Introduction

Climate shifts are leading to rapid, species-specific changes in phenology and ecosystem productivity (Boisvenue & Running, 2006; Menzel et al., 2006; Yang & Rudolf, 2010; Thackeray et al., 2016). In temperate forests, changes in the timing of spring leaf-out, autumn leaf-senescence and bud set are modifying water, energy and carbon cycles (Peñuelas et al., 2009; Richardson et al., 2013), with extended growing seasons increasing net ecosystem carbon uptake by up to 9.8 gC m⁻² day⁻¹ (Keenan et al., 2014). Therefore, understanding the interaction between climate change and temperate forest phenology is pivotal to improving forecasts of community dynamics and carbon sequestration.

The past few decades have seen delays in the onset of temperate autumn phenology, but these changes are much smaller in magnitude compared to the advances in spring leaf-out observed during the same period (Gill et al., 2015; Piao et al., 2019). This is unexpected, given that experiments have demonstrated a high sensitivity of leaf senescence to autumn warming, with phenological responses even surpassing the temperature sensitivity (days per °C) of spring leaf-out (Fu et al., 2018). One possible explanation for this discrepancy is that other factors may counterbalance the effects of autumn warming, with some studies finding that earlier leaf-out leads to earlier leaf senescence (Fu et al., 2014; Keenan & Richardson, 2015; Zani et al., 2020). This connection between spring and autumn phenophases could be due to developmental and nutrient constraints that affect carbon source-sink dynamics in temperate trees (Paul & Foyer, 2001; Zani et al., 2020; Zohner et al., 2023; Gessler & Zweifel, 2024).

The Solstice-as-Phenology-Switch hypothesis, supported by experiments and monitoring data, posits that warmer air temperatures before the summer solstice accelerate tree growth and development, leading to an earlier onset of leaf senescence, whereas warmer temperatures after the solstice slow the progression of leaf senescence (Zohner et al., 2023). The opposite is equally true in colder years, with pre-solstice cooling delaying autumn phenology and post-solstice cooling advancing it. This reversal in temperature effects provides an explanation for the less pronounced shifts in autumn phenology compared to spring (Piao et al., 2019). The effect reversal after the solstice points to the role of photoperiod in regulating plant physiology (Bauerle et al., 2012; Petterle et al., 2013; Singh et al., 2017), with trees becoming increasingly responsive to cooling temperatures as days continue to shorten. The precise timing of this reversal appears to be flexible and has been advancing in recent decades, potentially due to faster development driven by climate warming (Zohner et al., 2023). For temperate trees, the key outcomes of development are production of viable seeds, cessation of primary and secondary growth, and maturation of perennating tissues including leaf or flower buds (completion of bud set) before the onset of frost (Rohde & Bhalerao, 2007; Tanino et al., 2010; Cooke et al., 2012). Because opportunities for development will vary among years, the timing of the temperature effect reversal should be flexible. However, this flexibility has yet to be demonstrated in processes directly related to development such as autumn bud set.

In this study, we investigate how air temperature changes around the summer solstice affect end-of-season (EOS) timing in European beech (Fagus sylvatica L.), using bud set and leaf senescence as key physiological markers of autumn phenology (Singh et al., 2017; Zohner & Renner, 2019; Mariën et al., 2021). We ask three main questions: i) How does cooling before vs. after the solstice affect EOS timing? ii) How do diel (daytime vs. nighttime) temperature changes differ in their effects? iii) Does the timing of leaf-out modulate the reversal of temperature effects on autumn phenology? Diel temperature variations are relevant because trees typically grow more at night when temperatures and water deficit are lower (Steppe et al., 2015; Mencuccini et al., 2017; Zweifel et al., 2021). Thus, developmental effects mediated by temperature may be especially pronounced during nights. Moreover, long-term trends in climate show that nighttime temperatures rose faster than daytime temperatures from 1950 to 2004 (Vose et al., 2005), though this trend may have shifted since 1991 (Zhong et al., 2023). To address the third question, we experimentally manipulated spring conditions to create early-leafing and late-leafing individuals within the same growing season, allowing us to assess whether slowed early-season development postpones the reversal date of temperature effects on autumn phenology (Fig. 1). As depicted in our conceptual model (Fig. 1), trees are dynamic systems that continuously integrate and adapt their physiological responses to environmental conditions over time. We therefore expected their temperature responses to differ both across months (June-August) and between day and night.

Figure 1.

Materials and Methods

Selected species

Fagus sylvatica L. has a large temperate European distribution, is highly economically and ecologically important, and is likely threatened by climate change (Gessler et al., 2006). Therefore, improving our understanding of how F. sylvatica’s growing season is modulated is vital to the management of European forests. Moreover, F. sylvatica has frequently been used as a key species to study temperate tree phenology (Dittmar & Elling, 2006; Vitasse et al., 2011; Zohner & Renner, 2019; Zani et al., 2020; Zohner et al., 2023; Mariën et al., 2025; Švik et al., 2025).

Experiment 1

To test the antagonistic effects of early-season development and late-season air temperature on autumn phenology, we set up an experimental population (n = 267) of 40-60 cm tall European beech (F. sylvatica) trees in Zurich, Switzerland in 2023. The trees were sourced from a local nursery, and each tree was placed individually in a 20 L plastic pot containing a 1:1:1 sand / peat / organic soil mixture with a Nitrogen (N) concentration of ∼65 g m⁻³, a Phosphate (P₂O₅) concentration of ∼140 g m⁻³, and a Potassium (K₂O) concentration of ∼400 g m⁻³. Individual trees were assigned randomly to one of 10 treatment groups (26 ≤ n ≤ 27). Treatment groups were cooled at different times of the year, using different cooling levels (Fig. 2, Table 1). To arrest spring development and thereby generate early-leafing and late-leafing individuals, half of the experimental population was placed outside under ambient conditions, while the other half was cooled in climate chambers from 4 April to 24 May. The chambers were set to a low of 2°C at night and a high of 7°C during the day, following a simulated day-night cycle of temperature and light availability (13 h photoperiod at ∼4,300 lux). These cold conditions were not intended to mimic natural European conditions, but rather to slow spring development as much as possible without damaging the trees. Temperatures around 5°C are associated with low rates of growth and development processes such as cell division, expansion and maturation (Körner, 2003; Tumajer et al., 2021). From 24 May to 21 June, all trees were kept outside under ambient conditions in a randomised block design. All trees were monitored to observe their individual leaf-out dates, which was defined as the date when > 50% of their leaves had unfolded, corresponding to BBCH15 (Capdevielle-Vargas et al., 2015).

Figure 2.

Table 1.

During the summer treatments, control trees were placed outside under natural ambient conditions. We did not use climate chambers for the control groups because warm conditions in these chambers can introduce unique physiological stressors—such as aphid infestations— not present in cold chambers (Bezemer et al., 1998). In experiment 2, however, we included an additional chamber control to test for potential chamber effects. Although we observed higher aphid abundances in these warm control chambers, chamber exposure itself had no detectable effect on autumn phenology. This strengthens the inference that the phenological shifts observed in our treatments reflect the intended temperature manipulations. Nevertheless, for experiment 1, where chamber controls were not included, we cannot entirely rule out the possibility that chamber conditions exerted some unintended influence on treated trees compared with ambient controls.

The July treatments took place directly after the summer solstice from 22 June to 23 July. Treated trees were placed in climate chambers set to a low of 2°C at night and a high of 7°C during the day or a low of 8°C at night and a high of 13°C during the day depending on their cooling level (extreme and moderate, respectively). Trees in the chambers experienced a photoperiod of 16 h at ∼7,300 lux. The extreme cooling was designed to severely impair cell division, expansion, and maturation as described above. Additionally, under this temperature regime, photosynthesis should be reduced by > 40% (Körner, 2006). The moderate cooling regime, which was still much colder than the ambient conditions, should have also impaired growth and development as well as reduced photosynthesis by at least 30% (Körner, 2003, 2006; Lenz et al., 2014). These settings aimed to generate large temperature differences between treatments and maximise our ability to detect the mechanism underlying the solstice switch, rather than to represent naturally occurring conditions. The August treatments took place from 24 July to 25 August under the same conditions as the July treatments except with a 15 h photoperiod. For the remainder of the experiment, all trees were kept outside in a randomised block design. Throughout the experiment, all trees were watered frequently to ensure constant water supply (Fig. S1).

To observe the effects of our treatments on the development of overwintering buds, we monitored bud growth to derive bud set dates, our marker for the cessation of primary aboveground development and the beginning of autumn phenology, for all trees. On each tree, the terminal bud of the primary shoot and the terminal bud on a random lateral stem were selected and tagged for measurement. Each selected bud was measured to 0.01 mm precision using a digital calliper (CD-P8”M, Mitutoyo Corp, Japan). We measured all buds on a regular basis from 4 July to 2 November. Bud set was defined as the date when each bud reached 90% of its own maximum length, which is considered to be an indicative stage of aboveground primary growth cessation (Signarbieux et al., 2017; Zohner & Renner, 2019). Bud lengths were linearly interpolated between measurement dates to derive the date at which they reached the 90% threshold.

To obtain a more holistic perspective of autumn phenology, we also derived leaf senescence dates from leaf spectral index measurements taken using a SPAD-502 Plus (Soil Plant Analysis Development, Minolta Camera Co., Ltd, Tokyo, Japan). We measured nine leaves per individual (three each from the top, middle and bottom of the crown) on a monthly basis in summer, every other week in September, and on a weekly basis from October to mid-December. We removed measurements taken on 7 December from the analysis as they were unreasonably high, likely due to false readings caused by extensive leaf browning. SPAD readings were then converted to total chlorophyll content (Chl in µg/g fresh weight) using an empirically established equation for Fagus sylvatica leaves (Percival et al., 2008):

The chlorophyll content between two consecutive measurement dates was estimated using linear interpolation. For each treatment and measurement date, we removed individual chlorophyll measurements that were more than 1.5 × the interquartile range below the lower quartile or above the upper quartile. As an additional cleaning step, we completely removed any trees that had more than one data point removed in the last step. Finally, we calculated individual leaf senescence dates as the day-of-year when chlorophyll content last fell below 50% of the observed peak chlorophyll content.

Experiment 2

To observe the effects of pre- and post-solstice daytime and nighttime temperature on autumn phenology, we set up an experimental population (n = 180) of four-year-old Fagus sylvatica trees in Zurich, Switzerland in 2022. The trees were sourced from a local nursery and each tree was placed individually in a 20 L plastic pot containing a 1:1:1 sand / peat / organic soil mixture with a Nitrogen (N) concentration of ∼65 g m⁻³, a Phosphate (P₂O₅) concentration of ∼140 g m⁻³, and a Potassium (K₂O) concentration of ∼400 g m⁻³.

The ambient control treatment consisted of 36 trees exposed to natural ambient conditions. The remaining eight treatments were each applied to 18 trees and included cooling in climate chambers with simulated ambient day length (16 h) and light intensity (∼6,900 lux). The pre-solstice cooling treatments were applied between 22 May and 21 June. The post-solstice cooling treatments were applied between 22 June and 21 July. The pre- and post-solstice treatments included four levels each: Chamber control, where the trees were continuously subjected to 20°C; Day cooling, where trees were subjected to 8°C in the daytime and 20°C at night; Night cooling, where trees were subjected to 20°C in the day and 8°C at night; Full-day cooling, where trees were continuously subjected to 8°C (Fig. 3, Table 2). Due to warm temperatures, chamber control trees were subject to an increase in aphid abundance, however this did not alter their bud set timing (see data analyses). After treatment, all trees were placed in a randomised block design outside under ambient conditions. Soil moisture content was regulated by frequent watering. We measured all buds on a weekly basis from 25 August to 3 November following the same methodology as in experiment 1. We also measured leaf-level CO₂ assimilation rates during the pre-solstice treatment window (see Zohner et al., 2023 for methodology), and derived leaf senescence dates following experiment 1.

Figure 3.

Table 2.

Data analyses

For experiment 2, we performed one-way ANOVAs that showed no significant differences between the end-of-season dates of the ambient, pre-chamber and post-chamber control groups (for bud set: F_2,136 = 0.346, p = 0.708, see Fig. S7; for leaf senescence: F_2,63 = 0.931, p = 0.399). Therefore, for the following analyses we treated all three control treatments as one control treatment with 72 trees. For both experiments we ran linear models using treatment and bud type (apical vs. lateral) as predictors and bud set day-of-year, absolute bud growth or relative bud growth as the response variable. When modelling leaf senescence day-of-year, we used treatment as the sole predictor. For experiment 1, effect sizes were calculated in comparison to the corresponding control treatment, i.e., all early-leafing treatments were compared to the early-leafing control treatment, and all late-leafing treatments were compared to the late-leafing control. Absolute and relative bud growth were calculated as:

Where:

min length = the first measured bud length,

max length = the measured bud length when the bud first surpassed 90% of its final length. To determine the sensitivity of autumn bud set timing to spring leaf-out timing, we ran a linear mixed-effects model using leaf-out day-of-year and bud type as the fixed predictor variables, summer temperature treatment as random effect, and bud set day-of-year as the response variable. We ran the same analysis for leaf senescence timing without the bud type effect.

To quantify the relative contributions of early-season development and late-season temperature to variation in bud set timing in experiment 1, we ran a variance partitioning analysis. We fit a linear model with leaf-out day-of-year, summer cooling treatment (combination of cooling timing and level, e.g. July_Moderate), and bud type as explanatory variables. Variance partitioning was conducted using the varpart function in the vegan R package (Oksanen et al., 2025), which decomposes explained variance into unique and shared components. All statistical analyses were performed in R version 4.5.1 (R Core Team, 2025).

Results

Experiment 1

Linear modelling showed that across all treatments, late-leafing trees cooled during spring delayed their bud set by 4.6 ± 1.3 days (mean ± 2 SE, p < 0.01). Across all treatment pairings, the mean bud set date for the late-leafing group always occurred later than for the early-leafing group (Fig. S2). A linear mixed effects model including leaf-out day-of-year and bud-type as fixed effects and treatment as a random effect revealed that, on average, each day delay in spring leaf-out was associated with a delay of 0.24 ± 0.06 days in bud set timing. Across all treatments, bud type had a small effect, lateral buds set on average 1.1 ± 1.2-days earlier than apical buds (p = 0.06). When modelling only the early-leafing groups, bud type had no discernible effect (0.04 ± 1.64 days earlier for lateral buds, p = 0.96). However, when modelling only the late-leafing groups, lateral buds set earlier than apical buds (2.17 ± 1.64 days advancement, p = 0.01).

The effect of July cooling differed strongly between the early- and late-leafing trees: Within the early-leafing group, moderate cooling in July lead to a small, non-significant delay in bud set compared to the ambient July treatment (1.4 ± 2.6 days, p = 0.29). July cooling had a much greater impact on late-leafing trees, leading to a 4.8 ± 2.6-day delay in bud set compared to the ambient July treatment in the late-leafing group (p < 0.01).

In contrast to July cooling, the effects of August cooling did not differ between early- and late-leafing trees, advancing bud set in all treatment groups (Fig. 4b). Cooling in August lead to a 4.5 ± 2.6-day (p < 0.01) and a 4.4 ± 2.6-day (p < 0.01) advancement in bud set for early- and late-leafing trees, respectively. The extreme cooling treatments showed similar patterns, although slightly less clearly (Fig. S3). Variance partitioning revealed that the early-season development effect (leaf-out day-of-year) explained 8.8% of the total variance in bud set timing, the late-season temperature effect (summer cooling treatment) explained 14.6%, and bud type explained 0.3%. Shared variance values were ≍ 0%, indicating no meaningful overlap. Effects of absolute and relative growth on bud set date can be found in the supporting information (Figs. S4-S5). Bud set timing had no effect on final bud length (Fig. S6).

Figure 4.

Experiment 2

Linear modelling showed that pre-solstice full-day (day and night) cooling delayed autumn bud set by 4.1 ± 3.6 days (mean ± 2SE, p = 0.02) (Fig. 5). Pre-solstice nighttime cooling had a similar effect, delaying bud set by 4.2 ± 3.6 days (p = 0.02). By contrast, pre-solstice daytime cooling had no significant effect on bud set (0.1 ± 3.7 days, p = 0.94). Post-solstice full-day cooling advanced autumn bud set by 5.2 ± 3.6 days (p < 0.01). Similarly, post-solstice daytime cooling advanced bud set by 5.3 ± 4.3 days (p = 0.01). Conversely, post-solstice nighttime cooling delayed bud set by 3.8 ± 3.5 days (p = 0.03). Across all treatments, lateral buds set considerably earlier than apical buds (9.4 ± 2.08 days, p < 0.01). Effects of relative growth on bud set date can be found in the supporting information (Figs. S8).

Figure 5.

Comparison of phenological metrics

Analyses using leaf senescence (50% drop in chlorophyll content) as the phenological marker produced results that were overall consistent with the bud set analyses. For example, in experiment 1, senescence was delayed by 4.22 ± 1.61 days in late-leafing trees and each day delay in spring leaf-out led to a 0.22 ± 0.08-day delay in leaf senescence, closely matching with bud set. Across both experiments the observed patterns were largely the same, although the strengths of each effect differed slightly, and overall, the effects on leaf senescence tended to be weaker (Figs. S9-10). Out of all treatments, opposing responses from bud set and leaf senescence timing were only observed in the early-leafing extreme August cooling group (Treatment 9, bud effect = 1.9 ± 2.59 days advancement, p = 0.14, leaf effect = 1.77 ± 3.53 days delay, p = 0.32) from experiment 1, and the post-full-day cooling group from experiment 2 (bud effect = 5.2 ± 1.81 days advancement, p < 0.01, leaf effect = 1.66 ± 3.34 days delay, p = 0.32). Out of 66 pairwise comparisons of estimated marginal means (every treatment compared against every other treatment in the same experiment), 55 (83%) showed directional agreement between bud set and leaf senescence effects (Fig. S11, adjusted R² = 0.49).

Discussion

In this study, we conducted experiments on European beech to test how bud set—a marker of primary growth cessation—and leaf senescence respond to monthly and diel temperature changes around the summer solstice. We found large differences in the responses between trees subjected to daytime versus nighttime cooling before and after the solstice (Fig. 5) and between early- and late-leafing trees (Fig. 4). These differences suggest that early-season developmental timing not only influences the timing of autumn phenology per se but also plays a critical role in determining the timing of the summer solstice effect reversal. Therefore, our findings support our conceptual model (Fig. 1), highlighting development as a key factor underpinning the Solstice-as-Phenology-Switch hypothesis. In the following sections, we discuss the effects of pre-solstice and post-solstice air temperature on development, along with the distinct impacts of daytime versus nighttime temperature variations.

Early-season development rates alter responses to late-season temperature

Our trans-solstice climate manipulation experiments showed that trees delayed the end of their growing season in response to slow/late early-season development (delayed spring leaf-out). Regardless of the summer cooling treatments, late-leafing trees consistently set buds and senesced leaves after their early-leafing counterparts (Fig. S2), with each day delay in spring leaf-out delaying bud set by an average of 0.24 days and senescence by 0.22 days. This is in line with previous studies demonstrating a tight linkage between within-year variations in spring and autumn phenology (Fu et al., 2014; Keenan & Richardson, 2015; Signarbieux et al., 2017), likely governed by developmental constraints (Zohner et al., 2023), buildup of water and nutrient stress (Paul & Foyer, 2001; Buermann et al., 2018; Bigler & Vitasse, 2021), or leaf aging (Lim et al., 2007).

Despite the importance of early-season development, summer cooling treatment uniquely explained more variance in bud set timing than leaf-out day-of-year (Adjusted R² = 0.15 and 0.09, respectively). July cooling induced a delay in bud set dates 3.4 times greater in late-leafing trees compared to early-leafing ones (4.8 versus 1.4 days delay), which agrees with the expectations derived from our conceptual model (Fig. 1). As we had expected, the natural interannual variation in early-season development causes year-to-year differences in the point at which cool temperatures switch from delaying autumn phenology to advancing it. This offers a physiological explanation for the advancement in the effect reversal timing observed between 1966 and 2015 in Fagus sylvatica, Aesculus hippocastanum, Quercus robur, and Betula pendula (Zohner et al., 2023; because control trees did not experience chamber time, we cannot entirely rule out some influence of this factor on our comparisons).

August cooling induced comparable advances in bud set timing in both early- and late-leafing trees (4.4-4.5 days). The diminishing difference in cooling responses between the two groups from July to August suggests that the influence of early-season development weakens as individuals approach completion of their developmental requirements. By August, phenology appears primarily governed by the delaying effect of warm air temperature (see direct warming effect in Fig. 1b).

Two mechanisms could underlie this shift: shortening daylengths and declining photosynthetic assimilation, the latter of which has been linked to accelerated senescence (Krieger-Liszkay et al., 2019). However, an experiment that reduced August photosynthetic rates in beech by 52-72% – either through cooling or shading – showed that photosynthetic assimilation alone cannot account for autumn phenology (Zohner et al., 2023). Despite similar reductions in photosynthesis, August cooling advanced senescence, while August shading delayed it, revealing contrasting outcomes. This suggests that photosynthetic assimilation cannot have been the driver of the observed phenological responses in beech. Instead, the observed change in temperature responses is more likely regulated by daylength (Kramer, 1936; Petterle et al., 2013; Singh et al., 2021). As days shorten, trees become increasingly responsive to cooling (Delpierre et al., 2009; Körner et al., 2016). Together with the waning influence of developmental carry-over, this can explain why by August trees responded similarly to cooling regardless of their earlier developmental trajectories (Fig. 1). These findings highlight the critical interaction between photoperiod and temperature in shaping the autumn phenology of Fagus sylvatica.

Effects of daytime vs. nighttime temperature

Our experiments showed that daytime and nighttime temperatures had different effects on autumn phenology before and after the summer solstice: Before the solstice, daytime cooling had no impact on the timing of bud set, while nighttime cooling and full-day cooling delayed bud set by 4.2 and 4.1 days, respectively (Fig. 5). This pattern was similar when using leaf senescence as the end-of-season marker. Because experimental cooling reduced photosynthesis by 69-83% across all treatments (Fig. S12), these effects are unlikely to be explained by changes in carbon assimilation. Instead, they highlight the importance of developmental processes—such as cell division and expansion—which mostly occur at night (Steppe et al., 2015; Mencuccini et al., 2017; Zweifel et al., 2021; Fig. 6a). The developmental arrest induced by night cooling—and therefore also by full-day cooling—likely slowed growth and maturation, effectively extending the growing season.

Figure 6.

After the solstice, daytime and nighttime cooling of 8°C elicited opposite responses in both phenological markers, with weaker effects on senescence. Trees subjected to post-solstice daytime cooling and full-day cooling set their buds earliest, on average more than five days earlier than controls. As days shorten, the temperature threshold inducing this growth cessation must be lower at night, otherwise trees would risk prematurely ending their growing season due to the daily minimum temperatures occurring at night (Fig. 6b). This may explain why post-solstice nighttime cooling delayed, rather than advanced, autumn phenology: Cooling of 8°C was sufficient to trigger overwintering responses—growth cessation and maturation of perennating tissues—when applied during the day but insufficient when applied at night (see Fig. S13 for a conceptual schematic).

An alternative explanation is that daytime cooling indirectly triggered dormancy induction by suppressing photosynthesis (Fig 6a), under the assumption that trees prioritise dormancy once photosynthesis is no longer possible (Körner et al., 2016). Though, as discussed above, late-season photosynthesis appears to assert little control over the autumn phenology of F. sylvatica. Taken together, these results support a Diel Cooling Hypothesis, in which the impact of cooling depends on whether it occurs during the day or at night, because the temperature thresholds that trigger growth cessation differ between daytime and nighttime conditions.

Nighttime cooling always led to a delay in bud set of approximately four days (Fig. 5). As trees mainly grow at night (Steppe et al., 2015; Mencuccini et al., 2017; Zweifel et al., 2021), colder nighttime temperatures likely slowed down key developmental processes such as meristematic activity, tissue expansion and maturation, which in turn delayed primary growth cessation (Fig. 6). Similar responses may occur in other temperate tree species: Cold autumn nights have been shown to delay growth cessation and slow bud development in Populus, Pinus and Picea species (Kramer, 1956; Malcolm & Pymar, 1975; Kalcsits et al., 2009). Moreover, the summer solstice effect reversal has been observed consistently across Northern Hemisphere temperate forests (Zohner et al., 2023). Further experiments should explicitly test these diel responses in other temperate tree species.

Support for the Solstice-as-Phenology Switch Hypothesis

The Solstice-as-Phenology-Switch hypothesis posits that changes in temperature before and after the summer solstice have opposite effects on the autumn phenology of northern forest trees (Zohner et al., 2023). The hypothesis does not assume that the reversal is fixed precisely on June 21, but rather that it occurs around the solstice, when photoperiod cues shift trees from accelerating to decelerating their seasonal development. Our conceptual model (Fig. 1) explicitly incorporates this flexibility by showing how the timing of the reversal depends on developmental speed: individuals that develop more slowly (or leaf out later) cross the compensatory point later in the summer, whereas fast-developing individuals reach it earlier.

Our experiments support this framework: pre-solstice full-day cooling delayed bud set, whereas post-solstice full-day cooling advanced it, with differences between early- and late-developing individuals consistent with the model. Moreover, the contrasting impacts of daytime vs. nighttime cooling demonstrate how diel conditions can further shape when the reversal is expressed. Thus, our findings reinforce the Solstice-as-Switch hypothesis and extend it by showing how flexibility arises from interactions between developmental progression, diel temperature responses, and photoperiod.

In conclusion, earlier primary growth cessation in temperate trees under climate change may result from higher developmental rates under warmer temperatures. In European beech, we show that this effect is predominantly driven by nighttime temperatures, reflecting the fact that growth primarily occurs at night. To better predict future growing season lengths, models must begin to account for the differential impacts of the seasonal and daily temperature cycles that temperate zone trees are physiologically adapted to.

Data availability

The code and data for this study are available at Zenodo (Rebindaine et al., 2025).

Acknowledgements

C.M.Z. was supported by the SNF Ambizione Fellowship programme (no. PZ00P3_193646) and T.W.C. by DOB Ecology and the Bernina Foundation.

Additional information

Author contributions

D.R. conceived and developed the study, conducted the experiments and analyses, and wrote the manuscript. C.M.Z equally contributed to the conception and development of the study, contributed to the experiments and analyses, and the text. L.M., H.M., Z.W. and Y.Z. contributed to the conception and implementation of the first experiment. R.B. contributed to the conception and implementation of the second experiment. T.W.C. and S.S.R. contributed to the text. All authors provided comments and approved the final manuscript.

Funding

DOB Ecology

• Thomas W Crowther

Bernina Foundation

• Thomas W Crowther

Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung (SNF) (PZ00P3_193646)

• Constantin M Zohner

Additional files

Supporting Information