4.2 Article

The Late Middle Pleistocene mammalian fauna of Oumm Qatafa Cave, Judean Desert: taxonomy, taphonomy and palaeoenvironment

Journal

JOURNAL OF QUATERNARY SCIENCE
Volume 37, Issue 4, Pages 612-638

Publisher

WILEY
DOI: 10.1002/jqs.3414

Keywords

archaeology; early fire; fauna; Levant; palaeontology; Quaternary

Funding

  1. European Research Council [802752, DEADSEA_ECO]
  2. Humboldt Foundation
  3. University of Haifa
  4. European Research Council (ERC) [802752] Funding Source: European Research Council (ERC)

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This article presents a revised taxonomy of the macromammalian fauna from the Middle Pleistocene site of Oumm Qatafa in the Judean Desert, southern Levant. The findings provide insights into the paleoenvironment of the region and the impact of human activities on the fauna. Comparisons with other Pleistocene sites in the Levant contribute to a more comprehensive understanding of human evolution and intercontinental faunal biogeography.
The Middle Pleistocene archaeological record of the southern Levant has proven key to understanding human evolution and intercontinental faunal biogeography. Knowledge of archaeological sites of that period in the southern Levant is biased, with most Middle Pleistocene localities in the Mediterranean areas in the north, despite the mosaic of environments that mark the entire region. A key Middle Pleistocene location in the Judean Desert - on the eastern margin of the Mediterranean zone - is the site of Oumm Qatafa, excavated in the early 1900s, which yielded a faunal collection spanning an estimated time period of 500-200 kya. Here, we present a revised taxonomy of the macromammalian fauna from the site, discuss the palaeoenvironmental implications of this assemblage, and relate the finds to other Pleistocene sites from the Levant. These data enable a more precise palaeoenvironmental reconstruction which attests to an open landscape, but with the addition of a mesic Mediterranean component close by. In addition, detailed taphonomic observations on butchery marks and Fourier transform infrared spectroscopy analysis of burnt bone link the fauna for the first time to anthropogenic activities in the cave.

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