Abstract

We investigated rock varnish formed on sandstone and petroglyphs in the Hima area, southwestern Saudi Arabia. To characterize the rock varnish, we made in-situ measurements by portable x-ray fluorescence (pXRF) and analyzed samples by femtosecond laser-ablation inductively coupled–plasma mass spectrometry (fs LA-ICP-MS). Detailed chemical analysis of the rock varnish samples and adjacent soil or aeolian dust yielded information about the varnish’s geochemical context and formation mechanism. Untypically low positive Ce anomalies in the rock varnish samples correlated with negative Ce anomalies in the dust, supporting the hypothesis that the dust is the source of the varnish material. To study the varnish development, we made use of the fact that engraving the petroglyphs exposes a fresh bare sandstone surface without varnish, on which varnish regrows subsequently. We determined by pXRF the areal density of manganese (Mn) and iron (Fe) that had been deposited as rock varnish since the creation of the rock art. The rates of Mn deposition in the newly formed varnish were then estimated by correlating the areal density of Mn in Ancient Arabian and Old Arabic inscriptions with their known age ranges. The observed deposition rates showed substantial variability resulting from differences in exposure conditions of the rock surface, but were in a range comparable with that of our previous measurements in northwestern Arabia. This variability could be reduced significantly by referencing the measurements to the intact varnish adjacent to the individual petroglyphs. This normalization provided a much clearer relationship between varnish deposition and age, and enabled tentative ages to be assigned to rock art motifs without previously known ages. These tentative ages spanned most of the Holocene period and were consistent with the culturally or ecologically derived ages of the animal and human figures depicted in the rock art and the styles of scripts used in different periods.

Highlights

  • Petroglyphs are images and symbols engraved into the surface layers of rock faces and boulders

  • This is consistent with the conclusions by Goldsmith et al (2012), who found no clear correlation between Mn concentration in Holocene varnishes and rainfall amount in the arid Negev desert, and suggested that the number of days with rainfall or dew might be more important than the amount of rainfall

  • They are comparable with values measured on rocks from a piedmont in the Mojave Desert, where Reneau (1993) found median values of 104 μg cm–2 on mid- to late-Holocene surfaces, 130–220 μg cm–2 on early- to mid-Holocene surfaces, and 90–220 μg cm–2 on Pleistocene surfaces

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Summary

Introduction

Petroglyphs are images and symbols engraved into the surface layers of rock faces and boulders. They are found worldwide and provide unique and valuable information on humans and their environment, reaching from the pre-Neolithic period up to today In Arabia, as in many other regions, petroglyphs were usually engraved into dark rock varnish coatings on sandstone surfaces, which – at least initially – provides a strong contrast to the exposed lighter rock and creates images with strong artistic impact (Khan, 2013; Olsen, 2013). If the time of creation of the rock art is known or can at least be estimated, the rate of formation of the varnish can be derived from measurements of the amount of varnish formed on the petroglyphs. Varnish formed in recent times, when climatic and environmental characteristics are well constrained, may provide clues on its mechanism of formation and the role of climatic variables, such as rainfall and exposure (Broecker and Liu, 2001; Dorn and Meek, 1995; Elvidge and Iverson, 1983; Goldsmith et al, 2012)

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