The significance of the fossil hominid skull from Petralona,Greece

Evidence is accumulating that the hominid cranium found in the Petralona cave in 1960 is associated with cave deposits of middle Pleistocene age. If this is so, the fossil is the most complete middle Pleistocene cranium yet discovered and provides important morphological, metrical and radiographic information on the possible evolutionary transition from Homo erectus to Homo sapiens. The classification of the specimen is discussed and it is suggested that a grade system within Homo spaiens should be erected. The Petralona fossil would be allocated to Homo sapiens grade 1 rather than to Homo erectus or to a subspecies of Homo sapiens.     

Possible evidence of bone tool shaping by Swartkrans early hominids

Ever since Dart (J. Phys. Anthrop. 7 (1949) 1) interpreted certain bones from Makapansgat as tools, scientific consensus has fluctuated as to whether some bone objects from early hominid sites should be interpreted as artefacts, or the result of non-human taphonomic processes, which are known to produce pseudo-bone tools morphologically similar to human modified or used artefacts. Here we present possible evidence of bone tool shaping from Swartkrans (Members 1–3; ca. 1.8–1.0 Mya). Four horncores and the proximal end of an ulna used as tools in digging activities also have facets covered by parallel spindle-shaped striations characteristic of grinding. Identification of these traces as possibly resulting from deliberate shaping or re-sharpening of the bone tools is based on the characterisation of the use-wear pattern and other taphonomic modifications observed on the Swartkrans bone tools. This interpretation is also supported by the study of the remainder of the horncores from Swartkrans, horncores from other southern African Plio-Pleistocene sites (Sterkfontein, Makapansgat, Gondolin), modern horncores affected by pre- and post-mortem modification, ethnographic, LSA, African Iron Age and experimental bone tools shaped by grinding. These data suggest that early hominids had the cognitive ability to modify the functional area of bone implements to achieve optimal efficiency.     

A Case of Marked Bilateral Asymmetry in the Upper Limbs of an Upper Palaeolithic Male from Barma Grande (Liguria), Italy

Barma Grande 2, a male skeleton of upper palaeolithic age from Balzi Rossi (Liguria, Italy), shows a marked degree of upper limb bilateral asymmetry. Similar cases of asymmetry in palaeolithic hominid fossils have variously been attributed to high levels of behavioural asymmetry (related to handedness) or a pathologically induced alteration of upper limb skeletal remodelling processes. As in many of these cases, the skeleton from Barma Grande lacks any indications of trauma or pathology in the smaller left limb. Consideration of the morphology of the preserved upper limb elements and a comparative analysis of asymmetry in normal and pathological male palaeolithic fossils and normal recent human samples suggests that the asymmetry in Barma Grande 2 was a secondary effect of trauma or pathology in the left side. The degree and pattern of asymmetry in numerous humeral and ulnar measurements indicates an adult onset of altered loading patterns. Several possible aetiological factors are considered, with the most probable being an entrapment neuropathy, direct trauma to one or more muscles about the shoulder, or possibly glenohumeral joint instability. © 1997 by John Wiley & Sons, Ltd.     

Preliminary evidence for seasonal deposition patterns from member 2 of the Swartkrans hominid site,South Africa

Frequencies of specimens in juvenile age classes, based on an analysis of tooth eruption and wear sequences, in specimens of an extinct species of springbok, Antidorcas bondi Wells and Cooke, from Member 2 of the Swartkrans hominid site, suggest that the remains of this animal were deposited during summer months. These indications of seasonal activity may offer support for previous suggestions of annual game movements. Such periodic movements have implications for our understanding of the behaviour patterns of the animals, including perhaps the hominids, which are represented in the assemblages from Swartkrans and other sites in the vicinity.     

Two Careers across Two Cultures

Beginning with my recollection of hearing C. P. Snow's ‘Two Cultures’ lecture, I sketch my experience of building two academic careers in succession, first in one of the natural sciences and later in the history of such sciences. I outline both the difficulties and the rewards that I encountered in crossing the alleged gulf between the sciences and the humanities, but also emphasise the diversity of cultures that I experienced within each. I describe my own encounter with the academic culture of continental Europe, within which the concept of a monolithic singular ‘Science’ could be dismissed as an ‘anglophone heresy’, and viewed from which the Two Cultures debate could seem both provincial and redundant.     

Mobility, competition, and Plio-Pleistocene hominid foraging groups

Evidence for carcass access times and levels of early hominid mobility is synthesized using studies of carnivore ethology and theories of interspecific competition to arrive at tentative conclusions about the organization of Plio-Pleistocene hominid foraging groups. The model presented suggests that group foraging tactics, in combination with high mobility, are central to successful confrontational scavenging (interference competition), whereas individual foraging tactics and high mobility are central to successful nonconfrontational scavenging (exploitative competition). In contrast, group or individual foraging tactics and low mobility characterize the acquisition of fresh carcasses in low-competition contexts. Individual foraging tactics and low mobility are employed in response to extreme competition over marginal resources. Preliminary tests with data from Bed I Olduvai Gorge and Koobi Fora suggest that Plio-Pleistocene hominids, like other large-bodied predators, employed flexible foraging tactics involving changes in group size and levels of mobility to gain access to carcasses in both low-and high-competition contexts.     

A new early Silurian brachiopod genus,Thulatrypa, from Norway and South China,and its palaeobiogeographical significance

Huang, B., Baarli, B.G., Zhan, R.B. & Rong, J.Y., October 2015. A new early Silurian brachiopod genus, Thulatrypa, from Norway and South China, and its palaeobiogeographical significance. Alcheringa 40, xxx–xxx. ISSN 0311-5518.

The smooth atrypoid brachiopod Thulatrypa gen. nov. incorporates two species, a younger (T. gregaria) from Norway, and an older (T. orientalis) from South China, which collectively span the middle Rhuddanian through Aeronian. In Baltica, the genus thrived just below the storm wave base in a tropical BA4 setting extending slightly into BA3 and BA5 respectively, whereas in South China, its representative occurs in a much shallower assemblage (BA2–3). Their palaeobiogeographical implications are carefully investigated. This study supports the arguments that Thulatrypa may have originated in South China in the middle Rhuddanian and extended its range to eastern Baltica in the late Rhuddanian. Larvae may have drifted along a channel from the east to the southwest of Baltica, which supports the reconstructions of palaeocurrents in the early Silurian in previous palaeogeographical studies.

Bing Huang [bhuang@nigpas.ac.cn], Ren-bin Zhan [rbzhan@nigpas.ac.cn] and Jia-yu Rong [jyrong@nigpas.ac.cn], State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, 39 East Beijing Road, Nanjing, 210008, PR China; B. Gudveig Baarli [gudveig.baarli@williams.edu], Department of Geosciences, Williams College, Williamstown, MA 01267, USA.     

Palaeontology of the Chatham Islands,SW Pacific—a review

Despite their small area, the Chatham Islands host diverse and abundant fossils. Fossil assemblages of Permian to Late Cretaceous age preserved in terrestrial to shallow marine deposits represent the only record of plants and animals that once inhabited the eastern extension of Zealandia. Lower Cenozoic sediments have yielded a shallow marine fauna, including a rich molluscan assemblage linked to the oceanic inundation of this landmass. The late Cenozoic biota documents the re-emergence of the Chatham Islands and the establishment of major oceanic currents, which meet along the Chatham Rise. This review summarizes the fossil record of the Chatham Islands and the Chatham Rise, integrating data from published and unpublished sources.