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Abstracts available here - Society for Conservation Biology

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25th International Congress <strong>for</strong> <strong>Conservation</strong> <strong>Biology</strong> • Auckland, New Zealand • 5-9 December 2011<br />

2011-12-08 10:30 Climate change, Variability and conservation<br />

impacts in Australia<br />

Prowse, TAA, University of Adelaide; Brook, BW*, University of<br />

Adelaide;<br />

Australian conservation scientists, managers and decision makers must<br />

come to grips with anthropogenic climate change, imposed upon an already<br />

variable regional climate system. Pre- and post-instrumental records and<br />

climate proxies indicate that Australia has experienced wet and dry cycles<br />

over intra-decadal to millennial time scales. Precipitation variation across<br />

Australia is correlated with different climate features but reliable tools <strong>for</strong><br />

seasonal rainfall prediction are still some years away. Atmosp<strong>here</strong>-Ocean<br />

General Circulation Models predict a widening of the Hadley circulation<br />

and strengthening of the Southern Annular Mode, which should result in<br />

reduced cool season rainfall over southern Australia. Shifts in the Australian<br />

climate over the Holocene epoch, most notably increased ENSO variability<br />

after 5 000 years ago, are associated with substantial vegetation change and<br />

indicate the speed at which ecosystems may be altered. The CO2 fertilization<br />

of plant biomes may mitigate increasing aridity to some extent but, in<br />

general, climate change is expected to negatively affect native vegetation<br />

and agricultural productivity. Sea-level rise is predicted to be substantial<br />

over this century and, when coupled with increased storm intensity, poses<br />

threats in the <strong>for</strong>m of erosion, salinization and flooding. The best chance<br />

of building adaptable ecosystems and preserving ecosystem services requires<br />

the extension, integration and possibly optimization of reserve systems, in<br />

concert with improved management of other threatening processes (habitat<br />

loss, invasive species, overexploitation, pollution and disease). In addition,<br />

a price on carbon dioxide emissions would provide incentives <strong>for</strong> privately<br />

funded re<strong>for</strong>estation schemes, but additional incentives promoting mixed<br />

species over monoculture plantings would be required to assure maximum<br />

biodiversity benefits.<br />

2011-12-09 11:00 <strong>Conservation</strong> Management of Complex Edge Effects<br />

Pryke, J. S.*, Stellenbosch University; Samways, M.J., Stellenbosch<br />

University;<br />

Understanding edge effects between trans<strong>for</strong>med landscapes and<br />

conservation areas is critical to conservation planning. As conservation<br />

areas in landscape mosaics are often composed of linear corridors, t<strong>here</strong><br />

are more edges than would occur naturally. To determine minimum<br />

width of corridors, we would first need to determine the extent of edge<br />

effects. Plantation <strong>for</strong>estry has trans<strong>for</strong>med much of the South African<br />

grasslands, with ecological networks (ENs) currently being used to mitigate<br />

this biodiversity loss and to maintain ecosystem processes. We compare<br />

arthropod biodiversity along transects that ran from within plantation<br />

blocks or indigenous <strong>for</strong>est patches (as a natural reference) into indigenous<br />

grassland corridors. Two types of exotic commercial trees and various tree<br />

age classes were studied. We found a 32 m edge zone from plantation blocks<br />

into grassland corridors. Few significant edge effects from plantation blocks<br />

occurred at greater distances than this, suggesting that grassland corridors<br />

with a width

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