-type="fig" rid="fig1">Figure 1</xref>). In late may-June form buds; bloom in late July-August. Seeds ripen in October-early November. Throughout the growing season are in a green state. The length of the growing season—220 - 260 days.</p><p>Area and ecology: Grows on sandy and sandy loam soils in Kyzylkum, Muyunkum, middle and lower Volga region and other areas of sandy, rocky deserts.</p><p>The nutritional value of the Cochia is not lower than the nutritional value of oats (Larin 1951). In the budding phase contains 14.3% - 15.6% crude protein, 2.7% - 3.28% fat, 39.5% - 43.5% nitrogen-free extractives and 26.5% - 30.8% fiber.</p><p>The leaves contain a large amount of protein 14.7, little (4.7 - 39.6 mg/kg) of carotene and lignin (10.7% - 18.5%) from trace elements a lot of zinc—17.0 K/kg and amino acids (lysine, leucine, isoleucine) [<xref ref-type="bibr" rid="scirp.94921-ref8">8</xref>] .</p><p>Depending on season of use in 100 kg of feed contains Asenavage 83.5 - 45.1 food unit and 5.6 kg of digestible protein [<xref ref-type="bibr" rid="scirp.94921-ref20">20</xref>] .</p><p>Pasture value. It is perfectly eaten by sheep, goats and camels in all seasons of the year.</p><p>Cochia—valuable grazing, fattening plant in a culture of the Kyzylkum desert harvest his forage is 14 - 16 kg/ha. Due to its valuable feed advantages, high yield, salt resistance, izen stands out among other types of desert shrubs.</p><p>In Research Institute of Karakul and desert ecology and zoned 5 varieties (“Karnabchul”, “Desert”, “Sahra”, “Otavniy”, “Nurota”) of Cochia [<xref ref-type="bibr" rid="scirp.94921-ref21">21</xref>] .</p></sec><sec id="s3"><title>3. Ceratoides ewersmanninana (Stschegl. et. Losinsk.) Botsch. et. Ikonn.</title><p>Botanical characteristics: semi-shrub of the family of Chenopodiaceae from 40 to 120 cm in height.</p><p>The root system of the universal type penetrates to a depth of 5 - 6 m. The Leaves are all-cut, flat, alternate with short petioles, oblong-oval, strongly lowered. Shoots light green, straight at the base (<xref ref-type="fig" rid="fig2">Figure 2</xref>).</p><p>Phenology: blooms in July-August, bears fruit in September-October.</p><p>Area and ecology. It grows in the Aral-Caspian, Balkhash, Kyzylkum, near the Syrdarya, Tien-Shan, Pamir, Afghanistan and Western Mongolia. Inhabits sand, finely earthy-rubbly, stony-rubbly and loess slopes of the mountains and the lowlands, on dry roam rivers and sais.</p><p>Nutritional value: green shoots and leaves during flowering contain 16% crude protein, 2.7% fat, 3.4% crude fiber. 100 kg of dry food contains 9.1 kg of digestible protein and 37.9 kg of fodder food.</p><p>Pasture value. Good food for cattle, horses, sheep. Well eaten annual shoots and leaves, more likely in the autumn-winter season. The yield of teresken in the culture of Kyzylkum—10 - 12 C/ha. In culture in the first year of life reaches a height of 35 - 40 cm, in the second and subsequent years—50 - 70 cm.</p><p>Teresken has a high drought resistance, longevity, good yields and adaptability to the harsh conditions of the Kyzylkum desert.</p><p>It is a valuable object for improvement of pastures in saline desert.</p><p>In Research Institute of Karakul and desert ecology display a variety of teresken “Tulkin”.</p></sec><sec id="s4"><title>4. Salsola orientalis. G. Gmel. (S. Rigida Pall.)</title><p>Botanical characteristics: Perennial, polymorphic haloxerophyte height up to 85, usually 40 - 55 cm of the family Chenopodiaceae (<xref ref-type="fig" rid="fig3">Figure 3</xref>).</p><p>Annual shoots of gray-green color, straight or ascending, with linear, hairy leaves. The leaves are succulent, alternate, awl-shaped, drooping. Root system of universal type [<xref ref-type="bibr" rid="scirp.94921-ref22">22</xref>] .</p><p>Seeds with pericarp, yellowish-dark brown. The seed peel is two-layer with an intermediate cuticle (12 - 26 microns). The embryo is spirally twisted. Distinguish gypsophilous, halophilic ekofarma [<xref ref-type="bibr" rid="scirp.94921-ref23">23</xref>] .</p><p>The growth of keyreuk begins in March-April, blooms in June-August, bears fruit in October-November. Terminates the growing season after autumn frosts.</p><p>Area and ecology. Distributed in Central Asia, the Caspian coast of the Caucasus, Iran, Afghanistan and China. The most saturated areas of its area are the Aral Karakum, Kyzylkum, Ustyurt.</p><p>It grows on gray soils, gray-brown soils, takyrs, on low-power Sands; prefers a more dense soil and is rarely found on highly moist and plump saline soils. In plant communities with the participation of keyreuk shrubs are 7% - 15%, semi-shrubs—18 - 30%, annual and perennial herbs—12% - 60%.</p><p>Nutritional value: in the phase of regrowth (Kyzylkum) contains 16.9% protein, fiber—24.8%, ash—18.2%, BEV—36.5%. Rich in minerals: 1.35% - 2.23% calcium 0.12% - 0.31%, phosphorus, sulfur—0.64% - 1.42%, potassium—2.2% - 2.8% and 3.2% - 5.2% sodium.</p><p>In 100 kg of feed in the spring contains 64.4 feed. Units summer—45.4, autumn—38.0, winter—29.6.</p><p>Amino acid composition is also diverse: the largest number of amino acids contained in the spring: 0.7 g arginine, 1.7 g aspartic acid; 2.4 g glutamic acid, 1.2 g glycine, 1.1 g alanine, 1.4 g valine, 0.25 g methionine, 1.4 g leucine, 0.5 g tyrosine, etc. [<xref ref-type="bibr" rid="scirp.94921-ref8">8</xref>] .</p><p>The content of carotene in the vegetation phase is 85.4; vitamin C—781 mg/kg.</p><p>The grazing value: keyreuk eaten by sheep, goats, camels; often in the fall and winter. Eaten its parts are all above-ground vegetating parts of the current year in a green and dry state.</p><p>Feed productivity of keyreuk in various soil and soil conditions is 6.9 - 21.2 C/ha of hay [<xref ref-type="bibr" rid="scirp.94921-ref12">12</xref>] .</p><p>In Uzbekistan, launched and distributed a variety of keyreuk “the firstborn Karnab” (in Kazakhstan “Aydarli 1”) [<xref ref-type="bibr" rid="scirp.94921-ref24">24</xref>] .</p><p>Keyreuk is a valuable object for phytomelioration of arid pastures of saline, gypsum deserts of Central Asia [<xref ref-type="bibr" rid="scirp.94921-ref17">17</xref>] .</p></sec><sec id="s5"><title>5. Halothamhus subaphyllus (C. A. Mey) Botsch.; (Salsola subaphylla (C. A. Mey); Allenia subaphylla (C. A. Mey); Aellen.</title><p>Botanical characteristics: Shrub with a height of 50 - 120 cm of the family Chenopodiaceae. Escape is highly branched, light green. Leaves alternate, fleshy. The flowers are located in the axils of the bracts, single in spike inflorescences. Fruit: unopened nut, the size of the fruit is 12 - 20 mm (<xref ref-type="fig" rid="fig4">Figure 4</xref>).</p><p>Seeds: rounded, slightly concave 2 - 3.5 mm. Embryo spiral, with a yellowish spine, and the two dark green cotyledons.</p><p>Phenology: Grows in March, blooms in may-July, and bears fruit in October-early November. The growing season ends in the autumn after frosts.</p><p>Area and ecology. Distributed on gravelly saline soils, gray-brown and gray soils, takyrs, on low-power Sands of the arid zone of Central Asia.</p><p>Nutritional value: leaves and twigs contain (%) protein to 14%; fiber content—23%, ash substances—20%. Its dry food in the budding phase contains crude protein—24.7%, fat—2.7%, BEV—36.9%, and fiber—18.3%.</p><p>In 100 kg of dry food contains 52 summer, autumn—46 and winter 37 fodder food.</p><p>Pasture value: Valuable forage plant for sheep, goats, camels. Mainly eaten in</p><p>the autumn-winter season. Fodder productivity in nature 0.8 - 2.0, in culture 8 - 10 C/ha of air-dry mass. Seed productivity of 1.8 - 2.0 kg/ha.</p><p>Widely used in phytomeliorative arid pastures.</p><p>In Research Institute of Karakul and desert ecology (RIKDE) launched his sort “Jayhun”.</p></sec><sec id="s6"><title>6. Camphorosma lessingii Litv.</title><p>Botanical characteristics. Shrub of the family Chenopodiaceae with a height of 30 - 80 cm. Morphologically from other semi-shrub salt pans is characterized in that its vegetative shoots often tightly pressed to the ground, and the generative shoots are covered with a whitish drooping.</p><p>Areal komforsmi—Central Asia, South-East of the European part of Russia, Western Siberia, Iran, Afghanistan, China, Mongolia.</p><p>It is more common in steppe, desert, and semi-desert zones [<xref ref-type="bibr" rid="scirp.94921-ref20">20</xref>] .</p><p>Typical growing conditions are salt marshes, salt marshes, saline lands with close groundwater occurrence.</p><p>It is a drought-resistant, salt-tolerant, well-eaten by cattle plant for sheep, goats, and camels.</p><p>During the period of full fruiting camphor contains 14.4% protein, 2.2% fat, 35.2% fiber and 39.3% BEV.</p><p>100 kg of dry camphor feed contains 44.5 feed in winter units and 9.3 kg of digestible protein [<xref ref-type="bibr" rid="scirp.94921-ref25">25</xref>] .</p><p>Camphorosma is a plant capable of forming a deeply penetrating and powerfully developed root system.</p><p>Conclusions. Halophytes (there are more than 2000 of them in the world flora, more than 700 species in the flora of Central Asia) are specific plants and are adapted to function normally, produce phytomass, bear fruit, and renew themselves in a saline growing environment.</p><p>The halophytes objects diversified household purposes, fodder, medicinal, food, oil-bearing plants, energy and biomeliorants.</p><p>Promising feed halophytes are characterized by valuable economic and biological properties.</p></sec><sec id="s7"><title>Conflicts of Interest</title><p>The authors declare no conflicts of interest regarding the publication of this paper.</p></sec><sec id="s8"><title>Cite this paper</title><p>Ortiqova, L.S. (2019) Fodder Halophytes for Saline Lands of Kyzylkum Desert. 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