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Dmanisi

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Parent: Eurasia Hop 4
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Dmanisi
NameDmanisi
Map typeGeorgia
Coordinates41, 20, 10, N...
TypeSettlement
EpochsLower Paleolithic
CulturesOldowan
Excavations1936, 1983–present
ArchaeologistsDavid Lordkipanidze, Abesalom Vekua
ConditionRuined

Dmanisi. The archaeological site is a pivotal location for understanding early human dispersal out of Africa. Situated in the Kvemo Kartli region of Georgia, it has yielded an extraordinary collection of early hominin fossils and Oldowan stone tools. The findings have fundamentally reshaped scientific perspectives on the timing, anatomy, and behavior of the first hominins to colonize Eurasia.

Discovery and excavation

Initial investigations at the site in the 1930s, led by archaeologists like Vakhtang Chichinadze, focused on the medieval ruins atop a basalt promontory. Systematic paleontological work began in the 1980s after the discovery of extinct fauna, prompting a joint expedition by the Georgian National Museum and the Römisch-Germanisches Zentralmuseum. The landmark discovery of a hominin mandible, D 211, in 1991 by Anton Justus and David Lordkipanidze shifted the focus entirely to the underlying Pleistocene deposits. Subsequent decades of excavation, under the continued direction of Lordkipanidze and Abesalom Vekua, have revealed a rich stratigraphic sequence within the volcanic ash layers beneath the Dmanisi Sioni Cathedral.

Significance in human evolution

The site provides the earliest unequivocal evidence of hominins outside Africa, dating to approximately 1.8 million years ago. This discovery challenged previous models that linked the initial exodus from Africa solely with advanced Acheulean technology and larger-brained hominins. The relatively small-brained, small-bodied individuals, equipped with simple Oldowan tools, demonstrate that the first pioneers possessed the behavioral flexibility to adapt to diverse Palearctic environments. This has fueled major debates about taxonomic diversity and whether the fossil assemblage represents a single, variable population of early Homo erectus.

Dmanisi hominins

The hominin assemblage includes five remarkably well-preserved skulls, several mandibles, and numerous postcranial elements representing adolescents and adults. The most complete specimens, such as Skull 3 (D2700/D2735) and the toothless elderly individual represented by Skull 4 (D3444/D3900), provide an unprecedented snapshot of growth, variation, and potential social care. The morphology shows a mosaic of primitive features reminiscent of Homo habilis and derived traits characteristic of Homo erectus, leading some paleoanthropologists like G. Philip Rightmire to classify them as Homo georgicus. The fossils are housed and studied at the Georgian National Museum in Tbilisi.

Associated fauna and paleoenvironment

The bone-rich layers contain a diverse paleontological record of over 40 species of extinct mammals, birds, and reptiles. Key fauna include the saber-toothed cat Homotherium, the giant short-faced hyena Pachycrocuta, the Etruscan wolf, and numerous herbivores like the Etruscan rhinoceros, a primitive bovid, and the ostrich. This paleoecological community indicates a mosaic environment of open steppe grassland with forested river valleys, similar to modern East African savannas. The presence of both carnivores and evidence of hominin butchery on animal bones suggests competition and scavenging opportunities at this Paleolithic site.

Dating and geological context

The site is precisely constrained chronologically by a combination of paleomagnetic studies, radiometric techniques, and biostratigraphy. The fossil-bearing strata lie between two basalt flows; the underlying Mashavera Basalt has been dated by potassium-argon methods, while argon-argon dating of volcanic ash layers within the site consistently yields an age of 1.8 million years. This correlates with the Olduvai normal polarity subchron, confirming the early Pleistocene age. The rapid burial by volcanic ash from eruptions in the nearby Javakheti volcanic highland contributed to the exceptional preservation of the fossils.