Areni-1 Cave,Armenia: A Chalcolithic–Early Bronze Age settlement and ritual site in the southern Caucasus

Abstract

The beginning of the Bronze Age in the southern Caucasus has been thought to coincide with the appearance of the Kura Araxes (KA) culture around 3500 cal b.c. KA artifacts are known not only from the southern Caucasus but also from sites in Anatolia, Iran, and the Levant. Recent discoveries from Areni-1 Cave in the Vayots Dzor region of Armenia demonstrate that the origin of the distinctive KA artifact assemblage lies in the Late Chalcolithic of the late 5th to early 4th millennia b.c. The cave contains rich assemblages of desiccated botanical remains that allow the site to be precisely dated and that demonstrate that its inhabitants exploited a wide variety of domesticated and wild plants. It would appear that from 4000 cal b.c. onwards, people used Areni-1 Cave for habitation and for keeping goats, storing plant foods, and ritual purposes; unusual for this time period are ceramic vessels containing the skulls of children.     

Cranial pathology of Ursus spelaeus ROSENMÜLLER & HEINROTH from Chateau Pignon,Basque Territories (Spain)

A complex lesion, on a skull of a female cave bear (Ursus spelaeus) associated with perforations of the frontal sinus is described. Paleopathological analysis suggests that the lesion is attributable to complex cranial trauma, probably complicated by an infection which appears to have occurred following a fight, most likely with another bear or, possibly, a cave lion (Panthera leo spelaea); at least one of the perforations observed on the skull may have been produced by the canine of a large carnivore. This hypothesis is supported by the frequent intraspecific aggressiveness documented in modern bears, and by evidence suggesting interspecific fights between cave bears and cave lions. The case is discussed in the light of other evidence reported in the literature. © 1998 John Wiley & Sons, Ltd.     

New investigations into the Uluburun resin cargo

Resin found within Canaanite amphorae from the Late Bronze Age shipwreck discovered off the coast of southwest Turkey at Uluburun has previously been identified as Pistacia sp. Although evidence from Egypt suggests that this resin was in high demand and typically transported in such amphorae, it has also been proposed that the amphorae contained wine, with the resin used to seal the interior surfaces and to flavour and/or preserve the wine. To attempt to resolve this question, we have analysed five samples of pistacia resin found in amphorae from the shipwreck using a range of analytical techniques which have used in the past for the analysis of wine residues: spot tests, FT-IR, and HPLC-MS-MS. As well as the archaeological samples, we have analysed modern samples of pistacia resin, leaves and fruit to determine the effectiveness of each technique and to exclude the possibility of false positive results. In addition to the analyses for wine we also detail analysis (GC-MS) of the terpenoids for the purpose of further molecular characterisation of the resin. Bulk stable isotope analysis was used in comparison with similar resins to attempt to identify the geographical origin of the resin.     

Reevaluating the Age of the Iberomaurusian in Morocco

Chronological evidence for the Iberomaurusian is currently very limited and there are problems with some of the published radiocarbon dates. In this paper we present new AMS dating results from well-stratified cave sequences at Ghar Cahal, Kehf el Hammar and Taforalt in northern and eastern Morocco. The longest of these sequences, from Taforalt, shows an intermittent occupation history spanning the period ca. 18,000–11,000 bp (radiocarbon determinations presented in this paper are expressed as ka bp or bp, whilst approximate calendar ages are expressed as Cal bp) with a marked intensification of cave use soon after ca. 13,000 bp. Using calibrated AMS ages in comparison to sea surface temperature evidence from the Alboran Sea core MD95-2043 and more generally to Greenland ice δ¹⁸O core records, we suggest that there may have been a relationship, albeit a complex one, between climatic events and cave activity on the part of Iberomaurusian populations.     

First evidence of white wine in ancient Egypt from Tutankhamun's tomb

Wine has been considered to be mainly red in ancient Egypt linked with the blood of Osiris, the God of resurrection. No text that refers to white wines from the Dynastic Period (3150–332 BC) exists. The first white wine from ancient Egypt was made near Alexandria during the third century AD. To investigate the presence of white wine in ancient Egypt, dry residue samples from King Tutankhamun's amphorae are studied in this article using the LC/MS/MS method for wine markers. This investigation into the existence of white wines in Tutankhamun's tomb allows us to shed new light on the symbolism of white wine in ancient Egypt.     

Armenia in the Eurasian Economic Union: reasons for joining and its consequences

On 3 September 2013, the president of Armenia shifted the long-praised process of initialing political association and economic integration with the European Union and announced Armenia’s decision to join the Russia-led Customs Union and participate in the processes of formation of the Eurasian Economic Union (EAEU). Practitioners and observers interpreted it either as a U-turn or as a surprise move mainly assuming that what happened was the result of Russian pressure on Armenia. However, when tensions and uncertainty eased, it became obvious that what happened was a result of complex reasons. Geopolitical constraints and socio-political problems that had accumulated in Armenia during recent years coincided with an assertive expansion of Russia’s foreign policy. This research provides a number of explanations for that political decision to understand the primary determinants of that move. It also examines the political and economic implications of Armenia’s membership of the EAEU.     

The origin of the ancient Egyptian drink Shedeh revealed using LC/MS/MS

Ancient Egyptians were buried with the most precious food and drink as sustenance for their afterlife. One of these was Shedeh, the most valued and appreciated beverage in ancient Egypt. The botanic origin of Shedeh remains unclear as no mention of its raw material has survived. Some scholars have proposed that Shedeh was a pomegranate wine, while others, a grape wine. Presented here is the first ever analytical evidence of Shedeh's origin through the analysis of a sample of a residue from an extraordinarily well preserved Shedeh amphora from King Tutankhamun's collection. The previously developed LC/MS/MS wine markers method for archaeological samples was used and our results reveal Shedeh had a red grape origin.     

Preliminary conclusions on the Late Glacial vegetation in south-west Anatolia (Turkey): the complementary nature of palynological and anthracological approaches

The combined analysis of charcoal fragments retrieved from epipalaeolithic settlements in Öküzini cave (south-west Anatolia, Turkey) and of pollen in samples retrieved from outside the cave reveals the transformation of the vegetation in the region over the Late Glacial Period. The analyses provide consistent information on the use of natural resources and evidence as to the protodomestication of cereals in the region.     

The contents of unusual cone-shaped vessels (cornets) from the Chalcolithic of the southern Levant

Cornets are cone-shaped ceramic vessels, characteristic of the Chalcolithic period (ca. 4700–3700 BC) in Israel and Jordan. Their contents and use are unknown. Gas chromatography with flame ionization and mass-selective detection, showed that extracts of cornets from five different sites with different related activities (domestic, habitation cave and a cultic complex) all contain the same assemblage of mainly n-alkanes adsorbed within their walls. This assemblage differs from those found in other types of ceramic vessels from the same sites, as well as from the residues found within the associated sediments. The assemblage of odd and even-numbered n-alkanes found in the cornets is almost identical to that found in the residues of beeswax heated on modern ceramic fragments, as well as in a beehive from the Iron Age IIA strata at Tel Rehov, Israel. Thus the cornets are most likely to have contained beeswax. The presence of beeswax in the cornets contributes to our understanding of the Chalcolithic period; a time when secondary products such as milk, olive oil and wine are thought to have come into use.     

Tempo and mode of formation of the Late Epigravettian necropolis of Arene Candide cave (Italy): direct radiocarbon evidence

Existing ¹⁴C dates of charcoal and bone samples from different layers of the Late Epigravettian sequence at Arene Candide (Liguria, Italy) place the formation of the deposit between 12,000 and 10,000 (uncal.) BP, but it is unclear how long this cave was used for funerary purposes. Clarifying this point has important archaeological and anthropological implications, given number and variety of inhumations. These include single and double burials of richly ornamented adults, adolescents and children and disarticulated accumulations of bones. Six new direct ¹⁴C AMS dates obtained from human skeletons place more precisely the necropolis at the Late Pleistocene-Early Holocene boundary, and appear distributed in two distinct groups that indicate two phases of funerary utilisation of the cave. Although separated by many centuries, the two phases of interment show recurring formal elements. Both groups include skeletons in anatomical connection exhibiting similar grave goods as well as chaotic accumulations of bones and, more importantly, the double burial of an adult with a child lying to its left. The reappearance of similar funerary patterns in the same site at two widely separated points in time suggests that the cave held a symbolic significance over several centuries. This, and the additional evidence of funerary use of the cave during the preceding Gravettian, points to the endurance of Upper Palaeolithic cultural traditions.     

THE USE OF TEXTURAL PARAMETERS IN THE ANALYSIS OF CAVE SEDIMENTS

This paper considers the presentation of the results of the mechanical analysis of cave sediments, suggesting that the use of grain size parameter scatter diagrams is preferable to the older method of cumulative percentage frequency graphs. A sequence of samples was taken from an ideally-situated cave, the Badger Hole at Wookey, and first subjected to the standard soil analytical tests, followed by a detailed mechanical analysis. It is hoped that this preliminary work will encourage a more quantitative approach to granulometric analysis for archaeological purposes, leading eventually to the extraction of more precise environmental data from cave sediments.     

Micromorphology of a Late Woodland Cave Site,East-Central Iowa

Abstract

This article discusses a micromorphological investigation conducted at Bogus Cave (13JN23), a Late Woodland occupation in Jones County, Iowa. Micromorphology–the study of undisturbed soil and sediment in thin section–was used to evaluate, and differentiate between, natural and cultural processes evidenced within the cave sediments. Twenty-two thin sections were prepared from samples collected from test units excavated in the front room of the cave, the principal site of human occupation. The cultural material was confined to a 55-cm-thick surface layer that rests on an accumulation of angular to subangular boulder-size dolostone blocks, the result of one or more episodes of pre-Holocene ceiling collapse. The thin sections revealed an accumulation of exogenous mineral grains, chert microdebitage, microvertebrate remains, and charcoal fragments in an organic-rich clay matrix. The absence of microstratification in the samples collected from the artifact-bearing stratum supports previous macroscopic evidence for a thorough mixing of the deposits that precludes an accurate contextual interpretation of the archaeological component.     

Probable human hair found in a fossil hyaena coprolite from Gladysvale cave,South Africa

Until now, the oldest known human hair was from a 9000-year-old South American mummy. Here we report fossil hairs of probable human origin that exceed that age by about 200,000 years. The hairs have been discovered in a brown hyaena (Parahyaena brunnea) coprolite from Gladysvale cave in South Africa. The coprolite is part of a hyaena latrine preserved in calcified cave sediment dated between 195,000 and 257,000 years ago. This find supports the hypothesis that hyaenas accumulated some of the early hominin remains found in cave sites, and provides a new source of information on Pleistocene mammals in the Sterkfontein Valley.     

Mortality analysis of the Late Pleistocene bears from Grotta Lattaia,central Italy

Reported here are the results of a mortality analysis of an Ursus spelaeus death assemblage from Grotta Lattaia, southern Tuscany (central Italy), excavated in 1939. The Grotta Lattaia cave bears are among the latest representatives of the species. The large amount of cave bear remains indicates that the cavern was a lair for hibernating bears which repeatedly, but not necessarily yearly, occupied it. The mortality evidence indicates that deaths occurred primarily during hibernation from violent predation, and, therefore, that the bears had direct interaction with other carnivores. However, no sign of interrelation with humans could be found, even though Middle Paleolithic human remains and tools had been recovered associated with the bear material. Grotta Lattaia can be thus considered an example of cumulative, non-human-caused violent deaths in a hibernation context.     

New evidence for the Mousterian and Gravettian at Rio Secco Cave,Italy

Abstract

The dearth of evidence for late Neanderthals in Europe reduces our ability to understand the demise of their species and the impact of the biological and cultural changes that resulted from the spread of anatomically modern humans. In this light, a recently investigated cave in the northern Adriatic region at the border between the Italian Alps and the Great Adriatic Plain provides useful data about the last Neanderthals between 46·0 and 42·1 ky cal b.p. Their subsistence is inferred from zooarchaeological remains and patterns in Middle Palaeolithic lithic technology. Unexpected evidence of the ephemeral use of the cave during the early Upper Palaeolithic Gravettian period shows a change in lithic technology.     

U-series Dating of Fossil Teeth and Carbonates from Snake Cave,Thailand

Snake Cave (Thailand) is an important site for the study of the evolution in Southeast Asia, leading to a discovery of rich and various faunas, including a human tooth. Fossils of large and small mammals converge to indicate, on the basis of faunal assemblage, a late Middle Pleistocene age for the fossiliferous layers; on the other hand, previous U-series dating of carbonates furnished a lower limit for the fossils of about 130 ky.In order to achieve a better comprehension of the chronology of the cave, the Uranium-series method for absolute age determination has been applied to some carbonates older than those studied previously and to fossils themselves.We used the isochron technique approach to yield valuable ages because spleleothem samples consist in a mixture of calcite and detrital contamination. The results obtained suggest that the main fossiliferous level is older than about 160 ky. The application of the U-series method to tooth samples from this tropical cave leads to erroneous ages, probably because of post depositional groundwater movements.     

Revisiting Qumran Cave 1Q and its Archaeological Assemblage

Qumran Cave 1Q was the first site of Dead Sea scroll discoveries. Found and partly emptied by local Bedouin, the cave was excavated officially in 1949 and published in the series Discoveries in the Judaean Desert (Volume 1) in 1955. Contents of the cave are found in collections worldwide, and in different institutions in Jerusalem and Amman. While the scrolls are the most highly prized artefacts from this cave, in archaeological terms they are part of an assemblage that needs to be understood holistically in order to make conclusions about its character and dating. This study presents all of the known items retrieved from the cave, including those that are currently lost, in order to consider what we might know about the cave prior to its emptying and the changes to its form. It constitutes preliminary work done as part of the Leverhulme funded International Network for the Study of Dispersed Qumran Caves Artefacts and Archival Sources [IN-2015-067].     

A rallying point for different predators: the avian record from a Late Pleistocene sequence of Grotte des Barasses II (Balazuc,Ardèche,France)

The presence of processed birds in the archeological faunal record is considered key to assessing human dietary evolution. Taphonomic studies on birds from sites older than Marine Isotope Stage (MIS) 2 have become relevant in the last few years, leading to the proposal of more complex scenarios of human subsistence. Several works have demonstrated direct evidence of bird consumption by Homo prior to anatomically modern humans in Europe; however, others support the hypothesis of non-anthropogenic bird accumulations. This has led to the necessity of determining what elements or factors cause the human exploitation of birds in some archeological sites before the end of the Pleistocene. The Grotte des Barasses II site is located within this framework. Short-term human occupations have been attested by the presence of lithic tools and processed macrofaunal remains. Additionally, a small assemblage of bird bones has also been recovered. Here, we present a detailed taphonomic study with the aim of exploring possible relationships between these avian taxa and human occupations. Despite the fact that Neanderthals inhabited the cave, avian specimens show damage pointing to different causative agents. Direct evidence (digestion, gnawing) indicates that mammalian carnivores and nocturnal raptors were mainly involved in the accumulation of bird bones. We propose some factors that might determine whether or not small game was exploited in this specific locality and emphasize the importance of such analytical approaches in the general interpretations of the Pleistocene sites.     

Bear dentine aspartic acid racemization analysis: a proxy for the dating of Pleistocene cave infills

A high correlation between chronometric determinations based on aspartic acid racemization ratios and radioactive dating methods is described from samples of cave bear (Ursus deningeri and Ursus spelaeus) dentine. For samples from a very restrictive environment, as deep cave bear sites are (in view of their highly stable geochemical and thermal history), an age calculation algorithm was obtained. It has been found that there is a very close relationship between collagen preservation, from total aspartic acid in the > 3500 D fraction, and the amino acid racemization.     

The mobile herding economy of Kebarah Cave,Mt carmel: An economic analysis of the faunal remains

The faunal remains from Kebarah Cave provide evidence of the economic activities of the cave's inhabitants during the late Pleistocene and early Holocene. The variety of grazing resources around the cave is reflected in the proportions of the several species exploited, which changes gradually over time. A comparison of Bos remains indicates that locational factors appear to outweigh any chronological tendency towards size reduction. It is suggested that the same may be the case for animals not usually associated with human exploitation, in particular the hyaena. The data from an excavation conducted 40 years ago are inadequate to answer the questions posed by bioarchaeologists today, but the evidence from better known neighbouring sites has subsequently borne out much of what could be proposed here as hypothesis.