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In the last decade, the identification of bone fragments by peptide mass fingerprinting or zooarchaeology by mass spectrometry is developing as a powerful tool in Quaternary palaeontology. The sequence of amino acids that make up the bone collagen molecule shows slight variations between taxa, which can be studied by mass spectrometry for taxonomic purposes. This requires reference databases that allow peptide identification. Although the cave bear (Ursus spelaeus Rosenmüller, 1794) is a common component in many European Pleistocene cave sites, no peptide fingerprint taxonomic study has paid special attention to this species up to now. For peptide markers in Ursidae, the most recent proposal is based on collagen obtained from a modern brown bear sample. In this work we attempt to cover this gap by studying bone collagen of cave and brown bear samples from different origins and different chronology, applying matrix-assisted laser desorption/ionisation time-of-flight mass spectrometry (MALDI TOF). We also performed an in-silico study of ursid bone collagen sequences published in databases. In our results we detected some discrepancies between the peptides obtained from both in silico and MALDI TOF analysis of fossil collagen and those published in the literature, in which we conclude that there are some misidentified peptides. The identification of skeletal remains by means of their peptide fingerprint is proving to be a powerful tool in palaeontology, which will bear greater fruit once the limitations of a technique that is in its initial stages have been overcome. [ABSTRACT FROM AUTHOR]

During the Last Glacial cycle (MIS 4 to MIS 2), the isthmic Pyrenees mountain range acted as a biogeographical barrier, effectively restricting faunal exchanges to its western and eastern terminations. The study of the composition of megaherbivore communities has revealed the transitional character of the Cantabrian region (northwest Iberian Peninsula) during the MIS 3, between western European cold faunas and southern Iberian temperate faunas. In the Catalan area (northeastern Iberian Peninsula), cold‐adapted faunas are frequently recorded during the cold pulses of MIS 3 and MIS 2, albeit to a lesser extent. In the present paper, we provide the first direct evidence of a muskox record in the Iberian Peninsula, together with a morphometric study and the results of collagen δ13C and δ15N analysis. The results reveal that the Arbreda specimen fits biometrically within the Late Holocene Umingmak specimens (Banks Island, Canada). Moreover, its isotopic values fall into the range of Late Pleistocene Mammoth steppe muskoxen, which indicates a typical ecological behaviour for muskox. Indeed, it suggests a niche partitioning of this cold‐adapted specimen in relation to other Gravettian Iberian fauna. Chronologically, this occurrence is interpreted as an isolated southward expansion of the biogeographical limits of muskox during the Greenland Stadial 4, in the latest MIS 3. [ABSTRACT FROM AUTHOR]

L’Arbreda Cave is one of the southernmost of the Reclau Caves (Serinyà, Girona, northeastern Iberian Peninsula), located between the west margin of the Pla d’Usall and the Serinyadell river, at an altitude of about 211 m a.s.l. The Pla d’Usall forms part of the Banyoles-Besalú Basin, which is bounded by Eocene and Neogene reliefs. It is filled with sediments of Plio-Pleistocene age. The cave is a shelter formed by travertine cascades with a degree of karstification, and contains sedimentary deposits ranging from the end of the Middle Pleistocene to the Early Holocene, thus constituting an important archaeo-palaeontological record for an understanding of the prehistoric occupation of northeastern Iberia. It is one of the most complete and best-dated terrestrial sequences in Iberia from the Mousterian to the Early Holocene period. In this paper we present a palaeoenvironmental and palaeoclimatic reconstruction of the sequence based on non-flying small mammals (insectivores and rodents) and pollen analyses. The environmental and climatic results, together with the absolute dating of the sequence and direct comparison with NorthGRIP δ 18 O and the sea-surface temperatures (SST) of the Alborán Sea, allow us to identify various climatic periods within our sequence: a cold period between interstadials 12 and 10 in Level I, probably interstadial 10 in Level H, the Last Glacial Maximum (LGM) in Levels C and B, the Bölling-Allerød interstadial (B/A) in Level A, and the Preboreal/Boreal (Pr/B) in the Terra Rossa Level. [ABSTRACT FROM AUTHOR]

The aim of this study is to understand the feeding habits of the cave bear, Ursus spelaeus by investigating the dental microwear patterns of 106 molars from six Late Pleistocene caves in Catalonia (Spain): Ermitons Cave, Arbreda Cave, Mollet Cave, Llenes Cave, Toll Cave, and Teixoneres Cave. Dental microwear patterns of U. spelaeus were compared with a reference collection of extant ursid species. The results show an omnivorous and carnivorous diet in all sites analyzed with both intra- and inter-site pattern variability. Unlike previous studies, here dental microwear identified more carnivorous habits for the herbivorous cave bear during the days/weeks before death. More varied and higher energy items would help to cope with the hibernation period. The variability between the samples could be due to the characteristic climatic shifts of the Late Pleistocene and to the corresponding differences in the availability of resources. [ABSTRACT FROM AUTHOR]