40Ar/39Ar dating and paleoenvironmental reconstruction of the Lower Pleistocene sequence of Kvemo-Orozmani (Republic of Georgia): New chronological constraints for Dmanisi

Discovery of Early Pleistocene hominid remains about 15 years ago in Dmanisi (southwestern part of the actual Republic of Georgia) provides evidence on an early expansion of hominid out of Africa as early as the Olduvai subchron period (Gabunia et al., 2001). Two other Early Pleistocene sequences only few kilometers from Dmanisi: Zemo and Kvemo Orozmani are of prime interest to improve the dating of this exceptional site. They both display similar sediments than Dmanisi, but contrary to it, they both are overly by a lava flow allowing to precisely bracketing these sequences using radio-isotopic methods. In this contribution, we present the first high precision 40Ar/39Ar dating and paleoecological reconstruction (phytoliths record) of the Kvemo-Orozmani sequence. The 40Ar/39Ar ages we obtained on the lava flow bracketing the Kvemo Orozmani sequence are: 1.83 ± 0.02Ma and 1.77 ± 0.02Ma (95% confidence, relative to the ACR2 standard at 1.194 Ma). These numerical ages place the sequence exactly at the top of the Olduvai subchron. Furthermore, the lowermost lava flow (c.a. 1.83Ma) is only marginally younger than the lava flow found below the Dmanisi site and dated at 1.85 ± 0.01Ma (Gabunia et al.,(2000)), whereas, the uppermost one displays the same age than the one covering the Zemo Orozmani sequence (Gabunia et al., 2000) located only 2km East. Phytoliths analyses (silica opal produced by plants) show that lower part of the sequence is associated with herbaceous vegetations composed of both temperate and sub-tropical taxa whereas the upper part of the sequence shows an absence of subtropical phytoliths taxa suggesting dryer condition. The shift in the phytoliths assemblage we found in Kvemo-Orozmani is similar to the one described in Dmanisi at the top of the A stratum and corresponds paleomagnetically to the top of the Olduvai subchron (Messager et al., 2010). Both numerical ages and phytoliths assemblages we obtained suggest that the Kvemo Orozmani sequence corresponds to the period of occupation in Dmanisi and allow us to discuss both the age as well as the palaeoecological context of early hominids in Georgia. Gabunia et al., (2000), Science 288, 1019-1025; Messager et al., (2010), Palaeogeography, Palaeoclimatology, Palaeoecology, 288, 1-13