In 1810, G.A. Goldfuss was the first to identify the bones of a cave lion discovered in the Zoolithenhöhle cave (Germany), naming it Felis spelaea. But it was prehistoric man who first described it in numerous parietal and movable representations. Since the beginning of the 19th century, scientific knowledge of the cave lion Panthera (Leo) spelaea has progressed steadily, establishing its leonine character. Numerous discoveries led to paleontological studies of deposits throughout Eurasia, often in caves and linked to prehistoric sites. In the 20th century, this research benefited from the emergence of new dating methods, the development of palynology and the isotopic biochemistry of collagen. As the species' range became better defined, it expanded to include the whole of Eurasia and even North America. Finally, the 21st century is marked by the development of paleogenetics and the multiplication of synthetic studies, in many countries, while benefiting from a diffusion largely facilitated by Internet exchanges and the use of English. Phylogeny of the Felidae and understanding of the origins of Panthera spelaea are progressing rapidly. Today's knowledge makes it possible to envisage a true paleobiology of this extinct species.

A preliminary description is presented of the well-preserved frozen mummies of two cubs of the extinct cave lion Panthera spelaea (finds of 2017–2018, Semyuelyakh River, Yakutia, eastern Siberia, Russia). The fossil lion cubs were found in close proximity, but they do not belong to the same litter, since their radiocarbon ages differ: the female (named ‘Sparta’) was dated to 27,962 ± 109 uncal years BP, and the male (named ‘Boris’) was dated to 43,448 ± 389 uncal years BP. The lion cubs have similar individual ages, 1–2 months. The general tone of the colour of the fur coat of Sparta is greyish to light brown, whereas, in Boris, the fur is generally lighter, greyish yellowish. It is, therefore, possible that light colouration prevailed with age in cave lions and was adaptive for northern snow-covered landscapes. The article discusses the results of computed tomography of cubs of the cave lion, the possible reasons for their death, and the peculiarities of their existence in the Siberian Arctic.

The paper presents a description of a rare finding of the partial frozen corpse of the Yukagir horse. Discovered from thawing deposits in northern East Siberia (Yakutia, Russia), its age is confirmed to be Mid-Holocene (about 4600 BP). The mummy had a preserved head with the neck and the back of the torso with the legs and tail. The Yukagir horse was relatively short, with short ears and tail. Compared to the modern breeds, including the Yakutian domestic horse, wild Przewalski’s horse, and extinct Lena horse, Equus lenensis, the Yukagir horse was closest to the latter, which was also confirmed by studies of the hair microstructure. The pollen and plant remains from the horse’s intestines indicated a preference to grasses. The late geological age of the Yukagir horse is an indication that this species survived the Pleistocene–Holocene crisis and lived through the Mid-Holocene in northern Eastern Siberia.

This article discusses recent finds of Holocene polar bear and walrus from the northern regions of Russia. The ulna of a polar bear was found on Vaygach Island and radiocarbon dated to 1,971 +/- 25 BP (OxA-23631). This calibrates to 430-540 AD, taking into account the marine reservoir effect. The size of the bone is similar to that of a recent Ursus maritimus. The locality of the fossil bone is within the modern species range, which developed about two millennia ago. In 2014 a walrus tusk was found on the coast of New Siberia Island and is radiocarbon dated to 5,065 +/- 35 BP (GrA-62452). This calibrates to 3,510-3,370 BC, taking into account the marine reservoir effect. Its size and morphology are identical to that of an adult male of the subspecies Odobenus rosmarus laptevi. This subspecies populates the eastern parts of the Kara Sea, the entire Laptev Sea and the western parts of the East Siberian Sea. This new discovery could mean that populations of O. rosmarus laptevi inhabited the waters near the New Siberian Islands during the Middle Holocene, and that the present-day coastline of the Siberian Arctic Islands was already formed at that time.

The paper presents analyses of the exterior morphology of one of the extinct and dominating species of the Late Pleistocene megafauna of Eurasia, the steppe bison, Bison priscus. The frozen mummy of the Yukagir Bison found in northern Yakutia, Russia represents the most complete specimen of this species in the world. It belongs to a young, 4.1-4.5 year old male, which dates back about 10,500 cal BP. The analyses revealed that the overall size of this specimen was comparable to a 6-year old European and American bison. Its horn spread falls within the upper limits of B. bison athabascae and B. bison bison males, as well as within the average sizes of B. priscus occidentalis from East Siberia and North America. While most of the not fully-grown Yukagir Bison body size fell within the average parameters of both grown modern species, the body and hind foot lengths were closer to the lower limits of the European bison. The color and hair pattern appeared to be close to the Blue Babe mummy (B. priscus) and modern Wood bison (modern morphotype of B. bison athabascae) and European (B. bonasus) bison. The geological age of the Yukagir Bison, along with the data from other specimens indicate that this species, which survived the Pleistocene-Holocene boundary, became rare but was still widely distributed in the northern part of centraleastern Siberia until about 8000 years ago. The juxtaposed data from arctic latitude sediments and the Bison priscus stomach content pollen indicate that it was selective grazer in the environment dominated by unfavorable shrub and forest-tundra vegetation. The scarce Holocene steppe bison remains in Eastern Siberia reflects the dramatic decrease of suitable habitats and pastures during the early Holocene climatic optimum in the high Arctic, which was a major factor of irreversible population fragmentation and decline leading to the species' extinction. (C) 2015 Elsevier Ltd and INQUA. All rights reserved.