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dc.contributor.authorMeiri, M.en
dc.contributor.authorLister, A.en
dc.contributor.authorKosintsev, P.en
dc.contributor.authorZazula, G.en
dc.contributor.authorBarnes, I.en
dc.date.accessioned2021-08-31T14:57:37Z-
dc.date.available2021-08-31T14:57:37Z-
dc.date.issued2020-
dc.identifier.citationPopulation dynamics and range shifts of moose (Alces alces) during the Late Quaternary / M. Meiri, A. Lister, P. Kosintsev, et al. — DOI 10.1111/jbi.13935 // Journal of Biogeography. — 2020. — Vol. 47. — Iss. 10. — P. 2223-2234.en
dc.identifier.issn3050270-
dc.identifier.otherFinal2
dc.identifier.otherAll Open Access, Hybrid Gold3
dc.identifier.otherhttps://www.scopus.com/inward/record.uri?eid=2-s2.0-85088438725&doi=10.1111%2fjbi.13935&partnerID=40&md5=19b783da1b338d5c6784271eb438d7d3
dc.identifier.otherhttps://onlinelibrary.wiley.com/doi/pdfdirect/10.1111/jbi.13935m
dc.identifier.urihttp://elar.urfu.ru/handle/10995/101484-
dc.description.abstractAim: Late Quaternary climate oscillations had major impacts on species distributions and abundances across the northern Holarctic. While many large mammals in this region went extinct towards the end of the Quaternary, some species survived and flourished. Here, we examine population dynamics and range shifts of one of the most widely distributed of these, the moose (Alces alces). Location: Northern Holarctic. Taxon: Moose (A. alces). Methods: We collected samples of modern and ancient moose from across their present and former range. We assessed their phylogeographical relations using part of the mitochondrial DNA in conjunction with radiocarbon dating to investigate the history of A. alces during the last glacial. Results: This species has a relatively shallow history, with the most recent common ancestor estimated at ca. 150–50 kyr. Ancient samples corroborate that its region of greatest diversity is in east Asia, supporting proposals that this is the region of origin of all extant moose. Both eastern and western haplogroups occur in the Ural Mountains during the last glacial period, implying a broader contact zone than previously proposed. It seems that this species went extinct over much of its northern range during the last glacial maximum (LGM) and recolonized the region with climate warming beginning around 15,000 yr bp. The post-LGM expansion included a movement from northeast Siberia to North America via Beringia, although the northeast Siberian source population is not the one currently occupying that area. Main conclusions: Moose are a relatively recently evolved species but have had a dynamic history. As a large-bodied subarctic browsing species, they were seemingly confined to refugia during full-glacial periods and expanded their range northwards when the boreal forest returned after the LGM. The main modern phylogeographical division is ancient, though its boundary has not remained constant. Moose population expansion into America was roughly synchronous with human and red deer expansion. © 2020 The Authors. Journal of Biogeography published by John Wiley & Sons Ltden
dc.description.sponsorshipWe warmly thank the following museums, curators and people for access to samples: the late Andrei Sher, Severtsov Institute, Moscow; Andy Currant, Natural History Museum, London; Alfred Gardner, Smithsonian, Washington DC; R. Dale Guthrie, University of Alaska, Fairbanks; John de Vos, National Museum of Natural History (Naturalis), Leiden; Eileen Westwig, American Museum of Natural History, NY; Fyodor Shidlovsky, Ice-Age Museum, Moscow; Tong Haowen, Institute of Vertebrate Palaeontology and Paleoanthropology, Beijing; Mammoth Museum, Yakutsk; Geological Museum, Yakutsk; Paleontological Institute, Moscow; Royal Alberta Museum, Edmonton; Zoological Institute, Saint Petersburg; Museum of the Institute of Plant and Animal Ecology, Ekaterinburg. We thank our Yukon First Nation research partners for their continued support for our work on the ice age fossils of Yukon Territory. We are grateful to the placer gold mining community and the Tr'ond?k Hw?ch'in First Nation for their continued support and partnership with our research in the Klondike goldfields region; and the Vuntut Gwitchin First Nation for their collaboration with research in the Old Crow region. We would also like to thank Shai Meiri for help in drawing the map and useful discussion, Tony Stuart for access to radiocarbon dates, and Iris van Pijlen for laboratory assistance. This research was funded by NERC grant NE/G00269X/1 through the European Union FP7 ERA-NET program BiodivERsA. Funding for AMS dating was provided through NERC/AHRC/ORAU Grant NF/2008/2/15.en
dc.format.mimetypeapplication/pdfen
dc.language.isoenen
dc.publisherBlackwell Publishing Ltden
dc.rightsinfo:eu-repo/semantics/openAccessen
dc.sourceJ. Biogeogr.2
dc.sourceJournal of Biogeographyen
dc.subjectALCES ALCESen
dc.subjectANCIENT DNAen
dc.subjectLAST GLACIAL MAXIMUMen
dc.subjectMITOCHONDRIAL DNAen
dc.subjectMOOSEen
dc.subjectQUATERNARYen
dc.subjectCOMMON ANCESTRYen
dc.subjectDEERen
dc.subjectEXTINCTIONen
dc.subjectGEOGRAPHICAL DISTRIBUTIONen
dc.subjectHOLARCTIC REGIONen
dc.subjectLAST GLACIALen
dc.subjectLAST GLACIAL MAXIMUMen
dc.subjectOSCILLATIONen
dc.subjectPHYLOGEOGRAPHYen
dc.subjectPOPULATION DYNAMICSen
dc.subjectQUATERNARYen
dc.subjectRADIOCARBON DATINGen
dc.subjectRANGE EXPANSIONen
dc.subjectRANGE SIZEen
dc.subjectSURVIVALen
dc.subjectBERING ISLANDen
dc.subjectFAR EASTen
dc.subjectKAMCHATKAen
dc.subjectKOMANDORSKI ISLANDSen
dc.subjectNORTH AMERICAen
dc.subjectRUSSIAN FEDERATIONen
dc.subjectSIBERIAen
dc.subjectURALSen
dc.subjectALCES ALCESen
dc.subjectCERVUS ELAPHUSen
dc.subjectMAMMALIAen
dc.titlePopulation dynamics and range shifts of moose (Alces alces) during the Late Quaternaryen
dc.typeArticleen
dc.typeinfo:eu-repo/semantics/articleen
dc.typeinfo:eu-repo/semantics/publishedVersionen
dc.identifier.doi10.1111/jbi.13935-
dc.identifier.scopus85088438725-
local.contributor.employeeMeiri, M., The Steinhardt Museum of Natural History and Israel National Center for Biodiversity Studies, Tel Aviv University, Tel Aviv, Israel
local.contributor.employeeLister, A., Department of Earth Sciences, Natural History Museum, London, United Kingdom
local.contributor.employeeKosintsev, P., Institute of Plant and Animal Ecology, Urals Branch of the Russian Academy of Sciences, Ekaterinburg, Russian Federation, Ural Federal University, Ekaterinburg, Russian Federation
local.contributor.employeeZazula, G., Palaeontology Program, Department of Tourism and Culture, Government of Yukon, Whitehorse, YK, Canada, Collections and Research, Canadian Museum of Nature, Ottawa, ON, Canada
local.contributor.employeeBarnes, I., Department of Earth Sciences, Natural History Museum, London, United Kingdom
local.description.firstpage2223-
local.description.lastpage2234-
local.issue10-
local.volume47-
local.contributor.departmentThe Steinhardt Museum of Natural History and Israel National Center for Biodiversity Studies, Tel Aviv University, Tel Aviv, Israel
local.contributor.departmentDepartment of Earth Sciences, Natural History Museum, London, United Kingdom
local.contributor.departmentInstitute of Plant and Animal Ecology, Urals Branch of the Russian Academy of Sciences, Ekaterinburg, Russian Federation
local.contributor.departmentUral Federal University, Ekaterinburg, Russian Federation
local.contributor.departmentPalaeontology Program, Department of Tourism and Culture, Government of Yukon, Whitehorse, YK, Canada
local.contributor.departmentCollections and Research, Canadian Museum of Nature, Ottawa, ON, Canada
local.identifier.pure14155592-
local.identifier.puree900323c-4848-4bc9-9b0b-a720587f4c9cuuid
local.identifier.eid2-s2.0-85088438725-
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