Abstract
A gray, fine-grained arkosic sandstone tablet bearing an inscription in ancient Hebrew from the First Temple Period contains a rich assemblage of particles accumulated in the covering patina that includes calcite, dolomite, quartz and feldspar grains, iron oxides, carbon ash particles, microorganisms, and gold globules (1–4 μm in diameter). There are two types of patina present: thin layers of a black to orange-brown, iron oxide-rich patina, a product of micro-biogenetical activity, as well as a light beige patina mainly composed of carbonates, quartz and feldspar grains. The patina covers the rock surfaces and inscription grooves post-dating the incised inscription as well as a fissure that runs across the stone and several of the engraved letters. Accelerator Mass Spectrometry (AMS) analyses of the carbon particles in the patina yields a calibrated radiocarbon age of 2340–2150 Cal BP and a conventional radiocarbon age of 2250 ± 40 years BP. The presence of microcolonial fungi and associated pitting indicates slow growth over many years. The occurrence of pure gold globules is evidence of melting (above 1000 °C) indicates a thermal event. This study supports the antiquity of the patina, which in turn, strengthens the contention that the inscription is authentic.Keywords
- Jehoash Inscription;
- Archaeometric;
- Patina;
- Microcolonial fungi;
- Gold globules
1. Introduction
A rectangular dark stone tablet 31 × 25 × 9 cm in size was subjected to archaeometric examination by the authors. The stone tablet is engraved with an inscription in ancient Hebrew (Fig. 1A and B) known as the “Jehoash Inscription” (JI). The inscription commemorates the renovation of the First Temple carried out by King Jehoash, who reigned at the end of the 9th century B.C.E. (ca. 2800 years BP). A similar account of the Temple repairs is found in the Bible (Kings II: 12). This tablet represents the only Judahite royal inscription found to date. According to Cohen (2005), the translation of the 16 lines of the ancient Hebrew is as follows:“[I am Yeho'ash, son of A]hazyahu, k[ing over Ju]dah, and I executed the re[pai]rs. When men's hearts became replete with generosity in the (densely populated) land and in the (sparsely populated) steppe, and in all the cities of Judah, to donate money for the sacred contributions abundantly, in order to purchase quarry stone and juniper wood and Edomite copper/copper from (the city of) ‘Adam, (and) in order to perform the work faithfully (=without corruption), - (then) I renovated the breach(es) of the Temple and of the surrounding walls, and the storied structure, and the mesh-work, and the winding stairs, and the recesses, and the doors. May (this inscribed stone) become this day a witness that the work has succeeded (and) may God (thus) ordain His people with a blessing.”
- Fig. 1. A. The ‘Jehoash Inscription’ tablet composed of arkosic sandstone with an ancient First Temple Period Hebrew inscription (scale bar = 5 cm). B. Detail of panel A showing the prominent central fissure transecting the engraved letters. C. The sites of the rock and patina samples from the tablet. Samples Z-1 to Z-7 and Z-9 are from the patina on the inscription face of the tablet; Z-8 (not shown) was collected from the quartz vein on the back side of the tablet; and Z-10 to Z-12 (not shown) were taken from the tablet's side and include only the arkosic sandstone (scale bar = 5 cm).
2. Methods
The mineralogic composition of the tablet rock was determined by using a petrographic microscope and a Philips X-ray diffractometer. Samples were removed from the rock-tablet by using a diamond-tipped hand drill and from the patina by peeling with a sharp steel blade. A scanning electron microscope (SEM, JEOL-840), equipped with an energy dispersive spectrometer (EDS, Oxford–Link–Isis) was employed for detailed inspection of the physical properties and structural features of the tablet and its patina, as well as for chemical analysis. A Hitachi S-3200N SEM with low vacuum was used for further analyses of microorganism content within the patina layers. Additional geochemical analyses were carried out using inductively coupled plasma atomic emission spectroscopy (ICP-AES) in the geochemistry laboratories of the Geological Survey of Israel. A stereoscopic binocular and a light transmitting ore mineral microscope were also used to study the morphology, structural features and thin sections of the rock (see Fig. 1C for sample locations).3. Results
3.1. Rock-tablet
The general color of the fine-grained JI rock-tablet is medium gray. The gray color was observed in fresh breakage of the rock and in the samples of the drilling material. A fissure, less than 0.5 mm in width, runs across the central part of the tablet parallel to the broken upper edge, crossing ten letters in four lines (Fig. 1B). The fissure begins in the 8th line and descends at an angle of 18° toward the left margin of the 11th line (Fig. 1A and B). The tablet broke into two separate pieces along this fissure.
Petrographic analysis reveals that the rock, from which the tablet was produced, is an arkosic sandstone (Fig. 2) composed mainly of unsorted sub-angular quartz grains 50–500 μm in size, and angular to sub-rounded unsorted feldspar grains, up to 100 μm in size. Thin section analyses of the rock material indicate that it is composed of: quartz (35%), feldspars (albite and orthoclase; 55%), epidote (3%), chlorite (1%), rutile and sphene (up to 1%), iron oxides and opaques (2–5%). A similar composition was obtained by XRD examination (Fig. 3), however, the results are slightly different (e.g. here we note the presence of calcite and illite) because the XRD samples may have included material from the patina.
Many of the incised letters on the tablet exhibit defects in shape at the edges. These defects are due to the detachment of quartz and feldspar grains during subsequent weathering of the sandstone. Illuminating the tablet with ultraviolet light (Newman, 1990) did not exhibit the characteristic glow that would indicate fresh engraving scars.
According to the chemical analysis by ICP-AES, the oxide composition of the rock (samples Z-10 to Z-12; Fig. 1B) from which the tablet was engraved is (% oxides; normalized to 100%): SiO2 – 60; CaO – 13; Fe2O3 – 5.5; Al2O3 – 11.5; Na2O – 3.0; MgO – 2.5; K2O – 1.8; P2O5 – 0.3; MnO – 0.1; TiO2 – 0.7; SO3– <0 .1.="" p="">
- Fig. 2. Thin section of the arkosic sandstone from the tablet. Q, quartz; F, feldspar; E, epidote; O, iron oxide minerals (scale bar = 100 μm).
- Fig. 3. XRD diffractogram of the arkosic sandstone from the tablet (sample Z-10).
According to the chemical analysis by ICP-AES, the oxide composition of the rock (samples Z-10 to Z-12; Fig. 1B) from which the tablet was engraved is (% oxides; normalized to 100%): SiO2 – 60; CaO – 13; Fe2O3 – 5.5; Al2O3 – 11.5; Na2O – 3.0; MgO – 2.5; K2O – 1.8; P2O5 – 0.3; MnO – 0.1; TiO2 – 0.7; SO3– <0 .1.="" p="">
3.2. Patina
There are two areas on the tablet, one just above and to the left of the crack and the other just below and to the right of the crack, that lack a patina and so were almost certainly cleaned since the tablet's discovery. The patinated areas can be differentiated by their pale orange-brown color. The left lower part retains black to orange-brown as well as light beige patina layers up to 2 mm thick that cover the tablet and the inscription (Fig. 4). The first layer attached to the rock is a thin, up to 1 mm thick, metallic black orange-brown iron oxide layer that covers the surfaces of the tablet and the engraved letters. In places the black and orange-brown layers alternate, occurring one next to the other. As the rock-tablet contains about 5% iron oxides, we suggest that the formation of both black and brown layers may be related to natural geo-biological weathering processes. The overlying and uppermost layer, orange-brown to light beige in color and up to 1 mm thick, is found mostly within the letters but also on the surfaces that were partly cleaned. The black orange-brown patina forms a continuous cover on the surface of the tablet as well as within the grooves of the letters (Fig. 5). Some natural bleaching and incipient light patina formation (light gray zone just below the surface of the tablet) due to exposure to the air near its inscribed surface is also evident. Results of the SEM–EDS analysis of samples from the patina are presented in Table 1. We analyzed nine samples (Fig. 1C; Table 1) using the SEM–EDS backscattered method for detecting heavy elements. We did not detect the presence of any element, such as Cr and V, which would have indicated the use of modern tools in the engraving process.
- Fig. 4. A groove representing part of a letter and the layers of the patina that infills and covers it as well as the rock surface. The lower patina layer consists of black (B) and orange-brown (O) alternating layers occurring one next to the other. Both are composed of iron oxide that can be seen on lateral margins of the groove as well as on the surface of the tablet, above which is a light beige upper patina layer (L). Note the carbon ash particles represented by tiny black specks (A) integrated within the patina (scale bar = 500 μm).
- Fig. 5. The lower part of the broken tablet along the fissure. The arkosic sandstone is medium gray whereas the patina is light gray. A thin black, orange-brown patina layer as well as the light beige overlying layers cover all surfaces of the tablet as well as the grooves of the letters (scale bar = 10 mm).
- Table 1. The occurrence of carbon ash particles and gold globules within the patina of the Jehoash Inscription tablet based on SEM–EDS analysis
Sample number Carbon ash Gold globules Iron oxides Miscellaneous Z-1 Common; 10–30 μm Abundant; 1 μm Rare; monazite Z-2 Abundant; 0.5–1 μm Rare; angular; 10 μm Z-3 Common; 1–4 μm Z-4 Common; 10–50 μm Z-5 Common; 10–30 μm Abundant; 1–4 μm Common; 1–3 μm Rare; clay Z-6 Common, 10 μm Common; 10 μm Z-7 Abundant; 60–100 μm Z-8 Silica; calcsilicate Z-9 Rare; monazite, clay - All samples are from the front of the tablet, however, Z-8 is taken from the lower back of the tablet. Abundant = >10 particles/mm2; common = 4–10 particles/mm2; rare = <4 mm="" particles="" sup="">2
- Fig. 6. SEM photo of a carbon ash particle. The calibrated radiocarbon age of numerous particles ranges from 2340 to 2150 BP. Note a centrally located rectangular fragment. The composition of these particles was confirmed by EDS analysis.
- Fig. 7. SEM photo of pure gold globule found within the patina. These globules occur at about 10 spheres per mm2 .
- Fig. 8. XRD diffractogram of the patina (sample Z-6).
3.3. Age determination of the patina
The carbon ash particles are admixed within the patina, firmly and intimately associated with the other particles (Fig. 4 and Fig. 6). Samples of the patina were taken by the Israel Museum in Jerusalem and sent for radiocarbon dating to the Beta Analytic Radiocarbon Dating Laboratory in Miami, Florida, USA (Table 2). According to their report from June 5, 2002, the patina samples were combined into a single sample. The surface area was increased as much as possible and the sediment was dispersed and pretreated by hydrochloric acid (HCl) that was applied repeatedly to ensure the absence of carbonates and to separate out the carbon ash particles. According to the laboratory report, the sample provided sufficient carbon for an accurate measurement and the AMS analysis proceeded normally. The conventional radiocarbon age is 2250 ± 40 years BP whereas the calibrated radiocarbon age was calculated at 2340–2150 Cal BP.- Table 2. Radiocarbon age determination of the patina of the Jehoash Inscription tablet
Sample data Measured radiocarbon age 13C/12C ratio Conventional radiocarbon age Report date: 6/5/02 Material received: 5/20/02 Beta – 167445 2190+/−40 BP −21.1‰ 2250+/−40 BP Sample: BB Analysis: AMS Material/pretreatment Patina/acid and solvent washes 2 Sigma calibration Cal BC 390–200 (Cal BP 2340–2150 - Full-size table
3.4. Gold globules
Gold globules that we detected in the patina using backscattered SEM–EDS, are minute, usually 1–2 μm in diameter (Fig. 7) and were found in four of the nine samples taken from the patina. The gold is in the form of individual globules of well-sorted size. There are approximately 10 globules per mm2 in each of the four patina samples (Table 1). The total weight of the globules in the patina is calculated to be to less than 0.001 g for the entire tablet.3.5. Microcolonial fungi
Microcolonial fungi (MCF), known to concentrate and deposit manganese and iron, play a key role in the alteration and biological weathering of rocks and minerals (Staley et al., 1982 and Gurbushina, 2003). They are microorganisms of high survivability, inhabiting rocks in extreme conditions, and are also known to survive in subsurface and subaerial environments. Long-living black yeast-like fungi form pitted embedded circular structures of 5–500 μm in size (Fig. 9 and Fig. 10) (Krumbein, 2003, Krumbein and Jens, 1981 and Sterflinger and Krumbein, 1997). The MCF structures (Fig. 9) were found inside the last letter of the 14th row of the tablet. There is morphological continuity between the patina of the rock surface itself and the grooves of the letters (Fig. 5). The black orange-brown thin layers (films) of iron-oxide patina are the product of geomicrobiogenic activity that covers all surfaces of the tablet.
- Fig. 9. Biogenic pitting and black to orange-brown patina formation within the upper stroke letter ‘HEH’ (last letter in the 14th row, inverted) caused by black yeast-like fungi on arkosic sandstone of the JI tablet. Fused pits are visible in the middle of the photograph (groove width = 1 mm).
- Fig. 10. SEM photo showing the circular pits (P) and fungal hyphae (H) of the patina. The sample was taken from the border between letter incision and the natural rock, near the crack zone (scale bar = 30 μm).
4. Discussion
Layered platy arkosic sandstones occur in Cambrian formations exposed in southern Israel and in southwest Jordan (Bender, 1968) and were readily available to stone workers in Judea in ancient times. Such rocks are found south of the Dead Sea, in the Timna area and in southern Sinai, mainly in the Shechoret Formation (Weissbrod, 1987). In the Temple of Serabit el-Khadem in southern Sinai, many of stelae with hieroglyphic inscriptions from the Middle and New Kingdoms are carved from arkosic sandstone of the upper part of the Shechoret Formation. Goren et al. (2004) determined that the tablet was engraved in graywacke. However, there is no graywacke in Israel or Sinai.The patina coating the tablet carrying the inscription is composed of elements derived from the tablet itself (quartz and feldspar grains) as well as accretion from the environment (calcite and dolomite deposits, carbon ash particles, and gold globules). The patina from the back of the tablet is composed mostly of quartz and some carbonate. This siliceous-carbonate material could be an original vein filling along a bedding plane or a joint in the original rock, similar to those found in the Cambrian clastic rocks exposed in southern Israel and Sinai, and may represent a natural rock fissure along which the rock was detached for further processing as is the case in many quarries. No indications of adhesive materials or other artificial substances that could indicate addition, pasting, or dispersion of artificial patina on the inscribed face of the tablet have been observed.
The occurrence of pure gold globules (1–4 μm) is evidence of the melting (above 1000 °C) of gold artifacts or gold-gilded items. Gold powder comprised of globules 1–4 μm in diameter does not exist in the modern gold market, where gold globules have a wide range of sizes, the smallest diameter being 500 μm. On the other hand, gold powder, or gold dust, with an average size between 70 and 80 μm has an angular, flaky shape. Native gold dust from Sardis, Turkey contains irregular flattened flakes with rounded edges, 100–500 μm in size, but not globules (Geckinli et al., 2000). According to Meeks (2000), pure gold globules of 3–300 μm in diameter were found in the production and refining site of Sardis resulting from melting processes. One would thus expect many gold globules of various sizes to occur in clustered aggregates in the patina if it was of recent origin. This is clearly not the case. The small amounts detected would be difficult to produce within any artificial patina. Both the occurrence of carbon ash particles and gold globules in the patina are suggestive of a thermal event. It is proposed that the ‘apparent’ radiocarbon age of 2250 years BP is an average of a mixture of older and younger carbon fragments that have been incorporated into the patina over time, thus implying that there was more than one thermal event.
The microbiogenic patina is dense, coating all surfaces as well as the engraved letters, and indicates growth over extended periods of time. A Nabataean flint artifact from Avdat, southern Israel, 2000 years old (Krumbein, 1969) shows the following identical features to those found in the JI tablet: microcolonial fungi, a black orange-brown coloration and pitted circular structures.
Recently, the oxygen isotopic composition of the carbonate of the patina was analyzed and the results used to suggest that the JI tablet was not authentic (Goren et al., 2004). This conclusion was based on the assumption that the presence of oxygen in the carbonate could be explained by precipitation from meteoric groundwater in the Jerusalem area. The data of Goren et al.'s (2004) four analyses of patina taken from the surface of the tablet could, however, be interpreted differently. Two of their four results exhibit δ18O values (−1.7‰ and −0.9‰, PDB) that are anomalously enriched compared to local cave precipitates. However, these values are exactly what are to be expected from marine carbonate material. Exposures of Cretaceous marine carbonates are abundant in Jerusalem and provide a majority of its building stone. It is probably marine carbonates that were found within the JI tablet patina, with the particles derived from the weathering of these exposed rocks and deposited by wind. Indeed, well-preserved marine carbonate microfossils, such as Cretaceous to Eocene foraminifera, occur in abundance in everyday dust in Jerusalem ( Ehrenberg, 1860, Ganor, 1975 and Ganor et al., 2007) as well as in the local soils. Goren et al.'s (2004) other two reported δ18O values (−8.4‰ and −7.3‰) are depleted relative to modern carbonate formation data (−4‰ to −6‰) (Bar-Matthews and Ayalon, 1997). However, there are many ways that isotopically depleted carbonate can be generated and incorporated in a genuine patina, such as the process of decarbonation, that would indicate thermal events. Thermally induced decarbonation reactions of calcite and dolomite with the quartz or feldspar in arkosic sandstone or in the soil would result in residual carbonate with lowered δ18O values (Faure, 1986). Isotopic depletion, due to thermal metamorphism, occurs in lime-rich soils when they are intruded by igneous bodies (Katz et al., 1998). In the vicinity of Jerusalem, widespread lowering of δ18O values in normal marine carbonates of the Hatrurim Formation took place by decarbonation during (non-igneous related) thermal metamorphism (Kolodny and Gross, 1974). Calcite from the Negev oil shales exhibits δ18O values of −0.5‰ to −2‰ PDB; however, after heating these oil shales to 700–800 °C, depletion of δ18O values (−5.2‰ to −10.2‰ PDB) is obtained in the residual carbonate (Yoffe et al., 2002). Moreover, light oxygen isotope values are known to be deposited in the Judean mountains during years of high precipitation, that is, over 1000 mm of rainfall per year (e.g. see Fig. 6, Bar-Matthews and Ayalon, 1997). According to Kolodny et al. (2005), the dominance of the source effect in determining the oxygen isotopic composition of speleothems in the Levant reduces the power of δ18O as an independent climatic indicator. Because of the lack of knowledge of the mineralogical association of the oxygen isotopes, the burial and custodial history of the JI tablet, the oxygen data of Goren et al. (2004) is completely moot. No conclusions can be drawn from the oxygen isotope data. Further exposure, even for short periods of time, to surface conditions with varying amounts of rainfall, high temperature regimes and consecutive evaporation events may significantly alter oxygen isotope ratios. In addition, we would like to note that the modern cleaning processes of the JI tablet depending on the cleaner used could easily change the expected oxygen fractionation values in the patina.
5. Conclusions
Our analyses strongly support the authenticity of the Jehoash tablet and its inscription. All evidences indicate that the production of the tablet and the carving of its inscription occurred at essentially the same time. The critical evidence is as follows: (1) the central fissure and the upper breakage cut across several lines and letters and the patina extends down along the margins of the broken faces, (2) quartz and feldspar grains found within the patina are weathered from within the rock, (3) the patina is dense, microbiogenic and is indicative of growth over extended periods of time, (4) the two patina layers attached to the rock (black orange-brown and an upper lighter-colored one) that cover the tablet and inscription includes ash particles and minute, well-sorted globules of pure gold, a product of melting, (5) the age of the carbon ash interlocked within the patina is approximately 2250 years BP according to radiocarbon dating and, (6) no modern elements related to the use of modern tools were found.6. Note added in proof
Fig. 4, Fig. 5, Fig. 6, Fig. 7, Fig. 8 and Fig. 9 modified from Dahari, U., 2004. The James Ossuary: Ancient Relic or Modern Forgery? Cornerstone University Press, Symposium, 12 May 2004.Acknowledgments
We thank Dr. A. Honigstein, Ministry of National Infrastructures, Oil and Gas Section, Jerusalem, Israel, Dr. K. Kojonen, Geological Survey of Finland, and, Dr. A. Shimron, Geological Survey of Israel, Jerusalem, for their insightful reviews of an earlier version of the manuscript and suggestions for improvement. Constructive comments by two anonymous reviewers are gratefully acknowledged. We are grateful to M. Dvorachek, Geological Survey of Israel, Jerusalem, for help with the SEM–EDS work and Susan Feldman, Scarsdale, New York, for technical assistance. We thank Dr. Y. Natan, Geological Survey of Israel, Jerusalem, for identifying the carbon ash particles in the patina. WEK acknowledges the help of the ICBM electron microscopy unit and the Soil Science Department of Carl von Ossietzky Universität Oldenburg for microscopy and X-ray diffractometry as well as the Institute of Crystallography of the Würzburg University.References
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