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The present phylogeographic pattern of red deer in Eurasia is not only a result of the contraction of their distribution range into glacial refugia and postglacial expansion, but probably also an effect of replacement of some red deer s.l. mtDNA lineages by others during the last 50 000 years. To better recognize this process, we analysed 501 sequences of mtDNA cytochrome b , including 194 ancient and 75 contemporary samples newly obtained for this study. The inclusion of 161 radiocarbon-dated samples enabled us to study the phylogeny in a temporal context and conduct divergence-time estimation and molecular dating. Depending on methodology, our estimate of divergence between Cervus elaphus and Cervus canadensis varied considerably (370 000 or 1.37 million years BP, respectively). The divergence times of genetic lineages and haplogroups corresponded to large environmental changes associated with stadials and interstadials of the Late Pleistocene. Due to the climatic oscillations, the distribution of C. elaphus and C. canadensis fluctuated in north–south and east–west directions. Some haplotypes dated to pre-Last Glacial Maximum periods were not detected afterwards, representing possibly extinct populations. We indicated with a high probability the presence of red deer sensu lato in south-eastern Europe and western Asia during the Last Glacial Maximum. [ABSTRACT FROM AUTHOR]

The present distribution of many species is a result of climatic changes during the Pleistocene and human activity. The impact of climate has been accompanied by restrictions of populations into refugia during glacial periods, and subsequent expansions during more favourable conditions, whereas human influence has been associated with hunting practices and translocations. One mammalian species that has been subject to such transformations is the red deer, Cervus elaphus, but the exact nature of these changes has been difficult to determine using only modern DNA. In this study, we obtained new cytochrome b sequences from subfossil remains of deer found in the Crimean Peninsula. A comparison of these sequences with the available recent and ancient sequences allowed to us to reconstruct phylogeographic relationships between Cervus lineages and to determine their potential migration routes at both local and Eurasian scales. Our analyses showed that the Crimean Peninsula was not a glacial refugium for red deer, but rather that red deer colonized Crimea in three independent waves from both Western and Eastern red deer populations. The immigrations were related to local extinctions and replacements of native populations. [ABSTRACT FROM AUTHOR]

This work summarises the state of the art of the studies on the fossil cervids of Poland, from the Miocene through to the present, with an extensive reference to the faunas of the rest of Eurasia and the World. It deals with more than 5500 remains of 16 species from 68 localities. The study intends to give an overview on the taxa present in Poland. The primary focus is on the evolution and stages of dispersal of Cervidae in the frame of the environmental changes that took place across Central Europe. The authors propose to place the bioevents of cervids in the Western European Plio-Pleistocene mammalian biochronological framework, which includes the Ruscinian, Villafranchian, Galerian and Aurelian Mammal Ages. The cervid remains are shown to have great biochronological significance. [ABSTRACT FROM AUTHOR]

The Pleistocene lion Panthera spelaea was not a homogenous taxon; it was represented by three chronoforms. The oldest one, from the Early and Middle Pleistocene, was P. s. fossilis , the youngest was the Late Pleistocene cave lion P. s. spelaea. The intermediate form between them was P. s. intermedia. The scarcity of stratigraphically old lion made it difficult to understand the evolution of this carnivore. Therefore, we revised the fossil material of the Pleistocene lion from Polish excavation sites. The analysis revealed the presence of P. s. fossilis in 7 sites: Tunel Wielki, Południowa, Wschodnia, Draby, Biśnik, Deszczowa and Wierzchowska Górna caves. The remains from these localities significantly differed in their average size and teeth proportions from the nominate younger chronoform, i.e. the cave lion. Using this material and all other available data, we compared the lion remains grouped into four palaeoclimate periods: MIS 17-12, MIS 11-9, MIS 8-6 and MIS 5-2. We found significant time-related trends in many morphometric features of dentition and limb bones. Between the first two periods, the lion became larger but from MIS 8, it gradually decreased in size. The teeth showed a much greater rate of changes than the metapodial bones, which in turn were characterised by more heterogeneous and mosaic evolution. The changes observed in the fossil material can result from in situ evolution of lion populations occupying Europe or immigration and replacement of the native forms by those from other regions, for example Asia. • P. s. fossilis differs from P. s. spelaea in larger size and teeth proportions. • Remains of P. s. fossilis are known in Poland from Tunel Wielki, Południowa, Draby, Biśnik and Wierzchowska Góra caves. • Dental features occurred more diagnostic and demonstrated more significant differences than the tarsal and metapodial bones. • The largest fraction of statistically discriminative traits had canine, P4, p4 and interestingly metatarsus V. • Generally, most measurements decreased over time, which indicates that the lion became smaller. • The limb bones usually increased in size and thickness, which could be relate to the better adaptation to confrontation with large preys. [ABSTRACT FROM AUTHOR]