Abstract
Shifts in phenology with climate change can lead to asynchrony between interacting species, with cascading impacts on ecosystem services. Previous meta-analyses have produced conflicting results on whether asynchrony has increased in recent decades, but the underlying data have also varied—including in species composition, interaction types and whether studies compared data grouped by trophic level or compared shifts in known interacting species pairs. Here, using updated data from previous studies and a Bayesian phylogenetic model, we found that species have advanced an average of 3.1 days per decade across 1,279 time series across 29 taxonomic classes. We found no evidence that shifts vary by trophic level: shifts were similar when grouped by trophic level, and for species pairs when grouped by their type of interaction—either as paired species known to interact or as randomly paired species. Phenology varied with phylogeny (λ = 0.4), suggesting that uneven sampling of species may affect estimates of phenology and potentially phenological shifts. These results could aid forecasting for well-sampled groups but suggest that climate change has not yet led to widespread increases in phenological asynchrony across interacting species, although substantial biases in current data make forecasting for most groups difficult.
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Data availability
All data we scraped is available through the Knowledge Network for Biocomplexity (https://doi.org/10.5063/F12J69B2)56.
Code availability
Code developed for this analysis is available through the Knowledge Network for Biocomplexity (https://doi.org/10.5063/F12J69B2)56.
References
Parmesan, C. & Yohe, G. A globally coherent fingerprint of climate change impacts across natural systems. Nature 421, 37–42 (2003).
Parmesan, C. Influences of species, latitudes and methodologies on estimates of phenological response to global warming. Glob. Chang. Biol. 13, 1860–1872 (2007).
Root, T. L. et al. Fingerprints of global warming on wild animals and plants. Nature 421, 57–60 (2003).
Menzel, A. et al. European phenological response to climate change matches the warming pattern. Glob. Chang. Biol. 12, 1969–1976 (2006).
Vitasse, Y. et al. Phenological and elevational shifts of plants, animals and fungi under climate change in the European Alps. Biol. Rev. 96, 1816–1835 (2021).
Stenseth, N. C. & Mysterud, A. Climate, changing phenology, and other life history traits: nonlinearity and match–mismatch to the environment. Proc. Natl Acad. Sci. USA 99, 13379–13381 (2002).
Kharouba, H. M. & Wolkovich, E. M. Disconnects between ecological theory and data in phenological mismatch research. Nat. Clim. Change 10, 406–415 (2020).
Lindén, A. Adaptive and nonadaptive changes in phenological synchrony. Proc. Natl Acad. Sci. USA 115, 5057–5059 (2018).
Forrest, J. R. K. Complex responses of insect phenology to climate change. Curr. Opin. Insect Sci. 17, 49–54 (2016).
Beard, K. H., Kelsey, K. C., Leffler, A. J. & Welker, J. M. The missing angle: ecosystem consequences of phenological mismatch. Trends Ecol. Evol. 34, 885–888 (2019).
Fang, J., Lutz, J. A., Wang, L., Shugart, H. H. & Yan, X. Using climate-driven leaf phenology and growth to improve predictions of gross primary productivity in North American forests. Glob. Chang. Biol. 26, 6974–6988 (2020).
Gu, H. et al. Warming-induced increase in carbon uptake is linked to earlier spring phenology in temperate and boreal forests. Nat. Commun. 13, 1–8 (2022).
Visser, M. E. E. et al. Warmer springs lead to mistimes reproduction in great tits (Parus major). Proc. R. Soc. B 265, 1867–1870 (1998).
Cresswell, W. & McCleery, R. How great tits maintain synchronization of their hatch date with food supply in response to long-term variability in temperature. J. Anim. Ecol. 72, 356–366 (2003).
Visser, M. E., Lindner, M., Gienapp, P., Long, M. C. & Jenouvrier, S. Recent natural variability in global warming weakened phenological mismatch and selection on seasonal timing in great tits (Parus major). Proc. R. Soc. B 288, 1–10 (2021).
Thackeray, S. J. et al. Phenological sensitivity to climate across taxa and trophic levels. Nature 535, 241–245 (2016).
Cohen, J. M., Lajeunesse, M. J. & Rohr, J. R. A global synthesis of animal phenological responses to climate change. Nat. Clim. Change 8, 224–228 (2018).
Kharouba, H. M. et al. Global shifts in the phenological synchrony of species interactions over recent decades. Proc. Natl Acad. Sci. USA 115, 5211–5216 (2018).
Davis, C. C., Willis, C. G., Primack, R. B. & Miller-rushing, A. J. The importance of phylogeny to the study of phenological response to global climate change. Phil. Trans. R. Soc. Lond. B 365, 3201–3213 (2010).
Philippart, C. J. et al. Climate-related changes in recruitment of the bivalve Macoma balthica. Limnol. Oceanogr. 48, 2171–2185 (2003).
Lane, J. E., Kruuk, L. E., Charmantier, A., Murie, J. O. & Dobson, F. S. Delayed phenology and reduced fitness associated with climate change in a wild hibernator. Nature 489, 554–558 (2012).
Renner, S. S. & Zohner, C. M. Climate change and phenological mismatch in trophic interactions among plants, insects, and vertebrates. Annu. Rev. Ecol. Evol. Syst. 49, 165–182 (2018).
Cushing, D. H. The regularity of the spawning season of some fishes. ICES J. Mar. Sci. 33, 81–92 (1969).
Cushing, D. H. Plankton production and year-class strength in fish populations: an update of the match/mismatch hypothesis. Adv. Mar. Biol. 26, 249–293 (1990).
Pagel, M. Inferring the historical patterns of biological evolution. Nature 401, 877–884 (1999).
Paquette, A., Joly, S. & Messier, C. Explaining forest productivity using tree functional traits and phylogenetic information: two sides of the same coin over evolutionary scale? Ecol. Evol. 5, 1774–1783 (2015).
Arim, M. & Marquet, P. A. Intraguild predation: a widespread interaction related to species biology. Ecol. Lett. 7, 557–564 (2004).
Williams, R. J. & Martinez, N. D. Limits to trophic levels and omnivory in complex food webs: theory and data. Am. Nat. 163, 458–468 (2004).
Lafferty, K. D., Dobson, A. P. & Kuris, A. M. Parasites dominate food web links. Proc. Natl Acad. Sci. USA 103, 11211–11216 (2006).
LaSalle, J. & Gauld, I. D. Parasitic Hymenoptera and the biodiversity crisis. Redia 74, 315–334 (1992).
Davies, T. J., Mcgill, B. J., Regetz, J. & Wolkovich, E. M. Phylogenetically weighted regression: a method for modelling non-stationarity on evolutionary trees. Glob. Ecol. Biogeogr. 28, 275–285 (2019).
Prather, R. M. et al. Current and lagged climate affects phenology across diverse taxonomic groups. Proc. R. Soc. B 290, 1–11 (2023).
Kraft, N. J. & Ackerly, D. D. Functional trait and phylogenetic tests of community assembly across spatial scales in an Amazonian forest. Ecol. Monogr. 80, 401–422 (2010).
Best, R. J. & Stachowicz, J. J. Phenotypic and phylogenetic evidence for the role of food and habitat in the assembly of communities of marine amphipods. Ecology 95, 775–786 (2014).
Diamond, S. E. Contemporary climate-driven range shifts: putting evolution back on the table. Funct. Ecol. 32, 1652–1665 (2018).
Descamps, S. et al. Diverging phenological responses of Arctic seabirds to an earlier spring. Glob. Chang. Biol. 25, 4081–4091 (2019).
Ge, Q., Wang, H., Rutishauser, T. & Dai, J. Phenological response to climate change in China: a meta-analysis. Glob. Chang. Biol. 21, 265–274 (2015).
Prevey, J. et al. Greater temperature sensitivity of plant phenology at colder sites: implications for convergence across northern latitudes. Glob. Chang. Biol. 23, 2660–2671 (2017).
Alecrim, E. F., Sargent, R. D. & Forrest, J. Higer-latitude spring-flowering herbs advance their phenology more than trees with warming temperatures. J. Ecol. 111, 156–169 (2023).
Thackeray, S. J. et al. Food web de-synchronisation in England’s largest lake: an assessment based uponmmultiple phenological metrics. Glob. Chang. Biol. 19, 3568–3580 (2013).
Iler, A. M. et al. Maintenance of temporal synchrony between syrphid flies and floral resources despite differential phenological responses to climate. Glob. Chang. Biol. 19, 2348–2359 (2013).
Burgess, M. D. et al. Tritrophic phenological match-mismatch in space and time. Nat. Ecol. Evol. 2, 970–975 (2018).
Cayuela, L., Granzow-de la Cerda, Í., Albuquerque, F. S. & Golicher, D. J. Taxonstand: an r package for species names standardisation in vegetation databases. Methods Ecol. Evol. 3, 1078–1083 (2012).
Chamberlain, S. A. & Szöcs, E. taxize: taxonomic search and retrieval in R. F1000Res. 2, 1–30 (2013).
Revell, L. J. phytools: an R package for phylogenetic comparative biology (and other things). Methods Ecol. Evol. 3, 217–223 (2012).
Paradis, E. & Schliep, K. ape 5.0: an environment for modern phylogenetics and evolutionary analyses in R. Bioinformatics 35, 526–528 (2019).
Smith, S. A. & O’Meara, B. C. TreePL: divergence time estimation using penalized likelihood for large phylogenies. Bioinformatics 28, 2689–2690 (2012).
Kumar, S., Stecher, G., Suleski, M. & Hedges, S. B. TimeTree: a resource for timelines, timetrees, and divergence times. Mol. Biol. Evol. 34, 1812–1819 (2017).
Booth, B. B. B., Dunstone, N. J., Halloran, P. R., Andrews, T. & Bellouin, N. Aerosols implicated as a prime driver of twentieth-century North Atlantic climate variability. Nature 484, 228–232 (2012).
Navarro, J. C. A. et al. Amplification of Arctic warming by past air pollution reductions in Europe. Nat. Geosci. 9, 277–281 (2016).
Morales-Castilla, I. et al. Phylogenetic estimates of species-level phenology improve ecological forecasting. Nat. Clim. Change (in the press).
Gelman, A., Hill, J., & Vehtari, A. Regression and Other Stories (Cambridge Univ. Press, 2020).
Stan Development Team. RStan: the R interface to Stan. R package version 2.17.3. http://mc-stan.org/ (2018).
R Core Team. R: a language and environment for statistical computing. (R Foundation for Statistical Computing, 2020); https://www.R-project.org/
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).
Loughnan, D. et al. Data and code: phenology varies with phylogeny with similar shifts by trophic level with climate change. knb https://doi.org/10.5063/F12J69B2 (2024).
Acknowledgements
We thank the many researchers, citizen scientists and organizations who contributed data, including S. Thackeray, J. Cohen, Rothamsted Insect Survey, UK Phenology Network, Woodland Trust and Centre for Ecology & Hydrology T. J. Davies provided comments that improved the manuscript. Funding was provided by a Natural Sciences and Engineering Research Council (NSERC) Canada Graduate Scholarship-Doctoral award to D.L. and Canada Research Chair award in Temporal Ecology and NSERC Discovery awards to E.M.W.
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Conceptualization: D.L. and E.M.W.; methodology: D.L., E.M.W., G.L., S.J. and M.B.; critical insights: D.L., E.M.W., G.L., S.J. and M.B.; writing—original draft: D.L. and E.M.W.; writing—review and editing: D.L., E.M.W., H.M.K., G.L., S.J. and M.B.
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Extended data
Extended Data Fig. 1 Conceptual diagram of how phenological shifts by interacting species pairs effect species synchrony.
A conceptual diagram of how species within an interacting pair may differ in their phenological shifts and the resulting effects on species synchrony. a, Within an interacting pair, illustrated here using a consumer and resource species (shown in blue and red respectively) as an example (though our data includes five types of interactions), the resource species may shift at a greater, lesser, or equal rate than their consumer. b, This results in different synchrony responses, with negative asynchrony occurring when the consumers phenology shifts earlier (dotdash line), positive asynchrony occurring when the resources phenology shifts earlier relative to the consumer (dashed line), and no change when both species shift at the same rate (solid line).
Extended Data Fig. 2 The global distribution of our phenological time-series and lack of variation with latitudinal gradients.
Species time-series were observed across the globe, but with strong biases towards certain regions, a, with point colour representing the original source of the dataset and point size the number of species within a dataset. b, The observed trends in species phenological shifts do not vary with latitude despite spanning latitudinal gradients across temperate ecosystems (Table ED1), as shown using points coloured to depict the magnitude of species shift per decade.
Extended Data Fig. 3 Species pairs exhibiting variable shifts in phenology and the resulting changes in synchrony.
To assess how pairs of species differ in their phenological shifts and synchrony, we randomly sampled 1000 posterior estimates from both the high and low-level species within each interaction, as shown here for two sets of species pairs. a, Some pairs differ in their phenological shifts, as shown for the interaction between Parus major and it’s caterpillar prey, b, while others shift at similar rates, shown here for Accipiter nisus and Parus ater. c, Changes in synchrony are calculated as the differences between the high-level species, shown here as predators, and the low-level species, or prey.
Extended Data Fig. 4 Species phenological synchrony across suites of interactions when simulated for terrestrial and aquatic interactions separately.
Species phenological synchrony across a, pollination (n = 47), b, predation (n = 24), c, herbivory (n = 10), and d, competitive (n = 18) interactions amongst terrestrial species (a–c), in comparison to e, predation (n = 13), f, herbivory (n = 10), and g, competitive (n = 54) interactions amongst aquatic species (e–g), showed no differences in the distributions of posterior estimates of consumer or resource species phenological shifts for pairs of known interacting species (in blue) and randomly paired species (in red) for any of the four types of interactions. Plots are normalized by counts, with the x-axis spanning the total density distribution. Above the figures, the two lines depict the 90% uncertainty intervals (thinner line) and 50% interval (thicker line), and the point the median.
Extended Data Fig. 5 Estimated phenological shifts of the well-studied interaction between Parus major and caterpillars.
Our model replicates the strong asynchronies found in interactions of well studied species pairs. Illustrated here is the classic example of the estimated phenological shifts of Parus major and caterpillars, shown across each type of phenological event represented in our dataset.
Extended Data Fig. 6 Species phenological shifts across trophic levels, consumer types, habitats, and types of phenological events.
Shifts in species phenology are similar across several grouping factors, in- cluding: a, trophic levels, b, consumer types, and c, habitat types. d, We also observed similar shifts across phenological events, with the exception of juvenile bird first ap- pearance. Eye-plots of the posterior estimates from our full phylogeny model (including phylogenetic effects, Table ED1) include a gray distribution as the density of the posteri- ors, black circles for the median value, thick dark lines depict the 50% quantile interval, and thin black lines depict the 90% quantile interval. Letters denote groups of species — f = fish, mo = mollusc, a = arachnids, am = amphibians, b = birds, c = copeopod, d = diatom, f = fish, fu = fungi, i = insects, m = mammals, p = plants, plk = plankton, t = turtle.
Extended Data Fig. 7 Trophic level differences across our species phylogeny and well-studied evolutionary lineages.
a, Within our highly diverse and global dataset, species trophic level is highly confounded with phylogeny, limiting our ability to model trophic level directly. This is further illustrated for the four most well-sampled evolutionary lineages in our dataset, each of which map strongly to certain trophic levels, b, as all plants are primary producers, c, while most insects are primary consumers, c, the majority of birds (aves) secondary consumers, d, and all of amphibia are secondary consumers.
Extended Data Fig. 8 Species phenological shifts with temperature change across study sites.
Shifts in species phenology show no strong relationships to the rate of temperature change at each site of observation across a & e, North America (n = 42 sites), b & f, Europe (n = 109 sites), c & g, the United Kingdom (n = 98 sites), d & h, or independent studies in the United Kingdom, not including data from RIS or the Woodland trust (n sites = 14). Analyses were replicated for both the three month period around which an event occurred (a–d) and for the annual monthly temperatures (e–h). Gray bands represent the 50% quantile interval and crosses the 50%.
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Loughnan, D., Joly, S., Legault, G. et al. Phenology varies with phylogeny but not by trophic level with climate change. Nat Ecol Evol 8, 1889–1896 (2024). https://doi.org/10.1038/s41559-024-02499-1
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DOI: https://doi.org/10.1038/s41559-024-02499-1