systems and the physiognomy, demography and phenology of karoo plants. Secondly,
it characterizes the floristics, structure and dynamics of three subropical
thicket communities and a karroid shrubland community along an environmental
gradient in the lower Sundays River Valley, south eastern Cape. Both objectives
fall within the overall aims of the Karoo Biome Project of which this study is
part. From the two reviews, I conclude that most research in the semi-arid
Karoo has stalled in the descriptive phase and there has been little emphasis on
the demographic responses of plants to the stochastic events which characterize
this region. In addition, current views of the dynamics of karoo communities
are steeped in paradigms which consider the Karoo to be composed of relatively
stable populations. I present evidence that this may not be the case and
suggest that such views are thus probably unable to provide the necessary
insights to manage this resource effectively. Similarly, the rationale for
existing management systems consists mostly of untested or untestable statements
and there is a lack of critical investigation in the published literature. In
the gradient analysis study I show that the lower Sundays River Valley is
characterized by a complex gradient of increasing aridity. Rainfall
predictability, the occurrence of relatively severe night frosts and low plant
available water status of the Karoo are probably the chief factors which delimit
the boundary between this dwarf shrubland and the subtropical thicket
communities in the eastern Cape. I show that under sustained grazing pressure,
karroid species typical of the Central Lower Karoo, invade subtropical thicket
communities but this appears confined to the Noorsveld, a veld type adjacent to
it. There is not a wide-spread invasion of karroid elements into the Sundays
River Scrub and Addo Bush. Diversity within the lower Sundays River Valley
vegetation is not correlated with phytochorological or structural diversity and
there is no increase in the middle part of the gradient as has been reported in
a number of other studies. I confirm most of the earlier views concerning the
phytochorology of the eastern Cape flora. However, I present evidence to show
that the subtropical thickets may have been present in the eastern Cape for much
longer than previously suggested. An analysis of the phenology of the
subtropical thicket and karroid shrubland vegetation shows that the Karoo may
follow a "pulse-activity" response to a relatively unpredictable moisture
supply. This differs from current views of karoo dynamics which emphasize the
seasonal specialization of growth forms. Finally, I discuss the main findings
of this study in the light of the hypotheses tested and generated and I suggest
possible future research directions.
Reprint : In File,
Keywords : EASTERN CAPE; POPULATION; RAINFALL; GRAZING EFFECTS; PLANT
PHYSIOLOGY; SUCCULENT KAROO; VEGETATION DYNAMICS; VELD MANAGEMENT; BUSH
ENCROACHMENT; BIODIVERSITY; CLIMATE CHANGE
Ref ID : 44
1109. Hoffman, M.T. Is the Karoo spreading? Veld & Flora 77(1):4-7, 1991.
Reprint : In File,
Keywords : KAROO DESERTIFICATION; ENVIRONMENTAL HISTORY; NAMA KAROO; GRASSLAND;
DESERTIFICATION ASSESSMENT; VEGETATION CHANGE; RAINFALL
Notes : The author concludes that matched photographs and survey data indicate
that there is no evidence to suggest that the Karoo is steadily expanding its
range into the southern OFS grasslands, at least not at a predictable annual
rate. On the contrary, the opposite was found to be the case. (It is not
suggested, however, that the grasslands are "invading" the Karoo). There are,
however, alternative explanations. The semi-arid eastern Karoo is characterised
by large fluctuations in grass cover, determined mostly by the amount of summer
rainfall. On the other hand it is suggested that there is no change in the
Karoo and southern OFS vegetation apart from cyclical fluctuations which occur
over decades. Unfortunately, the validity of any one of a number of theories of
vegetation change in the eastern Karoo will only be decided by long-term
research, if at all. Such a venture, however, is costly and would yield few
immediate rewards. Perhaps because of this we may not receive a definitie
answer for some time to come.
Ref ID : 1069
1110. Hoffman, M.T. The potential value of historical ecology to environmental
monitoring. Paper presented at a conference on "Monitoring requirements for
fynbos management", 16-17 March 1993, Swellendam. 1993.
Reprint : In File,
Keywords : ENVIRONMENTAL HISTORY; MONITORING; GLOBAL CHANGE; ARCHAEOLOGY;
SOUTHERN AFRICA; STOCKING RATE; BOTANICAL SURVEY
Abstract : The current world-wide focus on global change has led to a co-
incident upsurge in the study of environmental history. This link between the
two is important since it allows researchers to better assess the rate and
extent of current and future changes in the light of past changes. Historical
environmental monitoring demands a synthetic approach to understanding landscape
change. It uses information from a wide range of diciplines including
palynology, archaeology, anthropology, geography, geology, history, ecology and
many more. The focus of this paper is to review the main historical sources and
tools that have and could be used to understand vegetation and landscape change
in southern Africa during the last two hundred years and in particular during
the last hundred years. Some examples of studies, which have used a variety of
hisorical documents such as land grant documents, Field Cornet's reports,
traveller's records, stocking rate records and newspaper reports, are listed.
The value and limitations to the information retrieved from such material is
discussed. Similarly, the value and use of botanical survey data is noted. A
main emphasis of this review is to highlight the value of using a Markov
modelling approach in the study of ground and aerial photograph interpretation
of landscape change. Finally, it is suggested that a study of landscape change
in southern Africa would benefit from as broad-based an historical approach as
possible and would include a wide variety of disciplines, sources and
techniques. However, the establishment of clear theoretical expectations,
hypotheses and questions based on a literature search of the problem, prior to
investigation, is crucial if success in historical enviornmental monitoring is
to be achieved.
Ref ID : 238
1111. Hoffman, M.T. Environmental history and the desertification of the Karoo,
South Africa. Giornale Botanico Italiano 129(1):261-273, 1995.
Reprint : In File,
Keywords : ENVIRONMENTAL HISTORY; VEGETATION CHANGE; DESERTIFICATION ASSESSMENT;
KAROO DESERTIFICATION; NAMA KAROO; GRASSLAND
Abstract : This paper reviews the desertification debate in South Africa and
emphasizes the methods that have been used to understand the environmental
history of the semi-arid rangelands in the eastern Karoo during the last 500
years. These mixed grass/dwarf shrub rangelands, with mean annual rainfall
totals typically between 300-400mm, are described and the main driving variables
discussed. A brief historical account of the European settlement of the region
is also presented. The desertification debate has focussed on three main issues.
Firstly, because arid and semi-arid lands appear to be heavily influenced by
climate, the changing climatic regime during the Holocene and particularly
during the last two hundred years has been the subject of intensive
investigation. While all studies conclude that there is no evidence in the
historical record to support the popular perception that rainfall totals have
decreased this century, the question of changing rainfall seasonality has not
been adequately explored. Although mean annual temperatures over the last 50
years have not changed there have been significant increases in mean monthly
maximum temperatures and significant decreases in mean monthly minimum
temperatures for some of the stations investigated. The second issue of great
interest in the South African desertification literature is that of the nature
of pre-conlonial environments. A wide variety of archaeological, historical and
ecological techniques have been used, including analyses of fossil mammal bones
in owl pellets, fossil pollen in hyrax middens, notes from fossil mammal bones.
While all authors agree that the eastern Karoo was more grassy at some stage in
the past there is disagreement as to both the timing and cause of the changes to
a more shrubby vegetation. The final issue of great concern to the
desertification debate in South Africa concerns the rate of change during the
last 100 years. Satellite imagery, matched ground and aerial photography, survey
data and an analysis of historical stock records cannot agree as to whether the
Karoo is degrading or not. Certainly, the classic view of an annually expanding
desert margin has been replaced in recent years by a more realistic
understanding of the seasonal dynamics of the vegetation. The recent trend to
detailed modelling of the demographic process in key species holds much promise
for our undestanding of the degradation process. The vibrant community of
researchers, employing a range of archaeological, historical and ecological
techniques, will make important contributions to South Africa's National Action
Plan to Combat Desertification.
Ref ID : 249
1112. Hoffman, M.T. Human impacts on vegetation. In: Vegetation of Southern
Africa. edited by Cowling, R.M., Richardson, D.M., and Pierce,
S.M.Cambridge:Cambridge University Press, 1997,p. 507-534.
Reprint : In File,
Keywords : ENVIRONMENTAL HISTORY; VEGETATION CHANGE; DESERTIFICATION ASSESSMENT;
LAND DEGRADATION; STOCKING RATE; KAROO DESERTIFICATION; CONSERVATION; BUSH
ENCROACHMENT; GRAZING EFFECTS; SOUTHERN AFRICA; MODELS; POPULATION; FOREST;
LEGISLATION; POLICY
Notes : The author concludes by saying that the 'classical' view of land
degradation in southern Africa, which holds that the most devastating influences
on the vegetation of the region have occurred in the past several decades, is
rejected as being too general. The extent and severity of human impacts cannot
be viewed simply as an exponential increase with time. Each region has its
unique history and even within-biome generalizations are problematic. Certainly
many areas in southern Africa fit this general model and remain under threat
from increasingly excessive exploitation. Also, the demands made on the land by
a burgeoning population are cause for deep concern within both governmental and
environmental agencies. However, there are cases (e.g. the Knysna forest, the
eastern Karoo, the Limpopo Basin and eastern Kalahari) where severe and
nonsustainable exploitation of the resource base occurred earlier this century
or even earlier this millennium. In many instances, current legislation,
coupled with an increasing environmental awareness amongst land users and
managers, has changed exploitation practices to those that are more sustainable
in the long term. It seems that one of the best ways to prepare for the future
is to understand the trends and patterns of the past. Although extrapolation of
these historical trends into the future is problematic, southern African policy
makers and indeed the community at large should take note of the political and
cultural devastation created by past environmental degradation such as has been
postulated for the Limpopo Basin state in and around Mapungubwe more than 600
years ago (Hall 1987). Perhaps more than anything else we need to understand
the long-term implications of the region's rapid population growth rate on our
environment, since the health of our primary resource base affects people's
livelihoods directly. Indeed, the future of all southern Africa's people rests
ultimately on its renewable, natural resources.
Ref ID : 228
1113. Hoffman, M.T., Barr, G.D., and Cowling, R.M. Vegetation dynamics in the
semi-arid eastern Karoo, South Africa: the effect of seasonal rainfall and
competition on grass and shrub basal cover. South African Journal of Science
86:462-463, 1990.
Reprint : In File,
Keywords : KAROO DESERTIFICATION; VEGETATION CHANGE; VEGETATION DYNAMICS
Abstract : Using regression analyses, we examined three hypotheses concerning
grass and shrub basal cover fluctuations in the eastern Karoo. We accepted the
hypothesis that an increase in summer rain would result in increased grass
cover. We rejected the hypothesis that an increase in winter rain would result
in an increase in shrub basal cover. We suggested instead that shrub cover
decrease may be influenced by grass cover increase and that these two growth
forms may compete for resources. We speculate on the implications of our
analysis for vegetation dynamics in the eastern Karoo.
Ref ID : 234
1114. Hoffman, M.T., Bond, W.J., and Stock, W.D. Desertification of the eastern
Karoo, South Africa - conflicting palaeoecological, historical, and soil
isotopic evidence. Environmental Monitoring & Assessment 37(1-3):159-177, 1995.
Reprint : In File,
Keywords : PALAEOENVIRONMENTS; ARCHAEOLOGY; KAROO DESERTIFICATION;
DESERTIFICATION ASSESSMENT; MONITORING; STOCKING RATE; VEGETATION DYNAMICS
Abstract : TP549-0012 The desertification debate in South Africa has benefitted
greatly in recent years from the contributions of a wide range of disciplines.
In this paper we review the conflicting and supporting evidence for degradation
in the eastern Karoo as reported in recent archaeological, historical, and
stable carbon isotope studies as it relates to three key aspects of the debate:
the precolonial environment, the rate and nature of change, and the relative
contributions of humans and climate to the process. First, all studies suggest a
greater grassiness at some time in the past, but researchers disagree on the
timing of the switch to more shrubby conditions in the eastern Karoo. Second,
regional rainfall records for the past 2 decades reveal an above-average
rainfall period, and numerous long-term surveys show an increase in grass cover
over the same period. These findings question the expanding Karoo hypothesis as
well as the argument that the Karoo's carrying capacity has decreased in recent
years. Finally, the relative responsibilities of humans and climate in the
degradation process remain poorly understood and generally have not formed the
focus of investigation. [References: 36] Reprint available from: Hoffman MT NATL
BOT INST PRIVATE BAG X7 CLAREMONT 7735 SOUTH AFRICA.
Ref ID : 49
1115. Hoffman, M.T., Cousins, B., Meyer, T.C., Petersen, A., and Hendricks, H.
Historical and contemporary agricultural land use and the desertification of the
Karoo. In: The Karoo: ecological patterns and processes. edited by Dean, W.R.J.
and Milton, S.J.Cambridge University Press, 1999,
Reprint : Not in File,
Keywords : LAND USE; COMMUNAL AREA; PRODUCTION POTENTIAL; KAROO DESERTIFICATION;
ENVIRONMENTAL HISTORY; GRAZING EFFECTS; DESERTIFICATION ASSESSMENT
Ref ID : 155
1116. Hoffman, M.T. and Cowling, R.M. Vegetation change in the semi-arid eastern
Karoo over the last 200 years: an expanding Karoo - fact or fiction? South
African Journal of Science 86:286-294, 1990.
Reprint : In File,
Keywords : VEGETATION CHANGE; ENVIRONMENTAL HISTORY; KAROO DESERTIFICATION;
GRAZING EFFECTS; VEGETATION DYNAMICS
Abstract : We present historical and photographic evidence and survey data to
test current theory of vegetation change in the eastern Karoo and southern
Orange Free State (OFS) over the last two hundred years. This theory states that
the eastern Karoo has been altered from a perennial grassland to a dwarf
shrubland which is invading the southern OFS grasslands at a predictable rate.
We find little support for this and propose an alternative view of vegetation
change in the region. We suggest that the pre-colonial eastern Karoo may not
have been dominated by perennial grasses and that seasonal rainfall effects
might be responsible for much of the perceived vegetation change in the eastern
Karoo and southern OFS.
Ref ID : 48
1117. Hoffman, M.T. and Cowling, R.M. Desertification in the lower Sundays River
Valley, South Africa. Journal of Arid Environments 19:105-117, 1990.
Reprint : In File,
Keywords : DESERTIFICATION ASSESSMENT; LAND USE; KAROO DESERTIFICATION;
VEGETATION DYNAMICS; GRAZING EFFECTS
Abstract : Extensive desertification, over the next 100 years, has been
predicted for the eastern parts of South Africa. Using multivariate
classification and ordination techniques for data from the lower Sundays River
Valley, eastern Cape, we provide supporting evidence for a limited expansion of
karroid shrublands into adjacent succulent sub-tropical thicket. Karroid
shrublands appear more resilient to sustained grazing pressure than do mesic
sub-tropical thicket vegetation types.
Ref ID : 1345
1118. Hoffman, M.T., Milton, S.J., Roux, P.W., and Palmer, A.R. Report to the
intergovermental panel on climate change (IPCC). On climate change and
Desertification in South Africa. 1994.
Reprint : In File,
Keywords : CLIMATE; CLIMATE CHANGE; SOUTHERN AFRICA; AGRICULTURAL PRODUCTION;
DROUGHT; MONITORING; SUSTAINABLE DEVELOPMENT; SUBSIDIES; AID; LEGISLATION;
POPULATION
Notes : The authors conclude that: (1) The establishment of the details of the
desertification process in southern Africa is essential. The question remains
in the minds of some: "Has the region become desertified"? The formulation of a
national strategy to address the question is crucial. (2) There exists an
important need to establish the role of range management and the role of range
management research in combating the problem of desertification. (3) Continued
evaluation of long-term climatic records to prepare realistic expectations for
agriculture in the region and to evaluate trends in climate. (4) Having
established realistic expectations for agricultural production, land
redistribution should be carried out within the constraints of these findings.
(5) The development of a comprehensive drought management strategy for SA that
benefits all users of the land. (6) Expansion of bench-mark sites (vegetation
monitoring sites) to more areas in the arid and semi-arid zones of southern
Africa so as to develop accurate assessments of changes in vegetation and
rangeland states. (7) Development of research programmes focused on the question
of sustainable development. (8) Investigation into the potential negative role
that subsidies and other financial aid packages may play in "keeping the farmer
on the land" at all costs. (9) Establish regional research and agricultural
ties so as to improve regional co-operation. (10) Development of adequate
legislation, incentives and law enforcement that deal specifically with
desertification. (11) Determine the role of regional and national population
pressure on the rate, severity and extent of desertification in southern Africa.
(12) Inclusion of South Africans in international desertification debates and
conventions is crucial if we are to learn from and contribute to regional plans
of action.
Ref ID : 2503
1119. Holbrook, G. Lessons to be learned from two irrigation schemes.
Development Southern Africa , 1996.
Reprint : Not in File,
Keywords : IRRIGATION; CISKEI; AGRICULTURAL DEVELOPMENT; ECONOMIC ASPECTS;
POLITICAL ASPECTS
Notes : The purpose of the study was to investigate the two irrigation schemes,
make a comparison in terms of development and context of each scheme, and draw
lessons to be learned for future use in similar schemes. The author did
fieldwork, which was conducted in 1987 and 1990 at the Tyefu Irrigation Scheme,
and in 1992 at the Keiskammahoek Irrigation Scheme. Although the Tyefu and
Keiskammahoek Irrigation Schemes (2 small, initially centralised schemes) were
implemented in the same year, they are quite different from each other. A
comparison of the development and the context of each scheme provided insight
into small capital-intensive irrigation projects. Lessons that can be learned
include the effects of politics and agricultural management on production, the
role of the environment in managing such schemes, and the importance of
considering changes in the relationship between management and local
participants. This article can be obtained from the Document Centre, Faculty of
Agriculture, University of Fort Hare. See also ID ref. no. 2339.
Ref ID : 2570
1120. Holbrook, G. The politics of livestock management: the case study of the
village of Guquka. Proceedings of a symposium on policy-making for the
sustainable use of Southern African communal rangelands.Anonymous Anonymous ,
1998.
Reprint : Not in File,
Keywords : CISKEI; POLICY; SOCIOECONOMIC ASPECTS; LIVESTOCK PRODUCTION;
POLITICAL ASPECTS
Notes : The purpose of the study was to explore the relationship between old
established households and moral authority, by looking at the way livestock
products are shared in the village. The method used was case study. In Guquka
the principles of race, ethnicity and centralisation that shaped politics in the
past have been de-emphasised. What has been stressed is age and
decentralisation. Though the way livestock and sharing are controlled in the
village, multiple homestead households and their leaders continue to influence
former village politics despite the apparent fluidity of contemporary political
organisation. This paper is available at the Document Centre, Agriculture,
University of Fort Hare. See also ID ref. no. 2339.
Ref ID : 2539
1121. Holbrook, G. Shoring up hydraulic despotism: class race and ethnicity in
irrigation politics in the Eastern Cape Province, South Africa. Journal of
Contemporary African Studies , 1998.
Reprint : Not in File,
Keywords : IRRIGATION; EASTERN CAPE; TRANSKEI; CISKEI; POLITICAL ASPECTS;
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