Climate change is affecting biodiversity and ecosystem function worldwide, and the lowland tropics are of special concern because organisms living in this region experience temperatures that are close to their upper thermal limits. However, it remains unclear how and whether tropical lowland species will be able to cope with the predicted pace of climate warming. Additionally, there is growing interest in examining how quickly thermal physiological traits have evolved across taxa, and whether thermal physiological traits are evolutionarily conserved or labile. We measured critical thermal maximum (CTmax) and minimum (CTmin) in 56 species of lowland Amazonian frogs to determine the extent of phylogenetic conservatism in tolerance to heat and cold, and to predict species’ vulnerability to climate change. The species we studied live in sympatry and represent ~65% of the known alpha diversity at our study site. Given that critical thermal limits may have evolved differently in response to different temperature constraints, we tested whether CTmax and CTmin exhibit different rates of evolutionary change. Measuring both critical thermal traits allowed us to estimate species’ thermal breadth and infer their potential to respond to abrupt changes in temperature (warming and cooling). Additionally, we assessed the contribution of life history traits and found that both critical thermal traits were correlated with species’ body size and microhabitat use. Specifically, small direct-developing frogs in the Strabomantidae family appear to be at highest risk of thermal stress while tree frogs (Hylidae) and narrow mouthed frogs (Microhylidae) tolerate higher temperatures. While CTmax and CTmin had considerable variation within and among families, both critical thermal traits exhibited similar rates of evolutionary change. Our results suggest that 4% of lowland rainforest frogs assessed will experience temperatures exceeding their CTmax, 25% might be moderately affected and 70% are unlikely to experience pronounced heat stress under a hypothetical 3°C temperature increase.
Citation: von May R, Catenazzi A, Santa-Cruz R, Gutierrez AS, Moritz C, Rabosky DL (2019) Thermal physiological traits in tropical lowland amphibians: Vulnerability to climate warming and cooling. PLoS ONE 14(8): e0219759. https://doi.org/10.1371/journal.pone.0219759
Editor: Stefan Lötters, Universitat Trier, GERMANY
Received: January 9, 2019; Accepted: July 2, 2019; Published: August 1, 2019
Copyright: © 2019 von May et al. This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Data Availability: All relevant data are within the manuscript and its Supporting Information files. S2 Appendix contains the voucher numbers and GenBank accession numbers for the taxa and genes sampled in this study.
Funding: Research was supported with grants from the National Science Foundation (Postdoctoral Research Fellowship DBI-1103087), the American Philosophical Society, and the National Geographic Society (Grant # 9191-12) to RvM; the Amazon Conservation Association to RvM and A. Catenazzi; and the Swiss National Science Foundation (#116305), the Rufford Small Grants Foundation, the Chicago Board of Trade Endangered Species Fund, the Amphibian Specialist Group and the Disney Worldwide Conservation Fund to A. Catenazzi. D.L. Rabosky thanks the David and Lucile Packard Foundation. A. Catenazzi thanks the Amazon Center for Environmental Education and Research for support during field courses. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.
Competing interests: The authors have declared that no competing interests exist.
Climate change is affecting biodiversity and ecosystem function worldwide, and the lowland tropics are of special concern because organisms living in this region experience temperatures that are already close to their upper thermal limits [1–4]. However, it remains unclear how and whether tropical lowland taxa will be able to cope with the predicted pace of climate warming. Given that lowland rainforest habitats are expected to become hotter in the coming decades [5–6], it is imperative that we obtain baseline data on critical thermal limits of lowland rainforest species. To this end, measuring physiological thermal limits such as critical thermal maxima (CTmax) will improve our predictions of species’ vulnerability to climate warming. Furthermore, measuring critical thermal minima (CTmin) is also important because it will allow us to estimate species’ thermal breadth (= CTmax−CTmin) and infer their potential to respond to extreme temperature fluctuations (warming and cooling). Although CTmax and CTmin measure two very different physiological end points to thermal performance curves (i.e., death occurring at temperatures immediately above CTmax, but typically not below CTmin), the ability of organisms to perform basic movements such as the righting reflex is very likely associated with individual fitness.
There is growing interest in examining whether physiological traits are evolutionarily conserved or labile, because knowing how quickly thermal physiological traits evolved can be used to improve predictions on species’ potential to respond to novel climates [7–8]. Growing evidence suggests that CTmax is relatively inflexible across elevation (e.g., [8–10], but see ), with a narrow upper limit and low plasticity [12–13], and that it is evolutionary stable across a variety of ectotherms . Consequently, one would predict that species living at the same elevation and experiencing the same thermal environment, such as those in lowland tropical rainforest, exhibit narrow upper thermal limits. While lowland taxa may experience environmental temperatures that are closer to their critical thermal limits, not all species in a lowland rainforest community may exhibit similarly narrow upper thermal limits. Likewise, not all species in a lowland rainforest community may be equally vulnerable to increased temperatures (as it would be predicted using bioclimatic variables, e.g., WorldClim ). If CTmax varies broadly among lowland species, one would infer that only a subset of the species in the community (i.e., those with lower CTmax values) is vulnerable to warming.
Another reason to study critical thermal limits pertains to the role of temperature in amphibian immunity and disease dynamics. Previous research has shown that frogs’ immune system might be more effective at deterring pathogen infection (e.g., chytridiomycosis) at warm or more stable temperatures than at cold and variable temperatures [16–18]. In western Amazonia, sudden drops in air temperature associated with incursions of cold air masses coming from southern South America and the Antarctic region are common [19–20]. These cold surges, locally called friajes (Peru), friagen (Brazil), or surazos (Bolivia), are common during the Austral winter and reduce animal activity in lowland Amazonia. Fewer mammals and birds are active during these periods [21–22] and some amphibians behaviorally adjust their vertical distribution along the forest habitat . Additionally, these cold surges may facilitate pathogen infection, such as chytridiomycosis, which is common in some lowland Amazonian habitats . How species respond to lower temperatures during a cold front might depend on their physiological thermal limits. If the temperature drops to 10–12°C, as often does during a cold front [20, 25], many lowland taxa may reach their CTmin. As a result, these organisms may stop moving and may become vulnerable to predators that tolerate colder temperatures. In turn, species that tolerate cooler temperatures and remain active during a cold front may be able to do so by maintaining a higher metabolic rate, which requires higher use of energy reserves or higher caloric intake . Additionally, given that temperature decreases at a relatively constant rate with increasing elevation (a result of adiabatic cooling), measuring tolerance to cold in lowland species can be useful for inferring their ability to shift to higher elevations.
Here we examined the variation of CTmax and CTmin in 56 species of lowland Amazonian rainforest frogs to test if tolerance to heat and cold are phylogenetically conserved or labile. We used a phylogenetic framework to account for non-independence of interspecific data resulting from shared ancestry. While we tested if tolerance to heat and cold are phylogenetically conserved or labile, we do not conclude that these traits are exclusively adaptive. Additionally, we assessed whether species are vulnerable to predicted warming trends across the Amazonian lowlands and comment on species’ vulnerability to low temperatures associated with cooling events that are common in the region. We estimated the operative warming tolerance by subtracting the maximum operative temperature from CTmax, as done in previous studies [11, 27]. Our specific goals were to assess (1) the extent of phylogenetic conservatism in heat and cold tolerance, (2) to determine whether heat-tolerance or cold-tolerance evolves more quickly among species, and (3) to determine whether key life history or morphological attributes predict variation in CTmax and CTmin across species. We used a phylogenetic comparative framework for all analyses. Using a hypothetical 3°C warming increase (e.g., IPCC warming scenarios RCP6.0 and RCP8.59 ), we predict the impacts of future climate warming on this diverse community of rainforest frogs.
Material and methods
We studied amphibian communities at Los Amigos Biological Station (12°34'07" S, 70°05'57" W, 250 m elev.), located in the Madre de Dios region, Peru, between 2012 and 2017. The lowland rainforests of this region contain 85 species of frogs in broad sympatry, and the humid lowlands of western Amazonia include some of Earth’s most species-rich amphibian communities. We previously described the study site, local climate, and amphibian fauna [29–30]. We obtained data on species’ elevational distributions from surveys conducted along the elevational gradient from Los Amigos Biological Station [11, 29–31] to Tres Cruces at 3,800 m [27, 32–34]. Daily temperatures at Los Amigos showed that maximum air temperatures in 2015–2017 were consistently higher than average since recording started in 2000 (e.g., maximum air temperatures of 30°C or higher were very common between November 2015 and April 2016 and 13 days had maximum air temperatures above 38°C ).
We used data loggers to obtain empirical data on microhabitat temperatures from lowland Amazonian habitats. We placed iButton data loggers (Maxim Integrated Products, Sunnyvale, California, USA) in two forest microhabitats, leaf-litter and understory vegetation, used by frogs across forest types. Daily temperatures were recorded in floodplain forest, terra firme forest, bamboo forest, and palm swamp during part of the wet season of 2008 (44 days), part of the wet season of 2016 (25 days), and part of the wet season of 2017 (24 days). Additionally, we placed HOBO data loggers (Onset Computer Corporation, Pocasset, Massachusetts, USA) in the leaf-litter in the floodplain and the terra firme forest to record the temperature from 16 November 2016 to 5 December 2017 (385 days). Daily temperatures measured in these forest types are summarized in  and in the Results section (see Temperature data).
Critical thermal limits
We measured CTmax in 384 individuals (56 species) and CTmin in 137 individuals (41 of the 56 species). We measured snout-vent length (SVL) to the nearest 0.1 mm with a Vernier caliper, and measured body mass to the nearest 0.1 g using a Pesola scale. Frogs included in our dataset (S1 Appendix) had an SVL range of 10.1–51.0 mm; we excluded large-bodied species (i.e., species exhibiting maximum outlying values of SVL and body mass). We captured animals in the field and transported them to a field laboratory, where we kept them in individual containers with a thin layer of water embedded in a paper towel for 2–3 days prior to measurements. Plasticity and adaptation likely influence the traits we measured, because we performed our experiments in the field where fully controlled conditions are difficult to achieve. Nevertheless, we strived to maintain similar ambient temperature and acclimation conditions for all taxa (within 24–26°C range). We used non-lethal experiments to evaluate critical thermal maxima (CTmax) and minima (CTmin). We measured CTmax and CTmin as the point when frogs lost their righting response, defined as the moment when a frog cannot right itself from being placed venter-up for a period longer than 5 sec [27, 35]. The righting response is relevant for considering selection on thermal physiology, because a frog that is unable to display their automatic righting reflex will likely be unable to escape predators. We placed each individual in a plastic cup with a thin layer of water (3–5 mm) and immersed the cups in a water bath. For CTmax, we increased the bath temperature from ~24°C to up to ~40°C at a rate of ~1°C/minute by adding warm water. For CTmin, we decreased the temperature from ~24°C to ~0°C by adding ice to the water bath . We forced animals to a venter-up position, and we used a quick-reading thermometer to measure temperature against the body of the frog immersed in the thin layer of water. In this procedure, the tip of the thermometer should be placed between two skin surfaces (e.g., groin region) so that most of it is in contact with the animal. We ended the experiments when the animals were unable to right themselves for >5 sec (i.e., when they lost their righting response). We included as controls individuals of representative species (N = 29 individuals, 14 species) that were similarly probed for their righting reflex over ~20 minutes, but without experiencing temperature change, to take into account any potential behavioral or fatigue effect . No individuals lost their righting reflex during these control trials.
After experimentation, animals were released at the point of capture and only a few individuals were euthanized by immersion in benzocaine hydrochloride solution (250 mg/L), where animals were kept for 10–20 minutes until movement ceased. After euthanasia, tissue samples (e.g., liver, muscle) were taken from the animals and preserved in 2 mL cryogenic tubes filled with RNAlater or 95% ethanol. Following tissue collection, specimens were fixed in 10% formalin, and permanently stored in 70% ethanol. Voucher specimens were deposited in the Herpetological Collections of the University of Michigan Museum of Zoology (UMMZ) and the Museo de Historia Natural of the Universidad Nacional Mayor de San Marcos (MUSM) in Peru.
Given the small size of the frogs included in this study (range 10.1–51.0 mm in SVL), we assumed that this temperature is equivalent to the core temperature of frogs . While we did not measure individuals’ body temperatures with thermocouple probes inserted into the frogs’ cloaca, it is reasonable to assume that our measurements (taken with a quick-reading thermometer placed against the body of the frog) reflect body temperatures. We justify this assumption on (i) empirical evidence shows that cloacal temperature and skin temperature are strongly correlated  and represent the core temperature; (ii) paired tests using live frogs reaching a maximum SVL of 21 mm and similarly-sized plaster models suggest that individual frogs achieve equilibrium body temperature within 1 min ; and, (iii) differences in heating rates (e.g., 1°C/1 min vs. 1°C/5 min) in individuals larger than 10 mm do not result in different heat tolerances . Our empirical data also supported the assumption that the body size of experimental individuals did not bias our measurements of critical thermal limits (see S1 File and S1 Fig, S2 Fig, S3 Fig and S4 Fig). Thus, differences in critical thermal traits among species, such as those reported here, likely reflect biological differences.
Our analysis included DNA sequences from three mitochondrial genes (12S, 16S, COI) and two nuclear genes (RAG-1, Tyr). Extraction, amplification, and sequencing of DNA followed protocols described previously  (see also S2 File). We used a multispecies coalescent approach implemented in *BEAST 2  to infer a Bayesian multilocus timetree of the focal taxa. The primary goal of the analysis was to obtain an ultrametric tree used in phylogenetic comparative analyses (see below). Our analyses depended on the relative branch lengths of the tree, but we preferred to illustrate our tree in rough units of time. Thus, we used an uncorrelated relaxed molecular clock with the rate of nucleotide substitution for 16S set at 1% per million years as done in recent studies [11, 42]. However, we note that the dates associated with the tree should only be viewed as approximate and that there are multiple sources of error when calibrating phylogenies . The tree included sequence data used in previous analyses  and sequence data obtained from specimens collected in the study region (S2 Appendix). The analysis in *BEAST included two independent runs, each with 1 billion generations and sampled every 100000 generations. Following the completion of the analysis, we used Tracer v1.5  to examine effective sample sizes, verify convergence of the runs, and to ensure the runs had reached stationarity. Observed effective sample sizes were sufficient for most parameters (ESS >200) except for substitution rates for a few partitions. We discarded the first 10% of samples from each run as burn-in. Subsequently, we used LogCombiner to merge all remaining trees from both runs and used TreeAnnotator  to summarize trees and obtain a Maximum Clade Credibility tree.
For a given quantitative trait, phylogenetic signal is present when related species tend to resemble one another [46–47]. We tested for phylogenetic signal by calculating the K statistic  and by estimating the λ parameter ; we used the R package ‘phytools’  to estimate K and λ. These methods account for non-independence of interspecific data resulting from shared ancestry [50–52]. For K, values smaller than 1 indicate that related species are less similar than expected under a Brownian motion model of trait evolution whilst values greater than 1 indicate that related species resemble each other more than expected under a Brownian motion model of trait evolution . The value of λ typically ranges from 0, indicating no phylogenetic signal, to 1, indicating strong phylogenetic signal (i.e., when patterns of covariance among species are exactly as predicted under a Brownian motion model of evolution ).
Rates of evolutionary change in critical thermal traits
Prior to comparing the rates of evolutionary change for CTmax and CTmin, we searched for a model of evolution that best explains the variation in the observed data. We used the fitContinuous function in GEIGER  to fit three models of evolution: Brownian Motion (BM), single-optimum Ornstein-Uhlenbeck (OU), and Early Burst (EB). The Brownian motion model assumes a zero net change, but the underlying evolutionary process has a constant variance per unit time, and the differences between species will be proportional to the time since their divergence. The Ornstein-Uhlenbeck model describes a stochastic process involving an overall global optimum, but with a restraining parameter that determines the intensity of attraction between a particular trait value and the optimum. With OU, differences between species will not necessarily relate to their time since divergence. Finally, the Early Burst model assumes an exponential decline in rates through time. This means that species with recent divergence times will be very similar, while species with deeper divergences will be proportionately more dissimilar than closely related lineages. After determining the best fitting model of evolution for each trait, we used the R package ‘APE’  and code developed by Adams  to estimate the rates of change.
Correlates of CTmax and CTmin
We explored the relationship between critical thermal traits and other life history characteristics including body size (SVL), body mass, and body mass index (BMI). We calculated BMI as the ratio of weight to size by dividing the mass (in g) by the square of SVL (in mm). We used analysis of covariance (ANCOVA) to test the effect of family membership on both CTmax and CTmin while controlling for the effect of SVL (co-variable). We also considered maximum air temperatures (Ta) obtained from a local weather station, and maximum operative temperatures (Te) estimated from field measurements taken with data loggers placed in the forest floor and understory vegetation in mature floodplain forest and terra firme forest. We calculated operative warming tolerance (OWT) by subtracting the average maximum Te from CTmax as in previous studies [11, 27]. In addition to OWT, we used bioclimatic data from WorldClim  to calculate warming tolerance (WTw) as in ; we calculated WTw by subtracting the maximum temperature of the warmest month (bioclimatic variable BIO6 in WorldClim ) from CTmax. Lastly, we calculated the thermal breadth, defined as the difference between CTmax and CTmin. We examined a pairwise scatterplot matrix to visualize the cross-correlations among variables (S5 Fig) and discarded predictor variables that were highly correlated with each other (r > 0.70). We used the R package ‘phylolm’ [57–58] to fit phylogenetic generalized linear regression models (PGLMs). This package implements a phylogenetic regression under various models for the residual error, including Brownian Motion (BM) and Ornstein-Uhlenbeck (OU). We used the AIC value to identify the model that best explains the variation of observed data .
We estimated the relative importance of each variable in explaining the observed variation of CTmax and CTmin with multiple regression . First, we used the pairwise scatterplot matrix (S5 Fig) and discarded variables that were highly correlated (r > 0.70). Then, we ran PGLMs for all possible additive models including the predictor variables. We calculated the Akaike weight for each model, and the relative importance of each factor was inferred by examining the extent of its contribution to highly scoring models. We used the sum of the relative Akaike weights for the models containing that factor to determine its relative importance.
Data recorded over a 1-year period (16 Nov. 2016–5 Dec. 2017) indicate that daily minimum, mean, and maximum temperatures measured in the leaf litter of the floodplain and terra firme forests were similar (S6 Fig). Daily maximum temperatures were similar most of the year, with the exception of some periods of higher maximum temperature in the floodplain than in the terra firme forest. During this year, there were two pulses of high temperature reaching 34.8 and 35.1°C, respectively, in the floodplain forest. These two pulses were four days apart and the intermediate days had maximum temperatures ranging from 29.5 to 31.8°C. However, the pulse with the highest temperature (35.1°C) was followed by four days with maximum temperatures above 33.3°C; this warming event took place between 29 August and 2 September 2017. During this period, minimum temperatures in the floodplain ranged between 23.3 and 24.0°C and minimum temperatures in the terra firme ranged between 23.5 and 24.2°C. Furthermore, there were two pulses of high temperature reaching 28.4 and 29.2°C, respectively, in the terra firme forest. However, these pulses occurred in different dates than those observed in the floodplain forest. Despite these differences in observed temperature in the two forest types, maximum daily temperatures in the leaf litter remained <28.0°C throughout most of the year, with average maximum temperature of 26.8°C. During this year, the lowest temperatures were 13.4°C in the floodplain and 13.9°C in terra firme. However, minimum temperatures in previous years were lower and similar to those recorded throughout the western Amazon (10–12°C [19, 25]).
Phylogenetic relatedness and critical thermal traits
We observed considerable differences in CTmax values (27.4–43.2°C; Fig 1). Eight pairs of close relatives had non-overlapping CTmax values (Adenomera andreae–Lithodytes lineatus, Rhinella marina–R. margaritifera, Allobates conspicuus–A. femoralis, Dendropsophus leucophyllatus–D. triangulum, Dendropsophus schubarti–D. minutus, Dendropsophus koechlini–D. kamagarini, Phyllomedusa vaillantii–P. camba, Elachistocleis muiraquitan–Hamptophryne boliviana). Rhinella marina (the cane toad, distributed in lowlands and lower montane forests < 1200 m) had the highest CTmax, whereas several members of the family Strabomantidae (Noblella myrmecoides, Pristimantis buccinator, P. toftae, P. ockendeni) had the lowest CTmax. CTmin varied considerably among species (4.9–16.2°C; Fig 2), and nine pairs of close relatives exhibited non-overlapping CTmin values (Leptodactylus leptodactyloides–L. petersii, Edalorhina perezi–Engystomops freibergi, Rhinella marina–R. margaritifera, Ameerega hahneli–A. trivittata, Boana sp. G–B. lanciformis, Pristimantis carvalhoi–P. ockendeni, Pristimantis toftae–P. reichlei, Oreobates cruralis–O. quixensis, Elachistocleis muiraquitan–Hamptophryne boliviana).
Multi-locus tree depicting the relationship among 50 species (top) and box plots depicting their CTmax values (bottom). The box plots show the median (black bar), interquartile range (box), and 1.5 times the inter-quartile range (bars); circles represent outliers. Species are color-coded according to family membership (blue = Leptodactylidae, gray = Bufonidae, pink = Dendrobatidae, green = Hylidae, orange = Strabomantidae, violet = Microhylidae). The orange line (dashes) represents the estimated maximum temperature near the forest floor, measured with iButton data loggers; the red line (dashes) represents a hypothetical 3°C increase in temperature.
Species tree depicting the relationship among 37 species (top) and box plots depicting their CTmin values (bottom). The box plots show the median (black bar), interquartile range (box), and 1.5 times the inter-quartile range (bars); circles represent outliers. Species are color-coded according to family membership (blue = Leptodactylidae, gray = Bufonidae, pink = Dendrobatidae, green = Hylidae, orange = Strabomantidae, violet = Microhylidae). The gray area represents the range of typical cold front minimum temperatures (10–12°C [20, 25]) and the blue line represents the average temperature recorded during cold fronts between 2001 and 2017.
We found moderate phylogenetic signal for CTmax (Table 1), as suggested by an overall trend in which closely related species (especially those in families Leptodactylidae, Strabomantidae, and Microhylidae) exhibited more similar CTmax than distantly related species (Fig 1). In contrast, no phylogenetic signal was detected for CTmin (i.e., close relatives were less similar than expected from Brownian motion along the tree). Additionally, there was no phylogenetic signal for body size (SVL) and body mass index (Table 1).
Log likelihood values included correspond to the λ estimates. Phylogenetic signal tests were done with the full dataset (50 species) for all traits except for CTmin. Phylogenetic signal tests were conducted for CTmin and repeated for CTmax with the reduced dataset (37 species). P-values are relative to the null hypothesis of phylogenetically-unstructured data (see text for details).
Rates of thermal physiological change
Comparisons across three models of trait evolution indicate that BM was the best model for CTmax, whereas OU was the best model for CTmin (Table 2). Given that the method used for estimating the rates of evolution  assumes a zero net change (BM), we performed this test assuming BM for both traits and using the reduced dataset (37 species). We found that CTmax and CTmin exhibit similar rates of thermal physiological change (likelihood ratio test, LRT = 0.362, AICc = 344.790, P = 0.547).
Likelihood estimates (lnL) and corrected Akaike Information Criterion (AICC) values for tests considering the reduced dataset (i.e., 37 species with both CTmax and CTmin data) are provided; AICC values in bold indicate the best-supported model.
Correlates of CTmax and CTmin
Interspecific variation in critical thermal limits was correlated with body size. Our PGLS analyses showed that CTmax tends to increase with increasing body size while CTmin tends to decrease with increasing body size (Table 3; Fig 3). Additionally, CTmax negatively correlated with CTmin (Table 3), whereas thermal breadth correlated with body size (S5 Fig). All tested relationships were significant under pure OLS regression, the Brownian motion (BM) model, and under the Lambda transform model. Nevertheless, these relationships were best supported under the Lambda model, and, in the case of CTmax vs. CTmin, both the Lambda and BM model provided equal support (i.e., had similar IAC values; Table 3). Most other models ran with two or more variables did not provide a better fit predicting CTmax compared to univariate models (i.e., AIC values of models with two or more variables were greater than AIC values of univariate models; S1 Table); the exception to this was a model ran with body size and height above the ground. In contrast, several models ran with two or more variables provided a better fit predicting CTmin compared to univariate models (S1 Table). The two best models predicting CTmin included (i) a model ran with body size and height above the ground and (ii) a model ran with BMI and height above the ground (S2 Table).
CTmax tends to increase with increasing body size (a) and CTmin tends to decrease with increasing body size (b). Species are color-coded according to family membership (see also Fig 1 and Fig 2), and the size of points is proportional to body mass index (BMI). The slope of the regression line reflects the phylogenetic correction in each model, considering the full dataset for CTmax (50 species) and the reduced dataset for CTmin (37 species).
Model fitting for CTmax included the full dataset (50 species); model fitting for CTmin included the reduced dataset (37 species). Bold font indicates significant values.
The ANCOVA indicated that both body size and family membership, but not their interaction, affected CTmax (Table 4). These results suggest that the slopes of the regression lines between CTmax and SVL were similar for all groups (families) considered in this test. Additionally, removing the interaction (between SVL and family) did not affect the fit of the model (F = 1.424, P = 0.2378). Thus, body size had a positive and significant effect on CTmax, and the effect was similar for all families included in the analysis. Nonetheless, terrestrial breeding frogs (Strabomantidae) had lower CTmax than that of other families (Fig 3). The ANCOVA ran on the reduced dataset (37 species) indicated that both body size and family membership, but not their interaction, affected CTmin (Table 4). These results suggest that the slopes of the regression lines between CTmin and SVL were similar for all groups. Moreover, removing the interaction (between SVL and family) did not affect the fit of the model (F = 0.687, P = 0.638). Thus, body size had a negative and significant effect on CTmin, and the effect was similar for all families included in the analysis. Hylid frogs (Hylidae) had lower CTmin than that of other families (Fig 3).
Model fitting for CTmax was done with the full dataset (50 species); model fitting for CTmin was done with the reduced dataset (37 species). Bold font indicates significant values.
Our tests using PGLMs and considering several predictor variables suggested that body size was the most important variable for CTmax, whereas height above the ground was the most important variable for CTmin (Fig 4). Additionally, height above the ground was the second most important variable for CTmax, whereas body mass index was the second most important variable for CTmin (Fig 4). Critical thermal traits did not correlate with the elevational midpoint of species. Additional tests also showed that critical thermal traits did not correlate with species’ maximum elevation and elevational range (both of which were correlated with elevational midpoint).
(a) Model fitting for CTmax was done with the full dataset (50 species); (b) model fitting for CTmin was done with the reduced dataset (37 species). The bars depict the relative importance of each variable, estimated across additive models and weighted by relative AIC weights, followed by the significance level (asterisk denotes a significant correlation, P < 0.05) and the directionality of the coefficient for each variable.
We provide critical thermal trait data for 56 species of lowland Amazonian frog species living in broad sympatry, increasing our knowledge of the thermal physiology of diverse tropical amphibian communities. Previous studies of critical thermal traits in tropical frog assemblages (e.g., [60–61]) included a relatively small number of species present in those assemblages (10–19 species), whereas our study included a larger portion (~65%) of the species present in a diverse Neotropical frog community. One of our key findings is the high variability in both CTmax (27.4–43.2°C) and CTmin (4.9–16.2°C) in species living in largely undisturbed habitats. The range of CTmax values is comparable to that observed in frogs found across a habitat gradient spanning forest to converted habitats such as palm, banana, and pineapple plantations (e.g., [61–62]). In some of these studies, frog species restricted to continuous forest exhibited CTmax values (~28°C) that were similar the lowest CTmax values reported in our study. However, our study also recovered high CTmax, previously associated with communities inhabiting disturbed habitats, in frogs inhabiting a largely pristine lowland rainforest.
About one third of the species included in our study exhibited intraspecific variation in CTmax and CTmin that is worth noting (in both cases, the range was 4–5°C), given that within-population variability is an important (yet underappreciated) attribute of species’ thermal physiology [63–64]. Alternatively, given so much variation, traits may be very plastic and could change quickly even over an individual’s lifetime. Our findings, along with those from a recent study focusing on frogs distributed along a tropical elevational gradient , suggest that niche divergence in tolerance to heat and cold is common in tropical ectothermic vertebrates. Additionally, both CTmax and CTmin exhibited similar rates of evolutionary change despite differing amounts of phylogenetic signal (CTmax exhibited a moderate phylogenetic signal and CTmin did not exhibit significant phylogenetic signal). Nonetheless, the potential for evolutionary response in CTmax might not be sufficient to absorb the rapid warming that is predicted to impact the humid lowland tropics . While all species evaluated here experienced the same (or very similar) thermal regime prior to measurements of CTmax and CTmin, our measures relate to thermal limits under field conditions and are likely influenced by both plasticity and adaptation.
We observed notable interspecific variation in both CTmax and CTmin for all families, and this trait variation was associated with body size and phylogenetic relatedness among taxa. Body size had a positive and significant effect on CTmax. Conversely, body size had a negative and significant effect on CTmin. When considering body size as a covariate, tree frogs (Hylidae) and microhylid frogs (Microhylidae) tolerated warmer temperatures than other taxa. In contrast, direct-developing frogs in the Strabomantidae family appear to be at highest risk of thermal stress. Likewise, in Central America, terrestrial breeding frogs in the Craugastoridae family (which according to some authors includes all species in the Strabomantidae clade) exhibit relatively low CTmax and are at risk of thermal stress . Thus, given that converted habitats experience warmer temperatures and broader temperature fluctuations than continuous forest habitat, both groups of terrestrial breeding frogs are susceptible to habitat conversion. This is particularly concerning because both frog families, along with three other families belong to a diverse amphibian clade (Terraranae) containing over 1,065 named species .
One important consideration is that CTmax and CTmin are physiological variables with different ecological implications and, as such, temperatures approaching CTmin or CTmax have different effects on the activity and survival of organisms. In most ectothermic vertebrates, the lower thermal limit is closely linked to behavior, and individuals experiencing temperatures below CTmin may experience inactivity but not necessarily death . In contrast, the upper thermal limit is closely linked to survival and temperatures exceeding CTmax may result in death . As a result, the interpretation of thermal breadth should be viewed in light of the potential effect of CTmax, which anticipates physiological collapse (i.e., death) at one extreme, and the potential effect of CTmin, which encompasses a broader range of physiological mechanisms (e.g., metabolic downregulation, behavioral impairment, physiological collapse) at the other extreme. In this context, it is not necessarily surprising that CTmin is generally more labile than CTmax in some clades (e.g., [8, 10]).
Our data suggest that most lowland frog species are not likely to experience critical temperatures as a consequence of modest increases in temperature. Specifically, our comparisons of CTmax vs. a hypothetical 3°C temperature increase (Fig 1) suggested that 4% of lowland rainforest frogs assessed will experience temperatures exceeding their CTmax, whereas 25% might be moderately affected and 70% are unlikely to experience pronounced heat stress. Thus, we predict that most frog species living in continuous, lowland Amazonian forests should be able to tolerate predicted temperature increases. Nonetheless, measuring critical thermal limits at a set temperature does not allow estimation of reaction norms and plasticity of thermal traits within and across species, which are likely to play an important role in species’ response to climatic conditions.
We used CTmax and CTmin to estimate thermal breadth and infer species’ potential to respond to abrupt changes in temperature, including cooling events such as the cold surges that take place in western Amazonia during the Austral winter. To our knowledge, the lowest ever recorded minimum temperature in Madre de Dios region is 4.5°C, measured in Puerto Maldonado during a cold front in July 1975 . During such extreme cold front, air temperatures remained below 8°C for five days . Only 10 out of 37 frog species we studied (27%) had CTmin values around or below 8°C, suggesting that most species (75%) might need to adjust their behavior (e.g., move to lower forest strata, seek thermal refugia in the leaf litter or underground retreat sites) to cope with lower temperatures.
Thermal ecology data from tropical lowland amphibians and other tropical ectotherms continue to be extremely limited . To date, most macroecological models using thermal physiology [4, 12–14] have used data that were primarily collected between the 1960’s and the 1980’s, and were heavily biased towards temperate taxa. Additionally, numerous studies that use macroclimatic data (e.g., WorldClim bioclimatic variables ) and species distribution modeling to infer species’ responses to climate change (e.g., ) have assumed that species within a given elevation share similar realized niches and might also share similar critical thermal limits. As a consequence, it is assumed that species need to track changes in their environment in order to survive. Many studies using these approaches do not take into account empirical data on species’ critical thermal traits. Given that tropical rainforests contain the most diverse organismal communities on Earth, we need more primary data on species thermal physiology to improve our assessment of species’ vulnerability to climate change. Additionally, further studies should also consider the effect of reduced moisture and water availability, which are major determinants of frog activity and fitness .
A widely held assumption is that organisms living in the same area share similar climatic niches. However, using a phylogenetic framework, our study documents high variability in tolerance to both heat and cold among closely related species living in sympatry. We examined the variation of tolerance to heat and cold in lowland Amazonian rainforest frogs to test if these thermal physiological traits are phylogenetically conserved or labile. Knowing how quickly thermal physiological traits evolved can be used to improve predictions on species’ potential to respond to novel climates. We observed notable interspecific variation in both tolerance to heat and cold, and this trait variation was associated with body size and phylogenetic relatedness among taxa. Our data suggested that thermal physiological traits in lowland frogs are evolutionarily labile and exhibit similar rates of thermal physiological change. Yet, CTmax and CTmin are physiological variables with different evolutionary implications in relation to climate, and it remains unclear how much variation in CTmax is adaptive. We also found that key life history traits have potentially different effect on CTmax and CTmin. Lastly, our data suggest that most lowland frog species are not likely to experience body temperatures exceeding their critical temperature maxima under a hypothetical warming scenario of 3°C increase in air temperature.
S1 File. Relationship between body size and critical thermal limits.
S2 File. Further methodological details on molecular phylogenetic analysis.
S1 Table. Results from phylogenetic generalized linear regression models to determine which factors best predict variation in CTmax.
Model fitting was done with the full dataset (50 species). Bold font indicates significant values. SVL = snout-vent length, BMI = body mass index, midpoint = elevational midpoint, Height = median height above the ground.
S2 Table. Results from phylogenetic generalized linear regression models to determine which factors best predict variation in CTmin.
Model fitting was done with the reduced dataset (37 species). Bold font indicates significant values. SVL = snout-vent length, BMI = body mass index, midpoint = elevational midpoint, Height = median height above the ground.
S1 Fig. Scatterplots showing the relationship between CTmax and SVL.
At the intraspecific level, CTmax was not correlated with body size in all species tested except Noblella myrmecoides.
S2 Fig. Scatterplots showing the relationship between CTmin and SVL.
At the intraspecific level, CTmin was not correlated with body size.
S3 Fig. Scatterplots showing the relationship between CTmax and mass.
At the intraspecific level, CTmax was not correlated with body mass in most species tested.
S4 Fig. Scatterplots showing the relationship between CTmin and mass.
At the intraspecific level, CTmin was not correlated with body mass in most species tested.
S5 Fig. Pairwise scatterplot matrix displaying the relationship between relevant pairs of variables measured in this study.
S6 Fig. Daily temperature data.
Daily temperatures recorded from 16 November 2016 to 5 December 2017 (385 days) in two forest types at Los Amigos Biological Station, Peru. Weather station data are shown in gray; temperature data collected in the leaf litter are shown in green (floodplain forest) and blue (terra firme forest). In each case, the maximum and minimum temperatures delimited the polygons and the line in the middle represents the mean temperature.
S1 Appendix. Data set analyzed in this study.
S2 Appendix. Voucher numbers and GenBank accession numbers for the taxa and genes sampled in this study.
Permits were issued by the administration of Manu National Park (N° 06-2013-SERNANP-PNM-JEF) and the Servicio Nacional Forestal y de Fauna Silvestre (N° 27 C/C-2007-INRENA-IANP, 49 C/C-2007-INRENA-IANP, 11-2008-INRENA-IFFS-DCB, 120-2012-AG-DGFFS-DGEFFS, 064-2013-AG-DGFFS-DGEFFS, 292-2014-AG-DGFFS-DGEFFS, R.D.G. No 029-2016-SERFOR-DGGSPFFS, R.D.G. 405-2016-SERFOR-DGGSPFFS, R.D.G. 116-2017-SERFOR-DGGSPFFS, and Contrato de Acceso Marco a Recursos Genéticos, N° 359-2013-MINAGRI-DGFFS-DGEFFS). Use of vertebrate animals was approved by the Animal Care and Use committees of the University of California (ACUC #R278-0412, R278-0413, and R278-0314), the University of Michigan (PRO00008306), Florida International University (IACUC #18–009), and Southern Illinois University (IACUC #13–027 and 14–011). We thank J.C. Cusi, park rangers, students and colleagues who assisted in fieldwork. AC thanks the Amazon Center for Environmental Education and Research for support during field courses. We thank members of the Moritz, Wake, Rabosky, and Davis Rabosky labs for providing helpful comments and suggestions.
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