Social integration on the Upper Canadian frontier: elements of community in Essex County 1790–1850

Individuals settling new areas have had to rely on a variety of resources, including the social structures inherent in their culture. This study focuses upon the elements of family, kinship and origin in part of nineteenth-century Ontario. It approaches them from the perspectives of interaction over distance and of sociological institution, the particular institution being that of land conveyancing. Data drawn from the surviving parts of the personal and agricultural schedules of the Census of Canada for 1851/52 were searched for the propinquity of individuals to one another. Social interaction seems to have occurred within two miles for most people. Random samples and a series of t-tests suggest that there were no differences in proximity for the members of the different cultural groups but that there were differences between immigrant and established groups with respect to the desires of kin for proximity to one another. These differences were paralleled by differences in the structure of the family. Kinship was also important in determining to whom land was sold; most sales occurred within the particular community. That this was so suggests, according to the model of Steeves, that the level of integration in mid-century Essex was simply embryonic.     

The bovids from Elandsfontein,South Africa,and their implications for the age,palaeoenvironment, and origins of the site

The bovid fossils from Elandsfontein, south-western Cape Province, South Africa, comprise 7257 individually numbered specimens from 18 species. Taxonomic comparisons with Olduvai Gorge and other African sites and the high percentage of extinct forms imply that the bones accumulated in the earlier part of the Middle Quaternary, probably sometime between 700,000 and 400,000 years ago. By extension, this is also the most likely age for the skull cap of archaicHomo sapiens (Saldanha Man) and for the occasional late Acheulean stone artifacts that accompany the animal bones. In keeping with geomorphological observations and other aspects of the fauna, the bovids indicate a relatively grassy and moist environment, apparently during an interglaciation that differed significantly from the Holocene. Geomorphological context, the frequent occurrence of partial skeletons, bone damage, and skeletal part representation suggest that carnivore feeding on carcasses scattered across a Mid-Quaternary land surface was probably the main factor shaping the Elandsfontein bone assemblage. Porcupines may also have played a role, but there is little evidence for human activity. The Elandsfontein assemblage thus provides a useful control for comparison with bone accumulations where context, associations, and bone damage indicate that people were heavily involved. For example, there are very few young animals in the otherwise attritional profile of giant buffalo from Elandsfontein, probably because carnivores often rapidly and completely consumed young carcasses. This suggests that few young carcasses would be available for human scavenging and thus that archaeological attritional profiles in which young individuals are common probably reflect active human hunting, at least of young animals.

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Résumé Les fossiles de bovidés d'Elandsfontein, sud-ouest de la Province du Cap, Afrique du Sud, comportent 7257 spécimens numérotés appartenant à 18 espèces. Les comparaisons taxonomiques avec Olduvai Gorge et d'autres sites africains, ainsi que le haut pourcentage de formes éteintes, indiquent que les os ont dû s'accumuler durant la partie la plus ancienne du Quaternaire moyen, probablement entre 700,000 et 400,000 ans. Par extension, il semble que ce soit aussi l'âge le plus probable de la calotte cranienne d'une forme archaïque d'Homo sapiens (l'homme de Saldanha) ainsi que des quelques outils de l'Acheuléen récent qui accompagnaient les ossements d'animaux. En accord avec les observations géomorphologiques et d'autres aspects de la faune, les bovidés indiquent un environnement relativement humide et herbeux, évidemment durant un interglaciaire qui differe de façon significative de l'Holocène. Le contexte géomorphologique, la présence fréquente de squelettes incomplets, les os endommagés et les parties du squelette représentées suggèrent que des carnivores se nourrissaient des carcasses dispersées sur un terrain du Quaternaire moyen sont le principal facteur de la formation de l'assemblage osseux d'Elandsfontein. Les porc-épics ont peut-être aussi joué un rôle, mais il y a peu de signes de l'activité humaine. L'assemblage d'Elandsfontein est donc un témoin utile pour des comparaisons avec d'autres accumulations de faune, dans lesquelles le contexte, les associations et l'état des os indiquent que les hommes y ont joué un rôle important. Par exemple, très peu d'animaux jeunes sont représentés dans le profil par ailleurs attritionel du buffle géant d'Elandsfontein, probablement parce que les carnivores dévoraient souvent rapidement et entièrement les carcasses jeunes. Ceci indique que très peu de carcasses jeunes étaient disponibles pour les charognards humains et que les profils archéologiques attritionels dans lesquels les animaux jeunes sont fréquents reflètent probablement une chasse humaine active, tout au moins d'animaux jeunes.