Chesowanja is a Kenian archaeological site located in the north of the Kenya Rift Valley, east of Lake Baringo. The Chesowanja sites consist of quaternary sediments. The sites are home to various discoveries like fossils, evidence of human activity over a period of 2 million years and the remains of Australopithecus. Also, artefacts belonging to Oldowan technology, Acheulean tradition and later stone industries have been found. [1]
Chesowanja was investigated first by the geologist John Carney. This investigation was part of a programme of regional mapping executed by the East African Geological Research Unit. Carney recovered fossil vertebrates from the Chemoigut Formation. A following faunal survey conducted by Andrew Hill unveiled a partial cranium of Australopithecus. In 1973, William Bishop, Andrew Hill, and Martin Pickford analysed the geological situation of Chesowanja. Extensive sequences of artifact horizons, and more hominid material was discovered. [2]
Miocene rocks are the oldest surface rocks, consisting of basalts and phonolites. They are found in the east and west areas of Chesowanja. Besides diatoms and silicified wood, the phonolites consist of little fossils. The phonolites are believed to date between 10.7 mya and 13.5 mya. Phonolite cobbles found in the area were favoured as raw material for artifact production. [2]
Besides phonolites, the deeply weathered ankaramatic basalt is part of the oldest exposed rocks in the region. This type of basalt is found extensively to the north (GR 8870, GR 8975). A relation between the phonolites and basalt is not observed anywhere. However, the basalt is thought to be younger than the phonolites. In certain parts of the area the ankaramatic basalt lays under three different layers - the Erinei trachyte, the Chemoigut Formation, and the Chesowanja Formation. [2]
The Erinei trachyte is found in the south of the extensive region, and is the first layer covering the ankaramatic basalt in streambeds at GR 8770. [2]
The Chemoigut Formation consists of layers of silts and clays with horizons consisting of unrefined tuffaceous and pumiceous sandstone and fine conglomerates. The formation is exposed in three windows ruptured crest of the Chesowanja anticline. This anticline runs from north to south and the windows get numbered from one to three. In the north the thickness of the layer is estimated to be around 50m. To the south, only 25 to 30m are exposed. In the Chemoigut Formation stone artefacts are found, providing the oldest local evidence for hominid activity. Also fossil bones, and the australopithecine partial cranium have been found in the formation.
The relationship between the Chemoigut Formation and Erinei trachyte is unknown. It seems like the sediments represent largely shallow water conditions recording the gradual burial of the landscape. [2]
On top of the Chemoigut Formation lies the Chesowanja Formation. The formation consists of two basalt flows. On the surface of the second flow a palaeosol developed to the east of the Chesowanja anticline. In the upperpart of this palaeosol Acheulian artefacts have been discovered. [2]
The Karau Formation, laying on top of the Chesowanja Formation, consists of basalt, consisting of two units of trachytic tuffs. The tuffs found to the east of the anticline are fine-grained and contain plant impressions. These tuffs are the result of lacustrine deposition, either by falling into the lake or being transported through water. To the west, the tuffs have been formed by airfall. The two tuffs are useful to relatively date the Acheulean artefact assemblages found on the palaeosol surface underneath. [2]
On the Karau Formation to the east, a layer of pisolitic ferruginous calcrete is present. This layer has a very similar consistency as the weathering profile on the surface of the Chesowanja basalt. Just like on this Chesowanja surface, the calcrete layer contains Acheulean or similar artifacts. [2]
Approximately 1 km east of the Chesowanja anticline the Mukutan Beds are exposed. They are stretched out along the Losokweta River and abandoned arms of the Mukutan River. In the upper reaches of the Losokweta, the basalt consists of a phonolite conglomerate, with tuffs and red silts. Artefacts and fossils are occasionally found in these deposits. [2]
The youngest rocks in the Chesowanja area are alluvial and colluvial deposits. To the east, the alluvium consists of floodplain silts of the Mukatan River. During sheet floods, the silts are still actively transported. The layer is maximum 2 m thick. [2]
The only layer rich in fossils is the Chemoigut Formation. Artefacts on the surface of the Chesowanja Formation and in the Mukutan Beds can be brought in association with some fauna. The australopithecine cranium (KNM-CH-1) found shows similarities with the Australopithecus robustus (Broom) and Australopithecus boisei (Leakey). Bishop et al. also discovered teeth fragments of another australopithecine individual (KNM-CH-302). Radiometric dating places the faunal evidence found in the Chemoigut Formation between 1.93 mya and 1.34 mya. This is in line with the Olduvai chronology.
The modern environment and its proxies show the link with bushed grassland habitats, with riverine and lacustrine components. [2]
Archaeological materials in Chesowanja are found in at least eight horizons within the geological succession. Harris and Bishop separate the materials found into three main categories. Tools from the Developed Oldowan industry have been found in the Chemoigut Formation. The surface of the Chesowanja Formation is known for its Acheulian industry. And lastly, the Mukutan Beds were home to later stone industry tools, obsidian tools, and pottery.
Artifacts in the Chemoigut Formation are rich in quantity and are found in five levels of the formation. Layers one and five (A1-A5) held remains of the Australopithecus. This Australopithecine cranium is dented by a lateral pressure and the palate was pushed inferiorly and anteriorly, creating an opening in the maxillary region. [3] The cranium belonged to a large brained robust Australopithecine. [4] In total the surface comprised 220 specimens from four main localities. All these specimens belong to a single cultural complex, the Oldowan/Developed Oldowan. The toolkit consists of choppers, side, end, and two-edged forms. The splintered ends of the stone tools indicate utilization. Also, two large symmetrical discoid/core tools with bifacially worked edges and a biconvex cross section have been found. This feature is atypical to the Oldowan/Developed Oldowan industry. There are also polyhedrons, discoids, light-duty scrapers made on flakes, and protobifaces found in the Chemoigut Formation. Real bifaces are absent. According to Bishop this industry probably dates back to 1.93 mya to 1.34 mya. [2] Later Karbon-Argon dating of the basalt reported an age of 1.42 to 0.07 mya for the Australopithecus remains and the associated Oldowan tool technology. [5]
The surface of the weathering profile developed on the upper basalt layer of the Chesowanja Formation shows evidence of the Acheulian industry. A collection of hand axes display a large range in size and shape, a high degree of fine-motoric skills, and are finished with fine flaking. Some hand axes are symmetrical and flaked to a sharp edge around the entire stone tool outline. Also cleavers, bifacially flaked choppers, pebble cortex, and scrapers have been found. The Chesowanja collection resembled the Late Auchelian assemblages to the west of Lake Baringo (Leakey 1969). The estimated date for these sites is 0.23 mya, though it could be later. Another surface collection of Acheulian tools came to light with the weathering of the later ‘Pisolitic ferruginous calcrete’. This assemblage also includes Levallois cores. [2]
A later stone tool industry is found in the former flood plain of the Mukutan. Places probably used as factory sites hold large mounds of artefacts. These artefacts consist of heavy duty core tools, including double ended picks and flakes. These stone tools are made of water cobbles and phonolites. Besides stone tools, pottery is present in the Mukutan Beds. No good estimates of age have been made for this region. [2]
Burnt clay found at one of the artefact localities dated to at least 1.42 to 0.07 mya. This is the earliest known evidence of fire associated with a hominid occupation site. The find strengthens the hypothesis that humans were controlling and using fire by 1.42mya. Glynn Isaac, however, doesn’t exclude the possibility of this evidence just being caused by natural causes, like a bush fire. He claims that we still don’t know whether humans used fire earlier than 0.5 mya. Gowlett, Harris and Wood replied that the clay was burned. The association of the fire with artefacts is thus direct and physical. The relatively low temperature for the baking of the clay forms more evidence for the nature of the fire. [6]
Kenyanthropus is a hominin genus identified from the Lomekwi site by Lake Turkana, Kenya, dated to 3.3 to 3.2 million years ago during the Middle Pliocene. It contains one species, K. platyops, but may also include the 2 million year old Homo rudolfensis, or K. rudolfensis. Before its naming in 2001, Australopithecus afarensis was widely regarded as the only australopithecine to exist during the Middle Pliocene, but Kenyanthropus evinces a greater diversity than once acknowledged. Kenyanthropus is most recognisable by an unusually flat face and small teeth for such an early hominin, with values on the extremes or beyond the range of variation for australopithecines in regard to these features. Multiple australopithecine species may have coexisted by foraging for different food items, which may be reason why these apes anatomically differ in features related to chewing.
Australopithecus is a genus of early hominins that existed in Africa during the Pliocene and Early Pleistocene. The genera Homo, Paranthropus, and Kenyanthropus evolved from some Australopithecus species. Australopithecus is a member of the subtribe Australopithecina, which sometimes also includes Ardipithecus, though the term "australopithecine" is sometimes used to refer only to members of Australopithecus. Species include A. garhi, A. africanus, A. sediba, A. afarensis, A. anamensis, A. bahrelghazali and A. deyiremeda. Debate exists as to whether some Australopithecus species should be reclassified into new genera, or if Paranthropus and Kenyanthropus are synonymous with Australopithecus, in part because of the taxonomic inconsistency.
A stone tool is, in the most general sense, any tool made either partially or entirely out of stone. Although stone tool-dependent societies and cultures still exist today, most stone tools are associated with prehistoric cultures that have become extinct. Archaeologists often study such prehistoric societies, and refer to the study of stone tools as lithic analysis. Ethnoarchaeology has been a valuable research field in order to further the understanding and cultural implications of stone tool use and manufacture.
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Acheulean, from the French acheuléen after the type site of Saint-Acheul, is an archaeological industry of stone tool manufacture characterized by the distinctive oval and pear-shaped "hand axes" associated with Homo erectus and derived species such as Homo heidelbergensis.
Meganthropus is an extinct genus of non-hominin hominid ape, known from the Pleistocene of Indonesia. It is known from a series of large jaw and skull fragments found at the Sangiran site near Surakarta in Central Java, Indonesia, alongside several isolated teeth. The genus has a long and convoluted taxonomic history. The original fossils were ascribed to a new species, Meganthropus palaeojavanicus, and for a long time was considered invalid, with the genus name being used as an informal name for the fossils.
The Oldowan was a widespread stone tool archaeological industry (style) in prehistory. These early tools were simple, usually made with one or a few flakes chipped off with another stone. Oldowan tools were used during the Lower Paleolithic period, 2.9 million years ago up until at least 1.7 million years ago (Ma), by ancient Hominins across much of Africa. This technological industry was followed by the more sophisticated Acheulean industry.
Sterkfontein is a set of limestone caves of special interest in paleoanthropology located in Gauteng province, about 40 kilometres (25 mi) northwest of Johannesburg, South Africa in the Muldersdrift area close to the town of Krugersdorp. The archaeological sites of Swartkrans and Kromdraai are in the same area. Sterkfontein is a South African National Heritage Site and was also declared a World Heritage Site in 2000. The area in which it is situated is known as the Cradle of Humankind. The Sterkfontein Caves are also home to numerous wild African species including Belonogaster petiolata, a wasp species of which there is a large nesting presence.
In the archaeology of the Stone Age, an industry or technocomplex is a typological classification of stone tools.
Abbevillian is a term for the oldest lithic industry found in Europe, dated to between roughly 600,000 and 400,000 years ago.
Australopithecus garhi is a species of australopithecine from the Bouri Formation in the Afar Region of Ethiopia 2.6–2.5 million years ago (mya) during the Early Pleistocene. The first remains were described in 1999 based on several skeletal elements uncovered in the three years preceding. A. garhi was originally considered to have been a direct ancestor to Homo and the human line, but is now thought to have been an offshoot. Like other australopithecines, A. garhi had a brain volume of 450 cc (27 cu in); a jaw which jutted out (prognathism); relatively large molars and premolars; adaptations for both walking on two legs (bipedalism) and grasping while climbing (arboreality); and it is possible that, though unclear if, males were larger than females. One individual, presumed female based on size, may have been 140 cm tall.
Paranthropus boisei is a species of australopithecine from the Early Pleistocene of East Africa about 2.5 to 1.15 million years ago. The holotype specimen, OH 5, was discovered by palaeoanthropologist Mary Leakey in 1959, and described by her husband Louis a month later. It was originally placed into its own genus as "Zinjanthropus boisei", but is now relegated to Paranthropus along with other robust australopithecines. However, it is also argued that Paranthropus is an invalid grouping and synonymous with Australopithecus, so the species is also often classified as Australopithecus boisei.
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Koobi Fora refers primarily to a region around Koobi Fora Ridge, located on the eastern shore of Lake Turkana in the territory of the nomadic Gabbra people. According to the National Museums of Kenya, the name comes from the Gabbra language:
In the language of the Gabbra people who live near the site, the term Koobi Fora means a place of the commiphora and the source of myrrh...
The Middle Awash is a paleoanthropological research area in the Afar Region along the Awash River in Ethiopia's Afar Depression. It is a unique natural laboratory for the study of human origins and evolution and a number of fossils of the earliest hominins, particularly of the Australopithecines, as well as some of the oldest known Olduwan stone artifacts, have been found at the site—all of late Miocene, the Pliocene, and the very early Pleistocene times, that is, about 5.6 million years ago (mya) to 2.5 mya. It is broadly thought that the divergence of the lines of the earliest humans (hominins) and of chimpanzees (hominids) was completed near the beginning of that time range, or sometime between seven and five mya. However, the larger community of scientists provide several estimates for periods of divergence that imply a greater range for this event, see CHLCA: human-chimpanzee split.
KNM ER 406 is an almost complete fossilized skull of the species Paranthropus boisei. It was discovered in Koobi Fora, Kenya by Richard Leakey and H. Mutua in 1969. This species is grouped with the Australopitecine genus, Paranthropus boisei because of the robusticity of the skull and the prominent characteristics. This species was found well preserved with a complete cranium but lacking dentition. He was known for his robust cranial features that showed the signs of adaptation of the ecological niches. The big chewing muscles attached to the sagittal crest are traits of this adaptation.
The Bouri Formation is a sequence of sedimentary deposits that is the source of australopithecine and Homo fossils, artifacts, and bones of large mammals with cut marks from butchery with tools by early hominins. It is located in the Middle Awash Valley, in Ethiopia, East Africa, and is a part of the Afar Depression that has provided rich human fossil sites such as Gona and Hadar.
LD 350-1 is the earliest known specimen of the genus Homo, dating to 2.8–2.75 million years ago (mya), found in the Ledi-Geraru site in the Afar Region of Ethiopia. The specimen was discovered in silts 10 m (33 ft) above the Gurumaha Tuff section of the site by Ethiopian palaeoanthropologist Chalachew Seyoum on 29 January 2013. It is currently unassigned to a species, and it is unclear if it represents the ancestor to H. habilis and H. rudolfensis which evolved around 2.4 mya.
Shangchen is a Lower Palaeolithic archaeological site in Lantian County, Shaanxi, China, some 25 km south of Weinan. It was discovered in 1964, and excavated during 2004 and 2017.
Gona is a paleoanthropological research area in the Afar Triangle of Ethiopia located in the Ethiopian Lowlands. The study area, near the Middle Awash and Hadar paleoanthropological study areas, is primarily known for it's archaeological sites and discoveries of Late Miocene and Early Pliocene fossils as well as Oldowan and Acheulean stone tools. Evidence of Homo erectus presence at Gona dates back to as early as 1.8 million years ago, making Gona's stone tools some of the world's oldest stone tool artifacts found to date. Gona is also known as a key site for the study of human evolution, with a rich hominin fossil record that includes evidence of Ardipithecus remains dating to around 4.5 million years old and Homo erectus fossils from approximately 1.8 to 1.7 million years ago. Likewise, faunal remains such as cutmarked bones from Gona give insight into early hominin diets and butchery practices, making it an important site for zooarchaeology.