Variation in Populus euphratica foliar carbon isotope composition and osmotic solute for different groundwater depths in an arid region of China.
Identifieur interne : 001A66 ( Main/Exploration ); précédent : 001A65; suivant : 001A67Variation in Populus euphratica foliar carbon isotope composition and osmotic solute for different groundwater depths in an arid region of China.
Auteurs : Jianhua Si [République populaire de Chine] ; Qi Feng [République populaire de Chine] ; Tengfei Yu [République populaire de Chine] ; Chunyan Zhao [République populaire de Chine] ; Wei Li [République populaire de Chine]Source :
- Environmental monitoring and assessment [ 1573-2959 ] ; 2015.
Descripteurs français
- KwdFr :
- MESH :
- analyse : Isotopes du carbone.
- composition chimique : Feuilles de plante, Nappe phréatique, Populus.
- croissance et développement : Populus.
- physiologie : Feuilles de plante.
- Chine, Environnement, Surveillance de l'environnement.
English descriptors
- KwdEn :
- MESH :
- chemical , analysis : Carbon Isotopes.
- chemistry : Groundwater, Plant Leaves, Populus.
- growth & development : Populus.
- physiology : Plant Leaves.
- China, Environment, Environmental Monitoring.
Abstract
Water use efficiency (WUE) is an important trait associated with plant acclimation caused by water deficits, and δ13C is a good surrogate of WUE under conditions of water deficits. Water deficiency also enhances the accumulation of compatible solutes in the leaves. In this study, variations in foliar δ(13)C values and main osmotic solutes were investigated. Those included total soluble sugar (TSS), sucrose, free proline, glycine betaine (GB), and inorganic ionic (K+, Ca2+, and Cl-) content of Populus euphratica for different groundwater depths in a Ejina desert riparian forest, China. Results indicated that foliar δ13C values in the P. euphratica for different groundwater depths ranged from -29.14±0.06 to -25.84±0.04 ‰. Foliar δ13C signatures became richer as groundwater levels declined. TSS, sucrose, free proline, GB, and K+ were accumulated in P. euphratica foliage with developing plant growth and increasing groundwater depth. Ca2+ and Cl- content increased under stronger P. euphratica transpiration rates for shallower groundwater depths (1-2.5 m) and decreased for deeper groundwater depths (greater than 3.0 m). Moreover, correlations between δ13C, osmotic solutes, and groundwater depths showed that the primary osmotic solutes were TSS, sucrose, proline, GB, and K+. Correlations also showed that δ13C was not only a useful measure for P. euphratica-integrated WUE but also could be used as an indicator reflecting some physiological osmotic indexes.
DOI: 10.1007/s10661-015-4890-y
PubMed: 26502726
Affiliations:
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sort="Zhao, Chunyan" uniqKey="Zhao C" first="Chunyan" last="Zhao">Chunyan Zhao</name><affiliation wicri:level="1"><nlm:affiliation>Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzou, 730000, China.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzou, 730000</wicri:regionArea><wicri:noRegion>730000</wicri:noRegion></affiliation></author><author><name sortKey="Li, Wei" sort="Li, Wei" uniqKey="Li W" first="Wei" last="Li">Wei Li</name><affiliation wicri:level="1"><nlm:affiliation>Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzou, 730000, China.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy 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Si</name><affiliation wicri:level="1"><nlm:affiliation>Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzou, 730000, China. jianhuas@lzb.ac.cn.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzou, 730000</wicri:regionArea><wicri:noRegion>730000</wicri:noRegion></affiliation></author><author><name sortKey="Feng, Qi" sort="Feng, Qi" uniqKey="Feng Q" first="Qi" last="Feng">Qi Feng</name><affiliation wicri:level="1"><nlm:affiliation>Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzou, 730000, China.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzou, 730000</wicri:regionArea><wicri:noRegion>730000</wicri:noRegion></affiliation></author><author><name sortKey="Yu, Tengfei" sort="Yu, Tengfei" uniqKey="Yu T" first="Tengfei" last="Yu">Tengfei Yu</name><affiliation wicri:level="1"><nlm:affiliation>Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzou, 730000, China.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzou, 730000</wicri:regionArea><wicri:noRegion>730000</wicri:noRegion></affiliation></author><author><name sortKey="Zhao, Chunyan" sort="Zhao, Chunyan" uniqKey="Zhao C" first="Chunyan" last="Zhao">Chunyan Zhao</name><affiliation wicri:level="1"><nlm:affiliation>Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzou, 730000, China.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzou, 730000</wicri:regionArea><wicri:noRegion>730000</wicri:noRegion></affiliation></author><author><name sortKey="Li, Wei" sort="Li, Wei" uniqKey="Li W" first="Wei" last="Li">Wei Li</name><affiliation wicri:level="1"><nlm:affiliation>Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzou, 730000, China.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzou, 730000</wicri:regionArea><wicri:noRegion>730000</wicri:noRegion></affiliation></author></analytic><series><title level="j">Environmental monitoring and assessment</title><idno type="eISSN">1573-2959</idno><imprint><date when="2015" type="published">2015</date></imprint></series></biblStruct></sourceDesc></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Carbon Isotopes (analysis)</term><term>China (MeSH)</term><term>Environment (MeSH)</term><term>Environmental Monitoring (MeSH)</term><term>Groundwater (chemistry)</term><term>Plant Leaves (chemistry)</term><term>Plant Leaves (physiology)</term><term>Populus (chemistry)</term><term>Populus (growth & development)</term></keywords><keywords scheme="KwdFr" xml:lang="fr"><term>Chine (MeSH)</term><term>Environnement (MeSH)</term><term>Feuilles de plante (composition chimique)</term><term>Feuilles de plante (physiologie)</term><term>Isotopes du carbone (analyse)</term><term>Nappe phréatique (composition chimique)</term><term>Populus (composition chimique)</term><term>Populus (croissance et développement)</term><term>Surveillance de l'environnement (MeSH)</term></keywords><keywords scheme="MESH" type="chemical" qualifier="analysis" xml:lang="en"><term>Carbon Isotopes</term></keywords><keywords scheme="MESH" qualifier="analyse" xml:lang="fr"><term>Isotopes du carbone</term></keywords><keywords scheme="MESH" qualifier="chemistry" xml:lang="en"><term>Groundwater</term><term>Plant Leaves</term><term>Populus</term></keywords><keywords scheme="MESH" qualifier="composition chimique" xml:lang="fr"><term>Feuilles de plante</term><term>Nappe phréatique</term><term>Populus</term></keywords><keywords scheme="MESH" qualifier="croissance et développement" xml:lang="fr"><term>Populus</term></keywords><keywords scheme="MESH" qualifier="growth & development" xml:lang="en"><term>Populus</term></keywords><keywords scheme="MESH" qualifier="physiologie" xml:lang="fr"><term>Feuilles de plante</term></keywords><keywords scheme="MESH" qualifier="physiology" xml:lang="en"><term>Plant Leaves</term></keywords><keywords scheme="MESH" xml:lang="en"><term>China</term><term>Environment</term><term>Environmental Monitoring</term></keywords><keywords scheme="MESH" xml:lang="fr"><term>Chine</term><term>Environnement</term><term>Surveillance de l'environnement</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Water use efficiency (WUE) is an important trait associated with plant acclimation caused by water deficits, and δ13C is a good surrogate of WUE under conditions of water deficits. Water deficiency also enhances the accumulation of compatible solutes in the leaves. In this study, variations in foliar δ(13)C values and main osmotic solutes were investigated. Those included total soluble sugar (TSS), sucrose, free proline, glycine betaine (GB), and inorganic ionic (K+, Ca2+, and Cl-) content of Populus euphratica for different groundwater depths in a Ejina desert riparian forest, China. Results indicated that foliar δ13C values in the P. euphratica for different groundwater depths ranged from -29.14±0.06 to -25.84±0.04 ‰. Foliar δ13C signatures became richer as groundwater levels declined. TSS, sucrose, free proline, GB, and K+ were accumulated in P. euphratica foliage with developing plant growth and increasing groundwater depth. Ca2+ and Cl- content increased under stronger P. euphratica transpiration rates for shallower groundwater depths (1-2.5 m) and decreased for deeper groundwater depths (greater than 3.0 m). Moreover, correlations between δ13C, osmotic solutes, and groundwater depths showed that the primary osmotic solutes were TSS, sucrose, proline, GB, and K+. Correlations also showed that δ13C was not only a useful measure for P. euphratica-integrated WUE but also could be used as an indicator reflecting some physiological osmotic indexes.</div></front></TEI><pubmed><MedlineCitation Status="MEDLINE" IndexingMethod="Curated" Owner="NLM"><PMID Version="1">26502726</PMID><DateCompleted><Year>2016</Year><Month>05</Month><Day>20</Day></DateCompleted><DateRevised><Year>2018</Year><Month>12</Month><Day>02</Day></DateRevised><Article PubModel="Print-Electronic"><Journal><ISSN IssnType="Electronic">1573-2959</ISSN><JournalIssue CitedMedium="Internet"><Volume>187</Volume><Issue>11</Issue><PubDate><Year>2015</Year><Month>Nov</Month></PubDate></JournalIssue><Title>Environmental monitoring and assessment</Title><ISOAbbreviation>Environ Monit Assess</ISOAbbreviation></Journal><ArticleTitle>Variation in Populus euphratica foliar carbon isotope composition and osmotic solute for different groundwater depths in an arid region of China.</ArticleTitle><Pagination><MedlinePgn>705</MedlinePgn></Pagination><ELocationID EIdType="doi" ValidYN="Y">10.1007/s10661-015-4890-y</ELocationID><Abstract><AbstractText>Water use efficiency (WUE) is an important trait associated with plant acclimation caused by water deficits, and δ13C is a good surrogate of WUE under conditions of water deficits. Water deficiency also enhances the accumulation of compatible solutes in the leaves. In this study, variations in foliar δ(13)C values and main osmotic solutes were investigated. Those included total soluble sugar (TSS), sucrose, free proline, glycine betaine (GB), and inorganic ionic (K+, Ca2+, and Cl-) content of Populus euphratica for different groundwater depths in a Ejina desert riparian forest, China. Results indicated that foliar δ13C values in the P. euphratica for different groundwater depths ranged from -29.14±0.06 to -25.84±0.04 ‰. Foliar δ13C signatures became richer as groundwater levels declined. TSS, sucrose, free proline, GB, and K+ were accumulated in P. euphratica foliage with developing plant growth and increasing groundwater depth. Ca2+ and Cl- content increased under stronger P. euphratica transpiration rates for shallower groundwater depths (1-2.5 m) and decreased for deeper groundwater depths (greater than 3.0 m). Moreover, correlations between δ13C, osmotic solutes, and groundwater depths showed that the primary osmotic solutes were TSS, sucrose, proline, GB, and K+. Correlations also showed that δ13C was not only a useful measure for P. euphratica-integrated WUE but also could be used as an indicator reflecting some physiological osmotic indexes.</AbstractText></Abstract><AuthorList CompleteYN="Y"><Author ValidYN="Y"><LastName>Si</LastName><ForeName>Jianhua</ForeName><Initials>J</Initials><AffiliationInfo><Affiliation>Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzou, 730000, China. jianhuas@lzb.ac.cn.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Feng</LastName><ForeName>Qi</ForeName><Initials>Q</Initials><AffiliationInfo><Affiliation>Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzou, 730000, China.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Yu</LastName><ForeName>Tengfei</ForeName><Initials>T</Initials><AffiliationInfo><Affiliation>Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzou, 730000, China.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Zhao</LastName><ForeName>Chunyan</ForeName><Initials>C</Initials><AffiliationInfo><Affiliation>Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzou, 730000, China.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Li</LastName><ForeName>Wei</ForeName><Initials>W</Initials><AffiliationInfo><Affiliation>Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzou, 730000, China.</Affiliation></AffiliationInfo></Author></AuthorList><Language>eng</Language><PublicationTypeList><PublicationType UI="D016428">Journal Article</PublicationType><PublicationType UI="D013485">Research Support, Non-U.S. Gov't</PublicationType></PublicationTypeList><ArticleDate DateType="Electronic"><Year>2015</Year><Month>10</Month><Day>26</Day></ArticleDate></Article><MedlineJournalInfo><Country>Netherlands</Country><MedlineTA>Environ Monit Assess</MedlineTA><NlmUniqueID>8508350</NlmUniqueID><ISSNLinking>0167-6369</ISSNLinking></MedlineJournalInfo><ChemicalList><Chemical><RegistryNumber>0</RegistryNumber><NameOfSubstance UI="D002247">Carbon Isotopes</NameOfSubstance></Chemical></ChemicalList><CitationSubset>IM</CitationSubset><MeshHeadingList><MeshHeading><DescriptorName UI="D002247" MajorTopicYN="N">Carbon Isotopes</DescriptorName><QualifierName UI="Q000032" MajorTopicYN="Y">analysis</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D002681" MajorTopicYN="N">China</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D004777" MajorTopicYN="N">Environment</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D004784" MajorTopicYN="Y">Environmental Monitoring</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D060587" MajorTopicYN="N">Groundwater</DescriptorName><QualifierName UI="Q000737" MajorTopicYN="Y">chemistry</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D018515" MajorTopicYN="N">Plant Leaves</DescriptorName><QualifierName UI="Q000737" MajorTopicYN="Y">chemistry</QualifierName><QualifierName UI="Q000502" MajorTopicYN="N">physiology</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D032107" MajorTopicYN="N">Populus</DescriptorName><QualifierName UI="Q000737" MajorTopicYN="Y">chemistry</QualifierName><QualifierName UI="Q000254" MajorTopicYN="N">growth & development</QualifierName></MeshHeading></MeshHeadingList><KeywordList Owner="NOTNLM"><Keyword MajorTopicYN="N">Groundwater depth</Keyword><Keyword MajorTopicYN="N">Osmotic solutes</Keyword><Keyword MajorTopicYN="N">Populus euphratica</Keyword><Keyword MajorTopicYN="N">Stable carbon isotope</Keyword><Keyword MajorTopicYN="N">Water use efficiency</Keyword></KeywordList></MedlineCitation><PubmedData><History><PubMedPubDate PubStatus="received"><Year>2015</Year><Month>03</Month><Day>30</Day></PubMedPubDate><PubMedPubDate PubStatus="accepted"><Year>2015</Year><Month>09</Month><Day>22</Day></PubMedPubDate><PubMedPubDate PubStatus="entrez"><Year>2015</Year><Month>10</Month><Day>28</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate><PubMedPubDate PubStatus="pubmed"><Year>2015</Year><Month>10</Month><Day>28</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate><PubMedPubDate PubStatus="medline"><Year>2016</Year><Month>5</Month><Day>21</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate></History><PublicationStatus>ppublish</PublicationStatus><ArticleIdList><ArticleId IdType="pubmed">26502726</ArticleId><ArticleId IdType="doi">10.1007/s10661-015-4890-y</ArticleId><ArticleId IdType="pii">10.1007/s10661-015-4890-y</ArticleId></ArticleIdList><ReferenceList><Reference><Citation>Environ Exp Bot. 2001 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Si</name></noRegion><name sortKey="Feng, Qi" sort="Feng, Qi" uniqKey="Feng Q" first="Qi" last="Feng">Qi Feng</name><name sortKey="Li, Wei" sort="Li, Wei" uniqKey="Li W" first="Wei" last="Li">Wei Li</name><name sortKey="Yu, Tengfei" sort="Yu, Tengfei" uniqKey="Yu T" first="Tengfei" last="Yu">Tengfei Yu</name><name sortKey="Zhao, Chunyan" sort="Zhao, Chunyan" uniqKey="Zhao C" first="Chunyan" last="Zhao">Chunyan Zhao</name></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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