Cervalces latifrons Temporal range: Early to Late Pleistocene | |
---|---|
Pair of antlers from the Geological-Paleontological Museum, Aalen | |
Scientific classification | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Chordata |
Class: | Mammalia |
Order: | Artiodactyla |
Family: | Cervidae |
Subfamily: | Capreolinae |
Genus: | † Cervalces |
Species: | †C. latifrons |
Binomial name | |
†Cervalces latifrons Johnson, 1874 | |
Synonyms | |
Cervalces latifrons, the broad-fronted moose, or the giant moose [3] 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. [4]
Cervalces latifrons was first described by Mr Randall Johnson in 1874. [5] A frontal bone attached to part of an antler of a previously unknown species of deer was found at low tide on the beachfront at Happisburgh, Norfolk, in the "Forest Bed". Johnson, who retained the specimen in his collection, named it Cervus latifrons, [6] Cervus being the only genus of deer known at that time. The specific name "latifrons" refers to the wide frontal bone of this large species. The morphology of the animal as deduced from this fossil and from others later found in this formation and in continental Europe differs little from modern moose. It was later placed in the genus Cervalces which it shares with the also extinct Cervalces scotti from North America. [7]
The antlers of the males had longer beams than living moose, with large vertically-oriented flat palmate lobes with a variable number of points. It has been suggested that due to their shape, it is unlikely that they were used for combat. [8] The average sized Cervalces latifrons was quite a bit more massive than other large moose-like deer, such Cervalces scotti, the largest races of the extant moose and the Irish elk (Megaloceros giganteus), despite some overlap in shoulder height, and is the largest deer ever known to exist. C. latifrons is estimated to have reached 2.1 m (6 ft 11 in) [7] [9] to 2.4 m (7 ft 10 in) high at the shoulder. [3] Body mass of C. latifrons was around 1,000 kg (2,200 lb), putting it around 30% heavier than C. scotti. In some cases, this species could have weighed perhaps up to 1,200 kg (2,600 lb) with the largest specimens perhaps reaching 2.5 m (8.2 ft) at the shoulder. [10] [11] It was about the same mass and far taller than a modern bull American bison (Bison bison) and could have weighed about twice as much as the Irish elk (Megaloceros giganteus) but is much less well known to the general public, probably because the span of its antlers at 2.5 m (8 ft 2 in) was smaller than that of the Irish elk. [7] [9] In comparison to the modern moose, the nares are not retracted and are similar to those of other deer. It is unclear whether C. latifrons had a prehensile upper lip like living moose.
Fossil remains of this deer are known from northern Europe and Asia but have not been found in the Iberian Peninsula, Italy south of the Apennines, Croatia or Greece. [3] In the United Kingdom, it is known only from the Cromer Forest Bed Formation. This is exposed at intervals along the coast of Norfolk and Suffolk and forms low cliffs between Cromer and Great Yarmouth. The holotype came from here. It is believed that Cervalces latifrons resembled its modern moose relations and lived in tundra, steppes, coniferous forests and swamps. It probably avoided deciduous forests because of the inconvenience that would be caused by its wide antlers when moving among bushes and saplings. Like its living relatives, it is likely to have lived a solitary life. It is believed to have fed on rough herbage and plants growing around lakes and swamps. [7] Further remains of Cervalces latifrons have been recovered from Sénèze (Haute-Loire, France), Mauer (Baden-Württemberg, Germany), Bilshausen (Niedersachsen, Germany), Mosbach (Hessen, Germany), Süßenborn (Thüringen, Germany), Ranica (Lombardy, Italy), Leffe (Lombardy, Italy) and Crostolo Creek (Emilia-Romagna, Italy) [12] and extensively from Siberia. [9]
Cervalces latifrons first appeared during the late Early Pleistocene. [3] Probably during the Middle Pleistocene, it entered North America, giving rise to Cervalces scotti . [13] In Europe, Cervalces latifrons became extinct around the end of the Middle Pleistocene and beginning of the Late Pleistocene, being replaced by its descendant the modern moose. [4]
A palaeobotanical study was made of clay found inside the skull of a specimen of Cervalces latifrons found at Fornaci di Ranica in northern Italy dating back to the early Pleistocene. The site was fluvial deposits in the basin of the Serio River. The infrared spectrum of the clay and the pollen grains found in it were compared with a previously available chronological sequence of pollens from sediments in the area. The results suggest that the vegetation in the region at the time in which the moose lived consisted of sparse coniferous forests with Pinus sylvestris and Pinus mugo , steppes and grassland. In the immediate vicinity, it correlated with a retreat of forest cover and an increase in herbaceous ground cover. The valley bottoms probably had standing water, marsh vegetation, moist meadows, bushes and flowering plants. [12] A morpho-functional analysis of Cervalces latifrons comparing it with its modern deer relatives, Cervus spp., suggests similarities in diet and in adaptations for living in a marshy environment with scattered scrub and debris. [12]
Cervalces latifrons shares many anatomical features with its living relative, the moose (British English "elk", Alces alces) with similarities in its grinding molars, narrow jaw, large mouth cavity, elongated muzzle and premaxillary bones. It is likely to have had a similar diet of bark, leaves and shoots of trees such as willow, aspen, rowan, birch, oak, larch and pine. It would also have grazed herbaceous vegetation in the boggy areas on the floors of valleys. Its limbs were long and show adaptations allowing for locomotion at a fast trot known as "stilt-locomotion". This involves a long stride with a high elevation of the feet at each step. This gait is helpful for moving through bogs or deep snow. The toes could be spread widely which would have aided swimming and prevented the foot sinking deeply when walking in marshy conditions. [7]
The moose or elk is the world's tallest, largest and heaviest extant species of deer and the only species in the genus Alces. It is also the tallest, and the second-largest, land animal in North America, falling short only of the American bison in body mass. Most adult male moose have broad, palmate antlers; other members of the deer family have pointed antlers with a dendritic ("twig-like") configuration. Moose inhabit the circumpolar boreal forests or temperate broadleaf and mixed forests of the Northern Hemisphere, thriving in cooler, temperate areas as well as subarctic climates.
A deer or true deer is a hoofed ruminant ungulate of the family Cervidae. Cervidae is divided into subfamilies Cervinae and Capreolinae. Male deer of almost all species, as well as female reindeer, grow and shed new antlers each year. These antlers are bony extensions of the skull and are often used for combat between males.
The elk is a large antlered mammal within the deer family.
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.
The Cervinae or the Old World deer, are a subfamily of deer. Alternatively, they are known as the plesiometacarpal deer, due to having lost the parts of the second and fifth metacarpal bones closest to the foot, distinct from the telemetacarpal deer of the Capreolinae.
The elk, or wapiti, is the second largest species within the deer family, Cervidae, and one of the largest terrestrial mammals in its native range of North America and Central and East Asia. The word "elk" originally referred to the European variety of the moose, Alces alces, but was transferred to Cervus canadensis by North American colonists.
Libralces was a genus of Eurasian deer that lived during the Pliocene epoch. Its main claim to fame is its 2+ meter wide antlers, comparable in size to those of Megaloceros.
Cervalces scotti, also known as stag-moose, is an extinct species of large deer that lived in North America during the Late Pleistocene epoch. It is the only known North American member of the genus Cervalces. Its closest living relative is the modern moose.
Six species of deer are living wild in Great Britain: Scottish red deer, roe deer, fallow deer, sika deer, Reeves's muntjac, and Chinese water deer. Of those, Scottish red and roe deer are native and have lived in the isles throughout the Holocene. Fallow deer have been reintroduced twice, by the Romans and the Normans, after dying out in the last ice age. The other three are escaped or released alien species. Moose were also formerly native to Britain, before dying out during the mid-Holocene, over 5,000 years ago. The comparably sized Irish elk, which has the largest antlers of any deer was also formerly native to Britain until becoming extinct in region around 12,000 years ago.
The Capreolinae, Odocoileinae, or the New World deer are a subfamily of deer. Alternatively, they are known as the telemetacarpal deer, due to their bone structure being different from the plesiometacarpal deer subfamily Cervinae. The telemetacarpal deer maintain their distal lateral metacarpals, while the plesiometacarpal deer maintain only their proximal lateral metacarpals. The Capreolinae are believed to have originated in the Middle Miocene, between 7.7 and 11.5 million years ago, in Central Asia.
Odocoileus lucasi, known commonly as the American mountain deer, is an extinct species of North American deer.
Rucervus is a genus of deer from India, Nepal, Indochina, and the Chinese island of Hainan. The only extant representatives, the barasingha or swamp deer and Eld's deer, are threatened by habitat loss and hunting; another species, Schomburgk’s deer, went extinct in 1938. Deer species found within the genus Rucervus are characterized by a specific antler structure, where the basal ramification is often supplemented with an additional small prong, and the middle tine is never present. The crown tines are inserted on the posterior side of the beam and may be bifurcated or fused into a small palmation.
There are at least 14 large mammal and 50 small mammal species known to occur in Glacier National Park.
Fallow deer is the common name for species of deer in the genus Dama of subfamily Cervinae.
The Alaska moose, or Alaskan moose in Alaska, or giant moose and Yukon moose in Canada, is a subspecies of moose that ranges from Alaska to western Yukon. The Alaska moose is the largest subspecies of moose. Alaska moose inhabit boreal forests and mixed deciduous forests throughout most of Alaska and most of Western Yukon. Like all moose subspecies, the Alaska moose is usually solitary but sometimes will form small herds. Typically, they only come into contact with other moose for mating or competition for mates. Males and females select different home ranges during different seasons. This leads to spatial segregation throughout much of the year. While males and females are spatially separate the habitat that they occupy is not significantly different. During mating season, in autumn and winter, male Alaska moose become very aggressive and prone to attacking when startled.
Cervalces is an extinct deer genus that lived during the Pliocene and Pleistocene epochs. Cervalces gallicus is either classified as a species of the related Libralces, or an ancestral species to other members of Cervalces. It lived in Europe from the Pliocene to the Pleistocene. Cervalces scotti, the stag-moose, lived in Pleistocene North America. Cervalces latifrons, the broad-fronted moose, and Cervalces carnutorum were found in Pleistocene Europe and Asia. The genus has been suggested to be paraphyletic and ancestral with respect to Alces, the genus which contains the modern moose, and as such, some authors synonymise Cervalces with Alces.
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.
Alceini is a tribe of deer, containing the extant genus Alces and the extinct genera Cervalces and Libralces.
{{cite book}}
: CS1 maint: multiple names: authors list (link){{cite journal}}
: Cite journal requires |journal=
(help)