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dc.contributor.authorJensen, Thomas Correll
dc.contributor.authorZawiska, Izabela
dc.contributor.authorOksman, Mimmi
dc.contributor.authorSłowiński, Michał
dc.contributor.authorWoszczyk, Michał
dc.contributor.authorLuoto, Tomi P.
dc.contributor.authorTylmann, Wojciech
dc.contributor.authorNevalainen, Liisa
dc.contributor.authorObremska, Milena
dc.contributor.authorSchartau, Ann Kristin
dc.contributor.authorWalseng, Bjørn
dc.coverage.spatialScandinavia, Skandinaviaen_US
dc.date.accessioned2020-03-27T10:54:38Z
dc.date.available2020-03-27T10:54:38Z
dc.date.issued2019
dc.identifier.issn0921-2728
dc.identifier.urihttps://hdl.handle.net/11250/2649081
dc.description.abstractWe conducted a paleolimnological study to examine how changes in human activity interacted with climate to influence productivity and biodiversity over the past millennium in oligotrophic Lake Atnsjøen, SE Norway. The study included analyses of sediment geochemistry, subfossil diatoms and cladocerans, and macrofossils. Results were compared with the historical record of human activities in the catchment, pollen analysis and paleoclimate inferences from the lake. During the first 750 years of the record (1000–1750 CE), a time of relatively low human activity, lake productivity and biodiversity were strongly related to climate. During the Little Ice Age (1550–1800 CE), lake productivity and diatom diversity were constrained by cold climate. A Century of climate warming (1780–1880 CE) initiated an increase in productivity. Accelerated human settlement after 1850 CE, however, had an even stronger impact on productivity, mediated by increased agriculture and/or forestry, which led to greater nutrient loading of the lake. Similarly, diatoms in the lake responded to the rise in temperature, but increasing human activity also had a moderate impact on the diatom community, which displayed weak signs of nutrient enrichment. From 1980 to 1990 CE onwards, lake productivity declined as a consequence of a recent decrease in human activity and changing land use. The human-induced increase in lake productivity starting ca. 1850 CE propagated through the food web and increased consumer productivity, as reflected by greater accumulation rates of cladocerans, trichopterans and turbellarians. The cladoceran community was likely under top-down control of fish, as indicated by changes in size structure and diversity. Our study showed that increasing human activity during the settlement period had a stronger impact on lake productivity than did climate. Furthermore, the slight human-mediated increase in nutrient loading had different impacts on productivity and biodiversity in the study lake. This study demonstrates that even relatively small changes in human activities in watersheds can have measurable impacts on nutrient-poor lakes.en_US
dc.language.isoengen_US
dc.subjectDiatomsen_US
dc.subjectCladoceraen_US
dc.subjectMacrofossilsen_US
dc.subjectLand useen_US
dc.subjectClimateen_US
dc.subjectScandinaviaen_US
dc.titleHistorical human impact on Productivity and biodiversity in a subalpine oligotrophic lake in Scandinaviaen_US
dc.typeJournal articleen_US
dc.description.versionacceptedVersionen_US
dc.rights.holder© Springer Nature B.V. 2019en_US
dc.subject.nsiVDP::Matematikk og Naturvitenskap: 400::Zoologiske og botaniske fag: 480en_US
dc.source.volume42en_US
dc.source.journalJournal of Paleolimnologyen_US
dc.source.issue4en_US
dc.identifier.doi10.1007/s10933-019-00100-5
dc.identifier.cristin1749550


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