Abstract
Shulgan-Tash (Kapova) cave in southern Ural, Russia, is the easternmost European site hosting Late Paleolithic cave art. Most of the 195+ drawings catalogued in the cave are made with red natural pigment (ochre), and only a handful of drawings are made with charcoal, see “Catalogue of images” [4], “Höhlenmalerei im Ural: Kapova und Ignatievka; die altsteinzeitlichen Bilderhöhlen im sudlichen Ural,” [5]. “Constraining the ages of the Late Palaeolithic cave paintings in the Shulgan-Tash cave, Southern Urals, Russia” [6]. None of the charcoal drawings were directly dated by 14C method so far.
Black lines delineating a figure similar to the outline of a fox are known in the cave. Here we present data on the 14C AMS date of charcoal with which the lines were drawn. Calibration of the data was performed using the Bomb13NH1 dataset, see “Atmospheric radiocarbon for the period 1950–2010” [7] and the IntCal13 dataset, see “IntCal13 and Marine13 radiocarbon age calibration curves 0–50,000 years cal BP” [8]. The calibrated age distribution has maximum probability density (65.3%) between 1877 and 1918.
Keywords: Shulgan-Tash cave, Radiocarbon, Cave art
Specifications table
Subject area | Archaeological science |
More specific subject area | Geochronology, history, archaeology |
Type of data | Tables, photo images, graph |
How data was acquired | The acceleration mass spectrometry (AMS) system at Oxford Radiocarbon Accelerator Unit (University of Oxford, UK) |
Data format | Raw and analyzed |
Experimental factors | Samples were treated with acid, base, acid sequence as per[1], [2], [3]. |
Experimental features | Samples were combusted in SHN analyzer furnace system, passed through a gas chromatograph and measured for δ13C values. An aliquot of CO2collected from the He stream was mixed with hydrogen, reduced to graphite on an Fe catalyst and pressed into a target for the ion source as per[1], [2], [3]. |
Data source location | Shulgan-Tash (Kapova) cave; 53°2′34.80″N; 57°3′57.60″E; Russia |
Data accessibility | Data is reported in this article. |
Value of the data
-
•
The data can be used by scientific community to constrain the age of charcoal of the lines, creating the figure “Black fox” in Shulgan-Tash (Kapova) cave, Russia.
-
•
This is the first direct radiocarbon dating of a charcoal drawing in Shulgan-Tash cave can be used by archaeologists and historians studying the use of the cave by humans in the past.
-
•
The data can be used to close the controversy as to whether this particular figure is of Paleolithic age or is a later artifact.
1. Data
Black charcoal lines, delineating a figure evocative of a running fox (Fig. 1) were sampled in the Hall of Drawings of the Shulgan-Tash (Kapova) cave in southern Ural, Russia. The length of the figure is 84 cm; its width is 18 cm. In contrast to several other charcoal drawings found in the cave, which are poorly preserved, faint and barely visible (and, therefore, not amenable to radiocarbon dating [4], [5]) the lines composing the figure are sharp and bright, with discrete particles of charcoal clearly visible (Fig. 2). The figure was identified as a drawing, and assigned the name “Black fox” in Ref. [4 p. 94].
The data presented in this paper consist of photo documentation of the sample collection site (Figs. 1 and 2), the 14C (AMS) dating results (Table 1), the results of calibration of the 14C date (Table 2), and graphical representation of obtained dates (Fig. 3).
Table 1.
Sample ID | Provenance | Material | δ13C (‰ VPDB) | F14С | 14C date (yrs BP) |
---|---|---|---|---|---|
OxA-33323 | Shulgan-Tash cave | charcoal | −27.32 | 0.99565 ± 0.00321 | 35 ± 26 |
Note: BP = Before present – AD 1950.
Table 2.
From (yrs AD) | To (yrs AD) | Probability (%) |
---|---|---|
68.2% probability | ||
1710 | 1718 | 7.9% |
1828 | 1832 | 3.6% |
1890 | 1910 | 55.4% |
1955 | 1955 | 1.3% |
95.4% probability | ||
1696 | 1725 | 16.2% |
1814 | 1836 | 11.1% |
1844 | 1851 | 1.3% |
1877 | 1917 | 65.3% |
1954 | 1955 | 1.4% |
The data was calibrated using OxCal (v4.3.2; © Bronk Ramsey 2017) using the Bomb13NH1 curve [7], which is valid for latitudes north of 40°N and is prepended with the last 300 years of the IntCal13 dataset [8]. Calibrated dates and their probabilities are shown in Fig. 3 and Table 2.
2. Experimental design, materials, and methods
A sample was collected by chipping small grains of charcoal from different parts of the drawing with a scalpel. This technique allowed collection of sufficient amount of material without affecting the visual appearance of the drawing.
The sample was analyzed in the Research Laboratory for Archaeology and the History of Art, University of Oxford (UK). Preparation of the sample (id:OxA-33323) and analysis by Acceleration Mass Spectrometry (AMS) was performed according to protocols and procedures reported in Refs. [1], [2], [3]. The measured radiocarbon age was corrected for stable isotope fractionation using the measured value δ13C = −27.3‰ VPDB.
Acknowledgments
Funding: This work was supported by a grant of the Head of Government of the Reublic of Bashkortostan (RB), Russia R. Khamitov. Logistical support was provided by Scientific-Production Center for Protection and Use of Objects of Cultural Heritage, the Ministry of Culture of the RB, Russia. The aforementioned entities had no role in study design; in collection, analysis and interpretation of the data; in preparation of the report; and in the decision to submit the article for publication.
Footnotes
Transparency data associated with this article can be found in the online version at doi:https://doi.org/10.1016/j.dib.2018.10.040.
Transparency document. Supplementary material
References
- 1.Ramsey C., Gigham T., Leach P. Towards high-precision AMS: progress and limitations. Radiocarbon. 2004;46(1):17–24. [Google Scholar]
- 2.Ramsey C., Higham T., Bowles A., Hedges R. Improvements to the pretreatment of bone at Oxford. Radiocarbon. 2004;46(1):155–163. [Google Scholar]
- 3.Ramsey C., Higham T., Owen D., Pike A., Hedges R. Radiocarbon dates from the Oxford AMS System: archaeometry Datelist 3. Archaeometry. 2002;44(3, Supplement 1):S1–S149. [Google Scholar]
- 4.Y. Lyakhnitsky, O. Minnikov, A. Yushko, Drawings and Signs of Shulgan-Tash (Kapova) Cave, Catalogue of Images, Kitap, Ufa, 2013.
- 5.Šcelinskij V., Širokov V. Höhlenmalerei im Ural: Kapova und Ignatievka; die altsteinzeitlichen Bilderhöhlen im südlichen Ural. Thorbecke; Sigmar: 1999. [Google Scholar]
- 6.Y. Dublyansky, G.E. Moseley, C. Spötl, Y. Liakhnitsky, H. Cheng, R. Lawrence Edwards, Constraining the ages of the Late Palaeolithic cave paintings in the Shulgan-Tash cave, Southern Urals, Russia, in: Proceedings of the International Symposium on “Ancient Sanctuaries: Archaeology, Ritual, Mythology”, Institute for History, Ufa, 2016, pp.120–125.
- 7.Hua Q., Barbetti M., Rakowski A. Atmospheric radiocarbon for the period 1950–2010. Radiocarbon. 2013;55(4):2059–2072. [Google Scholar]
- 8.Reimer P., Bard E., Bayliss A., Beck J., Blackwell P., Ramsey C., Buck C., Cheng H., Edwards R., Friedrich M., Grootes P., Guilderson T., Haflidason H., Hajdas I., Hatté C., Heaton T., Hoffmann D., Hogg A., Hughen K., Kaiser K., Kromer B., Manning S., Niu M., Reimer R., Richards D., Scott E., Southon J., Staff R., Turney C., van der Plicht J. IntCal13 and Marine13 radiocarbon age calibration curves 0–50,000 years cal BP. Radiocarbon. 2013;55(4):1869–1887. [Google Scholar]
Associated Data
This section collects any data citations, data availability statements, or supplementary materials included in this article.