Negative feedback adjustment challenges reconstruction study from tree rings: A study case of response of Populus euphratica to river discontinuous flow and ecological water conveyance.
Identifieur interne : 001296 ( Main/Exploration ); précédent : 001295; suivant : 001297Negative feedback adjustment challenges reconstruction study from tree rings: A study case of response of Populus euphratica to river discontinuous flow and ecological water conveyance.
Auteurs : Hongbo Ling [République populaire de Chine] ; Pei Zhang [République populaire de Chine] ; Bin Guo [République populaire de Chine] ; Hailiang Xu [République populaire de Chine] ; Mao Ye [République populaire de Chine] ; Xiaoya Deng [République populaire de Chine]Source :
- The Science of the total environment [ 1879-1026 ] ; 2017.
Descripteurs français
- KwdFr :
- MESH :
- physiologie : Populus.
- Chine, Eau, Nappe phréatique, Rivières, Stress physiologique, Sécheresses, Écologie.
English descriptors
- KwdEn :
- MESH :
- chemical : Water.
- physiology : Populus.
- China, Droughts, Ecology, Groundwater, Rivers, Stress, Physiological.
Abstract
Drought stress changes the relationship between the growth of tree rings and variations in ambient temperature. However, it is not clear how the growth of trees changes in response to drought of varying intensities, especially in arid areas. Therefore, Tree rings were studied for 6years in Populus euphratica to assess the impacts of abrupt changes in environment on tree rings using the theories and methods in dendrohydrology, ecology and phytophysiology. The width of tree rings increased by 8.7% after ecological water conveyance downstream of Tarim River compared to that when the river water had been cut off. However, during intermediate drought, as the depth of the groundwater increases, the downward trend in the tree rings was reversed because of changes in the physiology of the tree. Therefore, the growth of tree rings shows a negative feedback to intermediate drought stress, an observation that challenges the homogenization theory of tree ring reconstruction based on the traditional methods. Owing to the time lag, the cumulative effect and the negative feedback between the growth of tree rings and drought stress, the reconstruction of past environment by studying the patterns of tree rings is often inaccurate. Our research sets out to verify the hypothesis that intermediate drought stress results in a negative feedback adjustment and thus to answers two scientific questions: (1) How does the negative feedback adjustment promote the growth of tree rings as a result of intermediate drought stress? (2) How does the negative feedback adjustment lower the accuracy with which the past is reconstructed based on tree rings? This research not only enriches the connotations of intermediate disturbance hypothesis and reconstruction theory of tree rings, but also provides a scientific basis for the conservation of desert riparian forests worldwide.
DOI: 10.1016/j.scitotenv.2016.09.043
PubMed: 27639018
Affiliations:
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Electronic address: linghongbo0929@163.com.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences (CAS), Urumqi 830011</wicri:regionArea><wicri:noRegion>Urumqi 830011</wicri:noRegion></affiliation></author><author><name sortKey="Ye, Mao" sort="Ye, Mao" uniqKey="Ye M" first="Mao" last="Ye">Mao Ye</name><affiliation wicri:level="1"><nlm:affiliation>School of Geography Science and Tourism, Xinjiang Normal University, Urumqi 830054, China.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>School of Geography Science and Tourism, Xinjiang Normal University, Urumqi 830054</wicri:regionArea><wicri:noRegion>Urumqi 830054</wicri:noRegion></affiliation></author><author><name sortKey="Deng, Xiaoya" sort="Deng, Xiaoya" uniqKey="Deng X" first="Xiaoya" last="Deng">Xiaoya Deng</name><affiliation wicri:level="1"><nlm:affiliation>State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, Department of Water Resources, China Institute of Water Resources and Hydropower Research, Beijing 100038, China.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, Department of Water Resources, China Institute of Water Resources and Hydropower Research, Beijing 100038</wicri:regionArea><placeName><settlement type="city">Pékin</settlement></placeName></affiliation></author></analytic><series><title level="j">The Science of the total environment</title><idno type="eISSN">1879-1026</idno><imprint><date when="2017" type="published">2017</date></imprint></series></biblStruct></sourceDesc></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>China (MeSH)</term><term>Droughts (MeSH)</term><term>Ecology (MeSH)</term><term>Groundwater (MeSH)</term><term>Populus (physiology)</term><term>Rivers (MeSH)</term><term>Stress, Physiological (MeSH)</term><term>Water (MeSH)</term></keywords><keywords scheme="KwdFr" xml:lang="fr"><term>Chine (MeSH)</term><term>Eau (MeSH)</term><term>Nappe phréatique (MeSH)</term><term>Populus (physiologie)</term><term>Rivières (MeSH)</term><term>Stress physiologique (MeSH)</term><term>Sécheresses (MeSH)</term><term>Écologie (MeSH)</term></keywords><keywords scheme="MESH" type="chemical" xml:lang="en"><term>Water</term></keywords><keywords scheme="MESH" qualifier="physiologie" xml:lang="fr"><term>Populus</term></keywords><keywords scheme="MESH" qualifier="physiology" xml:lang="en"><term>Populus</term></keywords><keywords scheme="MESH" xml:lang="en"><term>China</term><term>Droughts</term><term>Ecology</term><term>Groundwater</term><term>Rivers</term><term>Stress, Physiological</term></keywords><keywords scheme="MESH" xml:lang="fr"><term>Chine</term><term>Eau</term><term>Nappe phréatique</term><term>Rivières</term><term>Stress physiologique</term><term>Sécheresses</term><term>Écologie</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Drought stress changes the relationship between the growth of tree rings and variations in ambient temperature. However, it is not clear how the growth of trees changes in response to drought of varying intensities, especially in arid areas. Therefore, Tree rings were studied for 6years in Populus euphratica to assess the impacts of abrupt changes in environment on tree rings using the theories and methods in dendrohydrology, ecology and phytophysiology. The width of tree rings increased by 8.7% after ecological water conveyance downstream of Tarim River compared to that when the river water had been cut off. However, during intermediate drought, as the depth of the groundwater increases, the downward trend in the tree rings was reversed because of changes in the physiology of the tree. Therefore, the growth of tree rings shows a negative feedback to intermediate drought stress, an observation that challenges the homogenization theory of tree ring reconstruction based on the traditional methods. Owing to the time lag, the cumulative effect and the negative feedback between the growth of tree rings and drought stress, the reconstruction of past environment by studying the patterns of tree rings is often inaccurate. Our research sets out to verify the hypothesis that intermediate drought stress results in a negative feedback adjustment and thus to answers two scientific questions: (1) How does the negative feedback adjustment promote the growth of tree rings as a result of intermediate drought stress? (2) How does the negative feedback adjustment lower the accuracy with which the past is reconstructed based on tree rings? This research not only enriches the connotations of intermediate disturbance hypothesis and reconstruction theory of tree rings, but also provides a scientific basis for the conservation of desert riparian forests worldwide.</div></front></TEI><pubmed><MedlineCitation Status="MEDLINE" IndexingMethod="Curated" Owner="NLM"><PMID Version="1">27639018</PMID><DateCompleted><Year>2018</Year><Month>06</Month><Day>04</Day></DateCompleted><DateRevised><Year>2018</Year><Month>12</Month><Day>02</Day></DateRevised><Article PubModel="Print-Electronic"><Journal><ISSN IssnType="Electronic">1879-1026</ISSN><JournalIssue CitedMedium="Internet"><Volume>574</Volume><PubDate><Year>2017</Year><Month>Jan</Month><Day>01</Day></PubDate></JournalIssue><Title>The Science of the total environment</Title><ISOAbbreviation>Sci Total Environ</ISOAbbreviation></Journal><ArticleTitle>Negative feedback adjustment challenges reconstruction study from tree rings: A study case of response of Populus euphratica to river discontinuous flow and ecological water conveyance.</ArticleTitle><Pagination><MedlinePgn>109-119</MedlinePgn></Pagination><ELocationID EIdType="pii" ValidYN="Y">S0048-9697(16)31961-1</ELocationID><ELocationID EIdType="doi" ValidYN="Y">10.1016/j.scitotenv.2016.09.043</ELocationID><Abstract><AbstractText>Drought stress changes the relationship between the growth of tree rings and variations in ambient temperature. However, it is not clear how the growth of trees changes in response to drought of varying intensities, especially in arid areas. Therefore, Tree rings were studied for 6years in Populus euphratica to assess the impacts of abrupt changes in environment on tree rings using the theories and methods in dendrohydrology, ecology and phytophysiology. The width of tree rings increased by 8.7% after ecological water conveyance downstream of Tarim River compared to that when the river water had been cut off. However, during intermediate drought, as the depth of the groundwater increases, the downward trend in the tree rings was reversed because of changes in the physiology of the tree. Therefore, the growth of tree rings shows a negative feedback to intermediate drought stress, an observation that challenges the homogenization theory of tree ring reconstruction based on the traditional methods. Owing to the time lag, the cumulative effect and the negative feedback between the growth of tree rings and drought stress, the reconstruction of past environment by studying the patterns of tree rings is often inaccurate. Our research sets out to verify the hypothesis that intermediate drought stress results in a negative feedback adjustment and thus to answers two scientific questions: (1) How does the negative feedback adjustment promote the growth of tree rings as a result of intermediate drought stress? (2) How does the negative feedback adjustment lower the accuracy with which the past is reconstructed based on tree rings? This research not only enriches the connotations of intermediate disturbance hypothesis and reconstruction theory of tree rings, but also provides a scientific basis for the conservation of desert riparian forests worldwide.</AbstractText><CopyrightInformation>Copyright © 2016 Elsevier B.V. All rights reserved.</CopyrightInformation></Abstract><AuthorList CompleteYN="Y"><Author ValidYN="Y"><LastName>Ling</LastName><ForeName>Hongbo</ForeName><Initials>H</Initials><AffiliationInfo><Affiliation>State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences (CAS), Urumqi 830011, China.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Zhang</LastName><ForeName>Pei</ForeName><Initials>P</Initials><AffiliationInfo><Affiliation>State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, Department of Water Resources, China Institute of Water Resources and Hydropower Research, Beijing 100038, China.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Guo</LastName><ForeName>Bin</ForeName><Initials>B</Initials><AffiliationInfo><Affiliation>College of Geomatics, Shandong University of Science and Technology, Qingdao 266590, China.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Xu</LastName><ForeName>Hailiang</ForeName><Initials>H</Initials><AffiliationInfo><Affiliation>State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences (CAS), Urumqi 830011, China. Electronic address: linghongbo0929@163.com.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Ye</LastName><ForeName>Mao</ForeName><Initials>M</Initials><AffiliationInfo><Affiliation>School of Geography Science and Tourism, Xinjiang Normal University, Urumqi 830054, China.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Deng</LastName><ForeName>Xiaoya</ForeName><Initials>X</Initials><AffiliationInfo><Affiliation>State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, Department of Water Resources, China Institute of Water Resources and Hydropower Research, Beijing 100038, China.</Affiliation></AffiliationInfo></Author></AuthorList><Language>eng</Language><PublicationTypeList><PublicationType UI="D016428">Journal Article</PublicationType></PublicationTypeList><ArticleDate DateType="Electronic"><Year>2016</Year><Month>10</Month><Day>14</Day></ArticleDate></Article><MedlineJournalInfo><Country>Netherlands</Country><MedlineTA>Sci Total Environ</MedlineTA><NlmUniqueID>0330500</NlmUniqueID><ISSNLinking>0048-9697</ISSNLinking></MedlineJournalInfo><ChemicalList><Chemical><RegistryNumber>059QF0KO0R</RegistryNumber><NameOfSubstance UI="D014867">Water</NameOfSubstance></Chemical></ChemicalList><CitationSubset>IM</CitationSubset><MeshHeadingList><MeshHeading><DescriptorName UI="D002681" MajorTopicYN="N">China</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D055864" MajorTopicYN="N">Droughts</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D004463" MajorTopicYN="N">Ecology</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D060587" MajorTopicYN="N">Groundwater</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D032107" MajorTopicYN="N">Populus</DescriptorName><QualifierName UI="Q000502" MajorTopicYN="Y">physiology</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D045483" MajorTopicYN="Y">Rivers</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D013312" MajorTopicYN="N">Stress, Physiological</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D014867" MajorTopicYN="Y">Water</DescriptorName></MeshHeading></MeshHeadingList><KeywordList Owner="NOTNLM"><Keyword MajorTopicYN="N">Ecological water conveyance</Keyword><Keyword MajorTopicYN="N">Intermediate drought stress</Keyword><Keyword MajorTopicYN="N">Negative feedback adjustment</Keyword><Keyword MajorTopicYN="N">Tarim River</Keyword><Keyword MajorTopicYN="N">Tree rings</Keyword></KeywordList></MedlineCitation><PubmedData><History><PubMedPubDate PubStatus="received"><Year>2016</Year><Month>07</Month><Day>24</Day></PubMedPubDate><PubMedPubDate PubStatus="revised"><Year>2016</Year><Month>09</Month><Day>05</Day></PubMedPubDate><PubMedPubDate PubStatus="accepted"><Year>2016</Year><Month>09</Month><Day>06</Day></PubMedPubDate><PubMedPubDate PubStatus="pubmed"><Year>2016</Year><Month>9</Month><Day>18</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate><PubMedPubDate PubStatus="medline"><Year>2018</Year><Month>6</Month><Day>5</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate><PubMedPubDate PubStatus="entrez"><Year>2016</Year><Month>9</Month><Day>18</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate></History><PublicationStatus>ppublish</PublicationStatus><ArticleIdList><ArticleId IdType="pubmed">27639018</ArticleId><ArticleId IdType="pii">S0048-9697(16)31961-1</ArticleId><ArticleId IdType="doi">10.1016/j.scitotenv.2016.09.043</ArticleId></ArticleIdList></PubmedData></pubmed><affiliations><list><country><li>République populaire de Chine</li></country><settlement><li>Pékin</li></settlement></list><tree><country name="République populaire de Chine"><noRegion><name sortKey="Ling, Hongbo" sort="Ling, Hongbo" uniqKey="Ling H" first="Hongbo" last="Ling">Hongbo Ling</name></noRegion><name sortKey="Deng, Xiaoya" sort="Deng, Xiaoya" uniqKey="Deng X" first="Xiaoya" last="Deng">Xiaoya Deng</name><name sortKey="Guo, Bin" sort="Guo, Bin" uniqKey="Guo B" first="Bin" last="Guo">Bin Guo</name><name sortKey="Xu, Hailiang" sort="Xu, Hailiang" uniqKey="Xu H" first="Hailiang" last="Xu">Hailiang Xu</name><name sortKey="Ye, Mao" sort="Ye, Mao" uniqKey="Ye M" first="Mao" last="Ye">Mao Ye</name><name sortKey="Zhang, Pei" sort="Zhang, Pei" uniqKey="Zhang P" first="Pei" last="Zhang">Pei Zhang</name></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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