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dc.contributor.authorSpeed, James David Mervyn
dc.contributor.authorEvankow, Ann
dc.contributor.authorPetersen, Tanja Kofod
dc.contributor.authorRanke, Peter Sjolte
dc.contributor.authorNilsen, Nellie Henriette
dc.contributor.authorTurner, Grace Winifred
dc.contributor.authorAagaard, Kaare
dc.contributor.authorBakken, Torkild
dc.contributor.authorDavidsen, Jan Grimsrud
dc.contributor.authorDunshea, Glenn
dc.contributor.authorHassel, Kristian
dc.contributor.authorFinstad, Anders Gravbrøt
dc.contributor.authorHusby, Magne
dc.contributor.authorHårsaker, Karstein
dc.contributor.authorKoksvik, Jan Ivar
dc.contributor.authorPrestø, Tommy
dc.contributor.authorVange, Vibekke
dc.date.accessioned2023-01-16T10:02:40Z
dc.date.available2023-01-16T10:02:40Z
dc.date.created2022-12-13T09:22:28Z
dc.date.issued2022
dc.identifier.citationEcology and Evolution. 2022, 12 (11), .en_US
dc.identifier.issn2045-7758
dc.identifier.urihttps://hdl.handle.net/11250/3043630
dc.description.abstractClimate change has dramatic impacts on ecological systems, affecting a range of ecological factors including phenology, species abundance, diversity, and distribution. The breadth of climate change impacts on ecological systems leads to the occurrence of fingerprints of climate change. However, climate fingerprints are usually identified across broad geographical scales and are potentially influenced by publication biases. In this study, we used natural history collections spanning over 250 years, to quantify a range of ecological responses to climate change, including phenology, abundance, diversity, and distributions, across a range of taxa, including vertebrates, invertebrates, plants, and fungi, within a single region, Central Norway. We tested the hypotheses that ecological responses to climate change are apparent and coherent at a regional scale, that longer time series show stronger trends over time and in relation to temperature, and that ecological responses change in trajectory at the same time as shifts in temperature. We identified a clear regional coherence in climate signal, with decreasing abundances of limnic zooplankton (on average by 7691 individuals m−3 °C−1) and boreal forest breeding birds (on average by 1.94 territories km−2 °C−1), and earlier plant flowering phenology (on average 2 days °C−1) for every degree of temperature increase. In contrast, regional-scale species distributions and species diversity were largely stable. Surprisingly, the effect size of ecological response did not increase with study duration, and shifts in responses did not occur at the same time as shifts in temperature. This may be as the long-term studies include both periods of warming and temperature stability, and that ecological responses lag behind warming. Our findings demonstrate a regional climate fingerprint across a long timescale. We contend that natural history collections provide a unique window on a broad spectrum of ecological responses at timescales beyond most ecological monitoring programs. Natural history collections are thus an essential source for long-term ecological research.en_US
dc.language.isoengen_US
dc.publisherJohn Wiley & Sons Ltden_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleA regionally coherent ecological fingerprint of climate change, evidenced from natural history collectionsen_US
dc.title.alternativeA regionally coherent ecological fingerprint of climate change, evidenced from natural history collectionsen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.source.pagenumber0en_US
dc.source.volume12en_US
dc.source.journalEcology and Evolutionen_US
dc.source.issue11en_US
dc.identifier.doi10.1002/ece3.9471
dc.identifier.cristin2092343
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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