Thursday, 27 August 2009

Adapting Conservation Strategies to Accommodate Impacts of Climate Change in Southern Africa

Adapting Conservation Strategies to Accommodate Impacts of Climate Change in
Southern Africa
G.P. Von Maltitz, R.J. Scholes, B. Erasmus and A. Letsoalo
CSIR, South Africa
AIACC Working Paper No. 35
August 2006

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Adapting Conservation Strategies to Accommodate Impacts of Climate Change in Southern Africa1
G. P. Von Maltitz, R. J. Scholes, B. Erasmus, and A. Letsoalo
1. Introduction

Current predictions are that global climate change will have substantial impacts on southern Africa’s biodiversity, including wide-scale extinctions over the next 50 years (Rutherford et al., 1999; Hannah et al., 2000a,b; Gitay et al., 2001, 2002 et al.; Midgley et al., 2002a,b; MA, 2005). At a global scale, Thomas et al. (2004) predicted that 15–37% of species in their sample (that covered 20% of the earth surface) may be at risk of premature extinction due to anthropogenically caused global change by 2050. The Millennium Ecosystem Assessment, using different models and assumptions based largely on habitat loss, reached similar conclusions (MA, 2005). Within South Africa, one of the few areas in sub-Sahara Africa where detailed analysis has been conducted, the predictions are that most of the current biomes will reduce in size and will be shifted to the east of the country. Up to half of the country will have a climatic regime that is not currently found in the country (Rutherford et al., 1999).

The succulent karoo biome, (a succulent-dominated semi-desert located on the southwestern coast of southern Africa) is projected to be the most severely impacted, with the grassland and fynbos (a Mediterranean-climate sclerophyllous thicket that approximates to the Cape Floristic 1 The research reported in this paper was supported by grant number AF04 from region) biomes also likely to suffer from high climate change impacts (Rutherford et al., 1999; Midgley et al., 2002a,b). Fynbos and succulent karoo are biodiversity hotspots of international importance (Myers et al., 2000), with the latter being one of only two globally important arid-climate biodiversity hotspots. Two main aspects of the climate have widespread influence on animal and plant species distributions: temperature and water balance (a combination of precipitation and evaporation, which, in turn, is directly influenced by temperature) (Cubasch, 2001). The dynamics of plant and animal populations change at the edge of individual species’ distribution, as net mortality becomes larger than net fecundity, with a spatial gradient of declining population numbers as a result. In a scenario of climate change, this will lead to the progressive extinction of nonvagile species in their natural range, beginning with population dieback in the so-called "trailing edge" of the historical distribution range (Davis and Shaw, 2001). This change in local population dynamics is affected directly by temperature and water balance, but it is also indirectly through aspects such as interspecies competition, fire frequency, pollinator distribution, herbivory and predation,
food availability, soil type, topography etc. (e.g., Gaston, 2003).

Few species occupy their "fundamental niche,", i.e., the range determined by the physiological tolerance limits.
Their actual range, the "realised niche," is a subset of this resulting from the outcome of interactions with other species. The degree to which species distribution can be predicted
based on their climatically defined habitat niche differs between species (e.g., Thuiller et al., 2006).

http://www.aiaccproject.org/working_papers/Working%20Papers/AIACC_WP35_vonMaltitz.pdf

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