Early Cretaceous Angiosperm Invasion of Western Europe and Major Environmental Changes
Identifieur interne : 000E83 ( Istex/Corpus ); précédent : 000E82; suivant : 000E84Early Cretaceous Angiosperm Invasion of Western Europe and Major Environmental Changes
Auteurs : C. Coiffard ; B. Gomez ; F. ThevenardSource :
- Annals of Botany [ 0305-7364 ] ; 2007-09.
Abstract
Background and Aims At the beginning of the Late Cretaceous, angiosperms already inhabited all the environments and overtopped previously gymnosperm-dominated floras, especially in disturbed freshwater-related environments. The aim of this paper is to define what fossil plant ecology occurred during the early Cretaceous in order to follow the early spread of angiosperm taxa. Methods Floristic lists and localities from the Barremian to the Albian of Europe are analysed with the Wagner's Parsimony Method. Key results The Wagner's Parsimony Method indicates that (a) during the Barremian, matoniaceous ferns formed a savannah-like vegetation, while angiosperms composed freshwater aquatic vegetation; (b) during the Late Aptian humid phase, conifers increased, while matoniaceous ferns decreased, reflecting the closure of the vegetation; and (c) from the Albian, warmer and drier conditions induced the recovery of the matoniaceous ferns, while core angiosperms first developed in floodplains. Conclusions During the late Early Cretaceous (BarremianAlbian), angiosperms showed a stepwise widening of their ecological range, being recorded first during the Barremian as aquatic plant mega-remains and at the Cenomanian onwards occurred in all the environments.
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DOI: 10.1093/aob/mcm160
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<record><TEI wicri:istexFullTextTei="biblStruct"><teiHeader><fileDesc><titleStmt><title>Early Cretaceous Angiosperm Invasion of Western Europe and Major Environmental Changes</title><author><name sortKey="Coiffard, C" sort="Coiffard, C" uniqKey="Coiffard C" first="C." last="Coiffard">C. Coiffard</name><affiliation><mods:affiliation>UCB Lyon 1 et UMR 5125, Palobotanique, 7 rue Dubois, F-69622 Villeurbanne, France</mods:affiliation></affiliation></author><author><name sortKey="Gomez, B" sort="Gomez, B" uniqKey="Gomez B" first="B." last="Gomez">B. Gomez</name><affiliation><mods:affiliation>UMR 6118 du CNRS Gosciences, Universit Rennes 1, Campus de Beaulieu, avenue du Gnral Leclerc, F-35042 Rennes, France</mods:affiliation></affiliation><affiliation><mods:affiliation>E-mail: bernard.gomez@univ-rennes1.fr</mods:affiliation></affiliation></author><author><name sortKey="Thevenard, F" sort="Thevenard, F" uniqKey="Thevenard F" first="F." last="Thevenard">F. Thevenard</name><affiliation><mods:affiliation>UCB Lyon 1 et UMR 5125, Palobotanique, 7 rue Dubois, F-69622 Villeurbanne, France</mods:affiliation></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:97AF08DB3918A6A53310B7257D0B3D2B57B0BEE8</idno><date when="2007" year="2007">2007</date><idno type="doi">10.1093/aob/mcm160</idno><idno type="url">https://api.istex.fr/document/97AF08DB3918A6A53310B7257D0B3D2B57B0BEE8/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">000E83</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">000E83</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a">Early Cretaceous Angiosperm Invasion of Western Europe and Major Environmental Changes</title><author><name sortKey="Coiffard, C" sort="Coiffard, C" uniqKey="Coiffard C" first="C." last="Coiffard">C. Coiffard</name><affiliation><mods:affiliation>UCB Lyon 1 et UMR 5125, Palobotanique, 7 rue Dubois, F-69622 Villeurbanne, France</mods:affiliation></affiliation></author><author><name sortKey="Gomez, B" sort="Gomez, B" uniqKey="Gomez B" first="B." last="Gomez">B. Gomez</name><affiliation><mods:affiliation>UMR 6118 du CNRS Gosciences, Universit Rennes 1, Campus de Beaulieu, avenue du Gnral Leclerc, F-35042 Rennes, France</mods:affiliation></affiliation><affiliation><mods:affiliation>E-mail: bernard.gomez@univ-rennes1.fr</mods:affiliation></affiliation></author><author><name sortKey="Thevenard, F" sort="Thevenard, F" uniqKey="Thevenard F" first="F." last="Thevenard">F. Thevenard</name><affiliation><mods:affiliation>UCB Lyon 1 et UMR 5125, Palobotanique, 7 rue Dubois, F-69622 Villeurbanne, France</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Annals of Botany</title><idno type="ISSN">0305-7364</idno><idno type="eISSN">1095-8290</idno><imprint><publisher>Oxford University Press</publisher><date type="published" when="2007-09">2007-09</date><biblScope unit="volume">100</biblScope><biblScope unit="issue">3</biblScope><biblScope unit="page" from="545">545</biblScope><biblScope unit="page" to="553">553</biblScope></imprint><idno type="ISSN">0305-7364</idno></series><idno type="istex">97AF08DB3918A6A53310B7257D0B3D2B57B0BEE8</idno><idno type="DOI">10.1093/aob/mcm160</idno><idno type="ArticleID">mcm160</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0305-7364</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass></profileDesc></teiHeader><front><div type="abstract">Background and Aims At the beginning of the Late Cretaceous, angiosperms already inhabited all the environments and overtopped previously gymnosperm-dominated floras, especially in disturbed freshwater-related environments. The aim of this paper is to define what fossil plant ecology occurred during the early Cretaceous in order to follow the early spread of angiosperm taxa. Methods Floristic lists and localities from the Barremian to the Albian of Europe are analysed with the Wagner's Parsimony Method. Key results The Wagner's Parsimony Method indicates that (a) during the Barremian, matoniaceous ferns formed a savannah-like vegetation, while angiosperms composed freshwater aquatic vegetation; (b) during the Late Aptian humid phase, conifers increased, while matoniaceous ferns decreased, reflecting the closure of the vegetation; and (c) from the Albian, warmer and drier conditions induced the recovery of the matoniaceous ferns, while core angiosperms first developed in floodplains. Conclusions During the late Early Cretaceous (BarremianAlbian), angiosperms showed a stepwise widening of their ecological range, being recorded first during the Barremian as aquatic plant mega-remains and at the Cenomanian onwards occurred in all the environments.</div></front></TEI><istex><corpusName>oup</corpusName><author><json:item><name>C. Coiffard</name><affiliations><json:string>UCB Lyon 1 et UMR 5125, Palobotanique, 7 rue Dubois, F-69622 Villeurbanne, France</json:string></affiliations></json:item><json:item><name>B. Gomez</name><affiliations><json:string>UMR 6118 du CNRS Gosciences, Universit Rennes 1, Campus de Beaulieu, avenue du Gnral Leclerc, F-35042 Rennes, France</json:string><json:string>E-mail: bernard.gomez@univ-rennes1.fr</json:string></affiliations></json:item><json:item><name>F. Thevenard</name><affiliations><json:string>UCB Lyon 1 et UMR 5125, Palobotanique, 7 rue Dubois, F-69622 Villeurbanne, France</json:string></affiliations></json:item></author><subject><json:item><value>Wagner's Parsimony Method</value></json:item><json:item><value>angiosperms</value></json:item><json:item><value>conifers</value></json:item><json:item><value>gymnosperms</value></json:item><json:item><value>ecology</value></json:item><json:item><value>environment</value></json:item><json:item><value>upper Lower Cretaceous</value></json:item><json:item><value>Europe</value></json:item></subject><articleId><json:string>mcm160</json:string></articleId><language><json:string>unknown</json:string></language><originalGenre><json:string>research-article</json:string></originalGenre><abstract>Background and Aims At the beginning of the Late Cretaceous, angiosperms already inhabited all the environments and overtopped previously gymnosperm-dominated floras, especially in disturbed freshwater-related environments. The aim of this paper is to define what fossil plant ecology occurred during the early Cretaceous in order to follow the early spread of angiosperm taxa. Methods Floristic lists and localities from the Barremian to the Albian of Europe are analysed with the Wagner's Parsimony Method. Key results The Wagner's Parsimony Method indicates that (a) during the Barremian, matoniaceous ferns formed a savannah-like vegetation, while angiosperms composed freshwater aquatic vegetation; (b) during the Late Aptian humid phase, conifers increased, while matoniaceous ferns decreased, reflecting the closure of the vegetation; and (c) from the Albian, warmer and drier conditions induced the recovery of the matoniaceous ferns, while core angiosperms first developed in floodplains. Conclusions During the late Early Cretaceous (BarremianAlbian), angiosperms showed a stepwise widening of their ecological range, being recorded first during the Barremian as aquatic plant mega-remains and at the Cenomanian onwards occurred in all the environments.</abstract><qualityIndicators><score>9.04</score><pdfVersion>1.2</pdfVersion><pdfPageSize>612.283 x 790.866 pts</pdfPageSize><refBibsNative>false</refBibsNative><keywordCount>8</keywordCount><abstractCharCount>1263</abstractCharCount><pdfWordCount>4940</pdfWordCount><pdfCharCount>40335</pdfCharCount><pdfPageCount>9</pdfPageCount><abstractWordCount>175</abstractWordCount></qualityIndicators><title>Early Cretaceous Angiosperm Invasion of Western Europe and Major Environmental Changes</title><refBibs><json:item><host><author></author><title>the Ministerio de Educación y Ciencia of the Spanish government and project 2005SGR-00890 of the Catalan government</title></host></json:item><json:item><author><json:item><name>C Alvárez-Ramis</name></json:item><json:item><name>P De Lorenzo</name></json:item></author><host><volume>14</volume><pages><last>332</last><first>327</first></pages><author></author><title>Acta Geológica Hispánica</title><publicationDate>1982</publicationDate></host><title>Estudio de la flora cretácica de Pola de Siero</title><publicationDate>1982</publicationDate></json:item><json:item><author><json:item><name>C Alvárez-Ramis</name></json:item><json:item><name>F Meléndez</name></json:item></author><host><volume>27</volume><pages><last>253</last><first>247</first></pages><author></author><title>Estudios geológicos</title><publicationDate>1971</publicationDate></host><title>Un nuevo yacimiento de flora cretácica en el Albiense de la Cordillera Ibérica. 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000000?010?000000111000000111111111?</title><publicationDate>2004</publicationDate></json:item></refBibs><genre><json:string>research-article</json:string></genre><host><volume>100</volume><publisherId><json:string>annbot</json:string></publisherId><pages><last>553</last><first>545</first></pages><issn><json:string>0305-7364</json:string></issn><issue>3</issue><genre><json:string>journal</json:string></genre><language><json:string>unknown</json:string></language><eissn><json:string>1095-8290</json:string></eissn><title>Annals of Botany</title></host><categories><wos><json:string>science</json:string><json:string>plant sciences</json:string></wos><scienceMetrix><json:string>natural sciences</json:string><json:string>biology</json:string><json:string>plant biology & botany</json:string></scienceMetrix></categories><publicationDate>2007</publicationDate><copyrightDate>2007</copyrightDate><doi><json:string>10.1093/aob/mcm160</json:string></doi><id>97AF08DB3918A6A53310B7257D0B3D2B57B0BEE8</id><score>1</score><fulltext><json:item><extension>pdf</extension><original>true</original><mimetype>application/pdf</mimetype><uri>https://api.istex.fr/document/97AF08DB3918A6A53310B7257D0B3D2B57B0BEE8/fulltext/pdf</uri></json:item><json:item><extension>zip</extension><original>false</original><mimetype>application/zip</mimetype><uri>https://api.istex.fr/document/97AF08DB3918A6A53310B7257D0B3D2B57B0BEE8/fulltext/zip</uri></json:item><istex:fulltextTEI uri="https://api.istex.fr/document/97AF08DB3918A6A53310B7257D0B3D2B57B0BEE8/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a">Early Cretaceous Angiosperm Invasion of Western Europe and Major Environmental Changes</title><respStmt><resp>Références bibliographiques récupérées via GROBID</resp><name resp="ISTEX-API">ISTEX-API (INIST-CNRS)</name></respStmt></titleStmt><publicationStmt><authority>ISTEX</authority><publisher>Oxford University Press</publisher><availability><p>The Author 2007. Published by Oxford University Press on behalf of the Annals of Botany Company. All rights reserved. For Permissions, please email: journals.permissionsoxfordjournals.org</p></availability><date>2007-08-06</date></publicationStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a">Early Cretaceous Angiosperm Invasion of Western Europe and Major Environmental Changes</title><author xml:id="author-1"><persName><forename type="first">C.</forename><surname>Coiffard</surname></persName><affiliation>UCB Lyon 1 et UMR 5125, Palobotanique, 7 rue Dubois, F-69622 Villeurbanne, France</affiliation></author><author xml:id="author-2"><persName><forename type="first">B.</forename><surname>Gomez</surname></persName><email>bernard.gomez@univ-rennes1.fr</email><affiliation>UMR 6118 du CNRS Gosciences, Universit Rennes 1, Campus de Beaulieu, avenue du Gnral Leclerc, F-35042 Rennes, France</affiliation></author><author xml:id="author-3"><persName><forename type="first">F.</forename><surname>Thevenard</surname></persName><affiliation>UCB Lyon 1 et UMR 5125, Palobotanique, 7 rue Dubois, F-69622 Villeurbanne, France</affiliation></author></analytic><monogr><title level="j">Annals of Botany</title><idno type="pISSN">0305-7364</idno><idno type="eISSN">1095-8290</idno><imprint><publisher>Oxford University Press</publisher><date type="published" when="2007-09"></date><biblScope unit="volume">100</biblScope><biblScope unit="issue">3</biblScope><biblScope unit="page" from="545">545</biblScope><biblScope unit="page" to="553">553</biblScope></imprint></monogr><idno type="istex">97AF08DB3918A6A53310B7257D0B3D2B57B0BEE8</idno><idno type="DOI">10.1093/aob/mcm160</idno><idno type="ArticleID">mcm160</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>2007-08-06</date></creation><abstract><p>Background and Aims At the beginning of the Late Cretaceous, angiosperms already inhabited all the environments and overtopped previously gymnosperm-dominated floras, especially in disturbed freshwater-related environments. The aim of this paper is to define what fossil plant ecology occurred during the early Cretaceous in order to follow the early spread of angiosperm taxa. Methods Floristic lists and localities from the Barremian to the Albian of Europe are analysed with the Wagner's Parsimony Method. Key results The Wagner's Parsimony Method indicates that (a) during the Barremian, matoniaceous ferns formed a savannah-like vegetation, while angiosperms composed freshwater aquatic vegetation; (b) during the Late Aptian humid phase, conifers increased, while matoniaceous ferns decreased, reflecting the closure of the vegetation; and (c) from the Albian, warmer and drier conditions induced the recovery of the matoniaceous ferns, while core angiosperms first developed in floodplains. Conclusions During the late Early Cretaceous (BarremianAlbian), angiosperms showed a stepwise widening of their ecological range, being recorded first during the Barremian as aquatic plant mega-remains and at the Cenomanian onwards occurred in all the environments.</p></abstract><textClass><keywords scheme="keyword"><list><head>Key words</head><item><term>Wagner's Parsimony Method</term></item><item><term>angiosperms</term></item><item><term>conifers</term></item><item><term>gymnosperms</term></item><item><term>ecology</term></item><item><term>environment</term></item><item><term>upper Lower Cretaceous</term></item><item><term>Europe</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="2007-08-06">Created</change><change when="2007-09">Published</change><change xml:id="refBibs-istex" who="#ISTEX-API" when="2016-12-22">References added</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/97AF08DB3918A6A53310B7257D0B3D2B57B0BEE8/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="corpus oup" wicri:toSee="no header"><istex:xmlDeclaration>version="1.0" encoding="utf-8"</istex:xmlDeclaration><istex:docType PUBLIC="-//NLM//DTD Journal Publishing DTD v2.3 20070202//EN" URI="journalpublishing.dtd" name="istex:docType"></istex:docType><istex:document><article article-type="research-article"><front><journal-meta><journal-id journal-id-type="publisher-id">annbot</journal-id><journal-id journal-id-type="hwp">annbot</journal-id><journal-title>Annals of Botany</journal-title><issn pub-type="ppub">0305-7364</issn><issn pub-type="epub">1095-8290</issn><publisher><publisher-name>Oxford University Press</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.1093/aob/mcm160</article-id><article-id pub-id-type="publisher-id">mcm160</article-id><article-categories><subj-group subj-group-type="heading"><subject>ORIGINAL ARTICLES</subject></subj-group></article-categories><title-group><article-title>Early Cretaceous Angiosperm Invasion of Western Europe and Major Environmental Changes</article-title><alt-title alt-title-type="left-running"><italic>Coiffard <italic>et al.</italic> — Mid-Cretaceous Plant Ecology of Europe</italic></alt-title><alt-title alt-title-type="right-running"><italic>Coiffard <italic>et al.</italic> — Mid-Cretaceous Plant Ecology of Europe</italic></alt-title></title-group><contrib-group><contrib contrib-type="author"><name><surname>Coiffard</surname><given-names>C.</given-names></name><xref ref-type="aff" rid="af1">1</xref></contrib><contrib contrib-type="author"><name><surname>Gomez</surname><given-names>B.</given-names></name><xref ref-type="aff" rid="af2">2</xref><xref ref-type="corresp" rid="cor1">*</xref></contrib><contrib contrib-type="author"><name><surname>Thevenard</surname><given-names>F.</given-names></name><xref ref-type="aff" rid="af1">1</xref></contrib></contrib-group><aff id="af1"><label>1</label><institution>UCB Lyon 1 et UMR 5125</institution>, <addr-line>Paléobotanique, 7 rue Dubois, F-69622 Villeurbanne</addr-line>, <country>France</country></aff><aff id="af2"><label>2</label><institution>UMR 6118 du CNRS Géosciences, Université Rennes 1</institution>, <addr-line>Campus de Beaulieu, avenue du Général Leclerc, F-35042 Rennes</addr-line>, <country>France</country></aff><author-notes><corresp id="cor1"><label>*</label>For correspondence. E-mail <email>bernard.gomez@univ-rennes1.fr</email></corresp></author-notes><pub-date pub-type="ppub"><month>9</month><year>2007</year></pub-date><pub-date pub-type="epub"><day>6</day><month>8</month><year>2007</year></pub-date><volume>100</volume><issue>3</issue><fpage>545</fpage><lpage>553</lpage><history><date date-type="received"><day>8</day><month>2</month><year>2007</year></date><date date-type="rev-recd"><day>26</day><month>3</month><year>2007</year></date><date date-type="accepted"><day>16</day><month>5</month><year>2007</year></date></history><copyright-statement>© The Author 2007. Published by Oxford University Press on behalf of the Annals of Botany Company. All rights reserved. For Permissions, please email: journals.permissions@oxfordjournals.org</copyright-statement><copyright-year>2007</copyright-year><abstract><sec><title>Background and Aims</title><p>At the beginning of the Late Cretaceous, angiosperms already inhabited all the environments and overtopped previously gymnosperm-dominated floras, especially in disturbed freshwater-related environments. The aim of this paper is to define what fossil plant ecology occurred during the early Cretaceous in order to follow the early spread of angiosperm taxa.</p></sec><sec><title>Methods</title><p>Floristic lists and localities from the Barremian to the Albian of Europe are analysed with the Wagner's Parsimony Method.</p></sec><sec><title>Key results</title><p>The Wagner's Parsimony Method indicates that (<italic>a</italic>) during the Barremian, matoniaceous ferns formed a savannah-like vegetation, while angiosperms composed freshwater aquatic vegetation; (<italic>b</italic>) during the Late Aptian humid phase, conifers increased, while matoniaceous ferns decreased, reflecting the closure of the vegetation; and (<italic>c</italic>) from the Albian, warmer and drier conditions induced the recovery of the matoniaceous ferns, while core angiosperms first developed in floodplains.</p></sec><sec><title>Conclusions</title><p>During the late Early Cretaceous (Barremian–Albian), angiosperms showed a stepwise widening of their ecological range, being recorded first during the Barremian as aquatic plant mega-remains and at the Cenomanian onwards occurred in all the environments.</p></sec></abstract><kwd-group><title>Key words</title><kwd>Wagner's Parsimony Method</kwd><kwd>angiosperms</kwd><kwd>conifers</kwd><kwd>gymnosperms</kwd><kwd>ecology</kwd><kwd>environment</kwd><kwd>upper Lower Cretaceous</kwd><kwd>Europe</kwd></kwd-group></article-meta></front></article></istex:document></istex:metadataXml><mods version="3.6"><titleInfo><title>Early Cretaceous Angiosperm Invasion of Western Europe and Major Environmental Changes</title></titleInfo><titleInfo type="alternative" contentType="CDATA"><title>Early Cretaceous Angiosperm Invasion of Western Europe and Major Environmental Changes</title></titleInfo><name type="personal"><namePart type="given">C.</namePart><namePart type="family">Coiffard</namePart><affiliation>UCB Lyon 1 et UMR 5125, Palobotanique, 7 rue Dubois, F-69622 Villeurbanne, France</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">B.</namePart><namePart type="family">Gomez</namePart><affiliation>UMR 6118 du CNRS Gosciences, Universit Rennes 1, Campus de Beaulieu, avenue du Gnral Leclerc, F-35042 Rennes, France</affiliation><affiliation>E-mail: bernard.gomez@univ-rennes1.fr</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">F.</namePart><namePart type="family">Thevenard</namePart><affiliation>UCB Lyon 1 et UMR 5125, Palobotanique, 7 rue Dubois, F-69622 Villeurbanne, France</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="research-article" displayLabel="research-article"></genre><originInfo><publisher>Oxford University Press</publisher><dateIssued encoding="w3cdtf">2007-09</dateIssued><dateCreated encoding="w3cdtf">2007-08-06</dateCreated><copyrightDate encoding="w3cdtf">2007</copyrightDate></originInfo><physicalDescription><internetMediaType>text/html</internetMediaType></physicalDescription><abstract>Background and Aims At the beginning of the Late Cretaceous, angiosperms already inhabited all the environments and overtopped previously gymnosperm-dominated floras, especially in disturbed freshwater-related environments. The aim of this paper is to define what fossil plant ecology occurred during the early Cretaceous in order to follow the early spread of angiosperm taxa. Methods Floristic lists and localities from the Barremian to the Albian of Europe are analysed with the Wagner's Parsimony Method. Key results The Wagner's Parsimony Method indicates that (a) during the Barremian, matoniaceous ferns formed a savannah-like vegetation, while angiosperms composed freshwater aquatic vegetation; (b) during the Late Aptian humid phase, conifers increased, while matoniaceous ferns decreased, reflecting the closure of the vegetation; and (c) from the Albian, warmer and drier conditions induced the recovery of the matoniaceous ferns, while core angiosperms first developed in floodplains. Conclusions During the late Early Cretaceous (BarremianAlbian), angiosperms showed a stepwise widening of their ecological range, being recorded first during the Barremian as aquatic plant mega-remains and at the Cenomanian onwards occurred in all the environments.</abstract><subject><genre>Key words</genre><topic>Wagner's Parsimony Method</topic><topic>angiosperms</topic><topic>conifers</topic><topic>gymnosperms</topic><topic>ecology</topic><topic>environment</topic><topic>upper Lower Cretaceous</topic><topic>Europe</topic></subject><relatedItem type="host"><titleInfo><title>Annals of Botany</title></titleInfo><genre type="journal">journal</genre><identifier type="ISSN">0305-7364</identifier><identifier type="eISSN">1095-8290</identifier><identifier type="PublisherID">annbot</identifier><identifier type="PublisherID-hwp">annbot</identifier><part><date>2007</date><detail type="volume"><caption>vol.</caption><number>100</number></detail><detail type="issue"><caption>no.</caption><number>3</number></detail><extent unit="pages"><start>545</start><end>553</end></extent></part></relatedItem><identifier type="istex">97AF08DB3918A6A53310B7257D0B3D2B57B0BEE8</identifier><identifier type="DOI">10.1093/aob/mcm160</identifier><identifier type="ArticleID">mcm160</identifier><accessCondition type="use and reproduction" contentType="copyright">The Author 2007. Published by Oxford University Press on behalf of the Annals of Botany Company. All rights reserved. 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