Burial Dating Research Articles

Speculation on an early Pleistocene origin of the Parker dunes of southwest Arizona, USA

The Parker Dunes in western Arizona, USA represent the largest dune system in the Sonoran Desert. This study presents a simple 10Be-26Al cosmogenic burial age of 1.90 ± 0.20 Ma, obtained from well cuttings 240–270 m deep in Butler Valley, just east of the dune field. Given the large errors associated with burial dating, we can only speculate that this oldest known aeolian sediment within the Parker Dunes is roughly concurrent with the Bat Cave flood event ca. 2.1 Ma of the nearby Colorado River, as well as regional climatic aridity during the early Pleistocene. Since older dune deposits may be present at other locations in the Parker Dunes, its origin dates back to at least the early Pleistocene. The more important, broader implication rests in highlighting the underutilized potential of well cuttings as a sediment source for cosmogenic burial dating in aeolian research.

Fluvial-lacustrine influences on linear dune erosion at Lake Caroline in the Simpson Desert of Australia

Linear dunes are frequently examined with regard to their formation and maintenance; however, erosion or degradation of these landforms is less commonly addressed, due in part to the lack of observable changes in the geologic record. This study investigates the significant erosion of linear dunes along Lake Caroline, a playa in the northern Simpson Desert of central Australia. Field observations, laboratory analyses, and remote sensing imagery document recent fluvial and lacustrine interactions at Lake Caroline. Compositional and geochemical sediment analyses from three ∼2 m deep hand-augured sample sites indicate that the playa is primarily filled with sand from linear dunes, but also contains evaporite minerals and weathered local bedrock. Satellite images show that the playa has flooded at least 58 times since 2001. Our results indicate that present-day aeolian processes are sufficient to mobilize and transport sediment but are dominated by fluvial-lacustrine processes, resulting in the playa-adjacent dunes becoming isolated and starved of local sediment. As a result, the dunes are currently eroding into the playa which supports the conclusion that long-distance sediment transport is not responsible for the formation or maintenance of linear dunes as suggested by the linear due extension hypothesis. Burial dates from optically stimulated luminescence (OSL) indicate the linear dunes have been eroding for as much as 24 ka, and sediment samples from the playa near one linear dune suggest an onset of dune formation in the area before 58 ka. This work documents an instance in geologic time during the late Quaternary when aeolian, fluvial, and lacustrine processes are competing with one another, offering new insights into the dynamics of linear dunes in the arid Simpson Desert.

26Al/10Be burial dating and technological strategies of hominins at the Jijiazhuang Paleolithic site, Nihewan Basin, China: Implications for understanding Middle Pleistocene human adaptations in east Asia

With the discovery of more than a hundred Pleistocene Paleolithic sites, the Nihewan Basin of North China has become an area of reference for the study of human evolution and behavioral adaptations during and after the spread of hominins out of Africa and into Eurasia. However, most research has focused on the Early and Late Pleistocene archaeological record, whereas studies of the Middle Pleistocene sequence are relatively limited. Here we contribute to fill this gap by introducing the archaeological assemblage and 26Al/10Be burial dating of the newly discovered Jijiazhuang (JJZ) Paleolithic site. Systematic excavations in recent years have yielded well-preserved stone artifacts and mammalian fossils in fluvio-lacustrine sediments at the site. Cosmogenic 26Al/10Be burial dating indicates that hominins occupied the site between 0.49 ± 0.10 and 0.63 ± 0.11 Ma, corresponding to the extra-long interglacial period of MIS 15-13. The JJZ lithic assemblage shows evidence of relatively long-distance resource procurement, and the increased number of retouched tools indicate standardized, extensive and refined modification, even shaping strategies. The JJZ lithic technology shows advanced features that may shed light on the regional emergence of Middle Paleolithic technologies, in a paleoecological context where the extra-long duration of interglacial/mild stadial climate events (MIS 15−13) may have provided favorable conditions for increased technological capabilities among Middle Pleistocene hominins from the Nihewan Basin. Our study is the first to present a detailed techno-typological analysis of a Middle Pleistocene lithic assemblage in the Nihewan Basin and contributes to the characterization of technological adaptions in the high latitudes of East Asia.

New Data on Armed Conflicts in the Altai During the Rouran Period: The Choburak I Cemetery

This study focuses on a burial at a Rouran period cemetery, Choburak I, in the Chemalsky District, Republic of Altai, where altogether twelve burials were excavated by an expedition from the Altai State University. In kurgan 34a, a burial of a 30–35-year-old male with a horse was excavated. The burial goods included weapons, items of horse harness, utensils and domestic artifacts. The head of the buried individual had been replaced by the cranium of a ram, and certain postcranial bones revealed multiple injuries inflicted by a cutting weapon. The burial is attributed to the Dàlián tradition, associated with the Bulan-Koba culture. The analysis of the burial goods and a radiocarbon estimate suggest that the burial dates to the middle or second half of the 4th century AD. Injuries testify to armed conflicts, in which males had taken part, and support the belief that violence in the Altai was high during the Rouran period. The case is interpreted as one of decapitation. Given the parallels in adjacent regions, is can be hypothesized that the head of a ram had been used as a basis for a mask. Apparently, this peculiar custom was associated with the ritual in which the missing bodily part was replaced in specific cases of violent death.

Результаты раскопок грунтового могильника Максимовка I в лесостепном Поволжье в 2019 г.

Introduction. The work publishes some results of excavations at the Maksimovka I grave field. Goals. So, the article seeks to introduce materials of the 2019 excavations. To facilitate this, the paper shall describe and characterize the investigated archaeological complexes, establish their cultural and chronological attributions. Materials. Archaeological material from the occupation layer comprises Neolithic, Chalcolithic, Bronze Age, and eighteenth/twentieth century pottery, flint tools, and stone processing waste. Six burials were investigated at the site. Two burials had been destroyed and are nothing but heaps of heavily fragmented bones with no grave goods observed. In the third burial, the skeleton was lying on back in a northern-northwestern direction, accompanied by an iron knife and goat/sheep bones. The next burial consisted of four skulls and compact clusters of skeletal bones located nearby. The latter’s grave goods included flint arrowheads, a scraper, a bone spearhead, a pendant, beads, piercings and marmot incisors. The fifth burial contained a seated skeleton facing northeast and accompanied by a flint plate, an arrowhead and beads. In the last burial, the skeleton was lying on back in a northern-northwestern direction, accompanied by an ornamented clay vessel. A part of structure 1 was also examined. Results. The work shows that a total of three burials date back to the Late Chalcolithic, one — to the Late Bronze Age, and one — to the Middle Ages. The cultural and chronological attribution of the remaining burial has not been determined yet. Conclusions. The excavations at the Maksimovka I grave field have yielded materials from different cultures and periods, including Neolithic, Chalcolithic, Bronze Age, and Medieval complexes.

Paleoanthropological Analysis of Osteological Material from the Myntobe Burial Ground

The article deals with the paleoanthropological analysis of the skeletons unearthed from the Myntobe necropolis and dated to the II – IV centuries AD. Myntobe necropolis is located 2 km south of Gani Muratbayev village in the Keles district of Turkestan province. The burial ground consists of more than 600 randomly located mounds of various sizes. All mounds have a dirt embankment. Archaeological excavations were carried out at the burial ground in 2017 and 2022, as a result of which burials in the catacombs and naus were unearthed. An analysis of the burial tradition and recovered material allows researchers to speak about the belonging of these burials to the Kangli tribes. Since the burials date back to the Kangli period, the theoretical part reveals the issues of the location and political structure of the tribes and, most importantly, the determination of the paleopathology of the Myntobints by conducting a macroscopic analysis of the discovered skeletons. The results of the analysis allowed for drawing preliminary conclusions about lifestyle, social life, and nutritional status. When writing the theoretical part of the article, electronic textbooks and resources from the book fund of the National Library of Kazakhstan and the library of the International Kazakh-Turkish University named after Kozh Ahmet Yasawi were used. In total, 9 skeletons were selected for paleoanthropological and paleopathological analysis, from mounds No. 3, No. 6, and No. 7. Paleoanthropological reasoning in the main section is written on the basis of materials in Turkish and English from the collections of Turkish libraries. The skeletons found were analyzed macroscopically and many diseases were identified, such as osteoarthritis (joint deformity), osteopathy, ankylosing spondylitis, heel spurs, thickening of the cranial bone, and deformity of the mandibular joint. Preliminary conclusions about the paleopathology of the discovered skeletons are made.

Jewellery of Pastyrske Circle among Materials of Saltiv Culture: Data Analysis

In the paper, jewellery from sites and assemblages of the Saltiv culture, which do not chronologically fit within the boundaries of its existence, are considered. In the article the jewellery characteristic of the Pastyrske hillfort is analysed (group II, subgroup 2). It is represented by two burial complexes and two hoards. Sukha Homilsha cemetery 1 was investigated by V. K. Mikhiev. Burial no. 29 (fig. 1) contained a medallion pendant similar to finds from Pastyrske hoard of 1949 and a number of other assemblages from the second half of the 7th to the first half of the 8th centuries. Burial date: late 8th — early 9th centuries. Staryi Saltiv cemetery was investigated by V. H. Borodulin and V. K. Mikheev. In catacomb no. 21 (fig. 3) in a female burial was found anthropozoomorphic fibula — type VI-D according to O. M. Prykhodniuk or type II.1 according to V. Rodinkova. The date of the burial is debatable: V. S. Aksionov dates it within the boundaries of 750—770, while O. V. Komar believes that it belongs to the Middle Saltiv horizon II, that is, from 790s. Varvarivka hoard discovered in 2017. The complex includes: tools associated with metalworking, handicraft products for general purposes and for the processing of organic raw materials, household items. Bronze items are divided into three groups: armour details (?), raw materials and jewellery. A fibula, similar to the find from catacomb no. 21 of the Staryi Saltiv cemetery, belongs to the items of the Pastyrske circle. Khorosheve hoard discovered in 2021. The asssemblage includes: implement for working with metal, raw materials and weapons. The rest of the items are bronze jewellery, most of which belong to the Pastyrske circle: one earring and three fibulae. All the considered monuments of the Saltiv culture with finds of jewellery from Pastyrske hillfort are concentrated in the Siverskyi Donets basin. The main stage of their existence is defined within the chronological boundaries of the Pastyrske hillfort existence — the middle of the 7th — the middle of the 8th centuries. Two hoards of the Pastyrske circle are known in this region — Zaitsiv and Korobovi Khutory. Archaeological finds of fibulae and an earring of this circle were also revealed in this region. These data indicate that the Slavic population with significant cultural and trade ties with Pastyrske hillfort lived in the Siverskyi Donets basin during the second half of the 7th — the first half of the 8th centuries. The chronology of burial no. 29 of the Sukha Homilsha cemetery differs from the chronology of the existence of the round pendant by at least half a century (table 1). The chronology of the hoards from Varvarivka and Khorosheve is embedded in the general boundaries of the Saltiv culture existence: from 740—750 — the first decades of the 10th century. The chronology of the female burial from catacomb no. 21 of the Staryi Saltiv cemetery is debatable: 750—770 or from the 790s. An analysis of items belonging to the Pastyrske circle from the sites and assemblages of the Saltiv culture indicates that these adornments could have been reused. They do not necessarily indicate the contacts of the Slavic population with the inhabitants of the Khazar Khaganate.

Coupled luminescence and cosmogenic nuclide dating of postglacial deflation surfaces and sand drift on a raised ice-contact delta at Veinge, SW Sweden

Wind-abraded cobbles (ventifacts) and aeolian sand are known from the sandy-gravelly coastal areas of south-western Sweden, especially in association with raised deltas. Ventifacts are recorded on at least two different stratigraphic levels, at some sites atop glaciofluvial sediment, at other sites atop littoral deposits, and in some places at both levels, while aeolian sand usually forms a surficial cover. The formation of ventifacts has usually been coupled to abrasion due to katabatic winds from the retreating ice sheet or with periglacial climate during the Younger Dryas stadial (12.8–11.7 ka).To determine the timing of these deflation events, we have applied a combination of dating methods to ventifacts and associated sediments on top of an ice-contact delta at Veinge, south-western Sweden. Quartz and feldspar luminescence dating as well as portable luminescence profiling has been used for littoral and aeolian sediments over- and underlying deflation surfaces, while rock surface luminescence burial dating and paired 14C–10Be cosmogenic nuclide dating were conducted on ventifacts. The results show that a first deflation event occurred c. 16.5 ka, just after deglaciation and prior to a regional transgression that peaked around 15.7 ka. At 12.4–11.4 ka, during the Younger Dryas stadial, a new set of ventifacts formed on the surface of the exposed littoral sands and gravels. Some wind abrasion also occurred in the early Holocene, but at c. 8.5 ka the surface was covered by aeolian sand, up to 2.5 m thick.The combination of different dating methods have allowed us to draw more informed conclusions on the timing and duration of these wind abrasion/transport events than would have been possible from the use of only single-method dating. It has also made it possible to infer some environmental conditions during deposition. For example, both glaciofluvial and littoral deposits show evidence of incomplete bleaching of the luminescence signal. This suggests short subaerial transport and brief reworking by waves, respectively, though bleaching conditions improved during shore regression. Rock surface burial luminescence profiles reveal that some ventifacts were repeatedly exposed, but that later event(s) were shorter in duration as indicated by quartz-feldspar age comparisons.

Exploring the potential of rock surface luminescence from glacial sediments: dating and transport history

The dating of moraine deposits can present challenges to standard geochronological methods; terrestrial cosmogenic nuclide (TCN), sediment luminescence and radiocarbon dating may suffer from problems of incomplete resetting (by inheritance, intermittent cover/exposure, transport under unfavourable conditions) and/or a lack of suitable (organic) material. Rock surface luminescence burial dating (RSLBD) offers an alternative approach with considerable potential in dating moraines. In RSLBD, large cobbles/boulders are targeted, rather than smaller grains usually used in luminescence dating. The age limit of RSLBD is much higher than that of radiocarbon dating, and rocks are much more readily available than organic material. In contrast to TCN dating, the effect of exposure prior to deposition can be measured. In this study, we sampled a broad selection of primarily granitic boulders of various sizes and shapes (e.g. different degrees of roundness and sphericity) from the Vimmerby Moraine, a prominent and accessible feature in southern Sweden dated using TCN to 14.4±0.9 ka. Our study was designed to test whether morphological characteristics can be used to discriminate in favour of the most light‐exposed boulders and minimize measurements of non‐exposed boulders. As expected, not all RSLBD ages can be attributed to the same depositional event, but the majority of the resulting ages provide a mean age of 13.0±1.5 ka, consistent with the cosmogenic nuclide dating of the Vimmerby Moraine. Despite the apparently successful TCN study, the luminescence–depth profiles measured in the buried surfaces of the sampled clasts indicate that >50% of these moraine boulders were exposed to light (and cosmic radiation) before final deposition, implying some (presumably small) TCN inheritance; seven of the 16 boulders identified as light exposed were sufficiently bleached to be useful for RSLBD. These results and their implications in regard to transport and deposition of the sampled cobbles are critically discussed and evaluated.

«Старые» и новые венгерские погребения на левобережье Днестра

The article analyzes the materials obtained during the study of five Hungarian burials on the left bank of the Lower Dniester. Description of the of the barrow and the grave: Burial near the Butora village, which was sunk into an Early Bronze Age mound and contained a horse’s humerus and fragments of gold foil, was studied in 1978; it was previously published with erroneous cultural-chronological attribution or as uncertain. Two more graves were discovered in 1992 in Early Bronze Age mounds near the town of Slobodzeya. Until recently, archival documentation was considered lost, and anthropological materials and grave goods were not identified. А fragment of an iron steel was found in one of the burials. Bone plates for a bow, iron arrowheads, two iron knives (a long combat one and a short household one) were found in another burial. A Hungarian grave sunk in a Scythian mound was studied near Glinoe village, Slobodzeya district, in 2022, in the kurgan group “Sever”. A fire flint, an iron arrowhead, an awl and a knife, as well as gold foil and a horse’s humerus were found in the grave. A burial containing the humerus of small cattle and an iron arrowhead was excavated in 2023 in the Early Bronze Age mound situated at the “Kulak” cemetery near the Korotnoe village. Grave from the Butory cemetery, one of the burials near the town of Slobodzeya, as well as graves in the “Sever” group and from the “Kulak” cemetery were radiocarbon dated. Burial dating: Analogies to grave goods, as well as seven radiocarbon dates obtained in the Poznan, Kiev and Debrecen laboratories, allow us to date graves to the second half of the 9th – the first half of the 10th century. Final remarks: These burials, together with the Hungarian graves previously discovered in the North-Western Black Sea region, are archaeological sites left by the Hungarians east of the Carpathians immediately before finding their homeland.

Dating the late Miocene marine sediments around the southern middle Durance valley (Provence, SE France): new evidences for a Tortonian age

The present study aims dating the topmost 50 m of a 115 m-long core retrieved from a valley located in the Cadarache Area (Upper Provence, South East France). Based on burial dating by in situ produced cosmogenic nuclides (10Be, 26Al and 21Ne), and paleomagnetic analyses, a Tortonian age was determined for the sedimentary succession exhibited in the core. In addition, thin sections, grain size analyses and quartz morphoscopy were used to characterize a shallow marine environment and to correlate the sediment core to the surrounding exposed sections. When comparing the studied sedimentary record to global sea level estimates, we establish that the local Tortonian transgression was not synchronous with the global scale sea level high-stand, but happened more likely later, during a global regressive trend. The timing of the Tortonian flooding in Upper Provence was therefore most probably driven by regional tectonic forcing. Finally, the Tortonian shallow marine sediments are topped by lacustrine tight carbonates. These carbonates protect the marine sediments from the following major erosional events resulting from the Messinian sea level drop and from interglacial-glacial fluctuations that both yielded to the present-day valley topography.

Luminescence rock surface exposure and burial dating: a review of an innovative new method and its applications in archaeology

Luminescence rock surface exposure and burial dating: a review of an innovative new method and its applications in archaeology

Indirect dating of secondary cave burials in the Massim region of Papua New Guinea reveals last millennium reorganisation of social practices

ABSTRACTIn the Massim Island region of southeastern Papua New Guinea secondary interment of skeletal remains was widely practiced historically, but its social context and regional expression in the deeper past remains uncertain. In this paper the chronology of secondary burial on Panaeati Island is established indirectly by reconstructing the cultural and spatiotemporal association of 21 clay pots placed with human skeletal remains at Biniwaga Cave, coincidently establishing the first whole vessel typology of Southern Massim Combed Pottery (SMCP) and Southern Massim Pottery (SMP). Comparison with excavated pottery assemblages on Panaeati and elsewhere in the region demonstrates that the Biniwaga pots are consistent with SMCP and early SMP, dating from 740 to 470 calBP. Secondary burial practices on Panaeati are contemporary with those recorded elsewhere in the region and coincide with changes in pottery production centres. Compared to excavated pottery assemblages from contemporary sites, a relatively narrow range of pots are represented at Biniwaga. It is hypothesised that pots were selected to reflect the cultural affiliation of deceased individuals during a period of increasing inter‐island interaction.

Miocene cave sediments record topographic, erosional and drainage development in the Western European Alps

The dynamic Neogene evolution of the Western European Alps included exhumation of the external crystalline massifs, thrust propagation to the foreland, drainage network reorganization, and major climatic variations. To constrain possible interactions between those factors, accurate geomorphological and sedimentological archives are required. However, intra-orogenic areas are subject to erosion, and extensive glacial cover during the Quaternary erased most of the geomorphic markers in the Alps. For these reasons, the genesis of the main features of the modern landscape, such as the major valleys and the drainage network, remains poorly understood. This study highlights how recently discovered karstic archives from the perched paleo-karst of the Obiou peak (Dévoluy massif, SE France) record the tectonic and drainage-network evolution of this part of the Alps during the Neogene. The Obiou caves are located at 2250-2380 m elevation, ∼1600 m above the modern Drac valley; they contain fluvial deposits including sand-clay units and rounded crystalline cobbles derived from the adjacent Ecrins-Pelvoux massif. As the Dévoluy and Ecrins-Pelvoux massifs are currently separated by the axial Drac valley (a major tributary of the Isère River), these cave sediments must have been deposited by a radial drainage system before incision of the modern Drac. We report new multi-method results from these sediments, including cosmogenic-nuclide burial dating (21Ne, 10Be, 26Al in quartz), provenance analysis (clast petrography and heavy-mineral analysis), and detrital thermochronology (apatite fission-track and (U-Th)/He) combined with a paleo-environmental reconstruction from palynology. 21Ne/10Be dating of cobbles and sand constrains the burial age to 11.5 ± 1.5 Ma, providing a maximum age for the modern axial drainage system and a minimum long-term incision rate of ∼140 m/Myr for the Drac valley. Comparison of the combined data to both modern rivers and nearby Oligocene foreland-basin deposits provides evidence for two successive drainage reorganizations. Early Miocene exhumation and development of high topography in the Ecrins-Pelvoux massif, linked to localized thrusting on a crustal-scale ramp, led to initial deflection of the antecedent radial drainage network, beheading its headwaters by establishment of the axial upper Durance valley. Subsequent propagation of thrusting into the subalpine Dévoluy massif and associated uplift during the mid to late Miocene led to establishment of the modern drainage system.

Jewellery of the Martynivka Circle among Materials of Saltiv Culture: Data Analysis

In the paper jewellery from sites and complexes of the Saltiv culture, which do not chronologically fit within the boundaries of its existence, is considered. The studied jewellery is typical for the hoards of Martynivka circle (group II, subgroup 1). It is represented by four burial complexes and one hoard. Dmytriivka cemetery was investigated by S. Pletneva. Two trapezoidal pendants ornamented with punched rows of dots on the edge from catacombs no. 151 and no. 154 (fig. 1A: 1). Items from the Khatskivskyi hoard, the Kovrai locality, and three finds from the Luchistoye burial ground are known with such an ornamentation system. In general, such pendants can be dated by the 5th—7th centuries (fig. 1). Sukha Homilsha cemetery 1 was investigated by V. Mikheev. Burial no. 54 contained a vorvorka (fig. 2). Burial date: late 8th—early 9th centuries. Analogies in size are presented in several hoards, in ornamentation — from the settlement of Kryvets 4. In general, these items are typical for the hoards of Martynivka circle, the second half of the 6th— the middle third quarter of the 7th centuries. Bochkove cemetery has been studied by O. Laptev since 2014. Grave no. 2 (fig. 3; 4) contained two trapezoidal pendants ornamented with four spherical protrusions and two rows of pressed dots along the edge (fig. 5; 6). Similar pendants are associated with the Penkivka monuments and hoards of the Martynivka circle. Myrna Dolyna hoard discovered in 2019. The complex includes: 1) blacksmith tools and several iron items (fig. 7: 1—11); 2) four screams (fig. 7: 12—15); 3) fragments of a bronze cauldron and a pair of phaleras (fig. 8); 4) heraldic belt decorations, including matrices and semi-finished products (fig. 9; 10); 5) Roman coins (fig. 11). Only six heraldic decorations (fig. 9: 1-3; 10: 1—3) are known among Slavic antiquities at the level of broad analogies. All the considered sites of the Saltiv culture with finds of jewellery from the Martynivka circle are concentrated in the Siverskyi Donets basin. Both individual finds and treasures are known here. In the upper reaches of the river, monuments of the Kolochyn culture are known, and below — of the Penkivka culture. The chronology of the complexes of the Dmytriivka cemetery and the Myrna Dolyna hoard can be determined within the general framework of the existence of culture. However, the chronology of burial no. 54 of the Sukha Homilsha-1, burial no. 2 of the Bochkove cemetery and the chronology of the Martynivka circle decorations differ by almost a century (table 1). Consequently, such adornments could be found by the inhabitants of the Khazar Khaganate and reused in everyday life or attire.

Новая находка провинциально-римских шарнирных брошей с эмалью и мозаичным стеклом на Северном Кавказе

In 2018, in the course of the works by the Joint North Caucasian Archaeological Expedition of the State Historical Museum, KBSU, KBNTs and IA RAS, female burial 124 was discovered at the Zayukovo-3 burial ground in the Kabardino-Balkarian Republic. Two Roman brooches with enamel inserts were found near the waist of the buried woman. Probably, the jewelry was used as fasteners of a woven belt. The burial dates to the first half of the 3 rd century AD.

LATE ARCHAIC BURIAL 470 FROM THE NECROPOLIS OF PHANAGORIA

As a result of the archaeological excavations of the Bosporus necropolises, anthropological collections have been collected and published over the years, giving an idea of the morphological type of ordinary rural and urban residents in different chronological periods. M. M. Gerasimova studied material from the necropolis of Phanagoria, which dates back to the III century BC — IV century AD. The series consists of 58 adult skulls (32 male, 24 female) and 2 children’s skull. The author concludes that the buried belonged to the Pontic variant of the Mediterranean race. The Hellenistic, Sarmatian and Sindo-Meotic components are distinguished, with the latter being predominant.
 The proposed publication is devoted to a find obtained from the necropolis of Phanagoria in 1988. A male skeleton (No. 470) was discovered on the southeastern outskirts of the settlement, among children’s burials, and was located in a ground pit with shoulder pads, rectangular in plan. The inventory consisted of a red clay amphora, a black-glazed kylix, an iron akinak dagger, an iron spearhead, a gray clay bowl, and a black-figure lekyph. The burial dates back to the last third of the VI — the first two decades of the V century BC and belonged, according to the author of the excavations O. A. Zavoykin, to a nobility. The deceased was buried at the age of 30—40. The skull is brachycranic, with a wide, medium-high face, has large longitudinal and transverse diameters and a rather powerful bone structure. The significant flattening of the facial area in the horizontal plane attracts attention. The height of the buried person (calculated according to the formula of M. Trotter and G. Glaser) is 169.6 cm. The set of features of the considered skull is a brachycrania in combination with a fairly wide, medium-high face, flattened in the horizontal plane, characteristic of archaeological sauromatians and early Sarmatians.
 The craniological parameters of the considered skull approach the maximum values on the world intergroup scale and are extremely far from the usual set of features characteristic of most ancient series in the territory of the entire Northern Black Sea region. Undoubtedly, the burial is unique, judging by the finds in the grave, which indicates a certain status of a man — a warrior. However, the noted features — brachycrania with weakened horizontal profiling at the upper and middle levels, in combination with the descriptive characteristics of the burial — do not fit into the framework of the known Mediterranean series. This may indicate his origin from a different ethnic environment than the Hellenic one. A similar set of features is characteristic of a number of Sarmatian groups. The material of this well-dated burial complex may be evidence of a rather early penetration of the barbarians into the local Hellenistic circle of the inhabitants of Phanagoria.

A Study of Silk Fabric from the Xiongnu Age Under-Headdress Discovered at Yaloman II Mound 51 in the Central Altai

We describe a large fragment of fabric from the under-headdress excavated from mound 51 at Yaloman II—a site on a high terrace near the place where the Bolshoy Yaloman fl ows into the Katun, Central Altai. Various criteria, including radiocarbon analysis, suggest that the burial dates to the Xiongnu Age (200 BC to 100 AD). The structure of the textile was assessed microscopically. On the basis of morphological criteria, the fi bers were identifi ed as silk. The fabric is described according to the accepted international standards. Results attest to the use of a treadle loom for producing polychrome silk fabric, from which the early nomads sewed a headdress in the form of a cap or bonnet. Such a prestigious material was produced in limited quantities in China to decorate details of clothing worn by the elite. Decorative silk items could have been imported from there to the Altai as gifts received by the leader of the nomadic Xiongnu Empire in Inner Asia. The Altai was part of this empire, as demonstrated by the entire assemblage of funerary items from Yaloman II.

Radiocarbon Dating of Late Bronze Age Burials from the Great Urals (Steppe Trans-Urals and Northern Kazakhstan) and Bayesian Modeling

ABSTRACT In the last two decades, the Bronze Age chronology of the Great Urals was revolutionized by the first large-scale radiocarbon dating programs. Since then, the chronology of the Bronze Age in this area has been under discussion. In this paper, we present 23 new AMS dates from Late Bronze Age sites in the steppe and forest steppe areas of the southern Trans-Urals and northwestern Kazakhstan. This includes the first successful dating of cremated bone samples from this area. Bayesian modeling was conducted to date the Late Bronze Age into three chronological phases. The considerable number of outliers suggests previously undetected biases in the material. In addition, we found differences between the Bayesian models of the steppe and forest steppe areas that are not reflected in the archaeological record. This study emphasizes the value of Bayesian modeling for the prehistoric chronology of the Great Urals but also highlights its issues.

Погребальные комплексы геоархеологического местонахождения Усть-Кеуль 1 (Северное Приангарье): проблемы культурно-хронологической идентификации

This paper presents results of a study of two burial complexes from the geoarchaeological site Ust-Keul 1 in Northern Angara region (excavations of 2012). Mortuary rites and grave goods were analyzed, thus making clear the issue of cultural affiliation of these complexes and defining their uniqueness for the Baikal-Yenisei Siberia. The burials were made by a method of inhumation in ground graves. In both cases structures above and within the graves are absent. The accompanying burial goods are presented by arrowheads with a triangular shape, a concave base and equally large barbs, and by a horn made connector (a cartridge case), the one that was used to attach the stone arrowhead to the arrow shaft. Results of the radiocarbon dating determine the age of the burials by the Late Bronze Age – the Early Iron Age. The dating raises the question about a time of the Tsepan culture bearers` infiltration into the Northern Angara region. Results of the odontological analysis are presented and even based on the description of the extremely fragmented remains, it was possible to define sex and age characteristics of the buried ones. The unearthed fragments and isolated teeth belonged to three individuals. The stage of tooth crowns formation and dental enamel erosion are indicators of the age of the buried ones. Two of them are adolescents (burials 1 and 2, individual 2), and the age of the third individual (burial 2, individual 1), based on the erosion, is between 35–45 years. The results of our research obtained not only with reliance on analogies with other burials in the Northern Angara region but also based on credible radiocarbon data, corroborate the assumption of a somewhat earlier dating of the Tsepan culture burials. There is a discussion about possible infiltration of the Tsepan culture bearers in the Northern Angara region at the end of the Late Bronze Age. However, the issue of a more reliable chronology of these burials under study still remains relevant. The radiocarbon data indicate, at first sight, their earlier age but measurements obtained for burial 2 from the two individuals have large discrepancies. Additionally, they may appear older due to a freshwater reservoir effect. The accompanying burial goods are scarce but allow us, with confidence, to define the burials from Ust-Keul 1 site as belonging to the Tsepan culture.