The European fallow deer, also known as the common fallow deer or simply fallow deer, is a species of deer native to Eurasia. It is one of two living species of fallow deer alongside the Persian fallow deer. It is historically native to Turkey and possibly the Italian Peninsula, Balkan Peninsula, and the island of Rhodes near Anatolia. During the Pleistocene it inhabited much of Europe, and has been reintroduced to its prehistoric distribution by humans. It has also been introduced to other regions in the world.
The Irish elk, also called the giant deer or Irish deer, is an extinct species of deer in the genus Megaloceros and is one of the largest deer that ever lived. Its range extended across Eurasia during the Pleistocene, from Ireland to Lake Baikal in Siberia. The most recent remains of the species have been radiocarbon dated to about 7,700 years ago in western Russia. Its antlers, which can span 3.5 metres (11 ft) across are the largest known of any deer. It is not closely related to either living species called the elk, with it being widely agreed that its closest living relatives are fallow deer (Dama).
Megaloceros is an extinct genus of deer whose members lived throughout Eurasia from the Pleistocene to the early Holocene. The type and only undisputed member of the genus, Megaloceros giganteus, vernacularly known as the "Irish elk" or "giant deer", is also the best known. Fallow deer are thought to be their closest living relatives. Megaloceros has been suggested to be closely related to other genera of "giant deer", like the East Asian genus Sinomegaceros, and the European Praemegaceros.
Panthera spelaea, commonly known as the cave lion, is an extinct Panthera species that was native to Eurasia and northwest North America during the Pleistocene epoch. Genetic analysis of ancient DNA has revealed that while closely related, it was a distinct species genetically isolated from the modern lion, with the genetic divergence between the two species estimated at around 500,000 years ago. The earliest fossils of the P. spelaea lineage in Eurasia date to around 700,000 years ago. It is closely related and probably ancestral to the American lion. The species ranged from Western Europe to eastern Beringia in North America, and was a prominent member of the mammoth steppe fauna, and an important apex predator across its range. It became extinct about 13,000 years ago. It closely resembled living lions with a coat of yellowish-grey fur though unlike extant lions, males appear to have lacked manes.
The Chibanian, more widely known as the Middle Pleistocene, is an age in the international geologic timescale or a stage in chronostratigraphy, being a division of the Pleistocene Epoch within the ongoing Quaternary Period. The Chibanian name was officially ratified in January 2020. It is currently estimated to span the time between 0.7741 Ma and 0.129 Ma, also expressed as 774.1–129 ka. It includes the transition in palaeoanthropology from the Lower to the Middle Paleolithic over 300 ka.
Panthera fossilis is an extinct species of cat belonging to the genus Panthera, known from remains found in Eurasia spanning the Middle Pleistocene and possibly into the Early Pleistocene.
Cave hyena are extinct species or subspecies of hyena known from Eurasia, which ranged from Western Europe to eastern Asia and Siberia during the Pleistocene epoch. It is well represented in many European caves, primarily dating to the Last Glacial Period. It was an apex predator that preyed on large mammals, and was responsible for the accumulation of hundreds of large Pleistocene mammal bones in areas including horizontal caves, sinkholes, mud pits, and muddy areas along rivers.
Acinonyx pardinensis, sometimes called the Giant cheetah, is an extinct felid species belonging to the genus Acinonyx, closely related to the cheetah, native to Eurasia during the Pliocene and Pleistocene epochs. It was substantially larger than the living cheetah.
Leptobos is an extinct genus of large bovine, known from the Late Pliocene and Early Pleistocene of Eurasia, extending from the Iberian Peninsula to northern China. Species of Leptobos weighed on average 320 kilograms (710 lb). The dietary preference across the genus includes species that were browsers, grazers and mixed feeders. The first appearance of Leptobos in Europe around 3.6-3.5 million years ago is considered to define the beginning of the Villafranchian European faunal stage. Leptobos is considered to be closely related to the insular genus Epileptobos from the Pleistocene of Java, and is considered to be ancestral to Bison. Leptobos became extinct after being replaced by their descendant Bison during the Early Pleistocene, after a period of temporal overlap. "Leptobos" syrticus from Libya likely belongs in a different genus.
Fallow deer is the common name for species of deer in the genus Dama of subfamily Cervinae. There are two living species, the European fallow deer, native to Europe and Anatolia, and the Persian fallow deer, native to the Middle East. The European species has been widely introduced elsewhere.
Cervalces latifrons, the broad-fronted moose, or the giant moose was a giant species of deer that inhabited Europe and Asia during the Pleistocene epoch. It is thought to be the ancestor of the modern moose, as well as the extinct North American Cervalces scotti. It was considerably larger than living moose, placing it as one of the largest deer to have ever lived.
Pliocrocuta is an extinct genus of hyena. It contains the species Pliocrocuta perrieri, known from the Pliocene to Early Pleistocene of Eurasia and possibly Africa. It is possibly ancestral to Pachycrocuta. The species is estimated to have weighed around 56 kilograms (123 lb) on average, with its skull showing evidence for adaptation to bone cracking.
Pseudodama is an extinct genus of deer found in Europe during the Late Pliocene to Early Pleistocene. It has been suggested by some authors to be ancestral to Dama, with some authors choosing to subsume its species into that genus.
Praemegaceros is an extinct genus of deer, known from the Pleistocene and Holocene of Western Eurasia. Praemegaceros is considered to be a genus of "giant deer", with many species having an estimated body mass of around 400 kilograms (880 lb), considerably larger than most living deer.
Megaceroides algericus is an extinct species of deer known from the Late Pleistocene to the Holocene of North Africa. It is one of only two species of deer known to have been native to the African continent, alongside the Barbary stag, a subspecies of red deer. It is considered to be closely related to the giant deer species of Eurasia.
Sinomegaceros is an extinct genus of deer known from the Late Pliocene/Early Pleistocene to Late Pleistocene of Central and East Asia. It is considered to be part of the group of "giant deer", with a close relationship to Megaloceros. Many members of the genus are noted for their distinctive palmate antler brow tines.
Haploidoceros is an extinct genus of deer that lived in Europe during the Pleistocene. It contains a single species, Haploidoceros mediterraneus. It had a distribution limited to southern France and the Iberian Peninsula.
Gallogoral is an extinct genus of caprine that lived in Europe during the Pliocene and Pleistocene epochs.
Dama celiae is an extinct species of the genus Dama that inhabited the Iberian Peninsula during the Middle Pleistocene.
Dama roberti is an extinct species of fallow deer that lived in Europe during the early Middle Pleistocene.
