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The metaphor is not a matter of language but of thought and reason (Lakoff ) Introduction Metaphors are more than rhetorical flourishes and idioms (Lakoff ; Thibodeau & Boroditsky ); they are tools for communicating complex concepts, opening ideas up for discussion, and processing information in all areas of knowledge and in everyday life (Lakoff & Johnson ; Väliverronen ; Carpenter et al . ). Consequently, they affect how we think and act with respect to societal concerns (Pickett et al . ; Thibodeau & Boroditsky ). Metaphors are common in ecological theory, where they help us understand complex concepts such as “niche,” “ecosystem,” or “resilience” that can perhaps be better understood thanks to the judicious use of metaphors (Carpenter et al . ; Pickett & Cadenasso ). They have also been very useful in conservation particularly for communicating problems that are not immediately apparent or clear to a wider public, for example, greenhouse gases, or acid rain (Väliverronen & Hellsten ), and environmental sustainability (Larson ). The purpose of this article is to present two complementary metaphors regarding ecosystem flows: leaks and clogs , and the terms describing the related actions: leak plugging and clog removal . These metaphors can help scientists and practitioners to understand and communicate in simple language and powerful imagery two crucial concepts: (1) the role of anthropogenic disturbances in altering flows among ecosystems, compromising not only one ecosystem but also its neighbors and (2) why ecological restoration needs to focus beyond specific and obvious disturbances and consider also the degraded ecosystems in its landscape or seascape context. Humanity's natural capital (Costanza et al . ; Blignaut & Aronson ), represented as stocks of matter, energy, information, and species within ecosystems, is not uniformly distributed in space, indeed, it flows across ecosystem boundaries. Ecosystems' equilibria—or meta‐stability—depend on a relatively balanced net flow of inputs and outputs. This is, of course, not a static balance; it is often disrupted by natural disturbances that interfere with the rate of inflows and outflows. This may cause loss or accumulation of any element, sometimes dramatically so when the disturbance is “catastrophic.” Typically, however, ecosystems are resilient, and after temporary upsets the flows usually return to a net exchange of zero, at least within the timeframe of the Holocene. Anthropogenic disturbances, in contrast, can drastically affect these natural flows between an ecosystem and its surroundings, causing a permanent loss or accumulation of any element that will have a transformative effect on the ecosystem. We call these significant alterations in flow leaks, and clogs, respectively, and advocate the need to restore both. We limit our discussion to anthropogenic leaks and clogs because these are the ones most likely to cause significant and recurrent alterations and loss of natural capital, and to which society should devote much more attention and resources in efforts to restore and transition toward sustainability. In the environmental sciences, the concept of “leakiness” has been sparsely used, and always in the context of anthropogenic disturbance. It was first used in the terrestrial ecosystems ecological literature in the context of nutrient loss and its relation to functional complexity (Van Voris et al . ; Lamont ). Recently, the term leakiness was introduced in the restoration ecology literature in two different and specific ways: (1) to refer to species loss (Aronson & Le Floc′h ) and (2) to name an index of landscape health that measures lack or loss of soil retention by vegetation clumps in arid and semiarid environments (Ludwig et al . ; Bautista et al . ; Ludwig et al . ). In all cases, the metaphor refers to a condition of an ecosystem, but does not refer to the process that alters the overall state of the ecosystem. Perhaps due to the very specific contexts in which it has been defined and used, this metaphor has not caught on or been developed in the various relevant literatures. Here, we refine and expand its definition and application, and introduce the complementary (converse) concept of accumulation, due to clogs, to generate a more powerful and more broadly applicable set of metaphors. Ecosystem leaks and clogs: redefining and expanding the concept of leakiness We propose a broad definition for ecosystem leaks that refers to any net loss of natural capital from any ecosystem with the potential of exerting a long‐term transformative effect . This can refer to losses of matter in general (e.g., soil, litter, nutrients, or water), energy, information, or species. Severe leaks negatively affect ecosystem functionality, structure, and composition, as well as interactions among ecosystems (Figure ). Consequently, there are adverse effects on the flow of ecosystem services to society (see below). Leaks and clogs among interacting ecosystems illustrated schematically. Panel A shows a landscape with balanced inflows and outflows among ecosystems 1, 2, and 3. Panel B shows changes in ecosystem flows and state with relative size of arrows representing relative changes in the amounts of material in transit; (+) or (–) signs indicate increased or decreased flow rates relative to initial conditions (Panel A). The black ecosystem (1) is “leaking” materials or energy toward the gray ecosystem (2), causing a clog (represented by the enlarged bulge on the right and accumulation of black): the clog in (2) changes the nature of the flow from (2) to a third (3) ecosystem (represented by a mixed colored arrow. The leak of materials from (1) can also affect (3) by the reduced availability of materials that now accumulate in (2). Hence, transfers between (1) and (3) and from (3) back to (2) may also be affected. Effects of a leak can be reciprocal or operate in a more complex fashion at the level of an ecosystem network, though cascading effects. Ecosystem leaks occur when—among other causes—human activities intensify outflows of a given element, causing a significant and continued net deficit in its stocks. In terrestrial Mediterranean Basin ecosystems, for example, volatilization of soil‐borne nitrogen triggered by natural wildfires represent recurrent natural ecosystem outflows that occur at intervals of years or decades, yet nitrification is sufficient to compensate for these outflow pulses (Blondel et al . ). However, anthropogenic activities in this region increase fire frequency at least 16‐fold (Jiménez‐Bermúdez ), turning an average nitrogen outflow into a “leak.” Similarly, anthropogenic underground peat fires in Kalimantan, Indonesia, that have run for at least a decade (Brown ), result in carbon leaks in the order of 3–8% of the carbon stocks per year (Page et al . ). A leak also entails the loss of ecological “memory” essential to an ecosystem's capacity to recover from profound disturbance. A topsoil leak, for example, often leads to ecologically detrimental outflows of water, sediments, nutrients, or seeds, and even the loss of drainage networks, soil profile, microbial and microarthropod communities, and soil banks. All these ecosystem components are the outcomes of historical and largely unrepeatable sequences of past and ongoing events and interactions. Beyond a certain threshold, loss of these abiotic and biotic legacies compromises the resources required for ecosystem reorganization after profound disturbance. This loss of “ecological memory” (Bengtsson et al . ) jeopardizes the historical continuity and resilience in ecosystems—both of which are necessary for the maintenance of natural capital (Brand ) and, ultimately, for the sustainable delivery of ecosystem services (Ekins et al . ). Whereas a leak refers to outflows or losses, a clog refers to accumulation. We define an ecosystem clog as a total or partial obstruction in the natural flows of natural capital within an ecosystem . A clog blocks, or otherwise impairs, the flow of one or more ecosystem element or service. Clogging occurs when human activities interfere with an ecosystem in such a way that the inputs become excessive with regard to the outputs, either because the outflows are blocked or because the inputs are in excess (Figure ). For example, a dam reduces or blocks the regular outflows of water from a basin, causing water accumulation and, consequently soil water logging and flooding. The short‐term consequence of this is often the death of most terrestrial organisms, and a pulse of decomposition and accumulation of organic matter, causing the natural ecosystem to dysfunction, or destroying it altogether. Clogging can also occur when an ecosystem receives inordinate amounts of materials for an adjacent ecosystem, in amounts or rates beyond the recipient ecosystem's capacity to eliminate it effectively and quickly. For example, sediments leaked from a quarry may result in a silt discharge too large to be washed away from the gravel bed of an adjacent river, with severe impacts on aquatic species that rely on such beds for spawning (FISRWG ). Another example of a clog caused by a leak is when a river dumps large amounts of silt into a lagoon, where it behaves as an immiscible fluid that interferes with the functioning, structure, and composition of that wetland system (Aronson et al . ). Leaks and clogs are often related and can have cascading effects The fact that leaks in one ecosystem can cause a clog in another (Figure ), and vice versa, invites us to expand our vision of how restoration should be done. If a clog is identified in an ecological system, we should not only think about fixing the clog but also about identifying and repairing the leak that caused the clog in the first place. Similarly, we should be aware that a leak can lead to clogs in an adjacent ecosystem, an additional reason for it to be addressed quickly and effectively. This forces scientists, practitioners—and the general public—to look beyond the target ecosystem. Permanent solutions to conservation and restoration problems require looking beyond the immediate leak or clog. Although a leak can be fixed and leave no apparent trace of its occurrence, there is the additional challenge of dealing with the unintended or unforeseen consequences of the leaked materials in the adjacent ecosystem. Disturbances that warrant active investment in restoration rarely affect a single ecosystem but rather tend to create cascading events that affect adjacent ones as well (Figure ). For example, a leak of nutrients from a fertilized cropland may result in the eutrophication of an adjacent lake and the load of silt, fresh water, or nutrients generates severe clogs. Similarly, a mudslide “leaking” down a mountain slope will often cause a “clog” in the riverbed downslope (Figure ). In some cases, the resulting clog can cause even more harm than the leak it originated from. For example, the Deep Water Horizon oil spill in 2010 leaked an estimated 4.5 million barrels of crude oil that contained 40% methane, from deep in the sea floor into the waters and beaches of the Gulf of Mexico where these materials never occur and there are no mechanisms for their transformation, incorporation, or elimination. And so they clogged these ecosystems (Kessler et al . ). The result of this clogging was toxicity and interference with the food chain and reproduction, and the concomitant loss of life (Mishra et al . ), productivity (McCrea‐Strub et al . ), and species richness (Campagna et al . ). Illustration of an anthropogenic leak in a tropical watershed of SE Brazil. A major “leak” in topsoil and vegetation was caused by inappropriate roadwork in this mountainous region, causing a “clog” in the river downslope (not shown). A tunnel would have been a better solution. Photo reproduced with permission of André Nave. Leaks and clogs can succeed one another in a cascade of effects and reinforcing feedbacks. For example, when a dam clogs a retention basin, a significant amount of nutrients and fine‐grained sediments become deposited (Baxter ). This triggers numerous leaks and clogs. As the suspended sediment load is reduced downstream, scouring lowers the streambed and erodes the stream banks, which often results in soil loss and incised stream channels (FISRWG ). The High Dam of Aswan (Egypt) provides a specific case that illustrates interrelated clog and leak effects. In addition to the obvious clogging of water that reduces water availability downstream, the newly erected dam retained a significant amount of dissolved silt that for decades was used in a nearby brick industry. To make up for this reduction and obtain the necessary materials, brick manufacturers excavated over 1,000 Km 2 to the depth of the groundwater table, and exported (leaked) that material (White ). In addition to this “leak,” the dam causes a loss of ca. 20 million cubic meters of water per year (to evaporation and seepage), which otherwise would have transited downstream (Waterbury ). Finally, the list of dam‐induced “clogs” at Aswan also includes the invasion of water hyacinth ( Eichornia crassipes [Mart.] Solms.), water pollution, salinization, and water logging of soils that, in turn, have triggered a “cascade” of further “leaks” in cultural heritage, and also biodiversity and losses of millions of hectares of highly productive cultivated land (Benedick ). The cascading repercussions of leaks and plugs can extend beyond the realm of ecological systems to affect the human world directly. Because the various forms of capital (natural, social, economic) are interlinked (De Groot et al . ), leaks in one kind of capital will most likely affect the others. A species leak from an ecosystem, for example, is likely to negatively affect ecosystem services, income, traditions, and cultural beliefs in those human communities that depend in part on those vulnerable and vanishing species. Similarly, clogs can cause serious harm to social well‐being if they cause the redistribution of materials in a way that hinders access to ecosystem goods and services for some and allow excesses of these goods and services to others (Myers & Kent ; Boardman et al . ). These further implications reinforce the notion that ecological restoration should involve a broader long‐term view and a landscape perspective that goes beyond treating the symptoms or specific disturbances. “Leaks” and “clogs” as didactical metaphors for conservation and restoration practice Metaphors help us understand what is happening through powerful images and prompt us into action by evoking emotions (Väliverronen ; Väliverronen & Hellsten ; Larson ). Hence, they can be very powerful didactic tools in discussing environmental and ecological issues (Larson ). In the broad context we address here, leaks, leakiness, and leak plugging (and their counterparts—clogs, clogging, and clog removal) have great potential as metaphors for communication, education, consensus building, transdisciplinary research, and problem solving among people engaged in conservation, restoration, and related disciplines (Pickett et al . ). This is language that anyone can understand and respond to, particularly if it is accompanied by illustrations (Figure ) and examples (Figure ) that help convey the message. Because the terms leaks and clogs are simple, everyday words that convey common images, they are particularly useful in explaining these concepts to local communities and other stakeholders. Furthermore, they translate well to other languages (e.g., “fugas” and “atascos” in Spanish; “fuites” and “bouchons” or “caillots” in French), a precondition to make these concepts universal, and cause little meaning loss in translation (Dobrzyńska ; Schäffner ; Meifang ). Thus, they can also help convey messages beyond scientific circles to the wider public, including corporate, international and national legislative audiences where clear concepts and practical tools for sustainability and conservation science need to be heard and integrated in policy debates. These metaphors are also effective for training undergraduate and master students in the analysis of ecosystem impairment. Humans are not particularly gifted in the conceptualization and envisioning of dynamic processes. For most students, the descriptors of ecosystem structure, such as species richness, tree density, or stream hydraulic geometry, are far more tangible than ecosystem processes, such as surface runoff, nutrient cycling, or seed dispersion. In this context, the leak and clog metaphors are useful conceptual tools that allow description of dysfunctional systems, not in terms of missing elements (e.g., water availability, scarcity of nutrients, or deforestation), but in terms of processes, from a dynamic perspective (e.g., leaks of water, sediments, or species, and clogs of organic matter or algal blooms). Conclusion We propose that, in a metaphorical sense, restoration and conservation scientists and practitioners are often confronted with the need to repair or plug “leaks” in stocks of natural capital, and to repair or remove “clogs” to the flow of ecosystem goods and services. However, this synthetic view of the disciplines has not often been elicited, possibly for lack of a good image or metaphor. While we do not claim universal applicability, these metaphors can help clarify, refine, and galvanize effective and long‐lasting efforts in landscape scale conservation, management, and restoration. Acknowledgments We warmly thank Paddy Woodworth for helpful comments on previous versions of the manuscript as well as Maria Nanette Roble, Thibaud Aronson, Michael Moens, Nikolay Aguirre, Jesús Muñoz, Gloria Calatayud, Valeria Garcia, Jelte van Andel, Porter P. Lowry II, Richard Hobbs, and two anonymous reviewers. We also thank Amada Pérez, Mar Soler, Dúval Cueva, Carlos Cajas, Melinda Hofmann, Javier Salgado, Bayanor Santana, and Alicia Maraver, who contributed to the initial development of these ideas. L.B. was funded by the Madrid Regional Government, Project REMEDINAL‐2, S2009/AMB‐1783.
Conservation Letters – Wiley
Published: Nov 1, 2013
Keywords: ; ; ; ; ;
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