The species diversity of lamellicorn beetles (Coleoptera, Scarabaeoidea) on the 20 islands of Peter the Great Gulf was considered and analyzed for the first time, where 83 species from 38 genera were identified. There are 60 species (72.3%) and 20 genera (52.6%) are new for the fauna of the islands, with reference to the literature data. The total fauna with Russky Island (21 islands) includes 87 species from 38 genera of 13 subfamilies and four families of the superfamily Scarabaeoidea. The diversity and degree of study of the group on individual islands is very uneven. Russky Island with 80 species (92% of the total fauna of 21 islands), Popov Island with 42 species (48.3%) and Putyatin Island with 39 species (44.8%) have the most species-rich fauna. On the islands of Kozlov, Rikord, Zheltukhin, and Durnovo, one species was recorded (1.1%). The Scarabaeidae Latreille, 1802 is dominates the fauna of 21 islands—77 species (88.5%), other families are represented by a single species: Trogidae Macleay, 1819—5 species (5.7%), Lucanidae Latreille, 1804—3 species (3.5%), Geotrupidae Latreille, 1802—2 species (2.3%). Scarabaeinae with 15 species (19.5%), Aphodiinae Leach, 1815 with 14 species (18.2%), and Rhizotroginae with 13 species (16.9%) are dominant in the Scarabaeidae fauna. The article deals with the annotated list of species and the studied material, discusses the ecological and zoogeographical features of the local faunas of Scarabaeoidea and features of the faunagenesis of the study area. The local Scarabaeoidea faunas of the islands are characterized by a significant depletion and mosaic composition of the species composition in comparison with the continental fauna. Despite the peculiarity of the climatic conditions of the islands and their significant isolation from the continental coast, the insular faunas of Scarabaeoidea demonstrate a high degree of similarity to the area, and have a logical structure with the continental fauna of lamellicorn beetles due to the geological youth of the island. The islands appeared during the post-Pleistocene transgression of the sea 11 to 8.5 thousand years ago.
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