ABSTRACT
Insights into causes of extinction in fossil animals can contribute to an understanding of how environmental or anthropogenic processes may affect extant animals. Cave bears that went ...extinct in the late Pleistocene in Europe have been considered largely herbivorous based on tooth, skull and jaw morphology. Nitrogen and carbon isotopic composition (δ15N, δ13C) of bone collagen of many cave bears having values similar to or lower than those of coeval herbivores support an exclusive plant diet and their occurrence in habitats with denser vegetation. A complicating aspect of this hypothesis is that isotopic compositions of bulk collagen, especially those of nitrogen, could reflect environmental fluctuation as well as behavioural and physiological traits, which are not related to trophic position and so may lead to uncertainty in palaeodietary reconstruction. Here we show that δ15N analysis of individual collagen amino acids of fossil bears from Goyet Cave (Belgium) indicates that cave bears had a constant trophic position of 1.9–2.1, indicating purely herbivorous diets, while brown bears had a trophic position of 2.0–2.4, indicating a slightly more omnivorous diet. Results might support the hypothesis of the extinction of cave bear due to the inflexibility in feeding habits.
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FZAB, GIS, IJS, KILJ, NLZOH, NUK, OILJ, SAZU, SBCE, SBMB, UL, UM, UPUK
In this paper we performed stable isotope analysis on bone collagen of 81 samples from at least 39 brown bears (Ursus arctos) dating from Late Pleistocene to nowadays, that lived in the western of ...the Cantabrian Mountains. To interpret the data obtained we compared brown bear stable isotope signatures with those of cave bears (Ursus spelaeus), red deer (Cervus elaphus), and humans (Homo sapiens) from the same area. We observed that the diet of cave bears and brown bears in the Cantabrian Mountains was based on vegetable matter, although their different isotopic signatures suggest different ecological niches: wooded lowlands for the cave bear and steep highlands with scarce tree cover for the brown bear. In the Holocene brown bear maintains isotopic signatures similar to the Pleistocene ones in spite of the climatic tempering, which seems to be related to an even greater displacement toward the uplands due to a greater anthropic pressure in the ecosystem.
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GEOZS, IJS, IMTLJ, KILJ, KISLJ, NLZOH, NUK, OILJ, PNG, SAZU, SBCE, SBJE, UL, UM, UPCLJ, UPUK, ZRSKP
The diet of the cave bear (Ursus spelaeus) is a controversial topic, as different paleobiological approaches (e.g. dental wear, isotopic biochemistry, skull morphometrics) result in different dietary ...inferences for the cave bear, ranging from carnivory to pure herbivory. Here, we review the main results obtained from these approaches, with special emphasis on those obtained from the morphometric analyses of the cave bear craniodental skeleton. Then, we compute a between-group Principal Components Analysis from a set of 3D-landmarks digitized on 103 mandibles of living bears and extinct cave bears and using a phylomorphospace approach. Moreover, we also reconstructed the evolutionary trajectory of the cave bear mandible from the hypothetical shape of its inferred ancestor. Our results indicate that the mandible of the cave bear possess specific traits indicative of a highly-herbivorous diet or, at least, more herbivorous than their closest living relative, the brown bear (Ursus arctos). Moreover, we also propose new directions for future research to obtain more detailed inferences on the potential food resources consumed by the cave bear being crucial to understand the 'life and death' of this vanished animal.
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BFBNIB, DOBA, GIS, IJS, IZUM, KILJ, KISLJ, NUK, PILJ, PNG, SAZU, UILJ, UKNU, UL, UM, UPUK
Few members of the Pleistocene megafauna have been as extensively studied as cave bears. Multidisciplinary research into cave bears has provided insights into their morphology, ecology, and ...evolution. Genetic studies have profited from the availability of large numbers of well-preserved remains. As a result, 'ancient DNA (aDNA)' from cave bears has provided significant insights into cave bear ecology, phylogeography and even potential causes of their extinction. Here I review the contributions that genetic research has made to our understanding of cave bear biology and evaluate the potential that new, genomic tools provide to shed further light onto how these iconic representatives of the Pleistocene megafauna lived and died.
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BFBNIB, DOBA, GIS, IJS, IZUM, KILJ, KISLJ, NUK, PILJ, PNG, SAZU, UILJ, UKNU, UL, UM, UPUK
The lower molar (m1) of cave bears from Late Pleistocene localities of the Urals was studied employing the methods of traditional morphometry and geometric morphometrics. On the basis of the size and ...shape variation of m1, the small cave bear (
Ursus
ex gr.
savini-rossicus
) was found to have been a part of the faunas from the caves Skazka, Viasher, Dynamitnaya, Chudesnitsa, and Chernye Kosti. The small cave bear presence in faunas from the Medvezhya, Makhnevskaya Ledyanaya, Asha 1, Ignat’evskaya, and Barsuchii Dol caves was confirmed as well. The species range of the small cave bear encompassed the Northern, Middle, and Southern Urals in the Late Pleistocene. The ranges of the small cave bear and cave bear (
Ursus kanivetz
) overlapped from the beginning (marine isotope stage 5e) to the middle (middle marine isotope stage 3) of the Late Pleistocene.
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EMUNI, FIS, FZAB, GEOZS, GIS, IJS, IMTLJ, KILJ, KISLJ, MFDPS, NLZOH, NUK, OILJ, PNG, SAZU, SBCE, SBJE, SBMB, SBNM, UKNU, UL, UM, UPUK, VKSCE, ZAGLJ
The article presents the findings of the paleoparasitological analysis of coprolites from the cave bear (
Ursus kanivetz
Vereshchagin, 1973). The material for research was obtained during excavations ...in the Ignatievskaya Cave (Southern Urals, Russia; 54°53′ N 57°46′ E). The deposits with coprolites date back to the middle of the Late Pleistocene (90 000–30 000 years ago). On the basis of the paleoparasitological analysis, eggs of the nematode characteristic of representatives of Ursidae, namely,
Baylisascaris transfuga
Rudolphi, 1819, have been established to be present in the coprolites. The eggs are well preserved and have not lost their morphological features. The large cave bear was infested by the nematode
B. transfuga
. This is the first find of the nematode
B. transfuga
in Pleistocene-aged sediments and the first find of parasites in coprolites of the cave bear.
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EMUNI, FIS, FZAB, GEOZS, GIS, IJS, IMTLJ, KILJ, KISLJ, MFDPS, NLZOH, NUK, OILJ, PNG, SAZU, SBCE, SBJE, SBMB, SBNM, UKNU, UL, UM, UPUK, VKSCE, ZAGLJ
Remains of a cave bear were studied from a new locality in the Prokoshev Cave in the Middle Urals (58°13´ N, 58°12´ E). Bones from all regions of the skeleton are present, bones are intact and ...without traces of human or animal activity. They all belong to the cave bear (
Ursus kanivetz
Vereshchagin, 1973). An AMS radiocarbon date of 53 375 ± 765 BP, IGAN
AMS
–8632, was obtained from an adult mandible. The bones belonged to at least 18 individuals, including 4 individuals aged about one year, 1 aged about two years, 1 aged about three years, and 12 individuals over four years of age. Three skulls belonged to males and seven skulls belonged to females. The analysis has shown that the taphonomic type of this locality is a “mass burial.” This is the first “mass burial” of the cave bear in the Urals, found in situ, untouched by humans.
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EMUNI, FIS, FZAB, GEOZS, GIS, IJS, IMTLJ, KILJ, KISLJ, MFDPS, NLZOH, NUK, OILJ, PNG, SAZU, SBCE, SBJE, SBMB, SBNM, UKNU, UL, UM, UPUK, VKSCE, ZAGLJ
The Sobrarbe-Pirineos UNESCO Global Geopark shows an extremely well-developed underground karst relief as a result of the great abundance and thickness of its limestone formations. The most important ...Pleistocene vertebrate site within the Geopark is Coro Tracito Cave at Tella. The fossil association is made up exclusively of bones belonging to Ursus spelaeus from the upper Pleistocene, accumulated over several thousand years. Based on scientific analysis of the fossil bones, an interesting public outreach project has been organized, involving the refurbishment of the site within the cave and the creation of a permanent exhibition called the Tella Cave Bear Museum. These two infrastructures are visited by thousands of tourists each year and constitute the main geoscientific tourist attraction of the Sobrarbe-Pirineos Geopark.
The proposed dietary pattern of extinct Late Pleistocene cave bears (Ursus spelaeus Rosenmüller, 1794) has become controversial, as some authors have suggested that they were strictly vegetarian, ...whereas others maintain they were omnivores that at times ate large amounts of animal protein. We evaluated these alternatives by compiling stable isotope data of carbon (δ¹³C) and nitrogen (δ¹⁵N) from the bone collagen of adult European cave bears from the Late Pleistocene (Marine Isotopic Stage 3). The data include previously published analyses and additional data from the southeastern European (Carpathian) sites of Cioclovina, Muierii, Oase, and Urşilor. The cave bear isotopic values from bone collagen were compared with those from hair keratin occurring in grizzly bears (Ursus arctos horribilis Ord, 1815) collected from 1989 to 2009 in the western United States (Yellowstone National Park). The Yellowstone bears have access to a wide diversity of plants and animals, such that their diets can range from vegetarian to carnivorous. Thus, there was considerable δ¹³C and δ¹⁵N variation among the grizzly bear isotopic values, and the cave bear isotopic variation was encompassed within the overall grizzly bear isotopic distribution. More importantly, the δ¹⁵N distributions, reflecting principally trophic level, were not different between the cave bears and the grizzly bears; the cave bear values are, on average, slightly higher or lower than those of the grizzly bears, depending on the criteria for inclusion in the comparisons. It is therefore no longer appropriate to view Late Pleistocene cave bears as strictly or even predominantly vegetarian but as flexible omnivores within their diverse communities.
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DOBA, IZUM, KILJ, NUK, PILJ, PNG, SAZU, SIK, UILJ, UKNU, UL, UM, UPUK
In this issue, we cover an exceptional topic in Vertebrate Paleobiology that has been an enjoyable challenge for scientists and the popular media alike: the life and death of the Pleistocene cave ...bear (Ursus spelaeus). As an icon of the ice-age, the cave bear inhabited the glacial ecosystems of Eurasia, and it was the inspiration of a popular book written in 1976 by Björn Kurtén, entitled The cave bear story: life and death of a vanished animal. Although 'The life and death' was a summary of the knowledge acquired on cave bear biology at that time, four decades later, many aspects of its palaeoecology, extinction and evolution are still a matter of debate. With this volume, we aim to bring together the most recent research on cave bear biology in order to provide an update on the palaeoecology, biogeography, systematics, and phylogeny of this recently extinct ursine bear. We thus organised a symposium on the 1st of August 2017 as part of the three-day Annual Meeting of the European Association of Vertebrate Palaeontologists (EAVP) in Munich, Germany, that was an additional opportunity to announce the volume and to discuss this exciting subject face-to-face among specialists.
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