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Bitumen from the Dead Sea in Early Iron Age Nubia

Abstract

Bitumen has been identified for the first time in Egyptian occupied Nubia, from within the town of Amara West, occupied from around 1300 to 1050 BC. The bitumen can be sourced to the Dead Sea using biomarkers, evidencing a trade in this material from the eastern Mediterranean to Nubia in the New Kingdom or its immediate aftermath. Two different end uses for bitumen were determined at the site. Ground bitumen was identified in several paint palettes, and in one case can be shown to have been mixed with plant gum, which indicates the use of bitumen as a ground pigment. Bitumen was also identified as a component of a friable black solid excavated from a tomb, and a black substance applied to the surface of a painted and plastered coffin fragment. Both contained plant resin, indicating that this substance was probably applied as a ritual funerary liquid, a practice identified from this time period in Egypt. The use of this ritual, at a far remove from the royal Egyptian burial sites at Thebes, indicates the importance of this ritual as a component of the funeral, and the value attributed to the material components of the black liquid.

Introduction

Black materials were excavated from different contexts in the pharaonic town of Amara West in Upper Nubia, dating from  around 1300 to 1050 BC  (19th–20th dynasties), and its cemeteries (1250–800 BC). The materials were of three types: black paints on ceramic sherds used as palettes; a black coating on a coffin plaster fragment; and a black friable material excavated from a tomb. Considering a group of contextually different black materials from a single site together offers an opportunity to understand the cultural and practical preferences for the choice of materials used to make black substances, and in which contexts they might be applied. Molecular analysis using gas chromatography-mass spectrometry (GC-MS) was used to identify the components of the different materials using three separate methods. Identifying the components allows the ingredients of the black substances to be connected to their end uses both in practical and symbolic terms.

Amara West

Amara West lies between the Second and Third Nile Cataracts, in the heart of Nubia, a region that stretched from Aswan in southern Egypt southwards to the Sixth Nile Cataract1 (Fig. 1). This region was intermittently occupied by pharaonic Egypt in the third and second millennium BC; during the New Kingdom (c. 1548–1086 BC), pharaonic towns were founded to control and administer resource extraction2. First excavated by the Egypt Exploration Society between 1939 and 19503, fieldwork was then undertaken at Amara West by the British Museum from 2008 to 20194,5,6. The town, founded around 1300BC (on the basis of inscriptional evidence), comprised a sandstone temple, a governor’s residence, storage facilities, and housing, set within a 108 m square enclosure wall2 (Fig. 1). From the late 19th Dynasty residents of the town began to build larger and more spacious houses outside the town wall, an area designated by the excavators as the “western suburb”7,8. While the latest architecture identified in the town dates to the late New Kingdom, ceramics scattered on the surface and burials in the associated cemeteries suggest a population living here, or nearby, through to the 8th century BC9.

Figure 1
figure1

Map of Egypt and Sudan showing the location of Amara West, and [inset] layout of the site of Amara West. Image: Amara West Project, Trustees of the British Museum. The map was created using Adobe Illustrator 2019 adobe.com.

Painting materials

Large quantities of painting materials were discovered in the form of ceramic sherds used as paint palettes (Fig. 2a), lumps of pigment, and grindstones, in an area at the front of storage magazines, which was possibly being used as a working area (E13.14)10. These magazines date to an early phase of the walled town in the 19th Dynasty, c. 1250 BC. Further finds, though in lower numbers, of palettes and pigments were found throughout the western suburb, which was constructed from the end of the 19th Dynasty and inhabited through the 20th Dynasty and later, c. 1180 BC to 1000BC. The colours of paint found in the palettes were red, yellow, white, black, blue, and green. Over 900 palettes were discovered in total, 31 containing black paint. No lumps of black pigment were identified, although charcoal was frequently found at the site.

Figure 2
figure2

(a) Black paint in palette F6167, from magazine E13.14.2 in the walled town (b) Friable black solid F8623 as uncovered  in tomb G321  in cemetery D (c) Friable black solid from G321 with textile impressions. Photos: Amara West Project, Trustees of the British Museum.

Funerary materials

Two cemeteries are associated with Amara West, referred to as Cemeteries C and D. A large rock-cut  tomb (G321) in Cemetery D, originally marked with a pyramid, was first used  for burials in the 20th Dynasty (c. 1190–1086 BC), with further use of the tomb into the 8th century BC. The archaeological deposits within, which have been disturbed in modern times (as evidenced by the presence of cigarette butts), included bone, wooden fragments and small pieces of painted plaster from coffins, and a large quantity of chunks of friable black material (F8623). The black material was scattered about in the fill, but one layer was preserved spread over an area approximately 20 cm square next to skeletal remains (Fig. 2b). The thickness was about 2 cm. The larger chunks retained textile impressions, indicating that it originally adhered to a textile, possibly wrappings on a body (Fig. 2c); the excavation records state that “bitumen with traces of wrapping” were found in this context. The chunks are too small to be able to tell if the wrappings adhered to the outside or inside of the textile. Either way, it appears that they formed part of the preparation of the body for burial, examples of this practice are known from other coffins (e.g. coffin EA20744 in the British Museum11).

A fragment of painted plaster from a coffin (F9743) found in tomb G244 in Cemetery C (19th–20th Dynasty) preserved a layer of a painted black substance, thicker than the usual decorative paint. The original scope of this black layer is not clear from the fragmentary state of the coffin remains, but it appears to have been applied to the exterior of the coffin over the outer plaster layer.

Results

Five samples of black paint were taken from palettes from the early walled town, and five from palettes from the Western Suburb. Two samples of applied black material were taken from coffin fragments from tomb G244, and five further samples were taken from the black friable lumps found in tomb G321. One reference sample of archaeological Dead Sea bitumen from the British Museum Reference Collection was analysed alongside the samples. This material was procured from Tel Aviv University in the 1970s. Results were compared to data in the literature. The presence in each sample of bitumen, lipids, and gums, determined using separate methods, is shown in Table 1.

Table 1 Samples analysed by GC-MS. E and D designate grid numbers at Amara West. Check mark indicates compound class was identified; Tr = trace; n = none detected; blanks indicate that the sample was not tested.

Results - Bitumen

Positive identification of bitumen in the samples analysed was determined by the presence of ions m/z 191 (hopanes) and m/z 217 (steranes)12,13,14, as shown in Figs. 3 and 4. Hopanes are abundant molecular fossils derived from terpenoids in bacteria and present in nearly all organic sediments15. Steranes are four-ring hydrocarbons derived from the degradation of steroids and sterols found in most higher plants and algae (but rare or absent from bacteria) via diagenesis and thermal maturation16.

Figure 3
figure3

Mass chromatogram for ion m/z 191 (terpanes and hopanes) for AS1932 from G321 (friable solid), palette PS152, and reference sample from the Dead Sea, showing positions of terpanes (20/3 to 30/3), hopanes (29αβH to 34αβH; hopanes 31–34 are split into S and R), Ts, Tm, and gammacerane (GCR).

Figure 4
figure4

Mass chromatogram for ion m/z 217 for AS1932 from G321, palette PS152, and reference sample from the Dead Sea, showing positions of steranes.

Of the 10 samples of paint from palettes (PS numbers), 9 were found to contain bitumen, although those from the suburb only in trace amounts. All samples from the friable solid in tomb G321 (AS numbers) were found to contain bitumen. Samples PS295 and PS297 from the painted coffin fragments in G244 also contained bitumen.

Ratio data for a range of bitumen biomarkers are shown in Table 2. The results given in Table 2 are for the samples which provided good enough chromatograms from which to take data. Other samples showed hopanes and steranes but at trace levels such that peaks could not be reliably integrated. The ratios were calculated using the areas under the peaks obtained by manual integration. Selected ratios are plotted in Fig. 5 with comparative reference data.

Table 2 Results of GC-MS analysis of Amara West and reference samples, biomarkers. Pr/Ph = pristane/phytane, data taken from total ion chromatogram (TIC). All other data from m/z 191: Ts = 18α(H)-22,29,30-trinorhopane, Tm = 17α(H)-22,29,30-trinorhopane; GCR = gammacerane; Ol = oleanane; CnαβH = 17α,21β-hopane at Cn; C31R = 17α,21β-22R-30-homohopane at C31; C29αβH = 17α,21β-norhopane at C29; Cn = 17α,21β-22S + R-29-homohopane at Cn; C26/C25 TT = C26/C25 tricyclic terpanes. ND = no data.
Figure 5
figure5

Radar plot for samples AS1932 from G321, palette PS119, black layer from coffin fragments PS295 (all group A), and palette PS121, as well as a reference sample from the Dead Sea, and data from Gebel Zeit37. See Table 2 for abbreviations.

Results - Lipids

The paint samples from the palettes (PS numbers) contained no resins, oils, fats, or waxes. Analysis results from G321 material (AS numbers) varied, due to the fact that this substance was not homogenous (Supplementary Table S1). Slightly different results were obtained for AS1932 and AS1994 by the two GC methods, most likely due to sample heterogeneity. AS1932 (Fig. 6), AS1933, and AS1994 contained several organic products. The presence of fatty acids, with stearic acid predominating, traces of triacylglycerols, and no diacids, suggests an animal fat17,18. Wax esters with carbon chain length 42, 44, 46, and 48, and long chain fatty acids, evidence a natural wax component19,20. The mass spectra of the wax esters have a peak at m/z 257 indicating an acid moiety with 16 carbons, thus are a series of even carbon number long-chain palmitate wax esters, probably indicating the presence of beeswax21, although no alcohols or alkanes were detected, possibly due to heating in ancient times19. In the mass spectra of the wax esters of carbon chain length 44, 46 and 48, m/z 257 is the base peak and there is also a peak at m/z 285 (Supplementary Fig. S1). For the ester with 42 carbons observed in the chromatogram for AS1933 m/z 257 is present but the base peak is m/z 285. The m/z 285 ion indicates an acid moiety in the wax ester with 18 carbons, suggesting the presence of another waxy material, possibly plant based22. Peaks for oleanonic acid and moronic acid, with traces of masticadienonic and isomasticadienonic acids indicate that the resin from Pistacia sp. was a component of the mixture23,24,25. The samples taken from AS1941, AS1948, and AS1949 gave very poor chromatograms for lipids. Sample PS295 from the coffin gave a poor chromatogram with a peak for moronic acid, indicating that this material also contained pistacia resin. Given the heterogeneity of the samples from G321, it is possible that a larger sample from this coffin may have included a wider range of ingredients.

Figure 6
figure6

Chromatogram for AS1932 (Method B1). FAn:0 = saturated fatty acids with n number of carbons; Wn = wax ester with n number of carbons.

Results - Gums

Plant gums are sugary substances composed of monosaccharides. Identifying the range of monosaccharides present can sometimes enable the identification of the plant from which the gum was taken; published analyses of plant gums report the presence of the monosaccharides arabinose, fucose, xylose, mannose, rhamnose, galactose and glucose in varying quantities26,27,28,29.

Of the three samples from palettes analysed for monosaccharides, one (PS121) contained fucose, mannose, galactose, and other unidentified sugars (Supplementary Fig. S2), which indicates that plant gum was used as a binder with the black pigment. The other two were either not mixed with a gum or the material was too degraded to be detected using this method. The presence of fucose suggests that the gum is tragacanth, obtained from the roots of Astragalus sp., but the presence of mannose points to a fruit gum, although mannose has been reported in tragacanth gum by one study26,29,30. Astragalus sp. grows in Turkey, Syria, Iraq and Iran, and would have been imported into Egypt31. A similar result was reported for paint samples from one New Kingdom object (17, mummy mask) and two Third Intermediate Period objects (21, mummy mask; 22, falcon) from the Museum of Fine Arts, Boston32. The authors concluded that the binders may have included tragacanth but were probably a mixture of gums32.

Discussion

Source of bitumen

Bitumen is composed of geologically old organic matter; its molecular make-up depends on the original living organisms that decayed to create it, which varies between formations33. Biomarkers are the “molecular fossils” from these organisms that are present in petroleum products, and can be used to identify types of source rock of petrochemicals and to match compounds from the same source14. A range of biomarkers should be considered because it is sometimes unclear to what extent each biomarker can predict the depositional environment14,34, and there are further issues with archaeological samples such as alterations to the chemical structure of the samples due to their archaeological depositional environment (rather than the geological one which formed the bitumen), and contamination from other substances. In addition, the pattern of hopanes (m/z 191) and steranes (m/z 217) can be studied for similarities with samples of known origin35,36.

Each biomarker is difficult to interpret independently, but the cumulative evidence seems to point to a marine carbonate source rock for most of the Amara West bitumen (Supplementary Table S2). The chromatograms of the friable material from G321, PS295 from the coffin, and palettes PS119, PS152, and PS415 (herein referred to as Group A) show a very similar pattern. Gammacerane (GCR) is prominent for Group A, and oleanane absent or very low. Diasteranes (m/z 259) are very low or absent for all of Group A. The patterns of the chromatograms for Group A are similar to those obtained for the Dead Sea from the reference sample and in the literature (Figs. 3 & 4). Dead Sea bitumen is characterised by a low pristane/phytane ratio of around 0.5, very low or absent diasteranes, low oleanane, high gammacerane, high C35/C34 homohopanes, and a complete series of tricyclic terpanes (C19–C30), maximizing at C2335,37,38,39. Ts/Tm varies slightly for Dead Sea samples reported in the literature, from 0.04 in geological samples to 0.08 in archaeological samples13,35. Most of the samples analysed from Amara West fit into this range, with the exception of PS121.

The black pigment from Amara West palette PS121 has different biomarker values from the other Amara West samples (Table 2). The oleanane index is higher (0.14 compared to average 0.013 from the AS samples from G321), and the gammacerane index lower (0.25 compared to average 0.67 from the AS samples from G321; Table 2). These results are unlikely to be explained by biodegradation, as it would be expected that both the oleanane and the gammacerane levels would be elevated40. It appears likely that this sample had a non-Dead Sea origin, especially considering the presence of oleanane, which is very low or absent for the Dead Sea and other Amara West samples. Another source of bitumen in Egypt is Gebel Zeit37,41, but as can be seen from Table 2 and the radar plot in Fig. 5, the data from Gebel Zeit does not match any of the samples in this study. The origin of the bitumen in PS121 cannot currently be identified, and may be from a mixture of sources, which would make definitive identification difficult.

Significance of bitumen as a pigment

The ground black material from the palettes contained bitumen in 9 out of 10 cases, and one of these was shown to have been mixed with a plant gum binder to make a paint. This is the first molecular identification of bitumen being used as a ground pigment in a pharaonic context. There is one other published example of bitumen used as a pigment in Egypt prior to the Roman Period, on a 19th Dynasty model boat from Gurob, but this finding has not been confirmed by molecular analysis42. Most black paints and inks from ancient Egypt have been identified as carbon, obtained from burning organic matter43,44,45, but given the difficulties of distinguishing elemental carbon from bitumen, which is only really possible using molecular analysis (GC-MS), it is possible that the use of bitumen as a pigment in ancient Egypt has been under identified. The use of bitumen could have been a lot more extensive than is indicated by the evidence to date, and this should be taken into account in future pigment studies. While some of the samples come from occupation and rubbish deposits found within storage magazines (E13.14), and thus might reflect the  period when apparatus of the pharaonic state was most prevalent at Amara West (inscriptions, storage facilities, seal impressions), other instances were identified in the latest phases of occupation, suggesting a continuing  use of bitumen as a pigment. Nonetheless, the Dead Sea origin of the bitumen indicates that this trade would have been coming from the north, through Egypt.

Given the ease with which carbon can be obtained, i.e. by burning anything organic, the use of bitumen as a pigment must have had a significance. We do not know the end-use of the black pigment in the palettes, but it is possible it was being reserved for a particular use.

Significance of bitumen in a funerary context

The friable material from tomb G321 was found to consist of resin from Pistacia sp., a lipid component (fat or oil), wax, and bitumen. The composition of the G321 material is very similar to mummification “balms”, however the black material from Amara West was not found on the body or in body cavities, but instead in scattered fragments and in one area quite a thick, flat puddle close to but not on a (disturbed) body. The black material was applied as a liquid, which allowed textile impressions to form on the surface of the substance when it solidified. This suggests it may have been applied to the exterior of a wrapped body. Black ritually applied liquids are known from the exterior of wrapped bodies and funerary containers from Egypt, and are the subject of current research at the British Museum. Analyses of these externally applied black liquids has shown them to consist of lipids, beeswax, bitumen, and conifer resin or pistacia resin in various combinations (for example, EA6662, EA6660, EA48001, and EA24906 in the collections of the British Museum46,47). The components of the black material from Amara West and the context in which it was found are consistent with the Egyptian black funerary liquids. The black material from the coffin fragments from G244 also contained bitumen and pistacia resin, and appears to have been applied to the surface of the coffin. Given the similarity in components and context to the material in G321, it seems likely that this was also a ritually applied black liquid. The use of similar ingredients in mummification balms and black varnishes on funerary statues suggests that this black liquid had multiple uses in funerary practice13,33,48,49,50,51,52,53,54. A link to Osiris may be inferred from the colour of the substance, Osiris is known as “the black one” and shown with black skin, and from the similarity of the liquid to mummification balms, the deceased is identified as an aspect of Osiris55.

Significance of bitumen at Amara West

The biomarkers in the black materials from Amara West are consistent with those of Dead Sea examples, which is likely to be evidence for a trade in solid bitumen from the Dead Sea into Nubia over the 19th and 20th dynasties (c. 1300 to 1070 BC). Evidence for the trade in bitumen into the Nile Valley during the New Kingdom has so far been very limited, so this would be a major contribution to this dataset. Alternatively, the bitumen found in G321 may relate to the later use of the tomb, in the period after Egyptian occupation, as ceramics diagnostic of that date and distinctive Nubian wooden funerary bed fragments were found in the same context. If this is the case, it may reflect the adoption, and perhaps reinterpretation, of Egyptian funerary practises by individuals who identified as Nubian. Previous studies have found bitumen in mummification materials from the Third Intermediate Period to the Roman Period (c. 1086 BC to 300 AD), most of which was shown to have come from the Dead Sea13,33,41,56,57,58,59,60, and a trade route for Dead Sea bitumen into Egypt in the 4th to 3rd millennium BC has been identified from lumps of archaeological bitumen38. Molecular evidence for bitumen from the New Kingdom (pre-dating the Third Intermediate Period) is limited to the black coating on the coffin of Henutmehyt in the British Museum (EA48001)46, the balm of a mummified man from Thebes13, an identification of Dead Sea bitumen in a 19th Dynasty “mummy balm”12, and the presence of hopanes in the black coatings on an 18th Dynasty canopic chest and anthropoid coffin49. Amara West was founded by the pharaonic state but the presence at the town of  individuals who identified as Nubian is suggested by the production and use of Nubian pottery, and building. E12.11 that reflects Nubian architectural traditions9,61,62,63. The evidence from the tombs at Amara West appears to demonstrate an integration of Egyptian funerary and technological traditions with those from Nubia, such as the tumulus superstructure over tomb G244, from which the coffin fragment comes9. In this context it is interesting to see evidence for the use of a ritual black liquid that is linked to the Egyptian embalming tradition.

Conclusion

This study provides evidence of the use of bitumen from the Dead Sea and another origin, in Nubia during the early Iron Age pharaonic occupation of the region and its immediate aftermath. This bitumen was found in two contexts, ground and mixed with gum to make a black paint, and as a component of an organic ritual liquid.

The results provide the first molecular identification of bitumen used as a ground pigment in a pharaonic context, albeit outside Egypt itself. It is possible that bitumen has hitherto been under recognised as a painting material in the ancient Nile Valley and should be considered by future pigment studies.

The black substance from G321 and the coffin fragments are examples of an Egyptian funerary ritual using long-distance imported ingredients, for at least two individuals on two separate occasions. The use of this ritual at a far remove from the royal Egyptian burial sites at Thebes, and in graves reflecting the entanglement of Egyptian and Nubian funerary traditions, indicates the importance of this ritual as a component of the funeral, and the value attributed to the material components of the black liquid. The liquid probably had important ritual associations with Osiris, who is associated with the dead and the colour black.

Given that evidence for bitumen use in Egypt in the New Kingdom has previously been limited to a few individual samples from objects with poor provenance12,13,42,46,49, this study provides proof for a much more extensive use than might have been suspected, with a secure archaeological context.

Methods

Three methods were used, each designed to analyse the samples for a different set of components: bitumen, lipids, and gums. The aim was to determine the extent of the use of bitumen at the site and whether the other components of the materials would provide clues for different end uses. Previous analysis of Egyptian paints has shown that plant gums were used as a paint binder31,64,65,66,67,68, whereas black funerary liquids were complex mixtures of organic products13,46,50,52,53,56,69,70. As stated in other publications13,71 the analysis method will determine the components that can be detected, so different methods were applied.

Method A - bitumen analysis

Samples were dissolved in 1 ml dichloromethane (DCM), and heated at 40 °C for 2 hours, after which the solution was decanted, and dried under a stream of nitrogen. This was done 3 times, combining the extracts. 20 µl DCM and 1 ml hexane were added to the soluble fraction, the asphaltene fraction precipitated out, and this was left overnight to settle. The solution was then decanted and dried under a stream of nitrogen to obtain the maltene fraction.

Each maltene fraction was then fractionated using column chromatography. 100 µl hexane was added to the maltene fraction. Each was decanted into a glass pipette held upright and plugged with glass wool and half filled with dried silica (chromatography grade 60–120 µm, pre-extracted with DCM/methanol 97:3 (v:v), followed by hexane, then oven dried) to which hexane had been added to exclude moisture. The first fraction was extracted using 3 ml hexane washed through the pipette; the second using 3 ml DCM:hexane 1:3 (v:v); the third using 3 ml DCM:methanol 2:1 (v:v). The elutes were collected and dried in a stream of nitrogen. For analysis, 50 µl of hexane was added to the first fraction and this was decanted to a micro vial.

The GC-MS analysis was carried out with an Agilent HP5-MS column (30 m × 0.25 mm, 0.25 µm film thickness) with splitless injection, coupled to an Agilent 5973 MSD. The mass spectrometer was operating in the electron impact (EI) mode at 70 eV and scanning m/z 50 to 550 amu. The oven was set at 60 °C to 290 °C at 4 °C/min with the final temperature held for 30.5 mins. GC-MS analysis was run in two modes: scan and Selective Ion Monitoring (SIM). Acquisition in SIM mode targeted ions: 177, 191, 217, 218, 259.

Method B - Lipid analysis

Samples were solvent extracted 3 times using DCM, as in Method A, and the resulting combined extracts were dried under a stream of nitrogen. Each was derivatised using 100 µl silylating reagent N,O-bis(trimethylsilyl)trifluoroacetamide (BSTFA) plus 1% trimethylchlorosilane (TMCS), heated at 70 °C for 1 hour. After cooling, samples in BSTFA were auto injected into the GC.

Method B1

The GC-MS analysis was carried out with a SGE HT5 GC column (12 m × 0.22 mm; 1 µm film thickness) with splitless injection, coupled to an Agilent 5975 C MSD. The mass spectrometer was operating in the electron impact (EI) mode at 70 eV and scanning m/z 50 to 1000. The oven was set at 50 °C to 370 °C at 10 °C per minute, isothermal for 15 minutes.

Method B2

Two further samples were taken from AS1932 and AS1994, which were prepared in the same way, and run on a longer method to further separate the peaks. The oven was set at 50 °C to 320 °C at 5 °C per minute and then 10 °C to 370 °C, isothermal for 15 minutes. PS295 was only run on the longer method, because the sample was taken at a later date.

Data were collected in scan and SIM mode. GC-MS analysis was run in two modes: scan and Selective Ion Monitoring (SIM). Acquisition in SIM mode targeted ions: 0–15 mins (aromatics) m/z 105, 205, 267, 297; 15–25 mins (conifer) m/z 219, 239, 253, 459; 25–35 mins (pistacia) m/z 189, 409, 421, 526.

Method C - Gum analysis

Samples for gum analysis were taken from PS119, PS121 and PS139

The method followed for the analysis of Amara West paints for plant gums was the standard operating procedure used at the British Museum for the preparation of polysaccharide samples for GC-MS analysis of neutral sugars and uronic acids, based on a published method26.

Samples and reference samples were hydrolysed by the addition of 500 µl of 0.5 M hydrochloric acid and heated at 80 °C for 20 hours. The solution was decanted and dried under nitrogen. Samples were derivatised by the addition of 300 µl Sigma-Sil A (1:3:9 ratio of trimethylchlorosilane (TMCS), hexamethyldisilazane (HMDS) and pyridine), and heated at 80 °C for 2 hours. Samples were dried under nitrogen and dissolved in 100 µl hexane in preparation for injection into the GC-MS instrument. A blank and three reference samples were prepared alongside the samples using the same method.

The instrument and column used were the same as for the bitumen analysis. The oven was set at 40 °C to 130 °C at 9 °C/min, then to 290 °C at 2 °C/min, with the final temperature held for 10 mins.

In all cases the data were analysed using Masshunter software and the NIST database.

Data availability

All relevant data are within the paper and its Supporting Information files. Archive documents referred to in the paper are held in the archives of the British Museum, Department of Scientific Research (Project Record no. 7671) and can be viewed in hard copy or electronically by appointment through science@thebritishmuseum.ac.uk.

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Acknowledgements

The samples were excavated as part of fieldwork of the British Museum Amara West Project, funded by the Qatar-Sudan Archaeological Project. This research would not have been possible without the assistance of the Sudan National Corporation for Antiquities & Museums, who generously allow the export of archaeological samples for scientific research. The research was conducted as part of an AHRC funded collaborative PhD between UCL and The British Museum. Thanks are also due to Professor Ian Freestone and Dr Ruth Siddall of UCL who co-supervised the PhD. Wellcome Trust grant 097365/Z/11/Z funded Open Access costs and technical support provided by Chris Mussell.

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K.F. collected samples, performed the analysis, and wrote the paper. R.S. supervised the analysis and revised the paper. N.S. directs the Amara West Research Project and  contributed towards the archaeological interpretation.

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Correspondence to Kate Fulcher.

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Fulcher, K., Stacey, R. & Spencer, N. Bitumen from the Dead Sea in Early Iron Age Nubia. Sci Rep 10, 8309 (2020). https://doi.org/10.1038/s41598-020-64209-8

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