Identifying priority landscapes and ecosystems for nature conservation in the Kangaroo Island NRM region Phil Pisanu, Dan Rogers, Jody O’Connor, David Thompson and Darcy Peters Department of Environment, Water and Natural Resources April 2014 DEWNR Technical Report 2013/14 i Department of Environment, Water and Natural Resources GPO Box 1047, Adelaide SA 5001 Telephone National (08) 8463 6946 International+61 8 8463 6946 Fax National (08) 8463 6999 International +61 8 8463 6999 Website www.environment.sa.gov.au Disclaimer The Department of Environment, Water and Natural Resources and its employees do not warrant or make any representation regarding the use, or results of the use, of the information contained herein as regards to its correctness, accuracy, reliability, currency or otherwise. The Department of Environment, Water and Natural Resources and its employees expressly disclaims all liability or responsibility to any person using the information or advice. Information contained in this document is correct at the time of writing. © Crown in right of the State of South Australia, through the Department of Environment, Water and Natural Resources 2013 This work is Copyright. Apart from any use permitted under the Copyright Act 1968 (Cwlth), no part may be reproduced by any process without prior written permission obtained from the Department of Environment, Water and Natural Resources. Requests and enquiries concerning reproduction and rights should be directed to the Chief Executive, Department of Environment, Water and Natural Resources, GPO Box 1047, Adelaide SA 5001. Preferred way to cite this publication Pisanu, P, Rogers, D, O’Connor, J, Thompson, D and Peters, D, 2013, Identifying priority landscapes and ecosystems for nature conservation in the Kangaroo Island NRM region, DEWNR Technical Report 2013, Government of South Australia, through Department of Environment, Water and Natural Resources, Adelaide ii Acknowledgements We received valuable feedback on an early draft of this report from Martine Kinloch, Phillipa Holden and David Taylor. Chris Butcher provided assistance with production of figures and maps. The final draft of the report was reviewed by Kane Aldridge, SMK. iii Table of Contents 1 INTRODUCTION 1.1 Project Description and Objectives 1.1.1 Linking Landscape Assessment and NatureLinks Planning 1.1.2 Structure of theReport 2 BACKGROUND 6 6 7 9 10 2.1 Conservation Planning Concepts 2.1.1 Landscape Drivers and Resilience 2.1.2 The Landscape State and Transition Model (LSTM) 2.1.3 Ecosystem Definition 10 11 13 13 2.2 14 3 Kangaroo Island Land Use History and Impacts on Natural Systems METHODS 17 3.1 Approach 3.2 Landscapes 3.2.1 Landscape Description 3.2.2 Landscape Analysis 17 18 18 18 3.3 Ecosystems 3.3.1 Ecosystem Assessment 19 19 4 22 RESULTS 4.1 Landscape Identification and Description 4.2 Key Ecological Drivers on Kangaroo Island 4.2.1 Fire Regimes 4.2.2 Landscape level patterns of clearance of native vegetation 4.2.3 Other drivers 4.2.4 Landscape Analysis – Summary 22 24 24 29 29 31 4.3 Ecosystem Assessment 4.3.1 Ecosystem Descriptions 4.3.2 Ecosystem level patterns of native vegetation clearance 4.3.3 Avifauna Decline 32 32 33 34 4.4 Eucalyptus cneorifolia Case Study 4.4.1 The Eucalyptus cneorifolia Ecological Community 4.4.2 Conceptual Model of Mallee Ecological Dynamics 34 34 35 5 37 DISCUSSION 5.1 Understanding Drivers of Ecological Change 5.2 The Potential Role of Corridors 5.3 Improving Knowledge 5.3.1 Fire Regimes 5.3.2 Other Threats and Drivers of Change 37 39 40 41 42 6 44 RECOMMENDATIONS 6.1.1 6.1.2 Priority landscapes and ecosystems for conservation activity Additional knowledge building 44 44 7 CONCLUSION 46 8 REFERENCES 47 9 APPENDICES 53 iv Summary The Kangaroo Island NatureLinks project presents the conceptual framework, analysis methods and results for identification of priority landscapes and ecosystems (ecological communities) for conservation on Kangaroo Island using a whole of island ‘landscape assessment’ approach. The report includes analysis of all major landscapes to identify broad scale landscape units that can be used in management, evaluates key drivers of change at the landscape scale, identifies a number of key ecosystem types, and presents a detailed case study of a Kangaroo Island ecosystem to demonstrate how the broad approach can be extended, in cases where sufficient high quality information is available, to identify fine scale priorities for conservation management and investment. The project addresses a key aim of the NatureLinks program for Kangaroo Island - 1) Identifying priority landscapes and corridors. The project addresses two key objectives to achieve this aim: 1. Identification of priority landscapes for conservation activity; and 2. For priority landscapes, identification of priority ecosystems for conservation activity. The ‘Landscape Assessment’ uses a nested approach to setting conservation goals, referred to as the ‘coarse-filter/fine-filter’ approach. This has been used successfully to identify priority ecosystems for restoration in South Australian agricultural landscapes by identifying those ecosystems whose dependent biota are at risk of local extinction, where these risks are associated with system-level changes in function. This type of information has then been used to identify priorities that provide a basis for developing conservation delivery programs in these regions. For Kangaroo Island, the landscape assessment essentially comprised four analytical components: 1. Define and spatially represent the landscapes of Kangaroo Island; 2. Identify island-wide drivers of landscape change with respect to biodiversity; 3. Identify where each landscape “sits” relative to these landscape-scale drivers, in order to identify the relative resilience of different landscapes; and 4. Target ecosystem-level analyses toward those landscapes that appear to be approaching or have crossed critical thresholds with respect to landscape-scale drivers. For the purposes of this assessment, three landscapes were defined for Kangaroo Island: 1) West and South Coast, 2) Central Plateau and North Coast, and 3) Eastern Plains and Dudley. The analysis identified 12 ecosystems within the three landscapes. Consideration of broad patterns of historical land use change and interpretation of empirical data where it was available indicates that a number of key drivers appear to operate at the landscape scale, and/or at the scale of individual patches of remnant vegetation. The key drivers identified were -fire regime, conversion of native vegetation cover for agricultural production; and species population processes (particularly metapopulation dynamics). In addition, a number of key drivers were identified that specifically relate to the dynamics of patches of remnant vegetation - grazing of remnant patches; and changes to physico-chemical processes (particularly dryland salinity). Of the three landscapes, the West and South Coast is the most intact and there is no evidence to suggest major declines at the ecosystem level are occurring. A dominance of young fire age classes following the large-scale 2007 fires is apparent, reinforcing the need for fire managers to encourage the reinstatement of older age classes over time. The terrestrial bird analysis presented here, as well as existing knowledge and new analysis that highlights less than optimal fire regimes, reinforces the need to keep addressing management issues in the most altered parts of Kangaroo Island, in particular the Eastern Plains and Dudley landscape. This landscape is essentially fragmented and has a number of highly altered ecosystems, such as associated with the Narrow-leaved Mallee community complex. Continued management efforts to address issues such as fire regime, grazing pressure, weeds and salinity will be needed to ensure that resilience in this landscape is maintained and improved over time. The second key landscape to focus on is the Central Plateau and North Coast. The fire regime for this landscape appears to be operating, at least in part, outside of optimal limits in terms of age classes, and the eastern section of the landscape is highly altered by clearing. At an ecosystem scale the terrestrial bird analysis did not flag any major declines in ecological resilience at this time, however, anecdotal evidence suggests that some changes may be occurring that could lead to losses of ecosystem function in the future. Preferential historical clearing of woodlands on ironstone soils makes these areas a logical priority for future management and restoration efforts. The study does not specifically identify corridors but discusses the relevance of corridors as a management option in the context of other management interventions that could be applied to improve ecological function in the agricultural matrix. The report makes a number of recommendations about how to improve the knowledge base for Kangaroo Island biodiversity and how to apply this in an adaptive management framework. 5 1 INTRODUCTION The Kangaroo Island NatureLinks project presents the conceptual framework, analysis methods and results for identification of priority landscapes and ecosystems (ecological communities) for conservation on Kangaroo Island using a whole of island ‘landscape assessment’ approach. The report includes analysis of all major landscapes to identify broad scale landscape units that can be used in management, evaluates key drivers of change at the landscape scale, identifies a number of key ecosystem types, and presents a detailed case study of a Kangaroo Island ecosystem to demonstrate how the broad approach can be extended, in cases where sufficient high quality information is available, to identify fine scale priorities for conservation management and investment. A key requirement of successful conservation is the clear articulation of goals (Wilson et al. 2006; Bottrill et al. 2008). These goals should describe the desired outcomes of the conservation activity, with regard to what components of biodiversity to target for investment in management actions. In order to achieve nature conservation for a region, particularly in situations where resources for undertaking action are limited, it is logical that the goals focus on the requirements of the biodiversity that is most at risk of being irreversibly lost (Diamond et al. 1976; Bottrill et al. 2008; Gibbons 2010). To put this into context for NRM, this means that investing in the restoration or management of ecosystems that are demonstrably in decline now is a priority. Any delay in this investment will lead to greater future costs and higher likelihood that intervention will fail. Practically, we recognize that NRM invests in biodiversity for a range of outcomes (or to meet a range of stakeholder expectations) so there are real challenges around making decisions when resources are limited, which is almost always the case in NRM. Biodiversity occurs at a range of interacting levels (such as landscape, ecosystem, species), and conservation goals need to reflect these levels. One way of approaching this challenge is to understand the state and trend of biodiversity at each of these levels, and the extent to which meeting the conservation requirements at higher levels will meet the requirements of biota at lower levels. For example, if we can identify and address the conservation requirements of those ecosystems that are at risk of irreversible deleterious change, we are likely to meet the requirements of most species that depend on those ecosystems functioning in a particular way. This nested approach to setting conservation goals has been termed the ‘coarse-filter/fine-filter’ approach (Noss 1987; Hunter et al. 1988). At the ecosystem level, this approach has been used successfully to identify priority ecosystems for restoration in South Australian agricultural landscapes (Rogers 2010; Willoughby 2010; Rogers 2011a; b; 2012a; Rogers 2012d; c; b; Rogers et al. 2012) by identifying those ecosystems whose dependent biota are at risk of local extinction, where these risks are associated with system-level changes in function. The information produced has then been used to identify priorities that provide a basis for developing conservation delivery programs in these regions. 1.1 Project Description and Objectives Natural Resources Kangaroo Island, along with DEWNR Policy, has identified five broad aims for the delivery of NatureLinks on Kangaroo Island: 1. Identify priority landscapes and corridors across Kangaroo Island 2. Facilitate stakeholder understanding of the importance of biodiversity corridors 6 3. New corridor projects identified, assessed and planned 4. KI NRM Plan reviewed and new actions/targets provided for the next plan 5. Facilitate NatureLinks delivery These aims focus on a range of planning requirements, some of which are beyond the scope of the project presented here. Following discussions with Kangaroo Island regional staff, a decision was made that SMK would primarily focus on aim 1) Identifying priority landscapes and corridors. The project addresses two key objectives to achieve this aim: 1. Identification of priority landscapes for conservation activity; and 2. Identification of priority ecosystems for conservation activity. The project identifies priorities for conservation activity on Kangaroo Island by identifying landscapes and ecosystems within landscapes, that appear to be in decline and thus requiring targeted conservation management. The issue of corridors is not assessed directly in this report. There are sound reasons to be cautious about implementing a corridor focused program (see discussion section) so the recommended approach is that regional staff consult with SMK to evaluate how the results of the landscape analysis could be used to spatially define parts of landscapes that could be the focus of on-ground restoration activities. The project does not provide a review of NRM targets and actions (aim 4) but the types of analysis used here can produce information useful for review processes. This could be achieved using an adaptive planning/management framework (see below). The project also highlights key knowledge gaps that currently limit conservation planning efforts. Finally, the landscape analysis will be useful as the basis for assessing some of the risks to biodiversity posed by global climate change. The landscape assessment provides new information on the current status and trajectory of key ecosystems, which could be combined with additional information on climate exposure to assess potential climate impacts under different change scenarios. 1.1.1 Linking Landscape Assessment and NatureLinks Planning New knowledge built through landscape assessment would be utilized most effectively for the NRM planning process if an adaptive management approach is adopted. Adaptive management is explicit about knowledge building as a key part of planning, and as such provides a structure for assimilating and testing new knowledge, as well as applying knowledge at crucial decision points in the planning process. Ecological and social systems are complex and as a result, whole-system responses cannot be easily predicted from the sum of individual components’ responses (Harris 2007). For example, how a system responds to a combination of human pressures, management interventions and the variation linked to natural cycles (e.g. such as drought), strongly depends on context (both historical and spatial). Moreover, is difficult to predict system responses with certainty based on previous experiences (simply because the world keeps changing) so expecting predictive certainty in natural resource management can often be counterproductive (Holling 1978). The landscape assessment for Kangaroo Island will produce a series of working hypotheses about processes (or drivers of change) and how different biotas are expected to respond to them. Because the adaptive management method treats management as a hypothesis, with alternative approaches 7 to natural resource management designed to test this hypothesis (Walker and Salt 2012), it would be ideal if regional NRM staff work with SMK to develop a set of actions for addressing key conservation priorities identified by the project. The adaptive management cycle includes up to seven critical steps, including specification of management objectives (1), modelling of existing knowledge (2), identification of goals and related assessment criteria (3), models of alternative management options (4), identification of how to structure decision-making (5), implementation of management actions (6), and monitoring and evaluation (7) (Figure 1). There are key feedback loops in adaptive management, particularly in relation to how models influence objectives and goals, and how management results influence objectives for new management cycles (Sabine et al. 2004). Figure 1. The adaptive management cycle (from Sabine et al. 2004). The adaptive management cycle is not linear, and we recognise that knowledge, management objectives and specified actions already exist for Kangaroo Island landscapes. Thus the new information generated by the landscape assessment project will essentially provide synthesis and models of existing knowledge which can be used to review or refine management objectives, or in some cases develop new goals. This process is a way of linking knowledge generation and priority or goal setting. Designing science to monitor outcomes is outside of the scope of this project but the types of analysis presented here can provide a foundation for monitoring design, or at least demonstrate how the scientific foundation or evidence base can be constructed. Overall, this approach should ultimately reduce (but not necessarily eliminate) uncertainty and provide evidence for sound management practice. If implemented these adaptive steps will contribute towards meeting NatureLinks objectives 4) KI NRM Plan reviewed and new actions/targets provided for the next plan, and 5) Facilitate NatureLinks delivery. 8 1.1.2 Structure of theReport The report is presented as seven sections, described below: 1. Introduction (project description, objectives, and conceptual background, NRM planning and adaptive management framework) 2. Methods (landscape and ecosystem analysis methodology) 3. Results (landscape analysis, ecosystem analysis and a fine scale case study) 4. Discussion (significant of key results, identification of knowledge gaps) 5. Recommendations (priority landscapes and ecosystems, future knowledge building) 6. Conclusion 7. References 9 2 BACKGROUND 2.1 Conservation Planning Concepts A number of different tools can potentially be used for setting conservation goals. These include the focal species (Lambeck 1997), coarse- and fine-filter ecosystem approaches (Poiani et al. 2000; Groves et al. 2002) and, more recently, resilience (Walker and Salt 2006). One of the key requirements of a successfully implemented conservation plan is the development of clearly articulated conservation goals that are designed to meet the conservation requirements of the landscape for which they have been designed. The complexity of biological diversity makes this a challenging task. The approach presented here for Kangaroo Island is based on identifying and addressing both the systemic conservation requirements of a landscape (coarse filter), along with the idiosyncratic conservation requirements of those species and populations whose needs aren’t met by the coarse filter (fine filter) (Noss 1987; Hunter et al. 1988; Hunter 1991; 2005). The coarse-fine filter concept rests on the assumption that biodiversity is hierarchical, where the ecological requirements of many components of the lower levels in a hierarchy (e.g. species) are nested within the ecological requirements of higher levels in a hierarchy (e.g. ecosystems). The ‘coarse-filter/fine-filter’ approach has received criticism because the spatial distribution of the coarse-filter surrogate (ecosystem) does not necessarily reflect the distribution of lower levels of biodiversity (Januchowski-Hartley et al. 2011), and surrogates have been criticised as not being representative of the wide range of biota in particular systems (Andelman and Fagan 2000; Saetersdal and Gjerde 2011), however, this assumes there is only interest in patterns of biodiversity, and not the processes that underpin these patterns (Bennett et al. 2009). In fact addressing processes should meet the requirements of biota that depend on these systems and this can be done by assessing the relatively transient biotic components of systems in the context of the more enduring abiotic elements of a system in which the biotic elements interact (Hunter et al. 1988). Thus in the landscape assessment framework presented here, birds are used to represent landscapescale processes and interactions under the assumption that they are effective coarse-filter surrogates. The decision to use avifauna for Kangaroo Island is based on previous applications of the landscape assessment approach. It is difficult to obtain useful information for most fauna that is informative about the state and trajectory of ecological communities. Birds, on the other hand, are a visible and relatively well-studied type of fauna in most agricultural settings. Also, in many landscapes, the spatial scale over which terrestrial bird populations operate are comparable to the scale over which human activities operate; thus the scale at which we define our landscapes may be comparable between terrestrial birds and human impacts (e.g. Major 2010). The fine filter analogy refers to those species with specific ecological requirements that cannot be conserved by addressing systemic landscape scale issues alone. These species are commonplace in conservation, typically being addressed through threatened species recovery programs. An example is the very small population, for which secondary threats associated with small population sizes are critical (Gilpin and Soúle 1986). Species that have been reduced to very small populations are susceptible to a range of threats linked to their population size and demographic processes (such as inbreeding depression, demographic stochasticity and genetic drift (Gilpin and Soúle 1986). 10 The external factors that influence the decline of a population are likely to vary on a case-by-case basis but for agricultural settings they tend to be processes associated with the alteration and fragmentation of landscapes that leads to habitat loss (Akçakaya 2001). In practice, uncommon species need to be managed as meta-population which persist in a balance between local extinction and colonisation (Harrison 1991). This balance is influenced by the colonisation ability of individual species, habitat patch size and isolation, compensation effects between colonisation and extinction rates, the effect of immigration on local dynamics (rescue effect), and heterogeneity among habitat patches (Hanski 1991). Threatened species sometimes require specific and targeted management interventions. On Kangaroo Island, the Glossy-Black Cockatoo and the nationally threatened plants found on the Eastern Plains are examples of these types of species. A key difference being that the work being undertaken by the Eastern Plains Fire Trial (EPFT 2008) is beginning to demonstrate that the conservation requirements of these plant species can be addressed at ecosystem and landscape scales (coarse-filter) because of the important influence of fire regime, whereas, the Glossy-Black Cockatoo is an idiosyncratic species with species -specific (fine filter) conservation management needs (Mooney and Pedler 2005). Thus from a practical perspective, one of the main aims of undertaking landscape assessment is to be able to reliably identify those small populations that have passed through the coarse filter, so that it is possible to clearly articulate specific conservation management requirements that cannot be addressed by management of systemic landscape level issues alone. 2.1.1 Landscape Drivers and Resilience In agricultural regions, such as Kangaroo Island, land use dictates the degree of removal and modification of native vegetation, a process that is typically not homogenous across different elements of a landscape and at regional scales (Paton et al. 1999). While the reasons for these patterns are complex, heterogeneous modification is typically driven by variation in the nature of the physical environment, which largely determines patterns of agricultural production in a given landscape. As a result, particular elements of the landscape are likely to be impacted more by human activity than other elements. Understanding these differences is an important step for understanding which landscape attributes are associated with components of biodiversity at risk that require conservation intervention, and what the drivers of these relationships are (Rogers et al. 2012). Thus one of the key underlying objectives of landscape assessment is to identify key drivers of change. Concepts about how ecosystems change in response to disturbance, external changes, or other forms of perturbation have developed over the last 100 years but there is still no agreed upon general conceptual framework concerning the controls on species turnover and ecosystem development. However, over past decades there has been a noticeable shift in ecological thinking from a focus on models based on gradual continuum dynamics to models that incorporate trajectories, thresholds and stochasticity (or chance events) (Suding and Hobbs 2009). These ideas are at the core of resilience theory. Resilience thinking can be applied at different levels of a biological hierarchy but application at a landscape level can be particularly useful for identifying and describing which landscapes are important for different reasons. The idea is to focus on describing and evaluating the characteristics of desirable states and how information on changes in species composition, habitat structure and ecological processes should be interpreted as evidence for transformation to undesirable ecosystem states (at landscape scales). This then becomes a first step towards prioritising which conversation assets need immediate attention. 11 Models that include alternative stable states are useful for predicting threshold dynamics, where a small change in environmental conditions can cause an abrupt change in ecosystem function and/or community structure. Being clear about feedback processes is also important because multiple states can exist under similar environmental conditions, feedbacks influence whether a system is maintained in a particular state, and there is no guarantee that a disturbed system will to return to its original state once a pressure has been removed. In fact it is possible that some changes can lead to irreversible collapse (Suding and Hobbs 2009). Thresholds are a breakpoint between two states of a system, and a characteristic feature of a threshold is a change in system feedbacks. Resilience is a property of systems that defines the capacity of a system to absorb disturbance and reorganise so to retain essentially the same function, structure, identity and feedbacks. As the resilience of an ecosystem declines, the amount of disturbance needed to cross the threshold declines (Suding and Hobbs 2009). King and Hobbs (2006) developed a conceptual model of ecosystem resilience (Figure 2) that incorporates the concept of abiotic and biotic thresholds. The model shows three stages of change (degradation), with thresholds between them that represent barriers to ecosystem recovery. As time goes on and degradation continues it becomes increasingly difficult to restore ecosystems back to their original state or starting point because functional thresholds have been crossed. Figure 2. Concept of biotic and abiotic thresholds indicating breakpoints in ecosystem redevelopment from a degraded state. In the first stage, biotic function is degraded but the system still has the capacity for autogenic recovery if the cause of degradation is removed. If degradation continues, the first threshold of recovery potential is crossed. This results in damage to biotic function. If the ecosystem has crossed over this threshold and is in the second stage, some manipulation of biotic components beyond removal of disturbance will be required for autogenic recovery to take place. Although abiotic functions may have been degraded in the second stage they still maintain some resilience in terms of their capacity to recover without direct manipulation. Beyond the second threshold, biotic processes are severely dysfunctional and abiotic function has been degraded beyond its resilience. In this final stage of degradation, abiotic components require manipulation in order to make autogenic recovery possible (from King and Hobbs 2006). 12 The application of resilience concepts is implicit in landscape assessment and is particularly important for developing conceptual models of how landscapes and ecosystems are structured. Resilience thinking is used throughout but was particularly important for development of the stateand-transition model (STM) presented in this study to describe Narrow-leaved mallee dynamics. 2.1.2 The Landscape State and Transition Model (LSTM) The Landscape State and Transition Model (LSTM) framework (Cale 2007; Cale and Willoughby 2009) is applied in this study as an analysis tool for describing broad scale drivers of change in key landscapes. The LSTM and the matrix threshold model of McIntyre and Hobbs (1999) are conceptually similar models of landscape change that describe relationships between remnant vegetation and the status of landscapes. The matrix threshold model describes a simple relationship between remnancy of native vegetation and the “state” of a landscape, with regard to its biodiversity (McIntyre and Hobbs 1999), and includes conservation management guidelines (McIntyre et al. 2000). It is applied in this study to describe landscape-scale patterns of vegetation remnancy. A limitation of the matrix threshold model is that it assumes that clearance of native vegetation for agriculture is the only driver of state change at the landscape scale, and that the biodiversity of landscapes within each vegetation remnant class is at equilibrium with the level of clearance impact (i.e. it doesn’t account for the temporal nature of clearance). The LSTM approach (Cale 2007) attempts to account for at least the former assumption, by explicitly describing the range of important drivers that determine the state of an ecological landscape (such as fire, grazing, hydrology and nutrient cycling, as well as clearance), and attempts to apply this reasoning at both the scale of the landscape, and to the patch. This approach has been applied in a case study of the South Australian Murray-Darling Basin NRM region (Cale and Willoughby 2009). While it does provide a description of the dynamics of ecological landscapes (and their response to modification) more explicitly, it is still based on general principles, such as those regarding remnancy. Thus further conservation planning is still required to increase understanding of the state and drivers of specific conservation assets (i.e. ecosystems and species) within landscapes. The LSTM is applied in this study to describe broad differences in key Kangaroo Island landscapes at a regional scale. 2.1.3 Ecosystem Definition An important biological unit assessed in this study of Kangaroo Island is the ecosystem (synonymous with the ecological community). In practice, the terms ecosystem and ecological community are often used interchangeably and the scientific literature includes different definitions of ecosystems. Despite some nuances, a key concept applicable to ecosystems is to explicitly recognise the link between biotic and abiotic components (Keith 2009). In South Australia, recent consultation with a range of ecologists and land managers interested in the management of threatened ecological communities has led to the following description of an ecosystem that can be broadly applied to the work presented here - a geographically distinct assemblage of interacting native species and their associated abiotic environment (Bonifacio and Pisanu 2013). Classifying ecosystems can be done on the basis of characteristic native biota, associated physical environment, processes and interactions between components and spatial extent. Characteristic native biota are also commonly used when describing ecological communities, along with structure and or habitat, whereas relatively few community descriptions address species interactions or other ecological processes and functions (Keith 2009; 2012). Descriptions of ecosystems are scaledependent in terms of spatial, temporal and thematic scales, and they can vary greatly. Thematic scale refers to the similarity of features within and between ecosystems, and their degree of 13 uniqueness in composition and processes. An ecosystem can appear stable at some temporal scales, while undergoing trends and fluctuations at others (Keith et al. 2013). South Australian ecological communities have previously been described largely on the basis of floristic and vegetation structural features, with limited explicit focus on the inherent physical environments that drive much of ecological variation. An example is the floristic classification used as the basis for mapping vegetation on Kangaroo Island (Robinson and Armstrong 1999), which still forms a base layer for many management decisions. This approach reflects widely applied conventions for classification, naming and mapping of vegetation types, which focus strongly on the description of structural or physiognomic attributes of vegetation and vascular plant species composition(e.g. Benson 2006). The focus on ecosystems presented here does represent a departure from conventional vegetation identification and mapping to some degree, but it is still possible to make clear linkages between the vegetation types typically used in NRM for management and the important underlying abiotic conditions and biological processes that drive change used to define ecosystems. 2.2 Kangaroo Island Land Use History and Impacts on Natural Systems An important aim of landscape assessment is to develop an understanding of how historical land use has influenced, and continues to influence the composition, structure and function of ecosystems within particular landscapes. Finding accurate, detailed and spatially-explicit data on land use is challenging, as it is often general, specific to particular enterprises or issues, or has simply not been recorded. Thus the overview presented here is meant to provide context for interpreting more detailed data where it exists, and as background for interpreting current observed patterns in landscapes. European discovery and early exploration of Kangaroo Island by Matthew Flinders (Investigator) and circumnavigation by Nicholas Baudin (Le Geographe) resulted in mapping and naming of a number of coastal locations. Sealing was the first industry on KI, established by an American expedition in the Union at American River. By 1880 the last major shipment of fur-seal skins occurred due to widespread depletion of seal numbers (Robinson 1999). A number of key historical events have since driven land use change on Kangaroo Island (Figure 3). These mainly relate to land clearing for agricultural production. Today, approximately 60% (or 230,370 ha) of Kangaroo Island is utilised for agriculture, with dryland agriculture the predominant land use, principally sheep grazing for wool and meat. Cropping and beef cattle are the next most significant industries and new industries have emerged since the mid- 1990s – primarily farm forestry, viticulture, horticulture (including seed potatoes), apiary and other minor livestock enterprises (Dohle 2007). In 2002/03 the value of major industries to the Kangaroo Island economy were $54.6 million (grazing), $10.8 million (cropping), $7.6 million (commercial fishing) and $53 million (tourism) (Gellard 2005). Cropping increased substantially from 8,000 ha in 1991 to 19,000 ha in 2011/12 (Dohle 2013). The key crops grown on the island are cereals (mainly wheat, barley and oats), canola and pulses (broad beans, lupins and peas), and cropping includes continuous cropping and mixed livestock/cropping enterprises. Cropping has the potential to increase the risk of a number of adverse land degradation impacts, such as soil erosion, soil acidity, water logging, salinity, fire risk (due to stubble burning) and fertiliser spray drift, which may have secondary impacts on remnant native vegetation (Dohle 2013). Land clearing associated with cropping tends to target isolated paddock trees which may reduce connectivity (e.g. stepping stones) between more substantive vegetation remnants for some native species (Lindenmayer and Fischer 2006). 14 1802 Early exploration of KI coastline (Matthew Flinders Investigator; Nicholas Baudin Le Geographe) Sealing – sea lion & fur seal 1836 KI settlement at Kingscote Most settlers return to mainland by 1840 1880 Sealing ceases Clearing of Eastern Plains commences Land clearance, changed fire regime 1919 Flinders Chase National Park proclaimed Soil deficiencies limit sheep and crop production – cobalt, copper 1923-25 18 koalas introduced to the island 1930s CSIRO solves ‘coast disease’ 1950s Post WW2 land improvement and soldier settlement schemes KI population doubles; agricultural production trebles 1969 Present broad acre clearance pattern established island-wide 1971 Cape Gantheaume Conservation Park proclaimed 1985 Native Vegetation Act 1985 gazetted 1991 Cereal cropping = 8,000 ha Soil enrichment and superphosphate fertiliser application increases Major clearing of land – Central Plateau Native Vegetation Act 1991 gazetted Large-scale land clearing ceases Dryland(secondary) salinity estimated at 5,600 ha Salinity impacts mainly on drainage lines and flats of Eastern Plains Phytophthora cinnamomi plant pathogen detected on KI Potential impacts on Eucalyptus, Xanthorrhoea, Banksia and Grevillea. 1997 Koala population estimated at 5000 Widespread defoliation of KI Stringybark woodlands 2001 Koala population estimate revised to 27,000 Koala control program commences 2008 Eastern Plains Fire Trial commences 2011-12 Cereal cropping = 19,000 ha 1993 Cropping increases risks of salinity, fertiliser drift, soil acidification & erosion Figure 3. Timeline of major historical events linked to land use change on Kangaroo Island. 15 Other factors that have significantly influenced the status of biodiversity on Kangaroo Island include proclamation of large protected area reserves such as Flinders Chase National Park in 1919, the introduction of koalas to the island in 1923-25, and the establishment of the South Australian Native Vegetation Act 1991, which saw the cessation of broad scale land clearance (Figure 3). The history of change for the early settlement period (yellow band: 1802 to late 1940s) is incomplete but it assumed that ecosystems on the island began to change gradually as agriculture expanded. The red zone between the late 1940s to the early 1990s represents a period of intensive change in natural systems associated with improved technologies, increased settlement and higher rates of agricultural production. A key limitation prior to this period was the constraint on agricultural production posed by soil deficiencies. CSIRO ultimately found a remedy for ‘coast disease’ in the 1930s. The subsequent introduction of superphosphate fertilisers, subterranean clover and minerals to address soil deficiencies (cobalt, zinc and some trace elements)(Robinson 1999) boosted agriculture. A further renewed push for settlement occurred after Second World War due to incentives for rural subdivision from government sponsored land improvement and soldier settlement schemes (1947 onwards) (Mooney and Grinter 2000; Dooley et al. 2002). The 1930s-40s resulted in increased primary production and agricultural development, including intensive clearing of the Central Plateau around Parndana. By the 1950s Kangaroo Island’s population had doubled and agricultural production had tripled (Robinson 1999). Native vegetation remained relatively intact until 1945 but by 1969 the clearance pattern across the island resembled what it does today (Robinson 1999). The consequences for native vegetation has been a progressive change in cover and in the most extreme cases, such as found on the eastern part of the island, fragmentation of large areas. Broad-scale land clearing has ceased since the introduction of South Australian clearance legislation (Native Vegetation Management Act 1985) and subsequent amendments resulting in the Native Vegetation Act 1991 (Figure 3). 16 3 METHODS 3.1 Approach The key concept in ‘landscape assessment’ is that particular ecosystems have been subjected to particular historic processes and these processes, coupled with the abiotic context or setting in which they occur, shape how ecosystems function. It is assumed that where a group of species that are commonly associated with a particular ecosystem are undergoing similar rates of decline, these declines can be attributed to a systemic issue (or set of issues) affecting the ecosystem itself. Thus by identifying the systemic issues commonly impacting on declining species (identified by measuring their trajectory of change), conservation goals can be designed to explicitly address the systemic issue. In practice, landscape assessment relies on the synthesis of landscape-specific information regarding the nature of ecosystems in the landscape; status and trend of species in the landscape; and environmental (and particularly land-use) history of the landscape. The integration of this information allows for identification of patterns of association between the ecological (and particularly ecosystem) requirements of species and their state and historic trajectory (Rogers et al. 2012). For Kangaroo Island, the landscape assessment essentially comprised four analytical components: 5. Define and spatially represent the landscapes of Kangaroo Island; 6. Identify island-wide drivers of landscape change with respect to biodiversity; 7. Identify where each landscape “sits” relative to these landscape-scale drivers, in order to identify the relative resilience of different landscapes; and 8. Target ecosystem-level analyses toward those landscapes that appear to be approaching or have crossed critical thresholds with respect to landscape-scale drivers (as these landscapes appear to be those that require some of kind of intervention to achieve island-wide nature conservation outcomes). The landscape assessment utilized a range of spatial data and survey data sources. The main GIS layers (SA EGIS data) included geology, topography, soils, rainfall, fire mapping and native vegetation cover. The biotic components of landscapes and ecosystems were analysed using two key survey datasets from the Biological Survey Databases of South Australia (BDBSA). Floristic survey data that have been collected using the standard survey design employed by the SA Biological Survey (Heard and Channon 1997) formed the basis for assessing ecosystem types. This dataset included all flora records that were collected on Kangaroo Island and stored in BDBSA. Variation in floristic composition was analysed using cluster analysis. Kangaroo Island bird data was obtained from the BDBSA in September 2013, and included all bird records that were collected on Kangaroo Island and stored in BDBSA between 1901 and 2013. All statistical analyses were performed using R-project for statistical computing for windows version 2.15.1 for windows (R Development Core Team 2008). 17 3.2 Landscapes 3.2.1 Landscape Description For the purposes of this analysis, landscapes were defined as contiguous areas with common biophysical and ecological features, whereby the relationship between the physical and ecological features was consistent, and where the response to key drivers was relatively consistent. The analysis largely precluded the differential impacts of post-colonial land-use history on landscape definition because of insufficient detailed and spatially explicit historical information. In order to create a common set of spatial boundaries, landscapes were spatially described by attributing each polygon in the soil landscape layer with the following additional information: Slope Class. Derived from the average slope across the polygon, which was calculated using the NASA SR-DEM (30m horizontal resolution). This average slope was then classified according to Australian Soil and Land Survey classification (National Committee on Soil and Terrain 2009). Relief Class. Derived from the minimum and maximum elevation across the polygon, which was calculated using the NASA SR-DEM (30m horizontal resolution). The difference between the minimum and maximum elevation (the relief) was then classified according to the relief classification of the Australian Soil and Land Survey(National Committee on Soil and Terrain 2009). Surface Geology. Derived from the Surface Geology layer. The existing geological classification was reclassified (based on geological age and description) to produce ecologically relevant surface geology. Rainfall. Derived from the Mean Annual Rainfall (MAR) model generated by ANUCLIM, using the NASA SR-DEM (30m horizontal resolution). The modelled MAR for each pixel was averaged across each soil polygon, and this average value was then classified to one of three rainfall classes: <600mm (Low), 600-750mm (Medium), and >750mm (High). Based on these four environmental features, polygons were attributed to the same landscape based on common patterns of geology, topography and rainfall. The landscape definitions that came from this did not necessarily have uniform physical features; rather, the patterns of variation within landscapes (environmentally equivalent to β-diversity (Anderson et al. 2011) were consistent relative to patterns of variation between landscapes. For practical reasons, the final landscapes used in this analysis were also required to be spatially contiguous, and be large enough in extent to warrant further within-landscape analyses, should it be required. 3.2.2 Landscape Analysis Following the definition of landscapes for Kangaroo Island, an assessment of each landscape was undertaken to determine if they are operating within acceptable limits in terms of their capacity to support dependent native biota. The application of the LSTM framework to Kangaroo Island was based on the following steps to assess landscape state and key ecological thresholds for each landscape: 1. Identify region-wide ecological drivers considered to be of primary importance to how landscapes function; 18 2. Identify the “position” of each landscape relative to key thresholds for each of these drivers (e.g. where a landscape sits relative to generally-derived remnancy thresholds); 3. Describe management recommendations for each landscape, including where more detailed analysis (at ecosystem level) is required. The outcome of step 3 informed the prioritisation of subsequent within-landscape analyses (that typically comprise the Landscape Assessment process). The information sources used to identify key thresholds for important drivers were dependent on the nature of these drivers. 3.2.2.1 Fire Regime A landscape-level evaluation of fire regime was undertaken based on thresholds for the upper and lower limits of the “acceptable “ fire regime, outlined in the Ecological Fire Management Guidelines for South Australian native vegetation (DENR 2012). These guidelines were applied to the Major Vegetation Sub-groups (MVS) found in each landscape (Table 1.). However, because the guidelines are based on a relatively small set of fire sensitive plant species there is little variation in the upper and lower thresholds for fire frequency across major vegetation types. Thus we have used a consistent upper threshold of 50 years, and lower threshold of 20 years, for all landscapes across the island. 3.2.2.2 Landscape level patterns of clearance of native vegetation For each landscape, an assessment of the proportion of the landscape that was mapped as remnant native vegetation was undertaken. This assessment was initially evaluated in the context of existing, generic thresholds for native vegetation of landscapes, particularly focussing on the 30% cover threshold. A number of authors have suggested that if native vegetation cover in a landscape falls below 30%, critical habitat functions for dependent flora and fauna are compromised (McIntyre and Hobbs 1999; Radford et al. 2005). However, the actual threshold for cover will depend on the requirements of the particular biota that depend on a system, and how different drivers (e.g. fire and fragmentation) interact to impact on these requirements (Cale 2007). 3.3 Ecosystems For landscapes that appear to approaching or have crossed critical ecological thresholds (as identified in the assessment of landscapes described above), an assessment of the state and trajectory of ecosystems within these landscapes was undertaken. This assessment was designed to determine if the systemic issues associated with landscapes at risk are related to drivers and impacts that are associated with particular ecosystems. 3.3.1 Ecosystem Assessment 3.3.1.1 Defining ecosystem types The description of Kangaroo Island ecosystems combines key physical drivers that are the primary determinant of an ecosystem’s distribution, and a description of the “typical” or “best remaining” floristic community that occurs in association with those key physical drivers. As with the definition of landscapes, the key physical drivers that determine the distribution of ecosystems on Kangaroo Island are geology, soil type, and rainfall. Topography also plays a minor role in some cases, such as for alluvial and drainage systems. 19 An analysis of existing floristic survey data was undertaken to quantitatively describe the different ecosystems of Kangaroo Island. This analysis investigated variation in floristic species composition among survey sites using hierarchical cluster analysis, using the “Jaccard” dissimilarity index and the “mcquitty” agglomeration method. This analysis was populated with an estimate of percent cover for each species at each site (taken from the survey dataset). Cluster analysis was implemented using ‘R’ statistical software, within the ‘vegan’ package. Based on the outputs of this analysis, ecosystems were defined based on the common physical attributes of the patches that occurred within clusters. The relationship between floristic similarity and physical attributes was done visually using the cluster outputs, with each patch attributed with its physical features. The physical features that were used to define ecosystems were soil type (taken from the DSM model), geology (1:50k mapping), rainfall, slope, relief and landscape (defined above). 3.3.1.2 Ecosystem level patterns of native vegetation clearance As with the analysis of vegetation clearance at the landscape level, an analysis of vegetation clearance patterns in relation to the ecosystems of landscapes at risk was undertaken. This was done on the basis of the spatial information for the key physical drivers identified for the ecosystem definition (see above), overlayed with the mapped remnant native vegetation. The results of this analysis then provided insight regarding the drivers of change to biodiversity at the ecosystem level, that was used in combination with other indicators (in particular, changes in the status of terrestrial birds and their association with different ecosystems). 3.3.1.3 Trends for Terrestrial Birds A key step in ‘landscape assessment’ is to determine the relative state and trajectory of different landscapes and ecosystems. In the past, this has been achieved by relating the state and trajectory of different terrestrial bird species, with their common ecological requirements, to determine the most parsimonious solution to patterns of state and trajectory among birds. They key assumption here is that if species that are commonly associated with a particular ecosystem also share similarities in their current state and historic trajectory, we can infer that this common state and trajectory is in some way related to the dynamics of the ecological requirements (particularly habitats or ecosystems) that they are commonly associated with (Rogers et al. 2012). In order to determine the status and trajectory of terrestrial bird species within the landscapes of Kangaroo Island, three analyses based on the historic and recent bird records of Kangaroo Island were applied. These analyses were constrained by the available records from the BDBSA and availability of expert knowledge and the outcomes of these analyses may be improved should additional datasets become available. The three analyses were: a. Difference in distribution between all-time, and “current” records, where current included all records that were collected after 1994 (method adapted from Franklin (1999)). i. The occurrence of bird species in each 100 ha polygon on Kangaroo Island was denoted for the period 1995-2013 (the recent period), or 1901-2013 (all-time). The degree of change between recent trends and all-time trends was then calculated as the proportion of hexagons in which a species was recently recorded (≥1995), compared to the number of times it had been recorded over the entire survey period (1901-2013). This analysis excluded 20 species with <10 records and/or those that had been recorded in <5 hexagons. b. Change in relative distribution through time, using linear regression between Year and Proportion of cells occupied. i. Linear regression was performed on the proportion of GIS mapping cells (hexagons) that were occupied by each species per year. Species were identified as declining in this analysis if the results of the regression indicated p values of <0.1, and a negative slope value. c. Expert Model (species status assessment) i. Expert scores of KI species ‘status’ and ‘trend’ (Gillam and Urban in prep.) were used to identify declining birds. Species were given the following ‘status scores’ based on their assigned conservation status: Extinct=6, Critically Endangered=5, Endangered=4, Vulnerable=3, Rare=2, Near Threatened=1, Least Concern or Data Deficient=0. Species trends were scored as: definite decline=-2, probable decline=-1, stable=0, probable increase=+1, or definite increase=+2. ii. Status and trend scores were combined to calculate an overall threat score: 0-1 = Least Concern, 2 = Rare but Stable, 3 = Widespread but Declining, 4 = Rare and Declining, 5 = Extinct (locally). Species that were assigned a threat score of 3 or 4 were identified as declining in this analysis. The results of these three analyses were used to calculate an overall ‘threat category’ for each species based on the number of analyses in which they were identified as declining (or not declining): 1. Threat Categories: 0. not identified as declining in any analyses 1. identified as declining in one analysis 2. identified as declining in two analyses 3. identified as declining in all three analyses. Species were assigned an overall ‘declining’ status if they were identified as declining in at least two of the three analyses. In addition to analysing state and trajectory of terrestrial bird species, a qualitative assessment of the requirements of terrestrial bird species, in the context of the ecosystem analysis, was also undertaken. This was done by using ornithological expertise and literature (e.g. Handbook of Australian, New Zealand and Antarctic Birds series). This allowed species to be assigned to “response groups” (Rogers et al. 2012), where species were assigned to groups based on their common ecological requirements. 21 4 RESULTS 4.1 Landscape Identification and Description For the purposes of this assessment, three landscapes were defined for Kangaroo Island: 1) West and South Coast, 2) Central Plateau and North Coast, and 3) Eastern Plains and Dudley (Figure 4). The primary discriminating features of these landscapes are their underlying geological patterns, together with rainfall and topography. Geological features are a primary determinant of soil properties, and soils can have a strong influence on the distribution and composition of ecological communities. The West and South Coast landscape is comprised of a coastal band that runs south from Cape Borda, along the entire south coast, almost as far as Cape Willoughby (a total area of 965 km2). The West and South Coast landscape also incorporates the entire ismuth between the Dudley Peninsula and main body of the Island. This landscape is dominated by Pleistocene calcrete that was formed as marine sediments during periods of high sea level. Along with this calcrete, recently deposited (and often active) Holocene marine sands are prominent. These near coastal environments largely support a range of coastal mallee and shrublands that are typical of these environments in other areas of the state (e.g. Eyre Peninsula and Yorke Peninsula). The Central Plateau and North Coast landscape is comprised of the higher elevation plateau of Kangaroo Island, and includes the entire north coast between Cape Borda and west of Emu Bay (a total area of 2,011 km2). This landscape is dominated by ironstone soils derived from Tertiary weathered materials. These Tertiary materials overlay Cambrian sedimentary materials that are expressed at the surface along areas adjacent to the north coast. Due to the erosional nature of these higher rainfall elevated environments, the Central Plateau and North Coast landscape is dissected by a number of drainage lines and narrow depositional areas that fan out to form the deeper depositional soils onto adjacent areas of the Eastern Plains and Dudley Peninsula. The Eastern Plains and Dudley landscape is comprised of the lower elevation depositional areas of Kangaroo Island. The geology and soils of this landscape are complex relative to the other landscapes of Kangaroo Island, but are largely dominated by the deposition of eroded soils from the Central Plateau (in the western parts of the landscape), along with a large number of lacustrine environments. The northern Dudley Peninsula contains Tertiary ironstone that is similar to the Central Plateau environment, although with lower rainfall. Other notable environments of the Eastern Plains and Dudley landscape include the igneous rises west of Kingscote that form the Wisanger Hills. 22 Figure 4. Map of Kangaroo Island highlighting the boundaries of the ecological landscapes used in this assessment. Blue= West and South Coast; Red = Central Plateau and North Coast; Green = Eastern Plains and Dudley. 23 4.2 Key Ecological Drivers on Kangaroo Island Consideration of broad patterns of historical land use change and interpretation of empirical data where it was available indicates that a number of key drivers appear to operate at the landscape scale, and/or at the scale of individual patches of remnant vegetation. These probably determine the state and trajectory of the majority of biota at these two scales. At the landscape scale, the key drivers identified were: fire regime; conversion of native vegetation cover for agricultural production; and population processes (particularly meta-population dynamics). In addition, a number of key drivers were identified that specifically relate to the dynamics of patches of remnant vegetation (noting that these drivers in turn can be derived from landscape-scale processes): grazing of remnant patches; and changes to physico-chemical processes (particularly dryland salinity). The logic framework of the Landscape State and Transition model (LSTM) is described above. Using this logic framework, critical ecological thresholds for the key drivers identified above were described, and the current state of the landscapes of Kangaroo Island, relative to these thresholds, was determined. The relationship between these thresholds and the current state of Kangaroo Island’s landscapes is presented graphically in Figure 8. The justification for this pattern is described below for each key driver. 4.2.1 Fire Regimes The pattern of fire across Kangaroo Island (equivalent to the current mosaic) for each landscape varies across the island and between different landscapes (Figure 5). This pattern shows that at a coarse level fire is a relatively infrequent occurrence in the Eastern Plains Dudley landscape, manifests as a gradient from relatively frequent fires in the west to fewer fires in the east of the Central Plateau and North Coast landscape, but is relatively common and close to evenly spread within the West and South Coast landscape. For each landscape, the average and current area within each decadal fire-age class was calculated, and compared with the critical thresholds identified for the dominant ‘Major Vegetation Subgroup’ MVS in each landscape (Table 1). The distribution of landscape area among these fire interval classes varied depending on whether the average fire interval or the current fire interval (i.e. time since last fire) is used as a measure of fire regime. West and South Coast The current fire interval for the West and South Coast (Figure 6) is skewed toward early fire-age classes, with 58% of native vegetation in the landscape having burnt in the last 20 years (<TPC1 for the dominant MVS in this landscape (Table 1). This skewness is driven by the recent large-scale wildfires across the intact, western end of Kangaroo Island. About 23% of native vegetation is currently within the acceptable fire interval range for the dominant MVS. However, given the requirement for ~30% of the MVS to have fire intervals less than the upper threshold, means the West and South Coast does not appear to contain enough area of older habitats (18%). This suggests that the requirements of plant species dependent on older seral stages (fire age classes) may be at risk. The average fire interval (based on the number of fires recorded since 1931) for the West and South Coast is dominated by older fire-interval classes, with 68% falling within the ‘acceptable’ thresholds for fire interval (2050 years), and another 30% having fire intervals greater than the upper threshold (TPC2, 40 years). Across the 24 landscape, only 1% of native vegetation has an average fire interval threshold of less than 20 years, suggesting that, while the recent (e.g. 2007) wildfires have placed large areas of the landscape in a young seral age class, over the past 81 years the average fire frequency is generally not higher than the acceptable thresholds for the dominant vegetation communities. Central Plateau and North Coast As with the West and South Coast landscape, the current fire interval for the Central Plateau and North Coast landscape is skewed toward early fire-age classes (58% burnt in the past 20 years, Figure 6), again with this pattern driven by recent large-scale wildfires across the intact, western end of the landscape. In addition, 33% of the native vegetation of the landscape currently occurs in fire interval classes greater than the upper threshold, again suggesting that the requirements of species dependent on older seral ages are currently being met. Only a small proportion of native vegetation (9%) is currently within the acceptable thresholds for fire interval (20-50 years). Furthermore, the distribution of fire interval classes is currently distributed non-randomly across the landscape, with older seral classes dominating the eastern end of the landscape, while younger seral classes dominate the western end of the landscape. Eastern Plains and Dudley The current distribution of seral classes in the Eastern Plains and Dudley landscape is heavily skewed toward older age classes. While 25% of native vegetation in the landscape has burnt in the last 20 years (i.e. is younger than the recommended lower threshold), 66% was last burnt more than 50 years ago (older than the recommended upper threshold). Thus just 7% of the native vegetation of the landscape current exists within the acceptable thresholds (Figure 6). This pattern of dominance by long fire interval classes in the landscape is further demonstrated when looking at average fire interval over the last 81 years. Across the 81 year period for which fire history data are available, 76% of native vegetation has an average fire interval greater than the recommended upper threshold (i.e. an average fire interval of >50 years; Figure 7). Only 23% of native vegetation has an average fire interval within the acceptable thresholds. 25 Figure 5. Distribution of current fire interval across the native vegetation of Kangaroo Island. The ecological landscape boundaries used for the purpose of this analysis are presented in relation to this fire regime. 26 MVS Name Area Central Plateau Eastern Plains TPC1: Lower threshold in years TPC2: Upper threshold in years Inter-fire intervals within TPC1 & TPC2 cross more than X% of the extent of of the MVS Percentage the this MVS within stay > TPC2 to area planning Avoid more than 2 fires within a period of X years Avoid more than 2 successive fires of low intensity (Yes/No) Some medium to high intensity fire needed to regenerate some species (Yes/No) Interval Spatial Criteria Frequen cy Intensity Season 8 Shrubby Eucalypt woodlands 1,529 39,086 6,868 20 50 40 30 40 Y Y Spring or during & following drought 26 Casuarina woodlands - 1,002 - 20 50 40 30 60 N N During & following drought 29 Mallee shrublands 76,01 3 49,472 15,49 2 20 40 40 30 40 Y Y Spring or during & following drought 47 Shrubby open Eucalypt woodlands - 13,045 1,017 20 50 40 30 60 N N During & following drought 49 Melaleuca shrublands - - 2,037 20 60 40 30 70 N N Spring Avoid more than 1 successive fires in season MVS West & South Coast Table 1. Ecological Fire Management Guidelines for fire-prone Major Vegetation Sub-groups (MVS) on Kangaroo Island. Fire-prone MVS were included in this list if >1,000 ha occurred in any one landscape. Two MVS (Chenopod shrublands, and Other shrublands), both of which are found on Kangaroo Island, were excluded from this table as they are not considered fire-prone, and therefore do not have acceptable fire regimes presented in the EFMG (DENR 2012). 27 Current Fire Interval Average Fire Interval Figure 6. Distribution of native vegetation by fire age classes (seral stages) for the three ecological landscapes of Kangaroo Island. Proportion (y-axis) of the area of native vegetation in different fire interval classes (x-axis). The current fire interval (years since last fire) are presented in the left column, the average fire interval (average years/fire, for period since 1931) are presented in the right column. The data for each landscape are colour coded: West and South Coast = green; Central Plateau and North Coast = blue; Eastern Plains and Dudley = red. Recommended acceptable limits for fire interval are bounded by red boxes for each chart. 28 4.2.2 Landscape level patterns of clearance of native vegetation West and South Coast The West and South Coast landscape can be considered Variegated-Intact (McIntyre and Hobbs 1999) (Figure 8), with 85% of the landscape mapped as native vegetation. The low level of fragmentation in this landscape is due to the dominant soil types, which are highly calcareous calcrete or sand, being unsuitable for agriculture (Hall et al. 2009). Central Plateau and North Coast Across the Central Plateau and North Coast landscape 54% of the landscape is mapped as native vegetation, and is considered Fragmented-Variegated (McIntyre and Hobbs 1999) (Figure 8). However, vegetation clearance is not evenly distributed across the landscape, with the majority of remnant vegetation being distributed at the western end. This uneven distribution of vegetation clearance is largely historical. The ironstone soils of the Plateau were considered unsuitable for agriculture until the end of the Second World War, and were only cleared for agriculture from that period. However, the Flinders Chase National Park was proclaimed in 1919, prior to the large wave of post-war vegetation clearance, and was thus protected from this period of clearance. Eastern Plains and Dudley The remnant vegetation of the Eastern Plains and Dudley landscape is fragmented (McIntyre and Hobbs 1999) (Figure 8) with only 27% of the landscape mapped as native vegetation. The remaining vegetation typically occurs as small isolated remnants, although a significant proportion of this mapped vegetation occurs on roadsides. 4.2.3 Other drivers The remaining key drivers particularly relate to the dynamics of remnant vegetation patches (particularly grazing, and physico-chemical changes). These were considered to be particularly relevant in discriminating the current state of the Eastern Plains landscape from the Central Plateau and West and South Coast landscapes. The key physico-chemical driver for the Eastern Plains is dryland salinisation, which in turn is driven by catchment-scale historic clearance of native vegetation (Robinson 1999). Soil salinisation within some remnants on the Eastern Plains is leading to the transformation of historic vegetation communities (e.g. mallee woodlands) to saline-tolerant communities (e.g. those dominated by samphire species and cutting-grass). Patches that cross thresholds relating to the nature of the physico-chemical environment (particularly in relation to dryland salinisation) are often considered irreversible, and as such management is often considered in relation to facilitated transformation based on these new physical conditions, rather than restoration of previously existing conditions and biotic communities (Standish et al. 2009). As with dryland salinisation, grazing impacts within remnant vegetation are particularly prevalent in the Eastern Plains and Dudley landscape. 29 Figure 7. Current distribution of remnant native vegetation on Kangaroo Island (Source: DEWNR EGIS Dataset). 30 Figure 8. Conceptual model of the three landscapes of Kangaroo Island, relative to key thresholds associated with landscape-scale and patch-scale drivers of ecological change. 4.2.4 Landscape Analysis – Summary The West and South Coast landscape appears to be largely operating within acceptable limits with regard to the key ecological drivers identified (Figure 8), although the recent large-scale wildfires suggest that consideration should be given to develop a more diverse fire age distribution across this landscape. The Central Plateau landscape is operating across a range of alternate states with regard to landscape-scale drivers, reflecting the variable land-use history of this landscape. While much of the landscape appears to be operating outside of acceptable limits with regard to fire regime, the interaction between fragmentation and land tenure (i.e. native vegetation on public versus private land) suggests that the fire regime in parts of the landscape may involve too frequent fire, while the fragmented eastern areas of the landscape appear to currently have a fire regime that is less frequent than desired (DENR 2012). The Eastern Plains and Dudley landscape appears to have crossed both the fire regime and fragmentation thresholds at the landscape scale, suggesting that the current regimes will lead to species decline and local extinction if not addressed. However, recent evidence from the Eastern Plains Fire Trial suggest that, due to the persistence of soil seed banks, population processes for many species have not yet broken down, as there appears in many cases to be adequate propagule banks to facilitate recovery, should these other processes be restored (Davies et al. 2013). 31 4.3 Ecosystem Assessment 4.3.1 Ecosystem Descriptions Based on the outcomes of the landscape-level assessment described above, the ecosystem-level assessments subsequently undertaken focused primarily on the Central Plateau and Eastern Plains landscapes. However, an initial analysis to describe the ecosystems of Kangaroo Island (with respect to both their physical and biotic components) was undertaken for the entire island. This analysis identified 12 broad ecosystems for Kangaroo Island. The key physical determinants of ecosystems were the landscape within which the ecosystem was typically found (which, in turn reflects the broad geology and climate drivers of the ecosystem – see landscape descriptions above), and, within landscapes, the soil types upon which the ecosystem was typically found. The 12 ecosystems used in subsequent assessments are listed below. The estimated distribution of soil types associated with the ecosystems listed in this document is shown in a series of maps in Appendix 1. The detailed descriptions of soil subgroups can be found in Hall et al. (2009). For each map, the shade of blue indicates the proportion of a soil landscape unit (SLU) polygon that is made up of the soil types of interest (light blue = <30%; med. blue = 30-60%; dark blue = >60%), and lists the vegetation types typically associated with the soil type. The mapping provides a general representation of the distribution of environmental settings that have the potential to support different ecosystems. As such it is analogous to a prediction of potential habitats at landscape scale. There may be finer scale drivers that override the predictions based on soil types, thus field data could be used to identify finer scale relationships between vegetation communities, soils types and landforms to improve the resolution of the mapping. West and South Coast 1. Eucalyptus diversifolia ± E. rugosa over Melaleuca lanceolata / Orthoxanthus multiflorus, on Shallow Soils over Calcrete. 2. Near coastal shrubland (Olearia axillaris, Leucopogon parviflorus, Carpobrotus rossii) ± E. diversifolia, on Deep Carbonate Coastal Sands and/or Shallow Soils on Calcrete near high energy coastlines. Central Plateau and North Coast 1. Allocasuarina verticillata open woodland, on Shallow Soil over Rock and/or occasionally Acidic Sandy Loams over Rock. 2. Eucalyptus cladocalyx over shrubland on Acidic Sandy Loams over Rock. 3. Eucalyptus baxteri ± E. cosmophylla over closed shrubland on Ironstone and/or Acidic Sandy Loams over Rock. 4. Mixed closed shrubland on Ironstone and/or Acidic Sandy Loams over Rock. 5. Riparian shrublands (Melaleuca gibbosa, Leptospermum continentale) and woodlands (Eucalyptus viminalis) along drainage lines. Eastern Plains and Dudley 1. Eucalyptus cneorifolia over mixed shrubland (Melaleuca uncinata) on a variety of soil types (predominantly Acidic Sandy Loams over clay). 2. Riparian shrublands along drainage lines. 3. Fringing vegetation of freshwater wetlands (Juncus pallidus, Melaleuca gibbosa, Callistemon rugulosus), 4. Low shrublands (Sarcocornia spp., Melaleuca oppositifolia) associated with Saline wetlands. 32 This analysis also identified some data gaps, particularly with respect to the relationship between soil type and vegetation type on the Eastern Plains. While a diversity of soil types occurs on the Eastern Plains, the floristic data suggest low diversity with respect to terrestrial ecosystems (in this broad analysis, one terrestrial ecosystem was identified for this landscape). However, observations suggest soil variation can promote floristic differences. This may require further analysis to broaden our understanding and guide restoration. 4.3.2 Ecosystem level patterns of native vegetation clearance As our descriptions of ecosystems were closely related to soil type, our analysis of vegetation clearance at the ecosystem level was done using the proportion of a mapped soil type that was mapped as native vegetation within each of the priority landscapes (i.e. excluding the West and South Coast landscape). The results of this analysis are presented in Table 2. Table 2. Area and proportion of remnant native vegetation for the dominant soil types in the priority landscapes of Kangaroo Island. Central Plateau and North Coast Soil Type Total Area (hectares) Vegetation Remnancy (%) Ironstone 83,041 38.9 Acidic Sandy Loam over Rock 76,594 62.4 Drainage Lines 15,745 82.6 Shallow Soil On Rock 5,127 79.4 Soil Type Total Area (hectares) Vegetation Remnancy (%) Ironstone 45,084 15.8 Acidic Sandy Loam over Rock 26,052 38.0 Drainage Lines 16,061 20.7 Deep Siliceous Sands Over Clay 12,193 26.4 Wet Saline Soils 7,315 46.4 Eastern Plains and Dudley For the Central Plateau, a pattern of preferential clearance appears to have focused on those ecosystems associated with Ironstone Soils, where remnancy is 38.9%. This compares with the remnancy of the shallower terrestrial soils (Acidic Sandy Loam over Rock – 62.4%, Shallow Soils over Rock – 79.4%), and the riparian systems (82.6%). This preferential removal of vegetation is strongly associated with the Eucalyptus baxteri /closed shrubland systems that are concentrated more in the east of the landscape. However, significant remnant patches of this ecosystem still occur within the protected areas of the western end of the landscape. For the dominant soil types of the Eastern Plains, the most heavily cleared soil type is Ironstone soils (15.8%). Riparian soils are also heavily cleared in this landscape (20.7%), while Acidic Soil over Rock has higher remnancy (38.0%). As expected, saline wetlands have the highest remnancy of the dominant types (46.4%). However, 33 compared with the rest of Kangaroo Island, even those ecosystems with higher remnancy have still been heavily impacted by historic vegetation clearance. 4.3.3 Avifauna Decline Of the three landscapes, a strong signal linking avian decline to particular ecosystems could only be found for the Eastern Plains landscape. Six species were considered declining by both data-driven analyses, with a further six species considered declining by one analysis. The six species that were considered declining in both analyses are Tawny-crowned Honeyeater Gliciphila melanops, Horsfield’s Bronze Cuckoo Chrysococcyx basalis, Golden Whistler, Pachycephala pectoralis, Brush Bronzewing, Phaps elegans, Bassian Thrush, Zoothera lunulata and Beautiful Firetail Stagonopleura bella. The strong relationship between shrub-dependent species and avian decline in the Eastern Plains is congruent with the decline in extent of Eucalyptus cneorifolia mallee woodlands, and changes in the condition of the understorey of remnants for this ecosystem. However, the mixed patterns of decline and lack of association between decline and particular ecosystems for the Central Plateau suggests inadequate information to guide restoration priority setting for this landscape. While the remnancy statistics presented above provide some guidance to focus on E. baxteri woodlands and closed shrublands on Ironstone, further analysis is required to determine the expected conservation outcomes of this restoration focus. A full list of species and predictions of their status in the three Kangaroo Island landscapes is presented in Appendix 2. 4.4 Eucalyptus cneorifolia Case Study The Eucalyptus cneorifolia community is arguably the most well studied ecological community on Kangaroo Island at present. This makes it ideal for demonstrating how detailed information can be used to develop fine scale analysis for conservation planning. The results that follow are based on work conducted as part of the Kangaroo Island Threatened Plants Project (Taylor 2003b) and the related Eastern Plains Fire Trial (EPFT 2008). The synthesis of these results in conceptual model format is relatively new, although some of the ideas for the patch scale state and transmission model (STM) were initially conceived in a study of KI mallee dynamics for the KI Biodiversity Monitoring Project (Pisanu 2007), and subsequently used for the recent EPBC Act nomination of the E. cneorifolia community complex. 4.4.1 The Eucalyptus cneorifolia Ecological Community Eucalyptus cneorifolia (Narrow-leaved) Mallee is critical habitat for five nationally threatened plant species (listed under the Environment Protection and Biodiversity Conservation (EPBC) Act 1999), four of which are endemic to KI and found only in the Eastern Plains area. Listed threatened plants are Beyeria subtecta (Vu), Caladenia ovate (Vu), Leionema equestre (En), Olearia microdisca (En), Pomaderris halmaturina ssp. halmaturina (Vu), Pultenaea insularis (En), and Spyridium eriocephalum var. glabrisepalum (Vu)(Taylor 2003b). Another 25 plant species are of conservation concern in the region (State or regionally listed) and the Eucalyptus cneorifolia Mallee community, that is almost entirely restricted to KI, has recently been nominated as a threatened ecological community complex under the EPBC Act. Key drivers of continued decline of the Eucalyptus cneorifolia community are habitat loss, habitat fragmentation and fire exclusion. Mallee was extensively cleared in eastern Kangaroo Island with the intensification of agriculture post Second World War. Native vegetation on has been progressively subdivided into smaller and more isolated fragments with 16% (15,198 ha) of the 95,205 ha cover now remaining in the Eastern Plains study area. One outcome of this fragmentation has been the effective restriction of wildfire spread. This has contributed to a situation where most E. cneorifolia patches have not been burnt for c35-70+ years. The exclusion of fire has created a senescent landscape where long lived overstorey species have become dominant at the expense of shorter lived understorey plants. Many remnants, including roadside strips, support as few as 3-8 perennial species, and vegetation structure is a canopy of mallee trees with a few shrub species and very 34 little ground layer diversity or cover in the understorey. Thus this landscape is currently dominated by senescent mallee remnants (EPFT 2008). Two projects have specifically addressed the impacts of habitat loss and fragmentation on E. cneorifolia communities. The Eastern Plains Fire Trial (2008-2013) implemented 42 prescribed burns to test fire as a means of stimulating the regeneration of senescent mallee and improve understanding of the role of fire in maintaining ecosystem health. The Kangaroo Island Nationally Threatened Plants project also directly addressed the causes of fragmentation by reinstating habitat to strategically buffer, enlarge and connect important E. cneorifolia remnants. Under this program 400,000 tubestock were planted over 212 ha to create highly diverse and selfsustaining habitats supporting threatened plant species. 4.4.2 Conceptual Model of Mallee Ecological Dynamics The conceptual model developed for Eucalyptus cneorifolia (Narrow-leaved Mallee) can broadly be described as a state-and-transition model (STM) in that it attempts to capture key vegetation states, describe different successional and disturbance pathways, and define where ecological thresholds are likely to occur (Figure 9). The model includes four gradients/drivers of change – landscape modification, fire, grazing pressure and dryland salinity. These all occur in this landscape to varying degrees and can influence the status of individual mallee patches. The model summarises a number of observations about the dynamics of Narrow-leaved Mallee and potential pathways of change as follows: 1. Landscape modification is a primary driver of change (Figure 9). The process involves change from intact vegetation cover to small remnants, through a process of patch scale change (Forman 1995) and ultimately results in alteration of the configuration of remnants at a landscape scale (McIntyre and Hobbs 1999). Patch (remnant) size is an important determinant of resilience because smaller patches are generally more susceptible to threatening processes than larger ones (States 1a-1d). Observations indicate a threshold exists between very small patches that still maintain some elements of native diversity (State 1d) and circumstances where small clumps of trees, or isolated individuals, remain in paddocks (1e). The most degraded state in the continuum in terms of biodiversity is 1f, which is effectively cleared pasture consisting of a mix of native and exotic grasses and forbs. 2. Fire is a second primary driver of change, shown in the STM as a time-dependent process, depicted as time from a point after a fire event (Figure 9). Narrow-leaved Mallee relies on fire for periodic regeneration of a diverse shrubby understorey, achieving a maximum level of diversity within a defined age range (estimated to be between 8-25 years) that coincides with an optimal regeneration time of c17-40 years (defined through vital attribute analysis)(Dowie 2006). The upper time limit for burning requires verification, therefore the STM places it conservatively at about 25 years based on observations that at 35+ years the transition to a community dominated by a mallee overstorey and a few shrubs tends to occur. It is assumed that in the absence of other major forms of landscape disturbance fire can be applied to restore the E. cneorifolia community at a patch scale but fire probably interacts with patch size. Therefore the STM shows this as being less important for intact areas and large patches (2a and 2b), under the assumption that they can become senescent but will respond positively to fire in terms of a transition back to high levels of understorey diversity. In contrast, we hypothesise that medium-small patches can cross thresholds to more highly degraded states (3c and 3d), where a combination of threatening processes may limit the influence of fire on restoring diversity. 3. A secondary driver of change (or threat) is grazing pressure. Grazing can impact on the native plant seedbank, resulting in lower rates of germination, establishment of fewer native species, or increased germination of exotic species following fire events (Davies et al. 2013). Also, grazing by stock and native herbivores can impact directly on above-ground regeneration post-fire. Thus while the STM shows this 35 pressure as being highest for medium-small patches (3c and 3d) where there is less resilience, it is plausible that secondary grazing impacts could occur in larger patches (2a and 2b). 4. The fourth driver of change is salinity that produces impacts associated with rising saline groundwater. In the STM the threshold for a transition to salt scalded terrain is shown in relation to its impact on cleared land (States 1f and 1g) but small salt scalds have been observed within some Narrow-leaved Mallee remnants. The resulting change in soil chemistry represents a substantial change in abiotic conditions and is considered to be a uni-directional transition to a different (degraded) vegetation type. As a result fire is assumed to have limited positive biodiversity benefits under these circumstances. Weeds are not shown in the STM but they can pose a significant threat to the Eucalyptus cneorifolia community, e.g. limiting post-fire regeneration of native species. Bridal Creeper (Asparagus asparagoides) and Bridal Veil (A. declinatus) are two of around 11 high impact weed species that occur in the study area. Bridal Creeper has been present on eastern KI for around 100 years, with the heaviest and most established populations occurring on roadsides (Ball 1996; Willoughby et al. 2001). Bridal Veil was first recorded on KI in 1984 (SA Herbarium record) and now infests an area of approximately 234 km2 in the east (Taylor 2004; 2005). Both species are highly competitive perennial climbers that, once established, can completely smother native vegetation. They are known to be sensitive to the direct impacts of high intensity fire but Bridal Creeper is an early post fire emergent. Plants such as Perennial Veldt Grass (Erharta calycina) are also fire sensitive but capable of invading burnt areas from adjacent sites (Willoughby et al. 2001). Figure 9. Conceptual model – Eucalyptus cneorifolia Mallee fire response in a fragmented landscape. 36 5 DISCUSSION 5.1 Understanding Drivers of Ecological Change Fire is clearly a key driver of change for terrestrial ecosystems on Kangaroo Island and its management currently involves a substantial commitment of resources, expended for both life and property protection and to promote various ecological values. This project has provided an opportunity to synthesise existing information on fire regimes at a landscape scale, and for the Eucalyptus cneorifolia ecological community, consider the role of fire on the basis of a more detailed dataset. Native vegetation fragmentation is also an important driver of change in natural systems and interacts with other drivers to shape ecosystems. The analysis of fire history for the West and South Coast landscape suggests that the fire regime, on average, is operating largely within acceptable limits (based on the current Ecological Fire Management Guideline, EFMG). Although, it is also clear that the recent large wildfires in 2007 that burnt over 90,000 ha have produced a dominance of early age classes. It is worth noting that fire ignitions in this landscape are largely lightning driven, with some deliberate fire based management interventions to protect specific assets, create buffers designed to limit the propagation of large fire events, and to mitigate fire impacts during emergencies (DEH 2009). This suggests that given the current dominance of young age classes, management should continue to facilitate an appropriate distribution of native vegetation in different seral classes by reinstatement of larger areas of older age classes through maintaining less frequent, large scale fires. The fact that the West and South Coast landscape is largely intact is a positive for conservation management but where vegetation has become variegated, management actions that actively promote habitat restoration and/or actions that promote maintenance of ecological function in the vegetation matrix should be considered. The bird analysis does not signal any significant declines in species or bird functional groups at this point. While beyond the scope of this project to comment on in any detail, continuing to build specific knowledge about species with specialist requirements, such as linked to fire regime, is a clear priority for conservation planning. With regard to average fire interval over the past 81 years, the Central Plateau and North Coast landscape has a fire history that suggests a higher than appropriate fire regime (with reference to the EFMG) has historically been in place. Since 1931, 25% of the landscape’s native vegetation has been exposed to fire intervals that, on average are lower than the recommended lower threshold (20 years). Fire ignition in this landscape is also lightning driven but where there is dense human settlement accidental ignitions do occur. Overall, 40% of the native vegetation of this landscape falls within the acceptable fire interval thresholds, while 35% of the landscape has fire intervals that are higher than the upper threshold. This pattern suggests that the requirements of biota that depend on older fire-age classes are largely being met in this landscape. At present 54% of the Central Plateau landscape is mapped as native vegetation, and this is either fragmented or variegated (McIntyre and Hobbs 1999). However, the distribution of vegetation clearance is not even across the landscape, with the majority of remnant vegetation being distributed at the western end. This uneven distribution of vegetation clearance is largely historical because the ironstone soils of the Plateau were considered unsuitable for agriculture until the end of the Second World War, and were only cleared for agriculture from that period. The Flinders Chase National Park had been proclaimed in 1919, prior to the large wave of post-war vegetation clearance, and was thus protected from this period of clearance. 37 Most ecosystems remain relatively intact with between 62.4% to 82.6% vegetation remnancy. However, in relative terms, ecological communities on ironstone soils (e.g. Eucalyptus baxteri ± E. cosmophylla over closed shrubland) appear to have been preferentially cleared in this landscape, suggesting that these could be a priority for management intervention such as restoration. Analysis of the pattern of disturbance on the Central Plateau indicates that more conservation effort should be focused on the eastern part where the combined effects of less than optimal fire regime and fragmentation signal that systemic alteration of landscape processes is taking place. The bird analysis presented here did not indicate any major declines in habitat quality but expert observations of the avifauna (not currently documented in detail) indicate that birds dependent on a shrubby understorey in woodland habitats have in fact declined historically since land clearing intensified (C. Baxter pers. comm. 2013). This suggests it would be advantageous to further elicit expert knowledge and collate local records more systematically to improve the bird dataset for this part of the island. A renewed focus on lessons learnt from existing habitat restoration and onground works programs to design conservation management for the Central Plains and North Coast landscape is also recommended. Something that land managers need to consider is the deliberate application of fire in fragmented areas where fire has been absent for long periods, however, this should be done with deliberate biodiversity objectives in mind to avoid adverse ecological outcomes. In practice, this will require consideration of the trade-offs for fire management around asset protection, particularly where large-scale buffers are to be implemented to prevent fire spread. In some cases buffer burns may include ecological benefits but in others cases, such as requirements to establish low fuel loads over the long-term, frequent burning is likely to bring dis-benefits for conservation. Thus NRM should be explicit about this in order to, for example, identify potential actions for positive outcomes in other areas The current distribution of fire classes in the Eastern Plains landscape is heavily skewed toward older age classes and only 7% of the native vegetation of the landscape current exists within the acceptable thresholds. This pattern of dominance by long fire interval classes in the landscape is further demonstrated when looking at average fire interval over the last 81 years, with only 23% of native vegetation having an average fire interval within acceptable thresholds. Based on the EFMG, the Eastern Plains landscape is currently operating outside of acceptable limits for biodiversity conservation with regard to fire regime. This is not surprising given the relatively long history of close settlement and intensive land use on this part of the island. The remnant vegetation of the Eastern Plains landscape is fragmented (McIntyre and Hobbs 1999) with only 27% of the landscape mapped as native vegetation. The remaining vegetation typically occurs as small isolated remnants, although a significant proportion of this mapped vegetation occurs on roadsides. All environments support low native vegetation remnancy and interestingly the small area of ironstone soils on the Dudley Peninsula has been heavily cleared (15.8% remnancy). Close to half of wet saline soils are also cleared, although this pattern probably includes soils that have become affected by dryland salinity. Managing these environments is challenging and lessons from studies of salt affected eucalypt woodlands in the WA wheatbelt suggest considerable investment is required to rehabilitate these landscapes to a productive state (Standish et al. 2009). Six species bird species also appear to be in decline in the Eastern Plains and Dudley landscape. Tawny-crowned Honeyeater Gliciphila melanops, Horsfield’s Bronze Cuckoo Chrysococcyx basalis, Golden Whistler Pachycephala pectoralis, Brush Bronzewing Phaps elegans, Bassian Thrush Zoothera lunulata and Beautiful Firetail Stagonopleura bella are all, to a greater or lesser extent, dependent on or have a preference for woodland habitats with a shrubby/heathy understorey. When coupled with the research on the ecology of threatened plants in the Eucalyptus cneorifolia community, 38 which has been identified as critical habitat for seven nationally threatened species and another 25 plant species that are rare in the region, it is obvious that the current prioritisation of the Eastern Plains and Dudley landscape as a high priority for conservation actions is a sound strategy. There are other lessons to be learnt from the Eastern Plains. Patch-scale data and observations strongly indicate that physico-chemical alterations to habitat conditions (e.g. dryland salinity), grazing pressure from both native and introduced herbivores and weeds can combine to substantially degrade ecological resilience. However, this assessment recognises that there is still a lack of detailed data (or synthesis of existing knowledge) on the impacts of many of these threats on both ecological communities and species. Some of this work is currently being done for Narrowleaved Mallee but there are still scientific and management challenges to address. A key overarching challenge is to gain a better understanding of how processes at different scales interact, an example being changes in landscape-scale fire regime that impact on biodiversity at the scale of individual patches of remnant vegetation, and a second relates to understanding how the drivers of change themselves interact. An example of the latter is that fire regime can be driven by the fragmentation of remnant vegetation (through conversion for agriculture) because small, isolated patches tend to burn less often than large, intact patches (see further discussion of fire regimes and knowledge building below). The STM presented for the Narrow-leaved Mallee community is an example of a useful tool for defining interactions, and developing hypotheses about processes and thresholds that signal ecosystem decline. For key ecological drivers, thresholds have been identified that once crossed it is predicted that ecosystem will operate in an inherently different way that no longer supports the full suite of biodiversity found historically or currently. At a regional scale, some information is available to suggest where landscapes sit in relation to grazing regime, physico-chemical processes and population processes, but quantitative thresholds have only identified for the landscape-scale drivers of fragmentation and fire regime. This highlights a general limitation related to a lack of high resolution time series data for many drivers of change in Kangaroo Island landscapes. From a management perspective, similar conceptual models for KI ecosystems could be developed relatively easily, particularly for situations where good data exists for some biota or biological processes and/or there is a good level of expert understanding. The decline of Stringybark woodlands due to koala browsing pressure is a good example, as there is sufficient knowledge available to develop a fine-scale management model for regional woodland recovery. These models can also ultimately have a practical application as a guide for target setting and investment in onground actions. While beyond the scope of this report, it would be possible to identify a range of priorities for conceptual model building in a workshop setting with regional experts. 5.2 The Potential Role of Corridors A key objective of this project is to “Identify priority landscapes and corridors across Kangaroo Island”. The project goes some way to identifying priority landscapes but has deliberately avoided explicit consideration of corridors as a means for achieving conservation outcomes. The reasons for this are discussed below. Corridors have long been a subject of interest in restoration ecology and they are promoted as part of programs both nationally, National Wildlife Corridors Plan (DSEWPC 2012), and within SA, through NatureLinks planning (DEH 2006). Substantial research effort has produced an impressive body of theoretical work on the importance of corridors for biological conservation, yet generalisations regarding how to implement them remain elusive (Schmiegelow 2007) and significant controversy still surrounds the design and efficacy of corridors for meeting conservation objectives (Rouget et al. 2006). 39 The use of corridors as a conservation approach stemmed from the theoretical ideas originating with the equilibrium theory of island biogeography (MacArthur and Wilson 1967) and the assertion that habitat fragments linked by corridors are likely to have greater conservation value than isolated fragments (all else being equal) (Diamond et al. 1976). Many large-scale processes such as biota movement, geographic speciation and responses to climate change are associated with environmental gradients at landscape scales, and large-scale corridors (or landscape linkages) could potentially capture environmental gradients and facilitate these sorts of biotic interactions and processes both spatially and temporally (Rouget et al. 2006). A common goal for establishing corridors cited in the conservation literature is to use them to enhance or maintain the viability of populations in heterogeneous landscapes, particularly animal population, under assumptions that corridors increase potential for immigration, reduce inbreeding depression and demographic stochasticity, increase accessibility to resources for far-ranging species and provide additional habitat (Schmiegelow 2007). Indeed, corridors have proven beneficial for some Australian species, such as facilitating the movement of Rufous Bristlebirds in Victoria (Du Guesclin, Smith et al. 1995). The literature on corridors highlights some disadvantages, such as potential for transmission of disease, fire and other catastrophes, conduits for invasive species and increased road kill (Schmiegelow 2007). The issue of whether road kill is strongly associated with native vegetation on roadsides (a form of corridor) on Kangaroo Island has been the subject of some debate. Thus current views about corridors tend to conclude that they are valuable for some species and landscapes and establishing physical corridors is one approach to facilitating movement and reducing isolation (Gilbert-Norton et al. 2010). However, it is recognised that other actions that are alternative or complimentary to corridor establishment, such as improving management of the agricultural matrix to increase landscape permeability, also deserve attention (see examples below). Ultimately, determining the best strategy to address connectivity involves careful consideration of the life-history characteristics of target species, the state and condition and dynamics of the landscapes they occupy, and spatial and temporal scales of concern (Schmiegelow 2007). When it comes to climate change, it is generally assumed that facilitating the maintenance of larger populations as well as shifts in species distributions, should help native species adjust to changing climates, however, it remains unclear exactly how to design landscapes to best achieve these goals. Part of the complexity is that a range of possible changes in land uses and shifts in species distributions are expected under climate change and these could interact with landscape design approaches for biodiversity (Doerr et al. 2013). Given the uncertainties surrounding the establishment of corridors for conservation, it is perhaps best to view the NatureLinks concept of corridors as representing a desire to increase ecological connectivity at a regional scale. This recognises corridors as one potential management response to restoring degraded or declining landscapes, while understanding that corridors are not a panacea for solving all conservation problems. Practically, it will be possible to use results from the landscape assessment to inform whether implementation of corridors is appropriate for landscapes of interest, and how other management actions may be used instead of or in conjunction with corridor restoration. This could potentially include establishment of corridors (both small and large-scale), buffers, understory plantings in degraded patches, new patches and/or implementation of other types of maintenance actions (fire, pest and weed control, and fencing) in cleared landscapes to achieve specified conservation objectives. 5.3 Improving Knowledge Comprehensive and spatially-explicit quantitative data are not available for many drivers of landscape change on Kangaroo Island, making it difficult to accurately estimate the magnitude of 40 impacts and rates of change, and reliably identify thresholds that determine ecosystem resilience. Knowledge building is a key part of adaptive management under the assumption that science and management can work together to produce evidence and refine conservation practice over time, and in a structured way. The knowledge gaps discussed here are based on an overview of evidence used for the purposes of this project, recognising that some knowledge may exist that has not be utilised fully or simply could not be used effectively within the time constraints of the project. 5.3.1 Fire Regimes Fire is recognised as a key driver of change on Kangaroo Island and considerable scientific and practical knowledge is available for fire management. However, understanding fire regimes is complex and remains challenging worldwide. The two most important factors for determining fire regimes are vegetation type (or ecosystem) and weather and climate patterns. At a site scale, fire regime is determined by intervals between fires, burn season, fire intensity and whether the fire burns surface fuels or below ground (Gill 2012). Two of these, fire season and fire intensity, are being investigated experimentally in Narrow-leaved Mallee by the EPFT (EPFT 2008). When scaled up to landscapes, fire regimes tend to be expressed as dynamic mosaics because landscapes are not uniform and fires do not burn evenly across them. Topography, rockiness, discontinuities in fuel and chance events (stochasticity) can all influence how fire occurs in landscapes (Keith 2012), as can the deliberate application of fire to manage fuel loads and/or biodiversity (prescribed burning) (Gill 2012). There is a reasonable body of empirical evidence that diversity in biological composition and structure at a range of spatial scales contributes to different aspects of landscape resilience. This includes diversity in relation to the age structure of a landscape (in terms of time since fire), fire intervals, intensity and season of occurrence (McCarthy 2012). Despite this general understanding of fire regimes, many assumptions about fire remain untested. There are particular gaps in knowledge about how fire influences fauna populations (Clarke 2008), including a widely held assumption that animals respond to fires as discrete events in time and space, primarily in terms of fire intensity and interval (Bradstock et al. 2005), and a lack of certainty around the importance of factors such as quantity (area) and configuration of patches of differing burn or fire interval status, particularly in relation to species that may require long-unburnt and infrequently burnt habitat (Bradstock et al. 2012). There is no detailed history of the management of bushfire on Kangaroo Island for the early postEuropean settlement period but it is likely that fire was used as part of the process for clearing vegetation such as mallee (Dowie 2005). Following the establishment of agriculture, fire appears to have been excluded from the landscape where possible to protect built assets and land used for agricultural production. Evaluation of historically recent data indicates that a number of ecological communities located in areas of intensive agricultural activity, such as Eucalyptus cneorifolia Mallee, currently fall outside of the recommended fire free interval of between c17-40 years defined through vital attribute analysis (Dowie 2006), and additional evidence presented here tends to reinforce that large parts of Kangaroo Island are in states outside of optimal in terms of fire age. There has been limited research and synthesis regarding fauna responses to fire on the island, although current work as part of the EPFT is addressing some gaps (e.g. J. March unpublished) and a limited baseline focusing on birds from the EPFT could be used to increase knowledge of fauna responses and fire requirements. A major practical management challenge is to implement a well thought out program for burning in a fragmented landscape where wildfire is largely absent and is routinely suppressed to protect life and property. One way forward is to more clearly articulate a‘ landscape ecology fire model’ and use 41 prescribed burning to test the veracity of the model over time, in much the same way as is being done at a patch-scale by the EPFT. This should help to increase certainly about the role of fire over time. Precedents for this type of adaptive management do exist in the conservation planning literature (e.g. McCarthy 2012). 5.3.2 Other Threats and Drivers of Change Large areas of remnant native vegetation remain unfenced, so stock probably negatively impacts on tree, shrub and groundcover recruitment and vegetation health, and stock also contribute nutrients to soils. However, there is a lack of detailed information on stocking rates and associated impacts, and while there is some evidence that fencing protects native vegetation we are not aware of a systematic evaluation of how stock management contributes to conservation outcomes across the island. Soil enrichment is a consequence of direct addition of nutrients to improve pasture and crop production that has clear production benefits (Dohle 2007). The secondary impacts of nutrients on remnant native vegetation, such as toxicity to native plants and promotion of weeds, would have increased following the establishment of widespread application of superphosphate, minerals and elements for conditioning of agricultural soils (Mooney and Grinter 2000) but these impacts remain unquantified at present. Salinity is recognised as a priority natural resource management issue on Kangaroo Island, affecting both land and water resources. The major type of salinity is groundwater driven salinity, or salinity associated with a saline watertable. An evaluation in 2002 identified large areas of primary (natural) salinity, estimated at 4100 ha, and secondary (human-induced) salinity, estimated at 5600 ha in 2002, and secondary salinity is predicted to increase to 8000 ha by the year 2050 (Dooley et al. 2002). Salt mostly affects areas with flat and low lying terrain and poorly drained soils, but also impacts on gullies, river courses and lagoons (Mooney and Grinter 2000). Salt scalding in native vegetation results in altered abiotic (soil and groundwater) conditions and replacement of dryland trees, shrubs and groundcover with salt tolerant plants such as reeds, sedges and grasses. This level of change in ecological conditions represents a major, largely irreversible state shift (see Narrowleaved Mallee case study). We are not aware of a systematic evaluation of salinity impacts on native vegetation at the ecosystem scale on Kangaroo Island. High population densities of native animals can have negative impacts on native vegetation and agricultural production. Land clearance and changed water availability seem to have favoured Tammar Wallaby (Macropus eugenii), Western Grey Kangaroo (Macropus fulignosus) and Common Brushtail Possum (Trichosurus vulpecular) (Willoughby et al. 2001). Herbivores can restrict the rehabilitation of fragmented native vegetation by reducing rates of plant recruitment, and significant investment in new or improved infrastructure (such as fencing) is required to ensure long term management outcomes are achieved. Some anecdotal evidence is available from the KI Threatened Plants Project to support the idea that restricting native herbivory has positive conservation benefits and it is being tested experimentally as part of the EPFT. Another native animal that has impacted substantially on native vegetation is the koala (Phascolarctos cinereus). In less than a century koalas shifted from a threatened species introduced to KI for conservation purposes to one of pest status. The original population of 18 animals in 192325 spread progressively across Kangaroo Island and by 1994 the population was estimated at ~5000. There were significant impacts on Eucalyptus viminalis ssp cygnetensis recorded at this time, with over 50% of the canopy of most trees defoliated. The South Australian Government (DEH) implemented a control program in 1997, and a more detailed census and analysis in 2001 revealed that the koala population was much larger at ~27,000 than previously thought (Masters et al. 2004). 42 After intensive management the population is estimated to currently be approximately 14,000 and tree health has shown significant improvement. As discussed earlier in this document it would be possible to undertake a synthesis of existing knowledge to better define restoration goals for E. vimanalis woodland. Weeds risks have been evaluated at a regional scale to determine biosecurity goals and to guide investment in control programs (e.g. Gellard and Pisanu 2005) but a further synthesis of weed impacts at an ecosystem scale would be beneficial for conservation management. Many questions also remain about how weeds interact with other drivers of change such as fire regime and soil nutrient enrichment. The EPFT will provide information about some of these processes once trial data is analysed. The plant pathogen Phytophthora cinnamomi was first detected on Kangaroo Island in the early 1990s but positive confirmation of its presence in many areas has been difficult (Taylor 2003a). It is known to have the potential to impact on Eucalyptus, Xanthorrhoea, Banksia and Grevillea, but it has proven to be difficult to study, both on Kangaroo Island and Australia-wide, and a number of questions remain about how it impacts on vegetation health in different ecological settings (Mooney and Macphee 2007). 43 6 RECOMMENDATIONS 6.1.1 Priority landscapes and ecosystems for conservation activity 1. The terrestrial bird analysis presented here, as well as existing knowledge and new analysis that highlights less than optimal fire regimes, reinforces the need to keep addressing management issues in the most altered landscapes of Kangaroo Island. The most obvious is the Eastern Plains and Dudley landscape which is essentially fragmented and has a number of highly altered ecosystems, such as associated with the Narrow-leaved Mallee community complex. Continued management efforts to address issues such as fire regime, grazing pressure, weeds and salinity will be needed to ensure that resilience in this landscape is maintained and improved over time. 2. The second key landscape to focus on is the Central Plateau and North Coast. The fire regime for this landscape appears to be operating, at least in parts, outside of optimal limits in terms of age classes. At an ecosystem scale the terrestrial bird analysis did not flag any major declines in ecological resilience at this time, however, anecdotal evidence suggests that some changes may be occurring that could lead to losses of ecosystem function in the future. However, preferential clearing of woodlands on ironstone makes these a logical priority for future management effort. 6.1.2 Additional knowledge building 3. For the Eastern Plains, better use could be made of existing knowledge by further testing the hypotheses presented in the STM that identify potential thresholds and highlight the potential synergistic impacts of different drivers and threats. We are also aware of existing thinking about management interventions arising from the EPFT that could be integrated with the science foundation from the Trial and the work presented here to develop an adaptive management framework. This would provide the advantage of making more explicit inks between on-ground works and ecological outcomes. This type of knowledge can then be used to review NRM management targets and determine the cost-effectiveness of investments. Extension of this type of approach could then form a model for a management framework for other ecosystems of concern. 4. Scaling up patch-scale results from the EPFT would be beneficial in terms of shaping a landscape-scale management program, but will require applying new analytical methods not previously used on KI. The lessons learnt from doing this would translate to fire management more generally and allow for better use of fire for achieving ecological outcomes. This is a general issue for the whole island and, indeed, a challenge Australia-wide that reflects limited understanding about how fire regimes manifest at landscape scales, including how fire shapes species meta-populations, particularly fauna. 5. Using bird species as indicators of landscape and ecosystem function is an effective way of evaluating ecological resilience but it does require good quality monitoring data. We recommend that KI considers further investment in bird monitoring in a targeted way to track changes in ecosystems of concern, such as fragmented parts of the Central Plateau. It is likely that local bird data is available for some ecosystems and this could be included in DEWNR databases to improve coverage for Kangaroo Island. 6. There are opportunities to make better use of existing data and expert knowledge in a structured way. The focus of this should be on evaluating how different threats impact on 44 ecosystems, and how these threats combine or manifest synergistically, and how management currently responds to these challenges. 7. While not a primary focus of this report, we recognise that climate change planning could be informed by the work presented here. The landscape scale analysis provides a baseline that when combined with information on potential exposure of biodiversity to future climates will allow for development of a biodiversity risk analysis for the terrestrial systems of the island. 8. We recommend continuing the partnership between SMK and the Kangaroo Island region to take advantage of existing science capability and the extensive local knowledge within the region. 45 7 CONCLUSION This study addresses a key objective of the NatureLinks program for Kangaroo Island – to identify priority landscapes (for biodiversity management). It has achieved this by focusing at a landscape scale to develop a regional (island wide) analysis and to further evaluate the finer scale of ecosystems nested within landscapes. Of the three broad landscapes identified for Kangaroo Island, one, the West and South Coast, is currently relatively intact with coastal mallee and shrublands having a high degree of ecological function and resilience overall. The fire regime is, on average, operating within acceptable limits but care will need in future to ensure that older age classes are reinstated in areas of the west and south coasts affected by the December 2007 fires. The Central Plateau and North Coast landscape is divided into variegated and fragmented sections from west to east, and the fire regime in more disturbed areas is dominated by older age classes . No major declines in ecological function were detected by the bird analysis but fragmented areas should be the focus of further assessment and management effort to prevent future declines. Where ecosystems have been cleared preferentially, such as on ironstone soils, further evaluation of the need for maintenance and restoration should be undertaken. The Eastern Plains and Dudley has had the most prolonged and intensive land use history on Kangaroo Island and it is now largely fragmented. This coupled with alteration of the natural fire regime has resulted in widespread senescence of remnant mallee communities. The bird analysis indicates that at least six species are declining, a further signal of changed ecological conditions on this part of the island. Other threats associated with intensive land use, such as salinity, weeds, changed soil conditions and grazing pressure, are also apparent. The recent interest by NRM in threatened plant species and the community they occur in has prompted knowledge building and the testing of management interventions such as fire. There is an opportunity to build this effort into a working adaptive management approach and use this as a model for ecosystem management on the island more widely. The work presented here does not explicitly identify corridors but recognises that corridor restoration may be one option to use in conjunction with others to improve the quality of biodiversity in the agricultural matrix. A number of opportunities for building new knowledge and future collaboration between SMK and regional NRM managers have been identified. 46 8 REFERENCES Akçakaya H. R. (2001) Linking population-level risk assessment with landscape and habitat models. 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For each map, the shade of blue indicates the proportion of a soil landscape unit (SLU) polygon that is made up of the soil types of interest (light blue = <30%; med. blue = 30-60%; dark blue = >60%). Figure A1.1. Distribution of shallow soils on calcrete (soil subgroups B1, B2 and B3) within the West and South Coast landscape. In this landscape, these soil types are typically associated with coastal/subcoastal mallee (Eucalyptus diversifolia and E. rugosa over Melaleuca lanceolata, Orthoxanthus multiflorus- ecosystems 1, 3 and 11). Figure A1.2. Distribution of carbonate sands (soil subgroup H1) within the West and South Coast landscape. In this landscape, this soil type is typically associated with coastal shrublands (e.g. Leucopogon parviflorus, Olearia axillaris - ecosystems 2 and 4). 53 Figure A1.3. Distribution of shallow soils over Pre-Cambrian sedimentary rocks (soil subgroup L1) in the Central Plateau landscape. In this landscape, this soil type is typically associated with she-oak (Allocasuarina verticillata) woodlands (ecosystem 5), although sclerophyllous woodlands dominated by Eucalyptus cladocalyx (ecosystem 7; ) can also occur. Figure A1.4. Distribution of acidic sandy loams over brown or grey clay over rock (soil subgroup K4) in the Central Plateau landscape. In this landscape, this soil type is typically associated with sclerophyllous woodlands dominated by Eucalyptus cladocalyx (ecosystem 7), although sclerophyllous woodlands dominated by Eucalyptus baxteri and E. cosmophylla (ecosystem 9; ) can also occur. 54 Figure A1.5. Distribution of ironstone soils (soil subgroup J2) in the Central Plateau landscape. In this landscape, this soil type is typically associated with sclerophyllous woodlands and shrublands dominated by Eucalyptus baxteri and E. cosmophylla (ecosystem 9). Figure A1.6. Distribution of wet saline soils (soil subgroup N2) in the Eastern Plains and Dudley landscape. In this landscape, this soil type is typically associated with low samphire shrublands and Melaleuca halmaturorum woodlands (ecosystem 6). 55 Figure A1.7. Distribution of soils associated with narrow-leaved mallee communities in the Eastern Plains and Dudley landscape. In this landscape, a range of communities exist with Eucalyptus cneorifolia as an overstorey dominant, on a range of soil types that are less susceptible to waterlogging and inundation. Other mallee, such as Kingscote mallee may occur where conditions are suitable. 56 Appendix 2. Trend analysis for terrestrial bird species within landscapes of Kangaroo Island Landscapes Trend analysis for terrestrial bird species within each of the three defined landscapes of Kangaroo Island. Change refers to the proportion of hexagonal cells (cell size = 100 ha) where a species was recorded after 1995, compared with those cells where the species was recorded all time (e.g. a value of 0.5 refers to the fact that the species was recorded in one half of cells in which it was recorded alltime, after 1995). Species were considered declining for this metric if dChange was less than 0.7. r2 refers to the r2 value for the linear regression between Year and the proportion of cells (within which any bird was recorded) that the species was recorded. Direction refers to the trend analysis direction; - refers to a significant (p<0.1) negative trend with time, + refers to a significant positive trend. Direction is left blank if the relationship between Year and proportion of cells occupied was not significant (p>0.1). Species were considered declining if Direction was negative and the regression analysis was significant (p<0.1). # analyses refers to the number of analyses (max=2) where a species was considered declining within a landscape Table A2.1. Eastern Plains and Dudley Landscape Species Bassian Thrush Beautiful Firetail Brush Bronzewing Golden Whistler Horsfield's Bronze-cuckoo Shining Bronze-Cuckoo Tawny-crowned Honeyeater Fan-tailed Cuckoo Change 0.63 0.67 0.6 0.69 0.53 0.57 0.57 0.6 r2 Direction # analyses 0.57 0.31 0.55 0.5 0.96 0.84 0.48 0.05 - 2 2 2 2 2 2 2 1 - 1 1 1 1 1 1 0 Grey Shrike-thrush Little Wattlebird Western Whipbird White-browed Scrubwren White-fronted Chat White-naped Honeyeater Australasian Pipit 0.72 0.71 0.83 0.83 0.76 0.91 0.95 0.73 0.51 0.9 0.35 0.33 0.33 0.36 Australian Magpie 0.88 0.01 Australian Raven Black-faced Cuckoo-shrike 0.92 0.82 0.36 0.001 1 0.04 0 Brown Falcon 0.71 0.06 0 Brown Goshawk 0.92 0.3 0 Brown Thornbill 0.87 0.08 0 Brown-headed Honeyeater 0.86 0.02 0 Bush Stone-curlew Collared Sparrowhawk 0.84 0.78 0.47 0.18 Common Bronzewing 0.82 0.03 Black-shouldered Kite 0 + + 0 0 0 0 0 57 Species Crescent Honeyeater Change 0.87 r2 Direction # analyses 0.04 0 Crimson Rosella 0.93 0.04 0 Dusky Woodswallow 0.85 0.2 0 Eastern Spinebill 0.82 0.11 0 Galah 0.86 0.04 0 Grey Currawong 0.78 0.05 0 0.9 0.19 0 Laughing Kookaburra 0.87 0.01 0 Little Corella Little Raven Magpie-lark 0.91 0.86 0.89 0.44 0.66 0.05 Nankeen Kestrel 0.93 0.001 0 New Holland Honeyeater 0.81 0.13 0 Peregrine Falcon 0.92 0.16 0 Purple-crowned Lorikeet 0.77 0.005 0 Purple-gaped Honeyeater 0.7 0.07 0 Rainbow Lorikeet 0.83 0.0004 0 Red Wattlebird 0.83 0.06 0 Red-browed Finch 0.92 0.24 0 Restless Flycatcher 0.79 0.29 0 0.8 0.59 0 Scarlet Robin 0.82 0.19 0 Shy Heathwren 0.71 0.07 0 Silvereye 0.81 0.08 0 Southern Boobook 0.8 0.01 0 Spotted Pardalote 0.87 0.11 0 Striated Pardalote 0.78 0.002 0 Striated Thornbill 0.86 0.01 0 Superb Fairy-wren Swamp Harrier Tree Martin 0.83 0.93 0.86 0.37 0.61 0.03 Wedge-tailed Eagle 0.94 0.04 0 Welcome Swallow 0.89 0.15 0 White-eared Honeyeater 0.84 0.01 0 Willie Wagtail Yellow-tailed Black-Cockatoo 0.89 0.88 0.31 0.05 Grey Fantail Rock Parrot + + + + + 0 0 0 0 0 0 0 0 58 Table A2.2. Central Plateau and North Coast Landscape Species Black-faced Cuckoo-shrike Australasian Pipit Brown Falcon Change 0.69 0.5 r2 0.31 0.03 Direction - # analyses 2 1 0.5 0.07 Crimson Rosella Fan-tailed Cuckoo 0.84 0.53 0.17 0.14 Horsfield's Bronze-cuckoo 0.38 0.03 Silvereye Southern Boobook 0.76 0.6 0.41 0.07 - 1 1 Western Whipbird White-browed Scrubwren White-fronted Chat 0.95 0.76 0.62 0.83 0.22 0.006 - 1 1 1 Yellow-tailed Black-Cockatoo Australian Magpie 0.8 0.91 0.33 0.02 - 1 0 Australian Raven 0.88 0.16 0 0.9 0.11 0 0.76 0.01 0 1 0.55 0 Brown Thornbill 0.85 0.05 0 Brown-headed Honeyeater 0.84 0.01 0 Brush Bronzewing 0.78 0.09 0 Bush Stone-curlew 0.7 0.12 0 Common Bronzewing 0.81 0.13 0 Crescent Honeyeater 0.86 0.07 0 Dusky Woodswallow 0.73 0.03 0 0.8 0.08 0 Elegant Parrot 0.71 0.17 0 Galah 0.78 0.006 0 Golden Whistler 0.7 0.16 0 Grey Currawong 0.87 0.05 0 Grey Fantail 0.87 0.07 0 Grey Shrike-thrush Laughing Kookaburra 0.74 0.9 0.22 0.45 + 0 0 Little Corella Little Raven 0.85 0.83 0.71 0.01 + 0 0 Little Wattlebird 0.78 0.23 0 Magpie-lark 0.88 0.01 0 Nankeen Kestrel 0.73 0.03 0 New Holland Honeyeater 0.81 0.09 0 Bassian Thrush Beautiful Firetail Black-shouldered Kite Eastern Spinebill 1 - 1 1 1 59 Species Painted Button-quail Change 0.83 r2 Direction # analyses 0.11 0 Peregrine Falcon 0.71 0.01 0 Purple-crowned Lorikeet 0.83 0.001 0 Purple-gaped Honeyeater 0.79 0.02 0 Rainbow Lorikeet 0.89 0.01 0 Red Wattlebird 0.86 0.06 0 Red-browed Finch 0.93 0.11 0 Restless Flycatcher Scarlet Robin 1 0.84 0.85 0.006 Shy Heathwren 0.72 0.08 0 Southern Emu-wren 0.98 0.03 0 Spotted Pardalote 0.92 0.01 0 Striated Pardalote 0.77 0.16 0 Striated Thornbill 0.84 0.03 0 Superb Fairy-wren 0.84 0.02 0 Swamp Harrier 0.83 0.29 0 Tawny-crowned Honeyeater 0.71 0.04 0 Tree Martin 0.74 0.02 0 Wedge-tailed Eagle 0.91 0.04 0 Welcome Swallow 0.81 0.03 0 White-eared Honeyeater 0.86 0.02 0 White-naped Honeyeater 1 0.33 0 0.89 0.05 0 Willie Wagtail + 0 0 60 Table A2.3. West and South Coast Landscape Fan-tailed Cuckoo Golden Whistler Grey Shrike-thrush Rainbow Lorikeet Red Wattlebird Southern Boobook Australasian Pipit Change 0.42 0.57 0.65 0.69 0.61 0.5 0.5 Bassian Thrush Brush Bronzewing 0.89 0.53 Common Bronzewing 0.56 Crimson Rosella Dusky Woodswallow Fairy Martin 0.82 0.83 0.57 Species slope r2 #analyses - 0.42 0.53 0.43 0.28 0.41 0.42 0.38 2 2 2 2 2 2 1 - 0.55 0.29 1 1 0.37 1 0.34 0.73 0.09 1 1 1 0.6 0.27 1 Grey Currawong 0.68 0.0004 1 Grey Fantail Horsfield's Bronze-cuckoo 0.78 0.27 0.37 0.4 1 1 Little Wattlebird 0.68 0.09 1 Nankeen Kestrel Peregrine Falcon 0.76 0.6 0.3 0.23 1 1 Purple-crowned Lorikeet 0.68 0.2 1 Purple-gaped Honeyeater 0.64 0.2 1 Rock Parrot 0.57 0.48 1 Silvereye Striated Thornbill 0.71 0.69 - 0.25 0.08 1 1 Wedge-tailed Eagle Welcome Swallow Western Whipbird White-browed Scrubwren 0.84 0.75 0.94 0.69 - 0.25 0.44 0.93 0.2 1 1 1 1 White-fronted Chat 0.27 0.39 1 Yellow-tailed Black-Cockatoo 0.69 0.18 1 Australian Magpie 0.85 0.005 0 Australian Raven 0.8 0.04 0 Beautiful Firetail 0.83 0.12 0 Black-faced Cuckoo-shrike 0.76 0.02 0 Brown Thornbill 0.72 0.18 0 Brown-headed Honeyeater 0.73 0.03 0 Bush Stone-curlew 0.87 0.29 0 Galah - - - 61 Species Crescent Honeyeater Change 0.82 slope r2 #analyses 0.02 0 Eastern Spinebill 0.83 0.0008 0 Little Raven 0.88 0.12 0 Magpie-lark 0.88 0.36 0 New Holland Honeyeater 0.71 0.07 0 0.9 0.03 0 Scarlet Robin 0.73 0.02 0 Shy Heathwren 0.71 0.01 0 1 0.04 0 Spotted Pardalote 0.74 0.09 0 Striated Pardalote 0.76 0.07 0 Superb Fairy-wren 0.75 0.03 0 Tawny-crowned Honeyeater 0.71 0.09 0 Tree Martin 0.73 0.09 0 White-eared Honeyeater 0.75 0.07 0 Willie Wagtail 0.86 0.02 0 Red-browed Finch Southern Emu-wren 62
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