Abstract
Less than a half of the modern insect fauna in the northern Yukon has its origin in the Pleistocene; the other species are recent immigrants, mainly from different regions of the East Beringia. The changes resulted from destruction of the steppe-tundra environment at the Pleistocene/Holocene boundary. The origin of the recent regional insect fauna cannot be reconstructed on the sole basis of its composition.
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ACKNOWLEDGMENTS
I am grateful to my Canadian and American colleagues D. Froese, B. Jensen, G. Zazula, E. Hall, F. Calmels, R. Mac-Phee, and C. Fleming for help during fieldwork in 2007 and 2008, and to the late A. Telka who participated in collecting recent insects in the southwestern Yukon. Thanks are also due to B.M. Kataev for help with processing the lists of ground beetle species.
Funding
The field research was supported under International Polar Year (IPY) Program ID No: 292, A. Completion of this work was possible due to support from the Russian Foundation for Basic Research, project 20-04-00165.
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Kuzmina, S.A. Local Insect Fauna, History of Its Origin, and Fossil Record: an Example from the Old Crow River Basin, Northwestern Yukon, Canada. Entmol. Rev. 102, 621–638 (2022). https://doi.org/10.1134/S0013873822050062
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DOI: https://doi.org/10.1134/S0013873822050062