Iberomaurusian

The Iberomaurusian is a backed bladelet lithic industry found near the coasts of Morocco, Algeria, and Tunisia. It is also known from a single major site in Libya, the Haua Fteah, where the industry is known as the Eastern Oranian. The Iberomaurusian seems to have appeared around the time of the Last Glacial Maximum (LGM), somewhere between c. 25,000 and 23,000 cal BP. It would have lasted until the early Holocene, c. 11,000 cal BP. The name "Iberomaurusian" means "of Iberia and Mauretania", the latter being a Latin name for northwest Africa. Paul Maurice Pallary (1909) coined this term to describe assemblages from the site of La Mouillah in the belief that the industry extended over the strait of Gibraltar into the Iberian Peninsula. This theory is now generally discounted (Garrod 1938), but the name has persisted. In Algeria, Tunisia, and Libya, but not in Morocco, the industry is succeeded by the Capsian industry, whose origins are unclear. The Capsian is believed either to have spread into north Africa from the Near East or to have evolved from the Iberomaurusian. In Morocco and western Algeria, the Iberomaurusian is succeeded by the Cardial culture after a long hiatus.