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dc.contributor.authorLarssen, Kari Egede
dc.coverage.spatial17124 Kragerø
dc.coverage.spatial19162 Tangen
dc.coverage.spatial18133 Sandefjord
dc.coverage.spatial15131 Bandak
dc.coverage.spatialSTANGE
dc.coverage.spatialOSLO
dc.coverage.spatialTOKKE
dc.date.accessioned2020-08-26T12:51:29Z
dc.date.available2020-08-26T12:51:29Z
dc.date.issued1961
dc.identifier.urihttps://hdl.handle.net/11250/2674727
dc.description.abstractIn 1959 an elk-horn was found in a bog in Høydalsmo, Lårdal, Telemark, about 580 m above sea level. The finder, Gunnar Aalandslid, collected samples for pollen analysis from the bog profile, from the surface down to the elk-horn level. The samples have been analysed, and an attempt has been made to correlate this very short and incomplete pollen diagram with the general climatic development of Southern Norway. At about 80 cm below the surface the more exacting tree species decline or disappear completely. This horizon probably corresponds to the deterioration in climate about half a thousand years B.C. Spruce pollen is found in a quantity only in the uppermost horizon (20 cm). Further down are found very small values, prpbably due to long-distance transport. This means that spurce migrated to Høydalsmo considerably later than to the Oslofjord region. Cultivation indicators, here Cerealia, are found in the two uppermost samples, where, furthermore, non-arboreal pollen increases at the expense of the arboreal pollen. This is obviously a result of the beginning of agriculture in the vicinity of the bog.
dc.language.isonor
dc.relation.ispartofseriesNGU (213)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectPALEONTOLOGI
dc.subjectSTRATIGRAFI
dc.subjectKLIMA
dc.subjectPLANTEGRUPPE
dc.subjectFOSSIL
dc.subjectHOLOCEN
dc.titleEt pollendiagram fra Høydalsmo, Telemark.
dc.typeJournal article
dc.description.localcode35626
dc.source.pagenumber20-28


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