Megaloceros giganteus had 88lb antlers. They are known as irish elk, or in greek: μεγαλος megalos “great” κερας keras “horn, antler”

The Irish elk (Megaloceros giganteus), or giant deer is an extinct species of deer in the genus Megaloceros. It is one of the largest deer that ever lived. Its range extended across Eurasia. From Ireland, to Lake Baikal in Siberia. During the pleistocene. The most recent remains of the species have been carbon dated 7000 years ago in western Russia.

The Irish elk or ‘great horn antler’ are known from abundant skeletal remains which have been found in bogs in Ireland. Skeletons, skulls and antlers are prized ornaments, and used in aristocratic homes. The remains of Irish elk were of high value: “In 1865, full skeletons might fetch £30, while particularly good heads with antlers could cost £15.” Leeds Philosophical and Literary Society bought a full skeleton in 1847, from Glennon’s in Dublin, for £38. This specimen, discovered at Lough Gur near Limerick, is still on display at Leeds City Museum. Nearby in Ballybetagh Bog near Dublin over 100 individuals have been found.

Description largest antlers of 88lbs were about 3.65 m (12.0 ft) from tip to tip.
The Irish elk stood about 2.1 m (6 ft 11 in) tall at the shoulders. Bucks may have ranged from 450–700 kg (990–1,540 lb), with an average of 575 kg (1,268 lb). Irish elk was the heaviest known cervine (“Old World deer”). Females weighed less.

Life restoration
80% of buck size, or 460 kg (1,010 lb). Is, on average comparable to modern moose. Minus the giant horns distinguishing characteristics. Concave frontals, proportionally long braincase, proportionally short front section of the skull (orbitofrontal region), and in proportion to supporting its horns.
There teeth had an absence of upper canines and the molarisation of the lower fourth premolar. Its large antlers, could create a skull and mandible with substantial thickening (pachyostosis), and with early and complete obliteration of cranial suture.

Cave paintings dipict a colouration of great horn antler. A dark stripe running along the back, a stripe on either side from shoulder to haunch, a dark collar on the throat and a chinstrap, and a dark hump on the withers (between the shoulder blades).
It is not closely related to either of the living species currently called elk: Alces alces (the European elk, known in North America as the moose) or Cervus canadensis (the North American elk or wapiti). It was a giant deer. Phylogenetic speaking analyses support that their closest living relatives are fallow deer (Dama).

It has been historically thought that, because both have palmated antlers, the Irish elk and fallow deer are closely related, this is supported by several other morphological similarities,including the lack of upper canines, proportionally long braincase and nasal bones, and proportionally short front portion of the skull.

Species identification:
Most had been identifying the remains as elk (known as the moose in North America). Thomas Molyneux, an irish physician, was the first to describe the irish elk or “great horn antler” in 1695. By 1812, french scientist Georges Cuvier documented that the Irish elk did not belong to any species of mammal currently living, declaring it “le plus célèbre de tous les ruminans fossiles”. And, in 1827 Joshua Brookes, in a listing of his zoological collection, named the new genus Megaloceros.

Orthogenesis or natural selection versus natural selection
Before the 20th century, the Irish elk, was believed to of evolved from smaller ancestors with smaller antlers. It was taken as a prime example of orthogenesis (directed evolution), an evolutionary mechanism in which antlers became larger and larger. Opposed to Darwinian evolution, or natural selection. Where, in undeviating direction, the successive species within the lineage become in favor of survival and reproduction. The theory was claimed orthogenesis evolutionary because antlers kept growing. The species went extinct because the antlers grew to sizes which prevented eating. The animal become trapped in tree branches. Many believed Irish elk evolution proceeding in a straight line direction, void of natural selection.

In the 1930s, orthogenesis was disputed by Darwinians led by Julian Huxley, who noted that antler size was not grossly large, and was proportional to body size. Theories changed. The current and favoured view is that sexual selection was the driving force behind the large antlers rather than orthogenesis or natural selection.

Evolution giant deer polyphylectic
Antler construction suggest a close relationship between M. stavropolensis and Asian Sinomegaceros. The oldest generally accepted records of the genus are from the late Early Pleistocene. Other species often considered to belong to Megaloceros include reindeer sized M. savini, which is known from (~700,000–450,000 years ago) localities in England, France, Spain and Germany.
The exact origin of M. giganteus remains unclear, and appears to lie outside Western Europe. (~1.2 Ma), partial skeleton remain in Libakos, Greece could be closely related to M. giganteus. It is being studied.

It was not exclusive to Ireland or the United kingdom. It was named because best preserved fossil specimens were been found in lake sediments and peat bogs in Ireland. The Irish elk had a far reaching range, extending Atlantic Ocean to Lake Baikal in Siberia. They have not been identified northbound onto open mammoth steppes (like mammoth and reindeer), rather more known in the boreal steppe-woodland environments. Mostly consisting of scattered spruce and pine, as well as low-lying herbs and shrubs including grasses. Like sedges, ephedra, artemisia and other brush.
‘Great horned antler’ antlers vary widely in form depending upon the habitat, such as a compact, upright shape in closed forest environments. They likely shed their antlers and re-grew a new pair during mating season. Antlers generally require high amounts of calcium and phosphate, especially those for stags which have larger structures, and the massive antlers of Irish elk may have required much greater quantities.
The large antlers are usually explained as for male-male battle and to attract females during mating season.

Dieting and feeding
Diet based on dental wear patterns and bone specimen analysis. A pattern towards mixed feeding and grazing is suggested, but included leaf browsing and a wide range. Based on the dietary requirements of similar deer, a 675 kg (1,488 lb) lean Irish elk stag would have needed to consume 39.7 kg (88 lb) of fresh forage daily.
Assuming antler growth occurred over a span of 120 days, a stag would have required 3lb of protein daily, as well as access to nutrient and mineral dense forage starting about a month before antlers began sprouting and continuing until they had fully grown. Larger stags perhaps sought after aquatic plants in lakes, or areas of more protein and nutrients. After antlers were grown, stags could probably satisfy their nutritional requirements in productive sedge lands bordered by willow and birch forests.

The Irish elk may have been preyed upon by the large carnivores of the time, including the cave lion, and the cave hyena.

As discussed by previous scientists. Antler size decreased through the Late Pleistocene and into the Holocene, and was probably not a primary cause of extinction.
It had been said: “environmental factors, cumulatively over thousands of years, reduced giant deer populations to a highly vulnerable state. In this situation, even relatively low-level hunting by small human populations could have contributed to its extinction.”
The range of ‘great horn antler’ appears to have greatly reduced during the Last Glacial Maximum. Between 27,500 and 14,600 years ago, few remains are known. Between 23,300 and 17,500 years ago none. From hunting they were dramatically reduced after the Pleistocene-Holocene transition. It managed to survive into the early northgrippian (around 8200 year ago) in Russia and Siberia. Extending from Maloarchangelsk in the East to Preobrazhenka in the west. It is suggested that extinction was contributed to by further climatic changes transforming preferred open habitat into uninhabitable dense forest.