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dc.creatorNiedzialkowska, Magdalena
dc.creatorDoan, Karolina
dc.creatorGorny, Marcin
dc.creatorSykut, Maciej
dc.creatorStefaniak, Krzysztof
dc.creatorPiotrowska, Natalia
dc.creatorJedrzejewska, Bogumila
dc.creatorRidush, Bogdan
dc.creatorPawelczyk, Slawomira
dc.creatorMackiewicz, Pawel
dc.creatorSchmoelcke, Ulrich
dc.creatorKosintsev, Pavel
dc.creatorMakowiecki, Daniel
dc.creatorCharniauski, Maxim
dc.creatorKrasnodebski, Dariusz
dc.creatorRannamaee, Eve
dc.creatorSaarma, Urmas
dc.creatorArakelyan, Marine
dc.creatorManaseryan, Ninna
dc.creatorTitov, Vadim V.
dc.creatorHulva, Pavel
dc.creatorBalasescu, Adrian
dc.creatorFyfe, Ralph
dc.creatorWoodbridge, Jessie
dc.creatorTrantalidou, Katerina
dc.creatorDimitrijević, Vesna
dc.creatorKovalchuk, Oleksandr
dc.creatorWilczynski, Jaroslaw
dc.creatorObada, Theodor
dc.creatorLipecki, Grzegorz
dc.creatorArabey, Alesia
dc.creatorStanković, Ana
dc.date.accessioned2021-10-12T13:32:25Z
dc.date.available2021-10-12T13:32:25Z
dc.date.issued2021
dc.identifier.issn0305-0270
dc.identifier.urihttp://reff.f.bg.ac.rs/handle/123456789/3323
dc.description.abstractAim The Expansion-Contraction model has been used to explain the responses of species to climatic changes. During periods of unfavourable climatic conditions, species retreat to refugia from where they may later expand. This paper focuses on the palaeoecology of red deer over the past 54 ka across Europe and the Urals, to reveal patterns of change in their range and explore the role of environmental conditions in determining their distribution. Location Europe and western Asia to 63 degrees E. Taxon Red deer (Cervus elaphus). Methods We collected 984 records of radiocarbon-dated red deer subfossils from the Late Pleistocene and the Holocene, including 93 original dates. For each deer sample we compiled climatic and biome type data for the corresponding time intervals. Results During the last 54 ka changes in red deer range in Europe and the Urals were asynchronous and differed between western and eastern Europe and western Asia due to different environmental conditions in those regions. The range of suitable areas for deer during the Last Glacial Maximum (LGM) was larger than previously thought and covered vast regions not only in southern but also in western and eastern Europe. Throughout the period investigated the majority of specimens inhabited forests in the temperate climatic zone. The contribution of forests in deer localities significantly decreased during the last 4 ka, due to deforestation of Europe caused by humans. Mean January temperature was the main limiting factor for species distribution. Over 90% of the samples were found in areas where mean January temperature was above -10 degrees C. Main conclusions Red deer response to climatic oscillations are in agreement with the Expansion-Contraction model but in contradiction to the statement of only the southernmost LGM refugia of the species. During the last 54 ka red deer occurred mostly in forests of the temperate climatic zone.en
dc.publisherWiley, Hoboken
dc.relationEuropean Social Fund (ESF) [UDAPOKL.04.01.01-00-072/09-00]
dc.relationUniversity of Wroclaw [0410/2990/18]
dc.relationInstitute of Environmental Biology, University of Wroclaw [0410/2990/18]
dc.relationMammal Research Institute Polish Academy of Sciences
dc.relationNarodowe Centrum Nauki National Science Centre, Poland [DEC-2013/11/B/NZ8/00888, UMO-2016/23/B/HS3/00387]
dc.relationRomanian National Authority for Scientific Research, UEFISCDI, Grant/Award Number: PN-IIIP4-IDPCE-2016-0676
dc.relationNational Centre for Atmospheric Science, UK
dc.relationCentre for Environmental Data Analysis, UK
dc.relationLeverhulme Trust [F00568W]
dc.rightsrestrictedAccess
dc.sourceJournal of Biogeography
dc.subjectungulatesen
dc.subjecttemperate climatic zoneen
dc.subjectradiocarbon datingen
dc.subjectpalaeoecologyen
dc.subjectLast Glacial Maximum refugiaen
dc.subjectJanuary temperatureen
dc.subjectHoloceneen
dc.subjectforest habitaten
dc.subjectexpansion-contraction modelen
dc.subjectenvironmental niche modellingen
dc.titleWinter temperature and forest cover have shaped red deer distribution in Europe and the Ural Mountains since the Late Pleistoceneen
dc.typearticle
dc.rights.licenseARR
dc.citation.epage159
dc.citation.issue1
dc.citation.other48(1): 147-159
dc.citation.rankM21~
dc.citation.spage147
dc.citation.volume48
dc.identifier.doi10.1111/jbi.13989
dc.identifier.scopus2-s2.0-85092404576
dc.identifier.wos000579027300001
dc.type.versionpublishedVersion


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