The historical biogeography of Scabiosa (Dipsacaceae): implications for Old World plant disjunctions
Identifieur interne : 000758 ( Istex/Corpus ); précédent : 000757; suivant : 000759The historical biogeography of Scabiosa (Dipsacaceae): implications for Old World plant disjunctions
Auteurs : Sara E. Carlson ; H. Peter Linder ; Michael J. DonoghueSource :
- Journal of Biogeography [ 0305-0270 ] ; 2012-06.
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Abstract
Aim To reconstruct the temporal and biogeographical history of Old World disjunctions in Scabiosa (Dipsacaceae) and the timing of diversification in the Mediterranean Basin, in order to evaluate the importance of biogeographical and climatological history (particularly the onset of a mediterranean climate) in shaping Scabiosa distributions.
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DOI: 10.1111/j.1365-2699.2011.02669.x
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<front><div type="abstract">Aim To reconstruct the temporal and biogeographical history of Old World disjunctions in Scabiosa (Dipsacaceae) and the timing of diversification in the Mediterranean Basin, in order to evaluate the importance of biogeographical and climatological history (particularly the onset of a mediterranean climate) in shaping Scabiosa distributions.</div>
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<abstract><p>Aim To reconstruct the temporal and biogeographical history of Old World disjunctions in Scabiosa (Dipsacaceae) and the timing of diversification in the Mediterranean Basin, in order to evaluate the importance of biogeographical and climatological history (particularly the onset of a mediterranean climate) in shaping Scabiosa distributions.</p>
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<abstract><p>Location Europe and the Mediterranean Basin, southern Africa and eastern Asia.</p>
</abstract>
<abstract><p>Methods This study uses maximum‐likelihood and Bayesian phylogenetic analyses of chloroplast DNA (atpB–rbcL, trnL–trnF, trnS–trnG, psbA–trnH) and nuclear ribosomal DNA [internal transcribed spacer (ITS) and external transcribed spacer (ETS)] from 24 out of c. 37 ingroup taxa, beast molecular dating, and the dispersal–extinction–cladogenesis method (Lagrange) to reconstruct ancestral geographical ranges and the timing of diversification of the major clades of Scabiosa.</p>
</abstract>
<abstract><p>Results Biogeographical and divergence time reconstructions showed that Scabiosa originated during the Miocene and diversified in Europe, followed by independent movements into Asia and Africa. Several of the major clades were inferred to have radiated sometime between the late Miocene and early Pleistocene, a timeframe that encompasses the onset of the mediterranean climate in Europe. More recent middle–late Pleistocene radiations in the Mediterranean Basin and southern Africa have played a large role in Scabiosa diversification.</p>
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<abstract><p>Main conclusions Members of Scabiosa appear to have capitalized on adaptations to montane and/or dry conditions in order to colonize similar habitats in different biogeographical regions. The formation of the East African Rift mountains is potentially of great importance in explaining the southward migration of Scabiosa. The initial diversification of Scabiosa in Europe during the Miocene is not consistent with the initiation of the mediterranean climate, but may instead be associated with increased aridity and the retreat of subtropical lineages during this time. However, the radiation of some of the major subclades within Scabiosa may have been associated with an emerging mediterranean climate. More recent and rapid radiations in both the Mediterranean Basin and southern Africa highlight the probable importance of Pleistocene climate fluctuations in Scabiosa diversification.</p>
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<correspondenceTo> Correspondence and present address: Sara Carlson, University of Neuchâtel, Department of Evolutionary Botany, Rue Emile‐Argand 11, Case Postale 158, 2009 Neuchâtel, Switzerland.
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<titleGroup><title type="main">The historical biogeography of <i>Scabiosa</i>
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<supportingInformation><p><b>Appendix S1</b>
Species sampled, voucher information, and GenBank accessions of DNA sequences analysed in this study.</p>
<p><b>Appendix S2</b>
Description of biogeographical models used in the Lagrange analysis.</p>
<p>As a service to our authors and readers, this journal provides supporting information supplied by the authors. Such materials are peer‐reviewed and may be re‐organized for online delivery, but are not copy‐edited or typeset. Technical support issues arising from supporting information (other than missing files) should be addressed to the authors.</p>
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<abstractGroup><abstract type="main" xml:lang="en"><title type="main">Abstract</title>
<p><b>Aim </b>
To reconstruct the temporal and biogeographical history of Old World disjunctions in <i>Scabiosa</i>
(Dipsacaceae) and the timing of diversification in the Mediterranean Basin, in order to evaluate the importance of biogeographical and climatological history (particularly the onset of a mediterranean climate) in shaping <i>Scabiosa</i>
distributions.</p>
<p><b>Location </b>
Europe and the Mediterranean Basin, southern Africa and eastern Asia.</p>
<p><b>Methods </b>
This study uses maximum‐likelihood and Bayesian phylogenetic analyses of chloroplast DNA (<i>atp</i>
B–<i>rbc</i>
L, <i>trn</i>
L–<i>trn</i>
F, <i>trn</i>
S–<i>trn</i>
G, <i>psb</i>
A–<i>trn</i>
H) and nuclear ribosomal DNA [internal transcribed spacer (ITS) and external transcribed spacer (ETS)] from 24 out of <i>c</i>
. 37 ingroup taxa, <sc>beast</sc>
molecular dating, and the dispersal–extinction–cladogenesis method (L<sc>agrange</sc>
) to reconstruct ancestral geographical ranges and the timing of diversification of the major clades of <i>Scabiosa</i>
.</p>
<p><b>Results </b>
Biogeographical and divergence time reconstructions showed that <i>Scabiosa</i>
originated during the Miocene and diversified in Europe, followed by independent movements into Asia and Africa. Several of the major clades were inferred to have radiated sometime between the late Miocene and early Pleistocene, a timeframe that encompasses the onset of the mediterranean climate in Europe. More recent middle–late Pleistocene radiations in the Mediterranean Basin and southern Africa have played a large role in <i>Scabiosa</i>
diversification.</p>
<p><b>Main conclusions </b>
Members of <i>Scabiosa</i>
appear to have capitalized on adaptations to montane and/or dry conditions in order to colonize similar habitats in different biogeographical regions. The formation of the East African Rift mountains is potentially of great importance in explaining the southward migration of <i>Scabiosa</i>
. The initial diversification of <i>Scabiosa</i>
in Europe during the Miocene is not consistent with the initiation of the mediterranean climate, but may instead be associated with increased aridity and the retreat of subtropical lineages during this time. However, the radiation of some of the major subclades within <i>Scabiosa</i>
may have been associated with an emerging mediterranean climate. More recent and rapid radiations in both the Mediterranean Basin and southern Africa highlight the probable importance of Pleistocene climate fluctuations in <i>Scabiosa</i>
diversification.</p>
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<name type="personal"><namePart type="given">Sara E.</namePart>
<namePart type="family">Carlson</namePart>
<affiliation>Department of Ecology & Evolutionary Biology, Yale University, PO Box 208106, New Haven, CT 06520‐8106, USA</affiliation>
<description>Correspondence and present address: Sara Carlson, University of Neuchâtel, Department of Evolutionary Botany, Rue Emile‐Argand 11, Case Postale 158, 2009 Neuchâtel, Switzerland. E‐mail: </description>
<role><roleTerm type="text">author</roleTerm>
</role>
</name>
<name type="personal"><namePart type="given">H. Peter</namePart>
<namePart type="family">Linder</namePart>
<affiliation>Institute for Systematic Botany, University of Zurich, Zollikerstrasse 107, CH‐8008, Switzerland</affiliation>
<role><roleTerm type="text">author</roleTerm>
</role>
</name>
<name type="personal"><namePart type="given">Michael J.</namePart>
<namePart type="family">Donoghue</namePart>
<affiliation>Department of Ecology & Evolutionary Biology, Yale University, PO Box 208106, New Haven, CT 06520‐8106, USA</affiliation>
<role><roleTerm type="text">author</roleTerm>
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</name>
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<originInfo><publisher>Blackwell Publishing Ltd</publisher>
<place><placeTerm type="text">Oxford, UK</placeTerm>
</place>
<dateIssued encoding="w3cdtf">2012-06</dateIssued>
<copyrightDate encoding="w3cdtf">2012</copyrightDate>
</originInfo>
<language><languageTerm type="code" authority="rfc3066">en</languageTerm>
<languageTerm type="code" authority="iso639-2b">eng</languageTerm>
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<abstract>Aim To reconstruct the temporal and biogeographical history of Old World disjunctions in Scabiosa (Dipsacaceae) and the timing of diversification in the Mediterranean Basin, in order to evaluate the importance of biogeographical and climatological history (particularly the onset of a mediterranean climate) in shaping Scabiosa distributions.</abstract>
<abstract>Location Europe and the Mediterranean Basin, southern Africa and eastern Asia.</abstract>
<abstract>Methods This study uses maximum‐likelihood and Bayesian phylogenetic analyses of chloroplast DNA (atpB–rbcL, trnL–trnF, trnS–trnG, psbA–trnH) and nuclear ribosomal DNA [internal transcribed spacer (ITS) and external transcribed spacer (ETS)] from 24 out of c. 37 ingroup taxa, beast molecular dating, and the dispersal–extinction–cladogenesis method (Lagrange) to reconstruct ancestral geographical ranges and the timing of diversification of the major clades of Scabiosa.</abstract>
<abstract>Results Biogeographical and divergence time reconstructions showed that Scabiosa originated during the Miocene and diversified in Europe, followed by independent movements into Asia and Africa. Several of the major clades were inferred to have radiated sometime between the late Miocene and early Pleistocene, a timeframe that encompasses the onset of the mediterranean climate in Europe. More recent middle–late Pleistocene radiations in the Mediterranean Basin and southern Africa have played a large role in Scabiosa diversification.</abstract>
<abstract>Main conclusions Members of Scabiosa appear to have capitalized on adaptations to montane and/or dry conditions in order to colonize similar habitats in different biogeographical regions. The formation of the East African Rift mountains is potentially of great importance in explaining the southward migration of Scabiosa. The initial diversification of Scabiosa in Europe during the Miocene is not consistent with the initiation of the mediterranean climate, but may instead be associated with increased aridity and the retreat of subtropical lineages during this time. However, the radiation of some of the major subclades within Scabiosa may have been associated with an emerging mediterranean climate. More recent and rapid radiations in both the Mediterranean Basin and southern Africa highlight the probable importance of Pleistocene climate fluctuations in Scabiosa diversification.</abstract>
<subject lang="en"><genre>keywords</genre>
<topic>Biogeographical disjunctions</topic>
<topic>biogeography</topic>
<topic>Dipsacaceae</topic>
<topic>divergence times</topic>
<topic>diversification</topic>
<topic>historical biogeography</topic>
<topic>Mediterranean</topic>
<topic>Miocene</topic>
<topic>Scabiosa</topic>
<topic>southern Africa</topic>
</subject>
<relatedItem type="host"><titleInfo><title>Journal of Biogeography</title>
</titleInfo>
<genre type="journal">journal</genre>
<note type="content"> Appendix S1 Species sampled, voucher information, and GenBank accessions of DNA sequences analysed in this study. Appendix S2 Description of biogeographical models used in the Lagrange analysis. As a service to our authors and readers, this journal provides supporting information supplied by the authors. Such materials are peer‐reviewed and may be re‐organized for online delivery, but are not copy‐edited or typeset. Technical support issues arising from supporting information (other than missing files) should be addressed to the authors. Appendix S1 Species sampled, voucher information, and GenBank accessions of DNA sequences analysed in this study. Appendix S2 Description of biogeographical models used in the Lagrange analysis. As a service to our authors and readers, this journal provides supporting information supplied by the authors. Such materials are peer‐reviewed and may be re‐organized for online delivery, but are not copy‐edited or typeset. Technical support issues arising from supporting information (other than missing files) should be addressed to the authors. Appendix S1 Species sampled, voucher information, and GenBank accessions of DNA sequences analysed in this study. Appendix S2 Description of biogeographical models used in the Lagrange analysis. As a service to our authors and readers, this journal provides supporting information supplied by the authors. Such materials are peer‐reviewed and may be re‐organized for online delivery, but are not copy‐edited or typeset. Technical support issues arising from supporting information (other than missing files) should be addressed to the authors.Supporting Info Item: Supporting info item - </note>
<subject><genre>article-category</genre>
<topic>ORIGINAL ARTICLE</topic>
</subject>
<identifier type="ISSN">0305-0270</identifier>
<identifier type="eISSN">1365-2699</identifier>
<identifier type="DOI">10.1111/(ISSN)1365-2699</identifier>
<identifier type="PublisherID">JBI</identifier>
<part><date>2012</date>
<detail type="volume"><caption>vol.</caption>
<number>39</number>
</detail>
<detail type="issue"><caption>no.</caption>
<number>6</number>
</detail>
<extent unit="pages"><start>1086</start>
<end>1100</end>
<total>15</total>
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<identifier type="DOI">10.1111/j.1365-2699.2011.02669.x</identifier>
<identifier type="ArticleID">JBI2669</identifier>
<accessCondition type="use and reproduction" contentType="copyright">© 2012 Blackwell Publishing Ltd</accessCondition>
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