Early Homo erectus skeleton from west Lake Turkana, Kenya

@article{Brown1985EarlyHE,
  title={Early Homo erectus skeleton from west Lake Turkana, Kenya},
  author={Francis H. Brown and JOHN M. Harris and Richard Erskine Frere Leakey and Alan W. Walker},
  journal={Nature},
  year={1985},
  volume={316},
  pages={788-792}
}
The most complete early hominid skeleton ever found was discovered at Nariokotome III, west Lake Turkana, Kenya, and excavated in situ in sediments dated close to 1.6 Myr. The specimen, KNM-WT 15000, is a male Homo erectus that died at 12 ± 1 years of age, as judged by human standards, but was already 1.68 m tall. Although human-like in many respects, this specimen documents important anatomical differences between H. erectus and modern humans for the first time. 

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References

SHOWING 1-10 OF 17 REFERENCES

Australopithecus, Homo erectus and the single species hypothesis

The evidence presented here deals not with the earlier stages of human evolution, but with the unequivocal occurrence of H. erectus from the Koobi Fora Formation, east of Lake Turkana (formerly Lake Rudolf).

Postcranial Remains of Homo erectus from Bed IV, Olduvai Gorge, Tanzania

  • M. H. Day
  • Environmental Science, Geography
    Nature
  • 1971
Anatomically, the postcranial remains of Olduvai Hominid 28 seem to have a close resemblance to the Homo erectus material from Choukoutien.

A hominine hip bone, KNM-ER 3228, from East Lake Turkana, Kenya.

  • M. D. Rose
  • Environmental Science
    American journal of physical anthropology
  • 1984
A male hominine partial hip bone from East Lake Turkana, Kenya is described, which is very similar to the Olduvai Hominid 28 and the Arago XLIV hip bones, both attributed to Homo erectus.

Age of the Okote Tuff Complex at Koobi Fora, Kenya

The Okote Tuff Complex crops out in the Koobi Fora region next to the north-eastern shores of Lake Turkana, northern Kenya. It occurs in the upper part of the ∼450 m thick, essentially flat lying,

Guide to fossil man

  • M. H. Day
  • Environmental Science, Geography
  • 1977
Michael H. Day's "Guide to Fossil Man" is the standard reference work on hominid remains found at the major palaeolithic sites throughout the world. This fourth edition now includes details of

K-Ar and 40Ar/39Ar dating of the hominid-bearing Pliocene-Pleistocene sequence at Koobi Fora, Lake Turkana, northern Kenya

In the Koobi Fora region, east of Lake Turkana, northern Kenya, there occurs a sequence ∼500 m thick of lacustrine, fluvial, and deltaic sediments that contains abundant vertebrate fossils, including

A possible case of hypervitaminosis A in Homo erectus

The partial skeleton from the Upper Member of the Koobi Fora Formation shows pathological changes consistent with chronic hypervitaminosis A, and is attributed to the high dietary intake of animal liver, most probably that of carnivores, during a period when the dietary habits of Homo erectus were changing.

Tooth Eruption Sequence in Fossil and Recent Man

The sequence of eruption of the permanent teeth has been used as a measure of the biological distance between early and recent man and it is held that this sequence “agrees closely with that of modern man”.