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One Hundred Years of Separation: The Historical Ecology of a South African ‘Coloured Reserve’

Published online by Cambridge University Press:  19 May 2011

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Abstract

During the twentieth century, the 20,000 hectares commons surrounding the village of Paulshoek as well as the neighbouring privately-owned farms have been significantly influenced by evolving land-use practices driven largely by socio-economic and political change in the broader Namaqualand and South African region. Land-use practices in the communal lands of Namaqualand were based initially on transhumant pastoralism, then on extensive dryland cropping associated with livestock production under restricted mobility, and more recently on a sedentarized labour reserve where agricultural production now forms a minor part of the local economy. For the first half of the twentieth century, farmers on communal and privately-owned farms shared similar transhumant pastoral practices and both moved across unfenced farm boundaries. By the middle of the century, however, fence-lines were established and commercial farming on privately-owned farms was increasingly managed according to rangeland science principles. As the population grew in the communal areas, families gravitated to new ‘service’ villages such as Paulshoek and became increasingly dependent on migrant labour and state welfare. While the majority of former croplands are now fallow, many of them for decades or more, communal livestock populations have remained relatively high, fluctuating with rainfall. The impact of this history of land use can be compared with that of neighbouring privately-owned farms where low stocking rates, coupled with a variety of state subsidies, have had a very different environmental outcome. This article charts the environmental transformations that have occurred in the area of Paulshoek as a direct result of the region's political history and the evolution of the regional economy. We present a variety of evidence drawn from archival sources, oral history, repeat aerial and ground photography, and detailed climate, cropping and livestock records to show that events far beyond the borders of Namaqualand's communal areas have had a profound influence on their environments.

Au cours du vingtième siècle, les 20,000 hectares de terrains communaux qui entourent le village de Paulshoek, ainsi que les fermes privées environnantes, ont été fortement influencés par l'évolution des pratiques d'utilisation des terres, largement déterminée par les changements socioéconomiques et politiques survenus dans la région du Namaqualand et plus largement en Afrique du Sud. Les pratiques d'utilisation des terres sur les terres communales du Namaqualand reposaient initialement sur le pastoralisme transhumant, puis sur la culture sèche intensive associée à la production de bétail avec mobilité limitée, et plus récemment sur une réserve de main-d'œuvre sédentarisée avec une production agricole qui ne représente plus qu'une faible partie de l'économie locale. Pendant la première moitié du vingtième siècle, les exploitants de terrains communaux et les exploitants de fermes privées avaient des pratiques pastorales transhumantes similaires et tous deux traversaient des terrains non clôturés. Pendant la seconde moitié du siècle, en revanche, les clôtures étaient posées et la gestion de l'activité agricole commerciale dans les fermes privées répondait de plus en plus à des principes de science des pâturages. Au fur et à mesure de l'accroissement de la population dans les zones communales, les familles ont gravité vers les nouveaux 〈villages services〉comme Paulshoek et leur dépendance vis-à-vis de la main-d'œuvre migrante et de la protection sociale de l'État s'est accrue. Alors que la majorité des terres de culture sont aujourd'hui en jachère, et ce depuis des décennies pour certaines, les populations de bétail communal sont restées relativement élevées, variant selon les précipitations. On peut comparer l'impact de l'histoire de l'utilisation de ces terres avec celui des fermes privées voisines dont la faiblesse des taux d'exploitation du bétail, associée aux subventions publiques diverses, a eu des conséquences très différentes sur l'environnement. Cet article retrace les transformations environnementales survenues dans la région de Paulshoek en conséquence directe de l'histoire politique de la région et de l'évolution de l'économie régionale. À partir de données variées issues d'archives, de l'histoire orale, de photographies aériennes et au sol répétées, ainsi que de registres détaillés du climat, des récoltes et de l'exploitation du bétail, il montre que des événements situés bien au-delà des zones communales du Namaqualand ont eu une influence profonde sur l'environnement.

Information

Type
Research Article
Copyright
Copyright © International African Institute 2008
Figure 0

Figure 1 Namaqualand is a relatively poorly defined geographic region in the north-west of South Africa covering about 50,000 square kilometres and straddling two provinces. It stretches from the Orange River in the north to the Olifants River, just south of Van Rhynsdorp, in the south and about 100 to 150 kilometres inland from the Atlantic seaboard. Most of the region prior to 1994 was held under private tenure but several communal reserves (shaded areas) formed discrete islands in the landscape. Paulshoek forms the south-eastern section of the Leliefontein communal reserve

Figure 1

Figure 2 Stockposts within the Paulshoek commons have been a persistent feature of the landscape during most of the twentieth century. The upper photograph was taken by Mr A. J. Andrews in 1938 before the creation of the village of Paulshoek, when most families would have been dispersed in small groups and alternated between seasonal croplands and grazing areas. Today (lower photograph taken 1 March 2004), although building materials have changed, such structures remain movable and semi-permanent

Figure 2

Figure 3 Transhumance routes of Nama livestock keepers in (a) Namaqualand during pre-colonial era c. 1700 (upper map); (b) Leliefontein mission station and reserve during the nineteenth century (centre map); and (c) Paulshoek (and other villages of Leliefontein) today (lower map)

Figure 3

Figure 4 The Kleinfontein school house in 1938 (top photograph) and 1998 (lower photograph). Prior to the creation of Paulshoek the area was heavily impacted by grazing and cropping. Sixty years later there has been little change in ground cover or species composition, due to continued heavy utilization. (Photos by A. J. Andrews and the authors)

Figure 4

Figure 5 The number of large stock units (LSU) in the magisterial district of Namaqualand between 1860 and 1996

Figure 5

Figure 5b Large stock units in Leliefontein Communal Area, 1824–2002

Figure 6

Figure 6 Rainfall (bars) and sheep and goat numbers in Paulshoek for the period 1971–2004. These two variables are related by the following relationship: y = 12.62x + 01133.7 (where y = number of animals in any one year and x = previous year's annual rainfall total) (n = 26; r2 = 0.4217; p < 0.001)

Figure 7

Figure 7 Aerial photographs of the boundary between Paulshoek commonage (upper half of photograph) and Rooiwal private farmland (lower half of photograph). The 1960 image was taken two years after the fence was first erected and shows that grazing had a severe impact on both areas, indicated by the low vegetation cover. Thirty-seven years later, recovery on the Rooiwal side of the fence has occurred due to reduced stocking rates, while little change is evident in the communal area.

Figure 8

Figure 8 (Top photograph taken in 1937, bottom photograph taken in 2005) This stock post has been in continuous occupation since 1937. The invasion of short-lived non-palatable perennials (Galenia africana) is indicative of ecological processes that have occurred throughout the landscape of Paulshoek in disturbed sandy areas during recent decades. Note the persistence of the low dark trees (Rhus undulata) in the rocky areas. These are the most highly valued source of firewood – this image illustrates the sustainable use of this resource. (Photos: A. J. Andrews and the authors)

Figure 9

Figure 9 (Top photograph taken in 1938, bottom photograph taken in 1999) Kleinfontein – threshing floor, croplands and rocky uplands. Note the transformation of the fallow croplands in the mid-ground. Much of this consists of non-palatable perennials (like Galenia africana), although there is some recruitment of long-lived palatable shrubs, indicating that recovery is possible as land-use intensity declines over long timeframes. (Photos: A. J. Andrews and the authors)