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RESEARCH ( RESEARCHARTICLE <br />reversible. The challenge to the research commu- <br />nity is to develop the knowledge base that allows <br />the screening of chemicals, before they are re- <br />leased into the environment, for properties that <br />may predispose them toward becoming global <br />problems. <br />As a first step toward meeting this challenge, <br />the three conditions outlined above have been <br />used as the basis for identifying scenarios of <br />chemical pollution that fulfill the conditions and <br />as a next step for pinpointing chemical profiles <br />that fit the scenarios (28). This proposal consti- <br />tutes a first attempt at adding the Earth - system <br />perspective when assessing hazard and risk of <br />chemicals and offers a vision for a systematic ap- <br />proach to a complex management situation with <br />many unknowns. <br />Despite this progress in developing an Earth - <br />system- oriented approach, there is not yet an <br />aggregate, global -level analysis of chemical pol- <br />lution on which to base a control variable or a <br />boundary value. It may also serve little purpose <br />to define boundary values and control varia- <br />bles for a planetary boundary of this complexity. <br />Nevertheless, there is a potential threat from <br />novel entities to disrupt the functioning of the <br />Earth - system and society needs to learn how to <br />mitigate these unknown risks and manage chem- <br />icals under uncertainty (28, 73). <br />Some precautionary and preventive actions <br />can be considered. These may include a stronger <br />focus on green chemistry (78), finding synergies <br />with risk- reducing interventions in other fields <br />such as occupational health (79), paying more <br />attention to learning from earlier mistakes (80, <br />81), and investing in science to better under- <br />stand and monitor vital Earth- system processes <br />in order to be able to detect disruptive effects <br />from novel entities as early as possible. <br />Hierarchy of boundaries <br />An analysis of the many interactions among the <br />boundaries (table S3 and fig. S10) suggests that <br />two of them — climate change and biosphere <br />integrity —are highly integrated, emergent system - <br />level phenomena that are connected to all of the <br />other PBs. They operate at the level of the whole <br />Earth system (7) and have coevolved for nearly <br />4 billion years (82). They are regulated by the <br />other boundaries and, on the other hand, pro- <br />vide the planetary -level overarching systems with- <br />in which the other boundary processes operate. <br />Furthermore, large changes in the climate or in <br />biosphere integrity would likely, on their own, <br />push the Earth system out of the Holocene state. <br />In fact, transitions between time periods in Earth <br />history have often been delineated by substantial <br />shifts in climate, the biosphere, or both (82, 83). <br />These observations suggest a two -level hierar- <br />chy of boundaries, in which climate change and <br />biosphere integrity should be recognized as core <br />planetary boundaries through which the other <br />boundaries operate. The crossing of one or more <br />of the other boundaries may seriously affect hu- <br />man well-being and may predispose the trans- <br />gression of a core boundary(ies) but does not by <br />itself lead to a new state of the Earth system. This <br />hierarchical approach to classifying the bounda- <br />ries becomes clearer by examining in more detail <br />the roles of climate and biosphere integrity in the <br />functioning of the Earth system. <br />The climate system is a manifestation of the <br />amount, distribution, and net balance of energy <br />at Earth's surface. The total amount of energy <br />sets the overall conditions for life. In Earth's cur- <br />rent climate, a range of global surface temper- <br />atures and atmospheric pressures allows the three <br />phases of water to be present simultaneously, <br />with ice and water vapor playing critical roles in <br />the physical feedbacks of the climate system. The <br />distribution of energy by latitude, over the land <br />and sea surfaces, and within the ocean plays a <br />major role in the circulation of the two great <br />fluids, the ocean and the atmosphere. These sys- <br />temic physical characteristics are key spatial de- <br />terminants of the distribution of the biota and <br />the structure and functioning of ecosystems and <br />are controllers of biogeochemical flows. <br />Biosphere integrity is also crucial to Earth - <br />system functioning, where the biosphere is de- <br />fined as the totality of all ecosystems (terrestrial, <br />freshwater, and marine) on Earth and their biota <br />(32). These ecosystems and biota play a critical <br />role in determining the state of the Earth system, <br />regulating its material and energy flows and its <br />responses to abrupt and gradual change (7). Di- <br />versity in the biosphere provides resilience to <br />terrestrial and marine ecosystems (83, 84). The <br />biosphere not only interacts with the other plan- <br />etary boundaries but also increases the capacity <br />of the Earth system to persist in a given state under <br />changes in these other boundaries. The ultimate <br />basis for the many roles that the biosphere plays <br />in Earth - system dynamics is the genetic code of <br />the biota, the basic information bank that de- <br />fines the biosphere's functional role and its ca- <br />pacity to innovate and persist into the future. <br />Planetary boundaries in a <br />societal context <br />A proposed approach for sustainable develop- <br />ment goals (SDGs) (85) argues that the stable <br />functioning of the Earth system is a prereq- <br />uisite for thriving societies around the world. This <br />approach implies that the PB framework, or <br />something like it, will need to be implemented <br />alongside the achievement of targets aimed at <br />more immediate human needs, such as provi- <br />sion of clean, affordable, and accessible energy <br />and the adequate supply of food. World devel- <br />opment within the biophysical limits of a stable <br />Earth system has always been a necessity [e.g., <br />(86, 87)]. However, only recently, for a number <br />of reasons, has it become possible to identify, <br />evaluate, and quantify risks of abrupt planetary - <br />and biome -level shifts due to overshoot of key <br />Earth - system parameters: (i) the emergence of <br />global - change thinking and Earth - system think- <br />ing (SS); (ii) the rise of "the Planetary" as a rel- <br />evant level of complex system understanding <br />(89 -92); and (iii) observable effects of the rapid <br />increase in human pressures on the planet (I6). <br />The PB approach is embedded in this emerg- <br />ing social context, but it does not suggest how to <br />maneuver within the safe operating space in the <br />quest for global sustainability. For example, the <br />PB framework does not as yet account for the re- <br />gional distribution of the impact or its histor- <br />ical patterns. Nor does the PB framework take <br />into account the deeper issues of equity and cau- <br />sation. The current levels of the boundary pro- <br />cesses, and the transgressions of boundaries that <br />have already occurred, are unevenly caused by <br />different human societies and different social <br />groups. The wealth benefits that these trans- <br />gressions have brought are also unevenly distrib- <br />uted socially and geographically. It is easy to <br />foresee that uneven distribution of causation and <br />benefits will continue, and these differentials <br />must surely be addressed for a Holocene -like <br />Earth - system state to be successfully legitimated <br />and maintained. However, the PB framework as <br />currently construed provides no guidance as to <br />how this may be achieved [although some po- <br />tential synergies have been noted (54)], and it <br />cannot readily be used to make choices between <br />pathways for piecemeal maneuvering within <br />the safe operating space or more radical shifts of <br />global governance (93). <br />The nature of the PB framework implies that <br />two important cautions should be observed when <br />application of the framework to policy or man- <br />agement is proposed: boundary interactions and <br />scale. <br />Boundary interactions <br />The planetary boundaries framework arises from <br />the scientific evidence that Earth is a single, <br />complex, integrated system —that is, the bound- <br />aries operate as an interdependent set [e.g., <br />(94)] (table S1 and fig. S10). Although a system- <br />atic, quantitative analysis of interactions among <br />all of the processes for which boundaries are <br />proposed remains beyond the scope of current <br />modeling and observational capacity, the Earth <br />system clearly operates in well- defined states in <br />which these processes and their interactions <br />can create stabilizing or destabilizing feedbacks <br />(16, 90, 95). This has profound implications for <br />global sustainability, because it emphasizes the <br />need to address multiple interacting environ- <br />mental processes simultaneously (e.g., stabilizing <br />the climate system requires sustainable forest <br />management and stable ocean ecosystems). <br />Scale <br />The PB framework is not designed to be "down - <br />scaled" or "disaggregated" to smaller levels, such <br />as nations or local communities. That said, the <br />PB framework recognizes the importance of <br />changes at the level of subsystems in the Earth <br />system (e.g., biomes or large river basins) on the <br />functioning of the Earth system as a whole. Also, <br />there are strong arguments for an integrated ap- <br />proach coupling boundary definitions at region- <br />al and global levels with development goals to <br />enable the application of "PB thinking" at lev- <br />els (nations, basins, and regions) where policy <br />action most commonly occurs [e.g., (85, 96)]. <br />This update of the PB framework is one step on <br />a longer -term evolution of scientific knowledge to <br />1259855 -8 13 FEBRUARY 2015 • VOL 347 ISSUE 6223 sciencemag.org SCIENCE <br />