<?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">OJAS</journal-id><journal-title-group><journal-title>Open Journal of Animal Sciences</journal-title></journal-title-group><issn pub-type="epub">2161-7597</issn><publisher><publisher-name>Scientific Research Publishing</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.4236/ojas.2015.53029</article-id><article-id pub-id-type="publisher-id">OJAS-56891</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>
 
 
  The Habitats, Burrowing Behavior, Physiology Adaptation and Life Cycle of Spadefoot Toads (&lt;i&gt;Pelobates syriacus, Boettge&lt;/i&gt;r, 1869) at the Southern Limit of Its Distribution in Israel
 
</article-title></title-group><contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>ad</surname><given-names>Degani</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>Faculty of Science and Technology, Tel Hai Academic College, Tel-Hai, Israel</addr-line></aff><author-notes><corresp id="cor1">* E-mail:<email>gad@MIGAL.org.il</email></corresp></author-notes><pub-date pub-type="epub"><day>15</day><month>05</month><year>2015</year></pub-date><volume>05</volume><issue>03</issue><fpage>249</fpage><lpage>257</lpage><history><date date-type="received"><day>13</day>	<month>March</month>	<year>2015</year></date><date date-type="rev-recd"><day>accepted</day>	<month>31</month>	<year>May</year>	</date><date date-type="accepted"><day>4</day>	<month>June</month>	<year>2015</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 present study describes the habitats, life cycle, larvae growth, burrowing behavior and terrestrial adaptation of Spadefoot toads in Israel based on observations and data collected during more than 30 years in northern Israel. The distribution area in Israel is from the north in the Upper Galilee and Golan Heights (annual rainfall range of 500 - 1000 mm) to the southern coastal plain (annual rainfall of about 250 mm). Among the 51 different breeding places of amphibians, only ponds where water was available for a few months were used by Spadefoot toads and metamorphosed populations were found around these ponds. The larvae underwent metamorphosis during the summer and autumn in northern Israel, and during the spring in central and southern Israel. A negative correlation exists between the percentage of toads burrowing and soil moisture levels, with greater burrowing behavior occurring under dry conditions. The plasma concentration increased during burrowing by electrolytes and urea accumulations. The burrowing behavior helped Spadefoot toads survive in this area at the southern border of its distribution.
 
</p></abstract><kwd-group><kwd>Breeding Places</kwd><kwd> Burrowing Behavior</kwd><kwd> Larvae</kwd><kwd> Life Cycle</kwd><kwd> &lt;i&gt;Pelobates syriacus&lt;/i&gt;</kwd><kwd> Plasma Concentration</kwd></kwd-group></article-meta></front><body><sec id="s1"><title>1. Introduction</title><p>The knowledge of the biology, ecology and genetics of Spadefoot toads (Pelobates syriacus) in Israel at the southern border of its distribution is important for understanding their adaptation to this area. This species is found in the southeastern Balkans, eastern to southeastern Transcaucasia, northern Iran, and south of the Levant [<xref ref-type="bibr" rid="scirp.56891-ref1">1</xref>] . Spadefoot toads are studied extensively in Europe. The populations are found around breeding places where the substrates of terrestrial habitats include sandy soils, heath lands and deciduous woodlands with loamy soils, while the spawning biotopes include a variety of permanent or semi-permanent ponds [<xref ref-type="bibr" rid="scirp.56891-ref1">1</xref>] [<xref ref-type="bibr" rid="scirp.56891-ref2">2</xref>] . Spadefoot toads were 7.4 years old on average (maximum age recorded 12), despite the fact that sexual maturity (i.e., the age of the youngest adults observed) was reached at a similar age [<xref ref-type="bibr" rid="scirp.56891-ref1">1</xref>] [<xref ref-type="bibr" rid="scirp.56891-ref2">2</xref>] . The size of the egg clutches varied from less than 1000 to almost 6000 eggs, with an average value of 2800 eggs per clutch [<xref ref-type="bibr" rid="scirp.56891-ref2">2</xref>] .</p><p>The distribution, habitat and breeding place selection of ponds are related to water availability during the spring and early summer in Israel [<xref ref-type="bibr" rid="scirp.56891-ref3">3</xref>] , larval growth and complete metamorphosis [<xref ref-type="bibr" rid="scirp.56891-ref4">4</xref>] [<xref ref-type="bibr" rid="scirp.56891-ref5">5</xref>] , burrowing behavior [<xref ref-type="bibr" rid="scirp.56891-ref6">6</xref>] , physiology adaptations to various environments [<xref ref-type="bibr" rid="scirp.56891-ref7">7</xref>] , and biology [<xref ref-type="bibr" rid="scirp.56891-ref8">8</xref>] [<xref ref-type="bibr" rid="scirp.56891-ref9">9</xref>] . The burrowing toad P. syriacus spends 8 - 10 months of the year being buried in soil (Warburg, 1971, 1972). During the summer, the soil dries out, and the osmotic relationship between the toad and the surrounding soil changes. At a certain point, water begins to pass from the toad to the soil (or the air) and the toad becomes dehydrated.</p><p>Spadefoot toads are highly specialized and have a narrow ecological niche that selects lower levels of diversity [<xref ref-type="bibr" rid="scirp.56891-ref10">10</xref>] . The genetic variation among their populations was studied in the southern area of the Mediterranean shoreline [<xref ref-type="bibr" rid="scirp.56891-ref11">11</xref>] [<xref ref-type="bibr" rid="scirp.56891-ref12">12</xref>] . Nevo [<xref ref-type="bibr" rid="scirp.56891-ref13">13</xref>] suggested that Pelobates was best explained by the environmental variability model based on selection for homozygosity as an adaptive strategy in the relatively constant and narrow subterranean niche. Although several aspects of Spadefoot toads in Israel have been studied, the life cycle of Spadefoot toads at the southern border of its distribution in Israel has not been described in detail. Due to their secretive behavior (nocturnal activity, weak underwater breeding call and cryptic coloration), their life histories are not well documented, and overall there is a scarcity of information regarding this genus. Moreover, this genus, Pelobates, is distributed in different climates, which affects life cycle, and some basic biological characteristics are similar and might help to complete the information of the species in Israel, Pelobates syriacus.</p><p>The purpose of the present study is to describe the habitats, life cycle, larvae growth, burrowing behavior and terrestrial adaptation of Spadefoot toads in Israel based on observations and data collected during more than 30 years in northern Israel.</p></sec><sec id="s2"><title>2. Materials and Methods</title><sec id="s2_1"><title>2.1. Study Area</title><p>The study was carried out over four consecutive decades (1979-2014). Different aquatic habitats were dispersed over an area of approximately 1400 km<sup>2</sup> in northern Israel. The habitats included springs and streams that were stable water bodies where water was available year-round, rock pool holes, which were filled by rainwater and whose hydroperiods were long (about 200 d/yr), and ponds, which were flooded during the autumn when rainfall began, and gradually dried out between the late winter months and early summer.</p></sec><sec id="s2_2"><title>2.2. Sampling</title><p>The water body was examined by nets (pore size 450 μm) from a depth of approximately 10 - 30 cm, as described previously by [<xref ref-type="bibr" rid="scirp.56891-ref3">3</xref>] . Rain pools and ponds in Israel that were filled by rain held the water for 3 - 4 months before drying up; large ponds dried up after a period of 6 - 12 years. The elevation of the breeding places is between 0 to 1000 m above sea level. The breeding places that were examined are presented in <xref ref-type="table" rid="table1">Table 1</xref> and <xref ref-type="fig" rid="fig1">Figure 1</xref>.</p></sec><sec id="s2_3"><title>2.3. Biotic and Abiotic Water Parameters</title><p>Water quality testing during larval growth, which was described in detail in the chapter on water quality, included dissolved oxygen (%), water temperature (˚C), pH, electrical conductivity (&#181;s/cm), ammonium concentration (mg/l), nitrate concentration (mg/l), chlorophyll a concentration (mg/l), water volume (m<sup>3</sup>) and aquatic invertebrates-number of taxa and biomass (&#181;g/l). Water parameters were measured at a depth of 10 cm every</p><fig id="fig1"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref></label><caption><title> The study area: (A) Samples taken in different northern breeding sites of amphibians (<xref ref-type="table" rid="table1">Table 1</xref>); (B) Area in Israel where Pelobates syriacus are distributed</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/4-1400325x5.png"/></fig><p>two weeks during the period in which the pools were filling up. Temperature (˚C) and level of oxygen dissolved in water (dissolved oxygen concentration, mg/L<sup>−1</sup> and oxygen saturation, %) were obtained by a hand-held oxygen meter (WTW, Oxi330 set, Germany) in situ, and one liter of water was sampled for the laboratory water quality tests, including pH (WTW, pH315i, Germany, electrical conductivity (EC, mS/cm<sup>−1</sup>) corrected to 25˚C (WTW, Multiline P4, Germany) [<xref ref-type="bibr" rid="scirp.56891-ref14">14</xref>] , chlorophyll a concentration (mg/L<sup>−1</sup>) extracted from GF/F filters in 90% ethanol [<xref ref-type="bibr" rid="scirp.56891-ref14">14</xref>] , and ammonium concentrations (NH<sub>4</sub>, mg/L<sup>−1</sup>) carried out using kits based on color changes. Color changes were measured using a dedicated spectrophotometer (NOVA 60, Merck; Germany) [<xref ref-type="bibr" rid="scirp.56891-ref14">14</xref>] .</p></sec><sec id="s2_4"><title>2.4. Buried Behavior Exterminate</title><p>Fifty juvenile P. syriacus were collected from beneath stones in the Sasa and Dovev pond area of northern Israel during the summer (August and September) and maintained in an aquarium measuring 100 &#215; 30 &#215; 20 cm at the Migal Laboratory in northern Israel. In the experimental room, the temperature was maintained at 26˚C and the aquarium was half full of moist soil. A light regime of 12 hours light and 12 hours darkness was maintained. Soil moisture level was determined according to [<xref ref-type="bibr" rid="scirp.56891-ref15">15</xref>] . Fully saturated soil was considered to have a moisture level of 100% and was determined in a 500 ml glass flask half full of soil and filled with water above the soil line for 1 hr. The glass flask was turned upside down for 10 minutes in order to allow all the free water to flow out. The flask was subsequently dried in a stove for 24 hrs at a temperature of 105˚C. Full saturation was calculated according to Degani (1988).</p></sec><sec id="s2_5"><title>2.5. Terrestrial Adaption</title><p>Ten juvenile P. syriacus were maintained in a 70% soil aquarium measuring 100 &#215; 30 &#215; 20 cm at the Migal Laboratory in northern Israel for three months, and after that period, blood samples were taken. The control group was maintained in the aquarium with 4 cm water for seven days and then the samples were taken. Blood samples were taken from acclimatized juveniles (tap water and burrowing juveniles) by heart puncture using micropipettes washed with lithium heparin. The blood samples were centrifuged immediately for 15 min at 300 g, and the plasma was either analyzed immediately or frozen for analysis later. Sample preparation was according to [<xref ref-type="bibr" rid="scirp.56891-ref16">16</xref>] . Sodium, potassium and chloride in plasma were determined using methods described by [<xref ref-type="bibr" rid="scirp.56891-ref16">16</xref>] . Urea was determined using a method described by [<xref ref-type="bibr" rid="scirp.56891-ref17">17</xref>] .</p></sec><sec id="s2_6"><title>2.6. Statistical Analysis</title><p>The range of biotic and abiotic parameters of aquatic habitats was calculated, and average water parameters</p><table-wrap-group id="1"><label><xref ref-type="table" rid="table1">Table 1</xref></label><caption><title> Aquatic systems examined in northern Israel; Si―Salamandra infra immaculata; Tv―Triturus vittatus vittatus; Hs―Hyla savignyi; Bv―Bufo viridis; Ps―Pelobates syriacus; Rb―Rana bedriaga</title></caption><table-wrap id="1_1"><table><tbody><thead><tr><th align="center" valign="middle" >Water Body</th><th align="center" valign="middle" >Type of Body</th><th align="center" valign="middle" >Galilee</th><th align="center" valign="middle" >Larvae of Spadefoot toads</th><th align="center" valign="middle" >Larvae of Amphibia</th></tr></thead><tr><td align="center" valign="middle" >Nimrod Pond</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Northern Golan</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Si, Bv</td></tr><tr><td align="center" valign="middle" >Nimrod Spring</td><td align="center" valign="middle" >Continuous Spring</td><td align="center" valign="middle" >Northern Golan</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Bv</td></tr><tr><td align="center" valign="middle" >Barn Pond</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Hula Valley</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Bv</td></tr><tr><td align="center" valign="middle" >Shunit Spring</td><td align="center" valign="middle" >Seasonal Spring</td><td align="center" valign="middle" >Hula Valley</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Bv</td></tr><tr><td align="center" valign="middle" >Pond North KS</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Hula Valley</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Bv</td></tr><tr><td align="center" valign="middle" >Pond South KS</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Hula Valley</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Bv</td></tr><tr><td align="center" valign="middle" >Nahalin Spring</td><td align="center" valign="middle" >Seasonal Spring</td><td align="center" valign="middle" >Naftali Heights</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Bv, Hs</td></tr><tr><td align="center" valign="middle" >Hula NR</td><td align="center" valign="middle" >Permanent Pond</td><td align="center" valign="middle" >Hula Valley</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Bv, Rb</td></tr><tr><td align="center" valign="middle" >Sal Pond</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Central Golan</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Rb, Hs</td></tr><tr><td align="center" valign="middle" >Katzarin Pond</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Central Golan</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Tv</td></tr><tr><td align="center" valign="middle" >Paras Pond</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Central Golan</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Tv, Bv, Hs</td></tr><tr><td align="center" valign="middle" >Surman Pond</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Central Golan</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Bv, Hs</td></tr><tr><td align="center" valign="middle" >Oil Pipe Pond</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Central Golan</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Bv, Hs, Rb</td></tr><tr><td align="center" valign="middle" >Gamla Pond</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Central Golan</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Bv, Hs</td></tr><tr><td align="center" valign="middle" >Tel Bazak Pond</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Central Golan</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Bv, Hs</td></tr><tr><td align="center" valign="middle" >Darach Pond</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Central Golan</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Bv</td></tr><tr><td align="center" valign="middle" >Sbina Pond</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Central Golan</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Bv, Hs, Rb</td></tr><tr><td align="center" valign="middle" >Bageria Pond</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Southern Golan</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Rb</td></tr><tr><td align="center" valign="middle" >Irsim Pond</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Southern Golan</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Rb</td></tr><tr><td align="center" valign="middle" >Irism Pond North</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Southern Golan</td><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td></tr><tr><td align="center" valign="middle" >Nov Pond North</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Southern Golan</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Rb</td></tr><tr><td align="center" valign="middle" >Hispin Pond</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Southern Golan</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Bv</td></tr><tr><td align="center" valign="middle" >Shachar Pond</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Northern Israel</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Tv, Bv, Hs</td></tr><tr><td align="center" valign="middle" >Kash Pond</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Northern Israel</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Bv, Hs</td></tr><tr><td align="center" valign="middle" >Dalton Pond 1</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Upper Galilee</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Bv, Hs</td></tr><tr><td align="center" valign="middle" >Dalton Pond 2</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Upper Galilee</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Bv, Hs</td></tr><tr><td align="center" valign="middle" >Gush Halav Pond</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Upper Galilee</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Si, Bv</td></tr><tr><td align="center" valign="middle" >Bechania Pond</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Upper Galilee</td><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td></tr><tr><td align="center" valign="middle" >Sasa Pond</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Upper Galilee</td><td align="center" valign="middle" >Ps</td><td align="center" valign="middle" >Si, Tv, Hs, Bv</td></tr><tr><td align="center" valign="middle" >Humama Spring</td><td align="center" valign="middle" >Continuous Spring</td><td align="center" valign="middle" >Upper Galilee</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Si</td></tr><tr><td align="center" valign="middle" >Zakin Spring</td><td align="center" valign="middle" >Continuous Spring</td><td align="center" valign="middle" >Upper Galilee</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Si</td></tr><tr><td align="center" valign="middle" >Bet Jan Reservoir</td><td align="center" valign="middle" >Permanent Pond</td><td align="center" valign="middle" >Upper Galilee</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Si</td></tr><tr><td align="center" valign="middle" >Fasuta Pond</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Western Galilee</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Si</td></tr><tr><td align="center" valign="middle" >Menachem Pond</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Western Galilee</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Tv, Hs</td></tr></tbody></table></table-wrap><table-wrap id="1_2"><table><tbody><thead><tr><th align="center" valign="middle" >Shetula Pond</th><th align="center" valign="middle" >Winter Pond</th><th align="center" valign="middle" >Western Galilee</th><th align="center" valign="middle" ></th><th align="center" valign="middle" ></th><th align="center" valign="middle" ></th></tr></thead><tr><td align="center" valign="middle" >Maron Pond</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Western Galilee</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Si, Hs</td><td align="center" valign="middle" ></td></tr><tr><td align="center" valign="middle" >Sumara Pond</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Western Galilee</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Si</td><td align="center" valign="middle" ></td></tr><tr><td align="center" valign="middle" >Tel Arad Pond</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Western Galilee</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Si, Hs, Tv</td><td align="center" valign="middle" ></td></tr><tr><td align="center" valign="middle" >Sasa Rock Pool</td><td align="center" valign="middle" >Rock Pool (all year)</td><td align="center" valign="middle" >Upper Galilee</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Si</td><td align="center" valign="middle" ></td></tr><tr><td align="center" valign="middle" >Tel Dan</td><td align="center" valign="middle" >Continuous Stream</td><td align="center" valign="middle" >Northern Galilee</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Si</td><td align="center" valign="middle" ></td></tr><tr><td align="center" valign="middle" >Balad Spring</td><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Si, Hs</td><td align="center" valign="middle" ></td></tr><tr><td align="center" valign="middle" >Navoraya Spring</td><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Si, Hs, Rb</td><td align="center" valign="middle" ></td></tr><tr><td align="center" valign="middle" >Maalot Rock Pool</td><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Si</td><td align="center" valign="middle" ></td></tr><tr><td align="center" valign="middle" >Manof Pool</td><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Tv, Hs, Bv, Ps Si, Bv</td><td align="center" valign="middle" ></td></tr><tr><td align="center" valign="middle" >Kash Pool</td><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Ps</td><td align="center" valign="middle" >Si, Tv, Hs, Bv, Rb</td><td align="center" valign="middle" ></td></tr><tr><td align="center" valign="middle" >Dovev Pool</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Upper Galilee</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Tv, Hs, Bv, Ps, Si</td><td align="center" valign="middle" ></td></tr><tr><td align="center" valign="middle" >Matityahu Pool</td><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td></tr><tr><td align="center" valign="middle" >Lehavot Pool</td><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Hs, Rb</td><td align="center" valign="middle" ></td></tr><tr><td align="center" valign="middle" >Fara Pool</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >Northern Galilee</td><td align="center" valign="middle" >Ps</td><td align="center" valign="middle"  colspan="2"  >Si, Tv, Hs, Bv, Rb</td></tr><tr><td align="center" valign="middle" >Raihaniya Pool</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Upper Galilee</td><td align="center" valign="middle" >Ps</td><td align="center" valign="middle"  colspan="2"  >Bv</td></tr><tr><td align="center" valign="middle" >Elrom Pond</td><td align="center" valign="middle" >Winter Pond</td><td align="center" valign="middle" >Northern Golan</td><td align="center" valign="middle" >Ps</td><td align="center" valign="middle"  colspan="2"  ></td></tr></tbody></table></table-wrap></table-wrap-group><p>were analyzed by one-way analysis of variance (ANOVA), with the level of significance between groups set at p &lt; 0.05 (ANOVA) (Tukey test).</p></sec></sec><sec id="s3"><title>3. Results</title><p>Spadefoot toads (Pelobates syriacus) are found in northern Israel from the north in the Upper Galilee and Golan Heights (annual rainfall range of 500 - 1000 mm) (<xref ref-type="fig" rid="fig1">Figure 1</xref>), to the southern coastal plain (annual rainfall of about 250 mm ). Among the 51 different breeding places of amphibians, only certain ponds (<xref ref-type="table" rid="table1">Table 1</xref>) are used by Spadefoot toads and metamorphosed populations were found around those ponds. Water in the breeding places of Spadefoot toads is available for more a few months and is sometimes available all year round, the time for the larvae to grow and complete metamorphosis (<xref ref-type="table" rid="table2">Table 2</xref>). Spadefoot toads can breed several times during the warm season, usually when there is a drop in barometric pressure, two or more inches of rainfall, and in the darkness of night.</p><p>The life cycle of Spadefoot toads is presented in <xref ref-type="fig" rid="fig2">Figure 2</xref>. Males are the first to arrive at the pond, sending out a mating call. This call consists of a short, explosive “wonk,” similar to the call of a crow. The females then arrive, and breeding occurs underwater. Breeding time in Israel varies according to location and geographical and ecological conditions. It takes place in March-April in northern Israel, Upper Galilee and the Golan Heights, and earlier in the lower locations and in central Israel. In central Israel, the breeding period is during the winter. The amplexus of Spadefoot toads involves the male holding the female above the back legs, they swim together, and the female lays 2 to 4 lies of eggs (<xref ref-type="fig" rid="fig2">Figure 2</xref>). The number of eggs differs, and ranges between 2000 to 10,000 per female. Larvae growth and complex metamorphosis take place in northern Israel during the summer and early autumn until October. Larvae growth in various breeding places is presented in <xref ref-type="fig" rid="fig3">Figure 3</xref>.</p><p>There is no information on adult terrestrial activity of Spadefoot toads. Considering the spatial distribution of rain pools and the dispersal ability of juvenile adults of only about 2 - 4 km, it seems that most of the population is isolated.</p><p>The results of this experiment show that a negative correlation exists between the percentage of toads burrowing and soil moisture levels. In soil having a low moisture level (40%), a relatively high percentage of toads</p><fig id="fig2"  position="float"><label><xref ref-type="fig" rid="fig2">Figure 2</xref></label><caption><title> Life cycle of P. syriacus: juveniles (A) and mature females (B); Amplexuses (Cogălniceanu et al., 2013) (C); Eggs (D); Tadpole (E); Metamorphosis (F)</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/4-1400325x6.png"/></fig><fig-group id="fig3"><label><xref ref-type="fig" rid="fig3">Figure 3</xref></label><caption><title> Growth rates of larvae of Pelobates syriacus. The Y axis shows larval size in mean of full length (cm), and the X axis shows time periods in the number of days that larvae had spent in the water body until they reached metamorphosis.</title></caption><fig id ="fig3_1"><label></label><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/4-1400325x7.png"/></fig><fig id ="fig3_2"><label></label><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/4-1400325x8.png"/></fig><fig id ="fig3_3"><label></label><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/4-1400325x9.png"/></fig><fig id ="fig3_4"><label></label><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/4-1400325x10.png"/></fig></fig-group><p>(73%) was buried compared to a low percentage (9%) at a high soil moisture level (100%) (<xref ref-type="fig" rid="fig4">Figure 4</xref> and <xref ref-type="fig" rid="fig5">Figure 5</xref>), and the concentration of plasma in the soil was higher (<xref ref-type="fig" rid="fig6">Figure 6</xref>). During burrowing in the soil, the urea in the plasma increased dramatically compared to other components.</p></sec><sec id="s4"><title>4. Discussion</title><p>Spadefoot toads (Pelobates syriacus) are highly specialized burrowing and nocturnal species having a narrow</p><table-wrap id="table2" ><label><xref ref-type="table" rid="table2">Table 2</xref></label><caption><title> Mean values and standard deviation (SD) of biotic and abiotic water quality parameters measured in breeding sites of Pelobates syriacus</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >Site</th><th align="center" valign="middle" >Taxa (no.)</th><th align="center" valign="middle" >Mean Biomass (&#181;g/l)</th><th align="center" valign="middle" >Rangechlor<sup>a</sup> (mg/l)</th><th align="center" valign="middle" >Mean hyd (days)</th><th align="center" valign="middle" >Mean Max. Volume (m<sup>3</sup>)</th><th align="center" valign="middle" >Residential/ Agricultural Areas</th></tr></thead><tr><td align="center" valign="middle" >Kash</td><td align="center" valign="middle" >6</td><td align="center" valign="middle" >1.2E+05</td><td align="center" valign="middle" >1.7 - 222.4</td><td align="center" valign="middle" >172 &#177; 8</td><td align="center" valign="middle" >2335 (444)</td><td align="center" valign="middle" >naa</td></tr><tr><td align="center" valign="middle" >Dovev</td><td align="center" valign="middle" >8</td><td align="center" valign="middle" >3.3E+03</td><td align="center" valign="middle" >1.9 - 89.2</td><td align="center" valign="middle" >183 &#177; 16</td><td align="center" valign="middle" >278 (31)</td><td align="center" valign="middle" >naa</td></tr><tr><td align="center" valign="middle" >Matityahu</td><td align="center" valign="middle" >10</td><td align="center" valign="middle" >5.9E+04</td><td align="center" valign="middle" >0.7 - 43.1</td><td align="center" valign="middle" >210 &#177; 4</td><td align="center" valign="middle" >4839 (847)</td><td align="center" valign="middle" >naa</td></tr><tr><td align="center" valign="middle" >Lehavot</td><td align="center" valign="middle" >6</td><td align="center" valign="middle" >2.3E+04</td><td align="center" valign="middle" >1.0 - 65.1</td><td align="center" valign="middle" >130 &#177; 19</td><td align="center" valign="middle" >10272 (2291)</td><td align="center" valign="middle" >naa</td></tr><tr><td align="center" valign="middle" >Sasa</td><td align="center" valign="middle" >7</td><td align="center" valign="middle" >1.7E+05</td><td align="center" valign="middle" >1.3 - 347.7</td><td align="center" valign="middle" >215 &#177; 18</td><td align="center" valign="middle" >11463 (1559)</td><td align="center" valign="middle" >naa</td></tr><tr><td align="center" valign="middle" >Fara</td><td align="center" valign="middle" >8</td><td align="center" valign="middle" >9.6E+05</td><td align="center" valign="middle" >0.9 - 581.7</td><td align="center" valign="middle" >297 &#177; 54</td><td align="center" valign="middle" >1109 (107)</td><td align="center" valign="middle" >naa</td></tr><tr><td align="center" valign="middle" >Raihania</td><td align="center" valign="middle" >7</td><td align="center" valign="middle" >3.2E+05</td><td align="center" valign="middle" >0.6 - 237.0</td><td align="center" valign="middle" >271 &#177; 18</td><td align="center" valign="middle" >7956 (390)</td><td align="center" valign="middle" >nra/naa</td></tr></tbody></table></table-wrap><p>chlor. <sup>a</sup>chlorophyll a; hyd―hydroperiods; ay―all year; nra―near residential areas; naa―near agricultural areas.</p><fig id="fig4"  position="float"><label><xref ref-type="fig" rid="fig4">Figure 4</xref></label><caption><title> The effect of soil moisture on burrowing behavior of Spadefoot toads (Pelobates syriacus)</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/4-1400325x11.png"/></fig><fig id="fig5"  position="float"><label><xref ref-type="fig" rid="fig5">Figure 5</xref></label><caption><title> Spadefoot toads dehydrated under different conditions: in air, burrowed in soil and in water</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/4-1400325x12.png"/></fig><fig id="fig6"  position="float"><label><xref ref-type="fig" rid="fig6">Figure 6</xref></label><caption><title> Changes in salinity and composition of plasma in juvenile Pelobates syriacus burrowed in soil and in water</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/4-1400325x13.png"/></fig><p>ecological niche among amphibians in Israel, and all of them are found in relatively extreme conditions [<xref ref-type="bibr" rid="scirp.56891-ref6">6</xref>] . Spadefoot toad tadpoles are the largest among Israel’s amphibian species [<xref ref-type="bibr" rid="scirp.56891-ref14">14</xref>] [<xref ref-type="bibr" rid="scirp.56891-ref18">18</xref>] , and the larval period can last several months until metamorphosis [<xref ref-type="bibr" rid="scirp.56891-ref4">4</xref>] [<xref ref-type="bibr" rid="scirp.56891-ref18">18</xref>] , as is supported by the present study. However, the selection of breeding places included only winter ponds where water was available for a few months, as was found in Europe [<xref ref-type="bibr" rid="scirp.56891-ref1">1</xref>] [<xref ref-type="bibr" rid="scirp.56891-ref2">2</xref>] and in the present study. According to previous studies at the southern border of its distribution of larvae growth and complete metamorphosis, we suggested that the selection of ponds where water was available for a few months should be correlated to the phenomena of this species (Pelobates syriacus)―large tadpoles and long periods to complete metamorphosis, as was found in the present study and previous studies [<xref ref-type="bibr" rid="scirp.56891-ref5">5</xref>] , and to the ecological conditions and water quality of the breeding places, e.g., the water temperature must be above 20˚C and most of the time above 25˚C for Spadefoot toad tadpoles to complete metamorphosis after a relatively long growth period (more than three months) [<xref ref-type="bibr" rid="scirp.56891-ref4">4</xref>] [<xref ref-type="bibr" rid="scirp.56891-ref5">5</xref>] [<xref ref-type="bibr" rid="scirp.56891-ref18">18</xref>] .</p><p>Due to their secretive behavior (nocturnal activity, weak underwater breeding call and cryptic coloration), their adaptation to semi-arid environments is not well-documented in central Israel [<xref ref-type="bibr" rid="scirp.56891-ref8">8</xref>] [<xref ref-type="bibr" rid="scirp.56891-ref19">19</xref>] and northern Israel [<xref ref-type="bibr" rid="scirp.56891-ref6">6</xref>] [<xref ref-type="bibr" rid="scirp.56891-ref7">7</xref>] [<xref ref-type="bibr" rid="scirp.56891-ref20">20</xref>] , and overall there is a scarcity of information regarding this genus. According to the results of the present study, the selection and adaptation to ecological conditions is not done according to the aquatic phase of Spadefoot toads but following metamorphosis. This hypothesis, which is supported by relatively many studies on the conditions of larvae growth of Spadefoot toads [<xref ref-type="bibr" rid="scirp.56891-ref14">14</xref>] , shows that the water analysis of larvae is suitable for other amphibians in Israel, and that the distribution of Spadefoot toads is in drier conditions [<xref ref-type="bibr" rid="scirp.56891-ref21">21</xref>] . The burrowing behavior of metamorphosed Spadefoot toads preventing dehydration, as was found in the present study, is very important adaptation to terrestrial life. The accumulation of urea and electrolytes in the plasma during burrowing behavior seems to be a physiological adaptation, as was found in the present study, and is supported by previous research on this species [<xref ref-type="bibr" rid="scirp.56891-ref7">7</xref>] [<xref ref-type="bibr" rid="scirp.56891-ref22">22</xref>] . The only better adaptation to terrestrial life in amphibians in Israel is Green toad (Pseudepidalea viridis (Syn. Bufo viridis)) whose burrowing behavior is less than Spadefoot toads but has a higher adaptation to terrestrial life [<xref ref-type="bibr" rid="scirp.56891-ref17">17</xref>] [<xref ref-type="bibr" rid="scirp.56891-ref23">23</xref>] [<xref ref-type="bibr" rid="scirp.56891-ref24">24</xref>] . 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