Fossil pollen records of extant angiosperms
Identifieur interne : 000F65 ( Istex/Corpus ); précédent : 000F64; suivant : 000F66Fossil pollen records of extant angiosperms
Auteurs : Jan MullerSource :
- The Botanical Review [ 0006-8101 ] ; 1981-01-01.
Abstract
Abstract: The fossil record for angiosperm pollen types which are comparable to recent taxa is evaluated, following a similar survey published in 1970. Special attention is paid to the dating of the sediments. Evidence for 139 families is considered to be reliable, for others the records are cited as provisional, pending the accumulation of more evidence. Some published records are shown to be erroneous. In the early Cretaceous only types occur indicating the presence of plants ancestral to Magnoliidae and Liliatae. In the Turonian increased differentiation is evident, culminating in the Maestrichtian when evidence for the presence of most major taxa of angiosperms is available. In the Tertiary diversification at lower taxonomic level continues and identification with living taxa becomes more certain. Herbaceous groups tend to appear later in the record than woody ones.
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DOI: 10.1007/BF02860537
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Rev</title><idno type="ISSN">0006-8101</idno><idno type="eISSN">1874-9372</idno><imprint><publisher>Springer-Verlag</publisher><pubPlace>New York</pubPlace><date type="published" when="1981-01-01">1981-01-01</date><biblScope unit="volume">47</biblScope><biblScope unit="issue">1</biblScope><biblScope unit="page" from="1">1</biblScope><biblScope unit="page" to="142">142</biblScope></imprint><idno type="ISSN">0006-8101</idno></series><idno type="istex">1C29B8268DA04948BDAFA82BE282BA21F75A0C65</idno><idno type="DOI">10.1007/BF02860537</idno><idno type="ArticleID">BF02860537</idno><idno type="ArticleID">Art1</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0006-8101</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Abstract: The fossil record for angiosperm pollen types which are comparable to recent taxa is evaluated, following a similar survey published in 1970. Special attention is paid to the dating of the sediments. Evidence for 139 families is considered to be reliable, for others the records are cited as provisional, pending the accumulation of more evidence. Some published records are shown to be erroneous. In the early Cretaceous only types occur indicating the presence of plants ancestral to Magnoliidae and Liliatae. In the Turonian increased differentiation is evident, culminating in the Maestrichtian when evidence for the presence of most major taxa of angiosperms is available. In the Tertiary diversification at lower taxonomic level continues and identification with living taxa becomes more certain. Herbaceous groups tend to appear later in the record than woody ones.</div></front></TEI><istex><corpusName>springer</corpusName><author><json:item><name>Jan Muller</name><affiliations><json:string>Rijksherbarium, University of Leiden, Leiden, The Netherlands</json:string></affiliations></json:item></author><articleId><json:string>BF02860537</json:string><json:string>Art1</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>OriginalPaper</json:string></originalGenre><abstract>Abstract: The fossil record for angiosperm pollen types which are comparable to recent taxa is evaluated, following a similar survey published in 1970. Special attention is paid to the dating of the sediments. Evidence for 139 families is considered to be reliable, for others the records are cited as provisional, pending the accumulation of more evidence. Some published records are shown to be erroneous. In the early Cretaceous only types occur indicating the presence of plants ancestral to Magnoliidae and Liliatae. In the Turonian increased differentiation is evident, culminating in the Maestrichtian when evidence for the presence of most major taxa of angiosperms is available. In the Tertiary diversification at lower taxonomic level continues and identification with living taxa becomes more certain. Herbaceous groups tend to appear later in the record than woody ones.</abstract><qualityIndicators><score>6.608</score><pdfVersion>1.3</pdfVersion><pdfPageSize>432 x 648 pts</pdfPageSize><refBibsNative>false</refBibsNative><keywordCount>0</keywordCount><abstractCharCount>882</abstractCharCount><pdfWordCount>51007</pdfWordCount><pdfCharCount>319053</pdfCharCount><pdfPageCount>142</pdfPageCount><abstractWordCount>134</abstractWordCount></qualityIndicators><title>Fossil pollen records of extant angiosperms</title><refBibs><json:item><author><json:item><name>O,S Adegoke</name></json:item><json:item><name>R,E Jan</name></json:item><json:item><name>A,E Chine</name></json:item><json:item><name> Agumanu</name></json:item></author><host><pages><last>283</last><first>267</first></pages><author></author><title>Palynology and age of the Kerri-Kerri Formation</title><publicationDate>1978</publicationDate></host><publicationDate>1978</publicationDate></json:item><json:item><author><json:item><name>J,M Agasie</name></json:item></author><host><volume>15</volume><pages><last>30</last><first>13</first></pages><author></author><title>Micropaleontology</title><publicationDate>1969</publicationDate></host><title>Late Cretaceous palynomorphs from northeastern Arizona</title><publicationDate>1969</publicationDate></json:item><json:item><author><json:item><name>J,A R Anderson</name></json:item><json:item><name>J Muller</name></json:item></author><host><volume>19</volume><pages><last>351</last><first>291</first></pages><author></author><title>Borneo. 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Pages 88-93 in The palynology of the cenophyte</title><publicationDate>1973</publicationDate></json:item></refBibs><genre><json:string>research-article</json:string></genre><host><volume>47</volume><pages><last>142</last><first>1</first></pages><issn><json:string>0006-8101</json:string></issn><issue>1</issue><subject><json:item><value>Life Sciences</value></json:item><json:item><value>Plant Sciences</value></json:item><json:item><value>Plant Systematics/Taxonomy/Biogeography</value></json:item><json:item><value>Plant Ecology</value></json:item><json:item><value>Life Sciences, general</value></json:item></subject><journalId><json:string>12229</json:string></journalId><genre><json:string>journal</json:string></genre><language><json:string>unknown</json:string></language><eissn><json:string>1874-9372</json:string></eissn><title>The Botanical Review</title><publicationDate>1981</publicationDate><copyrightDate>1981</copyrightDate></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>1981</publicationDate><copyrightDate>1981</copyrightDate><doi><json:string>10.1007/BF02860537</json:string></doi><id>1C29B8268DA04948BDAFA82BE282BA21F75A0C65</id><score>1</score><fulltext><json:item><extension>pdf</extension><original>true</original><mimetype>application/pdf</mimetype><uri>https://api.istex.fr/document/1C29B8268DA04948BDAFA82BE282BA21F75A0C65/fulltext/pdf</uri></json:item><json:item><extension>zip</extension><original>false</original><mimetype>application/zip</mimetype><uri>https://api.istex.fr/document/1C29B8268DA04948BDAFA82BE282BA21F75A0C65/fulltext/zip</uri></json:item><istex:fulltextTEI uri="https://api.istex.fr/document/1C29B8268DA04948BDAFA82BE282BA21F75A0C65/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a" type="main" xml:lang="en">Fossil pollen records of extant angiosperms</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>New York</pubPlace><availability><p>The New York Botanical Garden, 1981</p></availability><date>1981</date></publicationStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a" type="main" xml:lang="en">Fossil pollen records of extant angiosperms</title><author xml:id="author-1" corresp="yes"><persName><forename type="first">Jan</forename><surname>Muller</surname></persName><affiliation>Rijksherbarium, University of Leiden, Leiden, The Netherlands</affiliation></author></analytic><monogr><title level="j">The Botanical Review</title><title level="j" type="abbrev">Bot. Rev</title><idno type="journal-ID">12229</idno><idno type="pISSN">0006-8101</idno><idno type="eISSN">1874-9372</idno><idno type="issue-article-count">1</idno><idno type="volume-issue-count">4</idno><imprint><publisher>Springer-Verlag</publisher><pubPlace>New York</pubPlace><date type="published" when="1981-01-01"></date><biblScope unit="volume">47</biblScope><biblScope unit="issue">1</biblScope><biblScope unit="page" from="1">1</biblScope><biblScope unit="page" to="142">142</biblScope></imprint></monogr><idno type="istex">1C29B8268DA04948BDAFA82BE282BA21F75A0C65</idno><idno type="DOI">10.1007/BF02860537</idno><idno type="ArticleID">BF02860537</idno><idno type="ArticleID">Art1</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>1981</date></creation><langUsage><language ident="en">en</language></langUsage><abstract xml:lang="en"><p>Abstract: The fossil record for angiosperm pollen types which are comparable to recent taxa is evaluated, following a similar survey published in 1970. Special attention is paid to the dating of the sediments. Evidence for 139 families is considered to be reliable, for others the records are cited as provisional, pending the accumulation of more evidence. Some published records are shown to be erroneous. In the early Cretaceous only types occur indicating the presence of plants ancestral to Magnoliidae and Liliatae. In the Turonian increased differentiation is evident, culminating in the Maestrichtian when evidence for the presence of most major taxa of angiosperms is available. In the Tertiary diversification at lower taxonomic level continues and identification with living taxa becomes more certain. Herbaceous groups tend to appear later in the record than woody ones.</p></abstract><abstract xml:lang="fr"><p>Résumé: Notre connaissance des types de pollen fossile d’Angiospermes qui peuvent être identifiés avec des taxons vivants est evaluée suivant un aperçu pareil publié en 1970. On s’est occupé spécialement de la détermination de_ l’âge des sediments. Les données pour 139 familles sont acceptées comme dignes de confiance, pour d’autres les données sont citées comme étant provisoires, en attendant l’accumulation de plus d’évidence. Quelques données publiées se sont avérées êtres fausses. Dans le Crétacé inférieur on trouve seulement des types qui indiquent la présence de plantes ancestrales aux Magnoliidae et Liliatae. Dans le Turonien une plus grande différentiation est évidente, qui culmine dans le Maestrichtien, quand on a des indications de la présence de la plupart des taxons principaux des Angiospermes. Pendant le Tertiaire la diversification à des niveaux taxonomiques inférieurs continue et l’identification avec des taxons vivants devient plus sûre. Les groupes herbacées ont la tendance d’apparaître plus tard dans la succession stratigraphique que les groupes ligneuses.</p></abstract><abstract xml:lang="it"><p>Resúmen: Los datos sobre la distribución de tipos fósiles de pólen de los Angiospermos que son comparables a los taxa recientes son evaluados en continuación de una compilación semejante publicada en 1970. Los métodos usados para fechar los sedimentos son estudiados con mucha atención. La evidencia para la presencia de 139 familias es considerada como cierta, para algunas otras familias los datos son considerados como provisionales, en espera de la acumulación de más información. Algunos datos publicados son demostrados como equivocados. En el Cretáceo inferior solamente se encuentran tipos indicativos de la presencia de plantas ancestrales a los Magnoliidae y Liliatae. En el Turoniense es evidente un aumento en la differenciación, y ésto culmina en el Maestrichtiano cuando se hallan presentes la mayoría de los taxa superiores de los Angiospermos. En el Terciario la diversificación en niveles taxonómicos inferiores continúa, y la identificatión con taxa recientes se vuelve mas segura. Los grupos herbáceos tienden a aparecer más tarde que los grupos leñosos en la sucesión estratigráfica.</p></abstract><abstract xml:lang="de"><p>Zusammenfassung: Der Rekord fossiler Pollen-Typen der Angiospermen, die mit rezenten Taxa vergleichbar sind, wird ausgewertet, ähnlich wie dies in einer bereits 1970 erschienenen Veröffentlichung geschehen ist. Besondere Aufmerksamkeit wurde der Datierung der Sedimente gewidmet. Eine Übereinstimmung wird für 139 Familien für zuverlässig gehalten, für andere Familien wird diese als vorläufig angesehen, d.h. abhängig von der Häufung von mehr Gegebenheiten in der Zukunft. Einige früher veröffentlichte Rekorde werden als irrtümlich nachgewiesen. In der unteren Kreide kommen nur Pollen-Typen vor, welche die Anwesenheit von Pflanzen zeigen, die Vorläufer von Magnoliideae und Liliatae sind. Im Turon wird eine zunehmende Differenzierung deutlich, die im Maestrichtien kulminiert, in welcher die Anwesenheit der meisten höheren Angiospermen-Taxa deutlich wird. Im Tertiär setzt sich eine Differenzierung auf einem tieferen taxonomischen Niveau fort, und die Identität mit rezenten Taxa wird gewisser. Krautige Gruppen neigen dazu, später aufzutreten als Holzpflanzen.</p></abstract><textClass><keywords scheme="Journal-Subject-Group"><list><label>L</label><label>L24000</label><label>L24051</label><label>L19112</label><label>L00004</label><item><term>Life Sciences</term></item><item><term>Plant Sciences</term></item><item><term>Plant Systematics/Taxonomy/Biogeography</term></item><item><term>Plant Ecology</term></item><item><term>Life Sciences, general</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="1981-01-01">Published</change><change xml:id="refBibs-istex" who="#ISTEX-API" when="2016-11-22">References added</change><change xml:id="refBibs-istex" who="#ISTEX-API" when="2017-01-20">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/1C29B8268DA04948BDAFA82BE282BA21F75A0C65/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>New York</PublisherLocation></PublisherInfo><Journal><JournalInfo JournalProductType="ArchiveJournal" NumberingStyle="Unnumbered"><JournalID>12229</JournalID><JournalPrintISSN>0006-8101</JournalPrintISSN><JournalElectronicISSN>1874-9372</JournalElectronicISSN><JournalTitle>The Botanical Review</JournalTitle><JournalAbbreviatedTitle>Bot. Rev</JournalAbbreviatedTitle><JournalSubjectGroup><JournalSubject Code="L" Type="Primary">Life Sciences</JournalSubject><JournalSubject Code="L24000" Priority="1" Type="Secondary">Plant Sciences</JournalSubject><JournalSubject Code="L24051" Priority="2" Type="Secondary">Plant Systematics/Taxonomy/Biogeography</JournalSubject><JournalSubject Code="L19112" Priority="3" Type="Secondary">Plant Ecology</JournalSubject><JournalSubject Code="L00004" Priority="4" Type="Secondary">Life Sciences, general</JournalSubject></JournalSubjectGroup></JournalInfo><Volume><VolumeInfo TocLevels="0" VolumeType="Regular"><VolumeIDStart>47</VolumeIDStart><VolumeIDEnd>47</VolumeIDEnd><VolumeIssueCount>4</VolumeIssueCount></VolumeInfo><Issue IssueType="Regular"><IssueInfo TocLevels="0"><IssueIDStart>1</IssueIDStart><IssueIDEnd>1</IssueIDEnd><IssueArticleCount>1</IssueArticleCount><IssueHistory><CoverDate><DateString>January–March 1981</DateString><Year>1981</Year><Month>1</Month></CoverDate></IssueHistory><IssueCopyright><CopyrightHolderName>The New York Botanical Garden</CopyrightHolderName><CopyrightYear>1981</CopyrightYear></IssueCopyright></IssueInfo><Article ID="Art1"><ArticleInfo ArticleType="OriginalPaper" ContainsESM="No" Language="En" NumberingStyle="Unnumbered" TocLevels="0"><ArticleID>BF02860537</ArticleID><ArticleDOI>10.1007/BF02860537</ArticleDOI><ArticleSequenceNumber>1</ArticleSequenceNumber><ArticleTitle Language="En">Fossil pollen records of extant angiosperms</ArticleTitle><ArticleFirstPage>1</ArticleFirstPage><ArticleLastPage>142</ArticleLastPage><ArticleHistory><RegistrationDate><Year>2008</Year><Month>3</Month><Day>11</Day></RegistrationDate></ArticleHistory><ArticleCopyright><CopyrightHolderName>The New York Botanical Garden</CopyrightHolderName><CopyrightYear>1981</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>12229</JournalID><VolumeIDStart>47</VolumeIDStart><VolumeIDEnd>47</VolumeIDEnd><IssueIDStart>1</IssueIDStart><IssueIDEnd>1</IssueIDEnd></ArticleContext></ArticleInfo><ArticleHeader><AuthorGroup><Author AffiliationIDS="Aff1" CorrespondingAffiliationID="Aff1"><AuthorName DisplayOrder="Western"><GivenName>Jan</GivenName><FamilyName>Muller</FamilyName></AuthorName></Author><Affiliation ID="Aff1"><OrgDivision>Rijksherbarium</OrgDivision><OrgName>University of Leiden</OrgName><OrgAddress><City>Leiden</City><Country>The Netherlands</Country></OrgAddress></Affiliation></AuthorGroup><Abstract ID="Abs1" Language="En"><Heading>Abstract</Heading><Para>The fossil record for angiosperm pollen types which are comparable to recent taxa is evaluated, following a similar survey published in 1970. Special attention is paid to the dating of the sediments. Evidence for 139 families is considered to be reliable, for others the records are cited as provisional, pending the accumulation of more evidence. Some published records are shown to be erroneous.</Para><Para>In the early Cretaceous only types occur indicating the presence of plants ancestral to Magnoliidae and Liliatae. In the Turonian increased differentiation is evident, culminating in the Maestrichtian when evidence for the presence of most major taxa of angiosperms is available. In the Tertiary diversification at lower taxonomic level continues and identification with living taxa becomes more certain. Herbaceous groups tend to appear later in the record than woody ones.</Para></Abstract><Abstract ID="Abs2" Language="Fr"><Heading>Résumé</Heading><Para>Notre connaissance des types de pollen fossile d’Angiospermes qui peuvent être identifiés avec des taxons vivants est evaluée suivant un aperçu pareil publié en 1970. On s’est occupé spécialement de la détermination de_ l’âge des sediments. Les données pour 139 familles sont acceptées comme dignes de confiance, pour d’autres les données sont citées comme étant provisoires, en attendant l’accumulation de plus d’évidence. Quelques données publiées se sont avérées êtres fausses.</Para><Para>Dans le Crétacé inférieur on trouve seulement des types qui indiquent la présence de plantes ancestrales aux Magnoliidae et Liliatae. Dans le Turonien une plus grande différentiation est évidente, qui culmine dans le Maestrichtien, quand on a des indications de la présence de la plupart des taxons principaux des Angiospermes. Pendant le Tertiaire la diversification à des niveaux taxonomiques inférieurs continue et l’identification avec des taxons vivants devient plus sûre. Les groupes herbacées ont la tendance d’apparaître plus tard dans la succession stratigraphique que les groupes ligneuses.</Para></Abstract><Abstract ID="Abs3" Language="It"><Heading>Resúmen</Heading><Para>Los datos sobre la distribución de tipos fósiles de pólen de los Angiospermos que son comparables a los taxa recientes son evaluados en continuación de una compilación semejante publicada en 1970.</Para><Para>Los métodos usados para fechar los sedimentos son estudiados con mucha atención. La evidencia para la presencia de 139 familias es considerada como cierta, para algunas otras familias los datos son considerados como provisionales, en espera de la acumulación de más información. Algunos datos publicados son demostrados como equivocados.</Para><Para>En el Cretáceo inferior solamente se encuentran tipos indicativos de la presencia de plantas ancestrales a los Magnoliidae y Liliatae. En el Turoniense es evidente un aumento en la differenciación, y ésto culmina en el Maestrichtiano cuando se hallan presentes la mayoría de los taxa superiores de los Angiospermos. En el Terciario la diversificación en niveles taxonómicos inferiores continúa, y la identificatión con taxa recientes se vuelve mas segura. Los grupos herbáceos tienden a aparecer más tarde que los grupos leñosos en la sucesión estratigráfica.</Para></Abstract><Abstract ID="Abs4" Language="De"><Heading>Zusammenfassung</Heading><Para>Der Rekord fossiler Pollen-Typen der Angiospermen, die mit rezenten Taxa vergleichbar sind, wird ausgewertet, ähnlich wie dies in einer bereits 1970 erschienenen Veröffentlichung geschehen ist. Besondere Aufmerksamkeit wurde der Datierung der Sedimente gewidmet. Eine Übereinstimmung wird für 139 Familien für zuverlässig gehalten, für andere Familien wird diese als vorläufig angesehen, d.h. abhängig von der Häufung von mehr Gegebenheiten in der Zukunft. Einige früher veröffentlichte Rekorde werden als irrtümlich nachgewiesen.</Para><Para>In der unteren Kreide kommen nur Pollen-Typen vor, welche die Anwesenheit von Pflanzen zeigen, die Vorläufer von Magnoliideae und Liliatae sind. Im Turon wird eine zunehmende Differenzierung deutlich, die im Maestrichtien kulminiert, in welcher die Anwesenheit der meisten höheren Angiospermen-Taxa deutlich wird. Im Tertiär setzt sich eine Differenzierung auf einem tieferen taxonomischen Niveau fort, und die Identität mit rezenten Taxa wird gewisser. Krautige Gruppen neigen dazu, später aufzutreten als Holzpflanzen.</Para></Abstract><ArticleNote Type="Misc"><SimplePara>Reprints of this issue<Emphasis Type="Bold">[47(1)]</Emphasis> may be obtained from: Publications Office, The New York Botanical Garden, Bronx, NY 10458, USA. PRICE (includes postage and handling fee):<Emphasis Type="Bold">U.S. ORDERS</Emphasis>: $8.75;<Emphasis Type="Bold">NON-U.S. ORDERS</Emphasis>: $9.50. (Payment in U.S. currency drawn on a U.S. bank. Thank you.)</SimplePara></ArticleNote></ArticleHeader><NoBody></NoBody></Article></Issue></Volume></Journal></Publisher></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Fossil pollen records of extant angiosperms</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Fossil pollen records of extant angiosperms</title></titleInfo><name type="personal" displayLabel="corresp"><namePart type="given">Jan</namePart><namePart type="family">Muller</namePart><affiliation>Rijksherbarium, University of Leiden, Leiden, The Netherlands</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">New York</placeTerm></place><dateIssued encoding="w3cdtf">1981-01-01</dateIssued><copyrightDate encoding="w3cdtf">1981</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 fossil record for angiosperm pollen types which are comparable to recent taxa is evaluated, following a similar survey published in 1970. Special attention is paid to the dating of the sediments. Evidence for 139 families is considered to be reliable, for others the records are cited as provisional, pending the accumulation of more evidence. Some published records are shown to be erroneous. In the early Cretaceous only types occur indicating the presence of plants ancestral to Magnoliidae and Liliatae. In the Turonian increased differentiation is evident, culminating in the Maestrichtian when evidence for the presence of most major taxa of angiosperms is available. In the Tertiary diversification at lower taxonomic level continues and identification with living taxa becomes more certain. Herbaceous groups tend to appear later in the record than woody ones.</abstract><abstract lang="fr">Résumé: Notre connaissance des types de pollen fossile d’Angiospermes qui peuvent être identifiés avec des taxons vivants est evaluée suivant un aperçu pareil publié en 1970. On s’est occupé spécialement de la détermination de_ l’âge des sediments. Les données pour 139 familles sont acceptées comme dignes de confiance, pour d’autres les données sont citées comme étant provisoires, en attendant l’accumulation de plus d’évidence. Quelques données publiées se sont avérées êtres fausses. Dans le Crétacé inférieur on trouve seulement des types qui indiquent la présence de plantes ancestrales aux Magnoliidae et Liliatae. Dans le Turonien une plus grande différentiation est évidente, qui culmine dans le Maestrichtien, quand on a des indications de la présence de la plupart des taxons principaux des Angiospermes. Pendant le Tertiaire la diversification à des niveaux taxonomiques inférieurs continue et l’identification avec des taxons vivants devient plus sûre. Les groupes herbacées ont la tendance d’apparaître plus tard dans la succession stratigraphique que les groupes ligneuses.</abstract><abstract lang="it">Resúmen: Los datos sobre la distribución de tipos fósiles de pólen de los Angiospermos que son comparables a los taxa recientes son evaluados en continuación de una compilación semejante publicada en 1970. Los métodos usados para fechar los sedimentos son estudiados con mucha atención. La evidencia para la presencia de 139 familias es considerada como cierta, para algunas otras familias los datos son considerados como provisionales, en espera de la acumulación de más información. Algunos datos publicados son demostrados como equivocados. En el Cretáceo inferior solamente se encuentran tipos indicativos de la presencia de plantas ancestrales a los Magnoliidae y Liliatae. En el Turoniense es evidente un aumento en la differenciación, y ésto culmina en el Maestrichtiano cuando se hallan presentes la mayoría de los taxa superiores de los Angiospermos. En el Terciario la diversificación en niveles taxonómicos inferiores continúa, y la identificatión con taxa recientes se vuelve mas segura. Los grupos herbáceos tienden a aparecer más tarde que los grupos leñosos en la sucesión estratigráfica.</abstract><abstract lang="de">Zusammenfassung: Der Rekord fossiler Pollen-Typen der Angiospermen, die mit rezenten Taxa vergleichbar sind, wird ausgewertet, ähnlich wie dies in einer bereits 1970 erschienenen Veröffentlichung geschehen ist. Besondere Aufmerksamkeit wurde der Datierung der Sedimente gewidmet. Eine Übereinstimmung wird für 139 Familien für zuverlässig gehalten, für andere Familien wird diese als vorläufig angesehen, d.h. abhängig von der Häufung von mehr Gegebenheiten in der Zukunft. Einige früher veröffentlichte Rekorde werden als irrtümlich nachgewiesen. In der unteren Kreide kommen nur Pollen-Typen vor, welche die Anwesenheit von Pflanzen zeigen, die Vorläufer von Magnoliideae und Liliatae sind. Im Turon wird eine zunehmende Differenzierung deutlich, die im Maestrichtien kulminiert, in welcher die Anwesenheit der meisten höheren Angiospermen-Taxa deutlich wird. Im Tertiär setzt sich eine Differenzierung auf einem tieferen taxonomischen Niveau fort, und die Identität mit rezenten Taxa wird gewisser. Krautige Gruppen neigen dazu, später aufzutreten als Holzpflanzen.</abstract><relatedItem type="host"><titleInfo><title>The Botanical Review</title></titleInfo><titleInfo type="abbreviated"><title>Bot. Rev</title></titleInfo><genre type="journal" displayLabel="Archive Journal"></genre><originInfo><dateIssued encoding="w3cdtf">1981-01-01</dateIssued><copyrightDate encoding="w3cdtf">1981</copyrightDate></originInfo><subject><genre>Journal-Subject-Group</genre><topic authority="SpringerSubjectCodes" authorityURI="L">Life Sciences</topic><topic authority="SpringerSubjectCodes" authorityURI="L24000">Plant Sciences</topic><topic authority="SpringerSubjectCodes" authorityURI="L24051">Plant Systematics/Taxonomy/Biogeography</topic><topic authority="SpringerSubjectCodes" authorityURI="L19112">Plant Ecology</topic><topic authority="SpringerSubjectCodes" authorityURI="L00004">Life Sciences, general</topic></subject><identifier type="ISSN">0006-8101</identifier><identifier type="eISSN">1874-9372</identifier><identifier type="JournalID">12229</identifier><identifier type="IssueArticleCount">1</identifier><identifier type="VolumeIssueCount">4</identifier><part><date>1981</date><detail type="volume"><number>47</number><caption>vol.</caption></detail><detail type="issue"><number>1</number><caption>no.</caption></detail><extent unit="pages"><start>1</start><end>142</end></extent></part><recordInfo><recordOrigin>The New York Botanical Garden, 1981</recordOrigin></recordInfo></relatedItem><identifier type="istex">1C29B8268DA04948BDAFA82BE282BA21F75A0C65</identifier><identifier type="DOI">10.1007/BF02860537</identifier><identifier type="ArticleID">BF02860537</identifier><identifier type="ArticleID">Art1</identifier><accessCondition type="use and reproduction" contentType="copyright">The New York Botanical Garden, 1981</accessCondition><recordInfo><recordContentSource>SPRINGER</recordContentSource><recordOrigin>The New York Botanical Garden, 1981</recordOrigin></recordInfo></mods></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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