1. Introduction
Climate change is impacting ecosystems around the world. Global mean land surface temperatures were 1.34 to 1.83°C higher in 2011-2020 than in 1850-1900 [
1]. A common component of climate change is increased extreme climate events, such as heatwaves and droughts [
2]. Such events can drive rapid change in vegetation and wildlife populations [
3,
4]. Declining productivity is a common response of vegetation to climate extremes, including drought, and this may negatively impact higher trophic levels [
5,
6]. For example, declining forage productivity can reduce habitat suitability for browsing herbivores via reduced nutrient, energy, and water availability, and result in warmer microclimates from a loss of vegetation cover [
7,
8]. Analysing this process spatially can indicate the distribution of potentially suitable habitat in future environments (i.e. refugia).
Remotely-sensed measures of ecosystem function, such as the Normalised Difference Vegetation Index (NDVI), can reveal changes to vegetation suitability for animals during extreme conditions provided data are available across time and at multiple spatial scales [
9,
10,
11]. The NDVI is a measure of vegetation productivity and green biomass, it is the difference between red and near-infrared wavelengths in radiation reflected from vegetation (chlorophyll absorbance & mesophyll reflectance, respectively). NDVI is highly correlated with several vegetation characteristics including fraction of absorbed photosynthetically-active radiation, foliar nitrogen and chlorophyll, net primary production, and evapotranspiration [
12,
13]. Multiple studies have used NDVI to characterise the magnitude of drought impacts on vegetation condition and productivity [
14,
15]. The index also has been used in numerous studies of plant-animal interactions, including as a measure of forage phenology in assessing the trophic effects of climate on body mass of red deer (
Cervus elaphus, [
16]), and to test optimal foraging and species-energy theory by analysing vegetation productivity in relation to species diversity, abundance and landscape use for a review see [
12].
Species distributions have shifted under anthropogenic climate change partly because of changes in habitat suitability, including for specialist herbivores [
17,
18,
19]. In this study, we used the NDVI to identify productivity thresholds for the occurrence of a specialist arboreal folivore, the koala (
Phascolarctos cinereus), throughout most of its distribution across eastern Australia. Using a long-term, continental-scale koala observation dataset, vegetation mapping, and time-series NDVI from Landsat sensors, we tested the hypothesis (H
1) that locations where koalas had been observed would exhibit higher NDVI values than a random, representative sample from the same vegetation group (i.e. woodlands, open forests and tall open forests). We then obtained the minimum NDVI values at which koalas were observed for each vegetation group. We used these values to represent a NDVI threshold for koala occurrence and investigated how severe drought affected the distribution of potential koala habitat based on the thresholds and changes with drought to landscape NDVI, within vegetation groups. Potential habitat in this context means vegetation groups in which koalas are commonly found.
We tested the hypothesis that drought would reduce the area of potential habitat that is above the NDVI threshold for koalas (H2). We also investigated whether this suitable vegetation was significantly closer to perennial water than unsuitable vegetation (H3), before and during the drought. In this study, we use the term suitable or unsuitable vegetation to describe vegetation that is above or below koala NDVI thresholds in vegetation groups commonly associated with koala habitat. Whether koalas are present in a particular area can depend on several other factors that were beyond the scope of this study. By quantifying the responses both of our target species (the koala) and of the quality of its potential habitat via fluctuations in NDVI, we present a simple, powerful analysis capturing the impact of climate stress on vegetation and vegetation-dependant fauna which can be considered alongside other factors that influence habitat suitability.
2. Materials and Methods
Study Area
The study area encompasses most of the koala’s distribution, primarily across the Australian states of Queensland, New South Wales, Victoria, and the Australian Capital Territory (
Figure 1). Tree cover in the area is predominately temperate evergreen broadleaf forests and woodlands, dominated by trees from the genus
Eucalyptus, Angophora and
Corymbia. Maximum mean annual temperatures (MAT) across the range have increased by 0.4-0.6°C per decade since 1970 [
20], and the median MAT is 18.8°C, increasing to above 20°C in the north-west [
21].
Study Species
The koala (
Phascolarctos cinereus) is a specialist folivore that browses primarily on the foliage of eucalypt trees, from which they also obtain most of their water. Koalas have a wide distribution across the eastern states of Australia where they are associated with forests and woodlands dominated by evergreen trees in the genus
Eucalyptus. Koalas have relatively high site fidelity, with sometimes overlapping home ranges that can vary widely in size, from less than 2 ha to over 100 ha in more open woodland environments [
22]. Once common, large population declines, particularly in Queensland and New South Wales, have resulted in koalas in those states being recently listed as endangered [
17,
23,
24,
25]. Direct and indirect effects of heatwaves and droughts associated with climate change have contributed to koala mortality and population declines [
10,
26,
27,
28], along with habitat clearing and degradation [
17,
29,
30]. Population decreases in semi-arid bioregions tend to align with drought periods [
17,
24,
31].
NDVI of Koala Observations Compared to Landscapes
We obtained koala observations from the Species Profile and Threats Database (SPRAT) for the period 1995-2009 to identify koala observations for which NDVI and vegetation group could be determined [
32] (
Table 1). The observations extended throughout the koala range in eastern Australian states and territories (NSW, Queensland and ACT) where koalas are listed in legislation as endangered. For the state of Victoria, where the koala is not listed, we obtained observations from the Victorian Biodiversity Atlas [
33]. The koala records had been compiled from many sources, including structured scientific and community surveys, and opportunistic sightings. We filtered for locational uncertainty of 100m or less and removed all unlikely (e.g. aquatic) or duplicate observations. This included removing records that were not associated with a precise date, to allow us to obtain NDVI values associated with each koala observation.
Table 1.
Data sources of koala records and landscape layers used in this study.
Table 1.
Data sources of koala records and landscape layers used in this study.
Source |
Variable |
Study Use |
Native Resolution |
Source Website |
Landsat satellite data cube hosted by Geoscience Aus. & NCI |
Normalised Difference Vegetation Index [NDVI] (from corrected reflectance rasters) |
Landscape vegetation condition and koala site vegetation condition |
25 m x 25 m |
http://pid.geoscience.gov.au/dataset/ga/144643 |
Species Profile and Threats Database (SPRAT) |
Koala presence |
Identify associated vegetation condition |
Vector points |
https://www.environment.gov.au/sprat |
National Vegetation Information System (NVIS v6.0) |
Vegetation group (based on NVIS major vegetation groups [MVG]) raster |
Assign NDVI and koala presence observations into vegetation groups |
100 m x100 m |
https://www.environment.gov.au/fed |
Surface Hydrology Lines (Regional) |
Perennial water courses and bodies |
Calculate distance of observations and potential habitat to water |
Vector lines and polygons |
http://pid.geoscience.gov.au/dataset/ga/83107 |
Koala observation site NDVI
We extracted NDVI measurements at the filtered koala observation sites to derive suitability thresholds for koala associated vegetation groups. We used reflectance data from multispectral Landsat satellites 5 and 7 from 1995-2009 (25 m ground resolution,
Table 1), which have equivalent spectral bands (i.e. red: 0.6-0.7 µm & 0.63-0.69 µm, and near-infrared [NIR]: 0.7-0.8 µm & 0.77-0.90 µm, respectively). Before 1999, Landsat 5 operated and the image timeseries had a 16-day frequency; for the remainder, both satellites 5 and 7 were operating and two images were acquired, and used, in each 16-day interval. NDVI was calculated following [
34]:
We constrained the data to 0.2 ≤ NDVI ≤ 0.86, as values below this window are typically not considered vegetation and those above may be affected by saturation of NDVI for the vegetation groups and spatial resolution of our data [
35,
36]. These data were extracted from Landsat scenes stored in a timeseries datacube hosted by Digital Earth Australia (DEA), which is processed with a nadir-corrected bidirectional reflectance distribution function [
37]. We masked poor-quality pixels including cloud using the ‘Fmask’ function built-in to the DEA platform [
38]. We then collected the Landsat NDVI value nearest in time to each koala observation, within a maximum of 14-days either side of the observation. We used an arithmetic mean NDVI value from a 3x3 window of pixels around the location to get a measure more representative of the habitat and reduce the effect of NDVI outliers.
Vegetation group assignment
We assigned the retained koala observations to vegetation groups based on the Major Vegetation Groups dataset (MVG,
Table 1) and analysed each vegetation group separately, because differences in NDVI across these groups driven by differences in vegetation composition and biomass limits comparisons between them [
12]. To do this we used Python software packages xarray [
39], and geopandas [
40]. The MVG data are based on structural and floristic information including dominant genus, growth form, height, and cover [
41]. It has been assembled from data collected at various on-ground dates; here we used the most recent combined version (version 6.0, [
41]). We excluded records from MVGs including less than 500 koala observations, to maintain large sample sizes within groups and because less koala habitat occurs in these groups.
Comparing koala observation NDVI with mean NDVI for each vegetation group
To test whether the NDVI of koala sites differed from the mean NDVI for that vegetation group, we used generalised linear mixed modelling (GLMM). As a response variable, we used presence of koalas and drew an equally sized random subset of background points from the NDVI data source for respective vegetation groups in the landscape (woodland, open forest, and tall open forest, n=1,500 each). We paired these background landscape NDVI values to the times of koala observations, which were from anytime in 1995-2009, to control for temporal variation in NDVI. We modelled a binary response, either observation or background-landscape, with NDVI as a predictor in separate binomial GLMMs for each vegetation group. To account for spatial autocorrelation of NDVI, we included an exponential covariance term based on the spatial coordinates of observations. We then tested the model residuals for spatial autocorrelation. To fit these GLMMs, we used the software packages glmmTMB [
42] and DHARMa [
43] in the R environment [
44].
NDVI Thresholds for Suitable Vegetation
We determined minimum thresholds of NDVI associated with koala observations by analysing the empirical cumulative distribution functions for all observations (1995-2009), using the statsmodel Python package [
45]. The NDVI value, for each vegetation group, with an estimated probability equal to 5%.
is the NDVI below which koala occurrence is not likely and was selected as the threshold above which vegetation productivity is sufficient to support koalas.
Landscape NDVI in drought and non-drought periods
From 2001 to 2009, Australia experienced one of its worst droughts on record, dubbed the millennium drought [
46] which had many harmful ecological impacts [
47]. The rainfall anomaly was 12-13% below the mean of the previous century. We obtained landscape NDVI data for this period also from the DEA [
37]. We used a subset of the Landsat NDVI imagery across the koala range from 2005-2009, which was the latter part of the millennium drought, when cumulative effects would have been greatest. We reduced this timeseries to the 5
th percentile value for each pixel to produce an image of minimal vegetation productivity without capturing low outliers (e.g. unmasked cloud). We repeated this process for 1995-1999 to make comparisons with drought.
Vegetation group assignment
To limit the analyses to vegetation groups most frequently associated with koala observations in the landscape, we combined the NVIS-derived groups as described previously with the minimum NDVI images. Rasters of each vegetation group and the NDVI images were aligned spatially, to account for the different resolutions and projections. Taking a Boolean mask of each vegetation group we multiplied it by the NDVI, resulting in a landscape NDVI layer with resolution of the Landsat input, divided into vegetation groups. This process was repeated for the two time periods, using a raster calculator [
48].
Applying koala NDVI thresholds across the landscape
We applied the suitability thresholds for each vegetation group to the drought and non-drought NDVI images using a raster calculator. The result was a set of NDVI rasters of suitable vegetation, for pre- and drought periods which excluded potential habitat vegetation deemed unsuitable to support koalas because the NDVI value of that vegetation was below the relevant vegetation-group threshold. We then computed difference layers by subtracting pre-drought from drought to reveal how much potential habitat shifted from suitable pre-drought to unsuitable in drought.
Proximity of Suitable Vegetation to Water
To understand the spatial proximity of vegetation above the NDVI threshold for koalas in relation to distance to perennial surface water, we combined the suitability maps with surface hydrology data [
49]. These data describe perennial watercourses and water bodies for the continent (
Table 1). We converted the vectors to a raster at the spatial resolution of the NDVI data, then created a proximity raster of distance of each pixel to the target (water) pixels, using the
Rasterize function (GDAL, [
50]). With the same software, we multiplied the proximity raster by the mask of vegetation suitability rasters for each of two time periods and the two suitability groups, producing rasters of distance (km) to suitable and unsuitable vegetation pixels. To test whether the distance to perennial water of suitable pixels differed from the average distance to water for each vegetation group, we used generalised linear mixed modelling (GLMM). We used a subset of pixels from each vegetation group, which we randomly selected from across the landscape, made up of half suitable and half unsuitable (total n=4,500). The modelling approach was similar to that of koala site ~ NDVI (H
1), except the binomial response was pixels above or below NDVI thresholds and the predictor, distance to water, was logarithmically transformed because of its Euclidean structure. We used this same model structure to test if koala observations were closer to water than random sites, with the response variable being binary: koala site or random location. Here, we used the same coordinates as the subset of observations used in the methods for H
1.
3. Results
3.1. NDVI of Koala Observations Compared to Landscapes
The mean NDVI of observations and random landscape pixels differed significantly for all vegetation groups (all
p < 0.0001,
Figure 2,
Figure 3). Thus, koalas tended to be found in vegetation with greater-than-average productivity within each vegetation group, confirming our first hypothesis (H
1).
3.2. NDVI Thresholds for Suitable Vegetation
Figure 4 shows the minimum (5
th percentile) identified in the cumulative distributions of NDVI for koala observation pixels for each vegetation group (i.e., vegetation thresholds; woodlands = 0.393, open forests = 0.436, tall open forests = 0.549). Woodland followed by open forest, had thresholds lower than the tall open forests, reflecting the different productivity levels of each vegetation group.
Across the entire study area, the effect of drought was observed most strongly in the minimum NDVI rather than the mean NDVI; changes to the mean were small and not significant in all vegetation groups. The landscape NDVI minimum across vegetation groups declined significantly between pre- and late-drought periods (all
p < 0.01), due to declines in all vegetation groups across periods.
Figure 5 shows distributions in both periods for respective vegetation groups.
The total area of all three vegetation groups was 429,997 km
2. During the pre-drought period, 49% of this area remained above the koala NDVI threshold for all vegetation groups (
Table 2;
Figure 6). This means approximately half of potential koala habitat was not sufficiently productive to continuously support koalas (i.e. suitable vegetation). During the drought, we observed a 12% reduction in suitable vegetation area, across vegetation groups. This affirmed our second hypothesis, that NDVI decline in drought reduces the area of potential habitat for koalas (H
2).
Figure 7 shows an example of this reduction within a landscape, where of 606 ha of suitable vegetation prior to drought, 16.8% declined below thresholds in drought (102 ha).
3.3. Proximity of Suitable Vegetation to Water
The mean distance to water from koala observations was 5 km for woodland observations (SD=7.9 km), 1.8 km for open forest (SD=2.4 km), and 1.3 km for tall open forest (SD=1.6 km). The maximum distances at which koalas were observed from perennial water were 51.4 km, 32.2 km, and 21.1 km in the three vegetation groups respectively. Koala observations were significantly closer to water in open forests than random points taken from the same landscape type (p < 0.01), but this pattern was not found in woodlands or tall open forests (p = 0.93, and p = 0.3, respectively).
We found that suitable and unsuitable vegetation could occur 40 km or more from water, in all vegetation groups. However, there was a significant effect of distance to water on suitability (i.e. vegetation above or below NDVI minimum threshold) in tall open forest (p < 0.001) and open forests (p = 0.04) but not in woodlands (p = 0.8).
4. Discussion
Climate change is challenging our abilities to understand rapidly changing current and future habitat suitability and species distributions, creating a need for methods to monitor such changes and identify potential refugia, thus allowing better conservation for wildlife and their habitat [
51]. For the first time, we identified thresholds of the minimum NDVI associated with the presence of a specialist folivore, the koala, allowing us to assess the extent of potential habitat before and during a major drought. This study extends previous work focusing on local abundance of folivores with NDVI (e.g., [
52]) by considering the relationship between NDVI and ecological niche at broader spatial scales. Recognising a basic relationship with available energy, we did not aim to build a model of the whole NDVI-animal relationship, as has been done elsewhere (e.g. NDVI-abundance, [
53]), instead we identified bounds of that relationship and extrapolated these limits in space.
NDVI of Koala Observations Compared to Landscapes
In all three vegetation groups, we found that koalas were more likely to be observed in areas of the landscape that had higher NDVI values than the average for that vegetation group. These findings are consistent with earlier, regional koala occupancy modelling, based on acoustic detection, that showed landscape NDVI had a significant, positive effect even within a relatively mesic region, the North Coast and Northern Tablelands of NSW [
54]. Similarly, [
52] found that locations where another specialist eucalypt folivore, the greater glider (
Petauroides volans), was observed had significantly higher NDVI on average than areas where they were not observed. That study also showed a positive relationship between abundance and NDVI.
Several studies have suggested that NDVI may correlate to available energy from forage [
52,
55,
56] and preferentially foraging in patches of higher energy would allow animals to increase energy intake while reducing expenditure, although the ability to metabolise the forage in these patches is also important [
57,
58]. NDVI is linked to forage quality and available energy in several ways. NDVI is a measure of photosynthetic capacity, the system comprising pigments and proteins, of which the latter is a limiting nutrient for koalas and many other folivores [
59,
60]. Furthermore, NDVI is highly correlated with net primary productivity and canopy biomass that makeup forage energy [
12,
13,
61]. Declines in productivity and biomass will lead to lower NDVI values and can also reflect less available energy for folivores [
62]. Additionally, lower canopy biomass means less shade and evapotranspiration, resulting in hotter micro-climates that can reduce habitat suitability [
63].
Since our data were sourced from koala observations that included opportunistic sightings, rather than a random sample across the entire range, there may be bias in observations towards areas with more observers, which may also be more productive in terms of NDVI [
64]. We expect this effect to be less pronounced in the vegetation groups that are more common along the coast (e.g., tall open forest and open forest) where human populations are most concentrated and therefore tend to coexist with koalas. This potential bias could not be entirely avoided, but the inclusion of data from scientific surveys and research sites in more remote areas, as well as the consistent pattern across all forest groups and with earlier studies of folivore occurrence and NDVI, provide additional support to our findings.
NDVI Thresholds for Suitable Vegetation
The minimum NDVI thresholds for koala observations differed across vegetation groups, which is in keeping with the differing distributions of NDVI in those groups. However, in all vegetation groups, the minimum NDVI values associated with koala observations were always higher than the minimum value possible for that landscape group. Accordingly, we also found that a sizable area of all three vegetation groups fell below the NDVI minimum, even prior to drought. The area of potential habitat above the NDVI thresholds associated with koala occurrence declined by 12% during the millennium drought, supporting the notion that during drought, koala habitat contracts in spatial extent. The largest portion of potential habitat that fell below thresholds was in woodlands, but in all vegetation groups there was contraction.
The western, inland extent of the koala’s range is typically comprised of woodlands, with intersecting riparian areas where koalas may occur in higher densities relative to other areas [
65]. Water is thought to be a limiting factor for both tree and koala abundance in such regions, and previous studies have identified relationships between foliar NDVI and environmentally available water in these western woodlands, particularly in riparian areas predominated by the locally preferred koala browse species,
Eucalyptus camaldulensis [
17,
86]. Notably, these riparian forests, embedded in the broader woodland landscape, were often classified as tall open forests, due to their structural profile that differed from the surrounding woodland landscape. This likely contributed to the overall proportion of tall open forests that fell below the NDVI threshold during the drought period, and the significant relationship between distance to perennial water and tall open forest above the NDVI threshold. Although these riparian forests tend to be phreatophytic, maintaining hydration longer during dry conditions, other studies have found that the NDVI values associated with
E. camaldulensis dominated riparian forests can decline substantially during prolonged drought conditions [
86]. Other types of tall open forests in our study typically occur closer to the coast and experience higher rainfall, so water is less likely to be a limiting factor on vegetation productivity and NDVI.
In times of drought, koalas may be critically stressed in landscapes that fall below the vegetation productivity threshold associated with their occurrence. Reduced forage water supply can lead to heat-induced water stress in koalas if free water is not available [
51]. Dehydration of koalas has been documented within population crashes during drought [
31]. Koalas in refugial areas that remain above the threshold of vegetation productivity during times of drought or extreme heat are more likely to survive [
31]. The periodic loss of habitat suitability due to drought impacts is particularly concerning for species like the koala and other arboreal folivores that have less capacity for migration [
65] and due to forage specialisation, cannot adapt by expanding their dietary breadth [
66]. Such contractions in suitable vegetation may also impact populations by way of habitat fragmentation [
67].
Using the relationship between NDVI minimum thresholds and change in vegetation conditions from pre-drought to drought periods, we have revealed the extent of potential koala habitat contraction during the millenium drought. In a future of increasingly severe droughts [
68], both the extent of habitat contraction and the duration of time in which habitat drops below koala NDVI thresholds could increase. Our analysis considered the extant vegetation, by using reflectance data and forest-type mapping, unlike many distribution or population models [
51,
69,
70]. [
51] estimated the extent and distribution of suitability based on a biophysical, spatial model which does recognise the importance of changes to koala habitat quality. Like the results of that study, we found contractions in potential koala habitat during drought occurred mainly in the inland parts of the koala’s distribution (
Figure 6). Such contraction of populations to refugia during drought has been documented [
9,
31]; however, the contraction of potential habitat in drought has not, to our knowledge, been revealed before this study.
Our study overcomes some of the limitations of predicting species’ habitat distribution based on forecasts of climate averages. Such approaches do not incorporate climate extremes well, nor the trophic interactions caused by those extremes [
71]. Whereas NDVI integrates the many and varied effects of realised ecological drought across landscape vegetation. The drought studied here did contain spatial variability, including substantial effects in the south of Queensland [
47]. Our inclusion of the less affected northern, tropical regions may have reduced the observed drought effect for vegetation groups also occurring there.
Notably, a sizable portion of the vegetation in the Victorian central and eastern highlands that fell below NDVI thresholds during drought was directly affected by the Black Summer Fires of 2009 (
Figure 6, see also [
72]. The NDVI of burnt forest is typically lower than the same area before fire, particularly if canopy scorch occurs [
73]. The millennium drought conditions contributed to the intensity of the 2009 fires [
74,
75] and in the short-term, fire can reduce koala populations and habitat quality due to forage loss [
76]. Some vegetation may recover productivity quickly via epicormic regrowth, providing potential forage for koalas [
77], although this recovery was slowed in some areas by ongoing drought [
78]. Other possible drivers of NDVI minima in some cases, could include land clearing [
30] and tree dieback [
79].
Proximity of Suitable Vegetation to Water
On average, the distance between suitable vegetation and perennial water was 7km, which is greater than the width of even the largest koala home ranges. However, we did find that unsuitable vegetation tended to occur significantly farther from water bodies than suitable vegetation for some vegetation groups. During drought, the distance to water was slightly less for suitable vegetation than before drought, but still 6.4 km on average. Our analysis of the suitability maps does not suggest that access to free-standing water is a habitat requirement for most koalas; however, it’s possible that koalas in the western part of their range may rely on it more often [
17].
[
65] found that presence of free-standing water influenced the home range size of koalas in western Queensland, and koalas in arid sites spent more time in riparian parts of their habitat compared to those in relatively mesic sites (~80% compared to ~40%). Although koalas are thought to obtain most of their water from leaves, they will also drink free water with increasing frequency as temperatures increase [
80]. Sources of free water may be available in addition to those used in this study, including during some stages of drought. These sources include ephemeral creeks, waterholes, farm dams and bores, although koalas survived prior to the construction of the latter two sources. In addition, it is likely that trees in some areas also access water from underground sources that were not considered in this study but could contribute to NDVI and vegetation suitability. More research is needed to understand how water, both in the koala’s environment and in their diet of leaves, contributes to habitat suitability and the distribution and resilience of koala populations.
Further Applications, in Other Systems and in Management
Having confirmed the existence of vegetation-specific thresholds for koalas and mapped potential koala habitat during drought, it would be valuable to expand the study temporally. The full Landsat time-series could be utilised to estimate length of periods of suitability. This may reveal areas that are resistant to drought and only shift during the most extreme conditions (i.e., highly skewed temporal distributions). Perhaps more valuably, the Landsat data might also provide insight into the link between koala presence, recovery from drought and its interval, including interactions with temperature which may increase the speed of drought onset [
81].
Analyses of habitat productivity thresholds, like that here, need not be limited to specialist folivores, such as the koala. Other possible systems of study include herbivores that are limited by forage quality in environments that experience extreme periods, particularly those systems with vegetation sensitive to climate change. However, stressors other than climate extremes could also be studied using our approach, provided the stressor affects vegetation NDVI (e.g., seasonal insect outbreaks). Examples of other possible study systems include savanna grass specialists of El-Niño affected South Africa [
82], or environments in China where vegetation loss in drought is substantial [
83]. Such systems could feature generalist herbivores because the NDVI is responsive to productivity in most plants [
34,
84]; however, analyses may be more complicated if diets are diverse.
5. Conclusions
This section is not mandatory but can be added to the manuscript if the discussion is unusually long or complex.
Our results consider one measure of habitat quality based on vegetation productivity, but the results may be useful to environmental managers precisely because of that simplicity. This is because NDVI integrates many environmental effects on vegetation and indicates extant vegetation. Models that include more parameters and complex influences can be harder to comprehend for management purposes [
85]. The maps produced in this study provide an outline of areas of potential koala habitat that could be conserved through future climatic extremes.
Author Contributions
Conceptualization, I.K., K.Y., C.M. and B.M.; methodology, C.M. and I.K.; software, C.M. and I.K.; formal analysis, I.K., C.M., M.E. and K.Y.; investigation, I.K., C.M., M.E., K.Y. and B.M.; resources, C.M., K.Y., B.M.; data curation, C.M., I.K.; writing—original draft preparation, I.K.; writing—review and editing, I.K., C.M., J.E., K.Y. and B.M.; visualization, I.K., J.E.; supervision, K.Y., B.M.; project administration, I.K., K.Y., B.M.; funding acquisition, K.Y., B.M. All authors have read and agreed to the published version of the manuscript.
Funding
This research was funded by NSW Department of Climate Change, Energy, the Environment and Water (New South Wales, Australia), project number A13782.
Data Availability Statement
Conflicts of Interest
The authors declare no conflicts of interest.
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