SURFACE POLLEN DEPOSITION ON GLACIER FORELANDS IN SOUTHERN NORWAY I: LOCAL PATTERNS OF REPRESENTATION AND SOURCE AREA AT STORBREEN, JOTUNHEIMEN

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dc.contributor.author Pardoe H.S.
dc.date.accessioned 2025-05-02T03:57:59Z
dc.date.available 2025-05-02T03:57:59Z
dc.date.issued 2006
dc.identifier https://elibrary.ru/item.asp?id=11525854
dc.identifier.citation The Holocene, 2006, 16, 8, 1149-1161
dc.identifier.issn 0959-6836
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/49140
dc.description.abstract The relationship between vegetation and surface pollen deposition is examined at Storbreen glacier foreland where a clear plant succession exists. The aim is to determine whether the distinct plant communities present produce characteristic pollen assemblages. The influence of environmental factors is also considered. Pollen assemblages from moss polsters, collected from 22 paired sampling sites across the foreland, are compared with local vegetation. Two-way indicator species analysis and detrended correspondence analysis are employed to identify clusters and sequences, initially in the vegetation data and subsequently in the pollen data sets. Vegetation and pollen data are compared simultaneously using canonical correspondence analysis. Three main plant communities are distinguished: pioneer, heath and snowbed. Broadly, each community produces characteristic pollen assemblages. Boundaries between groups are not clear-cut, reflecting the mosaic of plant communities present. Recognition of distinct plant communities is hampered by the prevalence of long-distance arboreal pollen and poor representation of entomophillously pollinated taxa. Late in the succession up to 78% of pollen could originate locally. Use of the non-arboreal pollen sum significantly improves correspondence with vegetation. The importance of indicator taxa is considered and both Salix and Empetrum are found to distinguish successfully early phases of succession from later phases. Strong correlations exist between the primary ordination axes of vegetation and pollen and with terrain age and altitude (for example, the correlation between altitude and total land pollen Axis 1 is r= -0.76). The surface data add new information to the interpretation of tree colonization in the area during the Holocene.
dc.subject SURFACE POLLEN
dc.subject POLLEN REPRESENTATION
dc.subject PLANT SUCCESSION
dc.subject CLASSIFICATION AND ORDINATION
dc.subject RELEVANT SOURCE AREA OF POLLEN
dc.subject MOSS POLSTER
dc.subject GLACIER FORELAND
dc.subject JOTUNHEIMEN
dc.subject NORWAY
dc.subject Holocene
dc.title SURFACE POLLEN DEPOSITION ON GLACIER FORELANDS IN SOUTHERN NORWAY I: LOCAL PATTERNS OF REPRESENTATION AND SOURCE AREA AT STORBREEN, JOTUNHEIMEN
dc.type Статья
dc.identifier.doi 10.1177/0959683606069422
dc.subject.age Cenozoic::Quaternary::Holocene
dc.subject.age Кайнозой::Четвертичная::Голоцен


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