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Bartolini-Lucenti S, Cirilli O, Pandolfi L, Bernor RL, Bukhsianidze M, Carotenuto F, Lordkipanidze D, Tsikaridze N, Rook L. Zoogeographic significance of Dmanisi large mammal assemblage. J Hum Evol 2021; 163:103125. [PMID: 34954399 DOI: 10.1016/j.jhevol.2021.103125] [Citation(s) in RCA: 6] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/03/2021] [Revised: 11/23/2021] [Accepted: 11/23/2021] [Indexed: 11/26/2022]
Abstract
We undertake a comparative mammalian zoogeographic analysis with the aim of revealing the extent to which the Dmanisi Early Pleistocene large mammal assemblage resembles, at the genus level, African, Arabian, and Eurasian localities of similar age. The inclusion of Old World Pliocene and Pleistocene mammalian faunas provides us with insights into the provincial origins of specific mammalian taxa and permits us to assess the relative affiliation of the Dmanisi mammalian faunas to other faunas in the Old World. Our analysis also allows us to consider hypotheses about the timing and direction of zoogeographic connections between western Eurasia and Africa during the Early Pleistocene. We utilize multiple zoogeographic analytical tools as a cross-comparison of Dmanisi with 42 other Eurasian and African mammalian-bearing localities between 2.7 and 0.7 Ma. Overall, we find that Dmanisi compares most closely with a subgroup of Greek, Italian, and Spanish localities that are slightly younger than Dmanisi itself. This could suggest a progressive dispersal from East to West of the large mammal communities during the late Early Pleistocene and the first occurrence at Dmanisi, and then later in Western Europe, of some taxa such as Stephanorhinus ex gr. etruscus-hundsheimensis, Equus altidens, Bison georgicus, Soergelia minor, Megantereon whitei, Canis borjgali, Canis (Xenocyon) lycaonoides. Dmanisi's habitats included drier areas, probably of open wooded savannah and grassland and by mountainous to semiarid rocky terrain. There is evidence that Dmanisi records short intervals of increased aridity in the middle part of the succession contemporaneous with the occurrence of Homo.
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Affiliation(s)
- Saverio Bartolini-Lucenti
- Earth Science Department, Paleo[Fab]Lab, University of Florence, via La Pira 4, 50121, Firenze, Italy; Natural History Museum, Geology and Paleontology Section, via La Pira 4, 50121, Firenze, Italy
| | - Omar Cirilli
- Earth Science Department, Paleo[Fab]Lab, University of Florence, via La Pira 4, 50121, Firenze, Italy; Dottorato di Ricerca in Scienze della Terra, University of Pisa, via S. Maria 56, 56126, Pisa, Italy
| | - Luca Pandolfi
- Earth Science Department, Paleo[Fab]Lab, University of Florence, via La Pira 4, 50121, Firenze, Italy
| | - Raymond Louis Bernor
- Laboratory of Evolutionary Biology, Department of Anatomy, College of Medicine, Howard University, 20059, Washington DC, USA; Human Origins Program, Department of Anthropology, National Museum of Natural History, Smithsonian Institution, 20013, Washington, DC, USA
| | - Maia Bukhsianidze
- Georgian National Museum, 3, Rustaveli Avenue, Tbilisi-0105, Georgia
| | - Francesco Carotenuto
- Department of Earth Sciences, Environment and Resources, "Federico II" University of Naples, Via Cinthia 21, 80126, Naples, Italy
| | | | | | - Lorenzo Rook
- Earth Science Department, Paleo[Fab]Lab, University of Florence, via La Pira 4, 50121, Firenze, Italy.
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