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Resistance of ecosystem services to global change weakened by increasing number of environmental stressors

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Resistance of ecosystem services to global change weakened by increasing number of environmental stressors | Nature Geoscience

Abstract

Terrestrial ecosystems are subjected to multiple global changes simultaneously. Yet, how an increasing number of global changes impact the resistance of ecosystems to global change remains virtually unknown. Here we present a global synthesis including 14,000 observations from seven ecosystem services (functions and biodiversity), as well as data from a 15-year field experiment. We found that the resistance of multiple ecosystem services to global change declines with an increasing number of global change factors, particularly after long-term exposure to these factors. Biodiversity had a higher resistance to multiple global changes compared with ecosystem functions. Our work suggests that we need to consider the combined effects of multiple global changes on the magnitude and resistance of ecosystem services worldwide, as ecosystem responses will be enhanced by the number of environmental stressors and time of exposure.

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Data availability

The data supporting the findings of this study are available from figshare at https://doi.org/10.6084/m9.figshare.26200925(ref. 47).

Code availability

The code associated with this study is available from figshare at https://doi.org/10.6084/m9.figshare.26202050(ref. 48).

1.
Rillig, M. C. et al. Increasing the number of stressors reduces soil ecosystem services worldwide. Nat. Clim. Change 13, 478–483 (2023).
2.
Zandalinas, S. I. & Mittler, R. Plant responses to multifactorial stress combination. N. Phytol. 234, 1161–1167 (2022).
3.
Peters, M. et al. Climate–land-use interactions shape tropical mountain biodiversity and ecosystem functions. Nature 568, 88–92 (2019).
4.
Rillig, M. C. et al. The role of multiple global change factors in driving soil functions and microbial biodiversity. Science 366, 886–890 (2019).
5.
Terrer, C. et al. A trade-off between plant and soil carbon storage under elevated CO2. Nature 591, 599–603 (2021).
6.
Zhou, G. et al. Temperature and rainfall patterns constrain the multidimensional rewilding of global forests. Adv. Sci. 9, 2201144 (2022).
7.
Zhou, L. et al. Global systematic review with meta-analysis shows that warming effects on terrestrial plant biomass allocation are influenced by precipitation and mycorrhizal association. Nat. Commun. 13, 4914 (2022).
8.
Delgado-Baquerizo, M. et al. Soil microbial communities drive the resistance of ecosystem multifunctionality to global change in drylands across the globe. Ecol. Lett. 20, 1295–1305 (2017).
9.
Yang, G. et al. Multiple anthropogenic pressures eliminate the effects of soil microbial diversity on ecosystem functions in experimental microcosms. Nat. Commun. 13, 4260 (2022).
10.
Zandalinas, S. I. et al. The impact of multifactorial stress combination on plant growth and survival. N. Phytol. 230, 1034–1048 (2021).
11.
Orwin, K. H. & Wardle, D. A. New indices for quantifying the resistance and resilience of soil biota to exogenous disturbances. Soil Biol. Biochem. 36, 1907–1912 (2004).
12.
Isbell, F. et al. Biodiversity increases the resistance of ecosystem productivity to climate extremes. Nature 526, 574–577 (2015).
13.
Craven, D. et al. Multiple facets of biodiversity drive the diversity–stability relationship. Nat. Ecol. Evol. 2, 1579–1587 (2018).
14.
Ochoa-Hueso, R. et al. Ecosystem coupling: a unifying framework to understand the functioning and recovery of ecosystems. One Earth 4, 951–966 (2021).
15.
Dukes, J. et al. Responses of grassland production to single and multiple global environmental changes. PLoS Biol. 3, e319 (2005).
16.
Kuussaari, M. et al. Extinction debt: a challenge for biodiversity conservation. Trends Ecol. Evol. 24, 564–571 (2009).
17.
Winfree, R. Global change, biodiversity and ecosystem services: what can we learn from studies of pollination? Basic Appl. Ecol. 14, 453–460 (2013).
18.
Komatsu, K. et al. Global change effects on plant communities are magnified by time and the number of global change factors imposed. Proc. Natl Acad. Sci. USA 116, 17867–17873 (2019).
19.
Dornelas, M. et al. Assemblage time series reveal biodiversity change but not systematic loss. Science 344, 296–299 (2014).
20.
Blowes, S. A. et al. The geography of biodiversity change in marine and terrestrial assemblages. Science 366, 339–345 (2019).
21.
Yachi, S. & Loreau, M. Biodiversity and ecosystem productivity in a fluctuating environment: the insurance hypothesis. Proc. Natl Acad. Sci. USA 96, 1463–1468 (1999).
22.
Byron, J. et al. Chiral monoterpenes reveal forest emission mechanisms and drought responses. Nature 609, 307–312 (2022).
23.
Reich, P. et al. Even modest climate change may lead to major transitions in boreal forests. Nature 608, 540–545 (2022).
24.
Liu, H. et al. Phenological mismatches between above- and belowground plant responses to climate warming. Nat. Clim. Change 12, 97–102 (2022).
25.
Liu, L. et al. A cross‐biome synthesis of soil respiration and its determinants under simulated precipitation changes. Glob. Change Biol. 22, 1394–1405 (2016).
26.
Zhou, G. et al. Effects of livestock grazing on grassland carbon storage and release override impacts associated with global climate change. Glob. Change Biol. 25, 1119–1132 (2019).
27.
Hunt, H. & Wall, D. Modelling the effects of loss of soil biodiversity on ecosystem function. Glob. Change Biol. 8, 33–50 (2008).
28.
Shaw, M. et al. Grassland responses to global environmental changes suppressed by elevated CO2. Science 298, 1987–1990 (2002).
29.
Zhu, K. et al. Nonlinear, interacting responses to climate limit grassland production under global change. Proc. Natl Acad. Sci. USA 113, 10589–10594 (2016).
30.
Yang, S. et al. Fire affects the taxonomic and functional composition of soil microbial communities, with cascading effects on grassland ecosystem functioning. Glob. Change Biol. 26, 431–442 (2020).
31.
Møller, A. P. & Jennions, M. D. Testing and adjusting for publication bias. Trends Ecol. Evol. 16, 580–586 (2001).
32.
Mooney, K. A. et al. Interactions among predators and the cascading effects of vertebrate insectivores on arthropod communities and plants. Proc. Natl Acad. Sci. USA 107, 7335–7346 (2010).
33.
Viechtbauer, W. Conducting meta-analyses in R with the metafor package. J. Stat. Softw.
https://doi.org/10.18637/jss.v036.i03(2010).
34.
Eldridge, D. & Delgado-Baquerizo, M. Continental-scale impacts of livestock grazing on ecosystem supporting and regulating services. Land Degrad. Dev. 28, 1473–1481 (2017).
35.
Delgado-Baquerizo, M. et al. Microbial diversity factors multifunctionality in terrestrial ecosystems. Nat. Commun. 28, 10541 (2016).
36.
Poorter, L. et al. Multidimensional tropical forest recovery. Science 374, 1370–1376 (2021).
37.
Epskamp, S. & Fried, E. I. A tutorial on regularized partial correlation networks. Psychol. Methods 23, 617–634 (2016).
38.
Migliavacca, M. et al. The three major axes of terrestrial ecosystem function. Nature 598, 468–472 (2021).
39.
Lahouar, A. & Slama, J. B. H. Day-ahead load forecast using random forest and expert input selection. Energy Convers. Manag. 103, 1040–1051 (2015).
40.
Fick, S. E. & Hijmans, R. J. WorldClim 2: new 1‐km spatial resolution climate surfaces for global land areas. Int. J. Climatol. 37, 4302–4315 (2017).
41.
Poggio, L. et al. SoilGrids 2.0: producing soil information for the globe with quantified spatial uncertainty. Soil 7, 217–240 (2021).
42.
Loveland, T. R. et al. An analysis of the IGBP global land-cover characterization process. Photogramm. Eng. Rem. S. 65, 1021–1032 (1999).
43.
Warner, D. L., Bond-Lamberty, B., Jian, J., Stell, E. & Vargas, R. Spatial predictions and associated uncertainty of annual soil respiration at the global scale. Glob. Biogeochem. Cycles 33, 1733–1745 (2019).
44.
Piñeiro, G., Perelman, S., Guerschman, J. P. & Paruelo, J. M. How to evaluate models: observed vs. predicted or predicted vs. observed? Ecol. Model. 216, 316–322 (2008).
45.
UNEP-WCMC. A spatial analysis approach to the global delineation of dryland areas of relevance to the CBD Programme of Work on Dry and Subhumid Lands. Dataset based on spatial analysis between WWF terrestrial ecoregions (WWF-US, 2004) and aridity zones (CRU/UEA; UNEPGRID, 1991). Dataset checked and refined to remove many gaps, overlaps and slivers (July 2014). UNEP-WCMC
https://resources.unep-wcmc.org/products/789fcac8959943ab9ed7a225e5316f….
46.
Mallavan, B. P., Minasny, B. & McBratney, A. B. in Digital Soil Mapping Progress in Soil Science (eds Boettinger Howell, J. L. et al.) 137–150 (Springer, 2010).
47.
Zhou, G. Database.xls. figshare
https://doi.org/10.6084/m9.figshare.26200925(2024).
48.
Zhou, G. Code.pdf. figshare
https://doi.org/10.6084/m9.figshare.26202050(2024).

Acknowledgements

We acknowledge B. A. Hungate, C. B. Field and N. R. Chiariello for use of the plant biomass data from the Jasper Ridge Global Change Experiment. We thank all the scientists whose data and work were included in the global analysis. G.Z. and N.E. acknowledge support by iDiv (German Research Foundation [DFG]–FZT 118, 202548816) and the Gottfried Wilhelm Leibniz Prize (DFG; Ei 862/29-1), both granted by the German Research Foundation. The Jena Experiment is funded by the DFG (FOR 5000). G.Z. acknowledges funding from Spanish Ministry of Science and Innovation through a Ramón y Cajal Fellowship (RYC2022-035226-I), the NextGenerationEU programme of the European Union (MICIU/AEI/10.13039/501100011033y el FSE+) and the AYUDAS DE EXCELENCIA RYC-MAX 2023 project from the Spanish National Research Council. M.D.-B. acknowledges support from the Spanish Ministry of Science and Innovation for the I + D + i project PID2020-115813RA-I00 funded by MCIN/AEI/10.13039/501100011033. M.D.-B. is also supported by a project of the Fondo Europeo de Desarrollo Regional (FEDER) and the Consejería de Transformación Económica, Industria, Conocimiento y Universidades of the Junta de Andalucía (FEDER Andalucía 2014-2020 Objetivo temático ‘01 – Refuerzo de la investigación, el desarrollo tecnológico y la innovación’) associated with the research project P20_00879 (ANDABIOMA). M.B. acknowledges funding from Spanish Ministry of Science and Innovation through a Ramón y Cajal Fellowship (RYC2021-031797-I). D.J.E. is supported by the Hermon Slade Foundation. L.Z. acknowledges support by the National Natural Science Foundation of China (grant no. 32071593). X.Z. acknowledges support by the National Natural Science Foundation of China (grants nos. 31930072, 32241032 and 42261144688).

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Nature Geoscience thanks Masahiro Ryo, Jens-Arne Subke and the other, anonymous, reviewer(s) for their contribution to the peer review of this work. Primary Handling Editor: Xujia Jiang, in collaboration with the Nature Geoscience team.

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Extended data

Extended Data Fig. 1 The multiservice resistance of plant diversity (A) and microbial diversity (B) to single and multiple (>1) global change factors.

Data are presented with mean±bootstrap 95% confidence interval (CI). Kruskal-Wallis test was performed to examine the significant difference in multiservice resistance among two levels of global change factors. Number values with red and green color indicate the number of studies and samples, respectively.

Extended Data Fig. 2 Heat map showing the two-sided spearman correlation between between the resistance of multiple ecosystem services and environmental factors including climate, soil properties and duration of experiments.

(P < 0.05). GCFs, global change factors.

Extended Data Fig. 3 Maps of uncertainty in resistance for one and two and three global change factors.

A, B, and C respectively based on Mahalanobis distance. Areas of high uncertainty are spatially represented in red, while areas of low uncertainty are represented in blue. Gray areas represent areas with no data.

Extended Data Fig. 4 Predicted distribution of multiservice resistance in response to an increasing number of global change factors based on machine learning modelling.

This figure shows the distribution of multiservice resistance under three global change factors (25 km / pixel). The R2 value determined as predicted vs. observed multiservice resistance is 0.64. The gray color corresponds to areas without data, and the white color to areas masked as outliers. A map including information on model uncertainties is available in Extended Data Fig. 3. Due to the relatively lower number of samples this map needs to be considered with caution.

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Zhou, G., Eisenhauer, N., Terrer, C. et al. Resistance of ecosystem services to global change weakened by increasing number of environmental stressors. Nat. Geosci. (2024). https://doi.org/10.1038/s41561-024-01518-x

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DOI: https://doi.org/10.1038/s41561-024-01518-x