Showing posts with label Horn of Africa. Show all posts
Showing posts with label Horn of Africa. Show all posts

Saturday, 4 January 2025

Magnitude 5.8 Earthquake in the Afar Region of Ethiopia linked to activity on Mount Dafan.

The Ethiopian Geological Institute has reported a Magnitude 5.8 Earthquake at a depth of 10.0 km, in the Awash Fentale Woreda (District) of the Afar Region of Ethiopia, about 150 km to the northeast of Addis Ababa, slightly after 4.50 am local time (slightly after 0.50 am GMT) on Saturday 4 January 2025. There are no reports of any damage or injuries arising from this quake, but it was felt as far away as Addis Ababa, and it is possible that some minor damage has occurred.

The approximate location of the 4 January 2024 Ethiopian Earthquake. USGS.

This is the latest in a series of Earthquakes in the Central Ethiopia, which began in the third week of December 2024. Clusters of Earthquakes are concerning in northern or central Ethiopia, as the area is volcanic, and seismic movements can be linked to magma moving into chambers beneath volcanoes from deeper in the Earth, which in turn can be a predictor of future volcanic eruptions. On this occasion the Ethiopian Geological Institute has suggested that the Earthquakes may be linked to a fissure eruption on Mount Dafan, a shield volcanoe in the Dulacha Woreda, which opened on 2 January producing a sustained jet of steam and hot water. Residents of the area have been evacuated as a precaution against a future, larger eruption.

A vent which opened on Mount Dafan in the Dulacha Woreda of Ethiopia on 3 January 2024, producing a sustained jet of steam and hot water. Ethiopian Geological Institute/Facebook.

The deserts of Northern Ethiopia and Southern Eritrea are extremely volcanically active, with dozens of volcanoes fed by an emerging divergent margin along the East African Rift. The African Plate is slowly splitting apart along the Ethiopian Rift and the East African Rift to the south (which is splitting the Nubian Plate to the West from the Somali Plate to the East). Arabia was a part of Africa till about thirty million years ago, when it was split away by the opening of the Red Sea Rift (part of the same rift system), and in time the Ethiopian and East African Rifts are likely to split Africa into a number of new landmasses. This rifting exerts pressure on the rocks around the margin of the sea, slowly pushing them apart, not smoothly but in fits and starts as the pressure overcomes the tendency of the rocks to stick together, creating shocks that we experience as Earthquakes.

Rifting in East Africa. The Danakil Microplate is the red triangle to the east of the Afar depression at the southern end of the Red Sea. Università degli Studi di Firenze.

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Thursday, 7 November 2024

Malaria in Ethiopia.

Between 1 January and 20 October 2024 more than 7.4 million cases of Malaria were reported in Ethiopia, with 1157 deaths recorded, a case fatality rate of 0.02%, according to a press release issued by the World Health Organization on 31 October 2024. On these infections, 95% were causes by Plasmodium falciparum. This is the highest number of cases reported in Ethiopia in seven years, and part of an ongoing rising trend of Plasmodium falciparum infections; in 2023, 4.21 million Malaria infections, with 527 deaths, with 70% caused by Plasmodium falciparum.

The overwhelming majority of cases occurred in the west of the country, with four regions accounting for 81% of all recorded infections and 89% of known deaths, with 44% of cases and 667 deaths in Oromo, 18% of cases and 56 deaths in Amhara, 12% of cases and 250 deaths in Southwest Ethiopia, and 7% of cases and 45 deaths in South Ethiopia. 

Geographical distribution of Malaria cases as of 20 October 2024. World Health Organization.

Of Ethiopia's 523 worodas (districts), 222 have been identified as having a high Malaria burden, together accounting for 75% of recorded Malaria cases in 2023. Fifty of these high-burden worodas are considered to be hard-to-access due to ongoing conflicts.

A slight majority of cases are males, who accounted for 56% of cases treated as outpatients and 52% of inpatient admissions. Children accounted for 16% of outpatients and 25% of inpatient admissions. This age and sex distribution is thought to be due to patterns of seasonal migration, with large numbers of adult male migrant workers seeking work in high-risk areas during the peak of the Malaria season. 

From 2000-onwards, Ethiopia had a steady reduction in the number of Malaria cases each year, driven by improved surveillance, roll-out of malaria interventions, and community health extension program. The number of cases fell to an all-time low in 2019, when only 900 000 cases were recorded, and there was no wide-ranging major epidemic, only sporadic local outbreaks. However, the country began to suffer a resurgence of the disease from 2021 onwards, with 1.3 million cases in 2021, 3.3 million cases in 2022, and 4.1 million cases in 2023. This return appears to have been driven by the Plasmodium falciparum strain of the disease, which caused 70% of the infections in 2023, and which appears to have become endemic in areas where it was not previously known.

Weekly trend of malaria cases in Ethiopia, 01 January 2021 to 13 October 2024. World Health Organization.

Malaria is caused by parasitic unicellular Eukaryotes of the genus Plasmodium, and affects a wide range of terrestrial Vertebrates. Five different species of Plasmodium can cause Malaria in Humans, with most infections caused by either Plasmodium falciparum or Plasmodium vivax, both of which are endemic to Ethiopia. The parasites are primarily spread via the bite of the female Anopheles Mosquitoes (males do not bite), but can also be spread through blood transfusions, organ transplants, or practices such as needle-sharing.

Photomicrograph of a blood smear containing a macro- and microgametocyte of the Plasmodium falciparum parasite. Both macro- and microgametocytes are products of the erythrocytic life cycle. Within a few minutes after the Anopheles sp. vector ingests the gametocytes, microgametocytes develop into microgametes, which are able to fertilize gametes. Centers for Disease Control and Prevention/Wikipedia Commons.

Malaria manifests with approximately 10-15 days after infection, as a fever, headache, and chills. Mild cases often pass soon, and can be difficult to identify as Malaria, however, more severe cases can be fatal in as little as 24 hours after the onset of symptoms. 

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Sunday, 27 October 2024

What abandoned grinding stones can tell us about the medieval town of Handoga in Djibouti.

The abandoned town of Handoga in southern Djibouti covers an area of about 600 m north-to-south and 300 m east-to-west, and is located about 13 km from the border with Ethiopia. Archaeological investigations have suggested that the site was initially used in the twelfth century as an occasional campsite by nomadic herders passing through the region, becoming a permanent settlement in the thirteenth century, from when it evolved into a town, with buildings with stone-built lower portions and wattle-and-daub upper portions coming to replace earlier temporary structures. The town was abruptly abandoned in the sixteenth century, with no sign of any violent upheaval preceding this event. As well as dwellings, the town had a range of open spaces which may have been squares, junctions of streets, or other public spaces, as well as two mosques, both at the northern end of the settlement, and a cemetery, at its southern end.

In a paper published in the journal World Archaeology on 30 September 2024, Jorge de Torres Rodríguez of the Instituto de Ciencias del Patrimonio in Santiago de Compostela, Spain;, and Valeria Franco Salvi of the Instituto de Humanidades at the Universidad Nacional de Córdoba in Argentina present the results of an analysis of grinding stones recovered from C-6000, the first structure at the northern end of Handoga to be the subject of archaeological investigations.

Location of Handoga in the Horn of Africa. De Torres Rodríguez & Salvi (2024).

The C-6000 site comprises two circular stone structures, linked by a series of walls enclosing a central open area, interpreted as having been used for food preparation and other domestic activities. The remains unearthed within this area resemble those found within courtyards excavated towards the southern end of the settlement, with two notable exceptions. Firstly, the site has yielded a quantity of well-preserved charred fruits, seeds, and wood fragments, which are currently under study, and which it is hoped will yield radiocarbon dates which will enable a chronology of the site to be built up. Secondly, excavations at the site have produced 88 fragments of grinding stone stones of different types, the largest collection of such stones not just from Handoga, but from any medieval Islamic site excavated to date, providing a rare opportunity to analyse how these objects were made and used, and any changes in their use over time.

Compound C-600 with main rooms and areas. De Torres Rodríguez & Salvi (2024).

Grinding stones were found across the site, with roughly two thirds coming from collapse layers, while about one third were found on original occupation layers. Grinding stones were found in all areas, with 47% coming from Room A, identified as the principal occupation site, 11% from Room B, identified as a storage area, and 34% from the central area. The stones can be split into two types, passive grinding stones, upon which grains would have been ground, and handstones, which would have been used to grind grains upon the grinding stones. Of the two, passive grinding stones are more common (55, compared to 33 handstones).

Handstones (upper rows) and one of the passive grinding stones (bottom) found at C-6000. De Torres Rodríguez & Salvi (2024).

Many of the passive grinding stones were highly fragmented, with 17 deemed intact enough for study. All were made from a vesicular-textured basalt, which probably came from an outcrop about 500 m from the settlement. Such a rock would have been ideal for grinding dehydrated or floury products, as it would be relatively easy to clean, and would have maintained a rough surface through use. These grinding stones appear to have been made from nodules or similar, with most made from approximately spherical or approximately cylindrical pieces of rock, with minimal shaping to achieve the desired shape. Despite the fragmentary nature of the grinding stones. about 60% still weighed between 2 kg and 5 kg, with the remaining 40% weighing under 2 kg. Twelve of the grinding stones are thought to have been portable, while the remaining five would have been large objects, presumably immobile during their working lives. The average grinding surface of these stones is 373 cm², with the largest having a surface area of 495 cm².

(1) Outcrop where the material for grinding stones was likely collected. (2) Compound C-6000. De Torres Rodríguez & Salvi (2024).

A much lower number of handstones (32) were recovered, these being largely fragmented, and scattered about with no sign of having been stored. They were apparently left where they lay between uses, and then abandoned once they became to worn for use.  Few showed any signs of maintenance during use, and none of any attempts to prolong their lives. Many of the handstones had been worn-down to the point of uselessness. The often had two wear-facets, showing their users had attempted to gain the maximum utility from them. All the handstones weighed less than 1 kg, with about 40% weighing less than 500 g. The handstones were made from rock which could be collected from within less than a kilometre, with the majority being made from basalt, although granite examples were also present, and one was made from quartzite.

While there appears to have been some variation in the way in which grinding stones were made and used at Handoga, the defining feature that appears to link all of them is an apparent lack of care. Only a minimal amount of work appears to have been put into modifying stones from their natural state to make them into tools, and little investment in their upkeep has been made during their lifetimes. There was no apparent standardized way to make these tools, which suggests that they were not manufactured by specialist craftspeople.

One consistent pattern which can be seen throughout the sample is the division into handstones and passive grinding stones, with grinding stones being larger and made from a single material, vesicular basalt, while handstones are smaller and made from denser and smoother material, with more variation in the selection of that material. A similar pattern has been seen at sites in Cameroon and Mali. There was also a difference in the distribution of these two elements, although the significance of this is unclear.

Large passive grinding stone found during a survey in Handoga. De Torres Rodríguez & Salvi (2024).

De Torres Rodríguez and Salvi suggest that this apparent lack of importance placed upon the manufacture and conservation of grinding stones suggests that these objects were not particularly valued by the people of Handoga. They further suggest that this lack of importance has implications for how we understand the settlement itself. Handoga was initially interpreted as an agricultural settlement, likely deriving water from the nearby Wadi Chekheiti, and trading Sorghum and Millet with the surrounding nomadic groups. However, no archaeobotanical studies have been carried out at Handoga, so there has been no evidence to date to either support or counter this hypothesis. 

In agricultural societies, grinding stones are typically high value items, of considerable economic significance, whereas at Handoga they appear to have been poorly valued, and used within domestic settings. This leads de Torres Rodríguez and Salvi to conclude that while agriculture was probably caried out at Handoga, it was likely a low-status activity, not having the same prestige as traditional nomadic activities such as herding and trade.

This in turn has implications for the history of Handoga. The settlement appears to have been initially used on a temporary camp by nomads in the twelfth century, gradually becoming more permanent, and transitioning to a town with stone buildings sometime in the fourteenth century. De Torres Rodríguez and Salvi reason that the low importance given to the processing of agricultural products suggests that despite becoming a permanent settlement, Handoga never really lost it's nomadic emphasis, something which is also reflected in the design of its buildings.

This in turn helps to explain why Handoga was abandoned so easily in the mid-sixteenth century. During the sixteenth century the Sultanate of Barr Saʿd al-Dīn, which ruled over much of the Red Sea coast of the Horn of Africa, collapsed following a series of disastrous wars with Abyssinia, severely disrupting trade routes, and causing many settlements to be abandoned. For peoples who had become truly sedentary in nature, this would have been a difficult process, either abandoning practices such as agriculture and having to relearn nomadic ways or relocate to other settlements, possibly some distance away. However, if the inhabitants of Handoga had retained an essentially nomadic nature with their main income deriving from pastoralism, the abandonment of the town may have been a less painful process than for more settled communities.

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Monday, 4 December 2023

Evidence for Late Pleistocene net-hunting in southern Somalia.

Humans have been farming for about 12 000 years, a period which was preceded by hundreds of thousands of years of living a hunter/gatherer existence. It is logical to assume, therefore, that the social networking skills which made modern civilization possible developed largely before the event of farming. The advent of specialist hunting techniques such as net-hunting, which require advanced planning and co-operation between groups of hunters, and which can produce large amounts of meat in single events, are thought to have been a significant step in the development of Human social networks, connected to the emergence of social hierarchies and concepts of land ownership.

The lifestyle of Homo sapiens in East Africa from our emergence as a species onwards has been heavily investigated for decades, although curiously, despite the importance placed on the role of hunting as a driver of Human evolution by many early archaeologists, the techniques used to hunt have been relatively neglected, with an assumption that big game hunting was the dominant behaviour. Recent studies, however, have suggested that while big game hunting was important on the grassy plains of East Africa, in the coastal forests of the region, remote capture devices, such as snares, traps, or nets, used to target small Animals have been important for at least 125 000 years.

Given that such methods are thought to be closely associated with the emergence of social networks, the nature these hunting practices, and the ways in which they evolved over time, must be seen as an important part of the Human story. Examination of Later Stone Age sites in the semi-arid environment of southern Somalia, have shown that nets were being used to intensively hunt Dwarf Antelopes between about 26 000 and about 6000 years ago.

In a paper published in the journal Archaeological and Anthropological Sciences on 2 December 2023, Mica Jones of the School of Archaeology at the University of Oxford, presents the results of a study of Animal bones from the Late Pleistocene Guli Waabayo rock shelter in the Buur Heybe inselberg cluster, and the implications of this for the use of net-hunting by the Later Stone Age hunter/gatherers of the area.

Inselbergs are hills made from hard volcanic rock, which persists when other deposits are eroded away, typically forming elongate structures. In Somalia such structures are known as 'buurs', and in the inter-riverine region of southern Somalia, where rainfall is typically between 400 mm and 600 mm per year, clusters of these buurs can help to trap nutrient-rich soils and collect rainwater in pools and ponds, providing favourable habitats for a range of Plants and small Animals.

A previous study of the Rife Range Site at Buur Hakaba found that Later Stone Age hunters there specialised in hunting Dwarf Antelope, probably with nets, leading to the development of a more sedentary lifestyle and the holding of territories in the Early-to-Middle Holocene, a period of increased rainfall. However, the small number of remains recovered from this site, combined with an absence of dates, limits the usefulness of this study. The Guli Waabayo rock shelter at Buur Heybe, about 25 km to the northeast of Buur Hakaba, has yielded a much more extensive collection of Animal remains, combined with a series of robust dates, covering a period of 20 000 years, potentially enabling a good test site for hunting practices in the region before the start of the Holocene.

Map of inter-riverine southern Somalia with locations of the Buur Heybe and Buur Hakaba inselberg clusters. Jones (2023).

More than a hundred rock shelters and other archaeological sites have been identified in the inter-riverine region of southern Somalia since the 1930s. However, only three of these sites have been subject to any organised excavation work. The Gogoshiis Qabe site was excavated in the 1940s by the Italian archaeologist Paolo Graziosi. In the 1950s British archaeologist John Desmond Clark investigated the Guli Waabayo and Rife Range sites, establishing that there was a degree of cultural continuity between the two. Following Clark's activities, no further organised archaeological work was carried out in the region until the 1980s, when Steven Brandt and the Buur Ecological and Archaeological Project returned and carried out further excavations at all three sites. These excavations were brought to an abrupt halt with the onset of the Somali Civil War in 1989, although, with the consent of the Somali Academy of the Arts and Sciences, much of the excavated material was exported to the US, where it has been held in the collections of several institutions. 

Jones examined the material brought back from Guli Waabayo to establish the identity of the small Antelope bones present; these had previously all been assigned to the genus Madoqua (Dik Diks), but this is not the only genus of small Antelopes in the Horn of Africa, and, since different Antelope have different ecologies, the identity of these bones has implications for the techniques which would have been effective when hunting them. Next Jones looked at the overall assemblage, and calculated the proportion of remains coming from each type of small Mammal, and then the proportion of each age-set within the overall sample.

Studying hunting methods used to on large prey can be achieved by looking at the weapons involved, or the use and modification of the landscape by the hunters, such as cliff jumps or kite structures. However, the study of how small game is hunted requires less direct approach, as such Animals are often captured with snares, nets, or traps made from perishable materials such as plant fibres, wood, or leather. In order to address this Zooarchaeologists have developed methods of analysing the ways in which people in the past hunted small game, based upon analysis of the variety of remains.

The composition of collections of small Animal remains will vary depending on the hunting method used. Studies conducted in places where net-drives (driving Animals into net traps) are still used, such as the Congo Basin, Australia, and the southwestern United States, has shown that this method will tend to target only one or two species, but will trap almost all members of those species within the target area. This method is most useful for targeting small Animals in forested, bushy or rocky habitats. Pursuit hunting and setting of individual traps such as snares both tend to produce a more diverse range of prey, which will be reflected in the bone assemblage left behind. 

Furthermore, while net hunting captures individuals of all ages, both snare hunting and persuit hunting tend to produce a high proportion of remains from a single age group, since the young of small Animals generally lack the weight to trigger snares designed for adult Animals, and Humans hunting with bows or clubs will generally take a higher proportion of slower, juvenile Animals.

The excavations carried out at Guli Waabayo comprised 11 one metre by one metre pits, each excavated to a depth of 2.5 m. These uncovered a sequence of three Middle Stone Age/Later Stone Age technologies, although, the lower part of the exposed sequence could not be dated due to an absence of Animal remains. Dates were obtained from Ostrich shell fragments for the upper 1.5 m of the sequence, demonstrating at least sporadic occupation of the shelter from 26 000 to 6000 years ago. Two distinct Later Stone Age technologies could be seen within the sequence, the Eibian, which was used during the arid Marine Isotope Stage 2 from about 29 000 to about 14 500 years ago, and the Bardaale, used in the wetter African Humid Period from about 14 500 to about 6000 years ago.

Analysis of the faunal remains found at Guli Waabayo showed that Later Stone Age hunters across the Pleistocene/Holocene boundary targeted a diverse range of game, including large and small Mammals, Birds, Reptiles, and Fish, although they had a clear preference for Mammals massing less than 20 kg. This preference for small Mammals seems to have increased slightly in the African Humid Period, although this change in climate appears to have made relatively little difference to the site's occupants, probably because the African Humid Period was a lot less pronounced in southern Somalia than in other areas.

Of the bones present at Guli Waabayo, 3104 could be identified as coming from small Mammals, with 2111 identifiable to a lower taxonomic level. Of these 1263 have previously been identified as coming from Dwarf Antelope, with the assumption that they originated from Dik Dik. However, this assumption was never actually put to the test, and there is another form of Dwarf Antelope present in the Horn of Africa, the Suni, Neotragus moschatus.

Jones selected all of the first phalanges assigned to Dwarf Antelopes in the Guli Waabayo collection, and compared them to first phalanges from Dik Dik and Suni in the collection of the Field Museum in Chicago. The size ranges of the first phalanges did not overlap, and all of the specimens from the Guli Waabayo collection conformed with the Dik Dik form, although it was not possible to tell which species of Dik Dik they belonged to.

The Dik Dik genus, Madoqua, first appears in the fossil record in the Miocene. There are four living species within the genus, Madoqua guentheriMadoqua saltiana, and Madoqua piacentinii are endemic to the Horn of Africa, while the fourth, Madoqua kirkii is found from Somalia south to Tanzania and eastern Uganda, as well as on the west coast of Southern Africa in Namibia and Angola. All species favour rocky environments with low thicket vegetation, with the inselbergs of southern Somalia providing an excellent environment, that today supports a large population of Dik Dik, which live in monogamous pairs, with each pair occupying and defending a territory with an area of about 1 km².

A Salt's Dik Dik, Madoqua saltiana, in the wild. David Castor/Wikimedia Commons.

Dik Dik are not widely hunted in Africa today, although in places they are targeted for their meat and skins, which are used to make gloves and cloaks. The Hadza people of northern Tanzania occasionally hunt Dik Dik with bows and arrows, while the Mukogodo people, who lived in the area around Mount Kenya in the eighteenth century are believed to have hunted Dik Dik both with snares and by stalking. 

Modern Somali pastoralists have been recorded to chase down Dik Dik, which seems surprising, given that these Dwarf Antelopes can reach speeds of about 42 km per hour, but is possible because they are so reluctant to leave their territories that they will often run around the perimeter when chased, allowing much slower Human pursuers to keep them in sight until they become exhausted and are easily captured. In the 1940s and 1950s several agropastoralist groups in Somalia were reported to capture Dik Dik in net hunts.

During these hunts, the men used nets about 5 m in length, strung between 2 m long poles. These nets would be used to create semi-circular traps, into which Dik Dik could be driven by men and Dogs, before being dispatched with bows and arrows, a methodology which could conceivably have been used by Later Stone Age hunters in the same region.

Having established the Small Antelope remains at Guli Waabayo came from Dik Dik, Jones next sorted the remains into age groups, based upon examination of complete and partial tooth rows, as well as loose lower 3rd molars and 4th premolars. The dental aging of modern Dik Dik has not been extensively studied, but it was still possible to separate the remains into juvenile, older juvenile, adult, and older adults, based upon the relative eruption and wear seen in the teeth. 

Madoqua mandibles of different age sets from Guli Waabayo. Jones (2023).

Dik Dik remains dominated the faunal assemblage at Guli Waabayo in both Marine Isotope Stage 2 and the African Humid Period. Roughly twice as many remains assignable to Madoqua were found in Marine Isotope Stage 2 selection as in the African Humid Period selection, but this was also true of other Animals present, ab probably reflects the fact that Marine Isotope Stage 2 lasted about 14 000 years, while the African Humid Period lasted only about 6000 years. Nevertheless, the proportion of the assemblage made up by Dik Dik bones did increase, from 55.2% in Marine Isotope Stage 2, to 71.9% in the African Humid Period.

Small Mammal frequencies from Guli Waabayo, presented as % (number of identifiable specimens). Abbreviations: MIS 2, marine isotope stage 2; AHP, African humid period; ka. thousand years ago. Jones (2023).

In both intervals, the age-profile of the Dik Dik remained fairly constant, with all age groups present, but adults making up almost half of the assemblage in both cases, while the other three age groups each made up between 13.3% and 21.3% of the assemblage, although Jones notes that the sample size is very small for the African Humid Period, which may mask greater variation than is recorded.

Dik-dik mortality profiles from Guli Waabayo, presented as % (minimum number of individuals). Abbreviations: MIS 2, marine isotope stage 2; AHP, African humid period; ka, thousand years ago. Jones (2023).

There was a relatively high proportion of Carnivore remains in both Marine Isotope Stage 2 (4.4%) and the African Humid Period (5.4%). This could potentially indicate that the site had at times been occupied by Carnivores (for example Hyenas), and that they would have been responsible for some of the other remains present. Signs of such denning behaviour are considered to include juvenile Carnivore bones, gnaw marks on the bones of other Animals. Of 88 identified small Carnivore bones present in the total collection from Guli Waabayo, only three had unfused epiphyses (two from indeterminate Carnivores and one from a small Felid). In addition a mandible was identified with an erupting third molal (a sign that it came from a juvenile Animal), which could be assigned to a Dwarf Mongoose, Helogale sp.. No bones could be attributed to juvenile medium or large Carnivores, such as Hyenas or Lions, and no neonatal Carnivore bones of any type were found. A single Dik Dik bone from Marine Isotope Stage 2 showed signs of gnawing, but this was clearly by a Rodent Three Dik Dik bones from the African Humid Period also showed signs of gnawing, with two of these again clearly having been gnawed by Rodents. Conversely, none of the Dik Dik bones showed signs of butchery with tools, although this would not typically be expected with the bones of an Animal this small. Signs of burning, another clear indicator of a Human predator, were found on 12.3% of the Marine Isotope Stage 2 Dik Dik remains, and 7.8% of the African Humid Period Dik Dik bones.

Jones's investigation confirmed that Later Stone Age hunters had extensively targeted Dik Dik, small territorial Bovids, during both Marine Isotope Stage 2 and the African Humid Period, something in line with previous research at the site. However, unlike previous researchers, Jones did not concentrate on the toral diversity of remains at the site, but specifically upon the most abundant item, the Dik Dik, with a view to understanding the importance of these Antelopes to Later Stone Age hunting communities in the area. The evidence strongly suggests that the people here became specialist hunters of Dik Dik during the arid Late Pleistocene. 

This is different to the pattern observed at the Riffle Range Site, where a specialisation in net-hunting of Dik Dik appears to have developed during the African Humid Period, alongside a more general shift towards a more settled lifestyle and the permanent holding or territory by Later Stone Age groups. At Guli Waabayo the proportion of Dik Dik among the Animal remains increased in the African Humid Period, suggesting that they became a more important resource during this time, but they were clearly already a major prey species in Marine Isotioe Stage 2. This suggests that the change in climate did not provoke a major change in hunting methods or other behaviours at Guli Waabayo. This raises the possibility that the apparent change in behaviour at the Riffle Range Site 12 000 years ago may be actually indicate that the site was only sporadically inhabited prior to this, or simply that earlier remains have not been preserved. An increase in usage of the Riffle Range Site during the Holocene appears to be the more likely scenario, but why that should be is unclear.

The hunters of Guli Waabayo appear to have taken far more Dik Dik than any other Animal, even similar sized small Mammals, such as Hares or Hyraxes. Thus suggests that they had developed a specialised hunting technique which enabled them to reliably capture large numbers of Dik Dik, bur which did not work as readily on other prey. Furthermore, the Dik Dik remains have a distinct age profile, with all age groups present but adults being the most abundant. Based upon studies of modern Dwarf Antelope hunters, the most likely explanation for this is that communal net drives were used to target Dik Dik on a regular basis, but that other hunting methods were also used to catch other prey.

The selection of faunal remains present at Guli Waabayo makes it likely that both snare and pursuit hunting were also practiced, but the large proportion of Dik Dik in the remains cannot be explained by this. Snares will tend to target a range of Animals of the same size, including small Carnivores, which are present in the Guli Waabayo assemblage, but do not tend to capture juvenile Animals, which are typically too small to trigger them. Had snares been the primary hunting method at Guli Waabayo, then the overall assemblage of Animals would have been more varied, without any single species dominating, and juvenile Dik Dik would have been largely absent. Pursuit hunting, in contrast, tends to produce a far higher proportion of juvenile Animals, which are easier to run down, but again does not tend to produce an assemblage dominated by a single species. 

The bone assemblage from Guli Waabayo was accumulated over thousands of years, making it unlikely that all of the Dik Dik remains there are the result of a single hunting method. Nevertheless, it does appear likely that net hunting played a significant role in the life of Later Stone Age hunters in the region.

The most egalitarian hunter/gatherer societies tend to invest little effort in the manufacture of material goods. However, as societies become more complex, an increasing emphasis is placed upon resource management, and delayed-return technologies, which ensure the future supply of food. Such technologies include both devices used to store food, and to capture Animals for consumption, and are in turn associated with a decrease in mobility, with groups tending to remain in one place for longer. In environments with strong seasonal variations in the availability of food, this can lead to the development of flexible political systems or large resource-sharing networks. 

The Holocene Kansyore people of the Lake Victoria Basin are known to have used pottery and Fish weirs d to exploit seasonal Fish stocks, a specialization which resulted in long-term occupation of sites, and presumably a sense of ownership of those sites. The connection between subsistence, land use, and technology during earlier periods in East Africa is less clear, although the specialisation in hunting Dik Dik in the pre-Holocene Later Stone Age at Guli Waabayo suggests that these people had developed a lifestyle in Marine Isotope Stage 2 which was tied to long term resource management within a single environment, and the use of specialist equipment, in the form of nets, which would have required considerable investment in time to construct and maintain.

The traditional view of Late Pleistocene hunters in East Africa has been one of highly mobile groups which placed an emphasis on the hunting of large game. However, the evidence from s coastal and forested regions suggests that small game may have been a far more important resource than was previously thought, to at least some groups of hunter/gatherers. The use of delayed-return hunting technologies, such as snares, traps, or nets, would have allowed more settled populations in coastal and forested environments, enabling a diversity of survival strategies to survive alongside one another in East Africa during the Late Pleistocene. The evidence for specialist Dik Dik hunting at Guli Waabayo adds to this understanding, giving an example of a community surviving in a semi-arid environment by adopting a more settled lifestyle and a specialist method of hunting.

Most hunting methods target one Animal at a time, but net drives can trap numerous Animals at the same time, potentially leading to surpluses of meat following the hunt. Among modern communities which practice net hunting in the Congo Basin, hunts are typically communal activities, involving men, women, and children, and the re-enforcement of social bonds. In Australia the organisation of net-hunts has been associated with the emergence of political hierarchies, while in the southwestern US the organisation of communal net hunts for Rabbits has been associated with both forming co-operative bonds between different groups, and the establishment of temporary leaders.

No direct evidence of netting has been found at Guli Waabayo, however, the pattern of remains suggests that the hunters here were using communual net-drives to capture large numbers of Dik Dik during the Later Stone Age. Such hunts would likely have resulted in considerable amounts of meat becoming available at certain times, enabling the surplus to be shared among large extended communities.

If this were the case, then Dik Dik hunting would have enabled large communal gatherings, promoting social cohesion between groups and promoting further co-operation. However, the faunal data is not enough in itself to make many assumptions about these ancient societies, and further analysis of Human burials from Guli Waabayo and Gogoshiis Qabe, combined with studies of lithic tools from these sites and the Riffle Range Site, should help us gain a better understanding of these ancient East African communities.

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Wednesday, 2 August 2023

Magnitude 5.6 Earthquake to the south of Massawa, Eritrea.

The United States Geological Survey recorded a Magnitude 5.6 Earthquake at a depth of 10.0 km, roughly 42 km to the south of the city of Massawa in central Eritrea, at about 8.15 pm local time (about 5.15 pm GMT) on Tuesday 1 August 2023. There are no reports of any damage or injuries from this quake, but people have reported feeling the event in Asmara, the capitol of Eritrea, as well as in Tigray Province, Ethiopia.

The approximate location of the 1 August 2023 Eritrea Earthquake. USGS.

The deserts of Northern Ethiopia and Eritrea are extremely volcanically active, with dozens of volcanoes fed by an emerging divergent margin along the East African Rift; the volcano Erta Ale is on the Ethiopian Rift, the boundary between the Nubian Plate and the Danakil Microplate. The African Plate is slowly splitting apart along the Ethiopian Rift and the East African Rift to the south (which is splitting the Nubian Plate to the West from the Somali Plate to the East). Arabia was a part of Africa till about thirty million years ago, when it was split away by the opening of the Red Sea Rift (part of the same rift system), and in time the Ethiopian and East African Rifts are likely to split Africa into a number of new landmasses. This rifting exerts pressure on the rocks around the margin of the sea, slowly pushing them apart, not smoothly but in fits and starts as the pressure overcomes the tendency of the rocks to stick together, creating shocks that we experience as Earthquakes.

Rifting in East Africa. The Danakil Microplate is the red triangle to the east of the Afar depression at the southern end of the Red Sea. Università degli Studi di Firenze.

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