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The Limits of Planetary Boundaries
Erle Ellis, Barry Brook, Linus Blomqvist, Ruth DeFries
Part of a running Dot Earth discussion of good paths in the Age of Us – the Anthropocene
Steffen et al (2015) revise the “planetary boundaries framework” initially proposed in 2009 as
the “safe limits” for human alteration of Earth processes (Rockstrom et al 2009). Limiting human
harm to environments is a major challenge and we applaud all efforts to increase the public
utility of global-change science. Yet the planetary boundaries (PB) framework - in its original
form and as revised by Steffen et al - obscures rather than clarifies the environmental and
sustainability challenges faced by humanity this century.
Steffen et al concede that “not all Earth system processes included in the PB have singular
thresholds at the global/continental/ocean basin level.” Such processes include biosphere
integrity (see Brook et al 2013), biogeochemical flows, freshwater use, and land-system change.
“Nevertheless,” they continue, “it is important that boundaries be established for these
processes.” Why? Where a global threshold is unknown or lacking, there is no scientifically
robust way of specifying such a boundary - determining a limit along a continuum of
environmental change becomes a matter of guesswork or speculation (see e.g. Bass 2009;
Nordhaus et al 2012). For instance, the land-system boundary for temperate forest is set at 50%
of forest cover remaining. There is no robust justification for why this boundary should not be
40%, or 70%, or some other level.
While the stated objective of the PB framework is to “guide human societies” away from a state
of the Earth system that is “less hospitable to the development of human societies”, it offers little
scientific evidence to support the connection between the global state of specific Earth system
processes and human well-being. Instead, the Holocene environment (the most recent 10,000
years) is assumed to be ideal. Yet most species evolved before the Holocene and the
contemporary ecosystems that sustain humanity are agroecosystems, urban ecosystems and
other human-altered ecosystems that in themselves represent some of the most important
global and local environmental changes that characterize the Anthropocene. Contrary to the
authors’ claim that the Holocene is the “only state of the planet that we know for certain can
support contemporary human societies,” the human-altered ecosystems of the Anthropocene
represent the only state of the planet that we know for certain can support contemporary
civilization.
Human alteration of environments produces multiple effects, some advantageous to societies,
such as enhanced food production, and some detrimental, like environmental pollution with toxic
chemicals, excess nutrients and carbon emissions from fossil fuels, and the loss of wildlife and
their habitats. The key to better environmental outcomes is not in ending human alteration of
environments but in anticipating and mitigating their negative consequences. These decisions
and trade-offs should be guided by robust evidence, with global-change science investigating
the connections and tradeoffs between the state of the environment and human well-being in
the context of the local setting, rather than by framing and reframing environmental challenges
in terms of untestable assumptions about the virtues of past environments.
Even without specifying exact global boundaries, global metrics can be highly misleading for
policy. For example, with nitrogen, where the majority of human emissions come from synthetic
fertilizers, the real-world challenge is to apply just the right amount of nitrogen to optimize crop
yields while minimizing nitrogen losses that harm aquatic ecosystems. Reducing fertilizer
application in Africa might seem beneficial globally, yet the result in this region would be even
poorer crop yields without any notable reduction in nitrogen pollution; Africa’s fertilizer use is
already suboptimal for crop yields. What can look like a good or a bad thing globally can prove
exactly the opposite when viewed regionally and locally. What use is a global indicator for a
local issue? As in real estate, location is everything.
Finally, and most importantly, the planetary boundaries are burdened not only with major
uncertainties and weak scientific theory - they are also politically problematic. Real world
environmental challenges like nitrogen pollution, freshwater consumption and land-use change
are ultimately a matter of politics, in the sense that there are losers and winners, and solutions
have to be negotiated among many stakeholders. The idea of a scientific expert group
determining top-down global limits on these activities and processes ignores these inevitable
trade-offs and seems to preclude democratic resolution of these questions. It has been argued
that (Steffen et al 2011):
Ultimately, there will need to be an institution (or institutions) operating, with authority, above the
level of individual countries to ensure that the planetary boundaries are respected. In effect,
such an institution, acting on behalf of humanity as a whole, would be the ultimate arbiter of the
myriad trade-offs that need to be managed as nations and groups of people jockey for economic
and social advantage. It would, in essence, become the global referee on the planetary playing
field.
Here the planetary boundaries framework reaches its logical conclusion with a political scenario
that is as unlikely as it is unpalatable. There is no ultimate global authority to rule over humanity
or the environment. Science has a tremendously important role to play in guiding environmental
management, not as a decider, but as a resource for deliberative, evidence-based decision
making by the public, policy makers, and interest groups on the challenges, trade-offs and
possible courses of action in negotiating the environmental challenges of societal development
(DeFries et al 2012). Proposing that science itself can define the global environmental limits of
human development is simultaneously unrealistic, hubristic, and a strategy doomed to fail.
References cited
Bass, S. (2009) Planetary boundaries: keep off the grass. Nature Reports Climate Change, 113-
114. <http://www.nature.com/climate/2009/0910/full/climate.2009.94.html>
Brook, B.W., Ellis, E.C., Perring, M.P., Mackay, A.W., Blomqvist, L. (2013) Does the terrestrial
biosphere have planetary tipping points? Trends in Ecology & Evolution 28, 396-401.
<http://dx.doi.org/10.1016/j.tree.2013.01.016>
DeFries, R., Ellis, E., Chapin Iii, F.S., Matson, P., Turner Ii, B.L., Arun, A., Crutzen, P., Field, C.,
Gleick, P., Kareiva, P., Lambin, E., Ostrom, E., Sanchez, P., Syvitski, J., Liverman, D.
(2012) Planetary Opportunities: A Social Contract for Global Change Science to
Contribute to a Sustainable Future. BioScience 62, 603-606.
<http://dx.doi.org/10.1525/bio.2012.62.6.11>
Nordhaus, T., Shellenberger, M., Blomqvist, L., (2012) The Planetary Boundaries Hypothesis: A
Review of the Evidence. The Breakthrough Institute, Berkeley, California.
<http://bit.ly/PB_Review>
Rockstrom, J., W. Steffen, K. Noone, A. Persson, F. S. Chapin, E. F. Lambin, T. M. Lenton, M.
Scheffer, C. Folke, H. J. Schellnhuber, B. Nykvist, C. A. de Wit, T. Hughes, S. van der
Leeuw, H. Rodhe, S. Sorlin, P. K. Snyder, R. Costanza, U. Svedin, M. Falkenmark, L.
Karlberg, R. W. Corell, V. J. Fabry, J. Hansen, B. Walker, D. Liverman, K. Richardson,
P. Crutzen, and J. A. Foley. 2009. A safe operating space for humanity. Nature 461:472-
475. <http://www.nature.com/nature/journal/v461/n7263/full/461472a.html>
Steffen, W., Rockström, J., Costanza, R. (2011) How Defining Planetary Boundaries Can
Transform Our Approach to Growth. Solutions 2 (3)
<http://www.thesolutionsjournal.com/node/935>
Steffen, W., Richardson, K., Rockström, J., Cornell, S.E., Fetzer, I., Bennett, E.M., Biggs, R.,
Carpenter, S.R., de Vries, W., de Wit, C.A., Folke, C., Gerten, D., Heinke, J., Mace,
G.M., Persson, L.M., Ramanathan, V., Reyers, B., Sörlin, S. (2015) Planetary
boundaries: Guiding human development on a changing planet. Science. In press

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A Response to a New Estimate of Planetary Boundaries

  • 1. The Limits of Planetary Boundaries Erle Ellis, Barry Brook, Linus Blomqvist, Ruth DeFries Part of a running Dot Earth discussion of good paths in the Age of Us – the Anthropocene Steffen et al (2015) revise the “planetary boundaries framework” initially proposed in 2009 as the “safe limits” for human alteration of Earth processes (Rockstrom et al 2009). Limiting human harm to environments is a major challenge and we applaud all efforts to increase the public utility of global-change science. Yet the planetary boundaries (PB) framework - in its original form and as revised by Steffen et al - obscures rather than clarifies the environmental and sustainability challenges faced by humanity this century. Steffen et al concede that “not all Earth system processes included in the PB have singular thresholds at the global/continental/ocean basin level.” Such processes include biosphere integrity (see Brook et al 2013), biogeochemical flows, freshwater use, and land-system change. “Nevertheless,” they continue, “it is important that boundaries be established for these processes.” Why? Where a global threshold is unknown or lacking, there is no scientifically robust way of specifying such a boundary - determining a limit along a continuum of environmental change becomes a matter of guesswork or speculation (see e.g. Bass 2009; Nordhaus et al 2012). For instance, the land-system boundary for temperate forest is set at 50% of forest cover remaining. There is no robust justification for why this boundary should not be 40%, or 70%, or some other level. While the stated objective of the PB framework is to “guide human societies” away from a state of the Earth system that is “less hospitable to the development of human societies”, it offers little scientific evidence to support the connection between the global state of specific Earth system processes and human well-being. Instead, the Holocene environment (the most recent 10,000 years) is assumed to be ideal. Yet most species evolved before the Holocene and the contemporary ecosystems that sustain humanity are agroecosystems, urban ecosystems and other human-altered ecosystems that in themselves represent some of the most important global and local environmental changes that characterize the Anthropocene. Contrary to the authors’ claim that the Holocene is the “only state of the planet that we know for certain can support contemporary human societies,” the human-altered ecosystems of the Anthropocene represent the only state of the planet that we know for certain can support contemporary civilization. Human alteration of environments produces multiple effects, some advantageous to societies, such as enhanced food production, and some detrimental, like environmental pollution with toxic chemicals, excess nutrients and carbon emissions from fossil fuels, and the loss of wildlife and their habitats. The key to better environmental outcomes is not in ending human alteration of environments but in anticipating and mitigating their negative consequences. These decisions and trade-offs should be guided by robust evidence, with global-change science investigating the connections and tradeoffs between the state of the environment and human well-being in
  • 2. the context of the local setting, rather than by framing and reframing environmental challenges in terms of untestable assumptions about the virtues of past environments. Even without specifying exact global boundaries, global metrics can be highly misleading for policy. For example, with nitrogen, where the majority of human emissions come from synthetic fertilizers, the real-world challenge is to apply just the right amount of nitrogen to optimize crop yields while minimizing nitrogen losses that harm aquatic ecosystems. Reducing fertilizer application in Africa might seem beneficial globally, yet the result in this region would be even poorer crop yields without any notable reduction in nitrogen pollution; Africa’s fertilizer use is already suboptimal for crop yields. What can look like a good or a bad thing globally can prove exactly the opposite when viewed regionally and locally. What use is a global indicator for a local issue? As in real estate, location is everything. Finally, and most importantly, the planetary boundaries are burdened not only with major uncertainties and weak scientific theory - they are also politically problematic. Real world environmental challenges like nitrogen pollution, freshwater consumption and land-use change are ultimately a matter of politics, in the sense that there are losers and winners, and solutions have to be negotiated among many stakeholders. The idea of a scientific expert group determining top-down global limits on these activities and processes ignores these inevitable trade-offs and seems to preclude democratic resolution of these questions. It has been argued that (Steffen et al 2011): Ultimately, there will need to be an institution (or institutions) operating, with authority, above the level of individual countries to ensure that the planetary boundaries are respected. In effect, such an institution, acting on behalf of humanity as a whole, would be the ultimate arbiter of the myriad trade-offs that need to be managed as nations and groups of people jockey for economic and social advantage. It would, in essence, become the global referee on the planetary playing field. Here the planetary boundaries framework reaches its logical conclusion with a political scenario that is as unlikely as it is unpalatable. There is no ultimate global authority to rule over humanity or the environment. Science has a tremendously important role to play in guiding environmental management, not as a decider, but as a resource for deliberative, evidence-based decision making by the public, policy makers, and interest groups on the challenges, trade-offs and possible courses of action in negotiating the environmental challenges of societal development (DeFries et al 2012). Proposing that science itself can define the global environmental limits of human development is simultaneously unrealistic, hubristic, and a strategy doomed to fail. References cited Bass, S. (2009) Planetary boundaries: keep off the grass. Nature Reports Climate Change, 113- 114. <http://www.nature.com/climate/2009/0910/full/climate.2009.94.html>
  • 3. Brook, B.W., Ellis, E.C., Perring, M.P., Mackay, A.W., Blomqvist, L. (2013) Does the terrestrial biosphere have planetary tipping points? Trends in Ecology & Evolution 28, 396-401. <http://dx.doi.org/10.1016/j.tree.2013.01.016> DeFries, R., Ellis, E., Chapin Iii, F.S., Matson, P., Turner Ii, B.L., Arun, A., Crutzen, P., Field, C., Gleick, P., Kareiva, P., Lambin, E., Ostrom, E., Sanchez, P., Syvitski, J., Liverman, D. (2012) Planetary Opportunities: A Social Contract for Global Change Science to Contribute to a Sustainable Future. BioScience 62, 603-606. <http://dx.doi.org/10.1525/bio.2012.62.6.11> Nordhaus, T., Shellenberger, M., Blomqvist, L., (2012) The Planetary Boundaries Hypothesis: A Review of the Evidence. The Breakthrough Institute, Berkeley, California. <http://bit.ly/PB_Review> Rockstrom, J., W. Steffen, K. Noone, A. Persson, F. S. Chapin, E. F. Lambin, T. M. Lenton, M. Scheffer, C. Folke, H. J. Schellnhuber, B. Nykvist, C. A. de Wit, T. Hughes, S. van der Leeuw, H. Rodhe, S. Sorlin, P. K. Snyder, R. Costanza, U. Svedin, M. Falkenmark, L. Karlberg, R. W. Corell, V. J. Fabry, J. Hansen, B. Walker, D. Liverman, K. Richardson, P. Crutzen, and J. A. Foley. 2009. A safe operating space for humanity. Nature 461:472- 475. <http://www.nature.com/nature/journal/v461/n7263/full/461472a.html> Steffen, W., Rockström, J., Costanza, R. (2011) How Defining Planetary Boundaries Can Transform Our Approach to Growth. Solutions 2 (3) <http://www.thesolutionsjournal.com/node/935> Steffen, W., Richardson, K., Rockström, J., Cornell, S.E., Fetzer, I., Bennett, E.M., Biggs, R., Carpenter, S.R., de Vries, W., de Wit, C.A., Folke, C., Gerten, D., Heinke, J., Mace, G.M., Persson, L.M., Ramanathan, V., Reyers, B., Sörlin, S. (2015) Planetary boundaries: Guiding human development on a changing planet. Science. In press