Serveur d'exploration sur l'esturgeon

Attention, ce site est en cours de développement !
Attention, site généré par des moyens informatiques à partir de corpus bruts.
Les informations ne sont donc pas validées.

Suitability of lake sturgeon growth rings in chronology development

Identifieur interne : 000359 ( PascalFrancis/Corpus ); précédent : 000358; suivant : 000360

Suitability of lake sturgeon growth rings in chronology development

Auteurs : G. T. O. Lebreton ; F. W. H. Beamish

Source :

RBID : Pascal:00-0386788

Descripteurs français

English descriptors

Abstract

The purpose of this investigation was to determine if ring widths in the cross section of lake sturgeon pectoral fin rays satisfy three criteria required of structures used in the development of growth chronologies. First, ring widths must be related to the overall somatic growth of the organism. Second, ring widths must demonstrate synchrony of interannual growth variation among individuals within a population. Finally, fin ray rings and growth chronologies should be related to both interpopulation and interannual variations of known environmental factors. This research indicated that ring widths document variations in somatic growth. Average fin ray cross-sectional radii at age 25 were related to total length using data from seven populations sampled across North America. This investigation also suggested that growth ring widths were influenced by large-scale, population-wide, extrinsic factors in two ways. First, differences between populations in fin ray cross-sectional radii at age 25 were strongly correlated with mean annual, summer, and winter air temperatures. Second, growth chronologies developed from populations that demonstrate significant synchrony of interannual growth variations among members are consistently positively correlated to past air-temperature records. This research has provided evidence that growth rings contained in the cross section of the lake sturgeon pectoral fin ray can be used in the construction of growth chronologies.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

pA  
A01 01  1    @0 0002-8487
A02 01      @0 TAFSAI
A03   1    @0 Trans. Am. Fish. Soc. : (1900)
A05       @2 129
A06       @2 4
A08 01  1  ENG  @1 Suitability of lake sturgeon growth rings in chronology development
A11 01  1    @1 LEBRETON (G. T. O.)
A11 02  1    @1 BEAMISH (F. W. H.)
A14 01      @1 Department of Zoology, University of Guelph @2 Guelph, Ontario N1G 2W1 @3 CAN @Z 1 aut. @Z 2 aut.
A20       @1 1018-1030
A21       @1 2000
A23 01      @0 ENG
A43 01      @1 INIST @2 9749 @5 354000090854580100
A44       @0 0000 @1 © 2000 INIST-CNRS. All rights reserved.
A45       @0 1 p.1/4
A47 01  1    @0 00-0386788
A60       @1 P
A61       @0 A
A64 01  1    @0 Transactions of the American Fisheries Society : (1900)
A66 01      @0 USA
C01 01    ENG  @0 The purpose of this investigation was to determine if ring widths in the cross section of lake sturgeon pectoral fin rays satisfy three criteria required of structures used in the development of growth chronologies. First, ring widths must be related to the overall somatic growth of the organism. Second, ring widths must demonstrate synchrony of interannual growth variation among individuals within a population. Finally, fin ray rings and growth chronologies should be related to both interpopulation and interannual variations of known environmental factors. This research indicated that ring widths document variations in somatic growth. Average fin ray cross-sectional radii at age 25 were related to total length using data from seven populations sampled across North America. This investigation also suggested that growth ring widths were influenced by large-scale, population-wide, extrinsic factors in two ways. First, differences between populations in fin ray cross-sectional radii at age 25 were strongly correlated with mean annual, summer, and winter air temperatures. Second, growth chronologies developed from populations that demonstrate significant synchrony of interannual growth variations among members are consistently positively correlated to past air-temperature records. This research has provided evidence that growth rings contained in the cross section of the lake sturgeon pectoral fin ray can be used in the construction of growth chronologies.
C02 01  X    @0 002A14B02C2A
C03 01  X  FRE  @0 Croissance @5 01
C03 01  X  ENG  @0 Growth @5 01
C03 01  X  SPA  @0 Crecimiento @5 01
C03 02  X  FRE  @0 Taille corporelle @5 02
C03 02  X  ENG  @0 Body size @5 02
C03 02  X  SPA  @0 Talla corporal @5 02
C03 03  X  FRE  @0 Nageoire pectorale @5 03
C03 03  X  ENG  @0 Pectoral fin @5 03
C03 03  X  SPA  @0 Aleta pectoral @5 03
C03 04  X  FRE  @0 Anneau croissance @5 04
C03 04  X  ENG  @0 Growth ring @5 04
C03 04  X  SPA  @0 Anillo crecimiento @5 04
C03 05  X  FRE  @0 Age @5 05
C03 05  X  ENG  @0 Age @5 05
C03 05  X  SPA  @0 Edad @5 05
C03 06  X  FRE  @0 Température @5 06
C03 06  X  ENG  @0 Temperature @5 06
C03 06  X  SPA  @0 Temperatura @5 06
C03 07  X  FRE  @0 Variation interannuelle @5 07
C03 07  X  ENG  @0 Interannual variation @5 07
C03 07  X  SPA  @0 Variación interanual @5 07
C03 08  X  FRE  @0 Modèle linéaire généralisé @5 09
C03 08  X  ENG  @0 Generalized linear model @5 09
C03 08  X  SPA  @0 Modelo lineal generalizado @5 09
C03 09  X  FRE  @0 Etude comparative @5 10
C03 09  X  ENG  @0 Comparative study @5 10
C03 09  X  SPA  @0 Estudio comparativo @5 10
C03 10  X  FRE  @0 Lac @5 11
C03 10  X  ENG  @0 Lakes @5 11
C03 10  X  SPA  @0 Lago @5 11
C03 11  X  FRE  @0 Etats Unis @2 NG @5 12
C03 11  X  ENG  @0 United States @2 NG @5 12
C03 11  X  SPA  @0 Estados Unidos @2 NG @5 12
C03 12  X  FRE  @0 Acipenser fulvescens @2 NS @4 INC @5 64
C07 01  X  FRE  @0 Amérique du Nord @2 NG
C07 01  X  ENG  @0 North America @2 NG
C07 01  X  SPA  @0 America del norte @2 NG
C07 02  X  FRE  @0 Amérique @2 NG
C07 02  X  ENG  @0 America @2 NG
C07 02  X  SPA  @0 America @2 NG
C07 03  X  FRE  @0 Milieu eau douce @5 17
C07 03  X  ENG  @0 Freshwater environment @5 17
C07 03  X  SPA  @0 Medio agua dulce @5 17
C07 04  X  FRE  @0 Facteur milieu @5 18
C07 04  X  ENG  @0 Environmental factor @5 18
C07 04  X  SPA  @0 Factor medio @5 18
C07 05  X  FRE  @0 Pisces @2 NS @5 60
C07 05  X  ENG  @0 Pisces @2 NS @5 60
C07 05  X  SPA  @0 Pisces @2 NS @5 60
C07 06  X  FRE  @0 Vertebrata @2 NS
C07 06  X  ENG  @0 Vertebrata @2 NS
C07 06  X  SPA  @0 Vertebrata @2 NS
C07 07  X  FRE  @0 Acipenseridae @2 NS @4 INC @5 70
N21       @1 262

Format Inist (serveur)

NO : PASCAL 00-0386788 INIST
ET : Suitability of lake sturgeon growth rings in chronology development
AU : LEBRETON (G. T. O.); BEAMISH (F. W. H.)
AF : Department of Zoology, University of Guelph/Guelph, Ontario N1G 2W1/Canada (1 aut., 2 aut.)
DT : Publication en série; Niveau analytique
SO : Transactions of the American Fisheries Society : (1900); ISSN 0002-8487; Coden TAFSAI; Etats-Unis; Da. 2000; Vol. 129; No. 4; Pp. 1018-1030; Bibl. 1 p.1/4
LA : Anglais
EA : The purpose of this investigation was to determine if ring widths in the cross section of lake sturgeon pectoral fin rays satisfy three criteria required of structures used in the development of growth chronologies. First, ring widths must be related to the overall somatic growth of the organism. Second, ring widths must demonstrate synchrony of interannual growth variation among individuals within a population. Finally, fin ray rings and growth chronologies should be related to both interpopulation and interannual variations of known environmental factors. This research indicated that ring widths document variations in somatic growth. Average fin ray cross-sectional radii at age 25 were related to total length using data from seven populations sampled across North America. This investigation also suggested that growth ring widths were influenced by large-scale, population-wide, extrinsic factors in two ways. First, differences between populations in fin ray cross-sectional radii at age 25 were strongly correlated with mean annual, summer, and winter air temperatures. Second, growth chronologies developed from populations that demonstrate significant synchrony of interannual growth variations among members are consistently positively correlated to past air-temperature records. This research has provided evidence that growth rings contained in the cross section of the lake sturgeon pectoral fin ray can be used in the construction of growth chronologies.
CC : 002A14B02C2A
FD : Croissance; Taille corporelle; Nageoire pectorale; Anneau croissance; Age; Température; Variation interannuelle; Modèle linéaire généralisé; Etude comparative; Lac; Etats Unis; Acipenser fulvescens
FG : Amérique du Nord; Amérique; Milieu eau douce; Facteur milieu; Pisces; Vertebrata; Acipenseridae
ED : Growth; Body size; Pectoral fin; Growth ring; Age; Temperature; Interannual variation; Generalized linear model; Comparative study; Lakes; United States
EG : North America; America; Freshwater environment; Environmental factor; Pisces; Vertebrata
SD : Crecimiento; Talla corporal; Aleta pectoral; Anillo crecimiento; Edad; Temperatura; Variación interanual; Modelo lineal generalizado; Estudio comparativo; Lago; Estados Unidos
LO : INIST-9749.354000090854580100
ID : 00-0386788

Links to Exploration step

Pascal:00-0386788

Le document en format XML

<record>
<TEI>
<teiHeader>
<fileDesc>
<titleStmt>
<title xml:lang="en" level="a">Suitability of lake sturgeon growth rings in chronology development</title>
<author>
<name sortKey="Lebreton, G T O" sort="Lebreton, G T O" uniqKey="Lebreton G" first="G. T. O." last="Lebreton">G. T. O. Lebreton</name>
<affiliation>
<inist:fA14 i1="01">
<s1>Department of Zoology, University of Guelph</s1>
<s2>Guelph, Ontario N1G 2W1</s2>
<s3>CAN</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author>
<name sortKey="Beamish, F W H" sort="Beamish, F W H" uniqKey="Beamish F" first="F. W. H." last="Beamish">F. W. H. Beamish</name>
<affiliation>
<inist:fA14 i1="01">
<s1>Department of Zoology, University of Guelph</s1>
<s2>Guelph, Ontario N1G 2W1</s2>
<s3>CAN</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
</titleStmt>
<publicationStmt>
<idno type="wicri:source">INIST</idno>
<idno type="inist">00-0386788</idno>
<date when="2000">2000</date>
<idno type="stanalyst">PASCAL 00-0386788 INIST</idno>
<idno type="RBID">Pascal:00-0386788</idno>
<idno type="wicri:Area/PascalFrancis/Corpus">000359</idno>
</publicationStmt>
<sourceDesc>
<biblStruct>
<analytic>
<title xml:lang="en" level="a">Suitability of lake sturgeon growth rings in chronology development</title>
<author>
<name sortKey="Lebreton, G T O" sort="Lebreton, G T O" uniqKey="Lebreton G" first="G. T. O." last="Lebreton">G. T. O. Lebreton</name>
<affiliation>
<inist:fA14 i1="01">
<s1>Department of Zoology, University of Guelph</s1>
<s2>Guelph, Ontario N1G 2W1</s2>
<s3>CAN</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author>
<name sortKey="Beamish, F W H" sort="Beamish, F W H" uniqKey="Beamish F" first="F. W. H." last="Beamish">F. W. H. Beamish</name>
<affiliation>
<inist:fA14 i1="01">
<s1>Department of Zoology, University of Guelph</s1>
<s2>Guelph, Ontario N1G 2W1</s2>
<s3>CAN</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
</analytic>
<series>
<title level="j" type="main">Transactions of the American Fisheries Society : (1900)</title>
<title level="j" type="abbreviated">Trans. Am. Fish. Soc. : (1900)</title>
<idno type="ISSN">0002-8487</idno>
<imprint>
<date when="2000">2000</date>
</imprint>
</series>
</biblStruct>
</sourceDesc>
<seriesStmt>
<title level="j" type="main">Transactions of the American Fisheries Society : (1900)</title>
<title level="j" type="abbreviated">Trans. Am. Fish. Soc. : (1900)</title>
<idno type="ISSN">0002-8487</idno>
</seriesStmt>
</fileDesc>
<profileDesc>
<textClass>
<keywords scheme="KwdEn" xml:lang="en">
<term>Age</term>
<term>Body size</term>
<term>Comparative study</term>
<term>Generalized linear model</term>
<term>Growth</term>
<term>Growth ring</term>
<term>Interannual variation</term>
<term>Lakes</term>
<term>Pectoral fin</term>
<term>Temperature</term>
<term>United States</term>
</keywords>
<keywords scheme="Pascal" xml:lang="fr">
<term>Croissance</term>
<term>Taille corporelle</term>
<term>Nageoire pectorale</term>
<term>Anneau croissance</term>
<term>Age</term>
<term>Température</term>
<term>Variation interannuelle</term>
<term>Modèle linéaire généralisé</term>
<term>Etude comparative</term>
<term>Lac</term>
<term>Etats Unis</term>
<term>Acipenser fulvescens</term>
</keywords>
</textClass>
</profileDesc>
</teiHeader>
<front>
<div type="abstract" xml:lang="en">The purpose of this investigation was to determine if ring widths in the cross section of lake sturgeon pectoral fin rays satisfy three criteria required of structures used in the development of growth chronologies. First, ring widths must be related to the overall somatic growth of the organism. Second, ring widths must demonstrate synchrony of interannual growth variation among individuals within a population. Finally, fin ray rings and growth chronologies should be related to both interpopulation and interannual variations of known environmental factors. This research indicated that ring widths document variations in somatic growth. Average fin ray cross-sectional radii at age 25 were related to total length using data from seven populations sampled across North America. This investigation also suggested that growth ring widths were influenced by large-scale, population-wide, extrinsic factors in two ways. First, differences between populations in fin ray cross-sectional radii at age 25 were strongly correlated with mean annual, summer, and winter air temperatures. Second, growth chronologies developed from populations that demonstrate significant synchrony of interannual growth variations among members are consistently positively correlated to past air-temperature records. This research has provided evidence that growth rings contained in the cross section of the lake sturgeon pectoral fin ray can be used in the construction of growth chronologies.</div>
</front>
</TEI>
<inist>
<standard h6="B">
<pA>
<fA01 i1="01" i2="1">
<s0>0002-8487</s0>
</fA01>
<fA02 i1="01">
<s0>TAFSAI</s0>
</fA02>
<fA03 i2="1">
<s0>Trans. Am. Fish. Soc. : (1900)</s0>
</fA03>
<fA05>
<s2>129</s2>
</fA05>
<fA06>
<s2>4</s2>
</fA06>
<fA08 i1="01" i2="1" l="ENG">
<s1>Suitability of lake sturgeon growth rings in chronology development</s1>
</fA08>
<fA11 i1="01" i2="1">
<s1>LEBRETON (G. T. O.)</s1>
</fA11>
<fA11 i1="02" i2="1">
<s1>BEAMISH (F. W. H.)</s1>
</fA11>
<fA14 i1="01">
<s1>Department of Zoology, University of Guelph</s1>
<s2>Guelph, Ontario N1G 2W1</s2>
<s3>CAN</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
</fA14>
<fA20>
<s1>1018-1030</s1>
</fA20>
<fA21>
<s1>2000</s1>
</fA21>
<fA23 i1="01">
<s0>ENG</s0>
</fA23>
<fA43 i1="01">
<s1>INIST</s1>
<s2>9749</s2>
<s5>354000090854580100</s5>
</fA43>
<fA44>
<s0>0000</s0>
<s1>© 2000 INIST-CNRS. All rights reserved.</s1>
</fA44>
<fA45>
<s0>1 p.1/4</s0>
</fA45>
<fA47 i1="01" i2="1">
<s0>00-0386788</s0>
</fA47>
<fA60>
<s1>P</s1>
</fA60>
<fA61>
<s0>A</s0>
</fA61>
<fA64 i1="01" i2="1">
<s0>Transactions of the American Fisheries Society : (1900)</s0>
</fA64>
<fA66 i1="01">
<s0>USA</s0>
</fA66>
<fC01 i1="01" l="ENG">
<s0>The purpose of this investigation was to determine if ring widths in the cross section of lake sturgeon pectoral fin rays satisfy three criteria required of structures used in the development of growth chronologies. First, ring widths must be related to the overall somatic growth of the organism. Second, ring widths must demonstrate synchrony of interannual growth variation among individuals within a population. Finally, fin ray rings and growth chronologies should be related to both interpopulation and interannual variations of known environmental factors. This research indicated that ring widths document variations in somatic growth. Average fin ray cross-sectional radii at age 25 were related to total length using data from seven populations sampled across North America. This investigation also suggested that growth ring widths were influenced by large-scale, population-wide, extrinsic factors in two ways. First, differences between populations in fin ray cross-sectional radii at age 25 were strongly correlated with mean annual, summer, and winter air temperatures. Second, growth chronologies developed from populations that demonstrate significant synchrony of interannual growth variations among members are consistently positively correlated to past air-temperature records. This research has provided evidence that growth rings contained in the cross section of the lake sturgeon pectoral fin ray can be used in the construction of growth chronologies.</s0>
</fC01>
<fC02 i1="01" i2="X">
<s0>002A14B02C2A</s0>
</fC02>
<fC03 i1="01" i2="X" l="FRE">
<s0>Croissance</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="X" l="ENG">
<s0>Growth</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="X" l="SPA">
<s0>Crecimiento</s0>
<s5>01</s5>
</fC03>
<fC03 i1="02" i2="X" l="FRE">
<s0>Taille corporelle</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="X" l="ENG">
<s0>Body size</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="X" l="SPA">
<s0>Talla corporal</s0>
<s5>02</s5>
</fC03>
<fC03 i1="03" i2="X" l="FRE">
<s0>Nageoire pectorale</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="X" l="ENG">
<s0>Pectoral fin</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="X" l="SPA">
<s0>Aleta pectoral</s0>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="X" l="FRE">
<s0>Anneau croissance</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="X" l="ENG">
<s0>Growth ring</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="X" l="SPA">
<s0>Anillo crecimiento</s0>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="X" l="FRE">
<s0>Age</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="ENG">
<s0>Age</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="SPA">
<s0>Edad</s0>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="X" l="FRE">
<s0>Température</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="ENG">
<s0>Temperature</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="SPA">
<s0>Temperatura</s0>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="X" l="FRE">
<s0>Variation interannuelle</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="X" l="ENG">
<s0>Interannual variation</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="X" l="SPA">
<s0>Variación interanual</s0>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="X" l="FRE">
<s0>Modèle linéaire généralisé</s0>
<s5>09</s5>
</fC03>
<fC03 i1="08" i2="X" l="ENG">
<s0>Generalized linear model</s0>
<s5>09</s5>
</fC03>
<fC03 i1="08" i2="X" l="SPA">
<s0>Modelo lineal generalizado</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="X" l="FRE">
<s0>Etude comparative</s0>
<s5>10</s5>
</fC03>
<fC03 i1="09" i2="X" l="ENG">
<s0>Comparative study</s0>
<s5>10</s5>
</fC03>
<fC03 i1="09" i2="X" l="SPA">
<s0>Estudio comparativo</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="X" l="FRE">
<s0>Lac</s0>
<s5>11</s5>
</fC03>
<fC03 i1="10" i2="X" l="ENG">
<s0>Lakes</s0>
<s5>11</s5>
</fC03>
<fC03 i1="10" i2="X" l="SPA">
<s0>Lago</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="X" l="FRE">
<s0>Etats Unis</s0>
<s2>NG</s2>
<s5>12</s5>
</fC03>
<fC03 i1="11" i2="X" l="ENG">
<s0>United States</s0>
<s2>NG</s2>
<s5>12</s5>
</fC03>
<fC03 i1="11" i2="X" l="SPA">
<s0>Estados Unidos</s0>
<s2>NG</s2>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="X" l="FRE">
<s0>Acipenser fulvescens</s0>
<s2>NS</s2>
<s4>INC</s4>
<s5>64</s5>
</fC03>
<fC07 i1="01" i2="X" l="FRE">
<s0>Amérique du Nord</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="X" l="ENG">
<s0>North America</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="X" l="SPA">
<s0>America del norte</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="X" l="FRE">
<s0>Amérique</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="X" l="ENG">
<s0>America</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="X" l="SPA">
<s0>America</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="03" i2="X" l="FRE">
<s0>Milieu eau douce</s0>
<s5>17</s5>
</fC07>
<fC07 i1="03" i2="X" l="ENG">
<s0>Freshwater environment</s0>
<s5>17</s5>
</fC07>
<fC07 i1="03" i2="X" l="SPA">
<s0>Medio agua dulce</s0>
<s5>17</s5>
</fC07>
<fC07 i1="04" i2="X" l="FRE">
<s0>Facteur milieu</s0>
<s5>18</s5>
</fC07>
<fC07 i1="04" i2="X" l="ENG">
<s0>Environmental factor</s0>
<s5>18</s5>
</fC07>
<fC07 i1="04" i2="X" l="SPA">
<s0>Factor medio</s0>
<s5>18</s5>
</fC07>
<fC07 i1="05" i2="X" l="FRE">
<s0>Pisces</s0>
<s2>NS</s2>
<s5>60</s5>
</fC07>
<fC07 i1="05" i2="X" l="ENG">
<s0>Pisces</s0>
<s2>NS</s2>
<s5>60</s5>
</fC07>
<fC07 i1="05" i2="X" l="SPA">
<s0>Pisces</s0>
<s2>NS</s2>
<s5>60</s5>
</fC07>
<fC07 i1="06" i2="X" l="FRE">
<s0>Vertebrata</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="06" i2="X" l="ENG">
<s0>Vertebrata</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="06" i2="X" l="SPA">
<s0>Vertebrata</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="07" i2="X" l="FRE">
<s0>Acipenseridae</s0>
<s2>NS</s2>
<s4>INC</s4>
<s5>70</s5>
</fC07>
<fN21>
<s1>262</s1>
</fN21>
</pA>
</standard>
<server>
<NO>PASCAL 00-0386788 INIST</NO>
<ET>Suitability of lake sturgeon growth rings in chronology development</ET>
<AU>LEBRETON (G. T. O.); BEAMISH (F. W. H.)</AU>
<AF>Department of Zoology, University of Guelph/Guelph, Ontario N1G 2W1/Canada (1 aut., 2 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>Transactions of the American Fisheries Society : (1900); ISSN 0002-8487; Coden TAFSAI; Etats-Unis; Da. 2000; Vol. 129; No. 4; Pp. 1018-1030; Bibl. 1 p.1/4</SO>
<LA>Anglais</LA>
<EA>The purpose of this investigation was to determine if ring widths in the cross section of lake sturgeon pectoral fin rays satisfy three criteria required of structures used in the development of growth chronologies. First, ring widths must be related to the overall somatic growth of the organism. Second, ring widths must demonstrate synchrony of interannual growth variation among individuals within a population. Finally, fin ray rings and growth chronologies should be related to both interpopulation and interannual variations of known environmental factors. This research indicated that ring widths document variations in somatic growth. Average fin ray cross-sectional radii at age 25 were related to total length using data from seven populations sampled across North America. This investigation also suggested that growth ring widths were influenced by large-scale, population-wide, extrinsic factors in two ways. First, differences between populations in fin ray cross-sectional radii at age 25 were strongly correlated with mean annual, summer, and winter air temperatures. Second, growth chronologies developed from populations that demonstrate significant synchrony of interannual growth variations among members are consistently positively correlated to past air-temperature records. This research has provided evidence that growth rings contained in the cross section of the lake sturgeon pectoral fin ray can be used in the construction of growth chronologies.</EA>
<CC>002A14B02C2A</CC>
<FD>Croissance; Taille corporelle; Nageoire pectorale; Anneau croissance; Age; Température; Variation interannuelle; Modèle linéaire généralisé; Etude comparative; Lac; Etats Unis; Acipenser fulvescens</FD>
<FG>Amérique du Nord; Amérique; Milieu eau douce; Facteur milieu; Pisces; Vertebrata; Acipenseridae</FG>
<ED>Growth; Body size; Pectoral fin; Growth ring; Age; Temperature; Interannual variation; Generalized linear model; Comparative study; Lakes; United States</ED>
<EG>North America; America; Freshwater environment; Environmental factor; Pisces; Vertebrata</EG>
<SD>Crecimiento; Talla corporal; Aleta pectoral; Anillo crecimiento; Edad; Temperatura; Variación interanual; Modelo lineal generalizado; Estudio comparativo; Lago; Estados Unidos</SD>
<LO>INIST-9749.354000090854580100</LO>
<ID>00-0386788</ID>
</server>
</inist>
</record>

Pour manipuler ce document sous Unix (Dilib)

EXPLOR_STEP=$WICRI_ROOT/Wicri/Eau/explor/EsturgeonV1/Data/PascalFrancis/Corpus
HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 000359 | SxmlIndent | more

Ou

HfdSelect -h $EXPLOR_AREA/Data/PascalFrancis/Corpus/biblio.hfd -nk 000359 | SxmlIndent | more

Pour mettre un lien sur cette page dans le réseau Wicri

{{Explor lien
   |wiki=    Wicri/Eau
   |area=    EsturgeonV1
   |flux=    PascalFrancis
   |étape=   Corpus
   |type=    RBID
   |clé=     Pascal:00-0386788
   |texte=   Suitability of lake sturgeon growth rings in chronology development
}}

Wicri

This area was generated with Dilib version V0.6.27.
Data generation: Sat Mar 25 15:37:54 2017. Site generation: Tue Feb 13 14:18:49 2024