Proboscidea is a taxonomic order of afrotherian mammals containing one living family (Elephantidae) and several extinct families. First described by J. Illiger in 1811, it encompasses the elephants and their close relatives. Three species of elephant are currently recognised: the African bush elephant, the African forest elephant, and the Asian elephant.
Elephantidae is a family of large, herbivorous proboscidean mammals collectively called elephants and mammoths. These are large terrestrial mammals with a snout modified into a trunk and teeth modified into tusks. Most genera and species in the family are extinct. Only two genera, Loxodonta and Elephas, are living.
Elephas is one of two surviving genera in the family of elephants, Elephantidae, with one surviving species, the Asian elephant, Elephas maximus. Several extinct species have been identified as belonging to the genus, extending back to the Pliocene or possibly the late Miocene.
Stegodon is an extinct genus of proboscidean, related to elephants. It was originally assigned to the family Elephantidae along with modern elephants but is now placed in the extinct family Stegodontidae. Like elephants, Stegodon had teeth with plate-like lophs that are different from those of more primitive proboscideans like gomphotheres and mammutids. Fossils of the genus are known from Africa and across much of Asia, as far southeast as Timor. The oldest fossils of the genus are found in Late Miocene strata in Asia, likely originating from the more archaic Stegolophodon, subsequently migrating into Africa. While the genus became extinct in Africa during the Pliocene, Stegodon persisted in South, Southeast and Eastern Asia into the Late Pleistocene.
Gomphotheres are an extinct group of proboscideans related to modern elephants. First appearing in Africa during the Oligocene, they dispersed into Eurasia and North America during the Miocene and arrived in South America during the Pleistocene as part of the Great American Interchange. Gomphotheres are a paraphyletic group ancestral to Elephantidae, which contains modern elephants, as well as Stegodontidae.
Hadar or Hadar Formation is a paleontological fossil site located in Mille district, Administrative Zone 1 of the Afar Region, Ethiopia, 15 km upstream (west) of the A1 road's bridge across the Awash River.
Australopithecus anamensis is a hominin species that lived approximately between 4.3 and 3.8 million years ago and is the oldest known Australopithecus species, living during the Plio-Pleistocene era.
Palaeoloxodon recki, often known by the synonym Elephas recki, is an extinct species of elephant native to Africa and West Asia from the Pliocene or Early Pleistocene to the Middle Pleistocene. During most of its existence, the species represented the dominant elephant species in East Africa. The species is divided into five roughly chronologically successive subspecies. While the type and latest subspecies P. recki recki as well as the preceding P. recki ileretensis are widely accepted to be closely related to Eurasian Palaeoloxodon, the relationships of the other, chronologically earlier subspecies to P. recki recki and P. recki ileretensis are uncertain, with it being suggested they are unrelated and should be elevated to separate species.
Procavia is a genus of hyraxes. The rock hyrax (P. capensis) is currently the only extant species belonging to this genus, though other species were recognized in the past, including P. habessinica and P. ruficeps, both now relegated to subspecific rank.
Yohannes Haile-SelassieAmbaye is an Ethiopian paleoanthropologist. An authority on pre-Homo sapiens hominids, he particularly focuses his attention on the East African Rift and Middle Awash valleys. He was curator of Physical Anthropology at the Cleveland Museum of Natural History from 2002 until 2021, and now is serving as the director of the Arizona State University Institute of Human Origins. Since founding the institute in 1981, he has been the third director after Donald Johanson and William Kimbel.
Kolpochoerus is an extinct genus of the pig family Suidae related to the modern-day genera Hylochoerus, Phacochoerus, and Potamochoerus. It is believed that most of them inhabited African forests, as opposed to the bushpig and red river hog that inhabit open brush and savannas. There are currently eleven recognized species.
Mammuthus africanavus is a species of mammoth known from remains spanning the Late Pliocene-Early Pleistocene found in Central and North Africa in the countries of Chad, Morocco, Tunisia and Algeria. It was originally described by Camille Arambourg in 1952 based on remains found around Lake Ichkeul in north Tunisia as a species of Elephas. Some specimens from this sample may genuinely represent Elephas rather than Mammuthus, though the holotype has been argued to likely represent a true mammoth. Some authors have argued that the species should be placed in Loxodonta, reflecting the difficulty in distinguishing the teeth of early elephantids. It is distinguished from the earlier Mammuthus subplanifrons by having a higher number of ridges/lamellae on the teeth, which display a greater parallelity, the molars being more hypsodont, with the molars having a greater amount of cementum and thinner enamel, and the molar plates exhibit closer spacing.
Ardipithecus kadabba is the scientific classification given to fossil remains "known only from teeth and bits and pieces of skeletal bones", originally estimated to be 5.8 to 5.2 million years old, and later revised to 5.77 to 5.54 million years old. According to the first description, these fossils are close to the common ancestor of chimps and humans. Their development lines are estimated to have parted 6.5–5.5 million years ago. It has been described as a "probable chronospecies" of A. ramidus. Although originally considered a subspecies of A. ramidus, in 2004 anthropologists Yohannes Haile-Selassie, Gen Suwa, and Tim D. White published an article elevating A. kadabba to species level on the basis of newly discovered teeth from Ethiopia. These teeth show "primitive morphology and wear pattern" which demonstrate that A. kadabba is a distinct species from A. ramidus.
Mammuthus subplanifrons is the oldest representative of the genus Mammuthus, known from around 6.2-3.75 million years ago during the late Miocene-early Pliocene in what is today South Africa and countries of East Africa, especially Ethiopia. They already presented some of the unique characteristics of mammoths like the spirally, twisting tusks.
Kadanuumuu is the nickname of KSD-VP-1/1, a 3.58-million-year-old partial Australopithecus afarensis fossil discovered in the Afar Region of Ethiopia in 2005 by a team led by Yohannes Haile-Selassie, curator of physical anthropology at the Cleveland Museum of Natural History. Based on skeletal analysis, the fossil is believed to conclusively show that the species was fully bipedal.
Australopithecus deyiremeda is an extinct species of australopithecine from Woranso–Mille, Afar Region, Ethiopia, about 3.5 to 3.3 million years ago during the Pliocene. Because it is known only from three partial jawbones, it is unclear if these specimens indeed represent a unique species or belong to the much better-known A. afarensis. A. deyiremeda is distinguished by its forward-facing cheek bones and small cheek teeth compared to those of other early hominins. It is unclear if a partial foot specimen exhibiting a dextrous big toe can be assigned to A. deyiremeda. A. deyiremeda lived in a mosaic environment featuring both open grasslands and lake- or riverside forests, and anthropologist Fred Spoor suggests it may have been involved in the Kenyan Lomekwi stone-tool industry typically assigned to Kenyanthropus. A. deyiremeda coexisted with A. afarensis, and they may have exhibited niche partitioning to avoid competing with each other for the same resources, such as by relying on different fallback foods during leaner times.
Palaeoloxodonjolensis is an extinct species of elephant. The type specimen is located in the National Museum of Natural History in Paris. It is either considered the descendant species or last evolutionary stage of Palaeoloxodon recki in Africa. It is only known from isolated molars. The species is known from remains found across Africa, which are largely poorly dated to approximately the late Middle Pleistocene to Late Pleistocene, with some authors suggesting an exclusively late Middle Pleistocene age, as the only well dated specimens of the species are over 130,000 years old. Like P. recki, they are thought to have been dedicated grazers, being distinguished from earlier P. recki by having increased hypsodonty and enamel folding, with the plates being thicker along the long axis of the tooth. Following the extinction of the species, it was largely replaced by the modern African bush elephant.
Elephas planifrons is an extinct species of elephant, known from the Late Pliocene-Early Pleistocene of the Indian subcontinent.
Pliopapio is an extinct genus of Old World monkey known from the latest part of the Miocene to the early Pliocene Epochs from the Afar Region of Ethiopia. It was first described based on a very large series of fossils from the site of Aramis in the Middle Awash, which has been dated by 40Ar/39Ar to 4.4 million years old. It has since been found from similarly aged sediments at Gona, approximately 75 km to the North. Additional fossils from the Middle Awash extend its known time range back to at least 5.3 million years ago. There is only one known species, Pliopapio alemui.
MRD-VP-1/1 is a fossilized cranium of the species Australopithecus anamensis. The first piece of MRD, the upper jaw, was found by Ali Bereino, a local Afar worker, on February 10, 2016, at Miro Dora, Mille district of the Afar Region, in present-day Ethiopia.
