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    <skos:prefLabel xml:lang="en">POLLEN</skos:prefLabel>
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related concept uuid: fe06f678-7155-4f93-9e28-4c083d60cccc
relationship type: null
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    <skos:changeNote>Date=2024-10-24 User Id=tstevens Entity=Definition Operation=UPDATE Field=reference 
System Note=update Definition
Old Value=Jackson, J.A. 1997. Glossary of Geology, 4th edition. American Geological
Institute
Bradley, R.S. 1999. Paleoclimatology: Recnstructing Climates of the Quaternary,
2nd ed. Harcourt Academic Press.
New Value=Jackson, J.A. 1997. Glossary of Geology, 4th edition. American Geological
Institute
Bradley, R.S. 1999. Paleoclimatology: Recnstructing Climates of the Quaternary,
2nd ed. Harcourt Academic Press.</skos:changeNote>
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    <skos:changeNote>Date=2024-10-24 User Id=tstevens Entity=WeightedRelation Operation=INSERT 
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    <gcmd:reference gcmd:text="Jackson, J.A. 1997. Glossary of Geology, 4th edition. American Geological Institute Bradley, R.S. 1999. Paleoclimatology: Recnstructing Climates of the Quaternary, 2nd ed. Harcourt Academic Press." xml:lang="en"/>
    <skos:definition xml:lang="en">Pollen are several-celled microgametophyte of seed plants enclosed in amicrospore wall. Fossil pollen consists entirely of the microspore wall. Thestudy of pollen is called palynology or pollen analysis and is an importantaspect in reconstructing past climates. Paleoclimatic reconstructions by pollenanalysis is possible because (1) pollen grains possess morphologicalcharacteristics that are specif to a particular genus or species of plant; (2)they are produced in vast quantities by wind-pollinated plants and aredistributed widely from their source; (3) they are extremely resistant todecay; and (4) they reflect the natural vegetation at the time of pollendeposition, which can yield information about ast climatic conditions.</skos:definition>
    <dcterms:modified>2024-10-24 11:08:28.0</dcterms:modified>
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