The Iberomaurusian is a backed bladeletlithic 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 locally known as the Eastern Oranian. The Iberomaurusian seems to have appeared around the time of the Last Glacial Maximum, somewhere between c. 25,000 and 22,500 cal BP. It would have lasted until the early Holocene c. 11,000 cal BP. The name of the Iberomaurusian means "of Iberia and Mauritania". Pallary 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, but the name has stuck. 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.
Definition
Alternative names
Because the name of the Iberomaurusian implies Afro-European cultural contact now generally discounted, researchers have proposed other names:
Mouillian or Mouillan, based on the site of La Mouillah.
The Oranian, based on the Algerian region of Oran.
What follows is a timeline of all published radiocarbon dates from reliably Iberomaurusian contexts, excluding a number of dates produced in the 1960s and 1970s considered "highly doubtful". All dates, calibrated and Before Present, are according to Hogue and Barton. The Tamar Hat date beyond 25,000 cal BP is tentative.
Genetics
In 2013, Iberomaurusian skeletons from the prehistoric sites of Taforalt and Afalou were analyzed for ancient DNA. All of the specimens belonged to maternal clades associated with either North Africa or the northern and southern Mediterranean littoral, indicating gene flow between these areas since the Epipaleolithic. The ancient Taforalt individuals carried the mtDNA Haplogroup N subclades like U6 and M which points to population continuity in the region dating from the Iberomaurusian period. Loosdrecht et al. analysed genome-wide data from seven ancient individuals from the Iberomaurusian Grotte des Pigeons site near Taforalt in north-eastern Morocco. The fossils were directly dated to between 15,100 and 13,900 calibrated years before present. The scientists found that all males belonged to haplogroup E1b1b, common among Afroasiatic males. The male specimens with sufficient nuclear DNA preservation belonged to the paternal haplogroup E1b1b1a1, with one skeleton bearing the E1b1b1a1b1 parent lineage to E-V13, one male specimen belonged to E1b1b. These Y-DNA clades 24,000 years BP had a common ancestor with the Berbers and the E1b1b1b subhaplogroup that has been observed in skeletal remains belonging to the Epipaleolithic Natufian and Pre-Pottery Neolithiccultures of the Levant. Maternally, the Taforalt remains bore the U6a and M1b mtDNA haplogroups, which are common among modern Afroasiatic-speaking populations in Africa. A two-wayadmixture scenario using Natufian and modern sub-Saharan samples as reference populations inferred that the seven Taforalt individuals are best modeled genetically as of 63.5% Natufian-related and 36.5% sub-Saharan ancestry, with no apparent gene flow from the Epigravettian culture of Paleolithic southern Europe. The scientists indicated that further ancient DNA testing at other Iberomaurusian archaeological sites would be necessary to determine whether the Taforalt samples were representative of the broader Iberomaurusian gene pool.
