Life on the edge – to which degree does phreatic water sustain vegetation in the periphery of the Taklamakan Desert?
Identifieur interne : 000E89 ( Istex/Corpus ); précédent : 000E88; suivant : 000E90Life on the edge – to which degree does phreatic water sustain vegetation in the periphery of the Taklamakan Desert?
Auteurs : Helge Bruelheide ; Beatrix Vonlanthen ; Ute Jandt ; Frank M. Thomas ; Andrea Foetzki ; Dirk Gries ; Gang Wang ; Ximing Zhang ; Michael RungeSource :
- Applied Vegetation Science [ 1402-2001 ] ; 2010-02.
English descriptors
- KwdEn :
Abstract
Questions: Do the vegetation‐specific patterns in the forelands of river oases of the Taklamakan Desert provide clues to the degree to which a vegetation type depends on unsaturated soil moisture, brought about by extensive floodings, or phreatic water?
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DOI: 10.1111/j.1654-109X.2009.01050.x
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ISTEX:B8DCE0A116A061EE09A7BFFDF676DAC909EFB772Le document en format XML
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Thomas</name><affiliation><mods:affiliation>Department of Geobotany, University of Trier, Behringstrasse 21, DE–54296 Trier, Germany; E‐mail thomasf@uni‐trier.de</mods:affiliation></affiliation></author><author><name sortKey="Foetzki, Andrea" sort="Foetzki, Andrea" uniqKey="Foetzki A" first="Andrea" last="Foetzki">Andrea Foetzki</name><affiliation><mods:affiliation>Agroscope Reckenholz‐Tänikon Research Station ART, Biodiversity and Environmental Management, Reckenholzstrasse 191, CH–8046 Zurich, Switzerland; E‐mail andrea.foetzki@art.admin.ch</mods:affiliation></affiliation></author><author><name sortKey="Gries, Dirk" sort="Gries, Dirk" uniqKey="Gries D" first="Dirk" last="Gries">Dirk Gries</name><affiliation><mods:affiliation>XLAB, Justus‐von‐Liebig‐Weg 8, DE–37077 Göttingen, Germany; E‐mail dgries@gwdg.de</mods:affiliation></affiliation></author><author><name sortKey="Wang, Gang" sort="Wang, Gang" uniqKey="Wang G" first="Gang" last="Wang">Gang Wang</name><affiliation><mods:affiliation>Department of Biology, Key Laboratory of Arid and Grassland Agroecology, Lanzhou University, Tianshui South Road 222, 730000 Lanzhou, China; E‐mail wangg@lzu.edu.cn</mods:affiliation></affiliation></author><author><name sortKey="Zhang, Ximing" sort="Zhang, Ximing" uniqKey="Zhang X" first="Ximing" last="Zhang">Ximing Zhang</name><affiliation><mods:affiliation>Chinese Academy of Sciences, Xinjiang Institute of Ecology and Geography, 40 South Beijing Road, 830011 Urumqi, China; E‐mail zhxm@ms.xjb.ac.cn</mods:affiliation></affiliation></author><author><name sortKey="Runge, Michael" sort="Runge, Michael" uniqKey="Runge M" first="Michael" last="Runge">Michael Runge</name><affiliation><mods:affiliation>Department of Ecology and Ecosystem Research, Albrecht‐von‐Haller‐Institute for Plant Sciences, University of Göttingen, Untere Karspuele 2, DE–37073 Göttingen, Germany; E‐mail mrunge@gwdg.de</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Applied Vegetation Science</title><idno type="ISSN">1402-2001</idno><idno type="eISSN">1654-109X</idno><imprint><publisher>Blackwell Publishing Ltd</publisher><pubPlace>Oxford, UK</pubPlace><date type="published" when="2010-02">2010-02</date><biblScope unit="volume">13</biblScope><biblScope unit="issue">1</biblScope><biblScope unit="page" from="56">56</biblScope><biblScope unit="page" to="71">71</biblScope></imprint><idno type="ISSN">1402-2001</idno></series><idno type="istex">B8DCE0A116A061EE09A7BFFDF676DAC909EFB772</idno><idno type="DOI">10.1111/j.1654-109X.2009.01050.x</idno><idno type="ArticleID">AVSC1050</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">1402-2001</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>China</term><term>Desert vegetation</term><term>Groundwater map</term><term>Oasis vegetation</term><term>Phreatophytes</term><term>Soil matric potential</term><term>Soil texture</term><term>Soil water content</term><term>Soil water retention curves</term><term>Sum exceedance values</term><term>Vegetation map</term><term>Xinjiang</term></keywords></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract">Questions: Do the vegetation‐specific patterns in the forelands of river oases of the Taklamakan Desert provide clues to the degree to which a vegetation type depends on unsaturated soil moisture, brought about by extensive floodings, or phreatic water?</div></front></TEI><istex><corpusName>wiley</corpusName><author><json:item><name>Helge Bruelheide</name><affiliations><json:string>Martin Luther University Halle Wittenberg, Institute of Biology/Geobotany and Botanical Garden, Am Kirchtor 1, DE–06108 Halle, Germany</json:string><json:string>E-mail: helge.bruelheide@botanik.uni‐halle.de</json:string></affiliations></json:item><json:item><name>Beatrix Vonlanthen</name><affiliations><json:string>Martin Luther University Halle Wittenberg, Institute of Biology/Geobotany and Botanical Garden, Am Kirchtor 1, DE–06108 Halle, Germany</json:string><json:string>E‐mail beatrix.vonlanthen@botanik.uni‐halle.de</json:string></affiliations></json:item><json:item><name>Ute Jandt</name><affiliations><json:string>Martin Luther University Halle Wittenberg, Institute of Biology/Geobotany and Botanical Garden, Am Kirchtor 1, DE–06108 Halle, Germany</json:string><json:string>E‐mail ute.jandt@botanik.uni‐halle.de</json:string></affiliations></json:item><json:item><name>Frank M. Thomas</name><affiliations><json:string>Department of Geobotany, University of Trier, Behringstrasse 21, DE–54296 Trier, Germany; E‐mail thomasf@uni‐trier.de</json:string></affiliations></json:item><json:item><name>Andrea Foetzki</name><affiliations><json:string>Agroscope Reckenholz‐Tänikon Research Station ART, Biodiversity and Environmental Management, Reckenholzstrasse 191, CH–8046 Zurich, Switzerland; E‐mail andrea.foetzki@art.admin.ch</json:string></affiliations></json:item><json:item><name>Dirk Gries</name><affiliations><json:string>XLAB, Justus‐von‐Liebig‐Weg 8, DE–37077 Göttingen, Germany; E‐mail dgries@gwdg.de</json:string></affiliations></json:item><json:item><name>Gang Wang</name><affiliations><json:string>Department of Biology, Key Laboratory of Arid and Grassland Agroecology, Lanzhou University, Tianshui South Road 222, 730000 Lanzhou, China; E‐mail wangg@lzu.edu.cn</json:string></affiliations></json:item><json:item><name>Ximing Zhang</name><affiliations><json:string>Chinese Academy of Sciences, Xinjiang Institute of Ecology and Geography, 40 South Beijing Road, 830011 Urumqi, China; E‐mail zhxm@ms.xjb.ac.cn</json:string></affiliations></json:item><json:item><name>Michael Runge</name><affiliations><json:string>Department of Ecology and Ecosystem Research, Albrecht‐von‐Haller‐Institute for Plant Sciences, University of Göttingen, Untere Karspuele 2, DE–37073 Göttingen, Germany; E‐mail mrunge@gwdg.de</json:string></affiliations></json:item></author><subject><json:item><lang><json:string>eng</json:string></lang><value>China</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>Desert vegetation</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>Groundwater map</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>Oasis vegetation</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>Phreatophytes</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>Soil matric potential</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>Soil texture</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>Soil water content</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>Soil water retention curves</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>Sum exceedance values</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>Vegetation map</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>Xinjiang</value></json:item></subject><articleId><json:string>AVSC1050</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>article</json:string></originalGenre><qualityIndicators><score>5.456</score><pdfVersion>1.3</pdfVersion><pdfPageSize>595.276 x 782.362 pts</pdfPageSize><refBibsNative>true</refBibsNative><abstractCharCount>253</abstractCharCount><pdfWordCount>8831</pdfWordCount><pdfCharCount>54052</pdfCharCount><pdfPageCount>16</pdfPageCount><abstractWordCount>38</abstractWordCount></qualityIndicators><title>Life on the edge – to which degree does phreatic water sustain vegetation in the periphery of the Taklamakan Desert?</title><refBibs><json:item><author><json:item><name>H. 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Lu</name></json:item></author><host><volume>6</volume><pages><last>98</last><first>89</first></pages><issue>(Suppl.)</issue><author></author><title>Die Erde</title></host><title>A study on the formation and development of Aeolian landforms and the trend of environmental changes in the lower reaches of the Keriya River, Central Taklimakan Desert</title></json:item></refBibs><genre><json:string>article</json:string></genre><host><volume>13</volume><publisherId><json:string>AVSC</json:string></publisherId><pages><total>16</total><last>71</last><first>56</first></pages><issn><json:string>1402-2001</json:string></issn><issue>1</issue><genre><json:string>journal</json:string></genre><language><json:string>unknown</json:string></language><eissn><json:string>1654-109X</json:string></eissn><title>Applied Vegetation Science</title><doi><json:string>10.1111/(ISSN)1654-109X</json:string></doi></host><categories><wos><json:string>science</json:string><json:string>plant sciences</json:string><json:string>forestry</json:string><json:string>ecology</json:string></wos><scienceMetrix><json:string>natural sciences</json:string><json:string>biology</json:string><json:string>ecology</json:string></scienceMetrix></categories><publicationDate>2010</publicationDate><copyrightDate>2010</copyrightDate><doi><json:string>10.1111/j.1654-109X.2009.01050.x</json:string></doi><id>B8DCE0A116A061EE09A7BFFDF676DAC909EFB772</id><score>0.39590976</score><fulltext><json:item><extension>pdf</extension><original>true</original><mimetype>application/pdf</mimetype><uri>https://api.istex.fr/document/B8DCE0A116A061EE09A7BFFDF676DAC909EFB772/fulltext/pdf</uri></json:item><json:item><extension>zip</extension><original>false</original><mimetype>application/zip</mimetype><uri>https://api.istex.fr/document/B8DCE0A116A061EE09A7BFFDF676DAC909EFB772/fulltext/zip</uri></json:item><istex:fulltextTEI uri="https://api.istex.fr/document/B8DCE0A116A061EE09A7BFFDF676DAC909EFB772/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a" type="main" xml:lang="en">Life on the edge – to which degree does phreatic water sustain vegetation in the periphery of the Taklamakan Desert?</title></titleStmt><publicationStmt><authority>ISTEX</authority><publisher>Blackwell Publishing Ltd</publisher><pubPlace>Oxford, UK</pubPlace><availability><p>© 2009 International Association for Vegetation Science</p></availability><date>2010</date></publicationStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a" type="main" xml:lang="en">Life on the edge – to which degree does phreatic water sustain vegetation in the periphery of the Taklamakan Desert?</title><author xml:id="author-1"><persName><forename type="first">Helge</forename><surname>Bruelheide</surname></persName><email>helge.bruelheide@botanik.uni‐halle.de</email><affiliation>Martin Luther University Halle Wittenberg, Institute of Biology/Geobotany and Botanical Garden, Am Kirchtor 1, DE–06108 Halle, Germany</affiliation></author><author xml:id="author-2"><persName><forename type="first">Beatrix</forename><surname>Vonlanthen</surname></persName><affiliation>Martin Luther University Halle Wittenberg, Institute of Biology/Geobotany and Botanical Garden, Am Kirchtor 1, DE–06108 Halle, Germany</affiliation><affiliation>E‐mail beatrix.vonlanthen@botanik.uni‐halle.de</affiliation></author><author xml:id="author-3"><persName><forename type="first">Ute</forename><surname>Jandt</surname></persName><affiliation>Martin Luther University Halle Wittenberg, Institute of Biology/Geobotany and Botanical Garden, Am Kirchtor 1, DE–06108 Halle, Germany</affiliation><affiliation>E‐mail ute.jandt@botanik.uni‐halle.de</affiliation></author><author xml:id="author-4"><persName><forename type="first">Frank M.</forename><surname>Thomas</surname></persName><affiliation>Department of Geobotany, University of Trier, Behringstrasse 21, DE–54296 Trier, Germany; E‐mail thomasf@uni‐trier.de</affiliation></author><author xml:id="author-5"><persName><forename type="first">Andrea</forename><surname>Foetzki</surname></persName><affiliation>Agroscope Reckenholz‐Tänikon Research Station ART, Biodiversity and Environmental Management, Reckenholzstrasse 191, CH–8046 Zurich, Switzerland; E‐mail andrea.foetzki@art.admin.ch</affiliation></author><author xml:id="author-6"><persName><forename type="first">Dirk</forename><surname>Gries</surname></persName><affiliation>XLAB, Justus‐von‐Liebig‐Weg 8, DE–37077 Göttingen, Germany; E‐mail dgries@gwdg.de</affiliation></author><author xml:id="author-7"><persName><forename type="first">Gang</forename><surname>Wang</surname></persName><affiliation>Department of Biology, Key Laboratory of Arid and Grassland Agroecology, Lanzhou University, Tianshui South Road 222, 730000 Lanzhou, China; E‐mail wangg@lzu.edu.cn</affiliation></author><author xml:id="author-8"><persName><forename type="first">Ximing</forename><surname>Zhang</surname></persName><affiliation>Chinese Academy of Sciences, Xinjiang Institute of Ecology and Geography, 40 South Beijing Road, 830011 Urumqi, China; E‐mail zhxm@ms.xjb.ac.cn</affiliation></author><author xml:id="author-9"><persName><forename type="first">Michael</forename><surname>Runge</surname></persName><affiliation>Department of Ecology and Ecosystem Research, Albrecht‐von‐Haller‐Institute for Plant Sciences, University of Göttingen, Untere Karspuele 2, DE–37073 Göttingen, Germany; E‐mail mrunge@gwdg.de</affiliation></author></analytic><monogr><title level="j">Applied Vegetation Science</title><idno type="pISSN">1402-2001</idno><idno type="eISSN">1654-109X</idno><idno type="DOI">10.1111/(ISSN)1654-109X</idno><imprint><publisher>Blackwell Publishing Ltd</publisher><pubPlace>Oxford, UK</pubPlace><date type="published" when="2010-02"></date><biblScope unit="volume">13</biblScope><biblScope unit="issue">1</biblScope><biblScope unit="page" from="56">56</biblScope><biblScope unit="page" to="71">71</biblScope></imprint></monogr><idno type="istex">B8DCE0A116A061EE09A7BFFDF676DAC909EFB772</idno><idno type="DOI">10.1111/j.1654-109X.2009.01050.x</idno><idno type="ArticleID">AVSC1050</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>2010</date></creation><langUsage><language ident="en">en</language></langUsage><abstract><p>Questions: Do the vegetation‐specific patterns in the forelands of river oases of the Taklamakan Desert provide clues to the degree to which a vegetation type depends on unsaturated soil moisture, brought about by extensive floodings, or phreatic water?</p></abstract><abstract><p>Location: Foreland of the Qira oasis on the southern rim of the Taklamakan Desert, Xinjiang Uygur Autonomous Region, China.</p></abstract><abstract><p>Methods: A vegetation map was prepared using a SPOT satellite image and ground truthing. Measurements of soil water contents were obtained from a flooding experiment and transformed into water potentials. Sum excedance values were calculated as the percentage of days on which different thresholds of soil water potentials were transgressed. Groundwater depth was mapped by drilling 30 groundwater holes and extrapolating the distances to the whole study area.</p></abstract><abstract><p>Results: The vegetation was characterized by only six dominant or codominant species: Alhagi sparsifolia, Karelinia caspia, Populus euphratica, Tamarix ramosissima, Calligonum caput‐medusae and Phragmites australis. The vegetation patterns encountered lacked any linear features typical of phreatophytes, thus not allowing direct conclusions on the type of the sustaining water sources. Soil water potentials never transgressed a threshold of pF 5 (−10 MPa) in horizons above the capillary fringe during periods without inundation, thus representing water not accessible for plants. Depth to the groundwater ranged between 2.3 and 17.5 m among plots and varied between 1.7 and 8.0 m within a plot owing to dune relief. The seven main vegetation types showed distinct niches of groundwater depths, corresponding to the observed concentric arrangement of vegetation types around the oasis.</p></abstract><abstract><p>Conclusions: Inundation by flooding and unsaturated soil moisture are irrelevant for the foreland vegetation water supply. Although distances to the groundwater table can reach about 20 m, which is exceptionally large for phreatophytes, groundwater is the only water source for all vegetation types in the oasis foreland. In consequence, successful maintenance of oasis foreland vegetation will crucially depend on providing non‐declining ground water tables.</p></abstract><textClass xml:lang="en"><keywords scheme="keyword"><list><head>keywords</head><item><term>China</term></item><item><term>Desert vegetation</term></item><item><term>Groundwater map</term></item><item><term>Oasis vegetation</term></item><item><term>Phreatophytes</term></item><item><term>Soil matric potential</term></item><item><term>Soil texture</term></item><item><term>Soil water content</term></item><item><term>Soil water retention curves</term></item><item><term>Sum exceedance values</term></item><item><term>Vegetation map</term></item><item><term>Xinjiang</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="2010-02">Published</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/B8DCE0A116A061EE09A7BFFDF676DAC909EFB772/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="Wiley, elements deleted: body"><istex:xmlDeclaration>version="1.0" encoding="UTF-8" standalone="yes"</istex:xmlDeclaration><istex:document><component version="2.0" type="serialArticle" xml:lang="en"><header><publicationMeta level="product"><publisherInfo><publisherName>Blackwell Publishing Ltd</publisherName><publisherLoc>Oxford, UK</publisherLoc></publisherInfo><doi origin="wiley" registered="yes">10.1111/(ISSN)1654-109X</doi><issn type="print">1402-2001</issn><issn type="electronic">1654-109X</issn><idGroup><id type="product" value="AVSC"></id><id type="publisherDivision" value="ST"></id></idGroup><titleGroup><title type="main" sort="APPLIED VEGETATION SCIENCE">Applied Vegetation Science</title></titleGroup></publicationMeta><publicationMeta level="part" position="02001"><doi origin="wiley">10.1111/avsc.2010.13.issue-1</doi><numberingGroup><numbering type="journalVolume" number="13">13</numbering><numbering type="journalIssue" number="1">1</numbering></numberingGroup><coverDate startDate="2010-02">February 2010</coverDate></publicationMeta><publicationMeta level="unit" type="article" position="7" status="forIssue"><doi origin="wiley">10.1111/j.1654-109X.2009.01050.x</doi><idGroup><id type="unit" value="AVSC1050"></id><id type="supplier" value="1050"></id></idGroup><countGroup><count type="pageTotal" number="16"></count></countGroup><titleGroup><title type="tocHeading1">Original Articles</title></titleGroup><copyright>© 2009 International Association for Vegetation Science</copyright><eventGroup><event type="firstOnline" date="2009-09-18"></event><event type="publishedOnlineFinalForm" date="2010-01-12"></event><event type="xmlConverted" agent="Converter:BPG_TO_WML3G version:2.3.6 mode:FullText source:FullText result:FullText" date="2010-04-21"></event><event type="xmlConverted" agent="Converter:WILEY_ML3G_TO_WILEY_ML3GV2 version:4.0.1" date="2014-03-15"></event><event type="xmlConverted" agent="Converter:WML3G_To_WML3G version:4.1.7 mode:FullText,remove_FC" date="2014-10-15"></event></eventGroup><numberingGroup><numbering type="pageFirst" number="56">56</numbering><numbering type="pageLast" number="71">71</numbering></numberingGroup><correspondenceTo><sup>*</sup>Corresponding author; E‐mail <email normalForm="helge.bruelheide@botanik.uni-halle.de">helge.bruelheide@botanik.uni‐halle.de</email></correspondenceTo><linkGroup><link type="toTypesetVersion" href="file:AVSC.AVSC1050.pdf"></link></linkGroup></publicationMeta><contentMeta><unparsedEditorialHistory>Received 6 May 2009;Accepted 7 July 2009.</unparsedEditorialHistory><countGroup><count type="figureTotal" number="5"></count><count type="tableTotal" number="1"></count><count type="formulaTotal" number="0"></count><count type="referenceTotal" number="76"></count><count type="wordTotal" number="11254"></count><count type="linksCrossRef" number="118"></count></countGroup><titleGroup><title type="main">Life on the edge – to which degree does phreatic water sustain vegetation in the periphery of the Taklamakan Desert?</title><title type="shortAuthors">B<sc>ruelheide</sc>, H. <sc>et al</sc>.</title><title type="short">L<sc>ife on the edge</sc></title></titleGroup><creators><creator creatorRole="author" xml:id="cr1" affiliationRef="#a1" corresponding="yes"><personName><givenNames>Helge</givenNames><familyName>Bruelheide</familyName></personName></creator><creator creatorRole="author" xml:id="cr2" affiliationRef="#a1 #a2"><personName><givenNames>Beatrix</givenNames><familyName>Vonlanthen</familyName></personName></creator><creator creatorRole="author" xml:id="cr3" affiliationRef="#a1 #a3"><personName><givenNames>Ute</givenNames><familyName>Jandt</familyName></personName></creator><creator creatorRole="author" xml:id="cr4" affiliationRef="#a4"><personName><givenNames>Frank M.</givenNames><familyName>Thomas</familyName></personName></creator><creator creatorRole="author" xml:id="cr5" affiliationRef="#a5"><personName><givenNames>Andrea</givenNames><familyName>Foetzki</familyName></personName></creator><creator creatorRole="author" xml:id="cr6" affiliationRef="#a6"><personName><givenNames>Dirk</givenNames><familyName>Gries</familyName></personName></creator><creator creatorRole="author" xml:id="cr7" affiliationRef="#a7"><personName><givenNames>Gang</givenNames><familyName>Wang</familyName></personName></creator><creator creatorRole="author" xml:id="cr8" affiliationRef="#a8"><personName><givenNames>Ximing</givenNames><familyName>Zhang</familyName></personName></creator><creator creatorRole="author" xml:id="cr9" affiliationRef="#a9"><personName><givenNames>Michael</givenNames><familyName>Runge</familyName></personName></creator></creators><affiliationGroup><affiliation xml:id="a1" countryCode="DE"><unparsedAffiliation>Martin Luther University Halle Wittenberg, Institute of Biology/Geobotany and Botanical Garden, Am Kirchtor 1, DE–06108 Halle, Germany</unparsedAffiliation></affiliation><affiliation xml:id="a2"><unparsedAffiliation> E‐mail <email normalForm="beatrix.vonlanthen@botanik.uni-halle.de">beatrix.vonlanthen@botanik.uni‐halle.de</email></unparsedAffiliation></affiliation><affiliation xml:id="a3"><unparsedAffiliation> E‐mail <email normalForm="ute.jandt@botanik.uni-halle.de">ute.jandt@botanik.uni‐halle.de</email></unparsedAffiliation></affiliation><affiliation xml:id="a4" countryCode="DE"><unparsedAffiliation> Department of Geobotany, University of Trier, Behringstrasse 21, DE–54296 Trier, Germany; E‐mail <email normalForm="thomasf@uni-trier.de">thomasf@uni‐trier.de</email></unparsedAffiliation></affiliation><affiliation xml:id="a5" countryCode="CH"><unparsedAffiliation> Agroscope Reckenholz‐Tänikon Research Station ART, Biodiversity and Environmental Management, Reckenholzstrasse 191, CH–8046 Zurich, Switzerland; E‐mail <email normalForm="andrea.foetzki@art.admin.ch">andrea.foetzki@art.admin.ch</email></unparsedAffiliation></affiliation><affiliation xml:id="a6" countryCode="DE"><unparsedAffiliation> XLAB, Justus‐von‐Liebig‐Weg 8, DE–37077 Göttingen, Germany; E‐mail <email normalForm="dgries@gwdg.de">dgries@gwdg.de</email></unparsedAffiliation></affiliation><affiliation xml:id="a7" countryCode="CN"><unparsedAffiliation> Department of Biology, Key Laboratory of Arid and Grassland Agroecology, Lanzhou University, Tianshui South Road 222, 730000 Lanzhou, China; E‐mail <email normalForm="wangg@lzu.edu.cn">wangg@lzu.edu.cn</email></unparsedAffiliation></affiliation><affiliation xml:id="a8" countryCode="CN"><unparsedAffiliation> Chinese Academy of Sciences, Xinjiang Institute of Ecology and Geography, 40 South Beijing Road, 830011 Urumqi, China; E‐mail <email normalForm="zhxm@ms.xjb.ac.cn">zhxm@ms.xjb.ac.cn</email></unparsedAffiliation></affiliation><affiliation xml:id="a9" countryCode="DE"><unparsedAffiliation> Department of Ecology and Ecosystem Research, Albrecht‐von‐Haller‐Institute for Plant Sciences, University of Göttingen, Untere Karspuele 2, DE–37073 Göttingen, Germany; E‐mail <email normalForm="mrunge@gwdg.de">mrunge@gwdg.de</email></unparsedAffiliation></affiliation></affiliationGroup><keywordGroup xml:lang="en"><keyword xml:id="k1">China</keyword><keyword xml:id="k2">Desert vegetation</keyword><keyword xml:id="k3">Groundwater map</keyword><keyword xml:id="k4">Oasis vegetation</keyword><keyword xml:id="k5">Phreatophytes</keyword><keyword xml:id="k6">Soil matric potential</keyword><keyword xml:id="k7">Soil texture</keyword><keyword xml:id="k8">Soil water content</keyword><keyword xml:id="k9">Soil water retention curves</keyword><keyword xml:id="k10">Sum exceedance values</keyword><keyword xml:id="k11">Vegetation map</keyword><keyword xml:id="k12">Xinjiang</keyword></keywordGroup><supportingInformation><p><b>Appendix S1.</b> Sampling scheme of the vegetation reference plots. A plot had a total area of 1600 m<sup>2</sup>, of which 10.94% was sampled by seven subplots of 25 m<sup>2</sup> each.</p><p><b>Appendix S2.</b> <i>Populus euphratica</i> stand of plot A5.</p><p><b>Appendix S3.</b> Soil texture at different depths in five different landcover types. Layers that were difficult to penetrate with the manual auger are labeled with “Hard layer”.</p><p><b>Appendix S4.</b> Soil water retention curves for soil samples from five different landcover types. For details see Methods.</p><p>Please note: Wiley‐Blackwell is not responsible for the content or functionality of any supporting materials supplied by the authors. Any queries (other than missing material) should be directed to the corresponding author for the article.</p><supportingInfoItem><mediaResource alt="supporting info item" href="urn-x:wiley:14022001:media:avsc1050:AVSC_1050_sm_Appendixs1"></mediaResource><caption>Supporting info item</caption></supportingInfoItem></supportingInformation><abstractGroup><abstract type="main" xml:lang="en"><title type="main">Abstract</title><p><b>Questions: </b> Do the vegetation‐specific patterns in the forelands of river oases of the Taklamakan Desert provide clues to the degree to which a vegetation type depends on unsaturated soil moisture, brought about by extensive floodings, or phreatic water?</p><p><b>Location: </b> Foreland of the Qira oasis on the southern rim of the Taklamakan Desert, Xinjiang Uygur Autonomous Region, China.</p><p><b>Methods: </b> A vegetation map was prepared using a SPOT satellite image and ground truthing. Measurements of soil water contents were obtained from a flooding experiment and transformed into water potentials. Sum excedance values were calculated as the percentage of days on which different thresholds of soil water potentials were transgressed. Groundwater depth was mapped by drilling 30 groundwater holes and extrapolating the distances to the whole study area.</p><p><b>Results: </b> The vegetation was characterized by only six dominant or codominant species: <i>Alhagi sparsifolia, Karelinia caspia, Populus euphratica, Tamarix ramosissima, Calligonum caput‐medusae</i> and <i>Phragmites australis</i>. The vegetation patterns encountered lacked any linear features typical of phreatophytes, thus not allowing direct conclusions on the type of the sustaining water sources. Soil water potentials never transgressed a threshold of pF 5 (−10 MPa) in horizons above the capillary fringe during periods without inundation, thus representing water not accessible for plants. Depth to the groundwater ranged between 2.3 and 17.5 m among plots and varied between 1.7 and 8.0 m within a plot owing to dune relief. The seven main vegetation types showed distinct niches of groundwater depths, corresponding to the observed concentric arrangement of vegetation types around the oasis.</p><p><b>Conclusions: </b> Inundation by flooding and unsaturated soil moisture are irrelevant for the foreland vegetation water supply. Although distances to the groundwater table can reach about 20 m, which is exceptionally large for phreatophytes, groundwater is the only water source for all vegetation types in the oasis foreland. In consequence, successful maintenance of oasis foreland vegetation will crucially depend on providing non‐declining ground water tables.</p></abstract></abstractGroup></contentMeta><noteGroup><note xml:id="fn1" numbered="no"><p>Co‐ordinating Editor: S. Bartha</p></note></noteGroup></header></component></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Life on the edge – to which degree does phreatic water sustain vegetation in the periphery of the Taklamakan Desert?</title></titleInfo><titleInfo type="abbreviated" lang="en"><title>Life on the edge</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Life on the edge – to which degree does phreatic water sustain vegetation in the periphery of the Taklamakan Desert?</title></titleInfo><name type="personal"><namePart type="given">Helge</namePart><namePart type="family">Bruelheide</namePart><affiliation>Martin Luther University Halle Wittenberg, Institute of Biology/Geobotany and Botanical Garden, Am Kirchtor 1, DE–06108 Halle, Germany</affiliation><affiliation>E-mail: helge.bruelheide@botanik.uni‐halle.de</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Beatrix</namePart><namePart type="family">Vonlanthen</namePart><affiliation>Martin Luther University Halle Wittenberg, Institute of Biology/Geobotany and Botanical Garden, Am Kirchtor 1, DE–06108 Halle, Germany</affiliation><affiliation>E‐mail beatrix.vonlanthen@botanik.uni‐halle.de</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Ute</namePart><namePart type="family">Jandt</namePart><affiliation>Martin Luther University Halle Wittenberg, Institute of Biology/Geobotany and Botanical Garden, Am Kirchtor 1, DE–06108 Halle, Germany</affiliation><affiliation>E‐mail ute.jandt@botanik.uni‐halle.de</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Frank M.</namePart><namePart type="family">Thomas</namePart><affiliation>Department of Geobotany, University of Trier, Behringstrasse 21, DE–54296 Trier, Germany; E‐mail thomasf@uni‐trier.de</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Andrea</namePart><namePart type="family">Foetzki</namePart><affiliation>Agroscope Reckenholz‐Tänikon Research Station ART, Biodiversity and Environmental Management, Reckenholzstrasse 191, CH–8046 Zurich, Switzerland; E‐mail andrea.foetzki@art.admin.ch</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Dirk</namePart><namePart type="family">Gries</namePart><affiliation>XLAB, Justus‐von‐Liebig‐Weg 8, DE–37077 Göttingen, Germany; E‐mail dgries@gwdg.de</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Gang</namePart><namePart type="family">Wang</namePart><affiliation>Department of Biology, Key Laboratory of Arid and Grassland Agroecology, Lanzhou University, Tianshui South Road 222, 730000 Lanzhou, China; E‐mail wangg@lzu.edu.cn</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Ximing</namePart><namePart type="family">Zhang</namePart><affiliation>Chinese Academy of Sciences, Xinjiang Institute of Ecology and Geography, 40 South Beijing Road, 830011 Urumqi, China; E‐mail zhxm@ms.xjb.ac.cn</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Michael</namePart><namePart type="family">Runge</namePart><affiliation>Department of Ecology and Ecosystem Research, Albrecht‐von‐Haller‐Institute for Plant Sciences, University of Göttingen, Untere Karspuele 2, DE–37073 Göttingen, Germany; E‐mail mrunge@gwdg.de</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="article" displayLabel="article"></genre><originInfo><publisher>Blackwell Publishing Ltd</publisher><place><placeTerm type="text">Oxford, UK</placeTerm></place><dateIssued encoding="w3cdtf">2010-02</dateIssued><edition>Received 6 May 2009;Accepted 7 July 2009.</edition><copyrightDate encoding="w3cdtf">2010</copyrightDate></originInfo><language><languageTerm type="code" authority="rfc3066">en</languageTerm><languageTerm type="code" authority="iso639-2b">eng</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType><extent unit="figures">5</extent><extent unit="tables">1</extent><extent unit="references">76</extent><extent unit="words">11254</extent></physicalDescription><abstract>Questions: Do the vegetation‐specific patterns in the forelands of river oases of the Taklamakan Desert provide clues to the degree to which a vegetation type depends on unsaturated soil moisture, brought about by extensive floodings, or phreatic water?</abstract><abstract>Location: Foreland of the Qira oasis on the southern rim of the Taklamakan Desert, Xinjiang Uygur Autonomous Region, China.</abstract><abstract>Methods: A vegetation map was prepared using a SPOT satellite image and ground truthing. Measurements of soil water contents were obtained from a flooding experiment and transformed into water potentials. Sum excedance values were calculated as the percentage of days on which different thresholds of soil water potentials were transgressed. Groundwater depth was mapped by drilling 30 groundwater holes and extrapolating the distances to the whole study area.</abstract><abstract>Results: The vegetation was characterized by only six dominant or codominant species: Alhagi sparsifolia, Karelinia caspia, Populus euphratica, Tamarix ramosissima, Calligonum caput‐medusae and Phragmites australis. The vegetation patterns encountered lacked any linear features typical of phreatophytes, thus not allowing direct conclusions on the type of the sustaining water sources. Soil water potentials never transgressed a threshold of pF 5 (−10 MPa) in horizons above the capillary fringe during periods without inundation, thus representing water not accessible for plants. Depth to the groundwater ranged between 2.3 and 17.5 m among plots and varied between 1.7 and 8.0 m within a plot owing to dune relief. The seven main vegetation types showed distinct niches of groundwater depths, corresponding to the observed concentric arrangement of vegetation types around the oasis.</abstract><abstract>Conclusions: Inundation by flooding and unsaturated soil moisture are irrelevant for the foreland vegetation water supply. Although distances to the groundwater table can reach about 20 m, which is exceptionally large for phreatophytes, groundwater is the only water source for all vegetation types in the oasis foreland. In consequence, successful maintenance of oasis foreland vegetation will crucially depend on providing non‐declining ground water tables.</abstract><subject lang="en"><genre>keywords</genre><topic>China</topic><topic>Desert vegetation</topic><topic>Groundwater map</topic><topic>Oasis vegetation</topic><topic>Phreatophytes</topic><topic>Soil matric potential</topic><topic>Soil texture</topic><topic>Soil water content</topic><topic>Soil water retention curves</topic><topic>Sum exceedance values</topic><topic>Vegetation map</topic><topic>Xinjiang</topic></subject><relatedItem type="host"><titleInfo><title>Applied Vegetation Science</title></titleInfo><genre type="journal">journal</genre><note type="content"> Appendix S1. Sampling scheme of the vegetation reference plots. A plot had a total area of 1600 m2, of which 10.94% was sampled by seven subplots of 25 m2 each. Appendix S2. Populus euphratica stand of plot A5. Appendix S3. Soil texture at different depths in five different landcover types. Layers that were difficult to penetrate with the manual auger are labeled with “Hard layer”. Appendix S4. Soil water retention curves for soil samples from five different landcover types. For details see Methods. Please note: Wiley‐Blackwell is not responsible for the content or functionality of any supporting materials supplied by the authors. Any queries (other than missing material) should be directed to the corresponding author for the article. Appendix S1. Sampling scheme of the vegetation reference plots. A plot had a total area of 1600 m2, of which 10.94% was sampled by seven subplots of 25 m2 each. Appendix S2. Populus euphratica stand of plot A5. Appendix S3. Soil texture at different depths in five different landcover types. Layers that were difficult to penetrate with the manual auger are labeled with “Hard layer”. Appendix S4. Soil water retention curves for soil samples from five different landcover types. For details see Methods. Please note: Wiley‐Blackwell is not responsible for the content or functionality of any supporting materials supplied by the authors. Any queries (other than missing material) should be directed to the corresponding author for the article. Appendix S1. Sampling scheme of the vegetation reference plots. A plot had a total area of 1600 m2, of which 10.94% was sampled by seven subplots of 25 m2 each. Appendix S2. Populus euphratica stand of plot A5. Appendix S3. Soil texture at different depths in five different landcover types. Layers that were difficult to penetrate with the manual auger are labeled with “Hard layer”. Appendix S4. Soil water retention curves for soil samples from five different landcover types. For details see Methods. Please note: Wiley‐Blackwell is not responsible for the content or functionality of any supporting materials supplied by the authors. Any queries (other than missing material) should be directed to the corresponding author for the article. Appendix S1. Sampling scheme of the vegetation reference plots. A plot had a total area of 1600 m2, of which 10.94% was sampled by seven subplots of 25 m2 each. Appendix S2. Populus euphratica stand of plot A5. Appendix S3. Soil texture at different depths in five different landcover types. Layers that were difficult to penetrate with the manual auger are labeled with “Hard layer”. Appendix S4. Soil water retention curves for soil samples from five different landcover types. For details see Methods. Please note: Wiley‐Blackwell is not responsible for the content or functionality of any supporting materials supplied by the authors. Any queries (other than missing material) should be directed to the corresponding author for the article. Appendix S1. Sampling scheme of the vegetation reference plots. A plot had a total area of 1600 m2, of which 10.94% was sampled by seven subplots of 25 m2 each. Appendix S2. Populus euphratica stand of plot A5. Appendix S3. Soil texture at different depths in five different landcover types. Layers that were difficult to penetrate with the manual auger are labeled with “Hard layer”. Appendix S4. Soil water retention curves for soil samples from five different landcover types. For details see Methods. Please note: Wiley‐Blackwell is not responsible for the content or functionality of any supporting materials supplied by the authors. Any queries (other than missing material) should be directed to the corresponding author for the article.Supporting Info Item: Supporting info item - </note><identifier type="ISSN">1402-2001</identifier><identifier type="eISSN">1654-109X</identifier><identifier type="DOI">10.1111/(ISSN)1654-109X</identifier><identifier type="PublisherID">AVSC</identifier><part><date>2010</date><detail type="volume"><caption>vol.</caption><number>13</number></detail><detail type="issue"><caption>no.</caption><number>1</number></detail><extent unit="pages"><start>56</start><end>71</end><total>16</total></extent></part></relatedItem><identifier type="istex">B8DCE0A116A061EE09A7BFFDF676DAC909EFB772</identifier><identifier type="DOI">10.1111/j.1654-109X.2009.01050.x</identifier><identifier type="ArticleID">AVSC1050</identifier><accessCondition type="use and reproduction" contentType="copyright">© 2009 International Association for Vegetation Science</accessCondition><recordInfo><recordContentSource>WILEY</recordContentSource><recordOrigin>Blackwell Publishing Ltd</recordOrigin></recordInfo></mods></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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