Cave bear skeletons were first described in 1774 by Johann Friedrich Esper, in his book
Newly Discovered Zoolites of Unknown Four Footed Animals. While scientists at the time considered that the skeletons could belong to
apes,
canids,
felids, or even
dragons or
unicorns, Esper postulated that they actually belonged to
polar bears. Twenty years later,
Johann Christian Rosenmüller, an
anatomist at
Leipzig University, gave the species its binomial name. The bones were so numerous that most researchers had little regard for them. During
World War I, with the scarcity of
phosphate dung, earth from the caves where cave bear bones occurred was used as a source of phosphates. When the "dragon caves" in
Austria’s
Styria region were exploited for this purpose, only the skulls and leg bones were kept. Many caves in
Central Europe have skeletons of cave bears inside, such as the
Heinrichshöhle in
Hemer and the
Dechenhöhle in
Iserlohn,
Germany. A complete skeleton, five complete skulls, and 18 other bones were found inside
Kletno Bear Cave, in 1966 in
Poland. In
Romania, in a cave called
Bears' Cave, 140 cave bear skeletons were discovered in 1983. Remains assigned to "cave bears"
sensu lato from the Late Pleistocene exhibit a strong degree of morphological and size variability, and have often been assigned to their own species, including
Ursus rossicus (Eastern Europe, Central Asia and Siberia)
, Ursus ingressus (Central Europe to the Urals),
Ursus kanivetz, (Urals)
Ursus kudarensis (the Caucasus),
Ursus eremus (Central Europe, possibly a subspecies of
U. spelaeus s.s.) and
Ursus spelaeus sensu stricto (Western, Central and Southeast Europe). These populations/species show considerable genetic divergence from each other, (with genetic divergences estimated at hundreds of thousands to a million years)
Evolution Both the cave bear and the brown bear are thought to be descended from the Early Pleistocene species
Ursus etruscus. The date of
divergence between the ancestors of cave bears and brown bears has been estimated at around 1.2–1.5 million years ago. The transition between
Ursus deningeri and
Ursus spelaeus is often given as the
Last Interglacial (130-115,000 years ago), although the boundary between these forms is arbitrary, and intermediate or transitional
taxa have been proposed, e.g.
Ursus spelaeus deningeroides, while other authorities consider both taxa to be chronological variants of the same species. Cave bears found anywhere will vary in age, thus facilitating investigations into evolutionary trends. The three anterior
premolars were gradually reduced, then disappeared, possibly in response to a largely vegetarian diet. In a fourth of the skulls found in the
Conturines, the third premolar is still present, while more
derived specimens elsewhere lack it. The last remaining premolar became conjugated with the true
molars, enlarging the crown and granting it more cusps and cutting borders. This phenomenon, called
molarization, improved the
mastication capacities of the molars, facilitating the processing of tough vegetation. This allowed the cave bear to gain more energy for hibernation, while eating less than its ancestors. In 2005, scientists recovered and
sequenced the
nuclear DNA of a cave bear that lived between 42,000 and 44,000 years ago. The procedure used genomic DNA extracted from one of the animal's
teeth. Sequencing the DNA directly (rather than first replicating it with the
polymerase chain reaction), the scientists recovered 21 cave bear
genes from remains that did not yield significant amounts of DNA with traditional techniques. This study confirmed and built on results from a previous study using
mitochondrial DNA extracted from cave bear remains ranging from 20,000 to 130,000 years old. ==Description==