Caucasus connections? New data and interpretations for Armenian obsidian in Northern Mesopotamia

Contact across long distances is evident in the Neolithic of the Near East, whether driven by social networks, exchange links, or movement of individuals or populations. Movement of material, such as obsidian, can elucidate these processes but is often studied within a bounded world that places Mesopotamia at the center. This paper focuses on links that cut across the traditionally imposed boundaries between Northern Mesopotamia and the Caucasus. While Armenia is one of the world's most obsidian-rich landscapes, reports of Armenian obsidians in Northern Mesopotamia are scarce. The confirmation (or lack thereof) of these rare reports has important consequences regarding the movement of people, material, and information out of the Caucasus. As discussed here, all but one report either cannot be corroborated or are demonstrably erroneous. For one archaeological site, data processing methods led to overlaps in the signals for different obsidian sources. For another site, one element used in source identification suffered from unsystematic error. For other sites, data and key details went unpublished at the time. To corroborate past work that had identified Armenian obsidian at Domuztepe, 66 artifacts were newly sourced by electron microprobe analysis and confirmed by portable X-ray fluorescence. This sample was biased toward artifacts potentially from Armenia. Our analyses revealed that 15 artifacts match Pokr Arteni, one of the most used obsidian sources in Armenia. For reasons not yet clear, obsidian was brought to this Late Neolithic settlement over a distance of 670 km linearly and &gt; 800 km on foot. Additionally, there are artifacts from four other sources in the Kura-Araxes basin, lending extra support to movement of materials, if not people, between the Caucasus and Domuztepe. Furthermore, there are similar patterns in the two chemical varieties of Pokr Arteni obsidian at Domuztepe and at a Late Neolithic site in Armenia, Aratashen, potentially reflecting similar processes or behaviors at this source.</p

Short-term occupations at high elevation during the Middle Paleolithic at Kalavan 2 (Republic of Armenia)

The Armenian highlands encompasses rugged and environmentally diverse landscapes and is characterized by a mosaic of distinct ecological niches and large temperature gradients. Strong seasonal fluctuations in resource availability along topographic gradients likely prompted Pleistocene hominin groups to adapt by adjusting their mobility strategies. However, the role that elevated landscapes played in hunter-gatherer settlement systems during the Late Pleistocene (Middle Palaeolithic [MP]) remains poorly understood. At 1640 m above sea level, the MP site of Kalavan 2 (Armenia) is ideally positioned for testing hypotheses involving elevation-dependent seasonal mobility and subsistence strategies. Renewed excavations at Kalavan 2 exposed three main occupation horizons and ten additional low densities lithic and faunal assemblages. The results provide a new chronological, stratigraphical, and paleoenvironmental framework for hominin behaviors between ca. 60 to 45 ka. The evidence presented suggests that the stratified occupations at Kalavan 2 locale were repeated ephemerally most likely related to hunting in a high-elevation within the mountainous steppe landscape

Obsidian exchange networks and highland-lowland interaction in the Lesser Caucasus Borderlands

Obsidian sourcing studies have a long history in the Near East, but relatively few have focused on obsidian exchange after the Early Bronze Age. Here, we present a multi-technique analysis of an assemblage of 111 obsidian artifacts from excavated Late Bronze and Early Iron Age (LBA-EIA; c. 15th-6th c BCE) contexts at Mtsvane Gora, southern Georgia. Because the site is situated in the lowland Kura Valley and the nearest obsidian sources are in the highlands to the south and west, obsidian provenance can serve as a proxy for mapping highland-lowland interactions. Chemical compositions analyzed via portable X-ray fluorescence spectrometry (pXRF), electron microprobe analysis (EMPA), and laser ablation inductively-coupled plasma mass spectrometry (LA-ICP-MS), were compared with existing geological datasets of chemical analyses to identify the source of all but one of the artifacts analyzed. The results show that Chikiani, a source in the highlands of southern Georgia, was the geological origin of >90% of the objects analyzed. While acknowledging that obsidian exchange is just one aspect of highland-lowland interaction, this finding implies that Mtsvane Gora’s connections with the adjacent highlands were skewed towards greater engagement with some highland areas relative to others. More generally, the research suggests that geographic adjacency of highlands and lowlands does not necessarily mean that they were highly interconnected.Fieldwork at Mtsvane Gora was funded by the American Research Institute of the South Caucasus, the Rust Family Foundation, a Spatial Archaeometry Research Collaborations (SPARC) Grant, the Harvard University Davis Center for Russian and Eurasian Studies, and the Harvard Department of Anthropology. The authors would like to thank Project ARKK team members for their support during fieldwork. Paul Albert is supported by a UKRI FLF (MR/S035478) Note: guessed MRC by grant number but this could be overarching UKRI as it is a Future Leaders Fellowships award. Paul Albert is not a CU researcher

The earliest evidence for Upper Paleolithic occupation in the Armenian Highlands at Aghitu-3 Cave

With its well-preserved archaeological and environmental records, Aghitu-3 Cave permits us to examine the settlement patterns of the Upper Paleolithic (UP) people who inhabited the Armenian Highlands. We also test whether settlement of the region between ∼39–24,000 cal BP relates to environmental variability. The earliest evidence occurs in archaeological horizon (AH) VII from ∼39–36,000 cal BP during a mild, moist climatic phase. AH VI shows periodic occupation as warm, humid conditions prevailed from ∼36–32,000 cal BP. As the climate becomes cooler and drier at ∼32– 29,000 cal BP (AH V-IV), evidence for occupation is minimal. However, as cooling continues, the deposits of AH III demonstrate that people used the site more intensively from ∼29–24,000 cal BP, leaving behind numerous stone artifacts, faunal remains, and complex combustion features. Despite the climatic fluctuations seen across this 15,000-year sequence, lithic technology remains attuned to one pattern: unidirectional reduction of small cores geared towards the production of bladelets for tool manufacture. Subsistence patterns also remain stable, focused on medium-sized prey such as ovids and caprids, as well as equids. AH III demonstrates an expansion of social networks to the northwest and southwest, as the transport distance of obsidian used to make stone artifacts increases. We also observe the addition of bone tools, including an eyed needle, and shell beads brought from the east, suggesting that these people manufactured complex clothing and wore ornaments. Remains of micromammals, birds, charcoal, pollen, and tephra relate the story of environmental variability. We hypothesize that UP behavior was linked to shifts in demographic pressures and climatic changes. Thus, by combining archaeological and environmental data, we gain a clearer picture about the first UP inhabitants of the Armenian Highlands

Palaeoenvironmental and chronological context of hominin occupations of the Armenian Highlands during MIS 3:Evidence from Ararat-1 cave

Archaeological and palaeoenvironmental evidence from the Armenian Highlands and wider southern Caucasus region emphasises the significance of Marine Oxygen Isotope Stage 3 (c. 57–29 ka) as a crucial period for understanding hominin behaviours amidst environmental fluctuations. Ararat-1 cave, situated in the Ararat Depression, Republic of Armenia, presents potential for resolving emerging key debates regarding hominin land use adaptations during this interval, due to its well-preserved lithic artefacts and faunal assemblages. We present the first results of combined sedimentological, geochronological (luminescence and radiocarbon), archaeological and palaeoecological (macrofauna, microfauna and microcharcoal) study of the Ararat-1 sequence. We demonstrate sediment accumulation occurred between 52 and 35 ka and was caused by a combination of aeolian activity, cave rockfall and water action. Whilst the upper strata of the Ararat-1 sequence experienced postdepositional disturbance due to faunal and anthropogenic processes, the lower strata remain relatively undisturbed. We suggest that during a stable period within MIS 3, Ararat-1 was inhabited by Middle Palaeolithic hominins amidst a mosaic of semi-arid shrub, grassland, and temperate woodland ecosystems. These hominins utilised local and distant toolstone raw materials, indicating their ability to adapt to diverse ecological and elevation gradients. Through comparison of Ararat-1 with other sequences in the region, we highlight the spatia

Short-term occupations at high elevation during the Middle Paleolithic at Kalavan 2 (Republic of Armenia)

The Armenian highlands encompasses rugged and environmentally diverse landscapes and is characterized by a mosaic of distinct ecological niches and large temperature gradients. Strong seasonal fluctuations in resource availability along topographic gradients likely prompted Pleistocene hominin groups to adapt by adjusting their mobility strategies. However, the role that elevated landscapes played in hunter-gatherer settlement systems during the Late Pleistocene (Middle Palaeolithic [MP]) remains poorly understood. At 1640 m above sea level, the MP site of Kalavan 2 (Armenia) is ideally positioned for testing hypotheses involving elevation-dependent seasonal mobility and subsistence strategies. Renewed excavations at Kalavan 2 exposed three main occupation horizons and ten additional low densities lithic and faunal assemblages. The results provide a new chronological, stratigraphical, and paleoenvironmental framework for hominin behaviors between ca. 60 to 45 ka. The evidence presented suggests that the stratified occupations at Kalavan 2 locale were repeated ephemerally most likely related to hunting in a high-elevation within the mountainous steppe landscape.info:eu-repo/semantics/publishedVersio

Origin of an obsidian scraper at Yabroud Rockshelter II (Syria): Implications for Near Eastern social networks in the early Upper Palaeolithic

Identifying the movement of lithic materials to reconstruct social networks has been a mainstay of research into Palaeolithic cognition and behavior, but such datasets are often predicated on studies of cherts and similar siliceous rocks, the origins of which can be difficult to establish conclusively. Yabroud Rockshelter II (YR2) in southern Syria contained stratified Middle and Upper Palaeolithic layers and, therefore, played a key role in defining the Levantine Palaeolithic. One obsidian scraper was found in Layer 4, which, via techno-typological correlations with nearby sites, dates to similar to 41-32 ka. Here we report our attribution of this scraper, based on its elemental analysis, to the Komurcu outcrops at Gollu Dag volcano in central Turkey, >= 700 km on foot. This finding has three important implications. First, the earliest transport of obsidian into the Levant is usually associated with the Epipalaeolithic Natufian cultural complex (similar to 14.5-11.5 ka); however, the phenomenon dates farther back to a period following the Middle to Upper Palaeolithic transition. Second, Layer 4 is roughly contemporaneous with Layer C at Shanidar Cave in northern Iraq, where two obsidian flakes were sourced to eastern Turkey and/or the Caucasus, suggesting similar scales of interaction across the landscape. Lastly, the chert assemblage is presumed to be local (<= 10 km), but the obsidian scraper suggests that there are other far-travelled artifacts, underscoring that visual identification of cherts might be underestimating the extent of Late Pleistocene mobility and networks

Evidence for Middle Palaeolithic occupation and landscape change in central Armenia at the open-Air site of Alapars-1

Here we report the findings from excavations at the open-Air Middle Palaeolithic site of Alapars-1 in central Armenia. Three stratified Palaeolithic artefact assemblages were found within a 6-m-Thick alluvial-Aeolian sequence, located on the flanks of an obsidian-bearing lava dome. Combined sedimentological and chronological analyses reveal three phases of sedimentation and soil development. During Marine Oxygen Isotope Stages 5-3, the manner of deposition changes from alluvial to aeolian, with a development of soil horizons. Techno-Typological analysis and geochemical sourcing of the obsidian artefacts reveal differential discard patterns, source exploitation, and artefact densities within strata, suggesting variability in technological organization during the Middle Palaeolithic. Taken together, these results indicate changes in hominin occupation patterns from ephemeral to more persistent in relation to landscape dynamics during the last interglacial and glacial periods in central Armenia