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 />
CHAPTER 5<br />
POTENTIAL IMPACTS ON BIODIVERSITY OF CARBON DIOXIDE<br />
REMOVAL GEOENGINEERING TECHNIQUES<br />
5.1 GENERAL FEATURES OF CDR APPROACHES<br />
5.1.1 Reducing the impac<strong>ts</strong> of climate change<br />
By removing carbon dioxide (CO2) from the atmosphere, CDR techniques are int<strong>en</strong>ded to reduce the conc<strong>en</strong>tration<br />
of the main causal ag<strong>en</strong>t of anthropog<strong>en</strong>ic climate change. In addition, they are expected to ameliorate ocean<br />
acidification (Figure 2.1).<br />
Any reductions in the negative impac<strong>ts</strong> of climate change and ocean acidification on biodiversity (as summarized<br />
in Chapter 3) that might be achieved by effective and feasible CDR techniques would therefore be expected<br />
to have positive impac<strong>ts</strong> on biodiversity, in a way that is far more certain than for SRM. However, as noted in<br />
Chapter 2: (i) these b<strong>en</strong>eficial effec<strong>ts</strong> are g<strong>en</strong>erally slow-acting; (ii) the climatic conditions resulting from a specific<br />
atmospheric CO2 value may be differ<strong>en</strong>t if CO2 is falling (as a result of a CDR measure) from the conditions<br />
previously experi<strong>en</strong>ced at the same CO2 value wh<strong>en</strong> it was rising;259 and (iii) several CDR techniques are of only<br />
modest or doubtful effectiv<strong>en</strong>ess,260, 261 with few (if any) considered realistically capable of fully offsetting curr<strong>en</strong>t<br />
anthropog<strong>en</strong>ic carbon emissions.<br />
In addition, any positive effec<strong>ts</strong> from reduced impac<strong>ts</strong> of climate change and/or ocean acidification due to reduced<br />
atmospheric CO2 conc<strong>en</strong>trations may be offset (or, in a few cases, augm<strong>en</strong>ted) by additional, unint<strong>en</strong>ded impac<strong>ts</strong><br />
on biodiversity of the particular CDR technique employed. Such additional impac<strong>ts</strong> are summarised in Table 5.1,<br />
and are reviewed on a technique-specific basis in sections 5.2 -5.7 below.<br />
5.1.2 Carbon sequestration (removal and storage)<br />
The term “carbon sequestration” was (provisionally) defined by the t<strong>en</strong>th meeting of the Confer<strong>en</strong>ce of the Parties<br />
to the CBD262 as “the process of increasing the carbon cont<strong>en</strong>t of a reservoir/pool other than the atmosphere”.<br />
However, in a geo<strong>en</strong>gineering context this usage is ambiguous, since no temporal constrain<strong>ts</strong> are included. It is<br />
therefore preferable to clearly recognise that carbon sequestration (through CDR geo<strong>en</strong>gineering) necessarily<br />
involves two steps:<br />
54<br />
i) removal of CO2 from the atmosphere; and<br />
ii) long-term storage of the captured carbon, taking it out of circulation for a climatically-significant<br />
period (e.g., at least 10 years, and preferably > 100 years).<br />
These processes occur naturally, but the former does not necessarily lead to the latter. Thus most of the produc<strong>ts</strong><br />
of either terrestrial or marine photosynthesis are recycled annually or on shorter timescales by plant, animal or<br />
microbial respiration. Effective sequestration requires that both steps can be demonstrated. Nevertheless, the term<br />
is sometimes used as the descriptor for only the latter, storage compon<strong>en</strong>t,263 contrasting to the CBD’s definition<br />
above that seems to focus only on the initial removal.<br />
259 Chadwick et al. (2012).<br />
260 Vaughan & L<strong>en</strong>ton (2011).<br />
261 McLar<strong>en</strong> (2011).<br />
262 Footnote to CBD decision X/33, paragraph 8(w).<br />
263 In legal and/or financial usage, sequestration involves secure holding and access restrictions, e.g. of asse<strong>ts</strong>.