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Zonation may be extended as a relative dating device beyond the range of C.
Four-or five-phase models of glacial/interglacial pollen spectra have been applied in Europe and North America.
The basis for dating with pollen is the recognition of assemblages or zones, usually from the percentages of the taxa, but sometimes from pollen influx.
The determination of zones is influenced by a number of site-related variables and by preparation and analytical constraints.
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