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Ca. 37,000-year-old cub of Homotherium latidens found near the Badyarikha River, Siberia.. This is a list of Ice Age species preserved as permafrost mummies.It includes all known species that have had their tissues partially preserved within the permafrost layer of the Arctic and Subarctic.
The most obvious change associated with the termination of an ice age is the increase in temperature. Between 15,000 BP and 10,000 BP, a 6 °C increase in global mean annual temperatures occurred. This was generally thought to be the cause of the extinctions.
Cave bears of the last Ice Age lacked the usual two or three premolars present in other bears; to compensate, the last molar is very elongated, with supplementary cusps. [21] The humerus of the cave bear was similar in size to that of the polar bear , as were the femora of females.
The Pleistocene (/ ˈ p l aɪ s t ə ˌ s iː n,-s t oʊ-/ PLY-stə-seen, -stoh-; [4] [5] referred to colloquially as the Ice Age) is the geological epoch that lasted from c. 2.58 million to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations.
Approximate extent of the Karoo Glaciation (in blue), over the Gondwana supercontinent during the Carboniferous and Permian periods. The late Paleozoic icehouse, also known as the Late Paleozoic Ice Age (LPIA) and formerly known as the Karoo ice age, was an ice age that began in the Late Devonian and ended in the Late Permian, [1] occurring from 360 to 255 million years ago (Mya), [2] [3] and ...
The Huronian glaciation (or Makganyene glaciation) [1] was a period where at least three ice ages occurred during the deposition of the Huronian Supergroup. Deposition of this largely sedimentary succession extended from approximately 2.5 to 2.2 billion years ago (), during the Siderian and Rhyacian periods of the Paleoproterozoic era.
The last glacial period, commonly referred to as the "Ice Age", spanned 125,000 [40] –14,500 YBP [41] and was the most recent glacial period within the current ice age, which occurred during the last years of the Pleistocene era. [40]
In 1774, Zoolithenhöhle cave near the village of Burggaillenreuth in Bavaria, southern Germany was brought to scientific attention by Johan Friedrich Esper, who realised that the bones of extinct animals were present in the cave. [9] In 1810, a fossil skull from the cave was given the scientific name Felis spelaea by Georg August Goldfuss. [10]