Development and regional differentiation of the European vegetation during the Tertiary
Identifieur interne : 000966 ( Istex/Corpus ); précédent : 000965; suivant : 000967Development and regional differentiation of the European vegetation during the Tertiary
Auteurs : Dieter H. MaiSource :
- Plant Systematics and Evolution [ 0378-2697 ] ; 1989-03-01.
Abstract
Abstract: The Tertiary vegetation of Europe evolved from paratropical to warm-temperate and temperate forms in response to a progressive, non-linear, climatic cooling. Its vegetational forms are composed mainly of two separate ecological units: the evergreen, laurophyll “paleotropical geoflora” and the deciduous, broad-leaved “Arctotertiary geoflora”. The development of the Tertiary climate and its interaction with the vegetation are convincingly indicated by the geoflora's migration; the changes in its composition; and the development of the Tertiary forest, swamp, and aquatic plant communities. The “paleotropical geoflora” is characterized in the upper Cretaceous to the upper Miocene by paratropical rain forest, subtropical rain and laurel forests, temperate laurel forests and edaphically-mediated formation of laurel-conifer forests. The “Arctotertiary geoflora” advanced into Europe in waves since the Paleocene and formed the basis for the Tertiary mixed mesophytic forests. These can be divided into warm-temperate rain forests, oak-hornbeamchestnut or mixed beech-oak-hornbeam forests, and edaphic formations such as bottomland and swamp forests. Beginning in the lower Cretaceous, the hydrophytic vegetation developed independently of the forest vegetation and formed very diverse herbaceous fresh water, swamp, salt water, and coastal formations. Considerable differences in composition allow to separate floral regions and provinces in Eurosiberia. Instead of three ill-defined floral regions in the Paleocene, there are four well-defined floral regions in the Pliocene. A Mediterranean region cannot be recognized, although Mediterranean (eumesogeic) floral elements appear in the Eocene/Oligocene and thereafter. The Mediterranean sclerophyll forests probably arose after the destruction of the laurophyll forests during the Pleistocene.
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DOI: 10.1007/BF00936911
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<record><TEI wicri:istexFullTextTei="biblStruct"><teiHeader><fileDesc><titleStmt><title xml:lang="en">Development and regional differentiation of the European vegetation during the Tertiary</title><author><name sortKey="Mai, Dieter H" sort="Mai, Dieter H" uniqKey="Mai D" first="Dieter H." last="Mai">Dieter H. Mai</name><affiliation><mods:affiliation>Bereich Botanik und Arboretum des Museums für Naturkunde, Humboldt-Universität, Späthstrasse 80/81, DDR-1195, Berlin, German Democratic Republic</mods:affiliation></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:7972426BC6D1FCFA8E53DB451DE42B5CBA482B3F</idno><date when="1989" year="1989">1989</date><idno type="doi">10.1007/BF00936911</idno><idno type="url">https://api.istex.fr/document/7972426BC6D1FCFA8E53DB451DE42B5CBA482B3F/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">000966</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">000966</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a" type="main" xml:lang="en">Development and regional differentiation of the European vegetation during the Tertiary</title><author><name sortKey="Mai, Dieter H" sort="Mai, Dieter H" uniqKey="Mai D" first="Dieter H." last="Mai">Dieter H. Mai</name><affiliation><mods:affiliation>Bereich Botanik und Arboretum des Museums für Naturkunde, Humboldt-Universität, Späthstrasse 80/81, DDR-1195, Berlin, German Democratic Republic</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Plant Systematics and Evolution</title><title level="j" type="sub">Entwicklungsgeschichte und Systematik der Pflanzen</title><title level="j" type="abbrev">Pl Syst Evol</title><idno type="ISSN">0378-2697</idno><idno type="eISSN">1615-6110</idno><imprint><publisher>Springer-Verlag</publisher><pubPlace>Vienna</pubPlace><date type="published" when="1989-03-01">1989-03-01</date><biblScope unit="volume">162</biblScope><biblScope unit="issue">1-4</biblScope><biblScope unit="page" from="79">79</biblScope><biblScope unit="page" to="91">91</biblScope></imprint><idno type="ISSN">0378-2697</idno></series><idno type="istex">7972426BC6D1FCFA8E53DB451DE42B5CBA482B3F</idno><idno type="DOI">10.1007/BF00936911</idno><idno type="ArticleID">BF00936911</idno><idno type="ArticleID">Art4</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0378-2697</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Abstract: The Tertiary vegetation of Europe evolved from paratropical to warm-temperate and temperate forms in response to a progressive, non-linear, climatic cooling. Its vegetational forms are composed mainly of two separate ecological units: the evergreen, laurophyll “paleotropical geoflora” and the deciduous, broad-leaved “Arctotertiary geoflora”. The development of the Tertiary climate and its interaction with the vegetation are convincingly indicated by the geoflora's migration; the changes in its composition; and the development of the Tertiary forest, swamp, and aquatic plant communities. The “paleotropical geoflora” is characterized in the upper Cretaceous to the upper Miocene by paratropical rain forest, subtropical rain and laurel forests, temperate laurel forests and edaphically-mediated formation of laurel-conifer forests. The “Arctotertiary geoflora” advanced into Europe in waves since the Paleocene and formed the basis for the Tertiary mixed mesophytic forests. These can be divided into warm-temperate rain forests, oak-hornbeamchestnut or mixed beech-oak-hornbeam forests, and edaphic formations such as bottomland and swamp forests. Beginning in the lower Cretaceous, the hydrophytic vegetation developed independently of the forest vegetation and formed very diverse herbaceous fresh water, swamp, salt water, and coastal formations. Considerable differences in composition allow to separate floral regions and provinces in Eurosiberia. Instead of three ill-defined floral regions in the Paleocene, there are four well-defined floral regions in the Pliocene. A Mediterranean region cannot be recognized, although Mediterranean (eumesogeic) floral elements appear in the Eocene/Oligocene and thereafter. The Mediterranean sclerophyll forests probably arose after the destruction of the laurophyll forests during the Pleistocene.</div></front></TEI><istex><corpusName>springer</corpusName><author><json:item><name>Dieter H. Mai</name><affiliations><json:string>Bereich Botanik und Arboretum des Museums für Naturkunde, Humboldt-Universität, Späthstrasse 80/81, DDR-1195, Berlin, German Democratic Republic</json:string></affiliations></json:item></author><articleId><json:string>BF00936911</json:string><json:string>Art4</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>OriginalPaper</json:string></originalGenre><abstract>Abstract: The Tertiary vegetation of Europe evolved from paratropical to warm-temperate and temperate forms in response to a progressive, non-linear, climatic cooling. Its vegetational forms are composed mainly of two separate ecological units: the evergreen, laurophyll “paleotropical geoflora” and the deciduous, broad-leaved “Arctotertiary geoflora”. The development of the Tertiary climate and its interaction with the vegetation are convincingly indicated by the geoflora's migration; the changes in its composition; and the development of the Tertiary forest, swamp, and aquatic plant communities. The “paleotropical geoflora” is characterized in the upper Cretaceous to the upper Miocene by paratropical rain forest, subtropical rain and laurel forests, temperate laurel forests and edaphically-mediated formation of laurel-conifer forests. The “Arctotertiary geoflora” advanced into Europe in waves since the Paleocene and formed the basis for the Tertiary mixed mesophytic forests. These can be divided into warm-temperate rain forests, oak-hornbeamchestnut or mixed beech-oak-hornbeam forests, and edaphic formations such as bottomland and swamp forests. Beginning in the lower Cretaceous, the hydrophytic vegetation developed independently of the forest vegetation and formed very diverse herbaceous fresh water, swamp, salt water, and coastal formations. Considerable differences in composition allow to separate floral regions and provinces in Eurosiberia. Instead of three ill-defined floral regions in the Paleocene, there are four well-defined floral regions in the Pliocene. A Mediterranean region cannot be recognized, although Mediterranean (eumesogeic) floral elements appear in the Eocene/Oligocene and thereafter. The Mediterranean sclerophyll forests probably arose after the destruction of the laurophyll forests during the Pleistocene.</abstract><qualityIndicators><score>7.94</score><pdfVersion>1.3</pdfVersion><pdfPageSize>576 x 771 pts</pdfPageSize><refBibsNative>false</refBibsNative><keywordCount>0</keywordCount><abstractCharCount>1860</abstractCharCount><pdfWordCount>5610</pdfWordCount><pdfCharCount>32611</pdfCharCount><pdfPageCount>13</pdfPageCount><abstractWordCount>245</abstractWordCount></qualityIndicators><title>Development and regional differentiation of the European vegetation during the Tertiary</title><refBibs><json:item><author><json:item><name>Andreanszky </name></json:item><json:item><name>G </name></json:item></author><host><volume>5</volume><pages><last>151</last><first>5</first></pages><issue>5</issue><author></author><title>Eger. -Stud. Biol. Hung</title><publicationDate>1959</publicationDate></host><title>Die Flora der sarmatischen Stufe in Ungarn. -Budapest: Akad. 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Oregon</title><publicationDate>1954</publicationDate></json:item></refBibs><genre><json:string>research-article</json:string></genre><host><volume>162</volume><pages><last>91</last><first>79</first></pages><issn><json:string>0378-2697</json:string></issn><issue>1-4</issue><subject><json:item><value>Plant Ecology</value></json:item><json:item><value>Plant Sciences</value></json:item><json:item><value>Plant Anatomy/Development</value></json:item><json:item><value>Plant Systematics/Taxonomy/Biogeography</value></json:item></subject><journalId><json:string>606</json:string></journalId><genre><json:string>journal</json:string></genre><language><json:string>unknown</json:string></language><eissn><json:string>1615-6110</json:string></eissn><title>Plant Systematics and Evolution</title><publicationDate>1989</publicationDate><copyrightDate>1989</copyrightDate></host><categories><wos><json:string>science</json:string><json:string>plant sciences</json:string><json:string>evolutionary biology</json:string></wos><scienceMetrix><json:string>natural sciences</json:string><json:string>biology</json:string><json:string>evolutionary biology</json:string></scienceMetrix></categories><publicationDate>1989</publicationDate><copyrightDate>1989</copyrightDate><doi><json:string>10.1007/BF00936911</json:string></doi><id>7972426BC6D1FCFA8E53DB451DE42B5CBA482B3F</id><score>1</score><fulltext><json:item><extension>pdf</extension><original>true</original><mimetype>application/pdf</mimetype><uri>https://api.istex.fr/document/7972426BC6D1FCFA8E53DB451DE42B5CBA482B3F/fulltext/pdf</uri></json:item><json:item><extension>zip</extension><original>false</original><mimetype>application/zip</mimetype><uri>https://api.istex.fr/document/7972426BC6D1FCFA8E53DB451DE42B5CBA482B3F/fulltext/zip</uri></json:item><istex:fulltextTEI uri="https://api.istex.fr/document/7972426BC6D1FCFA8E53DB451DE42B5CBA482B3F/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a" type="main" xml:lang="en">Development and regional differentiation of the European vegetation during the Tertiary</title><respStmt><resp>Références bibliographiques récupérées via GROBID</resp><name resp="ISTEX-API">ISTEX-API (INIST-CNRS)</name></respStmt><respStmt><resp>Références bibliographiques récupérées via GROBID</resp><name resp="ISTEX-API">ISTEX-API (INIST-CNRS)</name></respStmt></titleStmt><publicationStmt><authority>ISTEX</authority><publisher>Springer-Verlag</publisher><pubPlace>Vienna</pubPlace><availability><p>Springer-Verlag, 1989</p></availability><date>1987-02-02</date></publicationStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a" type="main" xml:lang="en">Development and regional differentiation of the European vegetation during the Tertiary</title><author xml:id="author-1"><persName><forename type="first">Dieter</forename><surname>Mai</surname></persName><affiliation>Bereich Botanik und Arboretum des Museums für Naturkunde, Humboldt-Universität, Späthstrasse 80/81, DDR-1195, Berlin, German Democratic Republic</affiliation></author></analytic><monogr><title level="j">Plant Systematics and Evolution</title><title level="j" type="sub">Entwicklungsgeschichte und Systematik der Pflanzen</title><title level="j" type="abbrev">Pl Syst Evol</title><idno type="journal-ID">606</idno><idno type="pISSN">0378-2697</idno><idno type="eISSN">1615-6110</idno><idno type="issue-article-count">17</idno><idno type="volume-issue-count">4</idno><imprint><publisher>Springer-Verlag</publisher><pubPlace>Vienna</pubPlace><date type="published" when="1989-03-01"></date><biblScope unit="volume">162</biblScope><biblScope unit="issue">1-4</biblScope><biblScope unit="page" from="79">79</biblScope><biblScope unit="page" to="91">91</biblScope></imprint></monogr><idno type="istex">7972426BC6D1FCFA8E53DB451DE42B5CBA482B3F</idno><idno type="DOI">10.1007/BF00936911</idno><idno type="ArticleID">BF00936911</idno><idno type="ArticleID">Art4</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>1987-02-02</date></creation><langUsage><language ident="en">en</language></langUsage><abstract xml:lang="en"><p>Abstract: The Tertiary vegetation of Europe evolved from paratropical to warm-temperate and temperate forms in response to a progressive, non-linear, climatic cooling. Its vegetational forms are composed mainly of two separate ecological units: the evergreen, laurophyll “paleotropical geoflora” and the deciduous, broad-leaved “Arctotertiary geoflora”. The development of the Tertiary climate and its interaction with the vegetation are convincingly indicated by the geoflora's migration; the changes in its composition; and the development of the Tertiary forest, swamp, and aquatic plant communities. The “paleotropical geoflora” is characterized in the upper Cretaceous to the upper Miocene by paratropical rain forest, subtropical rain and laurel forests, temperate laurel forests and edaphically-mediated formation of laurel-conifer forests. The “Arctotertiary geoflora” advanced into Europe in waves since the Paleocene and formed the basis for the Tertiary mixed mesophytic forests. These can be divided into warm-temperate rain forests, oak-hornbeamchestnut or mixed beech-oak-hornbeam forests, and edaphic formations such as bottomland and swamp forests. Beginning in the lower Cretaceous, the hydrophytic vegetation developed independently of the forest vegetation and formed very diverse herbaceous fresh water, swamp, salt water, and coastal formations. Considerable differences in composition allow to separate floral regions and provinces in Eurosiberia. Instead of three ill-defined floral regions in the Paleocene, there are four well-defined floral regions in the Pliocene. A Mediterranean region cannot be recognized, although Mediterranean (eumesogeic) floral elements appear in the Eocene/Oligocene and thereafter. The Mediterranean sclerophyll forests probably arose after the destruction of the laurophyll forests during the Pleistocene.</p></abstract><textClass><keywords scheme="Journal Subject"><list><head>Life Sciences</head><item><term>Plant Ecology</term></item><item><term>Plant Sciences</term></item><item><term>Plant Anatomy/Development</term></item><item><term>Plant Systematics/Taxonomy/Biogeography</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="1987-02-02">Created</change><change when="1989-03-01">Published</change><change xml:id="refBibs-istex" who="#ISTEX-API" when="2016-11-23">References added</change><change xml:id="refBibs-istex" who="#ISTEX-API" when="2017-01-21">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/7972426BC6D1FCFA8E53DB451DE42B5CBA482B3F/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="Springer, Publisher found" wicri:toSee="no header"><istex:xmlDeclaration>version="1.0" encoding="UTF-8"</istex:xmlDeclaration><istex:docType PUBLIC="-//Springer-Verlag//DTD A++ V2.4//EN" URI="http://devel.springer.de/A++/V2.4/DTD/A++V2.4.dtd" name="istex:docType"></istex:docType><istex:document><Publisher><PublisherInfo><PublisherName>Springer-Verlag</PublisherName><PublisherLocation>Vienna</PublisherLocation></PublisherInfo><Journal><JournalInfo JournalProductType="ArchiveJournal" NumberingStyle="Unnumbered"><JournalID>606</JournalID><JournalPrintISSN>0378-2697</JournalPrintISSN><JournalElectronicISSN>1615-6110</JournalElectronicISSN><JournalTitle>Plant Systematics and Evolution</JournalTitle><JournalSubTitle>Entwicklungsgeschichte und Systematik der Pflanzen</JournalSubTitle><JournalAbbreviatedTitle>Pl Syst Evol</JournalAbbreviatedTitle><JournalSubjectGroup><JournalSubject Type="Primary">Life Sciences</JournalSubject><JournalSubject Type="Secondary">Plant Ecology</JournalSubject><JournalSubject Type="Secondary">Plant Sciences</JournalSubject><JournalSubject Type="Secondary">Plant Anatomy/Development</JournalSubject><JournalSubject Type="Secondary">Plant Systematics/Taxonomy/Biogeography</JournalSubject></JournalSubjectGroup></JournalInfo><Volume><VolumeInfo VolumeType="Regular" TocLevels="0"><VolumeIDStart>162</VolumeIDStart><VolumeIDEnd>162</VolumeIDEnd><VolumeIssueCount>4</VolumeIssueCount></VolumeInfo><Issue IssueType="Combined"><IssueInfo TocLevels="0"><IssueIDStart>1</IssueIDStart><IssueIDEnd>4</IssueIDEnd><IssueArticleCount>17</IssueArticleCount><IssueHistory><CoverDate><DateString>1989</DateString><Year>1989</Year><Month>3</Month></CoverDate></IssueHistory><IssueCopyright><CopyrightHolderName>Springer-Verlag</CopyrightHolderName><CopyrightYear>1989</CopyrightYear></IssueCopyright></IssueInfo><Article ID="Art4"><ArticleInfo Language="En" ArticleType="OriginalPaper" NumberingStyle="Unnumbered" TocLevels="0" ContainsESM="No"><ArticleID>BF00936911</ArticleID><ArticleDOI>10.1007/BF00936911</ArticleDOI><ArticleSequenceNumber>4</ArticleSequenceNumber><ArticleTitle Language="En">Development and regional differentiation of the European vegetation during the Tertiary</ArticleTitle><ArticleFirstPage>79</ArticleFirstPage><ArticleLastPage>91</ArticleLastPage><ArticleHistory><RegistrationDate><Year>2004</Year><Month>12</Month><Day>19</Day></RegistrationDate><Received><Year>1987</Year><Month>2</Month><Day>2</Day></Received></ArticleHistory><ArticleCopyright><CopyrightHolderName>Springer-Verlag</CopyrightHolderName><CopyrightYear>1989</CopyrightYear></ArticleCopyright><ArticleGrants Type="Regular"><MetadataGrant Grant="OpenAccess"></MetadataGrant><AbstractGrant Grant="OpenAccess"></AbstractGrant><BodyPDFGrant Grant="Restricted"></BodyPDFGrant><BodyHTMLGrant Grant="Restricted"></BodyHTMLGrant><BibliographyGrant Grant="Restricted"></BibliographyGrant><ESMGrant Grant="Restricted"></ESMGrant></ArticleGrants><ArticleContext><JournalID>606</JournalID><VolumeIDStart>162</VolumeIDStart><VolumeIDEnd>162</VolumeIDEnd><IssueIDStart>1</IssueIDStart><IssueIDEnd>4</IssueIDEnd></ArticleContext></ArticleInfo><ArticleHeader><AuthorGroup><Author AffiliationIDS="Aff1"><AuthorName DisplayOrder="Western"><GivenName>Dieter</GivenName><GivenName>H.</GivenName><FamilyName>Mai</FamilyName></AuthorName></Author><Affiliation ID="Aff1"><OrgDivision>Bereich Botanik und Arboretum des Museums für Naturkunde</OrgDivision><OrgName>Humboldt-Universität</OrgName><OrgAddress><Street>Späthstrasse 80/81</Street><Postcode>DDR-1195</Postcode><City>Berlin</City><Country>German Democratic Republic</Country></OrgAddress></Affiliation></AuthorGroup><Abstract ID="Abs1" Language="En"><Heading>Abstract</Heading><Para>The Tertiary vegetation of Europe evolved from paratropical to warm-temperate and temperate forms in response to a progressive, non-linear, climatic cooling. Its vegetational forms are composed mainly of two separate ecological units: the evergreen, laurophyll “paleotropical geoflora” and the deciduous, broad-leaved “Arctotertiary geoflora”. The development of the Tertiary climate and its interaction with the vegetation are convincingly indicated by the geoflora's migration; the changes in its composition; and the development of the Tertiary forest, swamp, and aquatic plant communities. The “paleotropical geoflora” is characterized in the upper Cretaceous to the upper Miocene by paratropical rain forest, subtropical rain and laurel forests, temperate laurel forests and edaphically-mediated formation of laurel-conifer forests. The “Arctotertiary geoflora” advanced into Europe in waves since the Paleocene and formed the basis for the Tertiary mixed mesophytic forests. These can be divided into warm-temperate rain forests, oak-hornbeamchestnut or mixed beech-oak-hornbeam forests, and edaphic formations such as bottomland and swamp forests. Beginning in the lower Cretaceous, the hydrophytic vegetation developed independently of the forest vegetation and formed very diverse herbaceous fresh water, swamp, salt water, and coastal formations. Considerable differences in composition allow to separate floral regions and provinces in Eurosiberia. Instead of three ill-defined floral regions in the Paleocene, there are four well-defined floral regions in the Pliocene. A Mediterranean region cannot be recognized, although Mediterranean (eumesogeic) floral elements appear in the Eocene/Oligocene and thereafter. The Mediterranean sclerophyll forests probably arose after the destruction of the laurophyll forests during the Pleistocene.</Para></Abstract><KeywordGroup Language="En"><Heading>Key words</Heading><Keyword>History of vegetation</Keyword><Keyword>Tertiary</Keyword><Keyword>paleotropical and Arctotertiary geofloras</Keyword><Keyword>forest types</Keyword><Keyword>herbs</Keyword><Keyword>aquatic angiosperm communities</Keyword><Keyword>floristic regions of Europe</Keyword></KeywordGroup></ArticleHeader><NoBody></NoBody></Article></Issue></Volume></Journal></Publisher></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Development and regional differentiation of the European vegetation during the Tertiary</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Development and regional differentiation of the European vegetation during the Tertiary</title></titleInfo><name type="personal"><namePart type="given">Dieter</namePart><namePart type="given">H.</namePart><namePart type="family">Mai</namePart><affiliation>Bereich Botanik und Arboretum des Museums für Naturkunde, Humboldt-Universität, Späthstrasse 80/81, DDR-1195, Berlin, German Democratic Republic</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="research-article" displayLabel="OriginalPaper"></genre><originInfo><publisher>Springer-Verlag</publisher><place><placeTerm type="text">Vienna</placeTerm></place><dateCreated encoding="w3cdtf">1987-02-02</dateCreated><dateIssued encoding="w3cdtf">1989-03-01</dateIssued><copyrightDate encoding="w3cdtf">1989</copyrightDate></originInfo><language><languageTerm type="code" authority="rfc3066">en</languageTerm><languageTerm type="code" authority="iso639-2b">eng</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType></physicalDescription><abstract lang="en">Abstract: The Tertiary vegetation of Europe evolved from paratropical to warm-temperate and temperate forms in response to a progressive, non-linear, climatic cooling. Its vegetational forms are composed mainly of two separate ecological units: the evergreen, laurophyll “paleotropical geoflora” and the deciduous, broad-leaved “Arctotertiary geoflora”. The development of the Tertiary climate and its interaction with the vegetation are convincingly indicated by the geoflora's migration; the changes in its composition; and the development of the Tertiary forest, swamp, and aquatic plant communities. The “paleotropical geoflora” is characterized in the upper Cretaceous to the upper Miocene by paratropical rain forest, subtropical rain and laurel forests, temperate laurel forests and edaphically-mediated formation of laurel-conifer forests. The “Arctotertiary geoflora” advanced into Europe in waves since the Paleocene and formed the basis for the Tertiary mixed mesophytic forests. These can be divided into warm-temperate rain forests, oak-hornbeamchestnut or mixed beech-oak-hornbeam forests, and edaphic formations such as bottomland and swamp forests. Beginning in the lower Cretaceous, the hydrophytic vegetation developed independently of the forest vegetation and formed very diverse herbaceous fresh water, swamp, salt water, and coastal formations. Considerable differences in composition allow to separate floral regions and provinces in Eurosiberia. Instead of three ill-defined floral regions in the Paleocene, there are four well-defined floral regions in the Pliocene. A Mediterranean region cannot be recognized, although Mediterranean (eumesogeic) floral elements appear in the Eocene/Oligocene and thereafter. The Mediterranean sclerophyll forests probably arose after the destruction of the laurophyll forests during the Pleistocene.</abstract><relatedItem type="host"><titleInfo><title>Plant Systematics and Evolution</title><subTitle>Entwicklungsgeschichte und Systematik der Pflanzen</subTitle></titleInfo><titleInfo type="abbreviated"><title>Pl Syst Evol</title></titleInfo><genre type="journal" displayLabel="Archive Journal"></genre><originInfo><dateIssued encoding="w3cdtf">1989-03-01</dateIssued><copyrightDate encoding="w3cdtf">1989</copyrightDate></originInfo><subject><genre>Life Sciences</genre><topic>Plant Ecology</topic><topic>Plant Sciences</topic><topic>Plant Anatomy/Development</topic><topic>Plant Systematics/Taxonomy/Biogeography</topic></subject><identifier type="ISSN">0378-2697</identifier><identifier type="eISSN">1615-6110</identifier><identifier type="JournalID">606</identifier><identifier type="IssueArticleCount">17</identifier><identifier type="VolumeIssueCount">4</identifier><part><date>1989</date><detail type="volume"><number>162</number><caption>vol.</caption></detail><detail type="issue"><number>1-4</number><caption>no.</caption></detail><extent unit="pages"><start>79</start><end>91</end></extent></part><recordInfo><recordOrigin>Springer-Verlag, 1989</recordOrigin></recordInfo></relatedItem><identifier type="istex">7972426BC6D1FCFA8E53DB451DE42B5CBA482B3F</identifier><identifier type="DOI">10.1007/BF00936911</identifier><identifier type="ArticleID">BF00936911</identifier><identifier type="ArticleID">Art4</identifier><accessCondition type="use and reproduction" contentType="copyright">Springer-Verlag, 1989</accessCondition><recordInfo><recordContentSource>SPRINGER</recordContentSource><recordOrigin>Springer-Verlag, 1989</recordOrigin></recordInfo></mods></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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