Out of the Palaeotropics? Historical biogeography and diversification of the cosmopolitan ectomycorrhizal mushroom family Inocybaceae
Identifieur interne : 002E87 ( PascalFrancis/Corpus ); précédent : 002E86; suivant : 002E88Out of the Palaeotropics? Historical biogeography and diversification of the cosmopolitan ectomycorrhizal mushroom family Inocybaceae
Auteurs : P. Brandon Matheny ; M. Catherine Aime ; Neale L. Bougher ; Bart Buyck ; Dennis E. Desjardin ; Egon Horak ; Bradley R. Kropp ; D. Jean Lodge ; Kasem Soytong ; James M. Trappe ; David S. HibbettSource :
- Journal of biogeography [ 0305-0270 ] ; 2009.
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- Pascal (Inist)
English descriptors
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Abstract
Aim The ectomycorrhizal (ECM) mushroom family Inocybaceae is widespread in north temperate regions, but more than 150 species are encountered in the tropics and the Southern Hemisphere. The relative roles of recent and ancient biogeographical processes, relationships with plant hosts, and the timing of divergences that have shaped the current geographic distribution of the family are investigated. Location Africa, Australia, Neotropics, New Zealand, north temperate zone, Palaeotropics, Southeast Asia, South America, south temperate zone. Methods We reconstruct a phylogeny of the Inocybaceae with a geological timeline using a relaxed molecular clock. Divergence dates of lineages are estimated statistically to test vicariance-based hypotheses concerning relatedness of disjunct ECM taxa. A series of internal maximum time constraints is used to evaluate two different calibrations. Ancestral state reconstruction is used to infer ancestral areas and ancestral plant partners of the family. Results The Palaeotropics are unique in containing representatives of all major clades of Inocybaceae. Six of the seven major clades diversified initially during the Cretaceous, with subsequent radiations probably during the early Palaeogene. Vicariance patterns cannot be rejected that involve area relationships for Africa-Australia, Africa-India and southern South America-Australia. Northern and southern South America, Australia and New Zealand are primarily the recipients of immigrant taxa during the Palaeogene or later. Angiosperms were the earliest hosts of Inocybaceae. Transitions to conifers probably occurred no earlier than 65 Ma. Main conclusions The Inocybaceae initially diversified no later than the Cretaceous in Palaeotropical settings, in association with angiosperms. Diversification within major clades of the family accelerated during the Palaeogene in north and south temperate regions, whereas several relictual lineages persisted in the tropics. Both vicariance and dispersal patterns are detected. Species from Neotropical and south temperate regions are largely derived from immigrant ancestors from north temperate or Palaeotropical regions. Transitions to conifer hosts occurred later, probably during the Palaeogene.
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NO : | PASCAL 09-0163619 INIST |
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ET : | Out of the Palaeotropics? Historical biogeography and diversification of the cosmopolitan ectomycorrhizal mushroom family Inocybaceae |
AU : | BRANDON MATHENY (P.); AIME (M. Catherine); BOUGHER (Neale L.); BUYCK (Bart); DESJARDIN (Dennis E.); HORAK (Egon); KROPP (Bradley R.); LODGE (D. Jean); SOYTONG (Kasem); TRAPPE (James M.); HIBBETT (David S.) |
AF : | Biology Department, Clark University/Worcester, MA/Etats-Unis (1 aut., 11 aut.); Department of Plant Pathology and Crop Physiology, Louisiana State University Agricultural Center/Baton Rouge, LA/Etats-Unis (2 aut.); Department of Environment and Conservation, Western Australian Herbarium, Bentley Delivery Centre/Perth, WA/Australie (3 aut.); Muséum National d'Histoire Naturelle, Département Systématique et Evolution, USM 602 -CP 39/Paris/France (4 aut.); Department of Biology, San Francisco State University/San Francisco, CA/Etats-Unis (5 aut.); Nikodemweg 5/Innsbruck/Autriche (6 aut.); Department of Biology, Utah State University/Logan, UT/Etats-Unis (7 aut.); Center for Forest Mycology Research, US Department of Agriculture, Forest Service, Northern Research Station/Luquillo/Porto Rico (8 aut.); Faculty of Agricultural Technology, King Mongkut's Institute of Technology Ladkrabang/Bangkok/Thaïlande (9 aut.); Department of Forest Science, Oregon State University/Corvallis, OR/Etats-Unis (10 aut.) |
DT : | Publication en série; Niveau analytique |
SO : | Journal of biogeography; ISSN 0305-0270; Coden JBIODN; Royaume-Uni; Da. 2009; Vol. 36; No. 4; Pp. 577-592; Bibl. 3 p.1/4 |
LA : | Anglais |
EA : | Aim The ectomycorrhizal (ECM) mushroom family Inocybaceae is widespread in north temperate regions, but more than 150 species are encountered in the tropics and the Southern Hemisphere. The relative roles of recent and ancient biogeographical processes, relationships with plant hosts, and the timing of divergences that have shaped the current geographic distribution of the family are investigated. Location Africa, Australia, Neotropics, New Zealand, north temperate zone, Palaeotropics, Southeast Asia, South America, south temperate zone. Methods We reconstruct a phylogeny of the Inocybaceae with a geological timeline using a relaxed molecular clock. Divergence dates of lineages are estimated statistically to test vicariance-based hypotheses concerning relatedness of disjunct ECM taxa. A series of internal maximum time constraints is used to evaluate two different calibrations. Ancestral state reconstruction is used to infer ancestral areas and ancestral plant partners of the family. Results The Palaeotropics are unique in containing representatives of all major clades of Inocybaceae. Six of the seven major clades diversified initially during the Cretaceous, with subsequent radiations probably during the early Palaeogene. Vicariance patterns cannot be rejected that involve area relationships for Africa-Australia, Africa-India and southern South America-Australia. Northern and southern South America, Australia and New Zealand are primarily the recipients of immigrant taxa during the Palaeogene or later. Angiosperms were the earliest hosts of Inocybaceae. Transitions to conifers probably occurred no earlier than 65 Ma. Main conclusions The Inocybaceae initially diversified no later than the Cretaceous in Palaeotropical settings, in association with angiosperms. Diversification within major clades of the family accelerated during the Palaeogene in north and south temperate regions, whereas several relictual lineages persisted in the tropics. Both vicariance and dispersal patterns are detected. Species from Neotropical and south temperate regions are largely derived from immigrant ancestors from north temperate or Palaeotropical regions. Transitions to conifer hosts occurred later, probably during the Palaeogene. |
CC : | 002A14B04A |
FD : | Historique; Biogéographie; Diversification; Dispersion; Ectomycorhize; Horloge moléculaire; Vicariance; Fungi; Basidiomycota |
FG : | Mycorhize; Symbionte |
ED : | Case history; Biogeography; Diversification; Dispersion; Ectomycorrhiza; Molecular clock; Vicariance; Fungi; Basidiomycota |
EG : | Mycorrhiza; Symbiont |
SD : | Estudio histórico; Biogeografía; Diversificación; Dispersión; Ectomicorriza; Reloj molecular; Vicariancia; Fungi; Basidiomycota |
LO : | INIST-15698.354000184838010020 |
ID : | 09-0163619 |
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Pascal:09-0163619Le document en format XML
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<sourceDesc><biblStruct><analytic><title xml:lang="en" level="a">Out of the Palaeotropics? Historical biogeography and diversification of the cosmopolitan ectomycorrhizal mushroom family Inocybaceae</title>
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<author><name sortKey="Bougher, Neale L" sort="Bougher, Neale L" uniqKey="Bougher N" first="Neale L." last="Bougher">Neale L. Bougher</name>
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<front><div type="abstract" xml:lang="en">Aim The ectomycorrhizal (ECM) mushroom family Inocybaceae is widespread in north temperate regions, but more than 150 species are encountered in the tropics and the Southern Hemisphere. The relative roles of recent and ancient biogeographical processes, relationships with plant hosts, and the timing of divergences that have shaped the current geographic distribution of the family are investigated. Location Africa, Australia, Neotropics, New Zealand, north temperate zone, Palaeotropics, Southeast Asia, South America, south temperate zone. Methods We reconstruct a phylogeny of the Inocybaceae with a geological timeline using a relaxed molecular clock. Divergence dates of lineages are estimated statistically to test vicariance-based hypotheses concerning relatedness of disjunct ECM taxa. A series of internal maximum time constraints is used to evaluate two different calibrations. Ancestral state reconstruction is used to infer ancestral areas and ancestral plant partners of the family. Results The Palaeotropics are unique in containing representatives of all major clades of Inocybaceae. Six of the seven major clades diversified initially during the Cretaceous, with subsequent radiations probably during the early Palaeogene. Vicariance patterns cannot be rejected that involve area relationships for Africa-Australia, Africa-India and southern South America-Australia. Northern and southern South America, Australia and New Zealand are primarily the recipients of immigrant taxa during the Palaeogene or later. Angiosperms were the earliest hosts of Inocybaceae. Transitions to conifers probably occurred no earlier than 65 Ma. Main conclusions The Inocybaceae initially diversified no later than the Cretaceous in Palaeotropical settings, in association with angiosperms. Diversification within major clades of the family accelerated during the Palaeogene in north and south temperate regions, whereas several relictual lineages persisted in the tropics. Both vicariance and dispersal patterns are detected. Species from Neotropical and south temperate regions are largely derived from immigrant ancestors from north temperate or Palaeotropical regions. Transitions to conifer hosts occurred later, probably during the Palaeogene.</div>
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<sZ>1 aut.</sZ>
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<sZ>2 aut.</sZ>
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<sZ>3 aut.</sZ>
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<s3>FRA</s3>
<sZ>4 aut.</sZ>
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<fA14 i1="05"><s1>Department of Biology, San Francisco State University</s1>
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<sZ>5 aut.</sZ>
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<fA14 i1="06"><s1>Nikodemweg 5</s1>
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<fA14 i1="07"><s1>Department of Biology, Utah State University</s1>
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<sZ>7 aut.</sZ>
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<fA14 i1="08"><s1>Center for Forest Mycology Research, US Department of Agriculture, Forest Service, Northern Research Station</s1>
<s2>Luquillo</s2>
<s3>PRI</s3>
<sZ>8 aut.</sZ>
</fA14>
<fA14 i1="09"><s1>Faculty of Agricultural Technology, King Mongkut's Institute of Technology Ladkrabang</s1>
<s2>Bangkok</s2>
<s3>THA</s3>
<sZ>9 aut.</sZ>
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<fA14 i1="10"><s1>Department of Forest Science, Oregon State University</s1>
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<fA66 i1="01"><s0>GBR</s0>
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<fC01 i1="01" l="ENG"><s0>Aim The ectomycorrhizal (ECM) mushroom family Inocybaceae is widespread in north temperate regions, but more than 150 species are encountered in the tropics and the Southern Hemisphere. The relative roles of recent and ancient biogeographical processes, relationships with plant hosts, and the timing of divergences that have shaped the current geographic distribution of the family are investigated. Location Africa, Australia, Neotropics, New Zealand, north temperate zone, Palaeotropics, Southeast Asia, South America, south temperate zone. Methods We reconstruct a phylogeny of the Inocybaceae with a geological timeline using a relaxed molecular clock. Divergence dates of lineages are estimated statistically to test vicariance-based hypotheses concerning relatedness of disjunct ECM taxa. A series of internal maximum time constraints is used to evaluate two different calibrations. Ancestral state reconstruction is used to infer ancestral areas and ancestral plant partners of the family. Results The Palaeotropics are unique in containing representatives of all major clades of Inocybaceae. Six of the seven major clades diversified initially during the Cretaceous, with subsequent radiations probably during the early Palaeogene. Vicariance patterns cannot be rejected that involve area relationships for Africa-Australia, Africa-India and southern South America-Australia. Northern and southern South America, Australia and New Zealand are primarily the recipients of immigrant taxa during the Palaeogene or later. Angiosperms were the earliest hosts of Inocybaceae. Transitions to conifers probably occurred no earlier than 65 Ma. Main conclusions The Inocybaceae initially diversified no later than the Cretaceous in Palaeotropical settings, in association with angiosperms. Diversification within major clades of the family accelerated during the Palaeogene in north and south temperate regions, whereas several relictual lineages persisted in the tropics. Both vicariance and dispersal patterns are detected. Species from Neotropical and south temperate regions are largely derived from immigrant ancestors from north temperate or Palaeotropical regions. Transitions to conifer hosts occurred later, probably during the Palaeogene.</s0>
</fC01>
<fC02 i1="01" i2="X"><s0>002A14B04A</s0>
</fC02>
<fC03 i1="01" i2="X" l="FRE"><s0>Historique</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="X" l="ENG"><s0>Case history</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="X" l="SPA"><s0>Estudio histórico</s0>
<s5>01</s5>
</fC03>
<fC03 i1="02" i2="X" l="FRE"><s0>Biogéographie</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="X" l="ENG"><s0>Biogeography</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="X" l="SPA"><s0>Biogeografía</s0>
<s5>02</s5>
</fC03>
<fC03 i1="03" i2="X" l="FRE"><s0>Diversification</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="X" l="ENG"><s0>Diversification</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="X" l="SPA"><s0>Diversificación</s0>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="X" l="FRE"><s0>Dispersion</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="X" l="ENG"><s0>Dispersion</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="X" l="SPA"><s0>Dispersión</s0>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="X" l="FRE"><s0>Ectomycorhize</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="ENG"><s0>Ectomycorrhiza</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="SPA"><s0>Ectomicorriza</s0>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="X" l="FRE"><s0>Horloge moléculaire</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="ENG"><s0>Molecular clock</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="SPA"><s0>Reloj molecular</s0>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="X" l="FRE"><s0>Vicariance</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="X" l="ENG"><s0>Vicariance</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="X" l="SPA"><s0>Vicariancia</s0>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="X" l="FRE"><s0>Fungi</s0>
<s2>NS</s2>
<s5>49</s5>
</fC03>
<fC03 i1="08" i2="X" l="ENG"><s0>Fungi</s0>
<s2>NS</s2>
<s5>49</s5>
</fC03>
<fC03 i1="08" i2="X" l="SPA"><s0>Fungi</s0>
<s2>NS</s2>
<s5>49</s5>
</fC03>
<fC03 i1="09" i2="X" l="FRE"><s0>Basidiomycota</s0>
<s2>NS</s2>
<s5>50</s5>
</fC03>
<fC03 i1="09" i2="X" l="ENG"><s0>Basidiomycota</s0>
<s2>NS</s2>
<s5>50</s5>
</fC03>
<fC03 i1="09" i2="X" l="SPA"><s0>Basidiomycota</s0>
<s2>NS</s2>
<s5>50</s5>
</fC03>
<fC07 i1="01" i2="X" l="FRE"><s0>Mycorhize</s0>
</fC07>
<fC07 i1="01" i2="X" l="ENG"><s0>Mycorrhiza</s0>
</fC07>
<fC07 i1="01" i2="X" l="SPA"><s0>Micorriza</s0>
</fC07>
<fC07 i1="02" i2="X" l="FRE"><s0>Symbionte</s0>
<s5>17</s5>
</fC07>
<fC07 i1="02" i2="X" l="ENG"><s0>Symbiont</s0>
<s5>17</s5>
</fC07>
<fC07 i1="02" i2="X" l="SPA"><s0>Simbionte</s0>
<s5>17</s5>
</fC07>
<fN21><s1>117</s1>
</fN21>
<fN44 i1="01"><s1>OTO</s1>
</fN44>
<fN82><s1>OTO</s1>
</fN82>
</pA>
</standard>
<server><NO>PASCAL 09-0163619 INIST</NO>
<ET>Out of the Palaeotropics? Historical biogeography and diversification of the cosmopolitan ectomycorrhizal mushroom family Inocybaceae</ET>
<AU>BRANDON MATHENY (P.); AIME (M. Catherine); BOUGHER (Neale L.); BUYCK (Bart); DESJARDIN (Dennis E.); HORAK (Egon); KROPP (Bradley R.); LODGE (D. Jean); SOYTONG (Kasem); TRAPPE (James M.); HIBBETT (David S.)</AU>
<AF>Biology Department, Clark University/Worcester, MA/Etats-Unis (1 aut., 11 aut.); Department of Plant Pathology and Crop Physiology, Louisiana State University Agricultural Center/Baton Rouge, LA/Etats-Unis (2 aut.); Department of Environment and Conservation, Western Australian Herbarium, Bentley Delivery Centre/Perth, WA/Australie (3 aut.); Muséum National d'Histoire Naturelle, Département Systématique et Evolution, USM 602 -CP 39/Paris/France (4 aut.); Department of Biology, San Francisco State University/San Francisco, CA/Etats-Unis (5 aut.); Nikodemweg 5/Innsbruck/Autriche (6 aut.); Department of Biology, Utah State University/Logan, UT/Etats-Unis (7 aut.); Center for Forest Mycology Research, US Department of Agriculture, Forest Service, Northern Research Station/Luquillo/Porto Rico (8 aut.); Faculty of Agricultural Technology, King Mongkut's Institute of Technology Ladkrabang/Bangkok/Thaïlande (9 aut.); Department of Forest Science, Oregon State University/Corvallis, OR/Etats-Unis (10 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>Journal of biogeography; ISSN 0305-0270; Coden JBIODN; Royaume-Uni; Da. 2009; Vol. 36; No. 4; Pp. 577-592; Bibl. 3 p.1/4</SO>
<LA>Anglais</LA>
<EA>Aim The ectomycorrhizal (ECM) mushroom family Inocybaceae is widespread in north temperate regions, but more than 150 species are encountered in the tropics and the Southern Hemisphere. The relative roles of recent and ancient biogeographical processes, relationships with plant hosts, and the timing of divergences that have shaped the current geographic distribution of the family are investigated. Location Africa, Australia, Neotropics, New Zealand, north temperate zone, Palaeotropics, Southeast Asia, South America, south temperate zone. Methods We reconstruct a phylogeny of the Inocybaceae with a geological timeline using a relaxed molecular clock. Divergence dates of lineages are estimated statistically to test vicariance-based hypotheses concerning relatedness of disjunct ECM taxa. A series of internal maximum time constraints is used to evaluate two different calibrations. Ancestral state reconstruction is used to infer ancestral areas and ancestral plant partners of the family. Results The Palaeotropics are unique in containing representatives of all major clades of Inocybaceae. Six of the seven major clades diversified initially during the Cretaceous, with subsequent radiations probably during the early Palaeogene. Vicariance patterns cannot be rejected that involve area relationships for Africa-Australia, Africa-India and southern South America-Australia. Northern and southern South America, Australia and New Zealand are primarily the recipients of immigrant taxa during the Palaeogene or later. Angiosperms were the earliest hosts of Inocybaceae. Transitions to conifers probably occurred no earlier than 65 Ma. Main conclusions The Inocybaceae initially diversified no later than the Cretaceous in Palaeotropical settings, in association with angiosperms. Diversification within major clades of the family accelerated during the Palaeogene in north and south temperate regions, whereas several relictual lineages persisted in the tropics. Both vicariance and dispersal patterns are detected. Species from Neotropical and south temperate regions are largely derived from immigrant ancestors from north temperate or Palaeotropical regions. Transitions to conifer hosts occurred later, probably during the Palaeogene.</EA>
<CC>002A14B04A</CC>
<FD>Historique; Biogéographie; Diversification; Dispersion; Ectomycorhize; Horloge moléculaire; Vicariance; Fungi; Basidiomycota</FD>
<FG>Mycorhize; Symbionte</FG>
<ED>Case history; Biogeography; Diversification; Dispersion; Ectomycorrhiza; Molecular clock; Vicariance; Fungi; Basidiomycota</ED>
<EG>Mycorrhiza; Symbiont</EG>
<SD>Estudio histórico; Biogeografía; Diversificación; Dispersión; Ectomicorriza; Reloj molecular; Vicariancia; Fungi; Basidiomycota</SD>
<LO>INIST-15698.354000184838010020</LO>
<ID>09-0163619</ID>
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