The Sunghir Human Skeletal Remains

Author(s):  
Erik Trinkaus ◽  
Alexandra P. Buzhilova ◽  
Maria B. Mednikova ◽  
Maria V. Dobrovolskaya

The Sunghir human remains originally consisted of the three associated skeletons from the two burials, Sunghir 1, 2, and 3, plus the remains of six other individuals. Sunghir 1 to 3 consist of largely complete skeletons that sustained the inevitable partial crushing, fragmentation, and bone disintegration that accompanies human remains buried in open air sites for 28,000 years. Sunghir 4 is the adult femur shaft that was ritually placed in the Sunghir 2 and 3 burial, next to the left shoulder of Sunghir 2 (chapter 3). Sunghir 5 is a partial adult cranium, found in the sediments above Grave 1. Sunghir 6 is a mature hemimandible, identified as human after excavation from among the faunal remains above Grave 2. There were also the unnumbered remains of the skeleton in Grave 2bis, which were not retained (see discussion in chapter 3). In addition to these human fossils, the remains of three additional individuals were originally found, numbered Sunghir 7 to 9. Sunghir 7 was found in the deposits between the two graves and consisted of a portion of a human femur, variously described as adolescent or from a young adult female. Sunghir 8 consisted of portions of a femur and a skull (a frontal bone, a probable parietal bone, and a temporal bone), found in 1969 in an additional clay pit. Sunghir 9 was a partial skeleton found in 1972 in an additional clay pit. None of the Sunghir 7 to 9 human remains can be currently located. The Sunghir 7 and 8 remains were briefly described by anthropologists and forensic scientists in Moscow, and the limited information on Sunghir 9 is based on reports by the Vladimir Ceramic Works workers. The available human remains from Sunghir therefore consist of the Sunghir 1 to 3 partial skeletons, the Sunghir 4 partial femur, and the Sunghir 5 and 6 cranium and mandible. These specimens are currently curated in the Laboratory of Anthropological Reconstruction of the Institute of Anthropology and Ethnology of the Russian Academy of Sciences.

Radiocarbon ◽  
2020 ◽  
pp. 1-10
Author(s):  
Adrián Pablos ◽  
Nohemi Sala ◽  
Alfonso Arribas

ABSTRACT Pleistocene human remains are rare inland on the Iberian Peninsula. Most are considered Neandertals, but anthropological analyses and direct dating are rare. Recently, we published a study of a navicular from this region found in the Torrejones Cave. The results showed it differed from that of Neandertals and it was re-identified as Homo sapiens. Following the previous stratigraphic and biochronologic descriptions, we suggested that it could correspond to an Upper Paleolithic human, since the navicular was apparently recovered in the Late Pleistocene from an in situ unit. Direct radiocarbon dating from this fossil (4855–5036 cal BP), believed to be the only Paleolithic Homo sapiens from inland Iberia, as well as other hominin and faunal remains from the site, show that the human bones actually date to the Chalcolithic. The unexpectedly recent chronology for the navicular implies that there is no evidence of human fossils from the Upper Paleolithic in Torrejones Cave. Thus, any date from the Middle/Upper Paleolithic human record should be taken with caution until in-depth paleoanthropological, stratigraphical and/or direct dating studies are conducted. Extraordinary caution is recommended when human remains are recovered from apparently Paleolithic units in contexts bearing Holocene sepulchral units on the uppermost levels and/or some evidence of bioturbation.


2014 ◽  
Vol 2014 ◽  
pp. 1-5 ◽  
Author(s):  
Nader Goodarzi ◽  
Toraj Shah Hoseini

This study provides some comprehensive osteometric and morphologic descriptions of the skull region of the Markhoz goat. Totally, 17 osteometric parameters of eight skulls of Markhoz goat were measured and expressed as mean ± SD. A skull length of18.67±0.66, a cranial length of11.1±0.38, a facial length of10.23±0.76, a skull index of47.77±1.96, a cranial index of54.04±2.29, a facial index of100.77±6.85and a foramen magnum index of89.32±14.1were recorded. Morphologically frontal bone did not constitute the caudal extent of frontal surface; rather it was formed by the parietal bone. There were two supraorbital foramina in both sides. The prominent facial tuberosity lies dorsally to the 3rd cheek tooth. The infraorbital foramen was single on either side which was located directly dorsally to the junction of the first and second upper premolar. The orbits were round and complete and located on a frontolateral oblique plane. The basilar part of the occipital bone was surrounded by two pairs of muscular tubercles with similar size. The temporal line was continuous of the temporal crest and ran over the parietal bone. In conclusion, the morphologic and osteometric data of Markhoz goat are comparable to other ruminants.


Author(s):  
V. Farina ◽  
A. Mura ◽  
V. Petruzzi ◽  
G. Lepore ◽  
E. Mura ◽  
...  

The study of ancient skeletons is of high interest, as the relationship between men and animals can be reconstructed. In dogs, head injuries frequently result from direct physical traumas. The excavation of a prehistoric well (Genomi, Sardinia) brought to light sixty canine bones of the Age Roman (2nd century AD), although this well was built during the Nuragic Age. (1st millennium BC). Two canine skulls showing three traumatic lesions underwent computed tomography in order to study the endocast of the brain cavity and indirectly locate possible brain lesions. In the first case, a traumatic lesion was found in the left parietal bone with depression of the outer surface. This lesion determined compression of the left frontal cortex and was compatible with life, as can be deduced by the inflammation of the periostenum. In the second case, two different traumatic lesions were found. The former was a wide fracture of the right frontal bone near the orbital cavity. The injured area showed clear signs of bone remodeling which took place many months before death. The latter was a severe comminuted fracture involving both the outer and inner surface of the left frontal bone, which provoked a deep wound in the left frontal cortex. The sharp outline of bone splinters with no signs of bone remodelling indicates that the trauma was not compatible with life. All lesions described were consequent to severe blows from humans and testify mistreatment of dogs in the Roman Age.


PLoS ONE ◽  
2015 ◽  
Vol 10 (10) ◽  
pp. e0138059 ◽  
Author(s):  
Shuli Li ◽  
Natalina Quarto ◽  
Kshemendra Senarath-Yapa ◽  
Nathaniel Grey ◽  
Xue Bai ◽  
...  

2017 ◽  
Vol 25 (1) ◽  
pp. 11-14
Author(s):  
TIAGO FERREIRA DE ALMEIDA ◽  
HOMAR TOLEDO CHARAFEDDINE ◽  
FERNANDO FLORES DE ARAÚJO ◽  
ALEXANDRE FOGAÇA CRISTANTE ◽  
RAPHAEL MARTUS MARCON ◽  
...  

ABSTRACT Objective: To evaluate using tomographic study the thickness of the cranial board at the insertions points of the cranial halo pins in adults Methods: This is a retrospective, cross-sectional, descriptive analysis of Computed Tomography (CT) scans of adult patients' crania. The study included adults between 20 and 50 years without cranial abnormalities. We excluded any exam with cranial abnormalities Results: We analyzed 50 CT scans, including 27 men and 23 women, at the original insertion points and alternative points (1 and 2 cm above the frontal and parietal bones). The average values were 7.4333 mm in the frontal bone and 6.0290 mm in the parietal bone Conclusion: There was no statistically significant difference between the classical and alternative points, making room for alternative fixings and safer introduction of the pins, if necessary. Level of Evidence II, Retrospective Study.


2015 ◽  
Vol 5 ◽  
pp. 255-261
Author(s):  
D. K. Mahamad Iqbal ◽  
Vivek B. Amin ◽  
Rohan Mascarenhas ◽  
Akther Husain

Objective The objectives of this study were to determine the thickness of skull bones, namely frontal, parietal, and occipital bones in Class I, Class II, and Class III patients. Materials and Methods Three hundred subjects who reported to the Department of Orthodontics requiring orthodontic treatment within the age group 17-35 were selected for the study. They were subdivided into three groups of 100 each according to the skeletal and dental relation. Profile radiographs were taken and the tracings were then scanned, and uploaded to the MATLAB 7.6.0 (R 2008a) software. The total surface areas of the individual bones were estimated by the software, which represented the thickness of each bone. Result Frontal bone was the thickest in Class III malocclusion group and the thinnest in Class II malocclusion group. But the parietal and occipital bone thickness were not significant. During gender differentiation in Class I, malocclusion group frontal bone thickness was more in males than females, In Class II, malocclusion parietal bone thickness was more in males than females. No statistically significant difference exists between genders, in Class III malocclusion group. During inter-comparison, the frontal bone thickness was significant when compared with Class I and Class II malocclusion groups and Class II and Class III malocclusion groups. Conclusion The differences in skull thickness in various malocclusions can be used as an adjunct in diagnosis and treatment planning for orthodontic patients. It was found that the new method (MATLAB 7.6.0 [R 2008a] software) of measuring skull thickness was easier, faster, precise, and accurate.


2019 ◽  
Vol 5 (1) ◽  
pp. 70-87 ◽  
Author(s):  
Erik Trinkaus ◽  
Sandra Sázelová ◽  
Jiří Svoboda

The rich earlier Mid Upper Palaeolithic (Pavlovian) sites of Dolní Vĕstonice I and II and Pavlov I (∼32,000–∼30,000 cal BP) in southern Moravia (Czech Republic) have yielded a series of human burials, isolated pairs of extremities and isolated bones and teeth. The burials occurred within and adjacent to the remains of structures (‘huts’), among domestic debris. Two of them were adjacent to mammoth bone dumps, but none of them was directly associated with areas of apparent discard (or garbage). The isolated pairs and bones/teeth were haphazardly scattered through the occupation areas, many of them mixed with the small to medium-sized faunal remains, from which many were identified post-excavation. It is therefore difficult to establish a pattern of disposal of the human remains with respect to the abundant evidence for site structure at these Upper Palaeolithic sites. At the same time, each form of human preservation raises questions about the differential mortuary behaviours, and hence social dynamics, of these foraging populations and how we interpret them through an archaeological lens.


2013 ◽  
Vol 2013 ◽  
pp. 1-5
Author(s):  
Ranganadh Nallamothu ◽  
Shanmukha Reddy Kallam ◽  
Srikanth Gunturu ◽  
Sukumar Singh ◽  
Vijay Kumar Rachalapally

A 9-year-old girl was referred to a trauma centre with severe head injury. 3D CT scan revealed depressed fracture involving the frontal bone on the right side, right parietal bone, and right superior orbital margin, right lamina papyracea. The frontal table was managed conservatively and open reduction and internal fixation was done for the supraorbital blow in to correct the ocular dystopia. The clinical course, possible mechanism, and management of the patient are discussed.


2013 ◽  
Vol 2 (1) ◽  
pp. 31-35
Author(s):  
Manoj Bhattarai

Introduction Skull has cranial vault and base. The cranial vault is called as calvarium which roofs the cranial cavity (brain box).Cranial vault consists of frontal, parietal and occipital bones. Total thickness of calvarial bones includes outer table, diploe and inner table. Diploe is made up of spongy bone whereas outer and inner table made up of compact bone. Objective To measure the thickness of Nepalese calvarial bones i.e. Frontal, Parietal and Occipital. Methods It is a hospital base cross-sectional study. CT records of one hundred and fifty adult people were studied. Nine various points on frontal bone, seven on parietal and six on occipital were located and their thickness were measured bilaterally with help of CT scan. Results The present study showed that Mean thickness+_SD of frontal bone were 6.1+_1.8mm; parietal 4.6+_2.2 and occipital 9.5+_3.4. The study also showed that frontal bone had 2.4+_0.8 mm thick outer table; 1.4+_0.6mm inner table and 3.5+_1.3mm diploe. Similarly parietal bone had 1.9+_0.6 mm thick outer table; 1.1+_0.4mm inner table and 0.8+_0.5mm diploe. The occipital bone had 3.5+_1.5 mm thick outer table; 2.2+_0.8mm inner table and 4.3+_1.8mm diploe. Similarly this present study also calculated the mean thickness+_SD of outer table in the calvarium as 2.7+_1.3mm and that of inner table 1.5+_0.9 mm. Thus it concluded that outer table was thicker than inner table. Journal of Nobel Medical College Vol. 2, No.1 Issue 3 Nov.-April 2013 Page 31-35 DOI: http://dx.doi.org/10.3126/jonmc.v2i1.7670


Author(s):  
Julian A. Sitters ◽  
Timothy K. Perttula

The Snipes site (41CS8) was excavated by Jelks in 1952 as part of the River Basins Surveys (RBS) program administered by the Smithsonian Institution in cooperation with the National Park Service, the U.S. Army Corps of Engineers, and the Bureau of Reclamation. Snipes was one of three sites excavated by the RBS prior to the inundation of a large part of the lower Sulphur River valley by Texarkana Reservoir, now Lake Wright Patman. The Snipes site was apparently occupied during at least some part of the Woodland period (ca. 500 B.C.- A.D. 800), mainly during the latter part of the period, and can be considered a component of the Fourche Maline Culture on the basis of the artifacts recovered from both habitation archaeological deposits and burial features. Other artifacts in the collection attest to the use of the Snipes site during Late Archaic and post-A.D. 900 ancestral Caddo times, as we will discuss below. The site was estimated to cover ca. 6-7 acres of an upland landform about 1.6 km south of the Sulphur River, and was marked by a scatter of lithic artifacts, mussel shell, animal bones, charcoal, pottery sherds, etc. Excavations were done in a series of 5-ft. squares dispersed across a 300 x 200 ft. area; according to Jelks, “additional squares were opened adjacent to the most productive test squares.” The archaeological deposits ranged from ca. 8-38 cm in thickness from the surface, and had been well disturbed by plowing. Apparent midden deposits marked by “a great deal of carbon and grease” were identified in several parts of the excavations. During the work at the site by Jelks, nine prehistoric burials were excavated there, including three (Burials 7-9) that were discovered an unknown distance northeast of Burials 1-6 during the last round of work at the site. Jelks reported that traces of human remains from adults of unknown sex were present in Burials 6 and 7, but failed to mention if such was the case for Burials 8 and 9. However, since Burial 8 was reported to have contained two individuals, and the orientation of the heads was recorded, human remains (again, probably from adults, although not noted) were obviously preserved in this burial as well, but apparently not recovered. For Burial 9, Jelks simply noted that preservation “was poor.” Burials 6, 7, and 8 contained individuals that were placed in graves in an extended supine (i.e., on their back) position. Burial 8 had two individuals in extended supine position. The position of the deceased individual in Burial 9 was not recorded. Burial 6 had a Coles Creek Incised, var. Stoner bowl by the right shoulder of the deceased, and one small bowl each had been placed as a funerary offering in Burials 7-9; in two instances, the small bowls were by the left shoulder of the deceased. Two other vessels were funerary offerings in Burial 1 and a separate burial feature excavated by I. B. (Bogey) Price after the main RBS investigations.


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