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dc.contributor.authorHjelle, Kari Loe
dc.contributor.authorHalvorsen, Lene Synnøve
dc.contributor.authorPrøsch-Danielsen, Lisbeth
dc.contributor.authorSugita, Shinya
dc.contributor.authorPaus, Aage
dc.contributor.authorKaland, Peter Emil
dc.contributor.authorMehl, Ingvild Kristine
dc.contributor.authorOverland, Anette
dc.contributor.authorDanielsen, Randi
dc.contributor.authorHøeg, Helge Irgens
dc.contributor.authorMidtbø, Inger
dc.date.accessioned2019-06-05T10:40:30Z
dc.date.available2019-06-05T10:40:30Z
dc.date.issued2018-05
dc.PublishedHjelle KL, Halvorsen LS, Prøsch-Danielsen L, Sugita S, Paus A, Kaland PE, Mehl IKM, Overland A, Danielsen R, Høeg HI, Midtbø I. Long-term changes in regional vegetation cover along the west coast of southern Norway: The importance of human impact. Journal of Vegetation Science. 2018;29(3):404-415eng
dc.identifier.issn1654-1103
dc.identifier.issn1100-9233
dc.identifier.urihttps://hdl.handle.net/1956/19875
dc.description.abstractQuestions: How open was the landscape prior to agriculture? Did agriculture start earlier in the south than in the north? How did the vegetation change in different regions after the introduction of agriculture? Location: Coast of SW and W Norway. Methods: The REVEALS (Regional Estimates of VEgetation Abundance from Large Sites) model is applied for pollen‐based vegetation reconstruction in 19 time windows over the last 9,000 years. Pollen data from 63 sites (lakes and bogs) are compiled and systematically used for data analysis so that the structure of vegetation change in space and time is captured. Results: Estimated cover of selected trees, shrubs, Calluna, graminids and herbs indicate a partly open outer coast throughout the Holocene. The highest tree cover is estimated for 8,200–6,200 cal. BP. Broad‐leaved trees (Fraxinus, Quercus, Tilia and Ulmus) spread from south to north and were present in the whole region at the end of the Mesolithic (5,950 cal. BP). Larger spatial variation in tree cover and a step‐wise reduction in deciduous trees after 5,700 cal. BP is concordant with increases in open‐land taxa indicating human activity. Vegetation changes caused by agriculture are indicated in the very south from ca. 5,950 cal. BP. Distinct human‐induced vegetation changes with spatial differentiation took place from 4,200 to 1,700 cal. BP, when most of the areas earlier covered by deciduous woodland had been transformed to cultivated fields, grasslands and heathlands. Increased Poaceae cover from 1,700 cal. BP probably reflects the expansion of mown meadows in addition to pastures. Conclusions: Capturing continuous changes of vegetation structure in space and time elucidates open areas along the western coast prior to the introduction of agriculture. Agriculture started earliest in the very south and spread rapidly along the whole coast prior to the Late Neolithic. Differences within the study area have existed in all time periods, reflecting different land‐use practices adapted to different natural conditions.en_US
dc.language.isoengeng
dc.publisherWileyeng
dc.subjectanthropogenic impacteng
dc.subjectcultivated fieldseng
dc.subjectforest covereng
dc.subjectgrasslandseng
dc.subjectheathlandseng
dc.subjectHoloceneeng
dc.subjectlong-term vegetation changeseng
dc.subjectpalaeoecologyeng
dc.subjectpollen analysiseng
dc.subjectREVEALS modeleng
dc.titleLong-term changes in regional vegetation cover along the west coast of southern Norway: The importance of human impacteng
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.date.updated2019-03-19T09:08:04Z
dc.description.versionpublishedVersion
dc.rights.holderCopyright 2018 International Association for Vegetation Scienceeng
dc.identifier.doihttps://doi.org/10.1111/jvs.12626
dc.identifier.cristin1605661
dc.source.journalJournal of Vegetation Science


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