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The extinctions during the Late Pleistocene are differentiated from previous extinctions by its extreme size bias towards large animals (with small animals being largely unaffected), and widespread absence of ecological succession to replace these extinct megafaunal species, [3] and the regime shift of previously established faunal ...
Pliocene–Pleistocene boundary extinction: 2 Ma: Possible causes include a supernova [7] [8] or the Eltanin impact [9] [10] Middle Miocene disruption: 14.5 Ma Climate change due to change of ocean circulation patterns. Milankovitch cycles may have also contributed [11] Paleogene: Eocene–Oligocene extinction event: 33.9 Ma
Macrauchenia became extinct as part of the end-Pleistocene extinction event at the end of the Late Pleistocene, around 12–10,000 years ago, along with most large mammals native to the Americas. The extinctions followed the arrival of humans in the Americas , [ 34 ] which in South America occurred at least 14,500 years ago (as evidenced by ...
The Late Pleistocene is an unofficial age in the international geologic timescale in chronostratigraphy, also known as the Upper Pleistocene from a stratigraphic perspective. It is intended to be the fourth division of the Pleistocene Epoch within the ongoing Quaternary Period. It is currently defined as the time between c. 129,000 and c ...
Biological taxa that went extinct during the Pleistocene epoch of geologic time, between 2.58 million and 11.7 thousand years ago, during the early Quaternary Period of the Cenozoic Era See also the preceding Category:Pliocene extinctions and the succeeding Category:Holocene extinctions
The holotype specimen was recovered from Poço Azul, an underwater cave system in Nova Redenção, Bahia state.(The same cave also yielded remains of another extinct sloth species, Ahytherium.)
Equus mauritanicus, the Saharan zebra, is an extinct species of equine which lived in North Africa during the Late Pleistocene and possibly the Holocene, as recently as 6,000 years ago. E. mauritanicus has in the past been considered synonymous with the living plains zebra (E. quagga) , but examination of several skulls show it to be distinct.
Bubalus palaeokerabau is an extinct species of water buffalo that was endemic to Java during the Late Pleistocene.. B. palaeokerabau can be distinguished from more recent domestic water buffalo introduced to Java by their larger size and their extremely long horns, which can be around 2.5 m (8.2 ft) long from tip to tip.
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