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[49] [50] With Homo erectus ' new environmental flexibility, favourable climate fluxes likely opened it the way to the Levantine corridor, perhaps sporadically, in the Early Pleistocene. [4] There is evidence that the Mid-Pleistocene Revolution facilitated mammalian turnovers during the Late Early and Early Middle Pleistocene that may have ...
The southern route dispersal is primarily linked to the Initial Upper Paleolithic expansion of modern humans and "ascribed to a population movement with uniform genetic features and material culture" (Ancient East Eurasians), which was the major source for the peopling of the Asia–Pacific region.
The formation of 3 to 4 km (1.9 to 2.5 mi) thick ice sheets equate to a global sea level drop of about 120 m (390 ft) The Quaternary glaciation , also known as the Pleistocene glaciation , is an alternating series of glacial and interglacial periods during the Quaternary period that began 2.58 Ma (million years ago) and is ongoing.
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 ...
In biogeography, geodispersal is the erosion of barriers to gene flow and biological dispersal (Lieberman, 2005.; [1] Albert and Crampton, 2010. [2]). Geodispersal differs from vicariance, which reduces gene flow through the creation of geographic barriers. [3]
Excavation site at Dmanisi in 2007. Dmanisi is located in southern Georgia, about 85 kilometres (52.8 miles) from the country's capital, Tbilisi.It was founded as a city in the Middle Ages and has thus been a site of archaeological interest for some time, with a prominent archaeological excavation site being located within the ruins of the old city on a promontory overlooking the Mashavera and ...
Oceanic dispersal is a type of biological dispersal that occurs when terrestrial organisms transfer from one land mass to another by way of a sea crossing. Island hopping is the crossing of an ocean by a series of shorter journeys between islands, as opposed to a single journey directly to the destination.
During the Pleistocene epoch, there were at least four species of tapir on the North American continent. Along with Tapirus californicus , Tapirus merriami was found in California and Arizona, Tapirus veroensis was found in Florida, Georgia, Kansas, Missouri, and Tennessee, and Tapirus copei was found from Pennsylvania to Florida. [ 4 ]