Please use this identifier to cite or link to this item: https://hdl.handle.net/2440/85886
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dc.contributor.authorHill, R.S.en
dc.date.issued1981en
dc.identifier.citationNew Zealand Journal of Botany, 1981; 19(2):241-242en
dc.identifier.issn0028-825Xen
dc.identifier.issn1175-8643en
dc.identifier.urihttp://hdl.handle.net/2440/85886-
dc.description.abstractLong-distance dispersal of plant macrofossils is a commonly recognised phenomenon, but in most fossil assemblages it is difficult to determine its extent. Long-distance dispersal will probably affect any analysis based on foliar physiognomy (leaf size and margin type), particularly if it causes species from more than one vegetation type to be present in the assemblage. Mbre serious objections to the use of foliar physiognomy, particularly for estimating palaeoclimates and vegetation types, arc the frequent over-abundance of streamand lake-side plants in deposits and the current lack of knowledge of the representation of surrounding vegetation in depositional sites.en
dc.description.statementofresponsibilityRobert S. Hillen
dc.language.isoenen
dc.publisherRoyal Society of New Zealanden
dc.rightsCopyright status unknownen
dc.subjectmacrofossils; long-distance dispersal; palaeoclimates; Tertiary; Quaternaryen
dc.titleConsequences of long-distance dispersal of plant macrofossilsen
dc.typeJournal articleen
dc.identifier.doi10.1080/0028825X.1981.10425123en
pubs.publication-statusPublisheden
dc.identifier.orcidHill, R.S. [0000-0003-4564-4339]en
Appears in Collections:Ecology, Evolution and Landscape Science publications

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