The Mammalian Faunas and Hominid Fossils of the Middle Pleistocene of the Maghreb

1975 ◽  
pp. 399-418 ◽  
1968 ◽  
Vol 33 ◽  
pp. 367-376 ◽  
Author(s):  
Phillip V. Tobias

For over 40 years South Africa and for over 25 years East Africa have been yielding fossilized remains of creatures identified on their bony structure as lowly members of the Hominidae or human family. From five sites in the Republic of South Africa (Taung, Sterkfontein, Kromdraai, Makapansgat and Swartkrans) and from three sites in the Republic of Tanzania (Garusi, Olduvai and Peninj) have emerged a considerable number of hominid fossils of the Lower and Middle Pleistocene. Most of them have been classified as members of an extinct hominid genus called by R. A. Dart, the discoverer of the first specimen, Australopithecus. Although variable among themselves, the structural features which aligu these fossils with the Hominidae, rather than with the family of the apes or Pongidae, are as follows:—(1) Australopithecus showed modifications of his skeleton—especially the pelvis, femur, ankle and foot—which permit us to infer that he walked upright, even though such modifications had not progressed as far as in hominids of the genus Homo.(2) The calvaria or brain-case of Australopithecus was characterized by a number of hominid features, such as marked flexion of the axis of the cranial base; forward displacement of the occipital condyles by which the skull articulates with the vertebral column; a small, low nuchal area at the back of the base of the cranium, for the attachment of those muscles which tether the back of the cranium to the trunk—the last two features suggesting a different, more man-like poise of the cranium on the spine; the consistent development, early in life, of a pyramidal mastoid process as in man, and unlike the apes in which this process develops inconsistently and then only later in life (Schultz 1950).(3) The canine teeth of Australopithecus, like those of Homo, lacked the enlargement and marked interlocking which characterizes the upper and lower teeth of the apes—correspondingly, Australopithecus lacked the diastemata or gaps which, in apes, lodge the projecting tips of the enlarged canines.(4) Another dental characteristic shared by Australopithecus with Homo was the bicuspid structure of the first lower premolar tooth: in apes, this tooth does not possess two sub-equal cusps but is a cutting or sectorial tooth with one predominating cusp, like a canine tooth.(5) Although the brain-size of Australopithecus (as inferred from the volumetric capacity of the brain-case) was no bigger than that of some largerbrained apes, the shape or morphology of the brain, as preserved in endocranial casts, approached more closely to that of early Homo than to that of the apes. We have, however, no direct evidence whether these external observable differences between the brains of Australopithecus and of apes were paralleled by internal, microscopic, structural differences such as those which have been demonstrated between modern man and modern apes.(6) Many other detailed morphological features of the skull, the teeth and other bones of Australopithecus showed human resemblances.


1987 ◽  
Vol 6 (1) ◽  
pp. 4-11
Author(s):  
A. Spies

Dating the Pleistocene and also the Ice Ages is necessary. A period of “normal” magnetism, called the Olduvai Event, occurred about 1,8 m.y.a. It can be considered the boundary between the Pliocene and the Pleistocene, lying within the Matuyama Reversed Epoch, which ended some 700 000 y.a. The boundary between the Middle and Upper or late Pleistocene we shall accept as 125 000 y.a., which is also the beginning of the Eemian interglacial. Hominid fossils were discovered in both Java and China. From publications the names “Peking Man” and “Java Man” are well known. Today, these are referred to as Homo erectus. They are known by their very prominent supraorbital torus and postorbital constriction, alveolar prognathism and receding chin. With the widest part of the skull toward the bottom, it has a pentagonal shape. The rest of the skeleton is very little different from the modern skeleton. Fossil bones from Europe are scarce, but the little that have been found correspond with Erectus from the Far East. They date from the Middle Pleistocene.


Author(s):  
Dasapta Erwin Irawan ◽  
Rubiyanto Kapid

Abstract The northern part of the East Java Basin has become a focus of research by earth scientists, among others, because of the existence of hominid fossils and remains of other vertebrate taxa within the Quaternary sedimentary sequence. Fossil-bearing layers are found in the Kendeng Zone, mostly within the well-known Pucangan and Kabuh Formations, which are distributed from Central to East Java. However, not all formations contain vertebrate fossils as well as hominid elements. It is important to consider what factors may have influenced the concentration of vertebrate fossils in those formations. In this study, we describe sedimentary facies at three key field locations: Sangiran, Ngawi, and Mojokerto. Our study indicates that vertebrate remains and hominid fossils mainly accumulated in continental sediments associated with lacustrine and fluvial systems. In this regard, Sangiran and Ngawi B offer the greatest prospect for yielding hominid remains, owing to their unique paleoenvironmental and paleogeographical settings as a highland during the Early–Middle Pleistocene period. Certain parts of the Kabuh Formation in the Mojokerto region also hold high potential, especially those displaying evidence of continental deposition.


1991 ◽  
Vol 35 (B) ◽  
pp. 1165-1173
Author(s):  
A. M. Kinyua ◽  
T. Plummer ◽  
N. Shimizu ◽  
W. Melson ◽  
R. Potts

AbstractXRF and Ion mfcroprobe analyses of fossils of known and uncertain provenance from the Lower-Middle Pleistocene locality of Kanjera. Kenya, are reported. The goal of this study was to develop a nondestructive technique of provenancixig fossils, which could be applied to the Kanjera sample. The fossils of known provenance were collected in the excavations of the 1987 Smithsonian Expedition. Three fossils of uncertain provenance, two specimens of Theropithecus oswaldi and a hominid fossil, were analyzed as test cases.Both qualitative and quantitative XRF analyses of Kanjera fossils were carried out. In the qualitative analysis, the elemental peak areas from each fossil's XRF spectrum were calculated and normalized to the peak area of the incoherently scattered radiation. Results of the analysis showed that fossils from the Lower-Middle Pleistocene Kanjera Beds, for the most part, had higher levels of yttrium (Y) and zirconium (Zr) than those of the younger Apoko (Ap) Bed. black cotton soil (BCS) and modem bones (MD). The relative concentrations of uranium (U) v strontium (Sri and thorium (Th) were diagnostic of the Kanjera Bed of origin. These findings were confirmed by quantitative XRF and ion microprobe analyses of a subsample of Kanjera fossils. The T. oswaldi and hominid fossils had trace element concentrations suggestive of K2 and BCS provenances, respectively. These findings provide a framework for the qualitative XRF provenancing of other surface collected fossils from the locality.


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