Acknowledgements
AM would like to thank the CSIR- Research Associate program for support during preparation of the manuscript
and the state forest departments of Kerala, Karnataka, Tamil Nadu, Goa and Maharashtra for facilitating the
fieldwork. VSP, VT, SP, and AS contributed the data for the analysis presented here. We acknowledge the support of
the Director, ZSI, Kolkata and the Officer-in-Charge, ZSI, WRC, Pune.
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Abstract
Anthropogenic climate change is altering the environment at unprecedented rates with severe consequences for most
living organisms. As a result, species may extend, truncate, or shift their ranges in order to adapt to changing
conditions. Species Distribution Models (SDMs) provide a data driven approach to predict future distributions under
climate change and prioritize areas for conservation. Here, using a 10-year dataset with 4049 occurrence records of
frogs from eight families and 27 genera as well as 733 occurrences of lizards from two families and 11 genera across
the Western Ghats, we built SDMs to assess the changes in species distributions due to climate change. As expected,
the temperature gradient across elevation and seasonality gradient across latitude contribute most to the climatic
limits of species distributions. Latitudinal extents of most species were narrower in future predictions compared to
the present, but there was little shift in latitudinal positions. On the other hand, most species shifted their
distributions towards higher elevations, but the elevational range sizes remained the same. A total of 75 species of
frogs (55%) and 15 species of lizards (45%) lose more than half of the suitable area, with few exceptions in both
taxa that show an increase. In cases where a shift or increase in distribution was observed, the ability of the species
to access and survive in these areas remains uncertain due to discontinuous topography and the presence of sister
species. Overall, the frog and lizard fauna of the Western Ghats will be severely affected by climate change in the
future due to a loss in climatic suitability.
Keywords
species distribution, climate change, extinction risk, western ghats
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Introduction
Anthropogenic climate change is altering the environment at unprecedented rates with severe consequences for most
living organisms (Walther et al. 2002, Malcolm et al. 2006, Parmesan 2006). Changes in the environment can
potentially cause mismatches between species adaptations and environmental conditions. The response of species to
novel environmental conditions can change species distributions towards new potentially suitable areas. As a result,
species may extend, truncate, or shift their ranges (Shoo et al. 2006, Colwell et al. 2008, Colwell & Rangel 2010,
Warren & Chick 2013). Additionally, natural and anthropogenic barriers to dispersal can reduce opportunities for
species to track environmental changes, ultimately causing extinctions (Boulangeat et al. 2012, Schloss et al. 2012).
Therefore, understanding the impacts of climate change on species distributions has become a critical conservation
challenge.
As global temperatures rise, species ranges are expected to shift along latitudes and elevation in order to track the
suitable climates (Chen, Hill, Ohlemüller, et al. 2011, Jacobsen 2020). Overall, the outcome of changes in species
distributions due to climate change will be determined by the ability of a species to survive the changing
environment and disperse towards suitable areas (Lenoir & Svenning 2015). Observations of latitudinal shifts due to
climate change are largely from temperate rather than tropical latitudes (Sheldon 2019), including latitudinal shifts
in the distributions of birds (Zuckerberg et al. 2009, Brommer et al. 2012) and butterflies (Parmesan et al. 1999)
among other taxa (Hickling et al. 2006) . On the other hand, tropical species are expected to respond by adjusting
elevational distributions. This is because the latitudinal temperature gradient in the tropics is comparatively flatter
(Sheldon 2019) and much of the change in climate takes place along elevational gradients (Colwell et al. 2008). For
instance, frogs in the North Americas are expected to shift poleward, whereas those in the tropical South Americas
are expected to shift to higher elevations (Lawler et al. 2009, Blaustein et al. 2010). Comparison of current and past
distributions of trees (Feeley et al. 2011) and birds (Dejean et al. 2011, Forero-Medina, Terborgh, et al. 2011) on the
Andean Mountains show evidence of upward shifts in species distribution. Model predictions from other regions for
diverse taxa, including invertebrates (Chen, Hill, Shiu, et al. 2011), frogs (Forero-Medina, Joppa, et al. 2011),
lizards (Jiang et al. 2023), birds (Sekercioglu et al. 2008) and mammals (Moritz et al. 2008, Rowe & Terry 2014),
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also support shifts in distributions towards higher elevations. Further, on mountain regions that span large latitudinal
extents, such as the Andean Mountain range in South America, and the Western Ghats escarpment in India,
latitudinal extents of species can reduce due to extinctions from local elevational gradients.
This is particularly important for the species in the Western Ghats (WG) – a region of high endemism and of global
importance for conservation – due to the combined effects of seasonality gradients, and discontinuous topography of
the mountain range. The Western Ghats (WG) harbors rich biodiversity, including numerous endemic species, and
provide valuable ecosystem services (Das et al. 2006, Gunawardene et al. 2007). Climatic gradients across the
latitudinal and elevational extents of the mountain range are important determinants of species distribution and
community composition (Page & Shanker 2018, Bose et al. 2019, Jins et al. 2021). These gradients are likely to be
altered in the near future due to climate change (Kumar et al. 2006). In addition, natural barriers in the mountain
range and habitat loss in recent decades is likely to prevent species from colonizing suitable habitats, thus
amplifying the impacts of climate change (Subba et al. 2018). Therefore, understanding potential species
distributions and resulting community composition under climate change becomes crucial for biodiversity
conservation in the Western Ghats.
The Western Ghats escarpment harbours a large number of endemic radiations of amphibians and reptiles due to a
combination of isolation during the geological past, historical climatic fluctuations, and natural breaks in the
mountain range (Vijayakumar et al. 2016, Mallik et al. 2020). As a result, there are numerous species with narrow
geographic extents and environmental tolerances. Such species are particularly vulnerable to climate change as they
are more likely to experience environmental mismatches in the future. Further, geographic barriers can prevent them
from tracking suitable landscapes in the future, ultimately accelerating extinctions. Studies on climate change
impacts in the Western Ghats on species of conservation focus (Priti et al. 2016, Sony et al. 2018), agriculturally
important organisms (Sen, Gode, et al. 2016, Pramanik et al. 2021), and invertebrates (Sen, Shivaprakash, et al.
2016) suggest that the species distributions will be considerably altered. Still, what geographic areas, or which range
attributes are vulnerable remains unknown as assessments across taxa have not been carried out.
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We used a framework which uses geometric constraints in both latitudinal and elevational domains to make
predictions regarding changes in range size and position (Colwell et al 2008). According to this framework, range
sizes and range locations (midpoints) are related through geometric constraints, and reduction in suitable area due to
elevational range shifts should be dependent on the range location. Therefore, there should be an interaction between
current elevational extents and elevational midpoints. The total land area decreases towards higher elevations
globally, however at landscape scales the relation between area and elevation can be variable (Elsen & Tingley
2015). Within the Western Ghats, land area decreases with elevation above 500m which is 80% of the total area of
the escarpment. Therefore, we expect that the species shifting towards higher elevations should show decrease in
suitable area.
Here, we use predictions from Species Distribution models (SDM) with climate in the present and future as a proxy
for range extents of species to provide an assessment of the vulnerability of frog and lizard species to climate change
in the Western Ghats. Our primary questions include: (1) What is the extent of change in climatic suitability for
frogs and lizards in the Western Ghats? (2) How do attributes of species range such as latitudinal as well as
elevational extents and location (midpoints) change under future conditions? (3) What range attributes explain the
loss or gain in climatic suitability? (4) What consequences does this have for the frogs and lizards of the Western
Ghats?
Methods
Occurrence data
We used occurrence records from extensive surveys across the Western Ghats from 2009 to 2016 as presence
locations for the distribution models. The surveys covered topographic, elevational, latitudinal and rainfall gradients
and were designed to capture latitudinal as well as elevational extents of frog and lizard species within the Western
Ghats. The final dataset contains 4049 occurrence records across 203 species of frogs, and 733 occurrences across
59 species of lizards. Among these, we first removed any occurrences for the same species that were present on the
same raster cell of the predictor variables, and further only considered species with five or more occurrence records.
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These criteria resulted in a set of 133 species with 3226 total occurrence records of frogs, and 32 species with 558
total occurrence records of lizards. All known families of frogs except Nasikabatrachidae which is represented by a
single genus Nasikabatrachus, are present in the data, while lizard data comprised species in Agamidae and
Gekkonidae only (and do not include Varanidae, Scincidae and Lacertidae).
Environmental data
We initially considered 19 ‘bioclim’ variables available from Worldclim (Hijmans et al. 2005), and aridity index
(Trabucco & Zomer n.d.) as climatic predictors, and finally used a subset of the layers after accounting for
collinearity. The resolution of climatic variables is 30 arc sec (approximately 1 km2).
Topographic information was
included through elevation, slope, and aspect derived from the ASTER DEM at 30m resolution (Abrams et al.
2020). Topographic variables were re-sampled to match the coarser resolution of climate data. All the raster layers
were clipped to the geographic extent (binding box) of the Western Ghats. We checked for cross correlations among
all possible pairs of predictor variables using Pearson’s correlation coefficient and removed one predictor from the
pairs that had correlation coefficient equal to or more extreme than ±0.7. The final subset represents variation in
annual mean values as well as seasonality of temperature and precipitation (Table 1). We used these variables as
predictors for all the species as a reduced subset of environmental variables for mean and annual variability in
rainfall and temperature is recommended for modeling distributions of large numbers of species with limited
ecological information (Low et. al. 2021).
Distribution modeling
We predicted geographic distributions of species based on climatic suitability using the MAXENT algorithm
(Philips et. al. 2006 ). As it is nearly impossible to infer true absences from survey records alone, we used the
species occurrence records as presence only data. The MAXENT algorithm contrasts distribution of environmental
variables at occurrence locations against environmental conditions in the entire region to generate predictions of
suitability. The observed distributions can be potentially biased due to unequal or incomplete sampling. While the
sampling effort was kept as comparable as possible across the latitudinal extents, inherent differences in habitat
availability and geography of the Western Ghats result in greater number of occurrence records towards lower
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latitudes. To account for this difference, we generated a bias layer which is an inverse distance weighted density
kernel, based on pairwise distances between occurrence points, using the command ‘kde2d’ in the package ‘MASS
v7.3’. The resolution and extent of the bias file was set to match the predictor variables. From the bias raster, 10,000
cell centroids were randomly sampled weighted by the value for each cell. Environment represented by these points
represents any geographic bias that may be present in the samples. These points were used as biased background
locations in MAXENT. We constructed separate bias layers for the different families of frogs and lizards.
We compare several maxent models with different combinations of feature classes, and regularization parameters to
select an optimum model by running the maxent algorithm through the R package ENMEval v2.0 ( ). The package
compares models with different combinations of feature classes, and regularization parameters, and estimates model
evaluation statistics. We used linear, quadratic, and hinge feature classes, and their combinations, as
linear+quadratic, linear+hinge,quadratic+hinge, and linear+quadratic+hinge, with a range of regularization
parameters from 0.5 to 5 at an interval of 0.5. Model cross validation was done using the Spatial block method with
default parameters for species with more than 10 occurrences and with Jackknife method for species with 10 or
fewer occurrences. Final model among the candidate models was selected based on sequential criteria of (1)
Training Area Under Curve >0.6 (2) minimum difference between training and testing AUC (3) minimum number of
coefficients (4) maximum value for regularization parameter (5) minimum number of feature classes. The AUC
(Area under receiver operator Curve) was used to evaluate model performance. AUC is analogous to ranked
correlation of predicted probability between presence and absence points. High correlation suggests the model can
effectively distinguish between potentially suitable areas from the background. All continuous predictions were
converted to binary (suitable/unsuitable) using the ‘Maximum sum of sensitivity and specificity’ threshold criterion
(Liu et al. 2005)
In addition, we also built models with an unbiased background using the same predictors and model parameters. We
visually examined the model predictions with and without bias. Accounting for bias appeared to have minimal
apparent effect on model predictions. However, for a small number of species, typically when the occurrence points
did not coincide with occurrence density of the family, predictions with a biased background extended far beyond
the latitudinal extents of occurrence records. Potential overpredictions were confirmed by consulting taxon experts
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who had participated in the survey effort to generate the occurrence data and have extensive taxonomic and
ecological knowledge of these groups. Following this consultation, predictions with unbiased background points
were used for some species (Supplementary data). In addition, we modeled distributions using Ensemble models
implemented in using R package biomod2 v3.4 visual inspections by experts suggested that these models performed
at best as well as MAXENT. Hence, we used only MAXENT for all predictions as it uses a single algorithm and is
easier to interpret.
The distribution models were projected to future climatic scenarios of SSP1-2.6, and SSP5-8.5 for the period
2061-2080. For selecting the climate models that will be used for future projection, we identified the most
pessimistic and optimistic conditions for the Western Ghats, by comparing trends in the projected temperature values
across the Western Ghats for all models available in the ‘Worldclim’ repository and ranked the models based on
predicted increase in temperature.We used three models with least projected increase in temperature for representing
the optimistic SSP1-2.6 scenario and three models with the most increase in temperature for representing the
pessimistic SSP5-8.5 scenario (See supplementary-1 for details) . We predicted the species distributions using the
three selected models in each scenario and used the mean of the predictions as the predicted distribution of the
species under each scenario.
Identifying predictions beyond biogeographic limits
The Western Ghats show marked climatic changes which generate a gradient of increasing seasonality towards
higher latitudes. These changes very likely limit species distributions in the region and in turn contribute to the
model predictions. In addition, the species distributions are limited by the discontinuity in the mountain range, such
that species are unable to access suitable climates separated across valleys. Due to evolutionary processes,
phylogenetically and ecologically related species may occupy similar environmental conditions on either side of
such barriers. For a larger proportion of frogs and lizards in the WG, sister species are distributed across topographic
barriers, likely a consequence of allopatric speciation events; these sister species are often morphologically similar
and occupy similar habitats (Vijayakumar et al. 2016, Robin et al. 2017, Mallik et al. 2020)
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However, the distribution models that are predicting climatic suitability do not directly account for these processes
and should predict suitability in areas that are either inaccessible to the species or areas that overlap the distributions
of sister species. This can result in overprediction of geographic distribution. Thus, to reduce overpredictions in
areas that are disconnected due to geographic features in the mountain range, we identified the subset of the
predicted distribution for every species that is most likely accessible to the species, using a combination of criteria
based on the known distribution, elevational extents, and elevation of the discontinuous contour.
We used information on the known distributions of phylogenetically related species of bush frogs (Rhacophoridae),
and torrent frogs (Nyctibatrachidae) to identify 17 massifs that are most likely to be dispersal barriers for frogs in the
Western Ghats. We then mapped the lowest contours that form discontinuous elevations between these massifs. We
considered all massifs within latitudinal limits of the observed distribution as potentially accessible areas. Then, we
identified suitable areas predicted in MAXENT that were present within these limits. Further, when sufficient
phylogenetic data was available, we confirmed the overpredictions using occurrences of phylogenetically related
species. The resulting predictions combine the effects of climatic constraints as well as biogeographic processes in
the Western Ghats and provide a more nuanced approach towards predicting habitat/climatic suitability in the
present or future. We report the suitable areas both within and across barriers for each species.
Identification of high diversity areas
Following Srinivasulu et. al. (2021), we mapped areas containing high diversity within the Western Ghats by
calculating the mean of the binary prediction for all species and rescaling the resulting raster from 0 to 1. Values of
0.5 or higher represent areas that have at least half the species compared to the maximum species richness.
Latitudinal and elevational extents of species
The latitudinal extent of the entire predicted distribution is an overestimation of the species actual latitudinal extents
in most cases. This is because small numbers of disconnected pixels may be predicted much beyond the extents
where a majority of the suitability is predicted. To reduce potential overpredictions, we excluded 5% of the area
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towards the northernmost and southernmost extents and the remaining 90% of the prediction was considered for
estimating latitudinal extents of each species. To obtain these estimates, we first divided the WG into 0.80 latitudinal
zones, and calculated the fraction of total predicted distribution within each latitudinal zone. The northern and
southern extreme latitudes that contained 90% of the predicted area were used as latitudinal extent of the species.
We estimated the elevational extents of species within each 0.80 degree latitudinal zone separately in the same
manner by using 200m elevation zones, such that each species had separate elevational extents in each latitudinal
zone. Further, we estimated elevational midpoints for each species as the mean of midpoints on all massifs weighted
by the suitable area for the species in the massif. We compared the latitudinal and elevational extents of species in
present and future predictions and confirmed the patterns using linear models.
Predictors of changes in suitable area under climate change
Species that occur across small geographic extents or are not adapted to withstand environmental variability are
more likely to go extinct due to climate change. We tested this using the latitudinal and elevational extents and
midpoints under current conditions and the decrease in suitability in future predictions. We tested if there is any
difference between the range attributes i.e midpoints and extents of species that show near complete loss of suitable
area in the future predictions and the entire species pool. For this, we considered species for which predicted area in
future is <1% of the current prediction. We obtained the distributions of current latitudinal/elevational extents and
midpoints for these species and compared these with the regional species pool. Standardized Effect Sizes (SES)
were calculated with 1000 bootstrap randomizations.
We also used linear regression models to test the relationship between change in area and attributes of current as
well as future predicted range extents; we used current latitudinal and elevational extents and midpoints along with
difference in the midpoints between present and future as predictors for the regression models. To test these
predictions, we used a linear regression model with all the possible predictors and simplified it based on AICc.
Further, for the frog data, we demonstrate the effects of difference in elevational midpoints and the interaction term
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by reporting change in AICc and R2. In the case of lizards, as there are only 32 species in the data, we only used
predictors relating to elevational ranges.
Results
Based on the data availability criteria, 133 species of frogs that had at least five occurrence records each located on
separate raster cells were selected for distribution modeling. The AUC values of distribution models ranged
between 0.6 and 0.99. However, 80% of the species had AUC values greater than 0.8. For lizards, 32 species were
used for distribution modeling. The AUC values ranged 0.62 and 0.99. Mean annual temperature and dry period
precipitation had the highest percentage contribution for most species (38 species of frogs, 10 species of lizards)
followed by precipitation seasonality ( 24 species of frogs, and 6 species of lizards).
A large proportion of species (92 out of 133 species) were recorded from up to four massifs out of the 16. Only two
species - Duttaphrynus melanostictus and Pedostibes tuberculosus were distributed across most of the massifs (14).
There are 33 species, mostly from the families Rhacophoridae and Nyctibatrachidae, that have occurrences on a
single massif. All species of lizards except for Agasthyagama bedommei occurred on more than one massif and for
7 species, 70% of the predicted area was on disconnected massifs.
For several species the suitable area identified as beyond elevational barriers, was across the Palaghat or Shencottah
gap, which are elevational barriers in the escarpment that separate allopatric species of several taxa. In other cases a
large proportion of area of the predicted distribution overlapped with a phylogenetically related sister species (eg
Nyctibatrachus sanctipalustris and Nyctibatrachus karnatakensis; Indosylvirana intermediatus and Indosylvirana
caesari).
Predictions for future climates
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Suitable area predicted by distribution models decreased for most species (Table 2; Figure 1). At least 19 species of
frogs may potentially go extinct as suitable areas in future are less than 1% of the current predictions. Most of these
species belong to the endemic genera Nyctibatrachus and Raorchestes. Among other species, the median of the
suitable area predicted was 50% of the current distribution. In the case of lizards, only two species, namely
Cnemaspis indica and Agastyagama beddomei, show nearly complete loss of suitable area in the future, while
Cnemaspis belarion (80% - 99% decrease) and Cnemaspis galaxia (15% - 98% decrease) lose a majority of their
suitable area.
As expected,the reduction in suitable area was less severe for the relatively optimistic conditions, but 10 species of
frogs and three species of lizards showed greater suitable area under SSP5-8.5 compared to SSP1-2.6 contrary to the
expectations. Forteen species of frogs show an increase in suitable area even under the most pessimistic projections.
In most areas of increase are spatially disconnected (eg. Nyctibatrachus urbis, and Nyctibatrachus shiradi) and
present on a separate elevational contour.
Latitudinal and elevational extents of species
Latitudinal extents were smaller in future compared to the present for frogs (w = 6023,p<0.05,Figure 2), but not for
lizards (Figure 2,w = , p ). Across all current latitudinal extents, the median of predicted extents in the future
(SSP5-8.5) was consistently smaller (Figure 2). The patterns in latitudinal midpoints or range locations were less
clear but statistically significant for frogs (Figure 2;w = ,p ) and not for lizards (Figure 2; wil).
Elevational extents (Figure 3) of frogs were smaller in future compared to the present (w = 9488, p<0.05) but not
for lizards (w = p = 0.3). On the other hand, Elevational midpoints were higher for both frogs and lizards (Figure 4;
Frogs: w = 6355, p<0.05; Lizards: w = , p<0.05).
Areas of high diversity under present and future climates
Based on the stacked binary distribution models, approximately 5% of the total area of the WG for frogs, and 8% for
lizards, was found to be suitable for at least half the species compared to the maximum reported species richness
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(Figure 5). Most of these areas were in the Southern Western Ghats, particularly the Agasthyamalai mountain (80 N
to 8.90N, and the peaks of the Anamalai and Meghamalai mountains above 1000m elevation (8.90 to 10.30N). North
of the Palghat gap, the high diversity areas mark the 600m contour with the exception of the Nilgiri plateau (11.00N)
at more than 1000m elevation, and the Castle rock region (14.50N – 15.70N) forming a low elevation plateau north of
the Agumbe range (14.00N)
Under climate change, the high diversity areas reduced to less than 2% for SSP1-2.6, and 0.4% for SSP5-8.5
scenarios. The areas predicted with future scenarios were subsets of the area predicted under the current conditions
and major shifts towards higher or lower latitudes were not observed. The predicted high diversity areas were
typically restricted within higher elevation contours with loss of suitability in lower elevations compared to the
present.
Predictors of change in area
Bootstrap analysis showed that species that are most likely to go extinct in the future have narrower latitudinal (SES
= -3.6, p<0.01) as well as elevational extents (SES = -1.7, p<0.05) and lower latitudinal midpoints (SES =
-2.2,p<0.05 ) and higher elevational midpoints (SES = 2.81) (Figure 6). Latitudinal extents and midpoints were
highly cross correlated (pearson's correlation = 0.8). Therefore, we only included latitudinal extents in the model and
did not include the interaction between the two predictors in the full model. The Regression model for percentage of
suitable area in future for frogs with all predictors explained 42% of variance. Dropping latitudinal extent from the
model did reduce the AICc. The final model contains negative effects of elevational location, as well as upward shift
in elevation. The interaction effect between elevational range and location is weak and it indicates that the effect of
elevational location is marginally smaller at larger elevational extents. On the other hand, exploratory analysis of
interaction between latitudinal extents and midpoints, showed a positive effect of latitudinal extents, at lower and
intermediate latitudes but not at higher latitude.
In the case for lizards,the model contains positive effect of elevational range and negative effect of elevational
position and elevational shift, along with interaction between elevational extents and midpoints. The proportion of
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area in the future projection, increases with elevational extent at low elevations but the relation becomes weaker
towards higher elevation.
Discussion
The Western Ghats Escarpment is a region of global importance for the conservation of biodiversity due to a large
number of endemic species. Therefore, estimating the effects of anthropogenic climate change on the biodiversity of
the Western Ghats is of critical importance for conservation. Our results show that a combination of shifts in
climatic suitability and geographic limits to species distribution will have adverse effects on the frog and reptile
fauna of the mountain range. While studies do confirm the negative impact of anthropogenic climate change on
plants (Sen, Gode, et al. 2016), invertebrates (Sen, Shivaprakash, et al. 2016) and mammals (Sony et al. 2018),
assessments for species groups representing a large assemblage of species are still rare, with the notable recent
exception of reptiles (Srinivasulu et al. 2021). Here, we present an assessment of the effects of climate change on the
geographic distributions of frogs (133 species) and lizards (32 species) in the Western Ghats using the most
comprehensive distribution data assembled to date for these taxa in the region.
Predicted suitable areas for most species decreased under climate change as shown in earlier studies (Sen, Gode, et
al. 2016, Sony et al. 2018, Pramanik et al. 2021, Srinivasulu et al. 2021). As expected, most species displayed a
large variation in predicted suitable area between the most optimistic and pessimistic scenarios. This confirms that
the failure to arrest the rate of emissions and increase in temperature will have a severe negative impact on
biodiversity. Of the 133 species, 35 species of frogs showed an increase in suitable area mostly on the periphery of
current distribution, in the SSP1-2.6 scenario only. Further, for nine species, at least part of the increase in area is
disconnected from the current distribution and so it is uncertain that these species can access these areas. This is
particularly true for species with small latitudinal extents such as Indosylvirana urbis, Nyctibatrachus deveni, and
Nyctibatrachus karnatakaensis but also the case for species with the largest increase in area - Nyctibatrachus
Shiradi, and Nyctibatrachus sylvaticus. Though suitable areas might be present, it is unlikely that most of these
species would be able to extend their ranges. On the other hand, some species with large latitudinal extents and
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large increase in suitability such as, Euphlyctis karaavali, and Uperodon anamalaiensis have disjunct distributions
where only one or two occurrences are reported across a large gap in latitude. Future work may fill the gaps in
distribution leading to different model predictions, or the species may be identified as cryptic species complexes, so
that the suitability for different populations/species should be predicted separately. On the other hand, the increase in
area for lizards takes place by extending the existing distribution around the existing suitable areas. For species that
show a particularly large increase in area, for instance Cnemaspis lithophilis and Sitana spinaecephalus, the increase
is not on spatially disconnected polygons where dispersal may be uncertain.
Within the Western Ghats, mean annual temperature shows less variation across latitude than across elevations (Page
& Shanker 2020). Therefore, it is likely that this variable represents elevational limits of the species. On the other
hand, seasonality in precipitation and temperature increases significantly towards higher latitudes (Page & Shanker
2020). Therefore, seasonality variables should contribute to the latitudinal limits of species distributions to a greater
degree. As expected, mean annual temperature and precipitation seasonality were important variables for most of the
species of frogs. On the other hand, temperature seasonality was found to be the most important variable, with
minimal importance for precipitation seasonality, for lizards in this study and for squamates in general in other
studies (Srinivasulu et al. 2021). Limits of water availability on amphibian life cycles very likely generate this
difference.
High diversity areas show striking reduction with future climate projections. The changes reported here are drastic
compared to similar results for reptiles. High diversity areas for reptiles covered a greater proportion of the Western
Ghats, and remained largely contiguous even under the most pessimistic scenario in our study, as well as others
(Srinivasulu et al. 2021). In comparison, the areas for amphibians are smaller and discontinuous even under current
conditions. Further, under the effect of climate change, the high diversity areas shrink in size and remain restricted to
higher elevations. This result confirms the prediction of ‘lowland biotic attrition’ (Colwell et al. 2008), i.e. low
elevation assemblages lose species due to shifts in species distribution towards higher elevations. Elevational range
shift is the most immediate response to climate change expected for tropical species (Colwell et al. 2008). Upward
shifts in elevational distributions and extinction threat for high elevation montane species are also predicted for
amphibian fauna of Madagascar (Raxworthy et al. 2008) and south-east Asia (Bickford et al. 2010). This is also
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supported in the present study as elevational distributions for frogs and lizards do shift towards higher elevation
(Figure 4). Because mountains are naturally narrower near the summit, the amount of area available decreases
towards higher elevations. Therefore, shifts in distributions towards higher elevations should decrease the total
suitable area, other factors being constant. Shift in elevational midpoints is an important predictor of change in
suitable areas for frogs as well as lizards, which supports the above prediction. As the space available for upward
movement will reduce towards higher elevation, the effect of increase in elevational extents on future suitability
should be greatest at low elevations and should reduce with increase in elevation. This should result in interaction
between the effect of elevational extents and elevational midpoints. While the interaction is not a strong predictor of
future suitability, exploratory analysis indicates that for frogs, the slopes of the relation are steeper at intermediate
elevations and latitude.
The projected changes in suitability should be seen as conservative estimates of climate vulnerability, as biological
mechanisms such as diseases, developmental errors due to accelerated metamorphosis, and decrease in dissolved
oxygen in streams among others can accelerate the negative effects of climate change beyond changes in the climate
envelope itself (Bickford et al. 2010, Blaustein et al. 2010, Li et al. 2013). The results presented here suggest that
temperature gradients across elevation, and seasonality gradients across latitude, contribute most to the climatic
limits of species distributions. Most species do not show latitudinal shifts in suitability as a response to climate
change and in the few cases where such shifts are observed, the ability of the species to access and survive in these
areas remains uncertain due to discontinuous topography and the presence of sister species. Overall, the results
suggest that the herpetofauna of the Western Ghats will be severely affected by climate change in the near future,
with greater impacts on frogs, in particular some endemic groups, than lizards.
Acknowledgements
AM would like to thank the CSIR- Research Associate program, and the IISC-DBT postdoctoral fellowship program
for support during preparation of the manuscript and the state forest departments of Kerala, Karnataka, Tamil Nadu,
Goa and Maharashtra for facilitating the fieldwork. VSP, VT, SP, and AS contributed the data for the analysis
presented here. KPD acknowledges the support of the Director, ZSI, Kolkata and the Officer-in-Charge, ZSI, WRC,
Pune for the support.
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Statements and Declarations
Funding : Critical Ecosystem Partnership Fund (CEPF) ( ), CSIR, DBT-IISc Partnership Programme ( ), Ministry of
Environment, Forest and Climate Change (MOEFCC) ( ); Council of Scientific and Industrial Research (CSIR) –
Research Associate fellowship ( ).
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was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made
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Permit: The following state forest departments provided permission for fieldwork and collection: Kerala, Karnataka,
Tamil Nadu, Goa and Maharashtra.
Field team: Mrugank Prabhu, SR Chandramouli, Mayavan
Author contributions:
KS and AM conceptualized the study. AM performed the statistical analysis. VT, SPV and KPD collected the data,
and provided key inputs for distribution models. AM wrote the first draft of the paper. KS edited the draft and
provided inputs at all stages.
Competing interests
The authors have no relevant financial or non-financial interests to disclose.
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Figure 1. Suitable areas predicted under climate change compared to currently suitable area for frogs (a) and for
lizards (b). Variation expected due to differences among scenarios is represented as vertical segments. Solid
segments show reduction in area while dotted segments show increase in suitable area in the future.
Figure 2. Latitudinal range extents of frogs (a) and lizards(b) in future (SSP5-8.5) compared to the present. The
Histograms in top panels show the number of species that have the corresponding range extents.
Figure 3. Latitudinal midpoints of frogs (a) and lizards(b) in future (SSP5-8.5) compared to the present. The
Histograms in top panels show the number of species that have the corresponding range extents.
Figure 4. Elevational extents and midpoints of frogs (a, c) and of lizards (b, d) in future (SSP5-8.5) compared to the
present. Dashed lines are 1:1 lines indicating no change.
Figure 5. Areas with High diversity of frogs (a,b,c) and for lizards (d,e,f) within the Western Ghats under current
(a,d), SSP1-2.6 (b,e) and SSP5-8.5 (c,f) scenarios and for lizards
Figure 6. Density kernel for elevational midpoints (a) latitudinal extents (b) elevational extents, (c) latitudinal
midpoints, and (d) elevational midpoints of entire species pool (black lines) and the species have suitable area in
SSP5-8.5 which less than 1% of current suitability (red lines).
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Figure 1
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Figure 2
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Figure 3
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Figure 4
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Figure 5
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Figure 6
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Table 1. predictor variable used in distribution models.
Predictor Description
Bioclimatic
Bio 1 Annual Mean Temperature
Bio 4 Standard deviation of temperature x 100
Bio 12 Annual Precipitation
Bio 14 Precipitation of Driest Month
Bio 15 Precipitation Seasonality (Coefficient of Variation)
Bio 18 Precipitation of Warmest Quarter
Bio 19 Precipitation of Coldest Quarter
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Table 2. Percentage of species within each family for which suitable area decreased or increased in the future
climate scenarios.
SSP1-2.6 SSP5-8.5
decrease increase decrease increase
Frogs Bufonidae 83.3 16.7 66.6 33.4
Dicroglossidae 100 100
Micrixalidae 81.8 18.2 100
Microhylidae 60 40 70 30
Nyctibatrachidae 78.5 21.5 85.7 14.3
Ranidae 84.6 15.4 84.6 15.4
Ranixalidae 66.6 33.4 66.6 33.4
Rhacophoridae 80.3 19.7 96 4
Lizards Agamidae 71.4 28.6 92.8 7.2
Geckonidae 72.2 27.8 61.1 38.9
30
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Table 3. Linear regression models for change in area between current and SSP5-8.5 projections for frogs.
Rank Models K AICc Delta
AICc
AICc
weight
R2
1 elevational range + elevational mid-point +
shift in elevational midpoint + shift in latitudinal midpoint
6 1163.75 0 0.65 0.43
2 elevational range + elevational mid-point +
elevational range:elevational mid-point +
shift in elevational midpoint + shift in latitudinal midpoint
7 1165.5 1.81 0.26 0.43
3 elevational range + elevational mid-point +
elevational range:elevational mid-point +
latitudinal range + shift in elevational midpoint + shift in
latitudinal midpoint
8 1167.64 3.88 0.09 0.43
31
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was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made
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Table 4. Coefficients of regression model for percentage of area in future predictions for frogs.
Predictors Estimate Std. Error p value
Intercept 54.5 2.87 <0.05
Elevation extents 5.76 3.04 0.06
Elevation midpoints -21.83 3.71 <0.05
Shift in elevation
midpoints
-8.38 3.53 0.01
shift in latitudinal
midpoint
10.13 3.12 <0.05
32
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was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made
The copyright holder for this preprint (whichthis version posted April 16, 2025. ; https://doi.org/10.1101/2025.04.10.648234doi: bioRxiv preprint
Table 5. Coefficients of regression model for percentage of area in future predictions for lizards. Elevational and
latitudinal predictors are part of two separate linear models. The response variable was log transformed.
Predictors Estimate Std. Error p value
Intercept 3.67 0.22 <0.05
Elevation extents 0.3 0.22 0.17
Elecation midpoints -0.2 0.3 0.5
Shift in elevation
midpoints
-0.63 0.22 <0.01
Elevation
extents:Elevational
midpoints
0.65 0.28 0.05
Latitudinal range 0.46 0.24 0.06
shift in latitudinal
midpoint
0.85 0.23 0.001
33
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was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made
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