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<record><TEI><teiHeader><fileDesc><titleStmt><title xml:lang="en">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><nlm:aff id="af1"><institution>UCB Lyon 1 et UMR 5125</institution>,<addr-line>Paléobotanique, 7 rue Dubois, F-69622 Villeurbanne</addr-line>,<country>France</country></nlm:aff></affiliation></author><author><name sortKey="Gomez, B" sort="Gomez, B" uniqKey="Gomez B" first="B." last="Gomez">B. Gomez</name><affiliation><nlm:aff id="af2"><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></nlm:aff></affiliation></author><author><name sortKey="Thevenard, F" sort="Thevenard, F" uniqKey="Thevenard F" first="F." last="Thevenard">F. Thevenard</name><affiliation><nlm:aff id="af1"><institution>UCB Lyon 1 et UMR 5125</institution>,<addr-line>Paléobotanique, 7 rue Dubois, F-69622 Villeurbanne</addr-line>,<country>France</country></nlm:aff></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">PMC</idno><idno type="pmid">17679689</idno><idno type="pmc">2533611</idno><idno type="url">http://www.ncbi.nlm.nih.gov/pmc/articles/PMC2533611</idno><idno type="RBID">PMC:2533611</idno><idno type="doi">10.1093/aob/mcm160</idno><date when="2007">2007</date><idno type="wicri:Area/Pmc/Corpus">000136</idno><idno type="wicri:explorRef" wicri:stream="Pmc" wicri:step="Corpus" wicri:corpus="PMC">000136</idno></publicationStmt><sourceDesc><biblStruct><analytic><title xml:lang="en" level="a" type="main">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><nlm:aff id="af1"><institution>UCB Lyon 1 et UMR 5125</institution>,<addr-line>Paléobotanique, 7 rue Dubois, F-69622 Villeurbanne</addr-line>,<country>France</country></nlm:aff></affiliation></author><author><name sortKey="Gomez, B" sort="Gomez, B" uniqKey="Gomez B" first="B." last="Gomez">B. Gomez</name><affiliation><nlm:aff id="af2"><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></nlm:aff></affiliation></author><author><name sortKey="Thevenard, F" sort="Thevenard, F" uniqKey="Thevenard F" first="F." last="Thevenard">F. Thevenard</name><affiliation><nlm:aff id="af1"><institution>UCB Lyon 1 et UMR 5125</institution>,<addr-line>Paléobotanique, 7 rue Dubois, F-69622 Villeurbanne</addr-line>,<country>France</country></nlm:aff></affiliation></author></analytic><series><title level="j">Annals of Botany</title><idno type="ISSN">0305-7364</idno><idno type="eISSN">1095-8290</idno><imprint><date when="2007">2007</date></imprint></series></biblStruct></sourceDesc></fileDesc><profileDesc><textClass></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en"><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></div></front></TEI><pmc article-type="research-article"><pmc-comment>The publisher of this article does not allow downloading of the full text in XML form.</pmc-comment>
<front><journal-meta><journal-id journal-id-type="nlm-ta">Ann Bot</journal-id><journal-id journal-id-type="publisher-id">annbot</journal-id><journal-id journal-id-type="hwp">annbot</journal-id><journal-title-group><journal-title>Annals of Botany</journal-title></journal-title-group><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="pmid">17679689</article-id><article-id pub-id-type="pmc">2533611</article-id><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><permissions><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></permissions><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></pmc></record>Pour manipuler ce document sous Unix (Dilib)
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