This project documents the current archaeological record of the Qaraçay River Basin in western Azerbaijan. Integrating intensive pedestrian survey, satellite imagery analysis and topographic mapping, the study identified 85 kurgans, six necropolises and nine sites from the Chalcolithic or medieval periods. The authors believe this demonstrates the potential for further archaeological studies in the region.

Current research indicates that full-fledged Neolithic societies emerged in the Southern Caucasus in the early sixth millennium BC, most likely through interaction with and/or the immigration of the Neolithic societies of Southwest Asia. However, the absence of late seventh millennium BC excavated sites has prevented us from being able to interpret the processes in relation to earlier indigenous foraging societies. The 2016–2019 excavations at Damjili Cave, west Azerbaijan, revealed a stratified cultural sequence of the key Mesolithic-to-Neolithic transition period for the first time. Its radiocarbon chronology identified a rather abrupt emergence of the Neolithic economy at around 6000 cal BC, at least in the study region, urging a reconsideration of the long-standing claim that some other form of earlier Neolithic society had existed before this. At the same time, the stratigraphic analysis of cultural remains revealed continuity in certain elements of tool manufacturing and use from the Mesolithic to the Neolithic. This complex situation shows the need for evaluating the degree to which indigenous foraging societies contributed to the Neolithization of the Southern Caucasus, rather than focusing merely on immigration models.

Despite recurring elections and the transition to multiparty systems, authoritarianism has re-emerged in the Post-Soviet Space. Along with domestic factors, the external dimension should also be considered to fully understand this regional trend. Scholars depict Russia as a typical ‘black knight’ for democracy. While most of the literature deals with the Kremlin's policies in the ‘new’ Eastern Europe, this article pays attention to Russia's actions in the relatively understudied Southern Caucasus. Specifically, it investigates why and how Moscow tried to thwart democratization in Armenia, Azerbaijan and Georgia. The diachronic analysis addresses three periods, namely, Yeltsin's presidency, the first Putin presidency and the Putin–Medvedev diarchy. Findings suggest that the Kremlin implemented an increasingly nuanced and intentional black knight strategy in Southern Caucasus, aimed at gaining primacy in the Post-Soviet Space and recognition of its great power status.

Recent ground surveys in the Samtskhe-Javakheti region of southern Georgia have investigated a previously undocumented group of sites along a ridge overlooking the upper Kura river valley. Features and artefacts recorded at Varneti suggest long but episodic occupation from the Chalcolithic to the later medieval periods, with prominent phases in the Early to Middle Bronze Age and the Late Bronze Age to Early Iron Age. Varneti has the potential to contribute to understanding economic and strategic aspects of the long-term settlement pattern in the southern Caucasus, especially the interplay between lowland and highland zones. Its position in the landscape, at a transitional point between the river valley and the upland pasture (yayla), may explain its persistent use by agro-pastoral communities that operated in varied cultural situations. The survey results help us frame a series of questions regarding economic and social dynamics at a local and regional scale and the continuity and discontinuity of practice in highland environments through long timespans.

The southern Caucasus was intensively settled through the Neolithic period to present. Studies of late Quaternary fluvial dynamics and landscape development at the lower Shulaveris Ghele River in southeastern Georgia aid understanding of the Quaternary history of this region. Our studies show that following river aggradation to form a fan-shaped alluvial surface during the late Pleistocene, fluvial sedimentation shifted west, leaving a fan surface subject only to local fluvial and colluvial processes as well as late Neolithic settlement. At about 6 ka, the river avulsed to the east and eroded some late Neolithic settlements occupying the eastern portion of the fan. The avulsion was followed by 3 distinct episodes of aggradation at about 6 ka, 3–2 ka, and since 1.0 ka. No such aggradation is evident in the early Holocene. Regional Holocene fluvial activity in this area was apparently influenced by vegetation dynamics, possibly controlled by regional climatic and/or anthropogenic factors, and significantly differs from the eastern Mediterranean region. All late Neolithic settlements were originally built far from an active river, possibly indicating late Neolithic water management systems.

The absolute chronology of the Kura-Araxes (KA) culture in the Southern Caucasus still represents a challenge due to the fragmentation and inadequacy of the radiocarbon record, as well as the inconsistencies in material typologies in the region. Recent archaeological fieldwork at the site of Aradetis Orgora in the Shida Kartli region of Georgia revealed four occupation levels dating to the KA II phase according to the local relative chronology. 14C samples were collected from reliable contexts and further selected according to reliability criteria, taking into account both archaeological issues and lab procedures. FTIR was applied in order to determine the preservation of charcoals and to monitor the efficiency of lab treatments on all the samples. Only accurate 14C measurements were selected for Bayesian analysis incorporating stratigraphic information. Two models were run, the second of which simulated intervals corresponding to unexcavated stratigraphy or due to a lack of samples. In this article, the available 14C dates for the KA occupation at Aradetis are presented for the first time and analyzed using Bayesian principles. The results of Bayesian modeling suggest that the occupation of the excavated KA II levels cover the period between 3040–2810 BC (simple model) or 3090–2720 BC (interval model).