Over a thousand people feared dead following landslide in the Darfur Region of Sudan.

Over a thousand people are feared to have died following a landslide which hit the village of Tarseen in the Mara Mountains in the Dafur Region of Sudan on Sunday 31 August 2025. The village is reported to have been completely destroyed by the landslide, with only a single known survivor having been found by local rescue teams. A United Nations humanitarian team in Sudan estimates that the village has a permanent population of about 370 people, however the Sudan Liberation Movement/Army, a rebel group fighting for independence for Darfur which is the effective authority in the region, has claimed that as over a thousand people may have died, as about 300 families internally displaced by fighting within the region had taken shelter in the remote village.

Local rescue teams searching for survivors following a landslide which destroyed the village of Tarseen in the Darfur Region of Sudan on 31 August 2025. Sudan Liberation Movement/Army/AFP/Getty Images.

The landslide occurred following weeks of heavy rain in the region, associated with the annual wet season of southern Sudan. Landslides are a common problem after severe weather events, as excess pore water pressure can overcome cohesion in soil and sediments, allowing them to flow like liquids. Approximately 90% of all landslides are caused by heavy rainfall. The annual wet season lasts from June to September, and with rain typically falling in a series of extended very heavy rainfall events. This makes the region extremely prone to landslides and flooding, something compounded by the country's week infrastructure and frequent civil conflicts, which make its population extremely vulnerable to such events. Such extreme weather events have become worse in recent years, driven by rising global temperatures, something which is also causing increased aridity in the drier north of the country, further fuelling internal conflicts as different populations compete for resources. 

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Outbreak of Hepatitis E in Ouaddai Province, Chad.

An outbreak of Hepatitis E has resulted in seven deaths and over 2000 people becoming sick in Ouaddai Province, Chad, according to a press release issued by the World Health Organization on 8 May 2024. The outbreak was first detected on 2 January 2024 when to cases of Acute Jaundice Syndrome were reported by medics from Médecins Sans Frontières who were operating a clinic at a temporary high school at a refugee camp in the Adré Health District of Ouaddai Province.

Between 2 January and 15 February 2024 the number of reported cases of Acute Jaundice Syndrome in Adré Health District rose to 113, of which 28 were confirmed as being Hepatitis E using rapid diagnostic test kits. On 19 February a case was reported at the Allasha Refugee Camp in the Hadjer-Hadid Health District, also Ouaddai Province.

Between 1 and 19 March 2024 forty blood samples taken from Acute Jaundice Syndrome sufferers in Ouaddai Province were sent to the Institute Pasteur of Dakar, Sénégal, where they were tested for Hepatitis E, Yellow Fever, Dengue, West Nile Fever, Zika, Chikungunya, Rift Valley Fever and Crimean-Congo Haemorrhagic Fever. Of these, 36 tested positive for Hepatitis E.

A refugee camp in eastern Chad in January 2024. Médecins Sans Frontières.

Between 2 January and 28 April 2024 a total of 2092 suspected cases of Hepatitis E were reported in Ouaddai Province, with seven fatalities. One hundred and three of these cases were members of the local conflict, while the remaining 1989 were refugees from the conflict in neighbouring Sudan, with the Lycée d'Adré, Aboutengué, and Metché refugee camps being particularly badly hit. 

Hepatitis E is caused by a single-stranded, nonenveloped, RNA Virus, and is usually a self-limiting infection, causing fever, nausea, loss of appetite, vomiting, jaundice, abdominal and joint pain and discolouration of the urine and stool, which typically passes within 2-6 weeks. However, in some cases the disease can cause acute liver failure (hepatitis) which is often fatal. Pregnant women are considered to be at particular risk from this disease, with a fatality rate of about 30%, compared to about 1% for the general population.

The Hepatitis E Virus. Centers for Disease Control and Prevention/Wikipedia.

Hepatitis E is spread through faeces and contaminated water, and thrives in unsanitary and crowded conditions. This makes it a particular problem in settings like refugee camps, where large numbers of people fleeing conflict situations arrive over short periods of time, overwhelming local sanitation systems. 

A queue of water containers at the Metché Refugee Camp in Ouaddai Province, Chad, where Médecins Sans Frontières is providing clean water. Médecins Sans Frontières.

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Looking for the origins of garnets from Lower Nubia.

From about the third century BC, garnets became highly valued gemstones to the peoples of the Mediterranean Basin, the Middle East, India, Sri Lanka, Southeast Asia, and China, along with other hard gemstones, such as emerald, aquamarine, and sapphire. Transparent red garnet was used to make engraved rings or seal stones; inlays in diadems; earrings or necklaces or even small sculptures; thin, doubly polished plates in cloisonné jewellery, as well as simple beads, merely drilled to be assembled into necklaces, bracelets, or applied to garments. Studies of garnets dating from the Hellenistic Period to Early Medieval times have identified seven distinctive garnet types (A-G), with unique compositions, some of which have been linked to sources in Europe, India, or Sri Lanka, while the source of others remains unknown.

Garnets were also used as gemstones prior to the Hellenistic Period in several places, although the origin and typology of these is less well understood. Green grossular, a calcic garnet, often intergrown with green vesuvianite was used to make seals, beads, and amulets by the Indus Valley Civilization, and to much lesser extent in ancient Mesopotamia. This material was worked in Harappa, Mohenjo-Daro, and Loal-Mari on the Indus River, and was probably sourced in Balochistan and northern Pakistan. Both grossular and vesuvanite have hardnesses of between 6.5 and 7.0 on the Moh scale (i.e. are slightly softer than quartz) making it possible to work these materials with the tools available to the Indus Valley Civilization.

Red aluminous garnet, however, is harder than quartz, making it much more difficult to work without specialist tools, and is rare in Asia before the advent of the Iron Age. Surprisingly, this material was worked early in Northeast Africa, with red garnet beads known from Predynastic Egypt and the contemporaneous A-group Cultures of Lower Nubia. The use of red garnet continued in Egypt till around the end of the New Kingdom, after which the mineral is seldom found. Thus, the red garnets of Egypt and Nubia are the oldest known examples of the working of this mineral.

In a paper published in the journal Archaeometry on 7 March 2024, Albert Gilg of Engineering Geology at the Technical University of Munich, Joanna Then-Obłuska of the Antiquity of Southeastern Europe Research Centre at the University of Warsaw, and Laure Dussubieux of the Elemental Analysis Facility at the Field Museum, present the results of an analysis of 34 garnet beads from burials in Lower Nubia, dated from the late A-Group to the Post-Meroitic, an age range of about 3200 BC to about 600 AD, as well as two garnets from separate alluvial deposits near the Fourth Cataract of the Nile in the Bayuda Desert of Upper Nubia.

Ancient Nubia is divided into Lower Nubia, which lay between the First and the Second Cataracts of the Nile, and Upper Nubia, to the south of the Second Cataract. Gilg et al. selected beads excavated  from graves in Qustul, Adindan, and Serra East, in the collection of the Museum of the Institute for the Study of Ancient Cultures at the University of Chicago, associated with the Early Nubian A-group Culture, the Middle Nubian C-group and Pan Grave cultures, and the New Kingdom, Napatan, Meroitic, and Post-Meroitic/Nobadian periods.

The A-group Culture (roughly 3700 to 2800 BC) and C-group Culture (roughly 2300 to 1550 BC) are known to have been wealthy societies, due to their location at a junction of trade routes between Egypt and the Mediterranean to the north and the African interior to the south. The Pan Grave people (2200 to1550 BC) lived in small, dispersed groups in the Eastern Desert. All of these peoples traded to differing extents with the Pre-Kerma and Kerma cultures of Upper Nubia. Between about 1570 and about 1069 BC Nubia was controlled by the Egyptian New Kingdon, then between 747 and 656 BC, Egypt was ruled by the Kushite 25th Dynasty, which ruled an area from the confluence of the Blue and White Niles to the Mediterranean. This interval forms part of the Napatan Period in Nubia, which lasted from about 750 BC to about 350 BC, and was another period of wealth in Lower Nubia. This was followed by the Meroitic Period, from about 350 BC to about 350 AD, when Lower Nubia became an intermediary in trade between the Kingdom of Meroë in Upper Nubia and the Hellenic and Roman rulers of Egypt. Between about 350 and 600 AD Lower Nubia was Kingdom of Nobadia, which often had less peaceful relations with both Egypt and the Blemmye peoples who controlled the Eastern Desert and the Red Sea Coast.

Map of Nubia. Gilg et al. (2024).

Gilg et al. analysed garnet beads from tombs 11, 17, 22, 24 of Royal Cemetery L at Qustul, which have been dated to Late A-Group/Naqada III (Naqada III is the final phase of Predynastic Egypt), as well as the late A-Group tombs W19 and V59; garnets from these tombs were commonly accompanied by similarly shaped carnelian beads. Another bead was from the  C-Group Phase III tomb T12B at Adindan, which is of equivalent age to the Egyptian 18th Dynasty (the first dynasty of the New Kingdom). Five more beads come from tombs K74 and K93 at Adindan, which were associated with the Pan Grave Culture; notably, garnet beads are more common in Pan Grave Culture burials than C-Group Culture burials, despite the two being roughly contemporary. Six more beads came from New Kingdom tombs VC45 and R19 at Qustul, three from the Amenhotep III to Amarna Period and three from the post-Amarna Period. A single short barrel bead came from the 25th Dynasty/Napatan tomb W43 at  Qustul. Also from Qustul came an oblate bead from the Meroitic tomb Q465, and a truncated hexagonal bicone bead from the Post-Meroitic tomb Q143.

Beads associated with the A-Group culture are all less than 5 mm in diameter and 2.5 mm wide. They were shaped into short cylinders, barrels, or oblates with a relatively poor polish, and perforated from each end by irregular pecking. Similar beads are known from Predynastic Upper Egypt, which were presumably made in the same way, possibly from the same people. A single bead of similar appearance has also been found at Mehrgarh in Pakistan, which is exotic to that site, but of unknown origin. C-Group and Pan Grave Culture beads are also typically poorly polished and of imperfect shape, though the shape varied slightly, with both rounded and short-barrel beads found. These beads were perforated from each end by drilling, forming either cylindrical or conical holes; the smooth nature of the hole suggests the drill made from a hard stone, such as flint, or possibly copper. Similar perforations have been observed in Middle Kingdom garnet beads from Egypt. Workshops producing carnelian beads are known from A-Group and C-Group sites in Lower Nubia, and while no trace of garnet-working has been found at these sites, the similarity between the carnelian and garnet beads suggests that the garnet beads are also likely to have been manufactured locally.

Microphotographs of garnet beads from lower Nubia. (a) A-group bead with irregular pecked hole (ISAC 13); (b) Pan Grave bead with a smooth drilled hole (ISAC 21); (c) C-group bead with silver beads (ISAC 20);  (d) New Kingdom long barrel-shaped beads with poor polish (ISAC 29-31); (e) Meroitic irregular oblate bead (ISAC33); (f) Post-Meroitic facetted bead (ISAC 34); (g) drill hole (about 1 mm in diameter) with concentric deep grooves from a diamond tipped drill (ISAC 34); (h) tiny short- and long-prismatic colourless inclusions (ISAC 34). Scale bar is 500μm. Gilg et al. (2024). 

The New Kingdom beads showed much improved shaping. The majority of these beads were globular in shape, but also present were unusually long barrel to tubular shapes with a length of up to 7.9 mm and a diameter of 4 mm. These beads all have a low polish, and again are drilled from both ends. The Napatan and Meroitic beads were similar in form to the Pan Grave and C-Group beads.

None of these beads had a high polish, something seen in Egyptian beads from the Great Aten temple at Amarna (18th Dynasty), which were made by polishing with corundum powder as an abrasive, a technique apparently unknown in Upper Nubia. How the Upper Nubian beads were polished is unclear at this time.

The youngest, Post-Merotic bead differs from all others in the study, having a faceted shape (a hexagonal truncated bicone), a well-polished surface, and deep, regularly spaced, concentric grooves in the drill hole, probably indicative of the use of a diamond drill bit. Similar garnet beads are known from Arikamedu in southern India, and sites in southern Sri Lanka. Microscopic examination of this bead revealed the presence of many tiny, short- and long-prismatic, colourless inclusions, something seen in Sri Lankan garnets but not garnets from southern India. Though this is not sufficient evidence to confirm the origin of this bead, Gilg et al. consider it highly likely that this bead comes from South Asia, and probably Sri Lanka.

Chemically, all of the garnets, including the alluvial samples from Upper Nubia were found to be of similar composition, with the exception of the single Post-Merotic bead. These beads have an almandine-rich composition, with a low calcium content (the Post-Merotic bead has a pyrope-rich composition with a low calcium content). Compositionally, these beads do not fit into any of the types used to classify Hellenistic to Early Medieval garnets, with magnesium oxide-calcium oxide ratios intermediate between type A and type B contents, combined with a high manganese and yttrium, low chromium composition not seen in either of these types. This suggests that the beads were made from alluvial garnets sourced from deposits in Upper Nubia, and that garnets from this source were not used in the Hellenistic to Early Medieval periods.

Almandine-rich garnet was the first mineral harder than quartz to be worked in northeast Africa, apparently being sourced at a site in the Bayunda Desert of Upper Nubia at least 670 km south of the most southerly known occurrence of worked garnet beads in Lower Nubia. These Upper Nubian deposits appear to have been the only source of garnets used in manufacturing for at least 3500 years. 

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Letti Desert 1: A new archaeological site associated with the ancient African Kingdom of Kerma.

The ancient Kingdom of Kerma is one of the oldest known states in Africa, emerging in the third millennium BC from the urbanisation of pastoral communities in the Selim Basin of the Third Cataract of the Nile, and persisting until 1504 BC, when it was conquered by the Egyptian Pharaoh Thutmose I. The Kermans built distinctive urban centres with monumental buildings and necropolises, although these have only been extensively studied around- the Third Cateract, with some funerary cites around the Fourth Cataract also known.

In a paper published in the journal Antiquity on 1 December 2023, Piotr Osypiński of the Institute of Archaeology and Ethnology of the Polish Academy of Sciences, Marta Osypińska of the Institute of Archaeology at the University of Wrocław, Justyna Kokolus, an independent researcher from Stara Dąbrowa in Poland, Paweł Wiktorowicz, also of the Institute of Archaeology and Ethnology of the Polish Academy of Sciences, Roman Łopaciuk of the Institute of Mediterranean and Oriental Cultures of the Polish Academy of Sciences, and Amel Hassan Gismallah of the National Corporation of Antiquities and Museums in Khartoum, describe a new archaeological site associated with the Kingdom of Kerma, from the Letti Basin of the Middle Nile Valley in Northern Sudan.

Osypiński et al. identified a number of new sites on the edge of the desert in the Letti Basin, sites which would have been located in close proximity to the seasonally overflowing Nile at the time when Kerma existed. Some of these sites appear to have been extensive settlements, from which were recovered characteristic Kerman ceramic objects, Animal bones, and stone tools, as well as carrying out excavations at one site, named Letti Desert 1.

Middle part of the Nile Valley and location of site Letti Desert 1. Osypiński et al. (2023).

Radiocarbon dates recovered from organic material at Letti Desert 1 suggest that the site was occupied for about 700 years, with the oldest dates being between 2205 and 2020 BC while the youngest come from between 1618 and 1497 BC, around the time of the Egyptian conquest. 

A mud brick building with a surviving thickness of about one metre was established to have been constructed around the beginning of the second millennium BC. Neighbouring structures contained large storage vessels, and had foundations made from boulders up to 3 m in diameter. A granary area with a pavement of square stones was surrounded by post holes. Another area was interpreted to be a metal workshop, with fragments of a large melting pot, and several bronze smelts recovered. 

Architectural elements recorded in the eastern part of the Letti Desert 1 settlement, marked in red. The size of opened excavation is 5 × 5 m. Osypiński et al. (2023).

Analysis of zooarchaeological remains from the site suggests that Cattle became progressively less important over time, with Sheep replacing them as the major form of livestock. This was probably associated with the drying of the local climate and spread of desert. Cattle are known to have remained culturally important, with the rulers of Kerma being buried with Cattle bucrania (the frontal part of the skull, with the horns) in the latest stages of the civilization. However, isotopic studies of these remains suggest that these Cattle came from outside the Nile Valley, possibly from North Kordofan to the south, from where Cattle could be driven to the Letti Basin via the dry channels of Wadi el Melik and Wadi Howar.

Stone pavements in the western part of the Letti Desert 1 settlement, view from the north Osypiński et al. (2023).

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Archaeologists discover body with Christian tattoo in medieval Nubian cemetery.

Archaeologists from the Polish Centre of Mediterranean Archaeology have discovered Christian tattoo on a body recovered from a medieval Nubian cemetery during one of a series of expeditions to the area between 2012 and 2018, according to a press release issued on 18 October 2023. The Christian theme of the is not in itself surprising, as Christianity was the predominant religion in region at the time and the body was found in a cemetery associated with the Ghazali Monastery, which is about 20 km from the modern town of Karima in Northern State, Sudan. However, this is only the second tattoo known from medieval Nubia, making it a significant discovery. The body is of unknown sex at the current time, although thought likely to have been male, due to its proximity to the monastery, and is thought to have been between 35 and 50 years old when they died, sometime between 667 and 774 AD. 

Images of tattoo on the dorsal (top) side of the right foot. Picture was taken with a full spectrum camera and digital enhanced using ImageJ software with a DStretch plugin. Kari Guilbault/Polish Centre of Mediterranean Archaeology.

The tattoo comprises a Christogram, which was a symbol combining the Greek letters 'chi' and 'rho' used to indicate Christ, plus the Greek letters alpha and omega, the first and last letters of the Greek alphabet, a combination often used to imply God as the beginning and ending of all things. The location of the tattoo, on the upper part of the foot, may also be significant, as it images of Christ often have a nail driven through this location.

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Using strontium isotope ratios to determine the origin of textiles from archaeological sites in Nubia.

The manufacture of textiles by pre-industrial societies was typically a demanding, multi-stage process, which involved obtaining fibres from an Animal or Plant, spinning it into a thread, and weaving it into a cloth, with dyes potentially being added at different stages to achieve colours or patterns. As such, textiles from archaeological sites can be important sources of information about the societies that produced them, giving evidence about trade routes and manufacturing techniques, as well as the social status, gender and age of the wearer. 

Textiles from archaeological sites in Sudan have been studied since the early twentieth century, with material recovered from many sites in the mid Nile Valley. Wool and cotton are the most common fibres in these archaeological assemblages. Linen is also present, but in much lower quantities. Silk has never been produced in Sudan, so any silk discovered there can automatically be assumed to have been imported. Spinning of threads in Sudan was almost exclusively done in the S-direction (anticlockwise), while woven cloths were usually plain tabbies (a plain weave, with warp and weft threads crossing at right angles to form a criss-cross pattern) or weft-facing tabbies (cloths in which the warp is covered up by multiple, complimentary weft layers, enabling the building up of a pattern, which is typically angular in nature), often having bands or stripes in different shades.

However, determining the origin of fabrics from archaeological sites is complex, as plain and weft-facing tabbies are widely manufactured, and the textiles recovered from archaeological sites are typically very fragmentary. Even spinning direction is of limited use, as even in areas where the majority of spinning is done in one direction, the presence of local communities or even individual spinners doing the opposite cannot be excluded.

In a paper published in the Journal of African Archaeology on 11 August 2022, Magdalena Wozniak of the Department of African Studies at the University of Warsaw, and Zdzislaw Belka of the Isotope Research Unit at Adam Mickiewicz University, present the results of a study which used strontium isotope ratios to determine the origin of cotton and wool fragments from Late Antiquity and the Early Medieval Period recovered from archaeological sites in the Middle Nile Valley.

Strontium isotope ratios in water are strongly linked to local geology, and can be preserved in the tissues of Animals and Plants, making them a powerful tool in archaeology. Strontium isotopes have been used to track the movements of ancient Human and Animal groups, as well as tracing ancient trade routes by determining the origin of stone tools, glass, and textiles. This technique requires an understanding of the ratio of the isotopes strontium⁸⁷ and strontium⁸⁶ in the geology of the area, both locally and regionally. Armed with this it is possible to determine whether or not a material (in this case fabric) was manufactured locally, and in some cases where a non-local item originated from. Both Animals and Plants (the producers of wool and cotton) take up strontium from the environment in the ratios at which they are present, without any fractionation, with the strontium isotope ratios found in their tissues reflecting a mixture of that found in the bedrock and overlying soil as well as that from ground and surface water. However, the different ecologies of Animals and Plants mean that even when they live in the same area, they will have slightly different isotopic ratios.

Although obtaining an accurate strontium isotope ratio only requires about 100-150 mg of material, the desiccated and friable nature of most archaeological fabrics means that the process typically leads to the destruction of one or two square centimetres of fabric, so the choice of materials sacrificed must be made very carefully.

Wozniak and Belka used four textile samples from recent excavations near the fourth cataract, made available for the study by the Polish Academy of Sciences, as well as three samples provided by the Sudan National Museum and the National Corporation for Antiquities and Museums in Khartoum. All bar one of these was from a burial site, and all are of either wool or cotton. The sample was chosen to include samples which were presumed to be of both local manufacture and imported. None of the samples showed signs of decomposition or degradation, making it unlikely that they had had their isotope signatures overwritten by strontium from groundwater after being buried, something which can be a severe problem in wetter climates, but is less so in arid Nubia.

The first sample chosen, NT1, was a section of decorated warp-faced woollen fabric (woollen fabric in which the threads are packed together closely, hiding the weft) with roughly 14-16 warp threads and 8 weft threads per cm². This fragment was recovered from the bottom of a funerary chamber beneath Tumulus 24 in the El-Ar 1 cemetery, near the El-Ar village in Shamkhiya District. The El-Ar 1 cemetery has been dated to the 2-3rd centuries AD, with decorated fabrics being very rare there.

Fragment of warp-faced wool tabby, sample NT1. Magdalena Wozniak in Wozniak & Belka (2022).

The second fragment used, NT2, is a piece of dark brown plain tabby woollen fabric, woven from S-spun threads, recovered from the El-Ar 4 Christian cemetery, and which could indicate a date anywhere between the sixth and fifteenth centuries AD. The fragment has 8-9 warp and 7 weft threads per cm², and comes from a section of shroud, which is in turn likely to have been a cloak or blanket used by the buried person and re-used as a shroud upon their death.

Fragment of the wool shroud, sample NT2. Magdalena Wozniak in Wozniak & Belka (2022).

Sample NT6 is a course wool plain tabby, woven with 8 warp and 8 weft threads per cm², taken from the shroud of a naturally mummified body (i.e. preserved by burial in a dry environment, rather than Human intervention). The fragment is brown in colour, and very desiccated. The mummy was buried in a supine position, with hands resting on hips, which is indicative of a Christian burial, again implying the 6th-15th centuries AD.

Close-up of mummy’s shroud, sample NT6. Magdalena Wozniak in Wozniak & Belka (2022).

Sample NT7 is a section of woollen kilim (woven tapestry rug). This has a dense weave with 7 warp threads and 32 weft threads per cm², and is woven in the slit-tapestry style, which creates the same pattern on both sides. The warp is a 2-ply z-spun (clockwise) cream wool, while the weft is single-ply z-spun wool in a variety of colours, including red, green, blue, orange, yellow and pink, giving a pattern of geometric and floral designs against a red background. The kilim was discovered in the town of Meinarti near the 2nd cataract in 1963, and has been dated to the 14th century AD.

Fragment of wool kilim from Meinarti, sample NT7, before conservation. Magdalena Wozniak in Wozniak & Belka (2022).

Sample NT3 is a piece of weft-faced tabby cotton cloth from the El-Ar 4 Christian cemetery. The threads are S-spun and of a golden colour, with the weft threads thicker than the warp threads, and a thread-density of 11 warp threads and 19 weft threads per cm². This is a common, medium-quality cloth type at archaeological sites on the Middle Nile.

Fragment of cotton tabby, sample NT3. Magdalena Wozniak in Wozniak & Belka (2022).

Sample NT4 is a fragment of cotton plain tabby from a Late Antique (2nd to 5th century AD) burial site at El-Ar. It is comprised of Z-spun white threads with traces of blue, green, and red pigments, probably a sign of resist dying (dying a finished fabric, while using wax or a similar substance to control which parts of the fabric the dye reaches), and a thread density of 22-24 threads per cm² for both warp and weft.

Bi-coloured threads from the cotton tabby, sample NT4. Magdalena Wozniak in Wozniak & Belka (2022).

Sample NT5 comes from the shroud of a naturally mummified body of unknown providence in the collection of the National Corporation for Antiquities and Museums. The textile is desiccated, low density, cotton tabby with a thread count of 8 warps and 8-9 wefts per cm². The threads are Z-spun, and have a golden colour. This mummy was also preserved in a supine position, with hands on hips, indicating a Christian burial, between the 6th and 15th centuries AD.

Fragment of cotton tabby woven from Z-spun threads, sample NT5. Magdalena Wozniak in Wozniak & Belka (2022).

Precambrian rocks of the Arabian-Nubian shield are widely exposed between the 2nd and 5th cataracts of the Nile. These exposures show a large variety of magmatic and metamorphic rocks, separated by suture zones with small occurrences of ophiolites and deep-water sedimentary rocks. To the west of the Nile Valley these are bordered by younger sedimentary rocks, predominantly Silurian sandstones. These rocks are overlain unconformably by the rocks of the Nubian Sandstone, which spreads across much of northern Africa, and includes a range of continental, esturine and marine sediments (predominantly sandstones), which in Sudan are predominantly of Cretaceous age. These Nubian Sandstone deposits have been mostly eroded away in the northeast of the country, exposing the underlying Precambrian basement, but extensive exposures are still present in the Bayuda Desert in the south, and the area to the west of the Nile. Tertiary Basalt rocks, which have intruded into these overlying strata, are exposed in the south of the country, around Abu Hamad. The floodplains of Nile Valley is also home to an extensive succession of Tertiary Sediments. 

Simplified geological map of northern Sudan. Red asterisks  indicate places where the investigated wool and cotton textiles were found. Numbers refer to the samples numbers. Inset shows the location of the study area. Wozniak & Belka (2022).

The volcanic rocks of the Precambrian basement of northern Sudan have strontium⁸⁷/strontium⁸⁶ ratios in the range 0.7024 to 0.7071, while the plutonic and metamorphic rocks of the basement have ratios in the range 0.7158 to 1.0039. The Cretaceous sediments of the Nubian Sandstone have strontium isotope ratios reflective of those of the basement rocks, with two clusters of values, around 0.7070 and 0.7160.

The alluvial sediments of the Desert Nile Valley are dominated by material derived from the Blue Nile and Atbara rivers, which drain from the Ethiopian Highlands, an area dominated by Cainozoic Volcanic rocks. These sediments have isotopic ratios in the range 0.7047 to 0.7076, a range which includes that of modern Nile water, at 0.7062. Nile muds dating from the end of the African Humid Period, about 45 000 years ago, show a strontium isotope ratio of 0.7052–0.7057, while those dating from between 1000 BC and 500 AD (i.e. between 3000 and 1500 years ago) show an isotope range of 0.7058–0.7076.

Samples NT1, NT2, and NT6 are all low-density woollen tabbies made from S-spun threads, technologically consistent with local manufacture. Sample NT1 contains cream and dark wool, used to make a pattern, while NT1 and NT6 are made entirely of undyed, dark wool. Lighter, cream-coloured wools are rare in the El-Ar assemblage, which may reflect the genetic structure of the local flocks (i.e. many brown Sheep and few cream Sheep). Alternatively, the local Sheep of the period may have been entirely brown, with cream wool being an imported commodity.

Sample NT7 is quite different from these, made up of coloured, Z-spun threads woven together using the split-tapestry technique to produce a decorative pattern, which is likely to indicate that this was an imported item. Furthermore, furthermore, the red dye used on some of the wool appears to have been treated with a lac dye, derived from the Scale Insect, Laccifer lacca, which is found in South and Southeast Asia and South China, but quite alien to the Nubia, where red dyes were traditionally derived from the Madder Plant. This apparently non-local item dates from the 14th century, a time when Meinarti was occupied by the Beni Ikrima, a nomadic group from the Maghreb region.

All four wool samples yielded strontium isotopic ratios within the range 0.7075 to 0.7084. In order to better compare these to the local environment, Wozniak and Belka also obtained strontium isotope ratios from Sheep and/or Goat remains (the two are hard to tell apart) from several archaeological sites between the 2nd and 4th cataracts. All of these remains are known to be older than the wool samples, dating to between 2500 and 500 BC, and gave isotopic ratios in the range 0.7068 to 0.7082 (one set of remains gave a much higher reading, of 0.7109, though this is likely to indicate that the Animal was of non-local origin).

Diagram showing the strontium isotope signatures of the  investigated wool textiles (yellow spots; numbers refer to sample numbers) in comparison to Strontium isotope  composition of Ovis/Capra remains found in the region  between the 2nd and 4th cataracts. Wozniak & Belka (2022).

Three of the investigated wool samples, NT1, NT6, and NT7, had isotopic ratios entirely consistent with archaeologically derived Sheep/Goat remains from the region, and the fourth, NT2, fell only slightly outside this range, and still within the range of Cattle and Human remains from the Desert Nile Valley.

Of the three cotton samples, only one, NT3, was made of a yarn spun in an anticlockwise, S-direction, typical of local manufacture in Nubia or Egypt. The other two, NT4 and NT5, were spun in a clockwise, Z-direction, which may indicate non-local manufacture. One of these, NT4, also shows signs of a resist-dying technique, not known in Nubia in the 2nd-5th centuries AD, but common in textiles from India during this period.

These three samples show a narrow isotope ratio range, from 0.7084 to 0.7086, which makes it likely that they were derived from crops grown within a limited geographical area. As a crop, cotton requires a rather specific set of conditions, with a hot dry climate, and large amounts of available water for several months of the year. This can be provided in the Nile Valley between the confluence of the White and Blue Niles and the 2nd cataract, although water and plants derived from this region show isotope ratios below 0.7075, ruling this region out as an origin point for the cotton in the study. Cotton is also grown around the Nile Delta, and ancient cotton fibres and seeds have been recovered from other sites along the Lower Nile, suggesting that cotton may have once been grown more widely. Strontium isotopic signatures are not available for sediments from all of these areas, but the isotopic signature of the Nile water, at about 0.7069, makes it unlikely that any of these floodplains have an isotopic ratio above about 0.7075. Similarly, the sediments of the Atabara and Blue Nile valleys have average isotope ratios between 0.7041 and 0.7060. All of these locations therefore seem unlikely as a point of origin for the cotton used to make the textiles included in the study. 

However, cotton grown in the Western Desert of lower Nubia typically has an isotopic value of about 0.7085, and limestones from the Western Desert of Egypt can have strontium isotope signatures in the range 0.7077 to 0.7078. Cotton is known to have been grown in this region in the 2nd-3rd centuries AD, using irrigation systems which drew upon shallow groundwater reservoirs, supplied by rainwater that had filtered through Eocene carbonates, which could conceivably produce a cotton with a strontium isotopic signature of about 0.7085.

Cotton is also known to have been produced in Meroe, on the lower White Nile to the south of Khartoum, during the Roman period, although both the water and plants from this region tend to have a higher isotopic ratio than the cotton from the study, excluding this region as a point of origin. 

Diagram showing the strontium isotope composition of the investigated cotton textiles (green spots; numbers refer to samples) in comparison to Sr isotope composition of selected elements of the natural environment in the Nile and White valleys. Wozniak & Belka (2022).

There is strong evidence for the production of cotton in Egypt and Sudan in Roman and later times, but the possibility of material also being imported from further afield should not be ruled out. Cotton was widely cultivated in India and on the Arabian Peninsula during antiquity, and both raw cotton and finished textiles could easily have been imported to Nubia via the Red Sea. Cotton seeds and textiles excavated at Mleiha in the modern United Arab Emirates have been shown to have originated from western India by their strontium isotope ratios. Unfortunately, strontium isotope information is only available for a few locations on the Arabian Peninsula or from India or Pakistan. However, several regions would be compatible with the isotope signatures obtained from the cotton samples, including the lower Indus River Basin, in India and Pakistan, the Kathijawar Peninsula on the west coast of India, the area covered by modern Kuwait, and the Oman Peninsula.

The isotope signatures obtained from the wool samples from archaeological sites in the Nubian Nile Valley all support a local origin. This is also supported by the technological features of three of the samples, NT1, NT2, and NT6, but not the fourth, NT7. This sample, a kilim rug from 14th century Meinarti, appears to have been made with a technology entirely alien to this part of the Nile Valley. However, it also dates from a time when the city of Meinarti was occupied by an alien group, the Beni Ikrima, who originated from the Maghreb region. Since the Maghreb has a geology with similar strontium isotopic ratios to that of northern Sudan, it is possible that the kilim was brought to the area by the Beni Ikrima from their homeland. However, it is also possible that the kilim was made locally by Beni Ikrima craftspeople from wool obtained from local, Nubian, flocks. Wozniak and Belka conclude that, given the available isotopic evidence, the more likely scenario is that the kilim was made locally, contrary to previous expectations.

In contrast, the isotopic signature of the cotton samples examined fits poorly with an origin in the Nile Valley. The samples all have very similar isotopic signatures, which seems to imply a common origin, although this is at odds with the different spinning techniques used. One of the samples, NT3, has an isotopic signature that fits well with the Dakhla/Kharga oasis in the Egyptian Western Desert, which has previously been identified as a possible site of ancient cotton cultivation. This piece also shows a technology consistent with production in the Nile Valley, notably an S-spun yarn. Importing cotton textiles from an oasis in the Western Desert would only make sense if local, Nubian, production was failing to meet demand. The frequency of cotton fabrics from archaeological sites in Nubia has been observed to have dropped during the Late Antique and Early Medieval periods, so this is not implausible, although an alternative explanation could be that the deceased person for whom this item was used as a shroud had travelled during their lifetime, either moving from the Western Desert to Nubia and bringing the cloth with them, or at some point visiting the Western Desert and obtaining the item there.

Sample NT4, on the other hand, appears much more likely to be of Indian origin, where a block printing technique using resist dying was common at this time. The isotopic signature of this sample matches that of the Kathijawar Peninsula on the west coast of India, leading Wozniak and Belka to conclude that this item was most likely imported from India. This adds evidence to the inclusion of the area around the 4th cataract into long distance trade networks, something previously indicated by the discovery of glass beads of foreign manufacture in the region.

Sample NT5 also appears to be non-local in origin, with a Z-spinning technique having been used, and a non-local isotopic signature. However, there is insufficient evidence to give a precise origin for this fragment at this time, with possible points of origin including  Indus River basin in Pakistan, the west coast of India, Kuwait, and the Oman Peninsula.

Although Wozniak and Belka were not able to determine the point of origin of all the fabrics in the study, their study shows the potential for determining the origin of ancient fabrics using strontium isotope ratios. The development of a wider data set of strontium isotope values for textiles could add to the information obtained by examining the technological aspects of textile-making, to provide a better understanding of the manufacture of and trade in cloth in the ancient world.

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