ICES Journal of Marine Science ICES Journal of Marine Science (2016), 73(5), 1306– 1318. doi:10.1093/icesjms/fsv192 Contribution to the Symposium: ‘Effects of Climate Change on the World’s Oceans’ Editor ’s Choice Empirical evidence for different cognitive effects in explaining the attribution of marine range shifts to climate change Ingrid E. van Putten 1,2,3 *, Stewart Frusher 2,3, Elizabeth A. Fulton 1,3, Alistair J. Hobday1,3, Sarah M. Jennings 3,4, Sarah Metcalf 5, and Gretta T. Pecl2,3 1 CSIRO Oceans and Atmosphere, GPO Box 1538, Hobart, TAS 7001, Australia Institute for Marine and Antarctic Studies, University of Tasmania, Hobart, TAS 7000, Australia 3 Centre for Marine Socioecology, University of Tasmania, Hobart, TAS 7000, Australia 4 Tasmanian School of Business and Economics, University of Tasmania, Hobart, TAS 7000, Australia 5 Murdoch University, School of Management and Governance, South Street, Murdoch, WA 6150, Australia 2 *Corresponding author: e-mail: [email protected] van Putten, I. E., Frusher, S., Fulton, E. A., Hobday, A. J., Jennings, Sarah M., Metcalf, S., and Pecl, G. T. Empirical evidence for different cognitive effects in explaining the attribution of marine range shifts to climate change. – ICES Journal of Marine Science, 73: 1306– 1318. Received 2 June 2015; revised 27 September 2015; accepted 2 October 2015; advance access publication 23 November 2015. The changing geographical distribution of species, or range shift, is one of the better documented fingerprints of climate change in the marine environment. Range shifts may also lead to dramatic changes in the distribution of economic, social, and cultural opportunities. These challenge marine resource users’ capacity to adapt to a changing climate and managers’ ability to implement adaptation plans. In particular, a reluctance to attribute marine range shift to climate change can undermine the effectiveness of climate change communications and pose a potential barrier to successful adaptation. Attribution is a known powerful predictor of behavioural intention. Understanding the cognitive processes that underpin the formation of marine resource users’ beliefs about the cause of observed marine range shift phenomena is therefore an important topic for research. An examination of the attribution by marine resource users of three types of range shifts experienced in a marine climate change hotspot in southeast Australia to various climate and non-climate drivers indicates the existence of at least three contributing cognitions. These are: (i) engrained mental representations of environmental phenomena, (ii) scientific complexity in the attribution pathway, and (iii) dissonance from the positive or negative nature of the impact. All three play a part in explaining the complex pattern of attribution of marine climate change range shifts, and should be considered when planning for engagement with stakeholders and managers around adaptation to climate change. Keywords: climate change, fisheries, perceptions, range shift. Introduction Climate change, clearly documented in many regions (Burrows et al., 2011; IPCC, 2013; Mora et al., 2013; Poloczanska et al., 2013), is one of many pressures that affect the marine environment, in addition to fishing, pollution, coastal development, and introduced species (Thomas et al., 2004; Halpern et al., 2008). Much science is aimed at ascertaining the mechanisms responsible for ocean changes and to untangling impact pathways to attribute causality between the different pressures, although there have been calls for caution in attributing individual impacts directly to rising # International greenhouse gas emissions (Brander et al., 2011). Parmesan et al. (2011) argue that it is rarely possible to attribute specific responses of individual wild species to human-induced climate change, partly as a result of the difference in scale of broad climate forcing processes and the more “local” climate experience of animals. Nevertheless, a range of studies have been able to directly link observed marine species shifts with the rate and direction of climate shifts across the seascape (Pinsky et al., 2013; Poloczanska et al., 2013; Sunday et al., 2015). There is a high level of scientific consensus on the contribution of humans to climate change (IPCC, 2013); however, the level of public Council for the Exploration of the Sea 2015. All rights reserved. For Permissions, please email: [email protected] Empirical evidence for different cognitive effects consensus on the issue is much lower (Charles, 2012; Leviston et al., 2012; Cook et al., 2013). Differences in public consensus on human contribution are linked to factors that determine individual attitudes to climate change which can be driven by personal values, political ideology, the media environment, and personal experience (Boykoff and Boykoff, 2007; McCright, 2011; McCright and Dunlap, 2011; Whitmarsh, 2011). Aside from beliefs and attitudes, which are precursors of behaviour (Ajzen, 1991), many different cognitive biases, such as confirmation and normalcy bias, also contribute to behavioural differences and decision-making within human populations (Kahneman, 2011). In the context of the public’s acceptance of human-induced climate change and climate-related behaviour and decision-making, a number of psychological barriers have been identified, including “limited cognition about the problem, ideological worldviews that tend to preclude pro-environmental attitudes and behaviour, comparisons with key other people, sunk costs and behavioural momentum, discredence toward experts and authorities, perceived risks of change, and positive but inadequate behaviour change” (Gifford, 2011, p. 290). Insights into the differing levels of public acceptance of climate-related issues come from attribution theory, and the concepts of cognitive dissonance, motivated reasoning, and other cognitive biases. Attribution theory (Heider, 1958) is concerned with how cognitive perception influences the attribution of causes to events or occurrences (Lewandowsky et al., 2012). Attribution is the process of assigning meaning where attribution is an explanation, or an inference (Malle, 2011). Attribution theory allows us to investigate the effects of cognitive dissonance and motivated reasoning on the attribution of a cause to an observed phenomenon. In this paper, we focus on attribution which may provide insight into perceptions of climate-driven changes in the marine environment by marine resource users. Cognitive dissonance is a psychological theory which states that contradicting cognitions serve as a driving force that compels the mind to acquire or invent new thoughts or beliefs, or to modify existing beliefs, so as to reduce the amount of cognitive dissonance (internal mental conflict) between cognitions (Festinger, 1957; Adams, 1973). Similarly, motivated reasoning (Kunda, 1990) provides insight into how motivation influences cognitive representations that drive decision-making. Motivated reasoning posits that people are motivated to selectively search their prior knowledge to support a pre-desired conclusion. The concept of motivated reasoning also provides insight into how people will avoid negative emotion or cognitive dissonance (Lewandowsky et al., 2012). People tend to seek out information that confirms what they already believe and arrive at conclusions consistent with those beliefs. For example, people might construct evidence for their belief that there is no drought from the fact that it is currently raining. However, their ability to arrive at such conclusions is constrained by their ability to construct seemingly reasonable justifications for these conclusions (Kunda, 1990). Both motivated reasoning and cognitive dissonance theories assume reconstruction and justification is associated with behaviour (Bersoff, 1999). Together cognitive dissonance and motivated reasoning theories can account for many cognitive biases. For example, filtering and/or ignoring information that conflicts with existing beliefs (confirmation bias, Nickerson, 1998) allows individuals to avoid the uncomfortable tension that results from having, or reconciling, two conflicting thoughts at the same time, and reinforces current 1307 beliefs. The filtering or ignoring of information is reinforced when attribution is complex (e.g. when the science is not straightforward or is not effectively communicated; Lewandowsky et al., 2012) which in turn influences the attribution of causes to events or occurrences. This same type of cognitive bias, ere information is ignored, is also observed when the impact of accepting the information is negative or comes at a cost (Broad and Wade, 1983). Other cognitive biases that can constrain shifts in attitudes and beliefs about climate change causation are, for instance, the false consensus effect (an overestimation of the extent to which someone’s belief or opinion is typical of the opinion held by others) and pluralistic ignorance (people privately reject a norm they publicly hold—under the false assumption that most others accept the norm; Leviston et al., 2012). The way people give meaning to, explain, or change their belief about events or occurrences is researched in many disciplines (Haidt, 2001; Lewandowsky et al., 2013; Lodge and Taber, 2013), but the science of certain ecological phenomena itself is sometimes difficult for individuals to accept due to the influence of the beforementioned cognitive biases. When evaluating questions of causation in science, the patternseeking function of the human brain may betray us because information may conflict with what our senses perceive. Illustrations of how this manifests empirically are not commonly found in the literature, especially in the context of marine climate change. However, understanding the empirical expression of cognitive dissonance is important, for instance, to effectively guide the design of climate change adaptation strategies (defined here as actions to reduce the impact of climate change) which may require behavioural change. Understanding resource user reasoning will allow tailored adaptation strategies to be developed and, importantly, provides decision makers and scientists with insights from the public they might not have previously considered. Although barriers to adaptation may be reduced, basic scientific process understanding does not automatically affect belief in climate change (Weber and Stern, 2011; Kahan et al., 2012; Tvinnereim and Fløttum, 2015). For example, although scientists attribute certain changes in the marine environment to climate change, similar changes observed by resource users such as fishers (Nursey-Bray et al., 2012; Gledhill et al., 2014), and the general public, do not necessarily receive the same attribution (Lewandowsky et al., 2012). Here, we discuss the insights that attribution, cognitive dissonance, and motivated reasoning theory can offer in explaining differences in ascribing change in the marine environment to climate change. In particular, we explore how cognitive dissonance can affect explanations of causation—specifically with regard to climate-related shifts in the distribution of marine species. We explore this by illustrating marine resource users’ cognitions of three categories of range shift that have been observed in eastern Tasmania, which lies within an ocean warming hotspot (Hobday and Pecl, 2014). Recognizing and being able to attribute the causes of biological change may be a first step to helping reduce barriers to adaptation to climate change (Nursey-Bray et al., 2012). Here, we hypothesize that three factors, either alone or in combination, create a level of cognitive dissonance and that they differentially affect the rejection or acceptance of the role of climate change in observed marine range shifts. These factors are (i) existing engrained mental representations, (ii) the complexity of cause and effect linkages, and (iii) the directional nature of the impact (positive/beneficial or negative/costly). 1308 Marine resource users’ exposure and experience Attribution of the causes of marine environment change is not straightforward, and evidence for the dominant causes of change can take some time to emerge, particularly given the complexity of the climate system (Pauly, 1995; Hobday and Evans, 2013; Parmesan et al., 2013; Chambers et al., 2014). This is particularly evident when attributing changes to anthropogenic causes, with increasing levels of confidence attached to the anthropogenic contribution to warming in over a decade of successive IPCC reports (e.g. IPCC, 2001 vs. 2013). There is some evidence that people struggle to gather and process complex climate science information (Guy et al., 2013). When information is complex, there is a cognitive tendency to find alternative and simpler explanation pathways that more readily fit into existing mental schemes (Sterman and Sweeney, 2007; Kahneman, 2011). Complex climate science information can be made more accessible and cognitively simpler if the actual biological and ecological changes can be observed by users (Kuruppu and Liverman, 2011). One way for the public to visually observe biological and ecological change is through direct exposure and experiences (Keller and McInerney, 2008). For instance, local level experience of the effects of climate events, such as erosion damage and coral bleaching, tends to shape current perception of climate change as a “real” issue and facilitates an understanding of the link (or attribution) between the event, the impact, and climate change (Huntington and Fox, 2005). This is one of the central theories behind establishment of Internet sites where public reporting of range-shifting species (e.g. Range Extension Database and Mapping or Redmap, www.redmap.org.au), phenological events (e.g. ClimateWatch www .climatewatch.org.au), and climate extremes (Witness King Tides http://www.witnesskingtides.org/) can occur. Generally, the perception of risk associated with climate change is that it is remote and removed from direct personal experience (Bord et al., 1998; Stamm et al., 2000; Kirby, 2004; Lowe et al., 2006). Therefore, direct experience of climate impacts can change people’s perception of the risk, increase people’s concern, and ultimately their willingness to change their behaviours or choices (Weber and Stern, 2011; Tam and McDaniels, 2013). On the other hand, direct experience has also been shown to have the opposite effect. Reduced support for any adaptation mounted in response to, for instance, climate change, can occur if there is a belief that the risk posed by the change is inevitable and cannot be prevented (Wolf, 2011). In general, however, the cognitive presence of risk associated with climate change increases through personal direct experience, especially experience associated with abrupt environmental change caused by extreme climatic events, such as floods (Höhle, 2002; Palutikof et al., 2013; Hodgkinson et al., 2014). If climate change is only experienced as a slow and gradual modification of average climate conditions coupled with considerable interannual variation, as is often the case with annual rainfall levels, then climate change is a difficult phenomenon to detect and track accurately based on personal experience (Weber and Stern, 2011). Direct experience of abrupt or fast change is likely to bring the risk of climate change to the fore, but the cognitive presence of climate risk can also be affected by slower changes. Regardless of whether the change is fast or slow, the observer has to have some mental baseline against which to compare the observed change. In other words, an observer has to have both the ability to observe and to put the observation in context. Although there is great diversity both between and within types of marine resource users, fishers in particular are known to be keen I. E. van Putten et al. observers of their environment with many experiencing the marine environment daily. The environment they typically experience is dynamic, affected by seasonality and shifting patterns of ecology and productivity (Hobday and Evans, 2013). Moreover, the marine environment is susceptible to environmental shocks caused by natural events (Coulthard, 2008; Garrabou et al., 2009; Wernberg et al., 2012). Fishers (especially small-scale fishers) are believed to develop intimate, detailed, and functionally oriented knowledge of the marine ecosystems they exploit and the main species they target (Silvano and Begossi, 2012). For the most part, fisher marine-ecological knowledge has a utilitarian purpose (related to catching), but often fishers are known to speculate more broadly on the nature of the marine organisms that they target and influences on the observed patterns of other marine species (Goodwin, 2001; Nursey-Bray et al., 2012; Gledhill et al., 2014). Studies have confirmed that as part of their personal and work experiences, most fishers have observed changes in the marine environment and associated fish populations (Nursey-Bray et al., 2012; Gledhill et al., 2014). Although these changes in the marine environment are often consistent with climate change (Zhang et al., 2011) not all fishers who acknowledge observing climate-consistent change also accept anthropogenic climate change as a driving factor. This observation is not exclusive to the marine environment as other studies have produced similar results related to perceptions and attributions of climatic impacts (Hodgkinson et al., 2014). For instance, in examining perceptions of drought and climate change among Australian farmers, Milne et al. (2008) found that most farmers attribute drought conditions to local stressors rather than climate change alone. Here, we present a clear empirical case for cognitive dissonance in a group of marine resource users, largely composed of recreational and commercial fishers, in northeast Tasmania, Australia. An understanding of dissonance can help to explain why some climate-related changes are more easily accepted than others, with implications for the development and implementation of adaptation options. Methods First, we describe a simple way of framing environmental change and classifying the different types of marine range shift that occur in the case study location. We then outline the data gathering process and method of analysis to evaluate fisher perspectives on these changes in the marine environment. Case study location and local range shift phenomenon The case study region lies within an ocean warming hotspot (Hobday and Pecl, 2014), with observed warming faster than 90% of the worlds’ oceans. Typically, range shifts have been fastest in regions with a greater rate of warming (Burrows et al., 2011; Chen et al., 2011; Neuheimer et al., 2011; Pinsky et al., 2013), and the east coast of Tasmania is no exception with large shifts in many species reported (Ling et al., 2009b; Pitt et al., 2010; Last et al., 2011; Robinson et al., 2015). To aid our analysis, we developed a relatively simple framing characterizing environmental change, and range shifts in particular. First, marine range shifts for any particular species in a region result in an outcome that can be categorized by three factors: the relative change in abundance (increase or decrease shown on the vertical axis in Figure 1) and the ecological effect (neutral/positive or negative shown on the horizontal axis at the top of Figure 1) on the existing ecosystem. Negative ecological outcomes are the highest concern to fishers and other users. The characterization of these two factors Empirical evidence for different cognitive effects 1309 Figure 1. Marine range shift classification according to abundance change, ecological effect, and relative commercial value of the range shifting species. Grey-highlighted cases (i), (ii), and (iii) are discussed in the text. in Figure 1 is a simplification from what in practice is a continuum, but it makes our subsequent analysis tractable. The third factor captures whether the species is commercially valuable; the potential income effect (indicated in the text inside the eight boxes in Figure 1). In this paper, we focus on commercial values, although we recognize that both commercial and non-commercial species can have recreational benefits, and that recreational and commercial activity may not be independent when targeting the same resource. To illustrate marine resource users’ cognitions of change in the marine environment and corresponding attribution (or lack of attribution) to climate change-related marine range shifts, we focus on three types of range shifts in eastern Tasmania where climate has been implicated by scientific studies as a causal factor in each case. The types of range shifts observed in Tasmania (Figure 2 and discussed in detail below) are also observed in other regions of the world. These range shifts are (i) decreasing abundance of existing commercial species with a neutral ecosystem effect (e.g. Sissener and Bjørndal, 2005; Hannesson, 2006, 2007; Stenevik and Sundby, 2007), (ii) increasing abundance of non-commercial species with negative ecosystem impacts, e.g. pests (e.g. Zeidberg and Robison, 2007), and (iii) increasing abundance of new commercial species with a neutral ecosystem effect (e.g. Engelhard et al., 2008; Figure 2). A reduction in abundance of commercial species (case i)— particularly southern rock lobster (Jasus edwardsii)—has been observed on the northeast Tasmanian coast (Last et al., 2011; Green et al., 2012; Robinson et al., 2015). This regional decrease in abundance and commercial catches of southern rock lobster have been attributed by scientists to the impact of climate changedriven sea surface temperature (SST) increases and ocean current changes on larval dispersal and settlement (Pecl et al., 2009, 2014; Johnson et al., 2011; Frusher et al., 2014). Most commercial species in this region generally also have a smaller recreational component. In the same region, a range shifting habitat-modifying species, the sea urchin (Centrostephanus rodgersii) has become more abundant, but with negative ecosystem consequences (case ii, Figure 2). High densities of this urchin lead to over-grazing and loss of kelp forest habitat (Ling et al., 2009b), resulting in urchin barrens (an area where no—or very little—marine vegetation remains) which in turn reduces abundance of commercial species such as rock lobster and abalone (Johnson et al., 2011) thereby reducing biodiversity (Ling, 2008). This native Australian species was first recorded in Tasmania in the late 1970s and has moved steadily southward since (Johnson et al., 2005; Ling et al., 2009b). However, consistent with other research on invasive species in this region (e.g. Valentine and Johnson, 2003; Thresher et al., 2003), the urchin was initially considered an invasive pest species, rather than the first of many range-expanding species. A range of scientific studies now show that the range extension has been facilitated by 1310 I. E. van Putten et al. Figure 2. Three different range shift phenomena along the northeast coast of Tasmania, Australia. CC stands for climate change. Cases (i), (ii), and (iii) are discussed in the text. two factors—larval movements facilitated by the strengthening East Australian Current (EAC) that also penetrates further south (Cai et al., 2005; Ridgway, 2007) and larval survival which is increased by warmer winter temperatures (Ling et al., 2009b). A second example of range-extending species with negative consequences for the environment in this region is an increased frequency of harmful algal blooms usually associated with more northern plankton species (Hallegraeff, 2010) which has led to fishery closures (http://www. dpiw.tas.gov.au/inter.nsf/WebPages/SWIS-92A3LJ?open). The third type of range shift involves arrival of new (and potential future) commercial species not previously abundant in the region (case iii; Figure 2) and now appearing further south due to the extending EAC and increasing water temperature. An octopus species (Octopus tetricus) has been increasingly reported in commercial fisher logbooks on the north Tasmanian coast (Ramos et al., 2014, 2015; Robinson et al., 2015). This species was first reported in 2005 and over the last 7 years has increased to 13% of the commercial catch of octopus in this region (unpublished data, Department of Primary Industries and Water, Wild Fisheries Management Branch Tasmania). A second example involves the eastern rock lobster (Jasus verreauxi) which is common further north off mainland Australia and is now found frequently in Tasmania (Robinson et al., 2015). Many of these future commercial species are initially many recreational until abundance is sufficient to make commercial effort an economic proposition. In addition, recreational fishers are reporting increasingly frequent catches of key recreational game fish, such as snapper and yellowtail kingfish (Last et al., 2011; Robinson et al., 2015), which are popular targets in mainland Australian waters but previously rarely caught in Tasmania, and may become targeted in commercial fisheries in the future. 1311 Empirical evidence for different cognitive effects Data collection From past research, there was some evidence that fishers in this region had been reluctant to acknowledge the impacts of a changing climate on their target species and fishing activities (Nursey-Bray et al., 2012; but see Frusher et al., 2014). Although some scientific uncertainties remain, largely related to the speed and magnitude of change, all examples of the three range shift cases in Tasmania (Figure 2) have been attributed to climate change by scientists (Engelhard et al., 2008; Ling et al., 2009a; Last et al., 2011; Frusher et al., 2014; Pecl et al., 2014; Robinson et al., 2015). An understanding of fisher perceptions with regard to each of these range shifts was gained via semi-structured interviews conducted in northeast Tasmania in February 2013, as part of a large project (Frusher et al., 2013). Interview respondents were contacted primarily by a local member of an independent organization, OceanWatch (http://www.oceanwatch.org.au/), who had been working in the region for a number of years and, as an ex-fisher, had good rapport with local fishers. Some additional respondents were recruited through snowball sampling (Goodman, 1961) and responses to public media. The primary purpose of these interviews was to understand the relationship between adaptive capacity and vulnerability (Metcalf et al., 2013, in press; van Putten et al., 2014). Over a period of 1 month, a total of 35 respondents were interviewed. Interviews were recorded with the respondent’s permission, and took place in the interviewees preferred location and lasted 60 min. New respondents were sought until preliminary analysis showed that no new data and insights were being reported (e.g. Hagerman et al., 2010). At this point, the number of interview respondents was deemed sufficiently robust to draw inferences about the relationship between adaptive capacity and vulnerability. Interview participants were from a variety of industries and backgrounds including commercial fishing, aquaculture, marine tourism, accommodation, retail, restaurants, education, local councils, boat maintenance, and marine safety. All interview participants had strong associations with the local marine environment and were current or retired recreational or commercial fishers, and we collectively refer to them as either fishers or resource users. It is estimated that 60% of local commercial fishers (who operate out of the local port) were interviewed including rock lobster, pippies, abalone, urchin, and finfish fishers. The majority (85%) of respondents were male. The interviews were semi-structured and organized around four topics. First, details of the respondents’ employment and/or business interests were recorded. This included social and economic detail such as how many years they had lived in the local area and their social connections to the community. In the second part of the survey, respondents were asked about their perception of the potential impact of socio-economic changes and changes in the marine environment on their business and their community. In the third section, the focus was narrowed to a description of the impact of (biological) change on marine sectors including the potential flow-on effects. In the final part of the survey, respondents were asked to identify any future opportunities to deal with change and potential adaptations to improve community outcomes. The interviews were free-flowing and the respondents were not specifically asked to comment on the three types of range shift but rather respondent comments about the range shifts were volunteered unprompted. Information provided in interview sections 2 and 3 provided the data used in the analysis. After the interview, the participants were also asked to take home and fill out a survey containing a set of demographic questions (such as age, time resident in the locality, education, community memberships, and income) and to indicate their level of involvement in different community organizations and activities. Fifty per cent of interviewees mailed this survey to the researchers in the weeks following the interviews. The vulnerability and adaptive capacity analyses are reported in Metcalf et al. (2013, in press) and van Putten et al. (2014). Recorded interviews were available for 24 respondents which were subsequently re-analysed for this study and a new database constructed to determine contributing cognitions of the three types of range shift. Although a total of 35 people were interviewed, participants who indicated they did not want the interview recorded, or in cases where the recording was of unusable quality due to back ground noise, these were excluded from the analysis. The information contained within the interviews (further referred to as the data) was entered in the database according to the number of mentions of topics, organized in four themes (Table 1) with each theme comprising between three and six subgroups. Each subgroup further consisted of several items. For example, data were recorded at the individual species level in each of the subgroups of the species change theme (using the range shift classification shown in Figures 1 and 2). The subgroup “inadequate management controls” contained items such as lack of regulation, wrong size limits, lack of bag limits, or high total allowable catch (TAC) limits. Each of the non-climate and indirect climate explanations were coded according to whether it applied to range shift case (i), (ii), or (iii) or any combination of these three types of range shift. Our results are based on an analysis of the content of the new database by counting each respondent’s number of mentions for each of the themes as they relate to the attribution of climate change to each of the three range shift types. The identified cognitions were later ascribed based on the relative count of climate Table 1. Coded interview data themes and subgroups. Theme Environmental change Species change Non-climate explanations Indirect climate explanations a Subgroup Barrens Turbidity Nutrients Silting/sedimentation Habitat decline Commercial (case i) Pests (case ii) Recreational (case iii)a Unusual sightings Education and science Inadequate management controls Overharvesting Species-specific issuesb (including bycatch) Disease Pollution Change in ocean (temp. and current) Change in drought/rain/floods Other (e.g. change in sea-level, ozone, etc.) The term recreational is used here because initially new species come into the region not in adequate numbers to “support” a commercial fishery. A commercial fishery would/could develop at a later stage if abundances grow thus increasing the commercial viability of catching the species. b This category includes issues that affect abundance, but these effects are indirect, through another species, such as due to an increase in prey species abundance. Another example is where the abundance of a particular species is affected because it is the bycatch species in a fishery for another species. 1312 I. E. van Putten et al. and non-climate mentions for the three range shifts, a broader interpretation of the interview statements, and extant background knowledge (available in the literature and residing with the authors) for each of the range shift phenomena. Results Interviewees who provided the information that we used to characterize the attributions of the three different cases of locally observed range shift were between 39 and 67 years of age (the average age was 52) and had lived in the case study area between 6 and 47 years (an average of 24 years). Despite the relatively long residency of respondents in the local area, most (81%) were not born there, but all indicated they had no intention to move elsewhere in the future. Nineteen respondents (79% of all respondents) had observed general environmental change, such as degradation of habitat and barrens formation, increased turbidity and nutrients, and siltation (38 mentions). Fifteen of these respondents observed general environmental change as well as at least one of the three cases of range shift. Four respondents observed general environmental changes without specifically raising examples in any of the three cases of range shifts. Interview respondents offered a total of 23 non-climate-related explanations for the three types of range shifts observed in the marine environment and included examples from each of the six subgroups (Table 1). As any one non-climate explanation could be mentioned more than once by any interviewee, there were a total of 86 mentions of non-climate explanations. The inadequacy of management controls was the most frequently mentioned explanation (32 times). Respondents mentioned eight different indirect climate-related explanations for range shift 53 times in the interviews, again providing examples of all three subgroups (Table 1). Interviewees were not explicitly asked if they believed in climate change; however, some volunteered an opinion. Only three respondents explicitly indicated that they believed climate change was happening and linked this to warming ocean waters and changing ocean currents. Four respondents expressed uncertainty about whether climate change was occurring but acknowledged there may be a link between changing ocean temperatures and ocean currents and climate change. Two respondents explicitly denied the existence of climate change, although they indicated changing ocean temperatures and changes in the currents were responsible for the increasing abundance of some recreational species. Of specific interest in this research were respondent observations of the three types of range shift. We used the interviews as a basis for understanding marine resource user’s acceptance or rejection of the role of climate change in attributing causal linkages to marine climate change. We illustrate support for our interpretation of the interviewee statements for range shift cases (i), (ii), and (iii) with representative quotes. Reduced abundance of seven commercial species (case i) was mentioned by 38% of respondents for a total of 13 times (Table 2). Non-climate-related explanations were given ten times more frequently for these abundance changes than were climate change explanations (63 vs. 6). Some interviewee statements around nonclimate attributions illustrate the perceived relationship between commercial species and inadequate management controls and overharvesting. For instance, one retired fisher compares the change in biomass levels of what was a virgin fishery (i.e. a fishery that has not yet been significantly affected by harvesting) then to lower biomass levels now due to commercial harvesting. It was rampant with virgin fisheries. We’ve had a reduction of virgin stocks—but that’s everywhere. You fish down virtually every commercial fishery (retired fisher 750010). I know we’ve had an impact with fishing—we’re catching less fish. More to do with habitat not being there—don’t know about the climate (fisher 750004). Crays can go to Flinders Island [a location further north] or somewhere else. . . . Not necessarily something to do with the climate (fisher 750006). Seventy-one per cent of respondents mentioned the increased abundance of eight different pest species in the local area (just over threequarter of these respondents mentioned the urchins). Changing abundance of pest species was mentioned a total of 34 times. A total of 28 non-climate vs. 29 climate explanations were given to explain increasing abundance of non-commercial species with negative ecological impacts (range shift case ii). This was evidenced by a wide range of statements consistent with climate change such as: Why have we got a bay full of jelly fish? . . . .Because of the [extended] currents [bringing them down] (fisher 750003). Changes in the environment are massive. We first noticed the first urchin barrens 15 –20 years ago. The temperatures here are insane it’s so much warmer some of the [commercial fishing] industries are really going to struggle (recreational diver 570027). Table 2. Relative number of climate and non-climate explanations and the number of mentions for three different types of range shift. Range shift type Case i—decreasing abundance of existing commercial species Case ii—increasing abundance of pest species Case iii—increasing abundance of new commercial species a Interviewees mentioning range shift type (proportion) 38% Total number of Total number of non-climate times mentioneda explanations 13 63 Proportion interviewees who mention non-climate explanations only 78% Total number of climate explanations 6 71% 34 29 18% 28 58% 41 30 14% 37 More than one mention possible for each respondent. Empirical evidence for different cognitive effects In other interviews, attributions of environmental change were less obviously related to climate change: 1313 affect the level of rejection or acceptance of the role of climate change in observed marine range shifts. That long string kelp was ripped out and created space for the urchin [that’s why they are here] (retired fisher 850001). The role of existing engrained mental representations as blocks to attribution If the water is warmer there it makes no difference on the barrens—they are here too [where it’s colder] (fisher 750006). It may be that in the absence of accurate or understandable schematic representations (or symbolized and simple representations) that link the elements of climate science to local effects, fishers are inclined to assimilate and associate their observations with existing local pressures for which schemas have been developed (Kuruppu and Liverman, 2011). In this way, individuals can reassert a sense of “control” over uncertainty by cognitively restructuring a situation where one is aware of the likely course of actions and outcomes (Mandler, 1990). Cognitive dissonance could thus be avoided by rejecting or avoiding the information that challenges the belief systems or by interpreting dissonant information in a biased way (Festinger, 1957; Adams, 1973; Bradshaw and Borchers, 2000). The effect of mental models on the differential acceptance of climate change as an explanation for abundance change was evident for all three range shift phenomena (cases i, ii, and iii). More than half of respondents already seem to have a clear mental model for the cause of any abundance change, particularly in relation to the decrease in abundance of existing commercial species (with 78% attribution to exclusively non-climate explanations). In the past, the main explanation (attribution) given by scientists for declines in the abundance of commercial fish species has been overfishing (e.g. Musick et al., 2000; Jackson et al., 2001). In the Tasmanian region, for example, declines in southern rock lobster (SRL) abundance led to implementation of fishery management changes in 1998, including a limit on TAC and the abundance of SRL subsequently increased (Hamon et al., 2009). Due to the apparent effectiveness of this management approach in increasing abundance, there was a deepening of understanding and acceptance that there is a link between overfishing and reduced abundance (Bradshaw, 2004) for most fishers. It is largely the same generation of fishers who are again observing changes in abundance. This overlap of experience and the existence of fishers’ previously hard-won mental model (i.e. it took time to convince fishers that overfishing was occurring and changes in behaviour were needed) may explain the fisher’s tendency to attribute this current abundance change also to overfishing. In other words, based on past experience, fishers associate reductions in the TAC as an appropriate response to overfishing (Costello et al., 2008) and use this to justify their belief that current observed reductions in abundance must therefore be due to overfishing. Recent reductions in TACs in the fishery in response to recruitment declines (which may be related to lesser abundance of females) may further mask the linkages between climate change and fisheries by way of enhancing fishers existing mental models of exploitation driving responses in fishery resources. The concomitant rejection of climate change as an explanation for current reductions in rock lobster abundance may be to avoid cognitive dissonance to the fact that fishers have an existing mental model that attributes reducing abundance to overfishing, which was the main reason respondents gave in the interviews. Moreover, during the earlier period when overfishing was the main reason for reduced fish abundance, fishers found overfishing difficult to accept. It required a significant amount of effort for fishers to accept overfishing as the reason evidenced for instance, by the number of public and private meetings between managers, fishers, and scientists that took place at the time. Furthermore, a long time elapsed between scientific evidence of overfishing, fisher The [urchin] Centro is definitely the biggest [environmental] change—but I don’t know why they are here (professional diver 750013). Everyone complains about the weed in the bay—we’ve watched it become more prolific—but maybe it’s coming back now as it was 80 years ago (recreational fisher and shop owner 750026). The increased abundance of 22 different fish species that had not previously been observed in large numbers in the local area was mentioned by 58% of respondents, a total of 41 times (we refer to these as recreational species as initially abundances are too low to support a commercial fishery). A greater number of climate explanations (37) vs. non-climate explanations (30) were given for the changing abundance range shift type iii. Although there remained a large number of mentions of non-climate explanations, the increased abundance of new commercial species (case iii) most often invoked climate change (or the symptom of the change expressed in terms of warming ocean waters). Snapper and whiting they are all seen here now and seem to be increasing in numbers (especially in the last 20 years or so). Most of these are from the warmer waters. You’d nearly have to think that way—that it [the current] is bringing them further down (fisher 750002). Now we were catching eels as far down as St Helens in our pots—this year we had flying fish—warm current is closer into shore [and further down] and that’s brought them in (fisher 750019). See more whales now—pretty much consistently—don’t know why. We see some flying fish in summer and they seem to come down in the warmer water (fisher 750028). Without any proof I would say I believe in climate change. For instance, all of a sudden we’re starting to get new species (e.g. tailor that are New South Wales or Queensland fish) not just in ones or twos (recreational fisher and diver 750030). Overall, these results show that climate change was invoked to different degrees when explaining how the three types of range shift may have occurred. Discussion As set out in the introduction to this paper, we hypothesize that attribution theory, cognitive dissonance, and motivated reasoning may help explain fishers’ ascription of climate change as a cause of the observed marine range shifts phenomena described in the Results section. We contend that cognitive dissonance is central to the ascription of climate change as a cause of the three range shift phenomena. In particular, the internal mental conflict created by (i) existing engrained mental representations, (ii) the complexity of the science between cause and effect, and (iii) the directional nature of the impact (positive/beneficial or negative/costly) may 1314 support, and management change. This may partly explain why it is more difficult to now shift this mental model. People have invested in the mental model and may subconsciously hold strongly to it. We acknowledge that, as in any survey involving people, some “strategic” answers (Dunning, 1999) might have been given by fishers whose aim was to make a point. For instance, fishers may have answered that there was no reduced abundance even if they might have observed it, due to their wariness of governments reducing TACs as a consequence. Similarly, fishers may have wanted to appear consistent with what they thought their peers might be saying in response to the same question. This phenomenon was previously referred to as pluralistic ignorance (Leviston et al., 2012). We do not think this has affected our conclusions here, because of the open discussions that were part of the interview process with a trusted interviewee. Mental schemes may already exist for the arrival of new noncommercial “negative” species. Attribution of the establishment of marine pests to discharge of wastewater from sea freight (Carlton and Geller, 1993) and run-off from some land-based activities (i.e. aquaculture) were mentioned in about one-third of the interviews. However, due to the long period of scientific research, effective science extension, and regional fisheries management meetings, the attribution of the range shifting urchin pest seemed to be increasingly recognized by fishers as climate driven, and mental schemes may thus be in the process of changing. In other words, the successful communication of the extensively studied urchins where the attribution to climate change was established (although somewhat complicated because there is also a potential feedback between urchin success and the lack of large predatory lobsters, Marzloff et al., 2011) seems to be creating a new mental schema for fishers. In contrast, our results indicate a weaker reliance on non-climate explanations and pre-existing mental schema around the arrival of new commercial species. This appears to have left the way open for a more ready attribution of this phenomena to climate change and willingness of fishers to entertain new possibilities as facilitated by the exchange of information of reported new sightings (e.g. www. redmap.org.au, Range Extension Database and Mapping project), or because the arrival can be simply (and intuitively) explained by ocean currents. The role of complexity The complexity of the underlying science linking changes in abundance of marine species and climate change also seems to affect the relative acceptance of climate change as an explanation of the different types of marine range shift. In fact, the complexity of the science, the relative number of existing studies, and the “indirectness” of the impact pathway from climate change to the biological response seemed to compound the adherence to existing schematic representation. The way the southern rock lobster is impacted by climatedriven change (i.e. larval dispersal and settlement) is complex and not well understood by scientists. Interview respondents did not seem to have absorbed the limited science that was available and were uncertain of the link between the complex ecological information and climate change. In contrast, there is a high level of scientific understanding of the way in which new pest species became resident in the region. For instance, the relationship between increasing temperature and the successful survival of organisms under warmer ocean temperatures in winter (Ling et al., 2009b) is relatively straightforward. The science underpinning the arrival of new commercial species is mainly around two interlinked biophysical I. E. van Putten et al. changes: ocean temperature increases, and the strengthening of the EAC (Ridgway, 2007; Frusher et al., 2014). These two concepts were well understood and the idea of fish following their most preferred habitat characteristics, and thus moving south (in the southern hemisphere case) is a relatively tangible concept for fishers. Consequently, the way that the arrival of new species was explained by fishers was not scientifically complex, with one fisher explaining that the fish simply “floated down” on the extending EAC. Negative or positive impact: influence on attribution The degree of acceptance of climate change as an explanation of the different types of marine range shift was not only affected by the existence of fixed mental schemes and scientific complexity, but we contend that it is also affected by whether the effect was positive (beneficial) or negative (costly; Figure 1). There are many cost (or loss) components associated with changing abundance, with some more obvious (direct) than others. For instance, the losses in revenue from reduced catches might be an obvious cost, but the need to learn new catching methods for new species is an indirect outcome and may not be as obvious. An obvious cost (loss) to resource users is associated with decreasing abundance of existing commercial species and results in a negative change in the form of extra financial costs or reduced profit margins. Such negative change can be very difficult to cope with especially for fishers who are already facing tight financial circumstances (more than 90% of fishers indicated that they were “struggling” financially). A small number of interviewed fishers indicated that climate-driven pressure on abundance was seen as a further impost and because they have already suffered financially they were unsure how to cope with further change. For (i) range shift (Figure 2), there is a personal cost in terms of behavioural change (e.g. changing fishing gear, travelling further, generating new expertise, or changing target species) for accepting climate change as a cause of changing abundance or the target species. In contrast, believing that fisheries management actions will contain the problem means there is no perceived pressure for costly large-scale change in practices. Significant costs can be associated with regional establishment of new pest species (i.e. the ecological impact on commercially fished species and/or cost of control and monitoring). The cost impact of pests can change over time, for instance, with development of a commercial harvest of the pest urchin. The shift from being a pest species and a cost, to providing commercial opportunities (and thus beneficial) may be associated with an increasing acceptance of attributing climate change driving this pest species range shift. Fishers may have embraced or may desire the climate-driven change under the assumption that benefits will be substantial (maybe greater than can actually be realized; Kahneman, 2011). New species (case iii) generate a potential (additional or alternative) profit for commercial fishers and recreational opportunities with new recreational game fish species. While range shifts of this type may also involve costs, for instance, acquiring new knowledge and expertise to efficiently catch these new species and establish a commercial enterprise, on first assessment, benefits may outweigh costs. Implications for climate change communication and adaptation The theories mentioned in the introduction may help explain an individual fishers’ rejection or acceptance of attributing marine range shift phenomena to climate change. Interview responses in a case 1315 Empirical evidence for different cognitive effects study area in a marine climate change hotspot in southeastern Australia indicate that existing mental models, scientific complexity, and the relative cost or benefit of the change may all contribute to explaining the different attribution of different types of range shifts (but essentially the same marine climate change phenomena) to climate and non-climate drivers. The increase in SST and the strengthening of the EAC are the main mechanisms through which climate change impacts range shifting species in the focal region. The arrival of new commercial species was the case for which resource users seem to most readily acknowledge an attribution to climate change. We suggest this is because the science was not complex, they had no pre-existing mental model, and impacts were at first glance beneficial. In contrast, reduced abundance (by the poleward movement) of a commercial species was not commonly attributed to climate change. This could be explained by a number of factors including the strong pre-existing mental model that overfishing negatively affects abundance and the difficulty in separating these effects from climate and other drivers. This rejection of the climate change explanation is compounded by the complexity of the science and the clear cost associated with reduced fish abundance. The study shows that the acceptance of one causal link for a change in a particular aspect of an ecosystem (i.e. climate change as an explanation for range shifting species) does not mean that the same causal links for other elements in the same system are also accepted. This information is useful not only when trying to understand human responses to climate-related information, but for managers and policy-makers seeking to advance climate change responses. Understanding on one aspect (e.g. one species) does not necessarily mean further acceptance will be easy or straightforward, and stakeholder engagement processes may need to repeat previous steps on each new issue. It must be emphasized to further unpack the process of attribution of a broad range of climate change-driven effects in the marine environment through targeted surveys. A dedicated understanding is needed to ensure that no time and opportunity is lost and more is learned of the way people experience and attribute change. This is particularly important where it concerns the individuals who directly and frequently interact with changing ecosystems who may have nonscientific insights that add to the pool of scientific understanding. The psychology that explains how climate change phenomena are observed and interpreted by key stakeholders and also the ways by which these same stakeholders attribute meaning to them has to be understood to adequately prepare people for potential climate-driven changes. This empirical study suggests that not only the biophysical outcome, but also the economic situation, the relative direction of change, the historical context of change, and the specific situation of individuals involved has to be fully understood to understand the likely attribution responses. This awareness can enhance approaches that seek efficient and effective adaptation to climate-driven change in the marine environment. With increased recognition of the need for planned adaptation by Governments to the increasing impacts of climate change, it is essential that individuals and industry perceive that there is a common cause that needs to be addressed. Our results demonstrate that there remains considerable work that still needs to be done to ensure that users recognize the cause of their observations, as attribution can vary across different outcomes from the same cause—in our case range shifting species. To provide additional insights into our thesis, future studies are deemed necessary. Further investigation is needed of the cognitions we have outlined and confirmation of the issue of cognitive effect in attribution has to be robustly investigated using methods and approaches common to empirical and experimental psychology. Acknowledgements We would like to thank the anonymous reviewers and the editor for their help and suggestions. This research was funded by the Fisheries Research and Development Corporation and the former Department of Climate Change. This research would not have been possible without the local participants. References Adams, R. L. A. 1973. Uncertainty in nature, cognitive dissonance, and the perceptual distortion of environmental information. Economic Geography, 49: 287– 297. Ajzen, I. 1991. The theory of planned behaviour. Organizational Behaviour and Human Decision Processes, 50: 179– 211. Bersoff, D. M. 1999. Explaining unethical behaviour among people motivated to act prosocially. Journal of Moral Education, 28: 413– 428. Bord, R. J., Fisher, A., and O’Connor, R. E. 1998. Public perceptions of global warming: United States and international perspectives. Climate Research, 11: 75 – 84. Boykoff, M. T., and Boykoff, J. M. 2007. Climate change and journalistic norms: a case-study of US mass-media coverage. Geoforum, 38: 1190– 1204. Bradshaw, G. A., and Borchers, J. G. 2000. Uncertainty as information: narrowing the science-policy gap. Conservation Ecology, 4: 7. Bradshaw, M. B. 2004. A combination of state and market through ITQs in the Tasmanian commercial rock lobster fishery: the tail wagging the dog? Fisheries Research, 67: 99 – 109. Brander, K., Bruno, J. F., Hobday, A. J., and Schoeman, D. S. 2011. The value of attribution. Nature Climate Change, 1: 70 – 71. Broad, W., and Wade, N. 1983. Betrayers of the Truth: Fraud and Deceit in the Halls of Science. Century Publishing, London. Burrows, M. T., Schoeman, D. S., Buckley, L. B., Moore, P. J., Poloczanksa, E. S., Brander, K. M., Brown, C. J., et al. 2011. The pace of shifting climate in marine and terrestrial ecosystems. Science, 334: 652– 655. Cai, W., Shi, G., Cowan, T., Bi, D., and Ribbe, J. 2005. The response of the Southern Annular Mode, the East Australian Current, and the southern mid-latitude ocean circulation to global warming. Geophysical Research Letters, 32: L23706. Carlton, J. T., and Geller, J. B. 1993. Ecological roulette: the global transport of nonindigenous marine organisms. Science, 261: 78 – 82. Chambers, L. E., Patterson, T. A., Hobday, A. J., Arnould, Y. J. P., Tuck, G. N., Wilcox, C., and Dann, P. 2014. Determining trends and environmental drivers from long-term marine mammal and bird data: examples from Southern Australia. Regional Environmental Change, doi:10.1007/s10113-014-0634-8. Charles, A. T. 2012. People, oceans and scale: governance, livelihoods and climate change adaptation in marine social – ecological systems. Current Opinion in Environmental Sustainability, 4: 351– 357. Chen, I. C., Hill, J. K., Ohlemuller, R., Roy, D. B., and Thomas, C. D. 2011. Rapid range shifts of species associated with high levels of climate warming. Science, 333: 1024– 1026. Cook, J. M., Nuccitelli, D., Green, S. A., Richardson, M., Winkler, B., Painting, R., Way, R., et al. 2013. Quantifying the consensus on anthropogenic global warming in the scientific literature. Environmental Research Letters, 8: 1– 7. Costello, C., Gaines, S. D., and Lynham, J. 2008. Can catch shares prevent fisheries collapse? Science, 321: 1678– 1681. 1316 Coulthard, S. 2008. Adapting to environmental change in artisanal fisheries—insights from a South Indian Lagoon. Global Environmental Change, 18: 479 – 489. Dunning, D. 1999. A newer look: motivated social cognition and the schematic of social concepts representation. Psychological Inquiry, 10: 1 – 11. Engelhard, G. H., Ellis, J. R., and Pinnegar, J. K. 2008. Report of WP1 Chapter 20—Red mullet. Festinger, L. 1957. A Theory of Cognitive Dissonance. Stanford University Press, Stanford, CA, USA. Frusher, S., Marshall, N., Tull, M., Metcalf, S., and van Putten, E. I. 2013. A marine climate change adaptation blueprint for coastal regional communities. FRDC Report 2010/542, Hobart, Tasmania. Frusher, S. D., Hobday, A. J., Jennings, S. M., Creighton, C., D’Silva, D., Haward, M., Holbrook, N. J., et al. 2014. A short history of a marine hotspot—from anecdote to adaptation in south-east Australia. Reviews in Fish Biology and Fisheries, 24: 593 – 611. doi:10.1007/ s11160-013-9325-7. Garrabou, J., Coma, R., Bensoussan, N., Bally, M., Chevaldonne, P., Cigliano, M., Diaz, D., et al. 2009. Mass mortality in Northwestern Mediterranean rocky benthic communities: effects of the 2003 heat wave. Global Change Biology, 15: 1090– 1103. Gifford, R. 2011. The dragons of inaction: psychological barriers that limit climate change mitigation. American Psychologist, 66: 290– 302. Gledhill, D. C., Hobday, A. J., Welch, D. J., Sutton, S., Lansdell, M. J., Koopman, M., Jeloudev, A., et al. 2014. Collaborative approaches to accessing and utilising historical citizen science data: a case-study with spearfishers from eastern Australia. Marine and Freshwater Research, 65: 1 –7. http://dx.doi.org/10.1071/MF14071. Goodman, L. A. 1961. Snowball sampling. Annals of Mathematical Statistics, 32: 148 –170. Goodwin, J. R. 2001. Understanding the Cultures of Fishing Communities: a Key to Fisheries Management and Food Security. FAO. Green, B. S., Gardner, C., Linnane, A. J., Hobday, D., Chandrapavan, A., Punt, A. E., McGarvey, R., Hartmann, K., Treloggen, R., Revill, H., Hoare, M., and Hawthorne, P. 2012. Spatial management of southern rock lobster fisheries to improve yield, value and sustainability. The Australian Seafood CRC, Adelaide. Guy, S., Kashima, Y., Walker, I., and O’Neill, S. 2013. Comparing the atmosphere to a bathtub: effectiveness of analogy for reasoning about accumulation. Climatic Change, 121: 579 – 594. Hagerman, S., Dowlatabadi, H., Satterfield, T., and McDaniels, T. 2010. Expert views on biodiversity conservation in an era of climate change. Global Environmental Change, 20: 192 – 207. Haidt, J. 2001. The emotional dog and its rational tail: a social intuitionist approach to moral judgment. Psychological Review, 108: 814– 834. Hallegraeff, G. M. 2010. Ocean climate change, phytoplankton community responses, and harmful algal blooms: a formidable predictive challenge. Journal of Phycology, 46: 220– 235. Halpern, B. S., Walbridge, S., Selkoe, K. A., Kappel, C. V., Micheli, F., D’Agrosa, C., Bruno, J. F., et al. 2008. A global map of human impact on marine ecosystems. Science, 319: 948– 952. Hamon, K. G., Thébaud, O., Frusher, S., and Little, L. R. 2009. A retrospective analysis of the effects of adopting individual transferable quotas in the Tasmanian red rock lobster, Jasus edwardsii, fishery. Aquatic Living Resources, 22: 549– 558. Hannesson, R. 2006. Sharing the Northeast Arctic cod: possible effects of climate change. Natural Resource Modeling, 19: 633– 654. Hannesson, R. 2007. Global warming and fish migrations. Natural Resource Modeling, 20: 301– 319. Heider, F. 1958. The Psychology of Interpersonal Relations. Wiley, New York. I. E. van Putten et al. Hobday, A. J., and Evans, K. 2013. Detecting climate impacts with oceanic fish and fisheries data. Climatic Change, 119: 49– 62. doi:10.1007/s10584-013-0716-5. Hobday, A. J., and Pecl, G. T. 2014. Identification of global marine hotspots: sentinels for change and vanguards for adaptation action. Reviews in Fish Biology and Fisheries, 24: 415 – 425. doi:10.1007/ s11160-013-9326-6. Hodgkinson, J. A., Hobday, A. J., and Pinkard, E. A. 2014. Climate adaptation in Australia’s resource-extraction industries: ready or not? Regional Environmental Change, 14: 1663– 1678. doi:10.1007/ s10113-014-0618-8. Höhle, E. 2002. Global climate change as perceived by the public. Chapter 5. In Perception and Evaluation of Risks. Findings of the “Baden-Württemberg Risk Survey 2001”, pp. 115– 130. Ed. by M. M. a. Zwick, and O. Renn. Joint working report by the Centre of Technology Assessment in Baden-Württemberg and the University of Stuttgart, Sociology of Technologies and Environment, Germany. Huntington, H., and Fox, S. 2005. The Changing Arctic: Indigenous Perspectives. Arctic Climate Impact Assessment. Cambridge University Press, Cambridge. IPCC, 2001. Climate Change 2001: the Scientific Basis. Contribution of Working Group I to the Third Assessment Report of the Intergovernmental Panel on Climate Change. Ed. by J. T. Houghton, Y. Ding, D. J. Griggs, M. Noguer, P. J. van der Linden, X. Dai, K. Maskell, and C. A. Johnson. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA. 881 pp. IPCC. 2013. Climate Change, 2013: the Physical Science Basis, Summary for Policymakers. Cambridge, UK and New York, NY, USA. Jackson, J. B. C., Kirby, M. X., Berger, W. H., Bjorndal, K. A., Botsford, L. W., Bourque, B. J., Bradbury, R. H., et al. 2001. Historical overfishing and the recent collapse of coastal ecosystems. Science, 293: 629 – 638. Johnson, C. R., Banks, S. C., Barrett, N. S., Cazassus, F., Dunstan, P. K., Edgar, G. J., Frusher, S. D., et al. 2011. Climate change cascades: shifts in oceanography, species’ ranges and subtidal marine community dynamics in eastern Tasmania. Journal of Experimental Marine Biology and Ecology, 400: 17 – 32. Johnson, C. R., Ling, S., Ross, J., Shepherd, S. A., and Miller, K. 2005. Range Extension of the Long-Spined Sea Urchin (Centrostephanus rodgersii) in Eastern Tasmania: Assessment of Potential Threats to Fisheries. School of Zoology, University of Tasmania. Kahan, D. M., Peters, E., Wittlin, M., Slovic, P., Larrimore Ouellette, L., Braman, D., and Mandel, G. 2012. The polarizing impact of science literacy and numeracy on perceived climate change risks. Nature Climate Change, 2: 732– 735. Kahneman, D. 2011. Thinking, Fast and Slow. Farrar, Straus and Giroux, New York. Keller, K., and McInerney, D. 2008. The dynamics of learning about a climate threshold. Climate Dynamics, 30: 321– 332. Kirby, A. 2004. Britons unsure of climate costs—polling results. BBC News Online. Kunda, Z. 1990. The case for motivated reasoning. Psychological Bulletin, 108: 480– 498. Kuruppu, N., and Liverman, D. 2011. Mental preparation for climate adaptation: the role of cognition and culture in enhancing adaptive capacity of water management in Kiribati. Global Environmental Change, 21: 657 – 669. Last, P. R., White, W. T., Gledhill, D. C., Hobday, A. J., Brown, R., Edgar, G. J., and Pecl, G. T. 2011. Long-term shifts in abundance and distribution of a temperate fish fauna: a response to climate change and fishing practices. Global Ecology and Biogeography, 20: 58 – 72. Leviston, Z., Walker, I., and Morwinski, S. 2012. Your opinion on climate change might not be as common as you think. Nature Climate Change, doi:10.1038/NCLIMATE1743. Lewandowsky, S., Ecker, U. K. H., Seifert, C. M., Schwarz, N., and Cook, J. 2012. Misinformation and its correction: continued influence and Empirical evidence for different cognitive effects successful debiasing. Psychological Science in the Public Interest, 13: 106– 131. Lewandowsky, S., Oberauer, K., and Gignac, G. E. 2013. NASA faked the moon landing—therefore, (climate) science is a hoax: an anatomy of the motivated rejection of science. Psychological Science, 24: 622– 633. Ling, S. D. 2008. Range expansion of a habitat-modifying species leads to loss of taxonomic diversity: a new and impoverished reef state. Oecologia, 156: 883– 894. Ling, S. D., Johnson, C. R., Frusher, S. D., and Ridgway, K. R. 2009a. Overfishing reduces resilience of kelp beds to climate-driven catastrophic phase shift. Proceedings of the National Academy of Sciences of the United States of America, 106: 22341 –22345. Ling, S. D., Johnson, C. R., Ridgway, K., Hobday, A. J., and Haddon, M. 2009b. Climate driven range extension of a sea urchin: inferring future trends by analysis of recent population dynamics. Global Change Biology, 15: 719– 731. Lodge, M., and Taber, C. S. 2013. The Rationalizing Voter. Cambridge University Press, Cambridge, UK. Lowe, T., Brown, K., Dessai, S., de Franca Doria, M., Haynes, K., and Vincent, K. 2006. Does tomorrow ever come? Disaster narrative and public perception of climate change. Public Understanding of Science, 15: 435– 457. Malle, B. F. 2011. Attribution theories: how people make sense of behaviour. In Theories in Social Psychology, pp. 72– 95. Ed. by D. Chadee. Wiley and Blackwell, Oxford, 320 pp. Mandler, G. 1990. Interruption (discrepancy) theory: review and extensions. In On the Move: the Psychology of Change and Transition, pp. 13 – 32. Ed. by S. Fisher, and C. Cooper. John Wiley and Sons, West Sussex, England. Marzloff, M. P., Dambacher, J. M., Johnson, C. R., Little, L. R., and Frusher, S. D. 2011. Exploring alternative states in ecological systems with a qualitative analysis of community feedback. Ecological Modelling, 222: 2651– 2662. McCright, A. M. 2011. Political orientation moderates Americans’ beliefs and concern about climate change. Climatic Change, 104: 243– 253. McCright, A. M., and Dunlap, R. E. 2011. The politicization of climate change and polarization in the American public’s views of global warming, 2001 – 2010. The Sociological Quarterly, 52: 155– 194. Metcalf, S. J., van Putten, E. I., Frusher, S. D., Marshall, N., Tull, M., Caputi, N., Haward, M., et al. in press. Vulnerability influences the successful implementation of climate change adaptations. Ecology and Society, 9: 247 – 261. Metcalf, S. J., van Putten, E. I., Frusher, S. D., Tull, M., and Marshall, N. 2013. Adaptation options for marine-industries and coastal communities using community structure and dynamics. Sustainability Science, doi:10.1007/s11625-013-0239-z. Milne, M., Stenekes, N., and Russell, J. 2008. Climate Risk and Industry Adaptation. Australian Bureau of Rural Sciences, Canberra. Mora, C., Frazier, A. G., Longman, R. J., Dacks, R. S., Walton, M. M., Tong, E. J., Sanchez, J. J., et al. 2013. The projected timing of climate departure from recent variability. Nature, 502: 183 – 187. Musick, J. A., Harbin, M. M., Berkeley, S. A., Burgess, G. H., Eklund, A., Findley, L., Gilmore, R. G., et al. 2000. Marine, estuarine and diadromous fish stocks at risk of extinction in North America (exclusive of Pacific salmonids). Fisheries, 25: 6 – 30. Neuheimer, A. B., Thresher, R. E., Lyle, J. M., and Semmens, J. M. 2011. Tolerance limit for fish growth exceeded by warming waters. Nature Climate Change, 1: 110 –113. Nickerson, R. S. 1998. Confirmation bias: a ubiquitous phenomenon in many guises. Review of General Psychology, 2: 175 – 220. Nursey-Bray, M., Pecl, G. T., Frusher, S., Gardner, C., Haward, M., Hobday, A. J., Jennings, S., et al. 2012. Communicating climate change: climate change risk perceptions and rock lobster fishers, Tasmania. Marine Policy, 36: 753 – 759. 1317 Palutikof, J., Boulter, S. L., Ash, A. J., Stafford Smith, M., Parry, M., Waschka, M., and Guitart, D. 2013. Climate Adaptation Futures. Wiley-Blackwell, Oxford. Parmesan, C., Burrows, M. T., Duarte, C. M., Poloczanksa, E. S., Richardson, A. J., Schoeman, D. S., and Singer, M. C. 2013. Beyond climate change attribution in conservation and ecological research. Ecology Letters, 16: 58– 71. Parmesan, C., Duarte, C., Poloczanska, E., Richardson, A. J., and Singer, M. C. 2011. Overstretching attribution. Nature Climate Change, 1: 1–4. Pauly, D. 1995. Anecdotes and the shifting base-line syndrome of fisheries. Trends in Ecology and Evolution, 10: 430. Pecl, G., Frusher, S., Gardner, C., Haward, M., Hobday, A., Jennings, S., Nursey-Bray, M., et al. 2009. East Coast, Tasmania, An Assessment of Climate Change Impacts on East Coast Rock Lobster Productivity, Interactions with Fisheries Management and Flow-on Effects to Local Communities. Canberra. Pecl, G. T., Ward, T., Briceño, F., Fowler, A., Frusher, S., Gardner, C., Hamer, P., et al. 2014. Preparing Fisheries for Climate Change: Identifying Adaptation Options for Four Key Fisheries in South Eastern Australia. Fisheries Research and Development Corporation, Project 2011/039. Pinsky, M. L., Worm, B., Fogarty, M. J., Sarmiento, J. L., and Levin, S. A. 2013. Marine taxa track local climate velocities. Science, 341: 1239– 1242. Pitt, N. R., Poloczanska, E. S., and Hobday, A. J. 2010. Climate-driven range changes in Tasmanian intertidal fauna. Marine and Freshwater Research, 61: 963 – 970. Poloczanska, E. S., Brown, C. J., Sydeman, W. J., Kiessling, W., Schoeman, D. S., M, P. J., Brander, K., et al. 2013. Global imprint of climate change on marine life. Nature Climate Change, 3: 919 – 925. Ramos, J. E., Pecl, G. T., Moltschaniwskyj, N. A., Strugnell, J. M., León, R. I., and Semmens, J. M. 2014. Body size, growth and life span: implications for the polewards range shift of Octopus tetricus in south-eastern Australia. PLoS ONE, 9: e103480. Ramos, J. E., Pecl, G. T., Semmens, J. M., Strugnell, J. M., Leon, R. I., and Moltschaniwskyj, N. A. 2015. Reproductive capacity of a marine species (Octopus tetricus) within a recent range extension area. Marine and Freshwater Research, http://dx.doi.org/10.1071/ MF14126. Ridgway, K. R. 2007. Long-term trend and decadal variability of the southward penetration of the East Australian Current. Geophysical Research Letters, 34: L13613. doi:10.1029/2007GL030393. Robinson, L. M., Gledhill, D. C., Moltschaniwskyj, N. A., Hobday, A. J., Frusher, S. D., Barrett, N., Stuart-Smith, J. F., et al. 2015. Rapid assessment of short-term datasets in an ocean warming hotspot reveals “high” confidence in potential range extensions. Global Environmental Change, 31: 28– 37. Silvano, R. A. M., and Begossi, A. 2012. Fishermen’s local ecological knowledge on Southeastern Brazilian coastal fishes: contributions to research, conservation, and management. Neotropical Ichthyology, 10: 133– 147. Sissener, E. H., and Bjørndal, T. 2005. Climate change and the migratory pattern for Norwegian spring-spawning herring—implications for management. Marine Policy, 29: 299 – 309. Stamm, K. R., Clark, F., and Eblacas, P. R. 2000. Mass communication and public understanding of environmental problems: the case of global warming. Public Understanding of Science, 9: 219 – 237. Stenevik, E. K., and Sundby, S. 2007. Impacts of climate change on commercial fish stocks in Norwegian waters. Marine Policy, 31: 19 – 31. Sterman, J. D., and Sweeney, L. B. 2007. Understanding public complacency about climate change: adults’ mental models of climate change violate conservation of matter. Climatic Change, 80: 213 – 238. Sunday, J. M., Pecl, G. T., Frusher, S. D., Hobday, A. J., Hill, N., Holbrook, N. J., Edgar, G. J., et al. 2015. Species traits and climate velocity explain geographic range shifts in an ocean-warming hotspot. Ecology Letters, doi: 10.1111/ele.12474. 1318 Tam, J., and McDaniels, T. L. 2013. Understanding individual risk perceptions and preferences for climate change adaptations in biological conservation. Environmental Science and Policy, 27: 114 – 123. Thomas, C. D., Cameron, A., Green, R. E., Bakkenes, M., Beaumont, L. J., Collingham, Y. C., Erasmus, B. F. N., et al. 2004. Extinction risk from climate change. Nature, 427: 145– 148. Thresher, R., Proctor, C., Ruiz, G., Gurney, R., MacKinnon, R., Walton, W., Rodriguez, L., et al. 2003. Invasion dynamics of the European shore crab, Carcinus maenas, in Australia. Marine Biology, 142: 867– 876. Tvinnereim, E., and Fløttum, K. 2015. Explaining topic prevalence in answers to open-ended survey questions about climate change. Nature Climate Change, doi:10.1038/NCLIMATE2663. Valentine, J. P., and Johnson, C. R. 2003. Establishment of the introduced kelp Undaria pinnatifida in Tasmania depends on disturbance to native algal assemblages. Journal of Experimental Marine Biology and Ecology, 295: 63 – 90. van Putten, E. I., Metcalf, S. J., Frusher, S., Tull, M., and Marshall, N. 2014. Fishing for the impacts of climate change in the marine sector: a case study. International Journal of Climate Change Strategies and Management, 6: 421 – 441. I. E. van Putten et al. Weber, E. U., and Stern, P. C. 2011. Public understanding of climate change in the United States. American Psychologist, 66: 315– 328. Wernberg, T., Smale, D. A., Tuya, F., Thomsen, M. S., Langlois, T. J., de Bettignies, T., Bennett, S., et al. 2012. An extreme climatic event alters marine ecosystem structure in a global biodiversity hotspot. Nature Climate Change, doi:10.1038/nclimate1627. Whitmarsh, L. 2011. Scepticism and uncertainty about climate change: dimensions, determinants and change over time. Global Environmental Change, 21: 690–700. Wolf, J. 2011. Climate change adaptation as a social process. In Climate Change Adaptation in Developed Nations: From Theory to Practice. Advances in Global Change Research. Ed. by J. D. Ford, and L. Berrang-Ford, Springer, Dordrecht, the Netherlands. 490 pp. Zeidberg, L. D., and Robison, B. H. 2007. Invasive range expansion by the Humboldt squid, Dosidicus gigas, in the eastern North Pacific. Proceedings of the National Academy of Sciences of the United States of America, 104: 12948– 12950. Zhang, D. D., Lee, H. F., Wang, C., Li, B., Pei, Q., Zhang, J., and An, Y. 2011. The causality analysis of climate change and large-scale human crisis. Proceedings of the National Academy of Sciences of the United States of America, 108: 17296– 17301. Handling editor: Sarah Kraak
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