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=====Acheulean out of Africa===== Mode 2 is first known out of Africa at '[[Ubeidiya prehistoric site|Ubeidiya]], Israel, a site now on the [[Jordan River]], then frequented over the long term (hundreds of thousands of years) by [[Homo]] on the shore of a variable-level palaeo-lake, long since vanished. The geology was created by successive "transgression and regression" of the lake<ref>{{harvnb|Belmaker|2006|p=9}}</ref> resulting in four cycles of layers. The tools are located in the first two, Cycles Li (Limnic Inferior) and Fi (Fluviatile Inferior), but mostly in Fi. The cycles represent different ecologies and therefore different cross-sections of fauna, which makes it possible to date them. They appear to be the same faunal assemblages as the Ferenta Faunal Unit in Italy, known from excavations at Selvella and Pieterfitta, dated to 1.6β1.2 mya.<ref>{{harvnb|Belmaker|2006|pp=119β120}}</ref> At 'Ubeidiya the marks on the bones of the animal species found there indicate that the manufacturers of the tools butchered the kills of large predators, an activity that has been termed "scavenging".<ref>{{harvnb|Belmaker|2006|p=149}}</ref> There are no living floors, nor did they process bones to obtain the marrow. These activities cannot be understood therefore as the only or even the typical economic activity of Hominans. Their interests were selective: they were primarily harvesting the meat of [[Cervid]]s,<ref>{{harvnb|Belmaker|2006|p=147}}</ref> which is estimated to have been available without spoiling for up to four days after the kill. The majority of the animals at the site were of "Palaearctic biogeographic origin".<ref>{{harvnb|Belmaker|2006|p=67}}</ref> However, these overlapped in range on 30β60% of "African biogeographic origin".<ref>{{harvnb|Belmaker|2006|p=21}}</ref> The [[biome]] was Mediterranean, not savanna. The animals were not passing through; there was simply an overlap of normal ranges. Of the Hominans, ''H. erectus'' left several cranial fragments. Teeth of undetermined species may have been ''H. ergaster''.<ref>{{harvnb|Belmaker|2006|p=20}}</ref> The tools are classified as "Lower Acheulean" and "Developed Oldowan". The latter is a disputed classification created by [[Mary Leakey]] to describe an Acheulean-like tradition in Bed II at [[Olduvai Gorge|Olduvai]]. It is dated 1.53β1.27 mya. The date of the tools therefore probably does not exceed 1.5 mya; 1.4 is often given as a date. This chronology, which is definitely later than in Kenya, supports the "out of Africa" hypothesis for Acheulean, if not for the Hominans. [[File:Biface (trihedral) Amar Merdeg, Mehran, Ilam, Lower Paleolithic, National Museum of Iran.jpg|thumb|upright=.8|Biface (trihedral) from [[Amar Merdeg]] at [[Zagros]] foothill, [[Ilam, Iran|Ilam]], National Museum of Iran]] From Southwest Asia, as the Levant is now called, the Acheulean extended itself more slowly eastward, arriving at [[Isampur]], India, about 1.2 mya. It does not appear in China and Korea until after 1mya and not at all in Indonesia. There is a discernible boundary marking the furthest extent of the Acheulean eastward before 1 mya, called the [[Movius Line]], after its proposer, [[Hallam L. Movius]]. On the east side of the line the small flake tradition continues, but the tools are additionally worked Mode 1, with flaking down the sides. In Athirampakkam at [[Chennai]] in [[Tamil Nadu]] the Acheulean age started at 1.51 mya and it is also prior than North India and Europe.<ref>{{cite web|title=Acheulian stone tools discovered near Chennai|url=http://www.hindu.com/2011/03/25/stories/2011032564021300.htm|archive-url=https://web.archive.org/web/20110823111619/http://www.hindu.com/2011/03/25/stories/2011032564021300.htm|url-status=dead|work=[[The Hindu]]|date=2011-03-25|archive-date=2011-08-23}}</ref> The cause of the Movius Line remains speculative, whether it represents a real change in technology or a limitation of archeology, but after 1 mya evidence not available to Movius indicates the prevalence of Acheulean. For example, the Acheulean site at Bose, China, is dated 0.803Β±3K mya.<ref>{{cite web | title=Bose, China | work=What Does It Mean to be Human? | publisher=Smithsonian National Museum of Natural History | url=http://humanorigins.si.edu/research/asian-research/bose-china| date=28 January 2010 }}</ref> The authors of this chronologically later East Asian Acheulean remain unknown, as does whether it evolved in the region or was brought in. There is no named boundary line between Mode 1 and Mode 2 on the west; nevertheless, Mode 2 is equally late in Europe as it is in the Far East. The earliest comes from a rock shelter at Estrecho de QuΓpar in Spain, dated to greater than 0.9 mya. Teeth from an undetermined Hominan were found there also.<ref>{{cite journal | first=Rex | last=Dalton | title=Europe's oldest axes discovered | journal=Nature News | date=2 September 2009 | url=http://www.nature.com/news/2009/090902/full/news.2009.878.html | doi=10.1038/news.2009.878}}</ref> The last Mode 2 in Southern Europe is from a deposit at Fontana Ranuccio near [[Anagni]] in Italy dated to 0.45 mya, which is generally linked to ''[[Homo cepranensis]]'', a "late variant of ''H. erectus''", a fragment of whose skull was found at Ceprano nearby, dated 0.46 mya.<ref>{{cite journal | journal=Earth and Planetary Science Letters | volume=286 | issue=1β2 | year=2009 | pages=255β268 | doi=10.1016/j.epsl.2009.06.032 |author=Giovanni Muttoni | title=Pleistocene magnetochronology of early hominid sites at Ceprano and Fontana Ranuccio, Italy | url=http://www.rci.rutgers.edu/~dvk/dvk_REPRINTS/Muttoni+2009b.pdf|display-authors=etal | bibcode=2009E&PSL.286..255M}}</ref>
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