Morphology of the Pliocene partial hominid skeleton (A.L. 288-1) from the Hadar formation,Ethiopia

The upper part of the Pliocene Hadar Formation, central Afar, Ethiopia, has yielded a 40% complete fossil hominid skeleton (A.L. 288-1, “Lucy”). This specimen is described in detail and selected measurements and illustrations are provided.     

Relationship of squamosal suture to asterion on external skull surfaces versus endocasts of pongids: Implications for Hadar early hominid AL 162-28

The relationship between the squamosal suture and asterion was quantified in 15 hemispheres of eight chimpanzee endocasts that were aligned in the conventional lateral view (i.e., with frontal pole [FP]–occipital pole [OP] horizontal). Using a three-dimensional digitizer, x, y, and z coordinates were collected for the highest and lowest points of the squamosal suture, and the most rostral point of the suture approximate to the coronal suture. Our results were compared to a similar study of the squamosal suture on the external surfaces of chimpanzee skulls that were oriented in the Frankfurt horizontal (Holloway and Shapiro, 1992). The relationship between the squamosal suture and asterion differs markedly between the outsides of skulls and endocasts. Whereas the squamosal suture is very rarely below asterion on the external skull, we found that most of the squamosal suture is located inferior to asterion on endocasts. We also found that the squamosal suture courses approximately 2.0 mm lower on the right side than the left. (An asymmetry of the same magnitude was reported for the external skull but, curiously, in the opposite direction.) It may be that a lowered right squamosal endosuture on chimpanzee endocasts is associated with earlier closure on that side. The discrepancy in results for the external skull versus endocast is partially attributable to orienting chimpanzee skulls in the Frankfurt horizontal, which usually results in the endocasts being tilted so that FP is above OP, i.e., FP-OP is not parallel with the Frankfurt horizontal. Falk's (1985) orientation of the early hominid endocast from Hadar (AL 162-28) is consistent with data determined from endocasts of chimpanzees. © 1994 Wiley-Liss, Inc.     

Geological summary of the Busidima Formation (Plio-Pleistocene) at the Hadar paleoanthropological site, Afar Depression, Ethiopia

The Hadar paleoanthropological site in Ethiopia preserves a record of hominin evolution spanning from approximately 3.45 Ma to 0.8 Ma. An angular unconformity just above the ca. 2.95 Ma BKT-2 complex divides the sediments into the Hadar Formation (ca. 3.8-2.9 Ma) and the Busidima Formation (ca. 2.7-0.15 Ma). The unconformity is likely a response to a major tectonic reorganization in the Afar Depression, and activation of the As Duma fault near the Ethiopian Escarpment (west of Hadar) created a half-graben in which the Busidima Formation was deposited. The pattern and character of sedimentation in the region changed dramatically above the unconformity, as cut-and-fill channel conglomerates and silt-dominated paleosols that comprise the Busidima Formation stand in sharp contrast to the underlying deposits of the Hadar Formation. Conglomerate deposition has been related to both the perennial, axial paleo-Awash and ephemeral, escarpment-draining tributaries. Overbank silts have yielded fossils attributed to early Homo and Oldowan stone tools. Numerous tuffaceous deposits exist within the Busidima Formation, but they are often spatially limited, fine-grained, and reworked. Recent work on the tephrostratigraphic framework of the Busidima Formation at Hadar has identified at least 12 distinct vitric tephras and established the first geochemical-based correlations between Hadar and the neighboring project areas of Gona and Dikika. Compared to Gona and Dikika, where Busidima Formation sediments are exposed over large areas, the highly discontinuous sediments at Hadar comprise less than 40 m in composite section and are exposed over an area of <20 km², providing only snapshots into the 2.7-0.15 Ma window. The stratigraphic record at Hadar confirms the complex depositional history of the Busidima Formation, and also provides important details on regional stratigraphic correlations and the pattern of deposition and erosion in the lower Awash Valley reflective of its tectonic history.     

Predictive models for reduction of Salmonella Hadar on chicken skin during single and double sequential spraying treatments with acetic acid

AIMS: The response surface methodology was used to evaluate the effect of acetic acid concentration, spraying time and temperature on the reduction of Salmonella Hadar on poultry skin in a laboratory spraying process, and to identify the best conditions required to develop this operation. METHODS AND RESULTS: A comparative analysis was carried out to ascertain the effects of the application of single (SS) and double sequential decontamination (DSS) treatments on skin samples inoculated with Salm. Hadar. While on the SS treatment, the linear and quadratic acid concentration terms and the interaction of the temperature and time term of the model are statistically significant at P < or = 0.001, P < or = 0.01 and P < or = 0.05, respectively, the other terms do not significantly affect (P > 0.05) the reduction of Salm. Hadar. On the DSS model the acid concentration and time linear terms significantly affected (P < or = 0.001 and P < or = 0.01) the Salm. Hadar reduction within the experimental range assayed. CONCLUSION: Any of the models could be used as an approach to optimize spray washing during chicken processing. SIGNIFICANCE AND IMPACT OF THE STUDY: Neither the SS or the DSS treatment has the capability of eliminating Salm. Hadar from carcasses. However, reductions of approx. 99% initial load could be attained if DSS treatment were put into practice.     

Revision of the subspecies ofAustralopithecus africanus (primates: Hominidae), including a new subspecies from the late pliocene of Ethiopia

The subspecies ofAustralopithecus africanus Dart, 1925 have been revised in a morphological and statistical analysis. Four subspecific names were previously proposed, but only one was found to be valid. The subspeciesA. africanus transvaalensis (Broom, 1936), from the Plio/Pleistocene of South Africa, cannot be sustained due to an insufficient sample, and is combined with the nominate race,A. a. africanus. The type ofA. africanus afarensis Tobias, 1980 is a mistake in identification and notA. africanus, but a pongid. The population ofA. africanus from the late Pliocene of Ethiopia does indeed represent a relatively small-toothed geographical race for which the nameA. africanus aethiopicus was conditionally proposed; and the lectotype for it, A.L. 288-1, is notA. africanus, but the type ofHomo antiquus Ferguson, 1984. The trinominalaethiopicus is thus unavailable for the Ethiopian race, which is redescribed as a new subspecies,A. africanus miodentatus n. ssp., and the mandible A.L. 266-1 is designated as the holotype.     

Reconstruction and re-evaluation of the skull ofHomo antiquus (hominoidea: Homininae) from Hadar

The skull ofHomo antiquus Ferguson, 1984, represented by cranial remains of a fossilized skeleton, A.L. 288-1, from the Plio/Pleistocene of Hadar in Ethiopia, is reconstructed and the procedure described. Re-evaluation of the skull shows that it is apparently the smallest, normal, unequivocal hominid skull known; and that its cranial morphology is not Australopithecine, but Hominine.     

Hominid environments at Hadar from paleosol studies in a framework of Ethiopian climate change

The amount and seasonal distribution of paleo-rainfall is a major concern of paleoanthropology because they determine the nature of the vegetation and the structure of the ecosystem, particularly in eastern Africa. The δ¹⁸O and δ¹³C of paleosol carbonates are quantitative proxies of these critical features of the paleoenvironment. The Afar region of Ethiopia lies between the African and Indian summer monsoons, and is prone to profound climate change. In the western Afar, the dominant paleoenvironment of the Hadar Formation during the late Pliocene was a major meandering river's distal low, flat floodplain, on which muds accreted that were continuously transformed into vegetated soils with Bk horizons rich in CaCO₃. The mean δ¹³C of paleosols throughout the Hadar Formation translates to an average vegetative cover across the extensive floodplain of about 30% of the C₄ grasses and 70% of unspecified C₃ plants. The character of the paleosols, such as the one at Locality 333, and their δ¹⁸O_Carbonate argue for a highly seasonal rainfall of about twice today's amount, implying that the C₃ plants were mostly sizeable trees and that the biome for Australopithecus afarensis was a grassy woodland. The amount of grasses abruptly increased in the lower Busidima Formation with its early Homo and artifacts to a more open grassy woodland of ca. 50% grasses. However, this transition in δ¹³C is not mirrored in the δ¹⁸O, which persists at a quite negative average value of −6.4‰ over the entire >2-Myr duration of both formations. This value for the carbonate means that the paleosoil water was a quite negative −4.1‰, a significant 5‰ more negative than our estimate of modern rain at Hadar. We put the negative δ¹⁸O of paleo-Hadar's rainfall into an isotopic framework of the dynamic history of climate change in sub-Saharan northern Africa. There have been two end-member climate regimes: (1) an earlier persistently pluvial Pliocene regime, with its strong summer monsoon, as registered in the Hadar Formation; and (2) the modern cyclical, mostly arid regime that began ca. 1 Myr ago, which has been punctuated by about ten cyclically predictable brief millennia-long pluvial episodes. The best known pluvial of the latter regime is the latest one, the African Humid Period (AHP), just 9.0-6.5 kyr ago, whose δ¹⁸O_Rainfall matches that for paleo-Hadar. The known climatological factors that brought on the AHP are probably the same ones that were persistently present for the Afar of the Pliocene. This dynamic rainfall history undoubtedly has influenced hominid occupation of the keystone Afar area at the gateway out of, and into, Africa.     

Reassessing manual proportions in Australopithecus afarensis

Previous analyses of hand morphology in Australopithecus afarensis have concluded that this taxon had modern human‐like manual proportions, with relatively long thumbs and short fingers. These conclusions are based on the A.L.333 composite fossil assemblage from Hadar, Ethiopia, and are premised on the ability to assign phalanges to a single individual, and to the correct side and digit. Neither assignment is secure, however, given the taphonomy and sample composition at A.L.333. We use a resampling approach that includes the entire assemblage of complete hand elements at Hadar, and takes into account uncertainties in identifying phalanges by individual, side and digit number. This approach provides the most conservative estimates of manual proportions in Au. afarensis. We resampled hand long bone lengths in Au. afarensis and extant hominoids, and obtained confidence limits for distributions of manual proportions in the latter. Results confirm that intrinsic manual proportions in Au. afarensis are dissimilar to Pan and Pongo. However, manual proportions in Au. afarensis often fall at the upper end of the distribution in Gorilla, and very lower end in Homo, corresponding to disproportionately short thumbs and long medial digits in Homo. This suggests that manual proportions in Au. afarensis, particularly metacarpal proportions, were not as derived towards Homo as previously described, but rather are intermediate between gorillas and humans. Functionally, these results suggest Au. afarensis could not produce precision grips with the same efficiency as modern humans, which may in part account for the absence of lithic technology in this fossil taxon. Am J Phys Anthropol 152:393–406, 2013. © 2013 Wiley Periodicals, Inc.