Preliminary Reports on the Excavations at Burgut Kurgan and Bobolangar in 2017
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STUDIA HERCYNIA XXII/1, 158–182 Preliminary Reports on the Excavations at Burgut Kurgan and Bobolangar in 2017 Jan Kysela– Anna Augustinová– Rebecca Kinaston ABSTRACT The current report presents the results of the 2017 excavations of two prehistoric sites in, or in the vicinity of, the Zarabag Oasis, South Uzbekistan. In the Yaz Isettlement of Burgut Kurgan, the 2017 excavation season focused on asmall portion of the stone wall and was not able to confirm the presence of agate hypothesised during the 2016 excavations. Atrial excavation consisting of three trenches (BBL01–BBL03) was conducted at the site of Bobolangar, which was discovered during aprevious field survey in 2016. The pottery sherds collected on the surface of Bobolanghar were from the Late Bronze Age and the date of the site was confirmed by the presence of Late Bronze Age pottery in secure stratigraphic contexts. Moreover, two burials were found in trench BBL03. Based on the characteristics of the burial traditions, it is likely that both individuals were interred during the Middle Ages and the graves were cut into the Late Bronze Age layers of the site. The human skeletons were exceptionally well ‑preserved and preliminary details of the bioarchaeological analyses are presented here. KEYWORDS Central Asia; Sapalli culture; Yaz Iculture; Late Bronze Age; Early Iron Age; burial; anthropological analysis. Similar to the previous years, the activities of the 2017 Czech ‑Uzbekistani archaeological mis‑ sion in the Pashkhurt Valley, south Uzbekistan, consisted of aseries of surveys complemented by targeted excavations. The results of the surveys are presented elsewhere in this volume, as are those of the excavations of the kurgan ‑like features. The present report summarises the excavations of two prehistoric settlement sites conducted in 2017: the Early Iron Age Burgut Kurgan and the Bronze Age site of Bobolangar. BURGUT KURGAN (JK) The excavation of the Yaz Isite of Burgut Kurgan was conducted over aperiod of three field seasons, from 2015–2017 (cf. Stančoetal. 2016; Kyselaetal. 2017). In comparison with the previous field seasons (2015 and 2016), the 2017 excavation took place in arather limited area corresponding with an enlargement of the south eastern part of trench BK06, which was initially excavated in 2016. The dimensions of the 2017 trench were 4×7 m (Pl. 4/1). The principal objective of the 2017 excavation was to confirm or deny the existence of a‘passage’ in the stone wall (BK06_031/043) that was preliminarily identified in the later stages of the 2016 excavation (Kyselaetal. 2017, 96). The possible ‘passage’ manifested itself as agap, slightly more than 1 meter wide, between two portions of the stone wall (BK06_031 and BK06_043), with alarge flat stone in the middle. In 2016, the working hypothesis of the interpretation of this gap was that it was agate that was contemporary with aphase of set‑ tlement discovered in the previous excavations. It was previously suggested that the possible
159JAN KYSELA– ANNA AUGUSTINOVÁ– REBECCA KINASTON gate had either been filled for one reason or another, or that the gate was contemporary with alater occupation that reused the older site– in this latter case the flat stone would act as athreshold. The excavation produced some rare evidence of occupation that probably occurred after the abandonment of the main phase of settlement of the site. This evidence included apit (BK06_048/049) dug into the upper levels of the wall that was topped with stones. The only pottery fragments from the fill of this pit date to the main occupation phase of Yaz I(Early Iron Age). However, these pottery fragments may have been redeposited within the fill when the pit was dug and therefore we cannot be sure if this pit was created during amuch later visit to the site. After removing the wind deposited upper layers (BK06_045, BK06_051, BK06_056), the top of mudbrick walls (BK06_052 and BK06_053) appeared in the eastern part of the trench. In the central and north ‑western part of the trench, similar structures appeared only at alater stage below layer BK06_057 and flush with the wall BK06_052. The stratigraphy indicates that structures in the central and western part of the trench (BK06_060 and BK06_065) were constructed earlier than BK06_052. Fig. 1: The trench BK06– state of research in 2016 and the extent of the 2017 excavation (black rectangle). In the insert above right– the position of the trench BK06 in the site. Drawing by J. Havlík.
160 STUDIA HERCYNIA XXII/1 Fig. 2: The presumed gateway. Photo by J. Kysela. Fig. 3: Overall plan of the 2017 excavation in Burgut Kurgan. Drawing by J. Kysela.
161JAN KYSELA– ANNA AUGUSTINOVÁ– REBECCA KINASTON The small structure BK06_060 was in the form of asemi ‑circular wall attached to the stone wall BK06_043/031. In the western part of the trench, another very similar structure to BK06_060, labelled BK06_065, appeared at an even deeper stratigraphic position. However, only the lowest mudbrick courses were preserved from both structures; both were probably contemporary and built on the same level. BK06_060 was filled in with very loose layer (BK06_059) which contained numerous pot‑ tery sherds. It had aclear, well ‑preserved beaten floor (BK06_074) that had traces of lime and organic temper in it. On the other hand, in BK06_065 the fill (BK06_064) was rather stony and poor in finds; the floor was paved with pottery fragments similar to the so called ‘kata’ in trench BK03. The area between the two structures was covered by alayer (BK06_066/067) containing numerous mudbrick fragments and pottery sherds that were lying flat. Asmall pit (BK06_068/069) was dug from layer BK06_066/067. This was apparently the first occupation horizon because all layers and structures rest directly on ‘anthropized virgin soil’– sterile soil that has cultural artefacts pressed in it from above– indicating the earliest period of human occupation. As far as the stone wall is concerned, the 2017 excavation aimed to clarify the existence of the presumed gateway between BK06_031 and BK06_043 and understand the chaotic state of the inner portion of BK06_043. First, the excavation failed to verify the hypothesis of agate in the wall. The space of the assumed gateway was filled with large stones (up to 70 cm) packed in compressed pakhsa; the stones were however mutually interlocked throughout the entire volume of the fill and at no level were we able to identify asurface which could have served as awalkable horizon. This was the case throughout the entire thickness of the wall down to its lowermost level consisting of huge boulders set into apakhsa bank. This pakhsa bank Fig. 4: Structures BK06_060 (left) and BK06_065 (right) excavated. Photos by J. Kysela.
162 STUDIA HERCYNIA XXII/1 (BK06_075 and BK06_070) could be identified throughout the entire excavated part of the wall. Aboulder facing was used on the outside. The inside was left without afacing in the western part of the wall (BK06_043), and was largely not preserved. In fact, the western portion of the wall was preserved only on the exterior while the interior seems to have been damaged as the entire inner face of the wall was missing. In the north ‑westernmost part of the trench, some stray stones (already outside the limits of the wall and therefore presumably remnants of its destruction) were in direct contact with structure BK06_065. The relationship between the fallen stones and BK06_065 could not be determined and it was unclear if BK06_065 was built at the foot of the stone wall and was covered by its destruction or if it was built after the stones had already fallen. What is clear is that the phase of the semi ‑circular structures was not earlier than the construction of the stone wall BK06_043 because the mudbrick structures either rest against it or are covered by its partial destruction. The structures are covered by the straight mudbrick walls (BK2017_06_053 and BK2016_06_027) and were possibly destroyed by activities taking place around the latter. The stone wall remained in service in this later phase. The supposed gateway is likely only arepair to maintain the function of the wall in the later period of its existence. The 2017 excavation provided new, valuable information on the site’sgeneral stratigraphy as well as so ‑far unknown construction features (i.e. the two semicircular structures en‑ countered for the first time at the site). The tasks for the near future include synthetising the Fig. 5: The phases of excavation of the assumed gateway. Photos by J. Kysela.
163JAN KYSELA– ANNA AUGUSTINOVÁ– REBECCA KINASTON stratigraphic sequences of the single trenches, all of which differ from each other in minor ways, and outlining asingle all ‑encompassing construction history for the site. THE TRIAL EXCAVATION ON THE SITE OF BOBOLANGAR, ZARABAG OASIS (AA, JK) INTRODUCTION The site of Bobolangar is situated at the west margin of the village and oasis of Zarabag above the abundant spring of Bobolangar (37°45’43.45”N, 66°44’25.40”E, 998 m.a.s.l.). The oasis of Zarabag, located in the Pashkhurt Valley of the Surkhan Darya province, south Uzbekistan, lies in the steppe belt of the Kugitang mountains piedmont, which also represent the boundary between Uzbekistan and Turkmenistan (15 km to the west from Zarabag village). Bobolanghar (bobo = Uzb. ‘old man’; langar = Uzb. ‘shadoof/well pole’) was detected during the field survey in the oases of Kugitang Piedmont in 2016 (Augustinováetal. 2017, 104–148, 185–188). The site is situated on asmall spur of adescending dry stony ridge on the right bank of the seasonal river Machayly1 (approximately 120 m from the riverbed). In the vicinity of the site there is awater source of identical name– Bobolangar Buloq (buloq = Uzb. ‘spring’). The site was vis‑ ibly disrupted by the activities of local inhabitants and arescue excavation was warranted. Based on the plentiful assemblage of ceramic fragments collected from the surface the site, Bobolanghar was preliminarily dated to the Bronze Age. Bobolanghar is situated on aflat platform on top of the spur with size 25×35 m (Fig. 6). The remainder of aprobable water canal, which is not in use today, skirts the site from the west, north and east sides. On the surface, there are clearly visible remains of stone struc‑ tures in two basic shapes– rectangular and circular (d. ca. 1.5 m). These structures, as well as abasic topographic plan of the site, were recorded by total station and are depicted on the plan Fig. 7. The site lies in the vicinity of gardens and, because it is shaped as amound, it offers an easy way to access clay for more recent building and agricultural activities. As aresult, these activities disrupted the surface of the site and brought to light archaeological materials and structures. There were two substantial terrain disturbances caused by more recent clay digging– one on the north ‑west and one on the south ‑east side of the site. Most of the rich archaeological material collected from the field prospection during the 2016 season came from these two areas, but numerous ceramic fragments were also scattered across the surface of the site. The areas of the surface disturbance determined the placement of the 2017 trenches. EXCAVATION Aim and methods of the excavation There were several objectives for the excavation of the Bobolanghar site. The first was arescue excavation to mitigate any further damage caused by the more recent disturbance of the site. 1 The majority of water flows through the Machayly River in the spring; during the rest of the year, only aslight stream flows or the riverbed remains dry.
164 STUDIA HERCYNIA XXII/1 The second aim was to collect the relevant data for dating and define the function of the site in each specific historical period. The third aim was to assess the site’ssignificance in the context of the other sites in the region– with afocus on the Late Bronze Age period. Three trenches were opened (BBL01–BBL03; Figs. 6–7) in areas adjacent to the disturbances at the site. The first trench (BBL01) was opened on the top platform and corresponded with an Fig. 6: The placement of trenches at the site Bobolangar– view from south ‑west. Photo by A. Augustinová. Fig. 7: Plan of the site of Bobolangar with trenches BBL01–BBL03 highlighted; dashed line– stone structures visible on surface. Mapping in the field conducted by P.Cejnarová and A. Augustinová; plan by A. Augustinová.
165JAN KYSELA– ANNA AUGUSTINOVÁ– REBECCA KINASTON oval stone line; the second one (BBL02) was located on the site’seast edge and acted to straight‑ en and clear the profile disrupted by more recent clay digging; the third trench (BBL03) was placed on the south ‑west of the site, and cleared the disrupted surface of an area delimited by astone structure visible on the surface, with afurther extension into the non ‑disrupted parts of the stratigraphy. The excavation was conducted and documented by Jan Kysela and Anna Augustinová (both Charles University, Prague– Czech Republic). The skeletal remains uncovered in trench BBL03 were excavated and studied by bioarchaeologist RebeccaL. Kinaston (University of Otago, New Zealand) and documented with photogrammetry by Tatiana Votroubeková (Charles University, Prague– Czech Republic). The basic topographic plan and other geodetic measurements were carried out by Petra Cejnarová and Anna Augustinová (Charles University, Prague– Czech Republic), and subsequently processed by Anna Augustinová. The archaeological finds were primarily dated according to the expert examination of Shapulat Shaydullaev (Termez State University, Uzbekistan). Trench BBL01 The trench BBL01 (2×3 m) was opened on the eastern part of the top platform of the site (Figs. 6–7). Its placement was chosen based on an oval feature delimited by stones (oriented to NNE ‑SSW) visible on the surface, that was preliminarily interpreted as the remains of agrave (Fig. 8). Excavations took place exclusively inside the oval stone structure where four stratigraphic layers were recognized (BBL01_002, BBL01_006, BBL01_007, BBL01_008). At the depth of 0.65 m (BBL01_008), several pieces of human bone were found. At the depth of 0.71 m, we discovered the remains of awooden structure, samples of which have been taken for analysis that are currently underway. Eleven stratigraphic units were distinguished within the trench (BBL01_001–BBL01_011). The ceramic fragments found in trench BBL01 were consistent with pottery from the Late Bronze Age and date to this period (overall, 183 ceramic fragments have been collected, 34 of them were diagnostic; Tab.1). The preliminary assumption that the oval stone structure represented agrave was con‑ firmed, nevertheless it does not correspond with the burial habits of the Bronze Age. 2 In Bobo ‑ langar the presence of Late Bronze Age ceramic fragments in the fill of the grave pit was likely aresult of secondary soil deposition during grave digging and filling. With the exception of the few bone fragments there was no skeleton present and it was therefore likely disturbed after burial. Remains of awooden container or possible structure were preserved in the north part of the grave pit and extended beyond its circumference to the west (Fig. 9). The wooden fragments may represent the remains of acoffin, but they may also have been part of some earlier construction. Based on the surface appearance of the grave (oval of stones) and its orientation (NNE ‑SSW), we suggest that it was dug in the Middle Ages after the coming of Islam into the Central Asia in 7th century AD. 2 There is variability in the Late Bronze Age grave types. The necropolis could be part of the settlement area as in the case of Sapalli Tepa (Askarov 1973; Teufer 2015, 7–14) or the burial ground could be created in separate area as in Džarkutan (Askarov– Abdulaev 1973; Teufer 2015, 19–22) or Bustan (Teufer 2015, 22). In none of these cases are the graves marked on the surface by loose lying stones. The shapes of the grave pits are variable (most frequented types of graves are catacomb graves, pit graves and ditch graves) and they take shape on surface of rectangle or irregular circle. The skeletons are situated on the side with bent limbs.
166 STUDIA HERCYNIA XXII/1 Fig. 8: The trench BBL01 at the site Bobolangar after cleaning of the surface. Photo by J. Kysela. Fig. 9: The remains of the wood container or structure at the bottom of the grave. Photo by J. Kysela.
173JAN KYSELA– ANNA AUGUSTINOVÁ– REBECCA KINASTON CONCLUSION During the 2017 trial excavation at the site of Bobolangar we confirmed the preliminary as‑ sumption, based on the surface collection of pottery fragments during the 2016 field survey, that the site was aLate Bronze Age settlement. During the excavation we detected several settlement horizons dated to the Late Bronze Age. In the trench BBL02 we documented several floor levels in addition to cultural layers. Asimilar situation was also observed in trench BBL03, where at least two Late Bronze Age settlement horizons (including aburnt horizon) could be distinguished that were later– probably in the Middle Ages– disrupted by burial activity (cf. below). The orientation of the human skeletons uncovered in trench BBL03 corresponded with the orientation of the grave pit inside the stone oval in trench BBL01. Both skeletons in BBL03 were aligned with the small stone quadrangular feature on the surface (BBL03_003) in terms of orientation and dimension. The quadrangular stone enclosure may therefore be considered asurface marking of agroup of graves akin to the stone oval that marked the assumed grave in BBL01. The same interpretation– i.e. surface markings of graves or grave clusters– may be at least hypothetically advanced for all the stone features documented on the surface. Even though the backfill of the graves contained pottery fragments dated to the Late Bronze Age, these were likely deposited when the graves disturbed the earlier– i.e. the Late Bronze Age– settlement layers. Based on the orientation and design of the graves, we suggest that they date to the Medieval Period– after the arrival of the Islamic culture into the area in the 7th c. AD. ANTHROPOLOGICAL ANALYSIS OF THE SKELETONS FROM THE SITE OF BOBOLANGAR, TRENCH BBL03 (RK) Two single interments, designated burials 1 and 2, were found in trench BBL03 at the site of Bobolangar. As discussed, it was originally thought that the burials were Bronze Age in‑ ternments. However, the burial position of the two individuals (flexed on right side), lack of burial goods, and presence of broken Bronze Age ceramics in the grave fill of both burials likely indicate that both individuals were from alater period– possibly the Medieval Period. The following is apreliminary description of the burials and amore in ‑depth publication is in preparation. AMS dating and ancient DNA analysis of both burials is currently underway at the Max Planck Institute for the Science of Human History, Jena, Germany. For both individuals, stable isotope analysis of carbon, nitrogen and sulphur will be undertaken to assess paleodiet. Strontium and oxygen isotope analyses will be conducted to assess migration. Microparticle analysis of dental calculus is currently being organised. Histological analyses of the ribs are currently underway to assess health. THE BURIALS Burial 1 Burial 1 was achild interred in asemi ‑flexed position on its right side oriented northwest by southeast, head facing west (Fig. 15). The bone preservation was excellent and the skeleton was complete with the exception of some missing hand and foot phalanges. The left parietal and orbit were crushed when first found but otherwise the skull was intact, albeit crumbly from sun exposure. Rocks were present around the pelvic area and these may have been part of the burial fill or intentionally placed there. There was adisturbance to the right upper
174 STUDIA HERCYNIA XXII/1 thorax of burial 1 after decomposition as the manubrium of the sternum was found above the left shoulder and the right upper ribs were not in anatomical position. The age of burial 1 was estimated as 8–10 years from the extent of epiphyseal fusion, tooth eruption and tooth formation (Scheuer– Black 2000). The only pathology observed on the postcranial skeleton was apossible healed periosteal reaction on the anterior surface of the proximal end of the left tibia, which is anon ‑specific indicator of physiological stress and infection, but may also result from trauma (Fig. 16). Burial 1 had amixed dentition (i.e. includes both permanent and deciduous teeth). The remaining deciduous teeth– the max‑ illary and mandibular molars– displayed high rates of tooth wear (grades 5–8, Scott 1979) (Fig. 17). The first permanent molar displayed less severe wear (grades 1, Scott 1979) and this is likely because the permanent first molar had only erupted within the last few years of this individual’slife. The extreme wear of the deciduous dentition indicates this child ate gritty and/or fibrous foods from an early age. Mild calculus deposits (calcified plaque) (grade 1 Brothwell 1981) were observed on both the deciduous and permanent teeth. Calculus can form as aresult of poor oral hygiene, but has also been associated with diets high in starch and/or protein (Hillson 1996). In the deciduous dentition, dental enamel defects in the form of brown hypocalcifications were present. In the permanent dentition, three teeth displayed linear enamel hypoplasia, and one of these was also affected by brown hypocalcifications. These dental enamel defects indicate that burial 1 underwent periods of physiological stress during the time of tooth formation (i.e. earlier in childhood and infancy) (Lewis– Roberts 1997). Fig. 15: Bobolanghar, Burial 1. Position of the burial, of the 8–10 year old child. Photo by J. Kysela.
175JAN KYSELA– ANNA AUGUSTINOVÁ– REBECCA KINASTON Burial 2 Burial 2 was ayoung/mid ‑age (mid 20s to late 30s) adult female interred semi ‑flexed on her right side, oriented north/northwest by south/southeast, facing west (the same position as burial 1) (Fig. 18). The grave ‑pit appeared slightly too small for the individual as the head of burial 2 was compressed on the north side of the grave so the skull was almost vertical instead of resting horizontal on the base of the grave (Fig. 19). The edge of the bottom of the grave appeared to be lined with stones, likely from the nearby river, and this was especially apparent on the east side of the burial. The bone preservation was excellent, and the skeleton was complete. The skeleton was very gracile. Sex was estimated using the pelvic and cranial morphology (Buikstra– Ubelaker 1994). Age was estimated using the pubic symphysis (Brooks– Suchey 1990), the auricular surface, sternal rib ends (İşcanetal. 1985), the presence of late ‑fusing epiphyses and cranial suture closure (Buikstra– Ubelaker 1994). Only the right pubic symphysis was assessed as there was apossible osteoclastic lesion present on the surface of the left pubic symphysis. Stature: Living stature was estimated using two methods that utilised regression equations of long bone lengths (Sjøvold 1990; Trotter– Gleser 1952; 1958). It should be noted that the reference populations used to develop these stature estimates are different from that of Burial 2, and this may introduce some error into the estimations (Tab.1). Although there is arange of stature estimates depending on what long bone measurement was used, both methods produced asimilar average height of 161.62 cm and 161.39 cm for burial 2, respectively. Fig. 16: Burial 1. Possible healed periosteal lesion on the superior, anterior aspect of the left tibial diaphysis. Photo by R. Kinaston. Fig. 17: Burial 1. Heavy tooth wear of right maxillary deciduous molars. Photo: R. Kinaston.
176 STUDIA HERCYNIA XXII/1 Pathology: The right and left wrists, hands and fingers were flexed, with the exception of the thumb of the left hand which was extended (Fig. 20). The feet appeared extended (plantarflex‑ ion) and rotated inwards (inversion) (Fig. 21). The extreme flexion of the hands and extension and inversion of the feet may suggest that this individual had acondition that led to spasticity (e.g. stroke, cerebral palsy, brain injury, multiple sclerosis and other neurological disorders). Fig. 18: Bobolanghar, Burial 2. General view of the burial of an adult female. Photo by J. Kysela.
177JAN KYSELA– ANNA AUGUSTINOVÁ– REBECCA KINASTON Long bone Side Length (mm) Stature estimate (1) ± 1 SD Stature estimate (2) ± 1 SD Humerus L 311 162.47 4.45 162.67 4.94 Humerus R 315 163.81 4.45 164.57 4.94 Radius L 233 165.37 4.24 163.86 4.98 Radius R 235 166.32 4.24 164.67 4.98 Ulna L 251 164.94 4.30 164.68 4.96 Ulna R 250 164.51 4.30 164.21 4.96 Femur L 400 152.90 3.72 155.16 4.52 Femur R 410 155.37 3.72 157.79 4.52 Tibia L 360 N/A 160.82 4.69 Tibia R 355 N/A 158.27 4.69 Fibula L 345 160.70 3.57 160.56 4.06 Fibula R 342 159.82 3.57 159.43 4.06 Average 161.62 161.39 Tab.1: Stature estimation for females from (1) Trotter– Gleser (1952; 1958) and for males/females from (2) Sjøvold (1990). Fig. 19: Position of the cervical vertebrae and cranium indicating that burial 2 was crammed into the grave. Photo by R. Kinaston.
178 STUDIA HERCYNIA XXII/1 Fig. 20: The flexed wrists, hands and fingers of burial 2 (note the left thumb was found extended into the soil). Photo by R. Kinaston. Fig. 21: The extended (planterflexed), inverted feet of burial 2. Photo by R. Kinaston.
179JAN KYSELA– ANNA AUGUSTINOVÁ– REBECCA KINASTON Some bony changes associated with pathology or trauma were observed on the post ‑cranial skeleton of burial 2. These included: septal aperture in the olecranon fossa of the left humerus and osteoclastic and osteoblastic lesions on the proximal aspect of the head of the left ulna; osteoclastic and osteoblastic lesions on the anterior, superior aspect of the proximal tibia, lateral to the medial condyle; asmall osteoclastic lesion on the inferior aspect of the mid ‑shaft of the intermediate phalanx of the right second digit of the hand; apossible osteoclastic lesion present on the surface of the left pubic symphysis; moderate to severe pitting located on the posterior aspect of the right and left patellae (Fig. 22), especially on the medial articular facet in addition to slight to moderate osteophyte formations around the margin of the articular facets of both patellae (no lesions were observed on the patellar surface of the right and left Fig. 22: Moderate to severe pitting located on the posterior aspect of the right and left patellae, osteophyte forma‑ tion around the margins of the articular surface and osteochondritis dissecans present on posterior surface between the medial and lateral articular surfaces of the patellae. Photo by R: Kinaston. Fig. 23: Extreme tooth wear on the labial surface of the maxillary incisors (heavier on left side). Photo by R. Kinaston. Fig. 24: Interproximal caries affecting the CEJ of the left second maxillary molar.
180 STUDIA HERCYNIA XXII/1 femurs); osteochondritis dissecans were present on posterior surface between the medial and lateral articular surfaces of the patellae; porosity of the vertebral body joint surfaces and osteophyte formation on the superior margin of lumbar vertebrae L3, L4 and L5. The patellae, tibia and lumbar spine pathologies may be indicative of degenerative joint disease or, in the case of the patellae, chondromalacia resulting from wear caused by physical deformity or traumatic injury. Osteochondritis dissecans is thought to form as aresult of minor repeated trauma to the articular patellar surface. The only pathology of the crania was observed in the dentition and surrounding alveolar bone, of which both the maxilla and mandible were available for analysis. Tooth wear was heavy on the anterior teeth (grades 4–6 Molnar 1971) and less so on the molars, especially the second and third molars (Molnar 1971; Scott 1979). The left dentition was more heavily worn than the right side, especially in the anterior dentition (Fig. 23). The pattern and extreme wear of the labial surface of the maxillary incisors was not consistent with corrosion and may suggest some type of use of the teeth for afunctional purpose other than eating. Caries (cavities) were observed on two teeth and included an interproximal caries of the cemento‑ Fig. 25: Heavy calculus deposits; advanced, active periodontal disease that had exposed the tooth roots; massive caries that destroyed the lower left first mandibular molar, leaving the mesial tooth root intact; and the antemortem tooth loss of the left, second mandibular premolar, with complete alveolar resorption of the tooth socket. Photo by R. Kinaston.
181JAN KYSELA– ANNA AUGUSTINOVÁ– REBECCA KINASTON ‑enamel junction (Fig. 24) and amassive caries. The massive caries destroyed amajority of the lower left mandibular first molar, leaving aresidual tooth root behind (Fig. 25). There were deposits of calculus (calcified plaque) on the teeth (grades 1–3 Brothwell 1981) and these were especially heavy (grade 2–3) on the lower mandibular incisors and canines and maxillary premolars and molars (Figs. 25–26). The calculus may have influenced the development of periodontal disease, which was severe and advanced enough to expose the tooth roots (Figs. 25–26). Two teeth (amandibular third molar and premolar) were lost before the time of death and the sockets of these teeth had completely remodelled before the time of death (Fig. 25). Caries are associated with diets high in refined carbohydrates and calculus deposits have been linked with diets high in starch and protein (Hillson 1996). Both conditions and associated pathologies (periodontal disease and antemortem tooth loss) are also caused by poor oral hygiene (Hillson 2008). Of the 26 observable teeth, Burial 2 had three teeth (11.5%) affected by linear enamel hypoplasia (LEH)‑ lines in the enamel that form as aresult of physiological stress in childhood. LEH is anon ‑specific indicator of stress, which can occur as aresult of periods of malnutrition and disease during the time of tooth formation (Lewis– Roberts 1997). BIBLIOGRAPHY Askarov 1973 = Аскаров, А. 1973: Сапаллитепа. Ташкент. Askarov– Abdullaev 1983 = Аскаров, А.А.– Абдуллаев, В.Н. 1983: Джаркутан. Кпроблеме протогородской цивилизации на юге Узбекистана. Ташкент. Augustinováetal. 2017 = Augustinová, A.– Stančo, L.– Damašek, L.– Mrva, M.– Shaydullaev, S. 2017: Ar‑ chaeological Survey of the Oases of Zarabag, Karabag and Kampyrtepa in the Piedmont of the Kugitang Mountains, South Uzbekistan– Preliminary Report for the Season 2016. Studia Hercynia XXI/1, 104–148. Brooks, S.– Suchey, J. 1990: Skeletal age determination base on the os pubis. Acomparison of the Acsádi‑ ‑Nemeskéri and Suchey ‑Brooks methods. Human Evolution 5, 227–238. Fig. 26: Heavy calculus deposits and advanced periodontal disease of the right maxilla. Photo by R. Kinaston.
182 STUDIA HERCYNIA XXII/1 Brothwell, D. 1981: Digging up Bones. Cornell. Buikstra, J.E.– Ubelaker, D.H. 1994: Standards for Data Collection from Human Skeletal Remains. Fayetteville. Hillson, S. 1996: Dental Anthropology. Cambridge. Hillson, S. 2008: Dental pathology. In,M.A. Katzenberg– S. Saunders (eds.): Biological Anthropology of the Human Skeleton. New York, 301–340. İşcan, M.Y.– Loth, S.R.– Wright, R.K. 1985: Age estimation from the rib by phase analysis: white females. Journal of Forensic Science 30/3, 853–863. Kaniuth, K. 2010: Tilla Bulak 2009. Vorbericht zur dritten Kampagne. Archäologische Mitteilungen aus Iran und Turan 42, 129–164. Kaniuth, K. 2011: Tilla Bulak 2010. Vorbericht zur vierte Grabungskampagne. Archäologische Mitteilungen aus Iran und Turan 43, 261–282. Kyselaetal. 2017 = Kysela, J.– Stančo, L.– Shaydullayev, Sh.– Palmeri, G. 2017: Preliminary Report on Ex‑ cavations at Burgut Kurgan in 2016. Studia Hercynia XXI/1, 89–103. Lewis, M.E.– Roberts, C. 1997: Growing Pains: the interpretation of stress indicators. International Journal of Osteoarchaeology 7, 581–586. Molnar, S. 1971: Human tooth wear, tooth function and cultural variability. American Journal of Physical Anthropology 34/1, 175–190. P’jankovaetal. 2009 = P’jankova, T.L.– Litvinskij,B.A.– Bobomulloev, S.– Kaniuth, K.– Teufer, M. 2009: Das bronzezeitliche Gräberfeld von Makonimor, Tadžikistan. Archäologische Mitteilungen aus Iran und Turan 41, 97–140. Scheuer, L.– Black, S. 2000: Developmental Juvenile Osteology. London. Scott, E. 1979. Dental wear scoring technique. American Journal of Physical Anthropology 51, 213–218. Širinov, T.– Baratov, S. 1997: Bronzezeitliche Grabstätten aus der Nekropole Džarkutan 4c (Süd ‑Uzbekistan). Archäologische Mitteilungen aus Iran und Turan 29, 65–120. Sjøvold, T. 1990: Estimation of stature from long bones utilizing the line of organic correlation. Human Evolution 5/5, 431–447. Stančoetal. 2016 = Stančo, L.– Shaydullaev, Sh.– Bendezu ‑Sarmiento, J.– Lhuillier, J.– Kysela, J.– Shay‑ dullaev, A.– Khamidov, O.– Havlik, J.– Tlustá, J. 2016: Preliminary Report on the Excavations at Burgut Kurgan in 2015. Studia Hercynia XX/2, 86–111. Trotter, M.– Gleser, G.C. 1952: Estimation of stature from long bones of American Whites and Negroes. American Journal of Physical Anthropology 10/4, 463–514. Trotter, M.– Gleser, G.C. 1958: Are‐evaluation of estimation of stature based on measurements of stature taken during life and of long bones after death. American Journal of Physical Anthropology 16/1, 79–123. Jan Kysela Anna Augustinová Institute of Classical Archaeology Faculty of Arts, Charles University in Prague Celetná 20, CZ‑11000 Prague 1 [email protected] [email protected] Rebecca Kinaston Research Fellow Biological Anthropology Research Group Department of Anatomy Otago School of Medical Sciences University of Otago P.O. Box 913,Dunedin, 9054,New Zealand Guest Researcher Department of Archaeogenetics Max Planck Institute for the Science of Human History Kahlaische Str.10, 07745 Jena, Germany rebecca. [email protected]