cbd-ts-66-en
cbd-ts-66-en
cbd-ts-66-en
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Part I: Impac<strong>ts</strong> of Climate-related Geo<strong>en</strong>gineering on Biological Diversity<br />
minimize the disadvantages and risks325, 326, 327 such as the use of monocultures and pot<strong>en</strong>tially invasive species.<br />
The CBD is also developing advice for the application of REDD+ biodiversity safeguards (reducing emissions<br />
from deforestation and forest degradation and the role of conservation, sustainable managem<strong>en</strong>t of fores<strong>ts</strong> and<br />
<strong>en</strong>hancem<strong>en</strong>t of forest carbon stocks in developing countries).<br />
In order to maximize biodiversity b<strong>en</strong>efi<strong>ts</strong>, ecosystem storage of carbon should be based on an <strong>en</strong>vironm<strong>en</strong>tal<br />
impact assessm<strong>en</strong>t including impac<strong>ts</strong> related to biodiversity and native species. Interv<strong>en</strong>tions should also incorporate<br />
resili<strong>en</strong>ce to anticipated climate change, and should prioritize climatically-appropriate native assemblages of species.<br />
Where such recomm<strong>en</strong>dations have not be<strong>en</strong> followed (e.g., in reforestation projec<strong>ts</strong> using non-native species), the<br />
result has oft<strong>en</strong> be<strong>en</strong> monoculture plantations which are unable to support viable population of <strong>en</strong>demic species.328<br />
Impac<strong>ts</strong> on ecosystem services<br />
Increased soil carbon can increase the amount of water retained in the soil, thereby increasing the resili<strong>en</strong>ce of<br />
ecosystems and pot<strong>en</strong>tially mitigating the water-depleting effec<strong>ts</strong> of climate change in arid areas. In addition,<br />
increased soil carbon has the pot<strong>en</strong>tial to <strong>en</strong>hance crop productivity. This may reduce the inc<strong>en</strong>tive to convert<br />
previously non-agricultural land into agricultural land, and could therefore help to safeguard biodiversity. As<br />
demonstrated by a watershed-scale study in Oregon, USA, increasing carbon storage through the introduction<br />
of land-use policies can b<strong>en</strong>efit a wide range of ecosystem services.329 Moreover, several regional studies have<br />
demonstrated that b<strong>en</strong>efi<strong>ts</strong> to ecosystem services such as water regulation, biodiversity conservation, and agriculture,<br />
can result from integrated land-use planning that delivers <strong>en</strong>hanced CO2 sequestration.330<br />
However, while increased soil water ret<strong>en</strong>tion (as a result of increased soil carbon) may g<strong>en</strong>erally have positive<br />
effec<strong>ts</strong>, in some areas, increased water ret<strong>en</strong>tion could lead to more anoxic conditions, increasing CH4 and N2O<br />
emissions. Moreover, <strong>en</strong>hanced plant productivity does not necessarily produce positive ecosystem impac<strong>ts</strong>, if fast<br />
growing species are favoured. This could lead to shif<strong>ts</strong> in ecosystem composition, interactions betwe<strong>en</strong> species,<br />
and changes within food webs.<br />
Risks and uncertainties<br />
Large-scale increases in forest cover can have an impact on both planetary albedo and the hydrological cycle, and<br />
can create a protecting buffer for neighboring ecosystems against floods and other <strong>en</strong>vironm<strong>en</strong>tal perturbations.<br />
Newly created fores<strong>ts</strong> are also likely to emit volatile organic compounds (VOCs), which increase the conc<strong>en</strong>tration<br />
of cloud cond<strong>en</strong>sation nuclei and therefore affect cloud formation. However, the combined effec<strong>ts</strong> of increased<br />
forest cover on the hydrological cycle,331 planetary albedo and cloud cover, and subsequ<strong>en</strong>t impac<strong>ts</strong> on biodiversity<br />
and ecosystem services, are curr<strong>en</strong>tly not well understood.332 This is an area where the need for further research<br />
and assessm<strong>en</strong>t has be<strong>en</strong> id<strong>en</strong>tified.333<br />
Other key uncertainties relate to which soil types are most suitable for carbon <strong>en</strong>hancem<strong>en</strong>t, to avoid adverse side<br />
effec<strong>ts</strong> (e.g. anoxic conditions and methane release). It is also curr<strong>en</strong>tly unclear how a soil carbon change might<br />
affect the community of species dep<strong>en</strong>d<strong>en</strong>t on a particular soil type, and whether biodiversity b<strong>en</strong>efi<strong>ts</strong> would<br />
ultimately increase or decrease.<br />
325 Secretariat of the Conv<strong>en</strong>tion on Biological Diversity (2009a).<br />
326 Secretariat of the Conv<strong>en</strong>tion on Biological Diversity (2003).<br />
327 CBD COP decision VI/22 Annex and X/33 paragraph 8(p).<br />
328 Ramanamanjato & Ganzhorn (2001).<br />
329 Nelson et al. (2009).<br />
330 The Royal Society (2001).<br />
331 Arora & Mont<strong>en</strong>egro (2010).<br />
332 Anderson et al. (2011).<br />
333 Russell et al. (2012).<br />
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