In the case of various ‘Ice Age’ megamalls, woolly rhino was not necessarily a resident of cool places or tundra-dominated habitats, with snow and thick snow on the ground. The Spanish specimens come from a dry, temperate habitat dominated by grasses and wide trees.
Wool rhinoceros (Quelodonta antiquityis) is an extinct species of rhizome that was prevalent throughout Europe and North Asia during the Pleistocene period and surviving until the end of the Ice Age. The genus Quelodonta means “cavity tooth”. woolly rhino was a member of the Pleistocene megafauna.
Woolly Rhino Evolution
As the last and most received member of the Pleistocene rhinoceros, wool rhinoceros adapted well to its environment. Stocky stungs and thick wool pelage make it a good fit for the conventional steppe-tundra environment throughout the Palearctic ecozone during the Pleistocene glaciation. Like the majority of rhinoceros, woolly rhino’s body plan adhered to a conservative morphology similar to the first rhinoceros seen at the end of the Eocene.
The earliest predecessors of wool rhinos probably appeared in the northern foothills of the Himalayas, about 2 million years ago in East Asia. The closest extinct name to the wool rhinoceros is Elasmotherium, which appeared in the evolutionary compound before the genus Quelodonta. These two lines were split in the first half of the Miocene.
The members of the Quelodonta were more likely to adapt to different conditions than the Elasmotheres. The early evolution of the genus probably occurred in humid places, which explains the decline of deposits of the Coledonta myosin.
The evolution of wool rhinoceroses began in a free-climate climate and adapted to winter because of climate fluctuations in the early Pleistocene in the Himalayas and in the northern regions. Other sources say that the closest group to the wool’s rhinoceros was the early Pleistocene Stefanorhinus, in particular, the species Stefanorhinus hemitichus.
Stefanorhinas, formerly known as GR, uses a method for paleoproteomics, a preserved rhinoceros of Damanisi. Age of Etruscus-Hundeshimanesis 1. It was 1.77 million years old. This refers to the anterior line associated with the aforementioned rhinoceros (Quelodonta antiquittis) and Mark’s rhinoceros (Stephanorhinus kirbergenensis). The genus Quelodonta originated in the early part of Stephaniorhinus.
For hundreds of thousands of years, the rhinoceros has lived in central China and east of the Baikal lake. It is believed that the wool rhizome originated from an earlier member of the genus Coledonta togolizensis. Another rhinoceros is also known as the ancestor of the wool rhinoceros, the Middle Pliocene of Kolodonta thaibetana.
The evolution of wool rhinoceros as a distinct species dates to the end of the Early Pleistocene about 4,000 years ago in Central Asia. From here the wool rhinoceros moved from north and west to Europe. The fur rhinoceros became one of the most common residents of Tundra-Steppe, a general representative of Megaphone.
Studies of DNA samples from 3 to 3, 000, 000 years old show that the closest relative is Sumatran rhinoceros.
The presence of rhinoceros wool is also known by mummified individuals from Siberia as well as by cave paintings. An adult wool rhinoceros was about 3 to 3.8 meters (9.8 to 12.5 feet) in length, with an estimated weight of about 1,800-22,700 kg (4,000-6,000 lb) or 2,000 kg (4,400 lb). Wool rhinoceroses can grow up to 2 meters (6.6 feet) tall; The body is thus larger or somewhat larger than the conventional white rhinoceros.
The two horns of the skull were made of keratin, the anterior horn being 61 cm (24 inches) in length,  with a small horn between the eyes. It had thick, long fur, short ears, short, thick legs and a stocky body. Cave images suggest wide dark bands between the front and back legs, but the feature is not universal and the identification of painted rhinoceros as a woolly rhinoceros is uncertain.
Its size was known only from prehistoric cave drawings until a fully preserved specimen (absent of fur and straw) was discovered in a tar hole in Ukraine’s Staruniya. An adult female specimen is now on display at the Museum of Natural History of the Polish Academy of Sciences in Krak ।w. Several frozen specimens have been found in Siberia, the last of the 20.
The rhinoceros had two horns, both male and female. The front horn reached a considerable size and was curved backwards. Its length reaches one meter or more, up to 1.4 meters, weight reaching 15 kg. The front horn had to move far beyond modern rhinoceros. A specimen found in the Kolima basin has a length of frontal horn 1.5 cm along the outer edge, 22.5 cm in base and 12.5 cm in width; The thickness in the middle was only 23mm. The second horn was 14.6। 8 cm early, 15 cm long.
The second horn was significantly shorter; Not more than half a meter. The nasal part was ossified, which is not observed in modern rhinoceros  It seems to be an adaptation to increase the pressure on the horn and the whole face when feeding. However, in females and calves, septum was often not completely ossified
The horns of woolly rhinoceros have found traces of friction with snow. The nature of the miscarriage implies that the rhinoceros often moved the head from one side to the other. This indicates that the rhinoceros dug snow with its horns and brought out the plants below.
Behavior and habitat
Restore a wool rhinoceros
Wool rhinoceros used its horn for protective purposes and to attract companions. Greenland Stadial 2 (most of the latest snow has returned to the northwest to the west, as the sea level was 125 meters (410 feet) lower than today).
Wool rhinoceroses roamed the open Duggarland and much of northern Europe and were prevalent in the cold, dry desert that later became southern England and the North Sea. Its geographical range has expanded and shrunk with alternate cold and warm cycles, forcing people to move as glaciers dwindle. Woolly rhinoceros woolly mammoths and Pleistocene megafauna existed together with the extinct large mammals. The nearest Elasmotherium was further south.
In the 21st, 3– million-year-old woolly rhino fossils were the oldest known, discovered in the cool Tibetan plateau, and meant that the general climate around the world existed during warming. They are believed to have migrated to North Asia and Europe after the onset of the Ice Age.
Little is known about the reproduction of wool rhinoceros. Compared with modern breeds, it is estimated that rhinoceros pairs are produced every 3-4 years for the shortest time required for mating. During this period, men fought each other for the rights of women. The presence of only two extracts in a woman indicates that she usually gives birth to one or at least two calves.
The pregnancy lasted about a year and a half. The calf stays with her mother for several months to two years before searching for her own separate territory, indicating that the natural breeding of wool rhinoceros was very slow – the female can only produce 6-8 calves during 20-25 years of fertility.
The development of young animals was similar to that of modern rhinoceros. The development and alteration of wool rhinoceros milk is related to the same information in white and black rhinoceros calves. However, the early life stages of wool rhinoceros are poorly studied due to the absence of a protected body of nursing calves.
Woolly Rhino Food
The controversy surrounding the choice of the correct dietary diet has long been around because past investigations have shown that both livestock and browsing methods are admirable. The paliodate of wool rhinoceroses has been reconstructed using different evidence lines. Climate restructuring indicates the desired environment as a cool and dry steppe-tundra, forming an important part of the response cycle of massive vegetarians. Pollen analysis shows the prevalence of grasses and seedlings in more complex plant mosaics.
Whitmoor hey, a strain vector biomechanical investigation of the head, abdomen and teeth of a good cold-stage individual recovered from Staffordshire, revealed muscle and dental features that favored a feed-feeding preference. In particular, the enhancement of the temporalis and neck muscles is consistent with the need to withstand the large tugging forces generated when receiving a large mouth chad from the ground. The presence of a large diastema supports this theory.
Comparison with conventional perisodactyl confirms that Coledonta was a single stomach-implanted handgun fermenter and was grown on cellulose-rich, protein-poor mice. This method of digestion required a large throughput of food and thus linked the large mouth size to the less nutritious material in the selected grass and sage.
Recent evidence suggests that in the last glacial period most of the woolly rhinos lived in the Arctic, devouring almost equal amounts of forbes such as Artemisia and Graminoid.
Like the woolly rhinoceros, many species of Pleistocene megafauna disappear during the same period. Human victims are often cited as a cause. Other theories as to the cause of extinction are related to climate change and the Hyperloads hypothesis related to the Ice Age (Q.v. Quaternary extinction phenomena).
One of the widely accepted theories is that although wool rhinoceros specialize in cold climates, it is capable of surviving in warmer climates (Shapiro). This suggests that climate change was not the only factor contributing to the extinction of the rhinoceros (Naish). Other cool-adapted species such as reindeer, muskox and witchcraft survived this climate change, and many others support the ‘overkill’ hypothesis for wool rhinoceros.
Recent radio carbon dating indicates that West Siberia had a population of as many as 8,000 BC. However, the accuracy of this date is uncertain, as a number of radio carbon plains are present nearby. The extinction does not coincide with the end of the last Ice Age, but coincides with a minor acute climate catastrophe that lasted approximately one -150 million years, marked by the Younger Dryas (GS1 – Greenland Stadial 1), glacial readings and severe global warming.
A brief break from the continued warming, after the end of the Ice Age (GS2), was thought to have cooled from earlier. Sea thermohaline circulation stopped due to large flow of fresh water thought to melt ice during warm interstadial (GI1 – Greenland Interstadial 1: ca. 16,000–11,450 14c year bp).
A late Paleolithic figure of a man carved on a rib bone in a pinhole Cave Man wool rug in Cresswell Crags, England.