Impact of global environmental changes on the range contraction of Eurasian moose since the Late Pleistocene

被引：0

作者：

Niedzialkowska, Magdalena ^{[1
]}

Górny, Marcin ^{[1
]}

Gornia, Joanna ^{[1
]}

Popović, Danijela ^{[2
]}

Baca, Mateusz ^{[2
]}

Ratajczak-Skrzatek, Urszula ^{[3
]}

Kovalchuk, Oleksandr ^{[3
]}

Sykut, Maciej ^{[1
,30
,31
]}

Suska-Malawska, Malgorzata ^{[4
]}

Mackiewicz, Pawel ^{[5
]}

Hofman-Kamińska, Emilia ^{[1
]}

Kowalczyk, Rafal ^{[1
]}

Czarniauski, Maxim ^{[6
]}

Pawlowska, Kamilla ^{[7
]}

Makowiecki, Daniel ^{[8
]}

Tataurova, Larisa ^{[9
]}

Bondarev, Alexey ^{[10
]}

Shpansky, Andrey ^{[11
]}

Protopopov, Albert V. ^{[12
]}

Sorokin, Aleksandr Dmitrievich ^{[13
]}

Saarma, Urmas ^{[14
]}

Kosintsev, Pavel ^{[15
,16
]}

Schmölcke, Ulrich ^{[17
]}

Wilczyński, Jaroslaw ^{[18
]}

Lipecki, Grzegorz ^{[19
]}

Nadachowski, Adam ^{[18
]}

Boeskorov, Gennady G. ^{[19
]}

Baryshnikov, Gennady F. ^{[20
]}

Zorzin, Roberto ^{[21
]}

Vorobiova, Nadezhda ^{[22
]}

Moskvitina, Nina S. ^{[23
]}

Leshchinskiy, Sergey ^{[24
]}

Malikov, Dmitriy ^{[25
]}

Berdnikov, Ivan M. ^{[26
]}

Balasescu, Adrian ^{[27
]}

Boroneant, Adina ^{[27
]}

Klementiev, Alexey ^{[28
]}

Fyfe, Ralph ^{[29
]}

Woodbridge, Jessie ^{[29
]}

Stefaniak, Krzysztof ^{[3
]}

机构：

[1] Mammal Research Institute, Polish Academy of Sciences, Stoczek 1c, Bialowieża,17-230, Poland

[2] Centre of New Technologies, University of Warsaw, S. Banacha 2c, Warsaw,02-097, Poland

[3] Department of Palaeozoology, Faculty of Biological Sciences, University of Wroclaw, Sienkiewicza 21, Wroclaw,50-335, Poland

[4] Faculty of Biology, University of Warsaw, Miecznikowa 1, Warsaw,02-096, Poland

[5] Department of Bioinformatics and Genomics, Faculty of Biotechnology, University of Wroclaw, Joliot-Curie 14a, Wroclaw,50-383, Poland

[6] Institute of History of National Academy of Sciences of Belarus, Academic str. 1, Minsk,220072, Belarus

[7] Adam Mickiewicz University in Poznań, Institute of Geology, Krygowskiego 12, Poznań,61-680, Poland

[8] Nicolaus Copernicus University, Institute of Archaeology, Department of Historical Sciences, Szosa Bydgoska 44/48, Toruń,87-100, Poland

[9] Omsk Laboratory of Archeology, Ethnography and Museology of the Institute of Archeology and Ethnography, Siberian Branch of the Russian Academy of Science, Prospekt Akademika Lavrent'yeva, 17, Novosibirsk,630090, Russia

[10] Omsk Regional Branch of the Russian Geographical Society, Muzeynaya 3, Omsk,644099, Russia

[11] Department of Palaeontology and Historical Geology, Tomsk State University, Lenina prospekt 36, Tomsk,634050, Russia

[12] Mammoth Fauna Research Department, Academy of Sciences of the Republic of Sakha (Yakutia), Lenina Prospekt, 33, Yakutsk,677007, Russia

[13] Federal State Budgetary Educational Institution of Higher Education Ukhta State Technical University, Pervomayskaya St. 13, Ukhta,169300, Russia

[14] Department of Zoology, Institute of Ecology and Earth Sciences, University of Tartu, J. Liivi 2, Tartu,50409, Estonia

[15] Ural Federal University, Lenin St. 51, Ekaterinburg,620002, Russia

[16] Institute of Plant and Animal Ecology, Ural Branch of the Russian Academy of Sciences, 8 Marta str. 202, Yekaterinburg,620144, Russia

[17] Leibniz-Zentrum für Archäologie,Centre for Baltic and Scandinavian Archaeology (LEIZA-ZBSA), Schloss Gottorf, Schleswig,24837, Germany

[18] Institute of Systematics and Evolution of Animals, Polish Academy of Sciences, Slawkowska 17, Kraków,31-016, Poland

[19] Diamond and Precious Metals Geology Institute, Siberian Branch of Russian Academy of Sciences, Lenin Avenue 39, Yakutsk,677000, Russia

[20] Zoological Institute, Russian Academy of Sciences, Universitetskaya emb., 1, Saint Petersburg,199034, Russia

[21] Museo Civico di Storia Naturale di Verona, Lungadige Porta Vittoria 9, Verona,37129, Italy

[22] Institute of Molecular and Cellular Biology, Siberian Branch of the Russian Academy of Sciences, Prospekt Akademika Lavrent'yeva 8/2, Novosibirsk,630090, Russia

[23] Department of Zoology Vertebrate and Ecology, Tomsk State University, 36 Lenin Ave., Tomsk,634050, Russia

[24] Independent researcher

[25] V. S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences, Koptyuga pr. 3, Novosibirsk,630090, Russia

[26] Irkutsk State University, K. Marx st. 1, Irkutsk,664003, Russia

[27] Vasile Pârvan Institute of Archaeology, Romanian Academy, 11 Henri Coandă str., Bucarest,010667, Romania

[28] Institute of the Earth's Crust, Siberian Branch of the Russian Academy of Sciences, Ulan-Batorskaya St, 1, Irkutsk,664033, Russia

[29] School of Geography, Earth and Environmental Sciences, University of Plymouth, Portland Square, Devon, Plymouth,PL4 8AA, United Kingdom

[30] Center for Ecological Dynamics in a Novel Biosphere (ECONOVO), Department of Biology, Aarhus University, Ny Munkegade 114-116, Aarhus C,8000, Denmark

[31] Department of Archaeology and Heritage Studies, Aarhus University, Moesgård Allé 20, Højbjerg,DK-8270, Denmark

来源：

Science of the Total Environment | / 957卷

关键词：

Abiotic; -; Anthropogenic; Biotic; Invertebrates; Jurassic; Livestock;

D O I：

10.1016/j.scitotenv.2024.177235

中图分类号：

学科分类号：

摘要：

Climatic oscillations are considered primary factors influencing the distribution of various life forms on Earth. Large species adapted to cold climates are particularly vulnerable to extinction due to climate changes. In our study, we investigated whether temperature increase since the Late Pleistocene and the contraction of environmental niche during the Holocene were the main factors contributing to the decreasing range of moose (Alces alces) in Europe. We also examined whether there were significant differences in environmental conditions between areas inhabited by moose in Europe and Asia, that could support the division of moose into western and eastern forms, as suggested by genetic and morphological data. We analysed environmental conditions in the locations of 655 subfossil and modern moose occurrences over the past 50,000 years in Eurasia. We found that the most limiting climatic factor for the moose distribution since the Late Pleistocene was July temperature. More than 90 % of moose records were found in areas where mean summer temperature was below 19 °C, with July temperatures showing over 3 times narrower interquartile range compared to January temperatures. We identified significant differences in environmental conditions between areas inhabited by the European and Asiatic moose. In Europe, the species occurred in regions with milder climates, higher primary productivity, and more frequently within forest biomes compared to Asiatic individuals. The moose range shifted more in the west-east than in the south-north direction during the Holocene climate warming in Europe. We conclude that although the area of suitable moose habitat has increased since 12–8 ka years BP, as demonstrated by environmental niche modeling, the retreat of A. alces in large areas of Europe was likely caused by anthropogenic landscape change (e.g., deforestation) and overhunting by humans during the late Holocene rather than by climate warming during the Pleistocene to Holocene transition. © 2024 The Authors

引用

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