| Nature 427, 145 - 148 (08 January 2004); doi:10.1038/nature02121 |
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CHRIS D. THOMAS1, ALISON CAMERON1, RHYS E. GREEN2, MICHEL BAKKENES3, LINDA J. BEAUMONT4, YVONNE C. COLLINGHAM5, BAREND F. N. ERASMUS6, MARINEZ FERREIRA DE SIQUEIRA7, ALAN GRAINGER8, LEE HANNAH9, LESLEY HUGHES4, BRIAN HUNTLEY5, ALBERT S. VAN JAARSVELD10, GUY F. MIDGLEY11, LERA MILES8,*, MIGUEL A. ORTEGA-HUERTA12, A. TOWNSEND PETERSON13, OLIVER L. PHILLIPS8 & STEPHEN E. WILLIAMS14
Correspondence and requests for materials should be addressed to C.D.T. (http://www.nature.com/cgi-taf/c.d.thomas@leeds.ac.uk).
Climate change over the past
30 years has produced numerous shifts in the distributions and
abundances of species1,
2
and has been implicated in one species-level extinction3.
Using projections of species' distributions for future climate scenarios, we
assess extinction risks for sample regions that cover some 20% of the Earth's
terrestrial surface. Exploring three approaches in which the estimated
probability of extinction shows a power-law relationship with geographical range
size, we predict, on the basis of mid-range climate-warming scenarios for 2050,
that 15–37% of species in our sample of regions and taxa will be 'committed to
extinction'. When the average of the three methods and two dispersal scenarios
is taken, minimal climate-warming scenarios produce lower projections of species
committed to extinction (
18%) than mid-range (
24%) and maximum-change (
35%) scenarios. These estimates show the importance of
rapid implementation of technologies to decrease greenhouse gas emissions and
strategies for carbon sequestration.
The responsiveness of species to recent1-3
and past4,
5
climate change raises the possibility that anthropogenic climate change could
act as a major cause of extinctions in the near future, with the Earth set to
become warmer than at any period in the past 1–40 Myr (ref. 6).
Here we use projections of the future distributions of 1,103 animal and plant
species to provide 'first-pass' estimates of extinction probabilities associated
with climate change scenarios for 2050. For each species we use the modelled association between current climates
(such as temperature, precipitation and seasonality) and present-day
distributions to estimate current distributional areas7-12.
This 'climate envelope' represents the conditions under which populations of a
species currently persist in the face of competitors and natural enemies. Future
distributions are estimated by assuming that current envelopes are retained and
can be projected for future climate scenarios7-12.
We assume that a species either has no limits to dispersal such that its future
distribution becomes the entire area projected by the climate envelope model or
that it is incapable of dispersal, in which case the new distribution is the
overlap between current and future potential distributions (for example, species
with little dispersal or that inhabit fragmented landscapes)11.
Reality for most species is likely to fall between these extremes. We explore three methods to estimate extinction, based on the species–area
relationship, which is a well-established empirical power-law relationship
describing how the number of species relates to area (S =
cAz, where S is the number of species, A
is area, and c and z are constants)13.
This relationship predicts adequately the numbers of species that become extinct
or threatened when the area available to them is reduced by habitat
destruction14,
15.
Extinctions arising from area reductions should apply regardless of whether the
cause of distribution loss is habitat destruction or climatic unsuitability. Because climate change can affect the distributional area of each species
independently, classical community-level approaches need to be modified (see
Methods). In method 1 we use changes in the summed distribution areas of all
species. This is consistent with the traditional species–area approach: on
average, the destruction of half of a habitat results in the loss of half of the
distribution area summed across all species restricted to that habitat. However,
this analysis tends to be weighted towards species with large distributional
areas. To address this, in method 2 we use the average proportional loss of the
distribution area of each species to estimate the fraction of species predicted
to become extinct. This approach is faithful to the species–area relationship
because halving the habitat area leads on average to the proportional loss of
half the distribution of each species. Method 3 considers the extinction risk of
each species in turn. In classical applications of the species–area approach,
the fraction of species predicted to become extinct is equivalent to the mean
probability of extinction per species. Thus, in method 3 we estimate the
extinction risk of each species separately by substituting its area loss in the
species–area relationship, before averaging across species (see Methods). Our
conclusions are not dependent on which of these methods is used. We use z
= 0.25 in the species–area relationship throughout, given its previous success
in predicting proportions of threatened species14,
15,
but our qualitative conclusions are not dependent on choice of z (Supplementary
Information). As there are gaps in the data (not all dispersal/climate
scenarios were available for each region), a logit–linear model is fitted to the
extinction risk data to produce estimates for missing values in the extinction
risk table (Table 1). Balanced estimates of extinction risk, averaged across
all data sets, can then be calculated for each scenario. For projections of maximum expected climate change, we estimate species-level
extinction across species included in the study to be 21–32% (range of the three
methods) with universal dispersal, and 38–52% for no dispersal (Table 1). For projections of mid-range climate change, estimates
are 15–20% with dispersal and 26–37% without dispersal (Table 1). Estimates for minimum expected climate change are
9–13% extinction with dispersal and 22–31% without dispersal. Projected
extinction varies between parts of the world and between taxonomic groups (Table 1), so our estimates are affected by the data available.
The species–area methods differ from one another by up to 1.41-fold (method 1
versus method 3) in estimated extinction, whereas the two dispersal scenarios
produce a 1.98-fold difference, and the three climate scenarios generate
2.05-fold variation. Given its role in conservation planning, we also use a different approach to
estimate extinction, modified from the IUCN Red Data Book listing
procedure16:
this is semi-numerical and includes components of expert judgement. Species are
assigned to different threat categories based on distribution sizes and
declines, with each category carrying a specified probability of
extinction16
(see Methods and Supplementary
Information). For scenarios of maximum expected climate change, 33% (with
dispersal) and 58% (without dispersal) of species are expected to become extinct
(Table 1). For mid-range climate change scenarios, 19% or 45%
(with or without dispersal) of species are expected to become extinct, and for
minimum expected climate change 11% or 34% (with or without dispersal) of
species are projected to become extinct. We can compare these values with the proportions of species projected to
become extinct as the result of global habitat losses, currently the most widely
recognized extinction threat. We apply the species–area relationship to changes
in global land use that have taken place since human land conversion
began17.
Estimates of extinction range from 1% to 29%, depending on the biome
(considering only species restricted to single biomes; Table 2). Given that a high proportion of the world's species
reside in tropical forests (extinction estimate 4%; Table 2), global extinction related to habitat loss would be
expected to be in the lower half of the range, and thus lower than the rate
projected for scenarios of mid-range climate change (24%; average of area
methods). Projected conversion of humid tropical forest at an annual rate of
0.43% (ref. 18)
from 1990 to 2050 predicts a further 6.3% of species committed to
extinction. Regional differences are expected, so we also compare the relative risks
during 2000–2050 associated with land use and climate change (using area
approaches) for the three region–taxon combinations that correspond most closely
to single habitat or biome types. First, for montane Queensland forests12,
extinction risk is dominated by climate change (7–13% and 43–58% predicted
extinction for minimum and maximum climate scenarios, respectively; 0% predicted
on the basis of further habitat destruction, given its legal protection).
Second, for cerrado vegetation in Brazil, high rates of habitat
destruction19
make it possible that only current reserves will survive. Making this
pessimistic assumption, an estimated additional 34% of all original species will
be committed to extinction due to habitat destruction during 2000–2050, a value
lower than the 48–56% of woody plant species projected to be committed to
extinction for mid-range climate warming (38–45% for minimum warming). Last, for
South African Proteaceae, 27% of all original species are projected to become
extinct as a result of land use changes during 2000–2050 (for a pessimistic
linear extrapolation of land use scenarios after 2020)20,
falling between the 30–40% (without dispersal) and 21–27% (with ubiquitous
dispersal, which is unlikely for these plants) projected extinction for
mid-range climate scenarios. Many unknowns remain in projecting extinctions, and the values provided here
should not be taken as precise predictions. Analyses need to be repeated for
larger samples of regions and taxa, and the selection of climate change
scenarios need to be standardized. Some of the most important uncertainties
follow (see also Supplementary
Information). We estimate proportions of species committed to future
extinction as a consequence of climate change over the next 50 years, not the
number of species that will become extinct during this period. Information is
not currently available on time lags between climate change and species-level
extinctions, but decades might elapse between area reduction (from habitat loss)
and extinction14.
Land use should also be incorporated into analyses: extinction risks might be
higher than we project if future locations of suitable climate do not coincide
with other essential resources (such as soil type or food resources). There is
also uncertainty over which species will inhabit parts of the world projected to
have climates for which no current analogue exists6.
Equally importantly, all parts of the world will have historically unprecedented
CO2 levels6,
which will affect plant species and ecosystems21,
22
and herbivores23,
resulting in novel species assemblages and interactions. Despite these uncertainties, we believe that the consistent overall
conclusions across analyses establish that anthropogenic climate warming at
least ranks alongside other recognized threats to global biodiversity. Contrary
to previous projections24,
it is likely to be the greatest threat in many if not most regions. Furthermore,
many of the most severe impacts of climate-change are likely to stem from
interactions between threats, factors not taken into account in our
calculations, rather than from climate acting in isolation. The ability of
species to reach new climatically suitable areas will be hampered by habitat
loss and fragmentation, and their ability to persist in appropriate climates is
likely to be affected by new invasive species. Minimum expected (that is, inevitable) climate-change scenarios for 2050
produce fewer projected 'committed extinctions' (18%; average of the three area
methods and the two dispersal scenarios) than mid-range projections (24%), and
about half of those predicted under maximum expected climate change (35%). These
scenarios would diverge even more by 2100. In other words, minimizing greenhouse
gas emissions and sequestering carbon25
to realize minimum, rather than mid-range or maximum, expected climate warming
could save a substantial percentage of terrestrial species from extinction.
Returning to near pre-industrial global temperatures as quickly as possible
could prevent much of the projected, but slower-acting, climate-related
extinction from being realized. Methods Climate scenarios Climate projections for 2050 were divided into three
categories: minimum expected change resulting in a mean increase in global
temperature of 0.8–1.7 °C and in CO2 of 500 p.p.m. by
volume (p.p.m.v.); mid-range scenarios with temperature increases of
1.8–2.0 °C and CO2 increases of 500–550 p.p.m.v.; and
maximum expected scenarios with temperature increases of >2.0 °C and
CO2 increases >550 p.p.m.v. (ref. 30).
Projections for the year 2100 were allocated to 2050 scenarios according to
their end temperatures and CO2 levels (Supplementary
Information). Species Within each region we use only data for endemic species
(near-endemic in two cases). Near-endemics are defined as >90% of the
distribution area known to occur (European birds) or thought to occur (cerrado
plants, given incomplete data) within the region modelled. For European birds,
near-endemics are included only if their extra-European distribution is similar
to climate space within Europe. The focus on endemics permits us to model all
range boundaries of each species (Supplementary
Information). Species–area approaches Method 1 analyses overall changes in
distribution areas, summed across species. The proportion of species in a region
going extinct (E1) is estimated as
Method 2 is based on the average proportional change in distribution area,
averaged across species. Regional extinction risk (E2) is
Method 3 estimates the extinction risk of each species in turn, averaging
across species to derive regional estimates of extinction
(E3):
Species for which Anew > Aoriginal
were analysed as though Anew = Aoriginal;
that is, zero extinction would be returned by each equation if every species was
projected to expand (Supplementary
Information). It is important to recognize that further work is required to
establish empirically how the absolute and proportional area losses of
individual species (in other words, the type of data from climate envelope
projections) are related to extinction risk. As yet, no agreed standard method
exists for such calculations: assumptions and uncertainties inherent in the
three methods will be considered in detail elsewhere. Extinction probability estimates were not available for all scenarios in
every region/taxon, so means of scenarios were calculated after using a
least-squares analysis of variance model to impute missing values. Region/taxon
mean probabilities of extinction for each scenario were logit-transformed and a
three-way analysis of variance was fitted (region/taxon Red Data Book criteria Each species is assigned to a threat
category16,
or classified 'Not Threatened' (0% risk), depending on the projected decline in
area over 50 or 100 years (Supplementary
Information) and the final distribution area. Existing areas were
considered, so we present only the extra extinction attributable to climate
change. Logit-transformed three-way analysis of variance was used to estimate
extinction risks for empty cells, as with the species–area approaches. Extinct: species with a projected future area of zero (100% of species
assumed to be committed to eventual extinction). Critically endangered: projected future distribution area
<10 km2, or decline by >80% in 50 years (species assigned
a 75% chance of extinction16). Endangered: projected area 10–500 km2, or 50–80% decline in
50 years (species assigned a 35% chance of extinction16). Vulnerable: projected area 500–2,000 km2, or >50% decline
in 100 years on the basis of linear extrapolation of 50-year projection (species
assigned a 15% chance of extinction16).
Climate-envelope modelling The statistical match
between climate variables and the boundaries of a species' distribution (climate
envelope) represents conditions in which a species (normally) shows a positive
demographic balance (rarely the absolute physical limits of a species, but the
set of conditions under which it survives in at least some multi-species
communities). The statistical approach is generic, but specific methods vary
between studies (Supplementary
Information). The approach has been validated by successfully predicting
distributions of invading species when they arrive in new continents and by
predicting distributional changes in response to glacial climate changes; its
scope has been discussed widely (see, for example, refs 12,
26–29).
Dispersal is assumed to be universal or zero (main text), except for the Mexican
study in which 'universal dispersal' is movement through contiguous
habitats11.


climate scenario
dispersal scenario; weighted by
(Nspecies) per region/taxon study). The
fitted model was used to impute expected values of the probability of extinction
for those region/taxon and scenario combinations for which direct estimates were
not available. Scenario means were then calculated from the combined direct
estimates and imputed values, using
(Nspecies) for each region/taxon as
weights.
Supplementary information accompanies this paper.
Received 10 September
2003;
accepted
13 October 2003
| 1. | Parmesan, C. & Yohe, G. A globally coherent fingerprint of climate change impacts across natural systems. Nature 421, 37–42 (2003) | Article | PubMed | ISI | ChemPort | |
| 2. | Root, T. L. et al. Fingerprints of global warming on wild animals and plants. Nature 421, 57–60 (2003) | Article | PubMed | ISI | ChemPort | |
| 3. | Pounds, J. A., Fogden, M. L. P. & Campbell, J. H. Biological response to climate change on a tropical mountain. Nature 398, 611–615 (1999) | Article | ISI | ChemPort | |
| 4. | Overpeck, J., Whitlock, C. & Huntley, B. in Paleoclimate, Global Change and the Future (eds Alverson, K., Bradley, R. & Pedersen, T.) 81–103 (Springer, Berlin, 2002) |
| 5. | Benton, M. J. & Twitchett, R. J. How to kill (almost) all life: the end-Permian extinction event. Trends Ecol. Evol. 18, 358–365 (2003) | Article | ISI | |
| 6. | Houghton, J. T. et al. Climate change 2001: the Scientific Basis. Contributions of Working Group I to the Third Assessment Report of the Intergovernmental Panel on Climate Change (Cambridge Univ. Press, 2001) |
| 7. | Bakkenes, M., Alkemade, J. R. M., Ihle, F., Leemans, R. & Latour, J. B. Assessing effects of forecasted climate change on the diversity and distribution of European higher plants for 2050. Global Change Biol. 8, 390–407 (2002) | Article | ISI | |
| 8. | Beaumont, L. J. & Hughes, L. Potential changes in the distributions of latitudinally restricted Australian butterfly species in response to climate change. Global Change Biol. 8, 954–971 (2002) | Article | ISI | |
| 9. | Erasmus, B. F. N., van Jaarsveld, A. S., Chown, S. L., Kshatriya, M. & Wessels, K. Vulnerability of South African animal taxa to climate change. Global Change Biol. 8, 679–693 (2002) | Article | ISI | |
| 10. | Midgley, G. F., Hannah, L., Rutherford, M. C. & Powrie, L. W. Assessing the vulnerability of species richness to anthropogenic climate change in a biodiversity hotspot. Global Ecol. Biogeogr. 11, 445–451 (2002) | Article | ISI | |
| 11. | Peterson, A. T. et al. Future projections for Mexican faunas under global climate change scenarios. Nature 416, 626–629 (2002) | Article | PubMed | ISI | ChemPort | |
| 12. | Williams, S. E., Bolitho, E. E. & Fox, S. Climate change in Australian tropical rainforests: an impending environmental catastrophe. Proc. R. Soc. Lond. B 270, 1887–1892 (2003) | Article | PubMed | ISI | |
| 13. | Rosenzweig, M. L. Species Diversity in Space and Time (Cambridge Univ. Press, 1995) |
| 14. | Brooks, T. M., Pimm, S. L. & Oyugi, J. O. Time lag between deforestation and bird extinction in tropical forest fragments. Conserv. Biol. 13, 1140–1150 (1999) | Article | ISI | |
| 15. | Brooks, T. M., Pimm, S. L. & Collar, N. J. Deforestation predicts the number of threatened birds in insular Southeast Asia. Conserv. Biol. 11, 382–394 (1997) | Article | ISI | |
| 16. | IUCN Red List Categories and Criteria, version 3.1. (IUCN Species Survival Commission, Gland, Switzerland, 2001). |
| 17. | Gaston, K. J., Blackburn, T. M. & Goldewijk, K. K. Habitat conversion and global avian biodiversity loss. Proc. R. Soc. Lond. B 270, 1293–1300 (2003) | Article | PubMed | ISI | |
| 18. | Achard, F. et al. Determination of deforestation rates of the world's humid tropical forests. Science 297, 999–1002 (2002) | Article | PubMed | ISI | ChemPort | |
| 19. | Myers, N., Mittermeier, R. A., Mittermeier, C. G., da Fonseca, G. A. B. & Kent, J. Biodiversity hotspots for conservation priorities. Nature 403, 853–858 (2000) | Article | PubMed | ISI | ChemPort | |
| 20. | Roget, M., Richardson, D. M., Cowling, R. M., Lloyd, J. W. & Lombard, A. T. Current patterns of habitat transformation and future threats to biodiversity in terrestrial ecosystems of the Cape Floristic Region, South Africa. Biol. Conserv. 112, 63–85 (2003) | Article | |
| 21. | Woodward, F. I. Potential impacts of global elevated CO2 concentrations on plants. Curr. Opin. Plant Biol. 5, 207–211 (2002) | Article | PubMed | ISI | ChemPort | |
| 22. | Bond, W. J., Midgley, G. F. & Woodward, F. I. The importance of low atmospheric CO2 and fire in promoting the spread of grasslands and savannas. Global Change Biol. 9, 973–982 (2003) | ISI | |
| 23. | Whittaker, J. B. Impacts and responses at population level of herbivorous insects to elevated CO2. Eur. J. Entomol. 96, 149–156 (1999) | ISI | |
| 24. | Sala, O. E. et al. Biodiversity—global biodiversity scenarios for the year 2100. Science 287, 1770–1774 (2000) | Article | PubMed | ISI | ChemPort | |
| 25. | Lackner, K. S. A guide to CO2 sequestration. Science 300, 1677–1678 (2003) | Article | PubMed | ISI | ChemPort | |
| 26. | Beerling, D. J. The impact of temperature on the northern distribution limits of the introduced species Fallopia japonica and Impatiens glandulifera in north-west Europe. J. Biogeog. 20, 45–53 (1993) | ISI | |
| 27. | Baker, R. H. A. et al. The role of climatic mapping in predicting the potential geographical distribution of non-indigenous pests under current and future climates. Agric. Ecosyst. Environ. 82, 57–71 (2000) | Article | ISI | |
| 28. | Peterson, A. T. & Vieglais, D. A. Predicting species invasions using ecological niche modeling. BioScience 51, 363–371 (2001) | ISI | |
| 29. | Pearson, R. G. & Dawson, T. P. Predicting the impacts of climate change on the distribution of species: are bioclimate envelope models useful? Global Ecol. Biogeog. 12, 361–371 (2003) | Article | ISI | |
| 30. | Intergovernmental Panel on Climate Change. Climate Change 2001: The Scientific Basis. http://www.grida.no/climate/ipcc_tar/wg1/figts-22.htm (2001). |
Acknowledgements. We thank the following for many contributions: E. Bolitho, V. Perez Canhos, D. A. L. Canhos, S. Carver, S. L. Chown, S. Fox, M. Kshatriya, D. Millar, A. G. Navarro-Sigüenza, R. S. Pereira, B. Reyers, E. Martínez-Meyer, V. Sánchez-Cordero, J. Soberón, D. R. B. Stockwell, W. Thuiller, D. A. Vieglais and K. J. Wessels, researchers involved in the Projeto de Cooperação Técnica Conservação e Manejo da Biodiversidade do Bioma Cerrado, EMBRAPA Cerrados, UnB, Ibama/DFID e RBGE/Reino Unido, and the European Bird Census Council. We thank G. Mace, J. Malcolm and C. Parmesan for valuable discussions, many funding agencies for support, and B. Orlando and others at IUCN for bringing together many of the coauthors at workshops. Comments from J. A. Pounds and S. Pimm greatly improved the manuscript.Authors' contributions The fourth and subsequent authors are alphabetically arranged and contributed equally.
Competing interests statement. The authors declare that they have no competing financial interests.