Article

Testing Predictions of the Resistance and Resilience of Vegetation Subjected to Extreme Events

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Abstract

We test the hypothesis that the responses of vegetation to extreme events is a function of the nutrient stress tolerance of species present. The nutrient stress tolerance of a range of species was defined by a formalized procedure in which traits measured by screening in the laboratory were synthesized using principle components analysis. 2. Results were then compared with the results from a large-scale field experiment which examined the responses of five herbaceous plant communities in Derbyshire, UK to three extreme events (frost, drought and fire). 3. Nutrient stress tolerance was positively correlated with resistance to initial damage and negatively correlated with resilience (speed of recovery). The results illustrate the use of laboratory data to predict the field responses of plants to extreme events and demonstrate that the axis from high to low nutrient stress tolerance can play an effective role in predicting these responses.

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... In generally, this statement was not confirmed by us (Fig. 6). Other studies (Grime & Campbell, 1991;MacGillivray et al., 1995;Fortunel et al., 2009) claim, in general, that plants with higher growth rates are predicted to have greater resilience. We can confirm this statement by the reaction of Sesleria tatrae in the Seslerietum tatrae biscutelletosum laevigatae community. ...
... This fact is inevitable. Based on vegetation responses to human trampling, the study of MacGillivray et al. (1995) clearly revealed that resistance and resilience, the two components of ecosystem stability, are strongly affected by environmental factors. For resistance, their results highlight background anthropogenic disturbance leading to species adaptations that potentially increase the ability to withstand disturbances. ...
... Other authors claim, that within the same ecosystem type, the ability to withstand disturbance events is likely to be depend on nutrient (MacGillivray et al., 1995;Breland & Hansen, 1996) and water availability (Gallet & Roze, 2001). Some ecosystems adapted to drought are known to be very resistant to trampling (Andrés-Abellán et al., 2006), while in general wet habitats seem to be most sensitive (Chapin & Chapin, 1980;Grime & Campbell, 1991;Francis et al., 2005). ...
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Trampling of vegetation as a result of recreation can adversely affect natural habitats, leading to loss of vegetation and degradation of plant communities. Many studies indicated that intrinsic properties of plant communities appear to be the most important factors determining the response of vegetation to trampling disturbance. Specifically, the dominant life-form of a plant community accounts for more variation in the resistance of communities to trampling than the intensity of the trampling experienced, suggesting that simple assessments based on this trait could guide decisions on access to natural sites. We verify these claims in the Belianske Tatry National Nature Reserve in Slovakia, which has been closed since 1978 due to destruction by mass tourism, with the exception of one trail made accessible since 1993. In researching the resistance of communities according to dominant life forms we adjusted the number of passes according to the minimum (75 tourists) and maximum (225 tourists) daily visitation during the tourist season. The studied communities occur in close proximity to the trails on the saddles through which the open trail passes. Available evidence from our studies suggests that vegetation dominated by hemicryptophytes is more resistant to trampling and recovers from trampling to a greater extent than vegetation dominated by other life forms. Therefore, we selected three alpine communities dominated by hemicryptophytes. In the Juncetum trifidi community, they almost completely dominate, they are mainly composed of grasses. Although they dominate the Junco trifidi-Callunetum vulgaris community, the species, Calluna vulgaris has been added to the woody chamephytes, and thus the woody Chamaephytes achieve a higher cover than in the Juncetum trifidi community. Although in the community Seslerietum tatrae biscutelletosum laevigatae hemicryptophytes dominate, it consists of several plant life forms and its grasses reach greater heights than in previous communities. We found that it is not possible to estimate the resilience of communities to trampling by dominant life forms. Life forms within one community react very similarly, but this statement cannot be generalized globally for all communities. At the same time, we found that if we damage the native community, which subsequently regenerates, the life forms of the community behave differently when damaged repeatedly. More detailed research is needed worldwide, which would point out patterns of behaviour of alpine plant vegetation to trampling.
... The impact of disturbances such as extreme drought on productivity is mostly quantified as resistance and resilience. Thereby, resistance quantifies the concurrent change in an ecosystem variable in the presence of the disturbance (MacGillivray et al., 1995;Pimm, 1984) and resilience the extent to which the variable returns to a reference state after its subsidence (Grimm and Wissel, 1997;MacGillivray et al., 1995). However, a general pattern as to the resistance and resilience of productivity to extreme drought is still debated (Felton et al., 2020;Hoover et al., 2018;Stuart-Haëntjens et al., 2018;Wu et al., 2011). ...
... The impact of disturbances such as extreme drought on productivity is mostly quantified as resistance and resilience. Thereby, resistance quantifies the concurrent change in an ecosystem variable in the presence of the disturbance (MacGillivray et al., 1995;Pimm, 1984) and resilience the extent to which the variable returns to a reference state after its subsidence (Grimm and Wissel, 1997;MacGillivray et al., 1995). However, a general pattern as to the resistance and resilience of productivity to extreme drought is still debated (Felton et al., 2020;Hoover et al., 2018;Stuart-Haëntjens et al., 2018;Wu et al., 2011). ...
... Theory suggests that resistance and resilience of productivity to a disturbance such as an extreme drought differ among ecosystems when their component species portend different life histories (Grime, 2001;Lepš et al., 1982;MacGillivray et al., 1995). For example, forests, composed of species with long-lived, slow growing life-histories, are theorized to be more resistant but less resilient in productivity than for example productive grasslands (Grime, 2001). ...
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Climate change is continuously intensifying droughts. Extreme droughts are expected to reduce soil water content and thus, ecosystem functioning such as above-ground primary productivity. Nonetheless, results of experimental drought studies vary from no impact to a significant decrease in soil water content and/or productivity. We experimentally imposed extreme drought as 30 % and 50 % precipitation reductions using rainout shelters for four years in temperate grasslands and in the forest understory. We studied the concurrent impact of two intensities of extreme drought on the soil water content and above-ground primary productivity in the last experimental year (resistance). Furthermore, we observed resilience as the extent to which both variables differ from ambient conditions after the removal of the 50 % reduction. We show a systematic difference in response to extreme experimental drought between grasslands and the forest understory irrespective of the intensity of the extreme drought. Namely, extreme drought resulted in a significant decrease of the soil water content and productivity in grasslands but not in the forest understory. Interestingly, the negative impacts in the grasslands did not persist as evidenced by the fact that soil water content and productivity were similar to ambient conditions after the removal of the drought. Our results indicate that extreme drought on small spatial scales does not necessarily result in a concurrent soil water decrease in the forest understory, while this is the case for grasslands, with respective consequences for the resistance of productivity. Grasslands, however, can be resilient. Our study highlights that considering the response of the soil water content is key to understanding divergent productivity responses to extreme drought among different ecosystems.
... In Supplementary Materials, we show that spurious covariation between resistance and resilience occurs in almost all of the pairs of resilience (R s )/resistance (R t ) indices found in the literature. Consistent with this, we employ the approach by MacGillivray et al. (1995) for all our subsequent analyses, because this approach ensures that resilience and resistance are mathematically independent from one another, albeit they may still show temporal covariation as a result of autocorrelation in the time series, reflecting a real biological property as opposed to a mathematical artefact. Using this definition, resistance R t is obtained dividing observed drought-year growth by the expected growth that would have taken place had the drought not occurred in that year. ...
... The use of ARIMA models (Martínez-Vilalta et al., 2012) achieves this goal perfectly. Using autocorrelation features to derive estimates of 'expected' growth is consistent with the definition of resilience (MacGillivray et al., 1995) and with our own earlier work on growth responses to drought events Ovenden et al., 2021). ...
... We show that it is possible to avoid spurious correlations in the analysis of the components of resilience via a reference null model. Conceptually, our approach is equivalent to (MacGillivray et al., 1995), originally intended for experimental comparisons against a control. Our null model maintains the temporal memory of the process via its autocorrelation structure (Peltier et al., 2016;Ovenden et al., 2021) and differs therefore from (Anderegg et al., 2015;Jiang et al., 2019), where null expectations of growth were obtained from static growth-climate relationships. ...
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Background: Plasticity in response to environmental drivers can help trees cope with droughts. However, our understanding of the importance of plasticity and physiological adjustments in trees under global change is limited. Methods: We used the International Tree-Ring Data Bank (ITRDB) to examine 20th century growth responses in conifer trees during (resistance) and following (resilience) years of severe soil and atmospheric droughts occurring in isolation or as compound events. Growth resilience indices were calculated using observed growth divided by expected growth to avoid spurious correlations, in which the expected values were obtained by the autoregressive moving average (ARIMA) model. We used high atmospheric vapour pressure deficit (VPD) to select years of atmospheric drought and low annual values of the Standardized Precipitation-Evapotranspiration Index (SPEI) to select years with soil drought. We acquired the sensitivities (i.e., the slopes of the relationships) by fitting the resilience indices as a function of environmental drivers, and assessed how these sensitivities changed over time for different types of drought events using linear mixed models. We also checked whether plasticity in growth responses was sufficient to prevent long-term trends of growth reductions during or after severe droughts. We acknowledge that by focusing on the response of surviving trees from the ITRDB we are potentially biasing our results towards higher resilience, as stand level responses (e.g., mortality) may result in lowered competition after the disturbance event. Results: Sensitivities of resilience to VPD and SPEI changed throughout the 20th century, with the directions of these changes often reversing in the second half of the century. For the 1961–2010 period, changing sensitivities had positive effects on resilience, especially following years of high-VPD and compound events, avoiding growth losses that would have occurred if sensitivities had remained constant. Despite sensitivity changes, resilience was still lower at the end of the 20th century compared to the beginning of the century. Conclusions: Future adjustments to low-SPEI and high-VPD events are likely to continue to compensate for the trends in climate only partially, leading to further generalized reductions in tree growth of conifers. An improved understanding of these plastic adjustments and their limits, as well as potential compensatory processes at the stand level, is needed to project forest responses to climate change.
... In Supplementary Materials, we show that spurious covariation between resistance and resilience occurs in almost all of the pairs of resilience (R s )/resistance (R t ) indices found in the literature. Consistent with this, we employ the approach by MacGillivray et al. (1995) for all our subsequent analyses, because this approach ensures that resilience and resistance are mathematically independent from one another, albeit they may still show temporal covariation as a result of autocorrelation in the time series, reflecting a real biological property as opposed to a mathematical artefact. Using this definition, resistance R t is obtained dividing observed drought-year growth by the expected growth that would have taken place had the drought not occurred in that year. ...
... The use of ARIMA models (Martínez-Vilalta et al., 2012) achieves this goal perfectly. Using autocorrelation features to derive estimates of 'expected' growth is consistent with the definition of resilience (MacGillivray et al., 1995) and with our own earlier work on growth responses to drought events Ovenden et al., 2021). ...
... We show that it is possible to avoid spurious correlations in the analysis of the components of resilience via a reference null model. Conceptually, our approach is equivalent to (MacGillivray et al., 1995), originally intended for experimental comparisons against a control. Our null model maintains the temporal memory of the process via its autocorrelation structure (Peltier et al., 2016;Ovenden et al., 2021) and differs therefore from (Anderegg et al., 2015;Jiang et al., 2019), where null expectations of growth were obtained from static growth-climate relationships. ...
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Plasticity in response to environmental drivers can help trees cope with droughts. However, our understanding of the importance of plasticity and physiological adjustments in trees under global change is limited. We examine 20th century growth responses in Gymnosperm trees during (resistance) and following (resilience) years of severe soil and atmospheric droughts occurring in isolation or as compound events. We use high atmospheric vapour pressure deficit (VPD) to select years of atmospheric drought and negative annual values of the Standardised Precipitation-Evapotranspiration Index (SPEI) to select years with a large negative balance between precipitation and evaporation. Sensitivities (i.e., the slopes of the relationships) of resilience to VPD and SPEI changed throughout the 20th century, with the directions of these changes often reversing in the second half of the century. For the 1951-2001 period, variable sensitivities had positive effects on resilience, especially following years of high VPD and compound VPD/SPEI events, avoiding growth losses that would have occurred if sensitivities had remained constant. Despite sensitivity changes, resilience recovered less at the end of the 20th century compared to the beginning of the century. Future adjustments to low SPEI and high VPD are likely to continue to compensate for the trends in climate only partially, leading to further generalised reductions in tree growth of Gymnosperm trees.
... The stability of ecosystems -the set of system properties that determines the magnitude, duration and reversibility of change resulting from a perturbation (Noy-Meir, 1974;Van Meerbeek et al., 2021)may be influenced by the availability of limiting nutrient resources (e.g., Lepš et al., 1982;MacGillivray et al., 1995), with nutrient limitation tending to stabilize ecosystem dynamics (DeAngelis et al., 1989). ...
... Specific life history and resource allocation traits (e.g., relative growth rate, leaf and twig longevity, antiherbivore defense; Coley et al., 1985;Lavorel & Garnier, 2002) may be universal moderators of the resistance (i.e., the ability to withstand instantaneous disturbance-induced change) and resilience (i.e., the capacity to return to a pre-disturbance reference condition; Van Meerbeek et al., 2021) components of stability in plant communities exposed to disturbances (Lepš et al., 1982). For instance, in herbaceous plant communities of contrasting soil fertility, nutrient stress tolerance correlated positively with resistance and negatively with resilience to frost, drought, and fire disturbance (MacGillivray et al., 1995). Further, the availability of limiting nutrient resources related strongly to the resistance and resilience of subtropical mangrove (Feller et al., 2015) and tropical forests to cyclone disturbances (Gleason et al., 2008(Gleason et al., , 2010Herbert et al., 1999). ...
... In Australia, the properties of low soil-P specialists dominated forest functioning in low-P forests (Gleason et al., 2008). Therefore, the moderator effect of soil P on litterfall cyclone resistance could be partially related to tree species compositions (Lepš et al., 1982;MacGillivray et al., 1995) that reflect distinct adaptive specializations related to the plant's acquisitive and retentive mechanisms of phosphorus utilization (Chapin, 1980;Coley et al., 1985;Endara & Coley, 2011;Fridley et al., 2011). ...
Article
While tropical cyclone regimes are shifting with climate change, the mechanisms underpinning the resistance (ability to withstand disturbance‐induced change) and resilience (capacity to return to pre‐disturbance reference) of tropical forest litterfall to cyclones remain largely unexplored pantropically. Single‐site studies in Australia and Hawaii suggest that litterfall on low‐phosphorus (P) soils is more resistant and less resilient to cyclones. We conducted a meta‐analysis to investigate the pantropical importance of total soil P in mediating forest litterfall resistance and resilience to 22 tropical cyclones. We evaluated cyclone‐induced and post‐cyclone litterfall mass (g/m2/day), and P and nitrogen (N) fluxes (mg/m2/day) and concentrations (mg/g), all indicators of ecosystem function and essential for nutrient cycling. Across 73 case studies in Australia, Guadeloupe, Hawaii, Mexico, Puerto Rico, and Taiwan, total litterfall mass flux increased from ~2.5 ± 0.3 to 22.5 ± 3 g/m2/day due to cyclones, with large variation among studies. Litterfall P and N fluxes post‐cyclone represented ~5% and 10% of the average annual fluxes, respectively. Post‐cyclone leaf litterfall N and P concentrations were 21.6 ± 1.2% and 58.6 ± 2.3% higher than pre‐cyclone means. Mixed‐effects models determined that soil P negatively moderated the pantropical litterfall resistance to cyclones, with a 100 mg P/kg increase in soil P corresponding to a 32% to 38% decrease in resistance. Based on 33% of the resistance case studies, total litterfall mass flux reached pre‐disturbance levels within one‐year post‐disturbance. A GAMM indicated that soil P, gale wind duration and time post‐cyclone jointly moderate the short‐term resilience of total litterfall, with the nature of the relationship between resilience and soil P contingent on time and wind duration. Across pantropical forests observed to date, our results indicate that litterfall resistance and resilience in the face of intensifying cyclones will be partially determined by total soil P.
... Resilience has become an increasingly popular concept in the past decades within the field of ecology (Bellwood et al., 2006;Isbell et al., 2015;Leps et al., 1982;Macgillivray & Grime, 1995;Sankaran & McNaughton, 1999;Wardle & Jonsson, 2014) and well beyond (Carpenter et al., 2001;Zell & Hubbart, 2013). Despite this growing interest, studies quantitatively documenting resilience in the field are still uncommon (e.g. ...
... Despite this growing interest, studies quantitatively documenting resilience in the field are still uncommon (e.g. López et al., 2013;Macgillivray & Grime, 1995;Sankaran & McNaughton, 1999). This lack of empirical evidence is especially true for arid and semi-arid woody ecosystems, where slow dynamics and high spatial heterogeneity make the study of temporal trends highly time-consuming, often exceeding the typical duration of research grants (Li et al., 2015;Lindenmayer et al., 2012;Meserve et al., 2003). ...
... Ecosystem responses to disturbances are mediated by different community attributes or components that underpin the ecosystem's capacity to bounce back. Such 'sources of resilience' include for example the number of species (Tilman & Downing, 1994), functional composition (Leps et al., 1982;Lipoma et al., 2016;Macgillivray & Grime, 1995;Walker, 1992) and the existence of biological legacies such as persistent seed or seedling banks (Lipoma et al., 2019(Lipoma et al., , 2020Plieninger et al., 2011). The absence or the deterioration of one or more sources of resilience as a consequence of land-use changeone of the most important disturbance factors affecting ecosystems globally, (IPCC, 2019;IPBES, 2019) and particularly in arid and semiarid ecosystems (Song et al. 2018)-can affect the capacity of ecosystems to recover after disturbance and maintain their functioning over time, or even push them to a different irreversible state (Folke et al., 2004). ...
Article
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Resilience—the capacity of an ecosystem to recover from disturbance—is a popular concept but quantitative empirical studies are still uncommon. This lack of empirical evidence is especially true for semi‐arid ecosystems in the face of the combined and often confounding impacts of land use and climate changes. We designed a methodology to disentangle vegetation responses to land‐use exclusion and weather variability, and piloted it at the southern extreme of the Gran Chaco forest, the most extensive seasonally dry forest in South America. We established 16 pairs of neighbouring fenced and unfenced plots in four ecosystem types resulting from different long‐term land‐use regimes under the same climate and on highly similar soil parental material. From lower to higher land‐use intensity, related with logging and livestock grazing and trampling, these types were: primary forest (no land use in the last 50 years), secondary forest, closed species‐rich shrubland and open shrubland. In each plot we monitored plant species composition during the first 5 years following land‐use exclusion, and evaluated the resilience as the rate of change of vegetation towards the primary forest, considered as the reference ecosystem. We found that during the first 5 years of exclusion and despite the high rainfall, only grass cover in the secondary forest showed positive resilience (recovery towards the reference ecosystem). The rest of the variables in the other ecosystem types showed either no significant change (null resilience) or even transitioned away from the reference state (negative resilience). Synthesis . The lack of detectable recovery after 5 years of exclusion suggests that (a) long‐term land use, even at lower intensities, has affected the sources of resilience of this ecosystem; (b) rainy periods do not necessarily speed up recovery as suggested in the literature; and (c) study designs should incorporate the variation of the reference ecosystem in order to differentiate the effect of land use from other factors in a context of climate change. Although still confined to the early post‐disturbance stages, our findings suggest that recovery of these systems may be slower and more complicated than predicted in the literature on the basis of space‐for‐time substitutions.
... Its response to drought may largely drive grassland biomass stability and impose substantial influences on the responses of other species (including other dominant species, Figure S4 in Supporting Information) to drought, with subsequent influences on community structural resistance and recovery. Our results are thus consistent with the findings of several previous studies that plant community functional resistance and recovery are modulated by the traits of dominant species (DeClerck et al., 2006;Hoover et al., 2014;MacGillivray and Grime, 1995). Together, these results provide strong support for the mass ratio hypothesis that properties of an ecosystem are largely determined by its dominant species (Grime, 1998). ...
... We quantified both functional (i.e., biomass based) and structural resistance and recovery of plant communities to examine their responses to our experimental treatments. Biomass resistance (B rst ) was quantified as the ratio of the mean AGB of three drought years (2015)(2016)(2017) to the AGB in the year before drought (2014) (MacGillivray and Grime, 1995). Biomass recovery (B rc ) was quantified as the ratio of the AGB in post-drought year (2018) to the mean AGB of the drought years (2015-2017) (Lloret et al., 2011). ...
Article
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Nitrogen enrichment and land use are known to influence various ecosystems, but how these anthropogenic changes influence community and ecosystem responses to disturbance remains poorly understood. Here we investigated the effects of increased nitrogen input and mowing on the resistance and recovery of temperate semiarid grassland experiencing a three-year drought. Nitrogen addition increased grassland biomass recovery but decreased structural recovery after drought, whereas annual mowing increased grassland biomass recovery and structural recovery but reduced structural resistance to drought. The treatment effects on community biomass/structural resistance and recovery were largely modulated by the stability of the dominant species and asynchronous dynamics among species, and the community biomass resistance and recovery were also greatly driven by the stability of grasses. Community biomass resistance/recovery in response to drought was positively associated with its corresponding structural stability. Our study provides important experimental evidence that both nitrogen addition and mowing could substantially change grassland stability in both functional and structural aspects. Our findings emphasize the need to study changes across levels of ecological organization for a more complete understanding of ecosystem responses to disturbances under widespread environmental changes.
... To aid the interpretation of figures, drought severity was then calculated as the absolute value of the Z score of MCWD. For each drought event, drought resistance was defined as the relative rate of change in forest condition during and before drought disturbance and drought resilience as the ability to recover to the predrought state (32)(33)(34). We studied resistance and resilience 2 years before and 2 years after the drought event; this time span accounts for the 2-year legacy effect of drought previously reported in rainforests (35). ...
... Drought severity was then taken to be the absolute value of the Z score of MCWD. Drought resistance and resilience were calculated following standard definitions in the ecological literature (32)(33)(34). Defining Y pre as the predrought radar signal, Y post as the signal postdrought, and Y e as the signal during the drought event, resistance was defined as (Y e À Y pre )/Y pre , and resilience as (Y post À Y pre )/Y pre (34). We used the maximum radar (wet season) signal values within 2 years before and 2 years after the drought event to represent forest pre-and postdrought conditions, respectively. ...
Article
Intact tropical rainforests have been exposed to severe droughts in recent decades, which may threaten their integrity, their ability to sequester carbon, and their capacity to provide shelter for biodiversity. However, their response to droughts remains uncertain due to limited high-quality, long-term observations covering extensive areas. Here, we examined how the upper canopy of intact tropical rainforests has responded to drought events globally and during the past 3 decades. By developing a long pantropical time series (1992 to 2018) of monthly radar satellite observations, we show that repeated droughts caused a sustained decline in radar signal in 93%, 84%, and 88% of intact tropical rainforests in the Americas, Africa, and Asia, respectively. Sudden decreases in radar signal were detected around the 1997–1998, 2005, 2010, and 2015 droughts in tropical Americas; 1999–2000, 2004–2005, 2010–2011, and 2015 droughts in tropical Africa; and 1997–1998, 2006, and 2015 droughts in tropical Asia. Rainforests showed similar low resistance (the ability to maintain predrought condition when drought occurs) to severe droughts across continents, but American rainforests consistently showed the lowest resilience (the ability to return to predrought condition after the drought event). Moreover, while the resistance of intact tropical rainforests to drought is decreasing, albeit weakly in tropical Africa and Asia, forest resilience has not increased significantly. Our results therefore suggest the capacity of intact rainforests to withstand future droughts is limited. This has negative implications for climate change mitigation through forest-based climate solutions and the associated pledges made by countries under the Paris Agreement.
... We also showed that MAT was negatively correlated with CWM of genome size, possibly because low temperatures favour plants with large genomes (Grime & Mowforth 1982;MacGillivray et al. 1995). For instance, species with large genomes gain an advantage in frost resistance (MacGillivray et al. 1995). ...
... We also showed that MAT was negatively correlated with CWM of genome size, possibly because low temperatures favour plants with large genomes (Grime & Mowforth 1982;MacGillivray et al. 1995). For instance, species with large genomes gain an advantage in frost resistance (MacGillivray et al. 1995). Altitude was a poor predictor for CWM of genome size, with variation among sites better explained by other properties of those sites; for example, alpine grasslands with low MAT were occupied by more species with large genomes. ...
Preprint
Elucidating mechanisms underlying community assembly and biodiversity patterns is central to ecology and evolution. Genome size (GS, i.e. nuclear DNA content) determines species’ capacity to tolerate environmental stress or to exploit new environments and therefore potentially drive community assembly. However, its role in driving β-diversity (i.e., the site-to-site variability in species composition) remains unclear. We measured GS for 169 plant species and investigated their occurrences within plant communities across 52 sites spanning a 3200-km transect in the temperate grasslands of China. We found environmental factors showed larger effects on β-diversity of large-GS than that of small-GS species. Community weighted mean GS increased with mean annual precipitation, soil total nitrogen and phosphorus concentrations, but decreased with mean annual temperature, suggesting a negative selection against species with large GS in resources-limited or warmer climates. These findings highlight the roles for GS in driving community assembly and predicting species responses to climate change.
... However, the greater water-holding capacity of nutrient-rich substrate may counteract this faster depletion. Moreover, recovery on nutrient-rich substrate is expected to be faster owing to greater abundance of resources (MacGillivray et al. 1995). ...
... In other words, nutrient-rich substrate can mitigate stress at the beginning of the drought via its higher water-holding capacity, but this protection fails for longer droughts. Recovery from the drought was expected to be faster on nutrient-rich substrate owing to more available resources there (MacGillivray et al. 1995), and this pattern was confirmed (Supporting information). We are familiar with only two other studies on the joint effects of soil heterogeneity and drought on plant communities. ...
Article
Heterogeneity is an intrinsic characteristic of soils, which regulates plant diversity and ecosystem functioning. However, whether soil heterogeneity also modulates responses of plant communities to climate change, including climate extremes, remains largely an open question. Here, we explore responses of plant communities to drought extremes across four levels of spatial soil heterogeneity, with cell sizes varying from very small to very large, i.e. 0, 12, 24 and 48 cm. These were created in mesocosms by alternating nutrient-rich and nutrient-poor substrate in three dimensions. A seed mixture of 24 grassland species was evenly sown on each mesocosm in spring. In late summer, a three-week drought was imposed with a rainout shelter. During the drought, soil water content at the mesocosm scale decreased more at intermediate (12 and 24 cm) than at small or large (0 and 48 cm) cell sizes, which was reflected in increased senescence and drought-induced heat stress. These responses could be traced to greater plant biomass coupled with higher water demand at those intermediate cell sizes, likely related to between-cell access to nutrients and effects of diversity and community composition. Our results indicate that soil heterogeneity can modulate the impact of drought extremes on plant communities, though more research is needed on the transition between intermediate and extreme cell sizes, where heterogeneity effects seem to change most. We propose that soil heterogeneity be considered more explicitly in studies of changing precipitation regimes.
... This is because of the different life and evolutionary histories of resident plant species in grasslands and forests that result in different functional responses to extreme drought. Generally, forests have a higher resistance to drought than grasslands, because of their deeper root systems and greater water storage capacity [58]. In addition, forests have a greater ability to regulate their water use through stomatal control, which enables them to maintain their water balance even during periods of drought [3]. ...
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It is projected that extreme drought events will become more frequent and more severe across many regions of the globe by the end of the 21st century. Despite the substantial efforts that have been made to explore the impacts of droughts on terrestrial ecosystems, our understanding of the response of diverse ecosystems, including resistance and resilience, remains unclear. A total of 16 site years of eddy covariance-based carbon flux data were used to reveal the different responses of forest and grassland ecosystems to two extreme summer droughts. We found that the carbon fluxes of the forest, namely gross primary productivity (GPP), ecosystem respiration (Re), and the net ecosystem carbon exchange (NEE), exhibited distinct seasonal patterns with a single peak. However, GPP and NEE of grassland showed multiple peaks owing to hay harvesting throughout one year. Meanwhile, all climate factors jointly affected the seasonal dynamics in the NEE of the forest, whereas solar radiation only dominated the variability in the NEE of grassland. Moreover, the optimal response relationship was quadratic between the vapor pressure deficit (VPD) and the NEE, with the thresholds being 5.46 and 5.84 for forest and grassland, respectively. Owing to the large increase in VPD during the droughts of 2003 and 2018, the carbon sequestration of forest and grassland reduced sharply and even altered from carbon sink to carbon source. Compared with grassland, forest GPP showed stronger resistance with weaker resilience to droughts. However, larger resilience appeared for both forest and grassland NEE relative to their resistance. All analyses reflect the different adaptive strategies among plant functional types, which is crucial to evaluate ecosystem carbon sequestration to overcome future climate change.
... with surprisingly simple methods, his design of experiments in which the lack of a dedicated budget was compensated with immense ingenuity is a very strong inspiration to younger generations of ecologists, even if they do not find CSR theory convincing or directly applicable to their work. He also was arguably the founding father of comparative plant ecology and the now widespread functional trait research programme, through the founding of the Integrated Screening Programme MacGillivray et al., 1995), and the books Comparative Plant Ecology (Grime, Hodgson, et al., 1988) and Methods in Comparative Plant Ecology (Hendry & Grime, 1993). ...
Article
Perhaps as much as any other scientist in the 20th century, J.P. Grime transformed the study of plant ecology and helped shepherd the field toward international prominence as a nexus of ideas related to global environmental change. Editors at the Journal of Ecology asked a group of senior plant ecologists to comment on Grime's scientific legacy. This commentary piece includes individual responses of 14 scientists from around the world attesting to Grime's foundational role in plant functional ecology, including his knack for sparking controversy, his unique approach to theory formulation involving clever experiments and standardized trait measurements of large numbers of species, and the continued impact of his work on ecological science and policy.
... In ecological research, researchers have placed a strong emphasis on the speed of recovery from disruption when describing resilience. Resilience has been defined as the speed of recovery to levels of control (MacGillivray et al., 1995). Fresco and Kroonenberg (1992) described resilience as the speed of restoration of the exit pattern after a disruption. ...
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This research aims, through a multi-perspective and multidisciplinary approach, to identify the key dimensions as well as the scale of measurement of the enterprise supply chain resilience for an in-depth understanding of the concept. This is among the first empirical research examining the key dimensions and appropriate measurement scale of enterprise supply chain resilience to address disruptions induced by unavoidable risk events. A detailed review of the literature was conducted to identify the dimensions of the construct under study. Then, a measurement instrument was developed from a set of items. The questionnaire was purified through a pretest, a pilot test, and reliability and validity tests. Data were collected from a final sample of 150 senior and middle managers, whose responses were considered for confirmatory factor analysis using SPSS Amos 22. The research results showed that the enterprise supply chain resilience construct is composed of seven distinct dimensions, including collaboration, alertness, preparedness, visibility, robustness, flexibility and velocity. Then, a measurement instrument containing measurement items for each of said dimensions was empirically validated. This research develops and validates a structured and comprehensive measurement scale for the concept under study while identifying measurement items that can guide further theoretical testing of this concept and thereby dilute the dimensional and measurement confusions surrounding this theoretical concept. Implications for Central European audience: This research develops and validates a structured and comprehensive measurement scale for the concept of firm supply chain resilience while identifying measurement items that can guide subsequent theoretical testing and thus dilute the dimensional and measurement confusions surrounding this theoretical concept.
... Resilience has a range of definitions, but it primarily refers to the ability of an ecosystem to return to a particular set of ecological states following changes in environmental or social (policy) pressures ( Figure 1). Resilience is generally used to describe a property exhibited by a particular ecological or socioecological system [4][5][6][7][8][9][10][11] , or as a measure of how well the population will recover from perturbation [12][13][14][15][16] . Understanding whether, and to what extent, an ecological or socioecological system is resilient helps us understand whether an ecosystem is at risk of collapse, or how far it can be pushed by environmental or social changes 1-3 . ...
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Resilient ecological systems will be better able to maintain their structure and function in the emerging Anthropocene. Estimating the resilience of different systems will therefore provide valuable insight for conservation decision-makers, and is a priority goal of resilience theory. Current estimation methods rely on the accurate parameterisation of ecosystem models, or the identification of important motifs in the structure of the ecological system network. However, both of these methods face significant empirical and theoretical challenges. In this paper, we adapt tools developed for the analysis of biochemical regulatory networks to prove that a form of resilience - robust perfect adaptation - is a property of particular ecological networks, and to explain the specific process by which the ecosystem maintains its resilience. We undertake an exhaustive search for robust perfect adaptation across all possible three-species ecological networks, under a generalised Lotka-Volterra framework. From over 20,000 possible network structures, we identify 23 network structures that are capable of robust perfect adaptation. The resilient properties of these networks provide important insights into the potential mechanisms that could promote resilience in ecosystems, and suggest new avenues for measuring and understanding the property of ecological resilience in larger, more realistic socioecological networks.
... However, it is unclear if cryptogams can reacclimate these cold-hardening attributes after an abrupt midwinter warming event to re-establish freeze-tolerance. This mid-winter deacclimation and reacclimation, in response to a winter heatwave, may be affected by the nutritional status of plants (MacGillivray et al., 1995). ...
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Arctic ecosystems are increasingly exposed to extreme climatic events throughout the year, which can affect species performance. Cryptogams (bryophytes and lichens) provide important ecosystem services in polar ecosystems but may be physiologically affected or killed by extreme events. Through field and laboratory manipulations, we compared physiological responses of seven dominant sub-Arctic cryptogams (3 bryophytes, 4 lichens) to single events and factorial combinations of mid-winter heatwave (6°C for 7 days), re-freezing, snow removal and summer nitrogen addition. We aimed to identify which mosses and lichens are vulnerable to these abiotic extremes and if combinations would exacerbate physiological responses. Combinations of extremes resulted in stronger species responses but included idiosyncratic species-specific responses. Species that remained dormant during winter (March), irrespective of extremes, showed little physiological response during summer (August). However, winter physiological activity, and response to winter extremes, were not consistently associated with summer physiological impacts. Winter extremes affect cryptogam physiology, but summer responses appear mild, and lichens affect the photobiont more than the mycobiont. Accounting for Arctic cryptogam response to multiple climatic extremes in ecosystem functioning and modelling will require a better understanding of their winter eco-physiology and repair capabilities. This article is protected by copyright. All rights reserved.
... Forest responses to drought and/or warming can be assessed by their resistance and resilience [29]. Resistance measures how an ecosystem changes immediately after a disturbance, and resilience evaluates the degree of ecological functioning that is restored to pre-disturbance equilibrium [30][31][32]. Therefore, it is important to quantify the sensitivity (resistance) and post-event recovery (resilience) of the subtropical coniferous forests to drought and/or warming under the climate change. ...
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The impacts of drought and/or warming on forests have received great attention in recent decades. Although the extreme drought and/or warming events significantly changed the forest demography and regional carbon cycle, the seasonality quantifying the impacts of these climate extremes with different severities on the productivity of subtropical coniferous forests remains poorly understood. This study evaluated the effects of seasonal drought and/or warming on the net primary productivity (NPP) of subtropical coniferous forests (i.e., Cunninghamia lanceolata and Pinus massoniana forests) from Hengyang–Shaoyang Basin in southern China using the Ecosystem Demography model, Version 2.2 (ED-2.2) and based on the datasets from forest inventory, meteorological reanalysis, and remotely sensed products. The results showed that the goodness of fit of the DBH-height allometric equations was better than that of the default in ED-2.2 after model calibration; the ED-2.2 model qualitatively captured the seasonality of NPP in the subtropical coniferous forests; and the mismatch between simulated annual NPP and MODIS-NPP (MOD17A3HGF) became smaller over time. The effect of seasonal drought on NPP was greater than that of warming; the decline rate of NPP gradually increased and decreased with time (from July to October) under the seasonal drought and warming scenarios, respectively; NPP decreased more seriously under the combined drought-warming scenario in October, with an average decrease of 31.72%, than the drought-only and warming-only scenarios; seasonal drought had an obvious legacy impact on productivity recovery of subtropical coniferous forests, but it was not the case for warming. With the increase in drought severity, the average values of soil available water and NPP together showed a downward trend. With the increase in warming severity, the average values of canopy air space temperature increased, but NPP decreased. Seasonal drought and/or warming limit forest production through decreasing soil moisture and/or increasing canopy air space temperature, which impact on plant photosynthesis and productivity, respectively. Our results highlight the significance of taking into account the impacts of seasonal warming and drought when evaluating the productivity of subtropical coniferous forests, as well as the significance of enhancing the resistance and resilience of forests to future, more severe global climate change.
... the status where growth returns to a historic norm (Ovenden et al., 2021). The capacities of grassland CG are different among species (Knapp et al., 2015), community components (Carlsson et al., 2017;Stampfli et al., 2018;Wilcox et al., 2020), life forms (Volaire, 2003;Nippert and Knapp, 2007), nutrient stress tolerances (Macgillivray et al., 1995;Bharath et al., 2020), interactions among soil microbes (De Vries et al., 2012a;Fry et al., 2018) and disturbance's properties (Chen et al., 2020;Saeidnia et al., 2020;Li et al., 2022). Besides, CG could be evaluated by a variety of quantitative indicators, such as productivity, biomass, species number, coverage, and so on . ...
Article
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Grasslands are structurally and functionally controlled by water availability. Ongoing global change is threatening the sustainability of grassland ecosystems through chronic alterations in climate patterns and resource availability, as well as by the increasing frequency and intensity of anthropogenic perturbations. Compared with many studies on how grassland ecosystems respond during drought, there are far fewer studies focused on grassland dynamics after drought. Compensatory growth, as the ability of plants to offset the adverse effects of environmental or anthropogenic perturbations, is a common phenomenon in grassland. However, compensatory growth induced by drought and its underlying mechanism across grasslands remains not clear. In this review, we provide examples of analogous compensatory growth from different grassland types across drought characteristics (intensity, timing, and duration) and explain the effect of resource availability on compensatory growth and their underlying mechanisms. Based on our review of the literature, a hypothetic framework for integrating plant, root, and microbial responses is also proposed to increase our understanding of compensatory growth after drought. This research will advance our understanding of the mechanisms of grassland ecosystem functioning in response to climate change.
... Recently, several studies have shown the significance of functional trait-based life history strategies in understanding the functional diversity-stability relationships (Craven et al., 2018;Li et al., 2021;Schnabel et al., 2021). It is generally accepted that "K-strategists" species with larger individuals and more conservative resource acquisition show greater resistance (ability to withstand perturbation) but less resilience (recovery from perturbation) to a disturbance (MacGillivray et al., 1995;Karlowsky et al., 2018). On the contrary, "rstrategists" species with smaller size and rapid resource uptake can recover rapidly after a disturbance and show greater resilience. ...
Article
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The biodiversity-stability relationship is a fundamental subject of ecological research. Considerable evidence demonstrates that biodiversity can either increase or decrease stability. Most relevant research mainly focuses on grassland and forest ecosystems. The biodiversity-stability relationship in aquatic ecosystems and the underlying mechanisms remain poorly understood. To fill the gap, we conducted a year-long study on the phytoplankton of reservoir ecosystems in the Xiangxi Bay of Three Gorges Reservoir (TGR) to test the following hypotheses: (H1) phytoplankton species richness and functional diversity directly reduce phytoplankton community stability in reservoir ecosystems; (H2) nutrient enrichment and water temperature increasing directly reduce phytoplankton community stability; and (H3) nutrients and water temperature indirectly reduce phytoplankton community stability via biodiversity. The structural equation model (SEM) found that functional diversity (community-weighted means of traits and functional divergence) had significant negative correlations with phytoplankton community stability ( p < 0.05), while the species diversity had no significant correlation with phytoplankton community stability ( p > 0.05). This finding partially supported the hypothesis H1, which suggested that the functional diversity had a closer tie with stability than the species diversity. SEM did not find any direct effect of environmental factors on phytoplankton community stability, which rejected our hypothesis H2. Instead, SEM found that water temperature and phosphate decreased phytoplankton community stability by increasing the first principal component of the community-weighted means of traits (CWM_PC1), which supported hypothesis H3. Further analysis showed that the increased water temperature and phosphate concentration can promote “r-strategists” species (larger CWM_PC1), which are less resistant to environmental disturbances, therefore decreasing the phytoplankton community stability. Our study highlights the importance of functional diversity in maintaining the relationship between biodiversity and stability in the phytoplankton community, which may provide a mechanistic understanding of the biodiversity-stability relationships in aquatic ecosystems.
... Root foraging behavior has a higher complexity for plants acclimated to karst soils. High Ca in karst soils can directly generate a stress that may induce a greater allocation of dry mass to roots [29] but may also influence root tissue density [30]. The response of root size to Ca stress increases uncertainties in foraging scale. ...
Article
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Ecosystem is vulnerable due to large areas of rocky desertification, which results in patchy soils and inlaid stone soils. Karst landform is typically characterized by heterogeneous phosphorus (P) distributions in soils at high calcium (Ca), but root foraging behavior has not been fully docu-mented in agronomical plants. In this study, Bidens pilosa and Plantago asiatica were raised in pots in a simulated soil environment with sands at high Ca (2.00 g kg-1) and low Ca levels (0.63 g kg-1). Inner spaces were divided into four sections to receive P in homogeneous (Homo.) (four quarters: 2.00 mg P kg-1) or heterogenous (Hete.) (one quarter: 8.00 mg P kg-1; three quarters: no-P input) patterns. Both species had longer roots in high P sections compared to no P sections. Foraging scale (highest length or SA) was higher in P. asiatica plants subjected to the Hete. pattern than to the Homo. pattern in low Ca pots. Foraging precision (length or SA differences between P patches as a proportion of the total) was also higher for P. asiatica subjected to the Hete. pattern but did not change in response to Ca level or P placement pattern. Overall, P. asiatica has a higher foraging ability than B. pilosa due to higher levels of foraging scale and precision from high-P (8.00 mg kg-1) patches in soils subjected to low Ca (0.63 g kg-1).
... Studies have reported a negative correlation between resistance (inverse of impact) and recovery (also named as resilience in many cases) (Gazol et al., 2017;MacGillivray and Grime, 1995;Orwin et al., 2006;Schwalm et al., 2017), which indicates that there is a trade-off between resistance and recovery. As in Stuart-Haëntjens et al. (2018), our study does not support the assumption of a trade-off between resistance and recovery. ...
Article
The concept of resilience can be helpful in describing the relationship between vegetation and climate, especially when considering the likelihood of more extreme climate events due to global warming. However, the quantification and characterization of resilience is a challenge, due to the inherent complexity of the concept, as well as difficulty in comparing different ecosystems across the globe. In order to explore ecosystem resilience to drought, we estimated the resilience and related metrics from a series of land surface model (LSM) simulations with altered climate forcing data, focusing on the responses to changing precipitation. These simulations were performed in the semi-arid region of Caatinga biome, northeastern Brazil. Results showed that the quantification of resilience can be represented as a function between precipitation variation and gross primary productivity (GPP) variation. We compared the resilience components estimated for different vegetation types, which showed differences in the response of vegetation to precipitation variability. The study shows the potential of using LSMs to improve our understanding of the vegetation response to climate change, allowing us to explore possible scenarios that are usually not available in field experiments.
... Extreme droughts have significant ecological impacts on semi-arid grassland ecosystems (Cherwin and Knapp, 2012;Luo et al., 2018;Luo et al., 2019;Yue et al., 2019). The drought resistance of an ecosystem is defined as its ability to maintain ecosystem function during drought (Macgillivray et al., 1995). Understanding how drought resistance changes through time during extended droughts (Smith, 2011) is critical for predicting impacts of future droughts on ecosystem function. ...
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Globally, extreme droughts are likely to become more frequent, more intense, and longer in duration with climate change. Understanding the impacts of drought on ecosystem function (i.e., resistance) and its recovery after drought (i.e., resilience) is critical for long-term sustainability of ecosystem services under climate change. We tested the effects of drought duration on ecosystem resistance by imposing four years of extreme drought (<5th percentile), and examined resilience by imposing two years of extreme drought followed by two years of recovery in a semi-arid grassland in Inner Mongolia, China. We found that the resistance of aboveground net primary productivity (ANPP) decreased as the drought progressed, i.e., ANPP was reduced from 33% in the first treatment year and 60% in the fourth treatment year. Resilience of the ecosystem was such that ANPP of drought plots was 83% of ambient plots one year post-drought. By the second year, ANPP of the drought plots fully recovered to ambient plot levels. Decreasing drought resistance through time was largely driven by forb reductions. High resilience of the system was due to grasses compensating for reductions in forb productivity. Based on these findings, we suggest that droughts may have progressively larger impacts as their duration increases , so single year responses may underpredict the effects of longer droughts likely to occur in the future. Additionally, longer recovery times after extreme drought events may be critical to ensure resilience and recovery of all plant functional types. Overall, we suggest that management should strive to support and maintain the high proportion of high drought resistance and resilience plant functional types in the community may enhance the stability of biomass production in a future climate with longer and more intense extreme droughts.
... two ecoregions. This study confirms that resistance and resilience are inversely correlated, which is consistent with previous studies (Leps et al., 1982;Macgillivray et al., 1995;van Ruijven and Berendse, 2010) who reported decreasing resistance and increasing resilience to extreme dry events across different vegetation types. Several studies reported that ecosystem resilience is lower after dry events due to changes in species composition during dry periods and increase of resource competition after dry events (e.g., Isbell et al., 2015;De Keersmaecker et al., 2016) and drought memory effects (Liu et al., 2018a(Liu et al., , 2018b, while our study showed an apparent higher resilience after dry events in cold steppe and humid temperate ecoregions. ...
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The growing season normalized difference vegetation index (NDVIGS) of vegetation and their responses to climate extremes are critical in assessing the resistance and resilience of the terrestrial ecosystem. Using satellite-derived NDVIGS and widely used Standardized Precipitation and Evapotranspiration Index (SPEI) datasets of 18 sites in cold steppe, humid temperate and temperate dry steppe ecoregions for the period of 1982-2012, the NDVIGS response, resistance, and resilience to climate extreme intensity were assessed. The results showed that the mean NDVIGS varied significantly across ecoregions, where higher mean NDVIGS was observed in humid temperate and lower was in temperate dry steppe. The NDVIGS at most sites in three ecoregions showed significantly positive correlations with increasing SPEI. The responses of NDVIGS to climate extreme intensity revealed that moderate and extreme dry events decreased NDVIGS, while moderate and extreme wet events increased NDVIGS in all ecoregions. The results showed that vegetation resistance and resilience were highly dependent on climate extreme intensity. Resistance and resilience to moderate wet, extreme wet, moderate dry and extreme dry events in all ecoregions varied significantly, where vegetation in cold steppe and humid temperate ecoregions showed lower resistance but higher resilience to moderate and extreme dry events, and higher resistance but lower resilience to moderate and extreme wet events. Vegetation in temperate dry steppe showed higher resistance to moderate dry and higher resilience to moderate wet events. The study results suggest that more productive ecosystems (i.e. higher NDVIGS in cold steppe and humid temperate ecoregions) generally provide a lower (higher) resistance but higher (lower) resilience to dry (wet) events. Knowledge from this study also implies that less productive ecosystem (i.e. lower NDVIGS in temperate dry steppe) provides higher resistance to moderate dry and higher resilience after moderate wet events. This study highlights the impacts of climate extremes on NDVIGS, and improves our understanding of the resistance and resilience of vegetation to climate extreme intensity, which is of importance in the face of climate change.
... La resistencia consiste en la capacidad del ecosistema de tolerar el impacto inmediato de un disturbio exógeno (Hodgson et al., 2015). En la práctica, se identifica como la disminución del valor en alguno de los atributos del ecosistema durante el disturbio o inmediatamente al finalizar el mismo y se puede estimar a través de la relación entre el valor que adopta el atributo antes y durante el disturbio (Kaufman, 1982;Lloret et al., 2011;MacGillivray y Grime, 1995). Por otra parte, la recuperación corresponde al restablecimiento del atributo afectado después del disturbio y se reconoce como un aumento en el valor del atributo afectado; se estima como la relación entre el valor del atributo una vez finalizado el disturbio y el valor adquirido durante el restablecimiento (Lloret et al., 2011). ...
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Este trabajo fue el último en el que participó el Dr Miguel Angel Martínez Morales (sin acento en Angel como él me corregía). Mi más profundo agradecimiento por la manera tan propositiva en la que siempre me brindó su apoyo durante mi doctorado. QEPD. RESUMEN. En este estudio se analizan los patrones de recuperación de la estructura, la composición y la diversidad de plantas en bosques secundarios de bosque tropical seco (BTS) en paisajes agrícolas de Tehuantepec, Oaxaca. Para ello, se estableció una cronosecuencia con 19 parcelas (incluyendo una de bosque maduro) de 20 m × 20 m con una edad conocida de abandono de entre 3 y 50 años. En cada parcela se censaron las plantas leñosas con diámetro a la altura del pecho mayor o igual a 5 cm; se identificaron las especies y se registró su diámetro y altura. Los resultados indican que tras el abandono de la actividad agrícola, los bosques se regeneran naturalmente, lo cual debe considerarse en las estrategias para la conservación de los BTS frente al cambio global. Asimismo, la composición de especies presente en los bosques secundarios puede ayudar a guiar las estrategias de restauración ecológica activa que aceleren el proceso de sucesión ecológica. La resiliencia ecológica del BTS en áreas de abandono agrícola está dada por la recuperación de atributos más que por la resistencia al disturbio agrícola.
... Several studies proved that ecosystem processes are mainly determined by functions of organisms rather than populations (Leps et al., 1982). For example, the differences in the response of five adjacent grasslands in northern England to frost, drought and fire can be predicted from the functional characteristics of the dominant vegetation, unrelated to the population of vegetation (Grime, 1997;MacGillivray and Grime, 1995;Schwartz et al., 2000). It indicated a biodiversity conservation project solely based on species richness rather than comprehensive consideration of the entire evolution of species would fail to identify the most crucial habitats for the conservation of species genetic information (Smith et al., 1993). ...
Article
Although the knowledge and understanding of biodiversity is rapidly increasing, very little of the total biodiversity is currently considered in applied conservation actions. In this sense, it is crucial to integrate independent fields of biodiversity models and perspectives with conservation issues, in particular, the views that address the links between biodiversity, ecosystem services and human well-being, species interaction, and focal charismatic species. This study overcomes the lack of framework necessary for this integration, and proposes three perspectives and approaches to assess biodiversity. The first perspective is biodiversity potential. It considers the correlation between renewable resources in local ecosystems and biodiversity potential, in terms of the possibility of maintaining a high degree of biodiversity. The energy cost is evaluated using both static and dynamic methods, based on the measure of the emergy of local renewable resources and of the total emergy throughput needed by components in ecosystem food webs, respectively, also highlighting the link between biodiversity and ecosystem services, species interactions via energy transfer respectively. The second perspective considers the contribution of biodiversity to human well-being, such as domestication. In this approach, we assess the contribution of biodiversity to humans by calculating the emergy of non-renewable resources required to domesticate animals or plants into agricultural products. The third perspective highlights the significance of local focal charismatic species to global biodiversity conservation. Taking rare species as an example, the emergy required to maintain rare species per unit area is used as a quantitative indicator of the role of local rare species in maintaining global biodiversity. By measuring biodiversity from these three perspectives (potential, contribution and significance) simultaneously, biodiversity conservation strategies are addressed for different regions. Taking China as a case study, it shows that the provinces featuring high potential, low contribution and low significance can moderately increase biodiversity development. The provinces with high significance to global biodiversity should strengthen conservation to halt biodiversity loss. The areas exhibiting overexploitation of biodiversity should in turn restrict biodiversity exploitation. The general approaches proposed in this study could be applied to different cases, situations and species, promoting the integration to biodiversity conservation actions at different scales.
... Based on these trade-offs, it is expected that communities dominated by slow-growing, conservative species are more stable over time and will be more resistant to extreme events [7,46,47]. First, the few existing results generally confirm the expectations that more conservative species have more stable populations [41,48], for example, characterized by higher leaf dry matter content (LDMC) and lower relative growth rates [37]. Second, communities dominated by plant species with greater LDMC are more stable, in terms of both composition and overall biomass [42,49]. ...
Article
Under global change, how biological diversity and ecosystem services are maintained in time is a fundamental question. Ecologists have long argued about multiple mechanisms by which local biodiversity might control the temporal stability of ecosystem properties. Accumulating theories and empirical evidence suggest that, together with different population and community parameters, these mechanisms largely operate through differences in functional traits among organisms. We review potential trait-stability mechanisms together with underlying tests and associated metrics. We identify various trait-based components, each accounting for different stability mechanisms, that contribute to buffering, or propagating, the effect of environmental fluctuations on ecosystem functioning. This comprehensive picture, obtained by combining different puzzle pieces of trait-stability effects, will guide future empirical and modeling investigations. Full text available till July 20 at https://authors.elsevier.com/a/1dAJLcZ3WqeVu
... These effects strongly depend on the type of climatic event climatic event type and its magnitude [15]. The effects of climate can be as follows: negative effects on community stability [16], extinction of species and plant communities [17], permanent changes on community [18], effects on individuals [16], shifts on ecotones [19], negative effects on amount of photosynthesis, productivity, carbon uptake, biotic interactions such as fine scale community assembly and functionality [20]. ...
Article
Species distribution models (SDMs) are useful tools for future potential distribution patterns of species in the face of climate change. Turkey is expected to be affected considerably from climatic change i.e., up to 6°C increase in temperature and 50% decrease in precipitation by 2070. Therefore, there is an urgent need for conservation and management practices for future patterns of species. It is aimed current and future (using CMIP5 projected to 2070) potential distribution areas of Campanula lyrata Lam., which is formerly an endemic species. To do this, presence-only data was used, which is obtained from the Global Biodiversity Information Facility (GBIF). Bioclimatic data from was downloaded from WorldClim dataset with 10 km2 resolution. Species distribution modelling was performed using R program. Two regression techniques and two machine learning techniques namely Generalized Linear Models (GLMs), Generalized Additive Models (GAMs), Support Vector Machine (SVM) and Random Forest (RF), were used, respectively. The bootstrapping method as partitioning resampling was also used for all analysis. Considerably high model performances as well as AUC values for all possible models were found. Significant range shifts between current and future climatic conditions were found. The most relevant relative importance variables were precipitation seasonality and precipitation of the wettest month. This study reveals the importance of the future distributional areas of species.Species distribution models (SDMs) are useful tools for future potential distribution patterns of species in the face of climate change. Turkey is expected to be affected considerably from climatic change i.e., up to 6°C increase in temperature and 50% decrease in precipitation by 2070. Therefore, there is an urgent need for conservation and management practices for future patterns of species. It is aimed current and future (using CMIP5 projected to 2070) potential distribution areas of Campanula lyrata Lam., which is formerly an endemic species. To do this, presence-only data was used, which is obtained from the Global Biodiversity Information Facility (GBIF). Bioclimatic data from was downloaded from WorldClim dataset with 10 km2 resolution. Species distribution modelling was performed using R program. Two regression techniques and two machine learning techniques namely Generalized Linear Models (GLMs), Generalized Additive Models (GAMs), Support Vector Machine (SVM) and Random Forest (RF), were used, respectively. The bootstrapping method as partitioning resampling was also used for all analysis. Considerably high model performances as well as AUC values for all possible models were found. Significant range shifts between current and future climatic conditions were found. The most relevant relative importance variables were precipitation seasonality and precipitation of the wettest month. This study reveals the importance of the future distributional areas of species.
... The rapid and severe human-caused contamination of aquatic ecosystems emphasizes the need to study the conditions allowing communities to persist and recover (Bell and Gonzalez 2011, Vander Wal et al. 2012, Geerts et al. 2015. We found that the temporal stability of the DO cycle could be maintained in an extremely acidified environment if the communities had previously been pre-exposed to moderate levels of the acid stressor (MacGillivray et al. 1995, Flöder and Hillebrand 2012, Wright et al. 2015. Prior exposure to acidification can attenuate the impact of strong acidification on the DO cycle's resistance and amplitude. ...
Article
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Ecosystem processes vary temporally due to environmental fluctuations, such as when variation in solar energy causes diurnal cycles in primary production. This normal variation in ecosystem functioning may be disrupted and even lost if taxa contributing to functioning go extinct due to environmental stress. However, when communities are exposed to the stress at sub‐lethal levels over several generations, they may be able to develop community‐level stress tolerance via ecological (e.g. species sorting) or evolutionary (e.g. selection for tolerant genotypes) mechanisms and thus avoid the loss of stability, as defined by the resistance of a process. Community tolerance to a novel stressor is expected to increase the resistance of key processes in stressed ecosystems. In freshwater communities we tested whether prolonged prior exposure to an environmental stressor, i.e. acidification, could increase ecosystem stability when the communities were exposed to a subsequent press perturbation of more severe acidification. As a measure of ecosystem stability, we quantified the diurnal variation in dissolved oxygen (DO), and the resistance of the DO cycle and phytoplankton biomass. High‐frequency data from oxygen loggers deployed in 12 mesocosms showed that severe acidification with sulfuric acid to pH 3 could cause a temporary (i.e. two‐week long) loss of diurnal variation in dissolved oxygen concentration. The loss of diurnal variation was accompanied by a strong reduction in phytoplankton biomass. However, the pre‐exposure to acidification for several weeks resulted in the maintenance of the diurnal cycle and higher levels of phytoplankton biomass, though they did not return to as rapidly to pre‐exposure functioning as non‐exposed mesocosms. These results suggest that ecosystem stability is intrinsically linked to community‐wide stress tolerance, and that a history of exposure to the stressor may increase resistance to it, though at the cost of some resilience.
... Species that fall into the slow spectrum of the continuum (similar to K strategy) have a higher resistance to environmental oscillation, whereas the opposite occurs for species within the fast spectrum (r-related strategists), for which the reduced resistance can be compensated by higher resilience (Ricklefs & Wikelski, 2002;Royauté et al., 2018). Slow body growth has often been highlighted as central in determining population stability, which stresses the importance of the life-history trade-off between growth and reproduction (Leps et al., 1982;MacGillivray & Grime, 1995;Májeková et al., 2014). ...
Article
• Understanding the factors that regulate temporal changes in population size is a core aspiration in ecology given the importance of population stability on the maintenance of species interactions, effects on local communities, the stability of ecosystems, and for biodiversity conservation. Understanding temporal trends in population size can support management practices as this may indicate demographic resilience for exploited species. Theoretical studies have long suggested that life‐history traits regulate population stability, but empirical support remains limited, especially for species‐rich environments. Additionally, harvesting has been suggested as an important factor increasing the fluctuation in the number of individuals in populations. • In this study, we analysed population stability of 70 Amazonian floodplain fish species in relation to life‐history traits and the degree of fishing pressure. Our data covered a long time scale and broad geographical range of the Amazon floodplain. For that, we compiled datasets of two monitoring programmes, one comprising data from a single lake for 15 years and a second dataset with information from three floodplain lakes sampled over 5 years. The resulting geographical range spanned one of the most fished areas in the upper Amazon River, between the municipalities of Coari and Manaus, in the Brazilian Amazon. Temporal stability was measured as the coefficient of variation in species abundance. Population life‐history traits and the degree of fishing pressure were estimated at the species level. • Population temporal stability had significant relationships with three life‐history traits: maximum body size, fecundity, somatic investment before sexual maturation (SIBSM), and the interaction of fecundity and SIBSM. Species with small body size, high fecundity, and low SIBSM displayed low stability; the opposite happened to species that invest highly in somatic tissue before the first reproduction and have large body size. Fishing pressure had no significant contribution to explaining population stability. However, the sampling technique employed and the set of species considered in the study do not represent main targets of fisheries. • Here we stress the importance of life‐history traits in controlling an essential part of the population size variation in a complex and species‐rich fish assemblage in the Amazon floodplains. Our results highlight the importance of the trade‐off between growth and reproduction in controlling population stability and complement explanations on how life‐history functional traits underlie differences in population dynamics over time. Our results contribute to theoretical development and can be used to support fisheries and biological conservation management strategies. Specifically, our results point to the possibility of inferring demographic resilience based on life‐history information in the absence of high‐quality population data.
... Studies that have explored legacy effects of short-term environmental changes on plant communities have found variable results (Smith 2011), from transient responses (e.g., Arnone et al. 2011) to lasting alterations to community structure (e.g., MacGillivray and Grime 1995). Nonetheless, these studies typically only consider short-term (e.g., <1 yr) responses following pulse events, neglecting impacts in the later years following the event. ...
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... The cumulative effects of repeated extreme episodes or disturbances on community composition are typically assessed via changes in community resilience (MacGillivray & Grime, 1995). The concept of resilience broadly refers to the capacity of ecological systems to absorb disturbances and yet maintain structure and function (Walker et al., 2004). ...
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John Philip ‘Phil’ Grime developed fundamental theory in plant ecology that emerged from a lifetime of fieldwork and experimental studies in the Sheffield region, South Yorkshire, UK. His approach was an unusual combination of observation, experiment and theory: he conducted detailed, intensive observations of natural communities, alongside experimental manipulation of those communities and simulated ‘microcosms’ in the service of formulating general rules (‘strategies’) by which plants evolve with respect to their environment. In this way, Grime was one of several key figures that propelled plant ecology away from descriptive methods focusing on vegetation composition and toward a science more integrated with other fields, including evolutionary biology and Earth science. Grime's investigative approach was an inspiration for the modern field of global change biology, and, by focusing on understanding the contrasting roles species and their traits play in the functioning of ecosystems, marked the beginning of the field of plant functional ecology. For much of his career Grime held the post of full professor (and in retirement, emeritus professor of ecology) at the University of Sheffield, where he also served as the director of the Unit of Comparative Plant Ecology and of the Buxton Climate Change Impacts Laboratory. Awarded an honorary doctorate by Radboud University (Nijmegen, The Netherlands) and a foreign membership of the Royal Netherlands Academy of Arts and Sciences, Grime was the first person awarded the Alexander von Humboldt Award of the International Association for Vegetation Science.
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Background: In arid and semi-arid ecosystems in Argentina, dominance of shrublands and the search to increase the forage supply for livestock motivates interventions such as roller-chopping and hand-cutting to reduce the abundance of shrubs. However, an integral analysis of the effects of these practices from a sustainability point of view, including not only forage productivity but also other ecosystem service is still missing. We evaluated at the ecosystem level the impact of shrub removal on total production and phenology; at the local level the responses in cover, botanical composition and diversity of vegetation functional groups, as well as the effects on soil physical properties. We combined evaluation methodologies with remote sensing and field sampling in control (woodland, shrubland) and treated (roller chopping, hand cutting) sites in 16 paddocks. Results: In treated sites, grass cover increased significantly compared to untreated sites. However, total production, growing season length were reduced. Tree cover was lower in treated sites, while shrub cover was reduced in the hand-cutting compared to the other treatments. Forbs cover was not modified. In addition, species richness decreased in the treated sites, being higher in roller-chopped sites than in the hand-cut sites, while the species diversity index was only reduced in the latter type of disturbance. Soil mechanical resistance and bulk density were higher in treated sites, while infiltration rate did not change. Conclusions: shrub removal and pasture seeding on woodland and shrubland sites increases herbaceous forage production, but decreases total production and increases its temporal variability and rainfall dependence; it decreases functional diversity and increases surface soil compaction. These responses depend on the intensity of the woody biomass removal disturbance (roller-chopping or hand-cutting). In this respect, roller chopping appears to be a more conservative practice than hand cutting, as it maintains high levels of herbaceous forage production and functional diversity. However, it is necessary to consider the importance of maintaining native forest regeneration, as both types of disturbance affected this process. Our study highlights the importance to design selective interventions in the vegetation, compatible with the maintenance of functional diversity, the regeneration of tree strata and the increase in grass production.
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The biotic mechanisms underlying ecosystem functioning and stability have been extensively — but separately — explored in the literature, making it difficult to understand the relationship between functioning and stability. In this study, we used community models to examine how complementarity and selection, the two major biodiversity mechanisms known to enhance ecosystem biomass production, affect ecosystem stability. Our analytic and simulation results show that while complementarity promotes stability, selection impairs it. The negative effects of selection on stability operate through weakening portfolio effects and selecting species that have high productivity but low tolerance to perturbations (“risk‐prone” species). In contrast, complementarity enhances stability by increasing portfolio effects and reducing the relative abundance of risk‐prone species. Consequently, ecosystem functioning and stability exhibit either a synergy, if complementarity effects prevail, or trade‐off, if selection effects prevail. Across species richness levels, ecosystem functioning and stability tend to be positively related, but negative relationships can occur when selection co‐varies with richness. Our findings provide novel insights for understanding the functioning‐stability relationship, with potential implications for both ecological research and ecosystem management.
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Quantifying drought-induced ecosystem vulnerability, e.g. in terms of plant productivity, based on vulnerability curves and coupled processes is a frontier issue and a challenge in the field of climate change risk. Primary productivity vulnerability to drought varies among and within ecosystem types, obscuring generalized patterns of ecological stability. Thus, we constructed drought vulnerability curves between aboveground net primary productivity (ANPP) and drought intensity for forest and grassland, through global data collection, bias checking, and systematic integration. Based on the improvement of theoretical analysis of ecosystem vulnerability and quantitative evaluation methods, we investigated the processes of sensitivity and adaptation to reveal vulnerability mechanisms. The ANPP was nonlinearly reduced along with drought intensity gradients, with an increasing trend for forests and a decreasing trend for grasslands. Under the same drought duration, both the forest and grassland ANPP decreased with increasing intensities (from light to severe drought). However, the forest and grassland ANPP exhibited divergent responses with durations under the same drought intensity. The combinations of drought duration and intensities also affected the ANPP. For example, negative responses of the grassland ANPP to increasing intensities differed among the durations (p = 0.001) and maximum occurred under the severe drought. Furthermore, we quantified the vulnerability by analyzing sensitivity and adaptation to short- (≤ 3years) and long-term (> 3 years) drought. Grasslands showed higher sensitivity to short-term drought than to long-term drought, and the contrary for forests. Forests exhibited a certain adaptation to long-term drought, but to a lesser extent than grasslands. Comprehensively, grasslands presented lower vulnerability to growing-season drought with higher adaptation and lower sensitivity than forests. These findings suggest that quantitative assessment on ecosystem response to drought from the viewpoints of vulnerability curves and processes should be promoted in and coupled with future climate change risks and sustainable management of different ecosystems.
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Understorey vegetation is a key component of plant biodiversity in forests. Events of extreme drought are a potential major driver of change of this layer. Although these are predicted to increase in frequency and duration due to climate change, their impacts on understorey communities are still unknown. In this paper, we re-surveyed a set of 36 plots in mature thermophilous deciduous forests eight months after the end of an extremely dry period in 2016–2017. The plots are part of a European network representing a gradient of overstorey richness from 1- to 5-tree species mixtures, with variable composition. We took advantage of this model system to test the hypothesis that species richness and identity of dominant trees in the overstorey may modulate the impact of drought on understorey cover, diversity and composition. In spring 2018, a ca. 50% reduction of understorey cover occurred in both mono-specific and mixed plots. Species evenness and Shannon α-diversity increased in the monospecific plots, due to a reduction of abundance of tree species at juvenile stage and the appearance of non-forest specialists that did not occur in the mixtures. Overstorey species identity effects on understorey diversity were negligible. Overall compositional changes were moderate, though larger in the mixed plots and in those with the less drought-adapted tree species in the overstorey. Ellenberg ecological profile of the community did not change significantly but light values tended to increase in the monospecific plots, contrary to the mixtures. Overall, our findings provide circumstantial support to a higher diversity stability in the understorey of mixed plots shortly after drought, despite compositional variations. More studies and monitoring programs are needed to assess understorey recovery capacity and resilience after such events in the long-term.
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Resilience is the central concept for understanding how an ecosystem responds to a strong perturbation, and is related to other concepts used to analyze system properties in the face of change such as resistance, recovery, sustainability, vulnerability, stability, adaptive capacity, regime shift, and tipping point. It is extremely challenging to formulate resilience thinking into practice. The current state-of-art approaches of assessing ecosystem resilience may be useful for policy makers and ecosystem resource managers to minimize climatological or natural disaster related impacts. Here, we review the methods of assessing resilience and classify and limit them to three cases: (a) forest resilience based mainly on remote sensing and tree-ring data; (b) soil microbial community resilience based on laboratory and field studies; and (c) hydrological resilience of terrestrial biomes based on the Budyko framework and climate data.
Thesis
Dans le contexte actuel du changement climatique et de l’augmentation de la fréquence et de l’intensité des épisodes climatiques extrêmes, une question centrale pour l’écologie scientifique est de comprendre les répercussions de ces changements sur le fonctionnement des écosystèmes. Les communautés microbiennes du sol contrôlent une grande partie des processus écosystémiques déterminant la circulation de l’énergie et des nutriments. Dans le cadre des agroécosystèmes se pose donc la question de l’influence des pratiques agricoles sur les communautés microbiennes du sol et sur leur aptitude à maintenir le fonctionnement des écosystèmes face au changement climatique. L’intensification écologique de l’agriculture a récemment été proposée comme une approche intégrant les processus écologiques dans la stratégie de gestion des agroécosystèmes, dans l’objectif d’optimiser leur fonctionnement et leur résilience. L’écologie fonctionnelle pourrait répondre à certains des enjeux posés par le changement climatique et l’intensification écologique de l’agriculture.Dans cette thèse, j’ai cherché à mobiliser le cadre conceptuel des traits fonctionnels pour apporter de nouveaux éléments de compréhension de l’influence de différentes modalités d’intensité de gestion d’agroécosystèmes prairiaux (gestion extensive, conventionnelle-intensive et écologiquement-intensive) : 1) sur les caractéristiques fonctionnelles des communautés microbiennes du sol; 2) sur la capacité de ces communautés microbiennes à maintenir le fonctionnement de l’écosystème face à des périodes de stress climatiques (résilience). Dans le cadre de ma thèse, trois expérimentations ont été réalisées en faisant varier le degré de contrôle des facteurs de gestion, le type de stress climatique et la durée de ces stress. S’appuyant sur des agroécosystèmes prairiaux répartis dans trois pays Européens (France, Suisse, Portugal), les résultats des deux premières expérimentations de cette thèse montrent que les communautés microbiennes des sols des prairies écologiquement-intensives disposent d’une plus faible capacité à maintenir les propriétés écosystémiques microbiennes durant les stress (faible résistance) mais disposent d’une meilleure capacité de récupération comparée aux communautés microbiennes des sols en gestion conventionnelle-intensive. Une autre étude montre que la gestion éco-intensive favorise des communautés microbiennes protéolytiques bénéfiques à l’assimilation de l’azote pour les plantes en conditions perturbés. L’étude des traits végétaux suggère que ces effets de la gestion sur la composition des communautés microbiennes et sur leur résilience passe par certains traits, notamment une augmentation de la richesse en phosphore des litières en gestion écologiquement-intensive. En effet ces traits fonctionnels des plantes semblent influencer les traits microbiens, favorisant des communautés microbiennes copiotrophes, caractérisées par un ratio azote:phospore faible de leur biomasse et un faible investissement dans la production d’enzymes extracellulaires, deux traits négatifs pour la résistance au stress mais favorisant une récupération rapide. Ainsi, ces deux expérimentations soulignent l’importance de la gestion des traits des plantes dans le contrôle des traits microbiens et de la résilience des écosystèmes au changement climatique. La troisième expérimentation a cherché à tester spécifiquement les effets d’un épisode de fertilisation minérale sur la résilience des communautés microbiennes à différents stress climatiques. Les résultats montrent que la fertilisation modifie la composition et les traits microbiens avec des répercussions négatives sur la stabilité de l’écosystème face à la sécheresse et à l’inondation.Mobilisant une approche par le concept de trait fonctionnel microbien, ce travail de thèse apporte de nouveaux éléments de compréhension des effets de l’intensité de gestion sur la résilience des écosystèmes prairiaux face aux stress climatiques.
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