Skip to main content
Proceedings of the Royal Society B: Biological Sciences logoLink to Proceedings of the Royal Society B: Biological Sciences
. 2021 Apr 7;288(1948):20210032. doi: 10.1098/rspb.2021.0032

Habitat loss, predation pressure and episodic heat-shocks interact to impact arthropods and photosynthetic functioning of microecosystems

Adam J Vanbergen 1,3,, Claire Boissieres 2, Alan Gray 3, Daniel S Chapman 3,4
PMCID: PMC8059533  PMID: 33823665

Abstract

Ecosystems face multiple, potentially interacting, anthropogenic pressures that can modify biodiversity and ecosystem functioning. Using a bryophyte–microarthropod microecosystem we tested the combined effects of habitat loss, episodic heat-shocks and an introduced non-native apex predator on ecosystem function (chlorophyll fluorescence as an indicator of photosystem II function) and microarthropod communities (abundance and body size). The photosynthetic function was degraded by the sequence of heat-shock episodes, but unaffected by microecosystem patch size or top-down pressure from the introduced predator. In small microecosystem patches without the non-native predator, Acari abundance decreased with heat-shock frequency, while Collembola abundance increased. These trends disappeared in larger microecosystem patches or when predators were introduced, although Acari abundance was lower in large patches that underwent heat-shocks and were exposed to the predator. Mean assemblage body length (Collembola) was reduced independently in small microecosystem patches and with greater heat-shock frequency. Our experimental simulation of episodic heatwaves, habitat loss and non-native predation pressure in microecosystems produced evidence of individual and potentially synergistic and antagonistic effects on ecosystem function and microarthropod communities. Such complex outcomes of interactions between multiple stressors need to be considered when assessing anthropogenic risks for biota and ecosystem functioning.

Keywords: photosystem disruption, microarthropod abundance, apex predator, ecosystem heating, mesocosm, body size

1. Introduction

Global biodiversity is undergoing an extinction crisis with declines in the diversity, occurrence and abundance of multiple plant and animal taxa [14]. These changes to life on Earth are being driven by multiple anthropogenic pressures (e.g. climate change, habitat loss and degradation, spread of invasive species) [1,4,5] that are, individually or in combination [68], profoundly disrupting the biotic communities and ecosystem functions supporting human wellbeing [1,4,9].

Among these pressures, climate change is advancing and becoming one of the pre-eminent direct drivers of anthropogenic changes to the natural world [1,9]. Climate change projections anticipate a rise in land temperature extremes with extreme hot days in mid-latitudes being 3–4°C above current global mean surface temperature and an increased frequency and duration of heatwaves in most terrestrial regions [9]. Such a climate shift is expected to have major impacts on species distribution, abundance and diversity and the ecological interactions maintaining ecosystem function [1,10,11]. Climate change is also likely to result in phenotypic shifts and altered selection pressure on ecological and physiological traits. For example, as a consequence of metabolic costs versus energetic gains [12,13], extremes of high temperature may elicit fundamental changes to organism body size, e.g. shrinkage versus increase [1416] or reproductive capacity [17,18]. Although data on the generality of such effects is lacking [19,20], should they occur then the consequences for an organism's survival and functional role would be profound.

Habitat loss is a common feature of land use change or land management intensification that modifies and degrades the functioning of biotic communities and processes at multiple scales [1,21,22]. Climate change is expected to interact with habitat loss to affect biota, potentially by edge effects modifying the temperature within remaining habitat patches [23,24] or by reducing the capacity for compensatory migration and elevating extinction likelihoods by altering population connectivity, microclimate, niche space or trophic interactions [1,7,25,26]. At a global scale, the negative effects of habitat loss have been shown to be exacerbated in geographical areas with the highest maximum temperatures [27], which raises the possibility of synergistic interactions between habitat loss and climate change [9] that further increase rates of biodiversity loss [1,25].

Invasive alien species are another historic and expanding driver of change in biodiversity [1,5,28]. Anthropogenic species introductions into novel habitats have tended to disrupt native biodiversity and ecosystem functions because species within the recipient community lack a coevolutionary history with the invader and hence the necessary adaptations enabling species coexistence [5,28]. Predators exert strong, top-down regulatory pressure on prey populations that can affect communities and functions [2933]. Among invasive alien species, predators tend to have the greatest impacts, compared to other functional groups, on recipient native communities, particularly in small island ecosystems where prey may experience greater predator encounter rates [5,34]. Moreover, there is evidence that predation pressure can interact with changes in habitat area [35] or environmental temperature [36,37] to modify top-down control of lower trophic levels.

Experiments on model microecosystems are one approach to understand the interplay of multiple global change drivers affecting biodiversity and ecosystem processes [18]. Bryophyte microecosystems are amenable to experimentation because, in addition to the primary producers, they support a community of microarthropods (e.g. Acari, Collembola ≤ 5 mm body length) spanning multiple trophic levels (fungivore, detritivore, predator) that individually operate at very fine spatial scales [38,39]. Such microecosystems allow the controlled manipulation of anthropogenic drivers (e.g. temperature flux, habitat loss, risk of predation) and easier observation of resultant biotic and ecosystem impacts than in larger-scale and more complex ecosystems [31,4042].

We used a microecosystem experiment to test the individual and combined effects of habitat loss, episodic extreme heat-shock and extreme predation pressure (simulating the introduction of a non-native apex predator) on an ecosystem function (bryophyte chlorophyll fluorescence) and microarthropod communities (abundance, density and body size). We tested three hypotheses (H1–H3) that explore the potential interactive effects of these episodic heat-shocks, introduced predation pressure and habitat loss.

  • H1: larger microecosystem patches are more resilient to episodic heat extremes because their greater surface area to edge ratio or provision of more microclimatic niches mitigates the effects of environmental heating on photosynthetic function [23,4345] or microarthropod communities [15,16,40,41]. We, therefore, expected effects of heat-shock episodes to elicit a greater reduction of chlorophyll fluorescence, microarthropod abundance/density and mean body size in the small microecosystem patches.

  • H2: top-down pressure from an introduced apex predator would be reduced in larger ecosystem patches that offer prey species more physical refugia from predator attack [5,35]. We, therefore, expected that greatly elevated predation pressure from the introduction of a voracious generalist predator (Dalotia coriaria Kraatz, Staphylinidae) lacking a shared coevolutionary history with the microarthropod prey populations would interact with patch size [35] to reduce prey abundance or densities most severely in smaller ecosystem patches.

  • H3: the negative effects of extreme heat-shocks, habitat loss and elevated top-down pressure from an introduced apex predator would interact synergistically [24,26,36,37] to compound the reductions in microarthropod abundance, densities and body size.

2. Material and methods

(a). Microecosystem

Ninety-six experimental replicates comprising a bryophyte microecosystem supporting Acari and Collembola communities [40,41] were randomly excised (21 June 2017) using domestic steel circular cookie cutters (110 mm or 50 mm diameter giving microcosms of 95 cm2 and 20 cm2, respectively) from a large, continuous bryophyte sward (Mnium hornum Hedw. + rare occurrences of Polytrichastrum formosum (Hedw.) G.L. Smith; Hypnum andoi A.J.E. Smith) on a brown earth soil in a woodland (Bush Estate, Scotland, UK: Latitude 55.861111, Longitude −3.205833, electronic supplementary material, figures S1 and S2). Each replicate was immediately placed into an individual plastic container (15 cm diameter, 5 cm height) capped by horticultural fleece (electronic supplementary material, figure S3). This fleece enclosed the microcosm and prevented invertebrate migration, but was sufficiently permeable to ensure aeration, the transmission of photosynthetic active radiation for bryophyte photosynthesis and to allow sprays of misted water to penetrate and maintain the moistness of the moss microecosystem within.

(b). Experimental design

The microecosystem experiment was carried out at the UK Centre for Ecology and Hydrology (UKCEH) Edinburgh (Latitude 55.861111, Longitude −3.205833, electronic supplementary material, figures S1 and S2) over eight weeks (21 June to 11 August 2017). We employed a randomized factorial blocked design with three treatments: (i) microecosystem size (95 cm2, n = 48; 20 cm2, n = 48); (ii) frequency of heat-shock episodes (‘unstressed’ controls: n = 32; two episodes: n = 32; three episodes: n = 32); and (iii) addition of an apex predator (present n = 48 or control, n = 48). We assigned the 96 microecosystems randomly to eight blocks (large plastic trays 100 cm × 50 cm × 16 cm) ensuring each contained a full replicate of the treatment combinations. These were placed outdoors 400 m from the source habitat (electronic supplementary material, figure S2) in a location shaded by trees and buildings. They were situated beneath plastic-covered aluminium mesh workbenches (electronic supplementary material, figure S3) to prevent flooding by rainfall, but otherwise exposed to ambient air movements and temperature (2017: June = 7.9–17.2°C; July = 11.5–19.1°C; August = 11.4–18.9°C). To keep the moss microecosystem replicates moist they were watered with a fine spray every 24 or 48 h depending on warm weather and immediately after experimental heat-shock episodes (see below) to aid ecosystem recovery.

(c). Apex predator treatment

To apply a high level of apex predator pressure in the microecosystem simulating that occurring with a non-native species invasion, we introduced a staphylinid beetle known to be an obligate and voracious generalist predator of soil invertebrates [46,47]. Dalotia (syn. Atheta) coriaria Kraatz (Staphylinidae) (electronic supplementary material, figure S4c) is a soil-dwelling predator used for commercial biocontrol because of its efficacy as a generalist predator [46]. It is considerably larger (3–4 mm body length) than most adult and juvenile microarthropods (approx. 0.5–5 mm), and it actively hunts and readily consumes eggs, juvenile or adult stages of many invertebrate orders [4648]. Dalotia coriaria was a good analogue of an invasive non-native predator because, although commercially supplied for glasshouse biocontrol, it is not known to naturally occur in Scotland, aside from a single 2003 record (UK National Biodiversity Atlas: Latitude 57.62525 Longitude –4.11732, Highland region) far from the study location and probably a glasshouse escape. Accordingly, D. coriaria lacks a coevolutionary history with the microarthropod fauna of these bryophyte microecosystems, a typical feature explaining the disproportionate impact of invasive non-native predators [5]. Under laboratory conditions, the D. coriaria lifespan is 47–60 days for females and males, respectively [49]. Replicates in the predator treatment were inoculated with a single D. coriaria (sourced from AGRALAN Ltd, https://www.agralan.co.uk/) at the onset of the experiment and following each heat-shock episode to maintain a consistently high level of introduced predation pressure (i.e. at least one surviving D. coriaria in the microecosystem). Given the area of the microecosystems (large = 95 cm2; small = 20 cm2) deployed in this experiment, the application of a single D. coriaria beetle per microcosm approximated to a 100- or 500-fold uplift of predation pressure relative to the biocontrol prescription (a single individual per m2 is estimated to consume 10–20 prey items per day—https://www.evergreengrowers.com/atheta-coriaria-8183.html). Coupled to the lack of a coevolutionary history between the apex predator and its prey, this large uplift in potential top-down pressure again mimics the disproportionate impact of a novel alien predator on recipient native communities.

(d). Episodic heat-shock treatment

Intergovernmental Panel on Climate Change (IPCC) observations and models show climate change is heating terrestrial environments worldwide [9]. In the UK, the latest climate projections anticipate that compared to the 1980–2000 baseline mean summer temperatures in central Scotland for 2060–2079 will be warmer by 0.1–2.8°C for low (IPCC Representative Concentration Pathway (RCP) 2.6) or by 0.6–4.8°C for high (IPCC RCP8.5) emission scenarios (UK Climate Projections, UKCP18, www.metoffice.gov.uk). These projections mean a potential raise in mean summer temperatures in Edinburgh by mid-end of the twenty-first century (1981–2010/RCP2.6/RCP8.5: June = 16.9/19.7/21.7°C; July = 18.8/21.6/23.6°C; August = 18.3/21.1/23.1°C). Extreme weather events, e.g. heat waves are projected to increase in frequency and strength [9]. During the late twentieth and early twenty-first centuries, high temperatures have been recorded in eastern Scotland by the UK meteorological office (www.metoffice.gov.uk) during heatwaves (30.8°C Leuchars, Fife, 2 August 1990; 31.4°C Edinburgh Airport, 4 August 1975; 32.9°C Greycrook, Borders, 9 August 2003).

We challenged the microecosystem replicates with experimental episodic heat-shocks (see below) to simulate short duration heat-waves. Replicates were randomly assigned to acute heat-shock episodes of 2 h duration on two or three occasions during the experiment or to a control (no heat-shock applied). We applied the experimental heat-shock treatment by temporarily and carefully removing the replicate microecosystems from their plastic containers and exposing them for 2 h beneath 40 W light bulbs set within racks of 54 Tullgren extraction funnels (Burkard Scientific Ltd, electronic supplementary material, figure S4a). These extract microarthropods (electronic supplementary material, figure S4b) from soil or litter by producing a temperature gradient and exploiting the behavioural response of microarthropods to descend into the soil or vegetation away from the heat source, where ultimately (if heating is protracted) they fall through the funnel to be collected and preserved in an alcohol containing vessel (70%). Between 2 h heat-shock episodes, we watered the replicates (see above) and left a period of 13 days to allow recovery of the moss microecosystem.

We performed a verification experiment to check that the microecosystem temperature attained under the experimental heat-shock treatments was field realistic given IPCC projections [9] and recorded heatwaves (see above). A 2 h heat-shock raised the mean (±s.e.) surface temperature of the microecosystem (n = 12 of each size class) from the ambient state (i.e. immediately prior to heating treatment: large = 17.9°C ± 0.08; small = 18.1 ± 0.12) to a level of temperature (end of 2 h heat-shock episode: large = 26.5°C ± 0.16; small = 29.5°C ± 0.91). This is greater than RCP8.5 projections of mean summer temperature, but below episodic heatwave temperatures recorded during recent decades (see above examples). Accordingly, we regarded the experimental heat-shock treatments as plausible and commensurate with projected climate change conditions in Scotland under the high emission RCP8.5 scenario [9].

(e). Microarthropod abundance and body size

All replicates were subjected to a final protracted heating of 24 h duration, an intensity of heat stress that destroyed the moss microecosystem and produced a total extraction of the remaining invertebrate fauna from every treatment. Following the 24 h destructive harvest, we sorted and counted all invertebrates collected to the level of the taxonomic subclass (Acari, Collembola) to provide an estimate of community size (total abundance and density per cm2) for the microecosystem. These two measures of population size give complementary information. Total abundance provided information on the potential carrying capacity of large and small microecosystem patches and how that interacted with the heating and predator treatments; whereas, community density informed on the effect of heating and predation on population size controlling for the influence of variation in habitat area. In addition to the 24 h destructive harvest, we also measured the body length (frons to end of abdomen) of subsamples of Collembola individuals extracted from each large or small microecosystem following application of each heat-shock (t1/t2/t3) treatment (Leica DM12.5 microscope, DFC290 camera and Leica Application Suite v. 3.0). Averaging across these temporal subsamples we estimated the mean body length for the Collembola assemblage for each microecosystem (n = 62, excluding unshocked controls) following a total frequency of two or three extreme heat-shocks.

(f). Chlorophyll fluorescence as an indicator of ecosystem function

To test the impact of the heat-shocks on microecosystem function over the experiment we quantified moss community chlorophyll fluorescence, as an indicator of photosynthetic capacity (photosystem II (PSII) function). We used a Continuous Excitation Chlorophyll Fluorimeter (HandyPEA, Hansatech Instruments Ltd, UK) on randomly selected bryophyte leaves from each microecosystem, each leaf was dark adapted for 20 min, prior to measurements at a photosynthetic photon flux density of 1500 µmol m−2 s−1. The rate of chlorophyll fluorescence (Fv/Fm) is calculated as

FvFm=FmFoFm, 2.1

where Fv is variable fluorescence, Fm is the maximum and Fo is the minimum rate of chlorophyll fluorescence. Fv/Fm is a normalized ratio that works on the principle that the ratio between variable florescence (Fv) and maximal florescence (Fm) approximates the maximum quantum yield of the photosystem (PSII), ranging between 0.75 and 0.84 in healthy mosses [44,50,51], with lower values indicating stress [52]. Chlorophyll fluorescence was measured in all hydrated replicates immediately prior to and following heat-shock episodes. Controls corresponded to the unstressed baseline chlorophyll fluorescence ratio (Fv/Fm) measured in all replicates per block in the unshocked state and was assumed to be unchanged over the short duration of the 2 h shock episode (based on a preliminary trial see the electronic supplementary material, figure S5).

(g). Statistical analysis

Data were modelled using linear mixed models (LMM) and generalized linear mixed models (GLMM) implemented in R (lme4 function lmer/glmer). The response of microecosystem function (chlorophyll fluorescence) was modelled as the natural log (ln) transformed difference in chlorophyll fluorescence (ln Fvt1 − ln Fvt0) measured immediately before (t0) and following (t1) each shock treatment (heat-shock controls = mean of all replicates in unshocked state immediately prior to onset of treatment). Modelling differential chlorophyll fluorescence (pre- and post-heat-shock) indicated if the microecosystem was able to maintain its photosynthetic function (no change in ln Fvt1 − ln Fvt0) or was degraded (negative value) or stimulated (positive value) by the heat-shock episodes. We tested with a LMM the sequential effect of heating episodes on differential chlorophyll fluorescence (ln Fvt1 − ln Fvt0). Fixed effects fitted were: (i) microecosystem patch size (large or small), (ii) apex predator (+ or −), (iii) the heat-shock episode (1, 2 or 3), and (iv) their two-way interactions.

We verified that the handling of the microcosms did not greatly affect the size of the ecosystem by establishing at the conclusion of the experiment a strong positive relationship between the excised microecosystem patch size (area) and the total mass (LMM estimate = 0.69, t96 = 19.90, p < 0.001), soil mass (LMM estimate = 0.67, t96 = 18.98, p < 0.001) and moss biomass (LMM estimate = 0.78, t96 = 17.43, p < 0.001) measured per microecosystem.

GLMMs (function glmer) of microarthropod abundance following the final heat-shock treatment (24 h duration) were fitted to both Acari and Collembola counts of individuals per microecosystem (Poisson models with log link) and densities per cm2 (Gaussian models with identity link on ln + 1-transformed densities). For Collembola body size, the ln-transformed mean community body length was analysed with a similar GLMM (Gaussian model with identity link). Fixed effects for all models were: (i) microecosystem patch size (large or small), (ii) apex predator (+ or −), (iii) frequency of heat-shock episodes (0, 2 or 3 events of 2 h duration), and (iv) their two-way and three-way interactions.

All models were fitted using maximum likelihood (Laplace approximation) and we report the best fitting model (lowest Akaike information criterion for small sample size (AICc)) from all subsets model comparisons performed using the MuMIn R package. Models fitted experimental block (n = 8) as a random effect, while a second random term of ‘microecosystem identity’ was fitted to the chlorophyll fluorescence LMM to account for the repeated measures at the replicate level (n observations = 192 over 96 replicates). As a feature of the experimental design, these random effects were retained even when attributable variance was near zero. Statistical significance was assessed with p-values (α = 0.05) based on asymptotic Wald tests (P) for Poisson models and following Satterthwaite's method (function ‘lmerModLmerTest’) for Gaussian models (microecosystem chlorophyll fluorescence, microarthropod densities, Collembola body size).

3. Results

(a). Microecosystem photosynthetic capacity

Chlorophyll fluorescence (Fv/Fm) was consistently and negatively affected by episodic heat-shocks to the microecosystem patches. Relative to unshocked control measurements (range 0.75–0.84 indicates normal function), the mean chlorophyll fluorescence ratio was progressively reduced in microecosystems with the sequence of heat-shocks (figure 1a). This was confirmed by the best model of differential chlorophyll fluorescence (ln Fvt1 – ln Fvt0) over the sequence of heat-shocks (figure 1b; heat-shock 1: t184 = −3.237, p = 0.001; heat-shock 2: t184 = −9.187, p < 0.001; heat-shock 3: t184 = −12.077, p ≤ 0.001), indicating a degradation of this microecosystem photosynthetic function.

Figure 1.

Figure 1.

The effect of a series of episodic heat-shocks on microecosystem photosynthetic function (chlorophyll fluorescence). (a) The mean ratio of chlorophyll fluorescence (Fv/Fm: the maximum quantum yield of PSII ranges from 0.75 to 0.84 in healthy mosses and indicated by the dotted line) measured before (t0) and following (t1) heat-shock treatments, and (b) the difference in chlorophyll fluorescence rate (ln Fvt1 − ln Fvt0) across heating episodes (0/1/2/3) and microecosystem patch sizes (large: 95 cm2, small: 20 cm2). Differential chlorophyll fluorescence indicated unperturbed (no change), degraded (negative value) or stimulated (positive value) photosynthetic function. Data in (a) are raw, untransformed means (±s.e.) of chlorophyll fluorescence ratios, and (b) marginal means (±s.e.) of the difference in chlorophyll fluorescence derived from the final LMM accounting for other model terms. Controls (open square) corresponded to the unstressed baseline ratio (Fv/Fm) derived by measuring chlorophyll fluorescence of all replicates per block in the unshocked state and were assumed to remain stable (crossed open square) over the duration of the 2 h shock episode applied to other replicates (see the electronic supplementary material).

The rate of differential chlorophyll fluorescence over the sequence of shocks was unaffected by the main effects of microecosystem patch size (estimate: −0.081 ± 0.134, t184 = −1.115, p = 0.266) and non-native predator presence (estimate: −0.062 ± 0.073, t184 = −0.851, p = 0.396). Moreover, contrary to our hypothesis (H1), the microecosystem patch size did not modulate the effect of sequential heat-shocks on differential chlorophyll fluorescence as shown by the lack of a statistical interaction (figure 1b; ecosystem size × heat-shock 1: −0.042 ± 0.215, t184 = −0.194 p = 0.846; ecosystem size × heat-shock 2: −0.252 ± 0.215, t184 = −1.172, p = 0.243; ecosystem size × heat-shock 3: 0.101 ± 0.248, t184 = 0.407, p = 0.684).

(b). Microarthropod abundance, density and body size

All subsets model comparison for GLMMs (AICc) for an abundance of both microarthropod taxa (Collembola and Acari) retained all main effects and their two and three-way interactions (tables 1 and 2). The clearest interpretation of these complex results comes from considering the higher-order three-way interactions between the experimental treatments. Although reduced microecosystem patch size negatively influenced microarthropod abundance, there was a complex interplay with heat-shock and predator treatments (figure 2, tables 1 and 2). In small microecosystem patches without the non-native predator, Acari suffered a progressive decrease in abundance with heat-shock frequency, while Collembola abundance tended to increase (figure 2). These trends were not generally evident in larger microecosystem patches or when predators were introduced, although Acari abundance was reduced in large patches that underwent heat-shocks and were exposed to the non-native predator (figure 2).

Table 1.

GLMM for Acari abundance responses to experimental treatments and their interactions. (All subsets model comparison based on AICc was used to determine the best set of fixed effects from the global model (R package MuMIN: function ‘dredge’, Akaike weight of presented model = 1). n = 96 microecosystems arrayed in eight blocks. Experimental block fitted as a random effect. Level of statistical significance α = 0.05.)

predictor of Acari abundance estimate ± s.e. z p
intercept 5.64 ± 0.135 41.76 <0.001
apex predator (+) 0.539 ± 0.026 21.05 <0.001
microecosystem size(small) −1.620 ± 0.050 −32.37 <0.001
heat-shock frequency (0/2/3)
 two episodes 0.044 ± 0.028 1.537 0.124
 three episodes −0.064 ± 0.029 −2.192 0.028
apex predator × heat-shock frequency (two episodes) −0.616 ± 0.038 −16.01 <0.001
apex predator × heat-shock frequency (three episodes) −0.563 ± 0.039 −14.32 <0.001
apex predator × microecosystem size (small) −0.379 ± 0.067 −5.628 0.001
microecosystem size (small) × heat-shock frequency (two episodes) −0.095 ± 0.071 −1.333 0.182
microecosystem size (small) × heat-shock frequency (three episodes) −0.077 ± 0.073 −1.055 0.291
appex predator × microecosystem size (small) × heat-shock frequency (two episodes) 0.610 ± 0.097 6.283 0.001
apex predator × microecosystem size (small) × heat-shock frequency (three episodes) 0.685 ± 0.098 6.973 0.001

Table 2.

GLMM for Collembola abundance responses to experimental treatments and their interactions. (All subsets model comparison based on AICc was used to determine the best set of fixed effects from the global model (R package MuMIN: function ‘dredge’, Akaike weight of presented model = 1). n = 96 microecosystems arrayed in eight blocks. Experimental block fitted as a random effect. Level of statistical significance α = 0.05.)

predictor of Collembola abundance estimate ± s.e. z p
intercept 4.554 ± 0.109 41.94 <0.001
apex predator (+) 0.244 ± 0.047 5.141 <0.001
microecosystem size(small) −1.621 ± 0.087 −18.56 <0.001
heat-shock frequency (0/2/3)
 two episodes 0.126 ± 0.049 2.598 0.009
 three episodes 0.061 ± 0.049 1.236 0.217
apex predator × heat-shock frequency (two episodes) −0.592 ± 0.070 −8.434 <0.001
apex predator × heat-shock frequency (three episodes) −0.155 ± 0.067 −2.310 0.021
apex predator × microecosystem size (small) −0.410 ± 0.127 −3.225 0.001
microecosystem size (small) × heat-shock frequency (two episodes) −0.862 ± 0.147 −5.627 <0.001
microecosystem size (small) × heat-shock frequency (three episodes) −0.617 ± 0.141 −4.376 <0.001
apex predator × microecosystem size (small) × heat-shock frequency (two episodes) 1.155 ± 0.201 5.757 <0.001
apex predator × microecosystem size (small) × heat-shock frequency (three episodes) −0.020 ± 0.212 −0.093 0.926

Figure 2.

Figure 2.

Microarthropod (Acari, Collembola) abundance for different experimental levels of microecosystem patch size (large: 95 cm2, small: 20 cm2), non-native apex predator presence and frequency of 2 h heat-shock episodes. Boxplots show the medians, interquartile ranges (IQRs) and whiskers (values up to 1.5 IQRs from the box). For effect significances see tables 1 and 2.

Another notable pattern to emerge from this experiment was that two-way interactions between treatments always produced negative effects on microarthropod abundance, yet considering the full interplay between all three treatments produced more heterogeneous outcomes with either positive or negative effects on abundance (tables 1 and 2).

Although the response of microarthropod density to the experimental treatments showed similar trends (electronic supplementary material, figure S6), the best subset of models for density retained only a negative effect of microecosystem patch size on Collembola density (estimate = −0.244, t88 = −3.584, p < 0.001). This disparity with the abundance models probably resulted from density removing the strong effect of microecosystem patch size on abundance (tables 1 and 2, figure 2) and as a consequence obscuring other trends in the data.

The mean Collembola body size of the individuals measured in the temporal subsamples obtained following heat-shock applications (t1/t2/t3) was 0.95 mm ± 0.62 s.d. ranging from 0.21 to 2.3 mm. The GLMM best subsets model comparison for log-transformed Collembola assemblage mean body size retained the negative main effects of higher shock frequency (estimate = −0.172, t54.3 = −2.966, p < 0.01) and small microecosystem patch size (estimate = −0.253, t54.4 = −4.418, p < 0.001) (figure 3), but eliminated on the basis of AICc effects of the introduced non-native predator and interactions between treatments. The drop in mean body size occurred following the first heat-shock episode (mean body size ± s.e. = 1.19 ± 0.09 mm) with no change between heat-shock 2 (0.79 ± 0.06 mm) and heat-shock 3 (0.81 ± 0.10 mm). Although the number of Collembola individuals available to be measured per time point varied between replicates (large: 3–88 individuals, mean ± s.d. = 20 ± 19; small: 2–32 individuals, mean ± s.d. = 11 ± 8), including this in the analysis by weighting the GLMM by number of individuals or including it as a fixed effect had no impact on the final model selected.

Figure 3.

Figure 3.

Collembola assemblage mean body size for different experimental levels of microecosystem patch size (large: 95 cm2, small: 20 cm2) and frequency of 2 h heat-shock episodes. Boxplots show the medians, interquartile ranges (IQRs) and whiskers (values up to 1.5 IQRs from the box). The GLMM analysis revealed only two statistically significant main effects (p < 0.01, see main text).

4. Discussion

The photosynthetic function (bryophyte chlorophyll fluorescence as an indicator of quantum yield of PSII) of these microecosystems was progressively reduced over the series of episodic heat-shocks, indicating a degradation of primary production capacity [50,51]. This finding is consistent with ecophysiological studies that have shown how high temperatures and desiccation affect chlorophyll α fluorescence to disrupt PSII and respiration [4345]. By repeatedly heating and desiccating the bryophyte tissues, the heat-shock treatments caused photosynthetic disruption, probably owing to a reduction in cell water content. Bryophytes possess the capacity to recover from repeated drying cycles and therefore can tolerate drought [51,53]. However, as a degree of cell degradation occurs in the immediate post-stress recovery period the severity, number and periodicity of stress events determine the degree of this cumulative effect [44]. Contrary to our first hypothesis (H1), however, we found that this direct reduction of microecosystem chlorophyll fluorescence by heat-shocks was not modulated by the size of the microecosystem patch (i.e. no interaction). Furthermore, there was no direct impact of the loss of habitat area (i.e. as a main effect) on photosynthetic function over this experimental timescale. This is in contrast to a habitat fragmentation study (c.f. habitat loss here) that reported effects on biogeochemical functions, e.g. C and N fluxes [31]. Here, the bryophyte community was dominated by a single species and it is possible that a more diverse community will have responded differently to the heat-shock episodes.

Although not a hypothesis a priori in our study, we found no indication that the non-native apex predator treatment affected photosynthetic function. Such an impact on photosynthesis could be postulated to occur via complex trophic interactions in the microarthropod food web [35,54], for example, if predation impacted on herbivores that have the potential to directly modulate plant photosynthesis by consuming leaf tissues or inducing shifts in resource allocation to defence [29,30]. Lacking data on the functional composition of the community meant that we could not test such a hypothesis. Accordingly, we are unable to determine whether the lack of a predator treatment effect on chlorophyll fluorescence was owing to the trophic effects being subtle, unmeasured or simply absent.

As hypothesized (H2 and H3), the interaction between episodic heat-shocks, predator presence and microecosystem size affected microarthropod abundance in complex and sometimes taxon-specific ways. In small microecosystem patches without the non-native predator, Acari decreased and Collembola increased in number in response to heat-shock frequency; whereas in large patches that underwent heat-shocks and were exposed to the non-native predator, Acari showed a tendency towards reduced abundance, while Collembola were unaffected. Future experiments should examine whether trophic interactions among microarthropod predators (e.g. Acari: Mesostigmata), detritivores and fungivores (e.g. Acari: Oribatidae, Collembola) or food web properties (e.g. modularity) affect the assemblage response to non-native apex predators and their interplay with other stressors [30,35,39,55].

Consistent with island biogeographic and metapopulation theory and evidence [22,40,42], the size of the microecosystem patch, and hence carrying capacity, was important in shaping the interaction with the heat-shock and non-native predator treatments that governed microarthropod abundance. This interaction reflected a meta-analysis showing how climate and habitat loss combine to alter species abundance or diversity [27]. It was also consistent with a previous bryophyte microecosystem experiment that revealed the interaction between environmental temperature and organism dispersal among habitat patches structured microarthropod communities [41]. Differences in ecological traits (e.g. body size, trophic position or functional group) shape an organism's perception of and sensitivity to environmental change [11,56,57]. We can, therefore, hypothesize that the contrasting total abundance responses of Acari and Collembola to the heat-shock × non-native predator × patch size interaction reflected responses by individual microarthropod species occupying different trophic positions (fungivore versus predator) or microhabitat niches [38,39] in the assemblage [41,58]. Time constraints meant we lacked the capacity to obtain the compositional data necessary to disentangle species or trait-based responses to the treatments. Moreover, our microecosystems were completely isolated so we cannot discern the influence of microecosystem connectivity and dispersal processes [21,31,40]. Future studies might examine the effect of multiple stressor interactions on microecosystems differing in patch fragmentation or isolation, but it should be noted that this is unlikely to modify heat-shock impacts that typically occur at a scale beyond the dispersal ability of many organisms.

Predators often exert substantive top-down pressure on prey populations [2933], but here compared to the heat-shock and patch size treatments, the presence of the non-native predator had a little overall effect. Predator presence, however, did interact with heat-shock frequency to reduce mite abundance in large patches, while in small patches the predator introduction dampened the impact of the heat-shock × patch size interaction. Predator–prey interactions under environmental heating are likely to be complex with the potential for direct or indirect trophic effects (e.g. cascades or mismatches) that affect ecological dynamics and functioning [33,54]. The cumulative effect of frequent heat-shocks may have had behavioural or physiological (e.g. reproductive capacity) impacts on microarthropods [17,18], which alongside shifts in predator foraging owing to elevated temperature or altered prey availability may have modified the top-down pressure. Further study of the compositional and predator–prey relationships would be needed to elucidate the precise mechanisms, but such an explanation is consistent with other experiments that have shown how predation pressure (mites, centipedes) on microarthropod prey is modified under elevated temperatures [33,36,59,60].

Although the pattern of microarthropod density responses to the three-way interaction of treatments mirrored that of total abundance, statistically there was little effect with only a negative effect of microecosystem patch size on Collembola density. Rather than invalidating the total abundance response, scaling microarthropod abundance (n individuals per cm2) to control for the influence of microecosystem area illustrated the pre-eminence of habitat loss in driving down population size and shaping interactions with other treatments. Indeed while Acari densities scaled linearly, Collembola reductions in density reveal that this taxon was disproportionately impacted by the smaller patch size. The dispersion of microarthropods within the microecosystem may have been altered in response to the treatments (e.g. aggregation in particular microhabitats to avoid predators or high temperatures). If so, this may have been reflected in the total abundance data in ways that were obscured once scaled to densities per unit area, which may have masked the signal of the interactive effects between treatments. Overall it is clear that the influence of microecosystem area on microarthropod abundance was crucial to understand the outcome of multi-stressor interactions for these communities [68,25,26].

Collembola assemblage mean body size was reduced by smaller microecosystem patch size and increased heat-shock frequency. This concurs with an earlier study that found an overall drop in mean body size of the collembolan species Folsomia candida with temperature treatments [54]. Although unlike Thakur et al. [54] and contrary to our hypotheses (H1 and H3), we found no evidence of treatment interactions or an effect of exposure to predation on mean assemblage body size. The observed reduction in mean body size may be a consequence of elevated temperature producing metabolic costs or mismatches for larger consumers [12,13]. Therefore, climate change may drive phenotypic plasticity or selection for smaller consumer body sizes [14,15], although this phenomenon remains to be well established [19,20]. Given the generation time of Collembola is about two to three weeks [61,62] it is possible that selection for smaller body size could have occurred during the experimental timespan (eight weeks). To confirm this would require an energetic and physiological analysis of the sampled individuals or assembling microcosms using laboratory populations of standardized body size [54] to monitor body size evolution over generations. An alternative, but not mutually exclusive, explanation is that in these systems closed to immigration, the heat-shock episodes eliminated the larger, more mobile individuals. This, coupled to the potential production of juveniles within our experimental timeframe [61,62], may explain the observed reduction in assemblage mean body size.

In conclusion, the experimental simulation of three major global change drivers (climate change, habitat loss and introduction of a ‘non-native’ predator) produced various individual and combined impacts on photosynthetic function (chlorophyll fluorescence) and microarthropod communities in a bryophyte microecosystem. The acute nature of the discrete heat-shock episodes were a major factor impacting both community chlorophyll fluorescence and consumer body size, but modified microarthropod abundance through complex interactions with microecosystem area and non-native predation pressure. This contrasts with the minimal or lack of an effect of chronic warming and drought in microarthropod communities [63] and highlights the potential risks from the cumulative effects on ecosystems from short-term pulse stressors, such as heatwaves predicted to increase in frequency and duration in the future [9]. A notable overall pattern emerging from the analysis of abundance was that two-way interactions between the different stressors (loss of microecosystem area/non-native apex predator/heat-shock frequency) were always negative. This implies that exposure to multiple stressors is potentially synergistic, i.e. disproportionately worse than would be predicted from their (main) effects in isolation [55]. However, accounting for the three-way interaction between the different stressors produced more positive than negative effects, suggesting stressors were antagonistically [55] affecting abundance via different mechanisms that had the effect of cancelling out the impact. This highlights the need to account for as much complexity as possible when assessing multi-stressor impacts on biodiversity in order to improve the accuracy of predicted impacts. This is important because the effects on biota of the interplay between multiple anthropogenic stressors is highly likely to be occurring in nature, but simultaneously remains poorly understood and relatively understudied [1,68].

Supplementary Material

Funding

We acknowledge the support of the post-graduate internship programme of L'Ecole Nationale Supérieure Agronomique de Toulouse (ENSAT), France, the UKCEH National Capability Resilience project and the ESREA project (ANER Bourgogne-Franche-Comté, France).

Data accessibility

This article has additional data available from the Dryad Digital Repository: https://doi.org/10.5061/dryad.kh1893259 [64].

Authors' contributions

A.J.V., A.G. and D.C. conceived the ideas and designed the experiment. C.B. performed the experiment and collected the data. A.J.V. and D.C. performed the statistical analysis and paper preparation. All authors contributed critically to the drafts and gave final approval for publication.

Competing interests

The authors declare no competing interests.

References

  • 1.IPBES. 2019. Summary for Policymakers of the Global Assessment Report of the Intergovernmental Science-Policy Platform on Biodiversity and Ecosystem Services Secretariat of the Intergovernmental Science-Policy Platform on Biodiversity and Ecosystem Services (eds S Díaz et al.), 56 pp. Bonn, Germany: IPBES Secretariat. ( 10.5281/zenodo.3553579) [DOI] [Google Scholar]
  • 2.Lister BC, Garcia A. 2018. Climate-driven declines in arthropod abundance restructure a rainforest food web. Proc. Natl Acad. Sci. USA 115, E10397. ( 10.1073/pnas.1722477115) [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 3.Seibold S, et al. 2019. Arthropod decline in grasslands and forests is associated with landscape-level drivers. Nature 574, 671-674. ( 10.1038/s41586-019-1684-3) [DOI] [PubMed] [Google Scholar]
  • 4.Díaz S, et al. 2019. Pervasive human-driven decline of life on Earth points to the need for transformative change. Science 366, eaax3100. ( 10.1126/science.aax3100) [DOI] [PubMed] [Google Scholar]
  • 5.Vanbergen AJ, Espíndola A, Aizen MA. 2018. Risks to pollinators and pollination from invasive alien species. Nat. Ecol. Evol. 2, 16-25. ( 10.1038/s41559-017-0412-3) [DOI] [PubMed] [Google Scholar]
  • 6.Bartlett LJ, Newbold T, Purves DW, Tittensor DP, Harfoot MBJ. 2016. Synergistic impacts of habitat loss and fragmentation on model ecosystems. Proc. R. Soc. B 283, 20161027. ( 10.1098/rspb.2016.1027) [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 7.Oliver TH, Morecroft MD. 2014. Interactions between climate change and land use change on biodiversity: attribution problems, risks, and opportunities. Wiley Interdiscip. Rev.-Clim. Change 5, 317-335. ( 10.1002/wcc.271) [DOI] [Google Scholar]
  • 8.Vanbergen AJ. 2013. The insect pollinators initiative. Threats to an ecosystem service: pressures on pollinators. Front. Ecol. Environ. 11, 251-259. ( 10.1890/120126) [DOI] [Google Scholar]
  • 9.IPCC. 2018. Summary for policymakers. In (ed. Masson-Delmotte V), p. 32. Geneva, Switzerland: World Meteorological Organization. [Google Scholar]
  • 10.Bokhorst S, Phoenix GK, Berg MP, Callaghan TV, Kirby-Lambert C, Bjerke JW. 2015. Climatic and biotic extreme events moderate long-term responses of above- and belowground sub-Arctic heathland communities to climate change. Glob. Change Biol. 21, 4063-4075. ( 10.1111/gcb.13007) [DOI] [PubMed] [Google Scholar]
  • 11.Lurgi M, Lopez BC, Montoya JM. 2012. Climate change impacts on body size and food web structure on mountain ecosystems. Phil. Trans. R. Soc. B 367, 3050-3057. ( 10.1098/rstb.2012.0239) [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 12.Lemoine NP, Burkepile DE. 2012. Temperature-induced mismatches between consumption and metabolism reduce consumer fitness. Ecology 93, 2483-2489. ( 10.1890/12-0375.1) [DOI] [PubMed] [Google Scholar]
  • 13.Brown JH, Gillooly JF, Allen AP, Savage VM, West GB. 2004. Toward a metabolic theory of ecology. Ecology 85, 1771-1789. ( 10.1890/03-9000) [DOI] [Google Scholar]
  • 14.Sheridan JA, Bickford D. 2011. Shrinking body size as an ecological response to climate change. Nat. Clim. Change 1, 401-406. ( 10.1038/nclimate1259) [DOI] [Google Scholar]
  • 15.Gardner JL, Peters A, Kearney MR, Joseph L, Heinsohn R. 2011. Declining body size: a third universal response to warming? Trends Ecol. Evol. 26, 285-291. ( 10.1016/j.tree.2011.03.005) [DOI] [PubMed] [Google Scholar]
  • 16.Horne CR, Hirst AG, Atkinson D. 2017. Seasonal body size reductions with warming covary with major body size gradients in arthropod species. Proc. R. Soc. B 284, 20170238. ( 10.1098/rspb.2017.0238) [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 17.Sales K, et al. 2018. Experimental heatwaves compromise sperm function and cause transgenerational damage in a model insect. Nat. Commun. 9, 4771. ( 10.1038/s41467-018-07273-z) [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 18.Beetge L, Krüger K. 2019. Drought and heat waves associated with climate change affect performance of the potato aphid Macrosiphum euphorbiae. Sci. Rep. 9, 3645. ( 10.1038/s41598-018-37493-8) [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 19.Siepielski AM, Morrissey MB, Carlson SM, Francis CD, Kingsolver JG, Whitney KD, Kruuk LEB. 2019. No evidence that warmer temperatures are associated with selection for smaller body sizes. Proc. R. Soc. B 286, 20191332. ( 10.1098/rspb.2019.1332) [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 20.Wilson RJ, Brooks SJ, Fenberg PB. 2019. The influence of ecological and life history factors on ectothermic temperature-size responses: analysis of three Lycaenidae butterflies (Lepidoptera). Ecol. Evol. 9, 10 305-10 316. ( 10.1002/ece3.5550) [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 21.Thompson PL, Rayfield B, Gonzalez A. 2017. Loss of habitat and connectivity erodes species diversity, ecosystem functioning, and stability in metacommunity networks. Ecography 40, 98-108. ( 10.1111/ecog.02558) [DOI] [Google Scholar]
  • 22.Rossetti MR, Tscharntke T, Aguilar R, Batáry P. 2017. Responses of insect herbivores and herbivory to habitat fragmentation: a hierarchical meta-analysis. Ecol. Lett. 20, 264-272. ( 10.1111/ele.12723) [DOI] [PubMed] [Google Scholar]
  • 23.Arroyo-Rodríguez V, Saldaña-Vázquez RA, Fahrig L, Santos BA. 2017. Does forest fragmentation cause an increase in forest temperature? Ecol. Res. 32, 81-88. ( 10.1007/s11284-016-1411-6) [DOI] [Google Scholar]
  • 24.Stangler ES, Hanson PE, Steffan-Dewenter I. 2015. Interactive effects of habitat fragmentation and microclimate on trap-nesting Hymenoptera and their trophic interactions in small secondary rainforest remnants. Biodivers. Conserv. 24, 563-577. ( 10.1007/s10531-014-0836-x) [DOI] [Google Scholar]
  • 25.Travis JMJ. 2003. Climate change and habitat destruction: a deadly anthropogenic cocktail. Proc. R. Soc. Lond. B 270, 467-473. ( 10.1098/rspb.2002.2246) [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 26.Lakeman-Fraser P, Ewers RM. 2014. Untangling interactions: do temperature and habitat fragmentation gradients simultaneously impact biotic relationships? Proc. R. Soc. B 281, 20140687. ( 10.1098/rspb.2014.0687) [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 27.Mantyka-Pringle CS, Martin TG, Rhodes JR. 2012. Interactions between climate and habitat loss effects on biodiversity: a systematic review and meta-analysis. Glob. Change Biol. 18, 1239-1252. ( 10.1111/j.1365-2486.2011.02593.x) [DOI] [Google Scholar]
  • 28.Traveset A, Richardson DM. 2006. Biological invasions as disruptors of plant reproductive mutualisms. Trends Ecol. Evol. 21, 208-216. ( 10.1016/j.tree.2006.01.006) [DOI] [PubMed] [Google Scholar]
  • 29.Vidal MC, Murphy SM. 2018. Bottom-up vs. top-down effects on terrestrial insect herbivores: a meta-analysis. Ecol. Lett. 21, 138-150. ( 10.1111/ele.12874) [DOI] [PubMed] [Google Scholar]
  • 30.Dorresteijn I, Schultner J, Nimmo DG, Fischer J, Hanspach J, Kuemmerle T, Kehoe L, Ritchie EG. 2015. Incorporating anthropogenic effects into trophic ecology: predator-prey interactions in a human-dominated landscape. Proc. R. Soc. B 282, 20151602. ( 10.1098/rspb.2015.1602) [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 31.Staddon P, Lindo Z, Crittenden PD, Gilbert F, Gonzalez A. 2010. Connectivity, non-random extinction and ecosystem function in experimental metacommunities. Ecol. Lett. 13, 543-552. ( 10.1111/j.1461-0248.2010.01450.x) [DOI] [PubMed] [Google Scholar]
  • 32.Clark RE, Singer MS. 2018. Keystone mutualism strengthens top–down effects by recruiting large-bodied ants. Oecologia 186, 601-610. ( 10.1007/s00442-017-4047-5) [DOI] [PubMed] [Google Scholar]
  • 33.Koltz AM, Classen AT, Wright JP. 2018. Warming reverses top-down effects of predators on belowground ecosystem function in Arctic tundra. Proc. Natl Acad. Sci. USA 115, E7541-E7549. ( 10.1073/pnas.1808754115) [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 34.Kotta J, Wernberg T, Jänes H, Kotta I, Nurkse K, Pärnoja M, Orav-Kotta H. 2018. Novel crab predator causes marine ecosystem regime shift. Sci. Rep. 8, 4956. ( 10.1038/s41598-018-23282-w) [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 35.Ostman O, Griffin NW, Strasburg JL, Brisson JA, Templeton AR, Knight TM, Chase JM. 2007. Habitat area affects arthropod communities directly and indirectly through top predators. Ecography 30, 359-366. ( 10.1111/j.0906-7590.2007.05123.x) [DOI] [Google Scholar]
  • 36.Thakur MP, Kunne T, Griffin JN, Eisenhauer N. 2017. Warming magnifies predation and reduces prey coexistence in a model litter arthropod system. Proc. R. Soc. B 284, 20162570. ( 10.1098/rspb.2016.2570) [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 37.Ingram T, Burns ZD. 2018. Top-down control by an aquatic invertebrate predator increases with temperature but does not depend on individual behavioral type. Ecol. Evol. 8, 8256-8265. ( 10.1002/ece3.4367) [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 38.Rusek J. 1998. Biodiversity of Collembola and their functional role in the ecosystem. Biodivers. Conserv. 7, 1207-1219. ( 10.1023/A:1008887817883) [DOI] [Google Scholar]
  • 39.Crotty FV, Adl SM. 2019. Competition and predation in soil fungivorous microarthropods using stable isotope ratio mass spectrometry. Front. Microbiol. 10, 1274. ( 10.3389/fmicb.2019.01274) [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 40.Gonzalez A, Lawton JH, Gilbert FS, Blackburn TM, Evans-Freke I. 1998. Metapopulation dynamics, abundance, and distribution in a microecosystem. Science 281, 2045-2047. ( 10.1126/science.281.5385.2045) [DOI] [PubMed] [Google Scholar]
  • 41.Perdomo G, Sunnucks P, Thompson RM. 2012. The role of temperature and dispersal in moss-microarthropod community assembly after a catastrophic event. Phil. Trans. R. Soc. B. 367, 3042-3049. ( 10.1098/rstb.2012.0241) [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 42.Rantalainen ML, Haimi J, Fritze H, Setala H. 2006. Effects of small-scale habitat fragmentation, habitat corridors and mainland dispersal on soil decomposer organisms. Appl. Soil Ecol. 34, 152-159. ( 10.1016/j.apsoil.2006.03.004) [DOI] [Google Scholar]
  • 43.O'Sullivan OS, et al. 2017. Thermal limits of leaf metabolism across biomes. Glob. Change Biol. 23, 209-223. ( 10.1111/gcb.13477) [DOI] [PubMed] [Google Scholar]
  • 44.Proctor MCF. 2003. Experiments on the effect of different intensities of desiccation on bryophyte survival, using chlorophyll fluorescence as an index of recovery. J. Bryol. 25, 201-210. ( 10.1179/037366803235001652) [DOI] [Google Scholar]
  • 45.Xu SJ, Liu CJ, Jiang PA, Cai WM, Wang Y. 2009. The effects of drying following heat shock exposure of the desert moss Syntrichia caninervis. Sci. Total Environ. 407, 2411-2419. ( 10.1016/j.scitotenv.2008.12.005) [DOI] [PubMed] [Google Scholar]
  • 46.Yinping L, Raymond AC, Nora MB. 2020. Predation efficacy of rove beetle (Coleoptera: Staphylinidae) adults in response to western flower thrips (Thysanoptera: Thripidae) pupal stage, predator–prey ratio, and searchable area. J. Entomol. Sci. 55, 350-365. ( 10.18474/0749-8004-55.3.350) [DOI] [Google Scholar]
  • 47.Cloyd R. 2019. Effects of predators on the belowground life stages (Prepupae and Pupae) of the western flower thrips, Frankliniella occidentalis (Thripidae: Thysanoptera): a review. Adv. Entomol. 7, 71-80. ( 10.4236/ae.2019.74006) [DOI] [Google Scholar]
  • 48.Echegaray EA, Cloyd RA, Nechols JR. 2015. Rove beetle (Coleoptera: Staphylinidae) predation on Bradysia sp. nr. coprophila (Diptera: Sciaridae). J. Entomol. Sci. 50, 225-237. ( 10.18474/JES14-38.1) [DOI] [Google Scholar]
  • 49.Echegaray ER, Cloyd RA. 2013. Life history characteristics of the rove beetle, Dalotia coriaria (Coleoptera: Staphylinidae) under laboratory conditions. J. Kansas Entomol. Soc. 86, 145-154. ( 10.2317/JKES120927.1) [DOI] [Google Scholar]
  • 50.Green TGA, Schroeter B, Kappen L, Seppelt RD, Maseyk K. 1998. An assessment of the relationship between chlorophyll a fluorescence and CO2 gas exchange from field measurements on a moss and lichen. Planta 206, 611-618. ( 10.1007/s004250050439) [DOI] [Google Scholar]
  • 51.Van Gaalen KE, Flanagan LB, Peddle DR. 2007. Photosynthesis, chlorophyll fluorescence and spectral reflectance in Sphagnum moss at varying water contents. Oecologia 153, 19-28. ( 10.1007/s00442-007-0718-y) [DOI] [PubMed] [Google Scholar]
  • 52.Maxwell K, Johnson GN. 2000. Chlorophyll fluorescence—a practical guide. J. Exp. Bot. 51, 659-668. ( 10.1093/jexbot/51.345.659) [DOI] [PubMed] [Google Scholar]
  • 53.de Carvalho RC, et al. 2014. Differential proteomics of dehydration and rehydration in bryophytes: evidence towards a common desiccation tolerance mechanism. Plant Cell Environ. 37, 1499-1515. ( 10.1111/pce.12266) [DOI] [PubMed] [Google Scholar]
  • 54.Thakur MP, Griffin JN, Kunne T, Dunker S, Fanesi A, Eisenhauer N. 2018. Temperature effects on prey and basal resources exceed that of predators in an experimental community. Ecol. Evol. 8, 12 670-12 680. ( 10.1002/ece3.4695) [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 55.Coors A, De Meester L. 2008. Synergistic, antagonistic and additive effects of multiple stressors: predation threat, parasitism and pesticide exposure in Daphnia magna. J. Appl. Ecol. 45, 1820-1828. ( 10.1111/j.1365-2664.2008.01566.x) [DOI] [Google Scholar]
  • 56.Raffaelli D. 2004. How extinction patterns affect ecosystems. Science 306, 1141-1142. ( 10.1126/science.1106365) [DOI] [PubMed] [Google Scholar]
  • 57.Oliver TH, et al. 2015. Biodiversity and resilience of ecosystem functions. Trends Ecol. Evol. 30, 673-684. ( 10.1016/j.tree.2015.08.009) [DOI] [PubMed] [Google Scholar]
  • 58.Bokhorst S, Berg MP, Wardle DA. 2017. Micro-arthropod community responses to ecosystem retrogression in boreal forest. Soil Biol. Biochem. 110, 79-86. ( 10.1016/j.soilbio.2017.03.009) [DOI] [Google Scholar]
  • 59.Schneider K, Maraun M. 2009. Top-down control of soil microarthropods - evidence from a laboratory experiment. Soil Biol. Biochem. 41, 170-175. ( 10.1016/j.soilbio.2008.10.013) [DOI] [Google Scholar]
  • 60.Santonja M, Aupic-Samain A, Forey E, Chauvat M. 2018. Increasing temperature and decreasing specific leaf area amplify centipede predation impact on Collembola. Eur. J. Soil Biol. 89, 9-13. ( 10.1016/j.ejsobi.2018.08.002) [DOI] [Google Scholar]
  • 61.Fountain MT, Hopkin SP. 2005. Folsomia candida (Collembola): a ‘standard’ soil arthropod. Annu. Rev. Entomol. 50, 201-222. ( 10.1146/annurev.ento.50.071803.130331) [DOI] [PubMed] [Google Scholar]
  • 62.Park EK. 2007. Effect of laboratory culture conditions on population growth of Proisotoma minuta (Tullberg) (Collembola: Isotomidae). Entomol. Sci. 10, 135-140. ( 10.1111/j.1479-8298.2007.00207.x) [DOI] [Google Scholar]
  • 63.Holmstrup M, et al. 2013. Soil microarthropods are only weakly impacted after 13 years of repeated drought treatment in wet and dry heathland soils. Soil Biol. Biochem. 66, 110-118. ( 10.1016/j.soilbio.2013.06.023) [DOI] [Google Scholar]
  • 64.Vanbergen AJ, Boissieres C, Gray A, Chapman DS. 2021. Data from: Habitat loss, predation pressure and episodic heat-shocks interact to impact arthropods and photosynthetic functioning of microecosystems. Dryad Digital Repository. ( 10.5061/dryad.kh1893259) [DOI] [PMC free article] [PubMed]

Associated Data

This section collects any data citations, data availability statements, or supplementary materials included in this article.

Data Citations

  1. Vanbergen AJ, Boissieres C, Gray A, Chapman DS. 2021. Data from: Habitat loss, predation pressure and episodic heat-shocks interact to impact arthropods and photosynthetic functioning of microecosystems. Dryad Digital Repository. ( 10.5061/dryad.kh1893259) [DOI] [PMC free article] [PubMed]

Supplementary Materials

Data Availability Statement

This article has additional data available from the Dryad Digital Repository: https://doi.org/10.5061/dryad.kh1893259 [64].


Articles from Proceedings of the Royal Society B: Biological Sciences are provided here courtesy of The Royal Society

RESOURCES