Kalimantsia

Last updated

Kalimantsia
Temporal range: 23.03–5.33  Ma
Kalimantsia bulgarica Iz1.JPG
Kalimantsia bulgarica, Asenovgrad Paleontological Museum
KalimantsiaJF.png
Life restoration of Kalimantsia bulgarica
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Mammalia
Order: Perissodactyla
Family: Chalicotheriidae
Subfamily: Chalicotheriinae
Genus: Kalimantsia
Geraads, Spassov & Kovachev, 2001
Species:
K. bulgarica
Binomial name
Kalimantsia bulgarica
Geraads, Spassov & Kovachev, 2001

Kalimantsia is an extinct chalicothere from the Miocene of Bulgaria, Europe. It contains one species, Kalimantsia bulgarica.

Contents

Description

Kalimantsia is named for the area in which it was discovered in 2001 by Geraads, Spassov, and Kovachev. The habitat would have been quite open and the remains of Kalimantsia are accompanied by those of horses, early deer, and various carnivorous mammals. Kalimantsia has a shorter muzzle than the horse-like shapes of the rest of the chalicotheres. It also has a domed head that would have resembled those of pachycephalosaurs and the schizotheriine Tylocephalonyx . It is believed that males often competed by butting their heads together. The teeth of Kalimantsia are long and low, and well adapted for eating leaves. [1]

Size

Lifestyle

See also

Related Research Articles

<span class="mw-page-title-main">Ancylopoda</span> Extinct suborder of mammals

Ancylopoda is a group of browsing, herbivorous, mammals in the Perissodactyla that show long, curved and cleft claws. Morphological evidence indicates the Ancylopoda diverged from the tapirs, rhinoceroses and horses (Euperissodactyla) after the Brontotheria; however, earlier authorities such as Osborn sometimes considered the Ancylopoda to be outside Perissodactyla or, as was popular more recently, to be related to Brontotheriidae.

<span class="mw-page-title-main">Perissodactyla</span> Order of hoofed mammals

Perissodactyla is an order of ungulates. The order includes about 17 living species divided into three families: Equidae, Rhinocerotidae (rhinoceroses), and Tapiridae (tapirs). They typically have reduced the weight-bearing toes to three or one of the five original toes, though tapirs retain four toes on their front feet. The nonweight-bearing toes are either present, absent, vestigial, or positioned posteriorly. By contrast, artiodactyls bear most of their weight equally on four or two of the five toes: their third and fourth toes. Another difference between the two is that perissodactyls digest plant cellulose in their intestines, rather than in one or more stomach chambers as artiodactyls, with the exception of Suina, do.

<i>Moropus</i> Extinct genus of mammals

Moropus is an extinct genus of large perissodactyl mammal in the chalicothere family. They were endemic to North America during the Miocene from ~20.4–13.6 Mya, existing for approximately 6.8 million years. Moropus belonged to the schizotheriine subfamily of chalicotheres, and has the best fossil record of any member of this group; numbers of individuals, including complete skeletons, have been found.

<span class="mw-page-title-main">Chalicotherioidea</span> Extinct superfamily of mammals

Chalicotherioidea is an extinct superfamily of clawed perissodactyls that lived from the early Eocene to the early Pleistocene subepochs. Based on the fossil record they emerged and thrived largely in Eurasia, although specimens have been found in both Africa and North America. They were likely browsers that fed mainly on leaves, twigs, and other nonresistant vegetation. Many of the contained genera had derived specializations of the forelimb and manus that allowed the claws to be used as hooks for browsing and to be kept off of the ground while walking. Chalicotheres lived primarily in forested areas. Size sexual dimorphism and morphological structures such as the domed skulls of Tylocephalonyx suggest agonistic behaviour in some sort of social setting. They are related to modern day horses, rhinoceroses, and tapirs, as well as the extinct brontotheres.

In east African folklore, the Nandi bear is a creature said to live in East Africa. It takes its name from the Nandi people who live in western Kenya, in the area the Nandi Bear is reported from. It is also known as Chemosit, Kerit, Koddoelo, Ngoloko, or Duba.

<i>Stegoceras</i> Genus of pachycephalosaurid dinosaurs

Stegoceras is a genus of pachycephalosaurid (dome-headed) dinosaur that lived in what is now North America during the Late Cretaceous period, about 77.5 to 74 million years ago (mya). The first specimens from Alberta, Canada, were described in 1902, and the type species Stegoceras validum was based on these remains. The generic name means "horn roof", and the specific name means "strong". Several other species have been placed in the genus over the years, but these have since been moved to other genera or deemed junior synonyms. Currently only S. validum and S. novomexicanum, named in 2011 from fossils found in New Mexico, remain. The validity of the latter species has also been debated, and it may not even belong to the genus Stegoceras.

<span class="mw-page-title-main">Chalicotheriidae</span> Family of extinct mammals

Chalicotheriidae is an extinct family of herbivorous, odd-toed ungulate (perissodactyl) mammals that lived in North America, Eurasia, and Africa from the Middle Eocene to the Early Pleistocene. They are often called chalicotheres, a term which is also applied to the broader grouping of Chalicotherioidea. They are noted for their unusual morphology compared to other ungulates, such as their clawed forelimbs. Members of the subfamily Chalicotheriinae developed elongate gorilla-like forelimbs that are thought to have been used to grasp vegetation. They are thought to have been browsers on foliage as well as possibly bark and fruit.

<i>Chalicotherium</i> Extinct genus of mammals

Chalicotherium is a genus of extinct odd-toed ungulates of the order Perissodactyla and family Chalicotheriidae. The genus is known from Europe and Asia, from the Middle Miocene to Late Miocene.

<i>Ancylotherium</i> Extinct genus of mammals

Ancylotherium is an extinct genus of the family Chalicotheriidae, subfamily Schizotheriinae, endemic to Europe, Asia, and Africa during the Late Miocene-Early Pleistocene, existing for approximately 9.8 million years.

<i>Homalodotherium</i> Extinct genus of mammals

Homalodotherium is an extinct genus of notoungulate mammals native to South America. Fossils of Homalodotherium have been found in the Middle Miocene Santa Cruz Formation of Argentina and the Río Frías Formation of Chile.

Eomoropidae is a family of odd-toed ungulates, a group which also includes horses, rhinoceroses, and tapirs. They were most closely related to the extinct chalicotheres, which they greatly resemble, and may have been their immediate ancestors. They were, however, much smaller than the later forms, being around the size of a sheep. Like their later relatives, they were probably browsers on leaves and other soft vegetation, and, unlike most other ungulates, had claws on their feet. The Eomoropidae is most likely a paraphyletic group within Chalicotherioidea.

<span class="mw-page-title-main">Mold gold cape</span> Solid sheet-gold object from the British Bronze Age

The Mold gold cape is a ceremonial cape of solid sheet-gold from Wales dating from about 1900–1600 BC in the British Bronze Age. It was found at Bryn yr Ellyllon burial mound near Mold, Flintshire in 1833.

<i>Tylocephalonyx</i> Extinct genus of chalicothere

Tylocephalonyx is an extinct chalicothere from the Miocene of North America.

<span class="mw-page-title-main">Schizotheriinae</span> Extinct subfamily of mammals

Schizotheriines are one of the two subfamilies of the extinct family Chalicotheriidae, a group of herbivorous odd-toed ungulate (perissodactyl) mammals that lived from the Eocene to the Pleistocene. The other clade is the Chalicotheriinae. Both clades had claws rather than hooves on their front feet, an adaptation understood as related to feeding. Schizotheriines also had claws on their hind feet. The fossils of both groups are found in environments that had trees and shrubs. While chalicotheriines developed very derived body forms, schizotheriines remained basically similar in shape to other perissodactyls such as horses and tapirs. Like most forest-dwelling ungulates, they had long necks and forelimbs longer than their hindlimbs. Schizotheriines had longer, higher-crowned cheek teeth than chalicotheriines, which indicates they typically fed on tougher vegetation. The sediments where their fossils are found show they also lived in a wider range of environments, from moist forests to drier woodland or savannah-like environments with trees. Perhaps for this reason, they became more widely distributed than chalicotheriines. Though chalicotheres likely evolved in Asia, schizotheriine fossils are also found in Africa and North America, which they reached by the Bering land bridge. The best-known schizotheriine genus is Moropus. The last survivor of the group was traditionally thought to be Nestoritherium, but it was found to actually be a member of Chalicotheriinae.

<span class="mw-page-title-main">Chalicotheriinae</span> Extinct subfamily of mammals

Chalicotheriines are one of the two subfamilies of the extinct family Chalicotheriidae, a group of herbivorous, odd-toed ungulate (perissodactyl) mammals that lived from the Eocene to the Pleistocene. The other subfamily is the Schizotheriinae. Chalcotheriines evolved unique characteristics for ungulates, with very long forelimbs, short hindlimbs, and a relatively gorilla-like physique, including knuckle-walking on their flexible forelimbs, which bore long curved claws. Members of this subfamily possessed some of the longest forelimbs and shortest hindlimbs in relation to each other out of all extinct animals. Analysis of dental wear implies that most chalicotheriines fed on seeds and fruit. Their claws were likely used in a hook-like manner to pull down branches, suggesting they lived as bipedal browsers.

<i>Hippika gymnasia</i> Tournaments performed by the cavalry of the Roman Empire

The hippika gymnasia were ritual tournaments performed by the cavalry of the Roman Empire to both practice their skills and display their expertise. They took place on a parade ground situated outside a fort and involved the cavalry practicing manoeuvring and the handling of weapons such as javelins and spears. The riders and their mounts wore highly elaborate armour and helmets specially made for display purposes, decorated with images from classical mythology. Such tournaments served several purposes, improving the riders' skills, helping to build unit morale and impressing dignitaries and conquered peoples.

<span class="mw-page-title-main">Brontotheriidae</span> Extinct family of odd-toed ungulates

Brontotheriidae is a family of extinct mammals belonging to the order Perissodactyla, the order that includes horses, rhinoceroses, and tapirs. Superficially, they looked rather like rhinos with some developing bony nose horns, and were some of the earliest mammals to have evolved large body sizes of several tonnes. They lived around 56–34 million years ago, until the very close of the Eocene. Brontotheres had a Holarctic distribution, with the exception of Western Europe: they occupied North America, Asia, and Eastern Europe. They were the first fossilized mammals to be discovered west of the Mississippi, and were first discovered in South Dakota.

<span class="mw-page-title-main">Paleontology in Delaware</span> Paleontological research in the U.S. state of Delaware

Paleontology in Delaware refers to paleontological research occurring within or conducted by people from the U.S. state of Delaware. There are no local rocks of Precambrian, Paleozoic, Triassic, or Jurassic age, so Delaware's fossil record does not begin until the Cretaceous period. As the Early Cretaceous gave way to the Late Cretaceous, Delaware was being gradually submerged by the sea. Local marine life included cephalopods like Belemnitella americana, and marine reptiles. The dwindling local terrestrial environments were home to a variety of plants, dinosaurs, and pterosaurs. Along with New Jersey, Delaware is one of the best sources of Late Cretaceous dinosaur fossils in the eastern United States. Delaware was still mostly covered by sea water through the Cenozoic era. Local marine life included manatees, porpoises, seals, and whales. Delaware was worked over by glaciers during the Ice Age. The Cretaceous belemnite Belemnitella americana is the Delaware state fossil.

<span class="mw-page-title-main">History of Roman and Byzantine domes</span>

Domes were a characteristic element of the architecture of Ancient Rome and of its medieval continuation, the Byzantine Empire. They had widespread influence on contemporary and later styles, from Russian and Ottoman architecture to the Italian Renaissance and modern revivals. The domes were customarily hemispherical, although octagonal and segmented shapes are also known, and they developed in form, use, and structure over the centuries. Early examples rested directly on the rotunda walls of round rooms and featured a central oculus for ventilation and light. Pendentives became common in the Byzantine period, provided support for domes over square spaces.

<i>Hesperotherium</i> Extinct genus of chalicotheres

Hesperotherium is a genus of chalicotheres from the Early to Middle Pleistocene of China. Along with Nestoritherium, it was one of the last of the chalicotheres to ever exist. It belonged to the subfamily Chalicotheriinae, which also includes Anisodon, Chalicotherium and Nestoritherium.

References

  1. 1 2 3 Dixon, Dougal (2008). World Encyclopedia of Dinosaurs & Prehistoric Creatures . New York: Lorenz Books. pp.  453. ISBN   978-0-7548-1730-7.