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Connecting Global Priorities Biodiversity and Human Health

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al. 2014), though advances in technology, prevention <strong>and</strong> treatment can combine to reduce the burden<br />

of diseases like malaria (Feachem et al. 2010). Climate change directly contributes to damage of both<br />

infrastructure <strong>and</strong> human settlements, resulting in human mortality <strong>and</strong> morbidity that includes the<br />

mental health <strong>and</strong> well-being of survivors (IPCC 2014d). In countries at all stages of development, these<br />

impacts are consistent with a lack of preparedness for climatic variability in some sectors; the most<br />

salient manifestations will be among the poorest <strong>and</strong> most vulnerable populations (IPCC, 2014d).<br />

Tertiary<br />

The third – “tertiary impacts” – category is, by a number of magnitudes, the most important health<br />

risk associated with climate change (Butler 2014b). These include the health impacts of large-scale<br />

famine, forced migration <strong>and</strong> human conict, which result from the geophysical <strong>and</strong> ecological<br />

consequences of climate change, including the alteration of ecosystems, sea-level rise, <strong>and</strong> longterm<br />

disruptions in water supply <strong>and</strong> food production. Surprisingly, with rare exceptions, this group<br />

of eects has been little mentioned in the intervening decades, including in the most recent IPCC<br />

reports released in 2014. These must be considered more holistically as we prepare to embark upon<br />

new global commitments on climate change <strong>and</strong> a post-2015 Development Agenda.<br />

Many authors in this volume point to numerous<br />

synergies (“co-benefits”) that could flow to both<br />

human well-being <strong>and</strong> ecological “health” from a<br />

more biosensitive approach to our relationship<br />

with nature (Boyden 2004), such as the co-benefits<br />

of cycling on both health <strong>and</strong> environment.<br />

Awareness of these co-benefits may also accelerate<br />

global social transformation (Haines et al. 2009;<br />

Raskin et al. 2002). On the other h<strong>and</strong>, many<br />

forms of inertia: social, institutional, technological<br />

<strong>and</strong> perhaps, above all, climatological, slow <strong>and</strong><br />

impede the likelihood of a successful transition,<br />

most notably an enormous countermovement,<br />

funded <strong>and</strong> fuelled by vested interests profiting<br />

from “environmental brinkmanship” (Butler<br />

2000). Delay is also worsened by the scientific<br />

knowledge gaps of many economists <strong>and</strong> policymakers,<br />

who have been very slow to awaken to the<br />

risks we face, <strong>and</strong> who are instead wedded to more<br />

conservative or sectoral measures of progress, or<br />

to the hope that technological innovation alone<br />

will eventually solve the problem.<br />

1.2 Vulnerability of biodiversity to<br />

impacts of climate change<br />

The earth’s biota was shaped by fluctuating<br />

Pleistocene concentrations of atmospheric<br />

carbon dioxide, temperature <strong>and</strong> precipitation;<br />

it has undergone multiple evolutionary changes<br />

<strong>and</strong> adopted natural adaptive strategies. Until<br />

the advent of industrialization, changes in<br />

climate occurred over an extended period of<br />

time, in a l<strong>and</strong>scape much less degraded <strong>and</strong><br />

fragmented than today, <strong>and</strong> with considerably<br />

less – if any – pressure from anthropogenic<br />

activity. Habitat fragmentation has confined<br />

many species to relatively small areas within<br />

their previous ranges, resulting in reduced genetic<br />

variability (Parmesan <strong>and</strong> Matthews 2006) <strong>and</strong><br />

other changes to structure <strong>and</strong> composition (CBD<br />

2009). Warming beyond the highest temperatures<br />

reached during the Pleistocene will continue to<br />

stress biodiversity <strong>and</strong> ecosystems far beyond<br />

the levels imposed by the climatic changes that<br />

occurred in the evolutionary past (Templeton et<br />

al. 1990; Parmesan 2006).<br />

The impacts of climate change on biodiversity<br />

operate at different levels (including microbial,<br />

individual, population, species, community,<br />

ecosystem <strong>and</strong> biome), with variable responses<br />

at each level (Bellard et al. 2012; Parmesan<br />

<strong>and</strong> Martens 2009). For example, increased<br />

temperatures coupled with decreases in the<br />

distribution of precipitation may reduce<br />

freshwater levels in lakes <strong>and</strong> rivers (Campbell<br />

et al. 2009). Warmer temperatures cause fish<br />

<strong>Connecting</strong> <strong>Global</strong> <strong>Priorities</strong>: <strong>Biodiversity</strong> <strong>and</strong> <strong>Human</strong> <strong>Health</strong><br />

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