AustralieFrV1, PascalFrancis, Curation, bibRecord, 005E38

Influence of cambial age and climate on ring width and wood density in Pinus radiata families

Identifieur interne : 005E38 ( PascalFrancis/Curation ); précédent : 005E37; suivant : 005E39

Influence of cambial age and climate on ring width and wood density in Pinus radiata families

Auteurs : Miloš Ivkovic [Australie] ; Washington Gapare [Australie] ; Harry Wu [Australie] ; Sergio Espinoza [Chili] ; Philippe Rozenberg [France]

Source :

Annals of forest science : (Print) [ 1286-4560 ] ; 2013.

RBID : Pascal:15-0049493

Descripteurs français

Pascal (Inist)
- Cambium, Age, Climat, Cerne bois, Bois initial, Densité, Changement climatique, Bois final, Foresterie, Pinus radiata.
Wicri :
- topic : Climat, Changement climatique.

English descriptors

KwdEn :
- Age, Cambium, Climate, Climate change, Density, Early wood, Forestry, Late wood, Pinus radiata, Tree ring.

Abstract

Context The correlation between tree ring width and density and short-term climate fluctuations may be a useful tool for predicting response of wood formation process to long-term climate change. . Aims This study examined these correlations for different radiata pine genotypes and aimed at detecting potential genotype by climate interactions. . Methods Four data sets comprising ring width and density of half- and full-sib radiata pine families were used. Correlations with climate variables were examined, after the extraction of the effect of cambial age. . Results Cambial age explained the highest proportion of the ring to ring variation in all variables. Calendar year and year by family interaction explained a smaller but significant proportion of the variation. Rainfall had a positive correlation with ring width and, depending on test site, either a negative or positive correlation with ring density. Correlations between temperature during growing season and ring density were generally negative. . Conclusion Climate variables that influence ring width and wood density can be identified from ring profiles, after removing the cambial age effect. Families can be selected that consistently show desirable response to climate features expected to become prevalent as a result of climate change.

A01	`01`	`1`		`@0 1286-4560`
A03		`1`		`@0 Ann. for. sci. : (Print)`
A05				`@2 70`
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A08	`01`	`1`	`ENG`	`@1 Influence of cambial age and climate on ring width and wood density in Pinus radiata families`
A11	`01`	`1`		`@1 IVKOVIC (Miloš)`
A11	`02`	`1`		`@1 GAPARE (Washington)`
A11	`03`	`1`		`@1 WU (Harry)`
A11	`04`	`1`		`@1 ESPINOZA (Sergio)`
A11	`05`	`1`		`@1 ROZENBERG (Philippe)`
A14	`01`			`@1 Plant Industry, Commonwealth Scientific and Industry Research Organisation, GPO Box 1600 @2 Canberra, ACT 2601 @3 AUS @Z 1 aut. @Z 2 aut. @Z 3 aut.`
A14	`02`			`@1 Dryland Technological Center, The Catholic University of Maule @2 Talca @3 CHL @Z 4 aut.`
A14	`03`			`@1 Unité de Recherche Amelioration, Génétique et Physiologie Forestières, INRA @2 Orléans @3 FRA @Z 5 aut.`
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A21				`@1 2013`
A23	`01`			`@0 ENG`
A43	`01`			`@1 INIST @2 959 @5 354000509071880080`
A44				`@0 0000 @1 © 2015 INIST-CNRS. All rights reserved.`
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A64	`01`	`1`		`@0 Annals of forest science : (Print)`
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C01	`01`		`ENG`	@0 Context The correlation between tree ring width and density and short-term climate fluctuations may be a useful tool for predicting response of wood formation process to long-term climate change. . Aims This study examined these correlations for different radiata pine genotypes and aimed at detecting potential genotype by climate interactions. . Methods Four data sets comprising ring width and density of half- and full-sib radiata pine families were used. Correlations with climate variables were examined, after the extraction of the effect of cambial age. . Results Cambial age explained the highest proportion of the ring to ring variation in all variables. Calendar year and year by family interaction explained a smaller but significant proportion of the variation. Rainfall had a positive correlation with ring width and, depending on test site, either a negative or positive correlation with ring density. Correlations between temperature during growing season and ring density were generally negative. . Conclusion Climate variables that influence ring width and wood density can be identified from ring profiles, after removing the cambial age effect. Families can be selected that consistently show desirable response to climate features expected to become prevalent as a result of climate change.
C02	`01`	`X`		`@0 002A33`
C03	`01`	`X`	`FRE`	`@0 Cambium @5 01`
C03	`01`	`X`	`ENG`	`@0 Cambium @5 01`
C03	`01`	`X`	`SPA`	`@0 Cambio @5 01`
C03	`02`	`X`	`FRE`	`@0 Age @5 02`
C03	`02`	`X`	`ENG`	`@0 Age @5 02`
C03	`02`	`X`	`SPA`	`@0 Edad @5 02`
C03	`03`	`X`	`FRE`	`@0 Climat @5 03`
C03	`03`	`X`	`ENG`	`@0 Climate @5 03`
C03	`03`	`X`	`SPA`	`@0 Clima @5 03`
C03	`04`	`X`	`FRE`	`@0 Cerne bois @5 04`
C03	`04`	`X`	`ENG`	`@0 Tree ring @5 04`
C03	`04`	`X`	`SPA`	`@0 Anillo madera @5 04`
C03	`05`	`X`	`FRE`	`@0 Bois initial @5 05`
C03	`05`	`X`	`ENG`	`@0 Early wood @5 05`
C03	`05`	`X`	`SPA`	`@0 Madera inicial @5 05`
C03	`06`	`X`	`FRE`	`@0 Densité @5 06`
C03	`06`	`X`	`ENG`	`@0 Density @5 06`
C03	`06`	`X`	`SPA`	`@0 Densidad @5 06`
C03	`07`	`X`	`FRE`	`@0 Changement climatique @5 07`
C03	`07`	`X`	`ENG`	`@0 Climate change @5 07`
C03	`07`	`X`	`SPA`	`@0 Cambio climático @5 07`
C03	`08`	`X`	`FRE`	`@0 Bois final @5 08`
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C03	`09`	`X`	`FRE`	`@0 Foresterie @5 09`
C03	`09`	`X`	`ENG`	`@0 Forestry @5 09`
C03	`09`	`X`	`SPA`	`@0 Ciencias forestales @5 09`
C03	`10`	`X`	`FRE`	`@0 Pinus radiata @2 NS @5 10`
C03	`10`	`X`	`ENG`	`@0 Pinus radiata @2 NS @5 10`
C03	`10`	`X`	`SPA`	`@0 Pinus radiata @2 NS @5 10`
C07	`01`	`X`	`FRE`	`@0 Climatologie dynamique`
C07	`01`	`X`	`ENG`	`@0 Dynamical climatology`
C07	`01`	`X`	`SPA`	`@0 Climatología dinámica`
C07	`02`	`X`	`FRE`	`@0 Coniferales @2 NS`
C07	`02`	`X`	`ENG`	`@0 Coniferales @2 NS`
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C07	`03`	`X`	`FRE`	`@0 Gymnospermae @2 NS`
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C07	`03`	`X`	`SPA`	`@0 Gymnospermae @2 NS`
C07	`04`	`X`	`FRE`	`@0 Spermatophyta @2 NS`
C07	`04`	`X`	`ENG`	`@0 Spermatophyta @2 NS`
C07	`04`	`X`	`SPA`	`@0 Spermatophyta @2 NS`
C07	`05`	`X`	`FRE`	`@0 Arbre forestier résineux @5 31`
C07	`05`	`X`	`ENG`	`@0 Softwood forest tree @5 31`
C07	`05`	`X`	`SPA`	`@0 Arbol forestal resinoso @5 31`
N21				`@1 166`
N44	`01`			`@1 OTO`
N82				`@1 OTO`

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Le document en format XML

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<profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Age</term>
<term>Cambium</term>
<term>Climate</term>
<term>Climate change</term>
<term>Density</term>
<term>Early wood</term>
<term>Forestry</term>
<term>Late wood</term>
<term>Pinus radiata</term>
<term>Tree ring</term>
</keywords>
<keywords scheme="Pascal" xml:lang="fr"><term>Cambium</term>
<term>Age</term>
<term>Climat</term>
<term>Cerne bois</term>
<term>Bois initial</term>
<term>Densité</term>
<term>Changement climatique</term>
<term>Bois final</term>
<term>Foresterie</term>
<term>Pinus radiata</term>
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<keywords scheme="Wicri" type="topic" xml:lang="fr"><term>Climat</term>
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<front><div type="abstract" xml:lang="en">Context The correlation between tree ring width and density and short-term climate fluctuations may be a useful tool for predicting response of wood formation process to long-term climate change. . Aims This study examined these correlations for different radiata pine genotypes and aimed at detecting potential genotype by climate interactions. . Methods Four data sets comprising ring width and density of half- and full-sib radiata pine families were used. Correlations with climate variables were examined, after the extraction of the effect of cambial age. . Results Cambial age explained the highest proportion of the ring to ring variation in all variables. Calendar year and year by family interaction explained a smaller but significant proportion of the variation. Rainfall had a positive correlation with ring width and, depending on test site, either a negative or positive correlation with ring density. Correlations between temperature during growing season and ring density were generally negative. . Conclusion Climate variables that influence ring width and wood density can be identified from ring profiles, after removing the cambial age effect. Families can be selected that consistently show desirable response to climate features expected to become prevalent as a result of climate change.</div>
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<fA11 i1="05" i2="1"><s1>ROZENBERG (Philippe)</s1>
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<fA14 i1="01"><s1>Plant Industry, Commonwealth Scientific and Industry Research Organisation, GPO Box 1600</s1>
<s2>Canberra, ACT 2601</s2>
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<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
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<fA14 i1="02"><s1>Dryland Technological Center, The Catholic University of Maule</s1>
<s2>Talca</s2>
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<sZ>4 aut.</sZ>
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<fA14 i1="03"><s1>Unité de Recherche Amelioration, Génétique et Physiologie Forestières, INRA</s1>
<s2>Orléans</s2>
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<sZ>5 aut.</sZ>
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<fA20><s1>525-534</s1>
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<fC01 i1="01" l="ENG"><s0>Context The correlation between tree ring width and density and short-term climate fluctuations may be a useful tool for predicting response of wood formation process to long-term climate change. . Aims This study examined these correlations for different radiata pine genotypes and aimed at detecting potential genotype by climate interactions. . Methods Four data sets comprising ring width and density of half- and full-sib radiata pine families were used. Correlations with climate variables were examined, after the extraction of the effect of cambial age. . Results Cambial age explained the highest proportion of the ring to ring variation in all variables. Calendar year and year by family interaction explained a smaller but significant proportion of the variation. Rainfall had a positive correlation with ring width and, depending on test site, either a negative or positive correlation with ring density. Correlations between temperature during growing season and ring density were generally negative. . Conclusion Climate variables that influence ring width and wood density can be identified from ring profiles, after removing the cambial age effect. Families can be selected that consistently show desirable response to climate features expected to become prevalent as a result of climate change.</s0>
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<s5>03</s5>
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<s5>03</s5>
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<fC03 i1="04" i2="X" l="FRE"><s0>Cerne bois</s0>
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<fC03 i1="04" i2="X" l="ENG"><s0>Tree ring</s0>
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<s5>04</s5>
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<s5>05</s5>
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<fC03 i1="05" i2="X" l="ENG"><s0>Early wood</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="SPA"><s0>Madera inicial</s0>
<s5>05</s5>
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<fC03 i1="06" i2="X" l="FRE"><s0>Densité</s0>
<s5>06</s5>
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<fC03 i1="06" i2="X" l="ENG"><s0>Density</s0>
<s5>06</s5>
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<s5>07</s5>
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<s5>08</s5>
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<s5>08</s5>
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<fC03 i1="08" i2="X" l="SPA"><s0>Madera final</s0>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="X" l="FRE"><s0>Foresterie</s0>
<s5>09</s5>
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<fC03 i1="09" i2="X" l="ENG"><s0>Forestry</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="X" l="SPA"><s0>Ciencias forestales</s0>
<s5>09</s5>
</fC03>
<fC03 i1="10" i2="X" l="FRE"><s0>Pinus radiata</s0>
<s2>NS</s2>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="X" l="ENG"><s0>Pinus radiata</s0>
<s2>NS</s2>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="X" l="SPA"><s0>Pinus radiata</s0>
<s2>NS</s2>
<s5>10</s5>
</fC03>
<fC07 i1="01" i2="X" l="FRE"><s0>Climatologie dynamique</s0>
</fC07>
<fC07 i1="01" i2="X" l="ENG"><s0>Dynamical climatology</s0>
</fC07>
<fC07 i1="01" i2="X" l="SPA"><s0>Climatología dinámica</s0>
</fC07>
<fC07 i1="02" i2="X" l="FRE"><s0>Coniferales</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="02" i2="X" l="ENG"><s0>Coniferales</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="02" i2="X" l="SPA"><s0>Coniferales</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="03" i2="X" l="FRE"><s0>Gymnospermae</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="03" i2="X" l="ENG"><s0>Gymnospermae</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="03" i2="X" l="SPA"><s0>Gymnospermae</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="04" i2="X" l="FRE"><s0>Spermatophyta</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="04" i2="X" l="ENG"><s0>Spermatophyta</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="04" i2="X" l="SPA"><s0>Spermatophyta</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="05" i2="X" l="FRE"><s0>Arbre forestier résineux</s0>
<s5>31</s5>
</fC07>
<fC07 i1="05" i2="X" l="ENG"><s0>Softwood forest tree</s0>
<s5>31</s5>
</fC07>
<fC07 i1="05" i2="X" l="SPA"><s0>Arbol forestal resinoso</s0>
<s5>31</s5>
</fC07>
<fN21><s1>166</s1>
</fN21>
<fN44 i1="01"><s1>OTO</s1>
</fN44>
<fN82><s1>OTO</s1>
</fN82>
</pA>
</standard>
</inist>
</record>

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   |texte=   Influence of cambial age and climate on ring width and wood density in Pinus radiata families
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Influence of cambial age and climate on ring width and wood density in Pinus radiata families

Influence of cambial age and climate on ring width and wood density in Pinus radiata families

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