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Hille Ris Lambers, J.

Publications and source records attributed to Hille Ris Lambers, J..

5 recordsLinked to original sources

Experimental flowering order shapes priority effects in plant-pollinator interactions

Climate change is disrupting life's seasonal rhythms, altering the timing of key phenophases and reshaping how communities assemble. Beyond shifting flowering times, climate change can modify the extent of floral overlap and the sequence in which species bloom, generating novel assemblages with uncertain consequences for plant-pollinator interactions. Here, we ask whether flowering order generates priority effects in plant-pollinator communities, much like germination order does in plant communities. We tested how flowering order influences bee foraging behaviour and plant reproductive success in two co-flowering species, Hypochaeris radicata and Campanula rotundifolia, using a greenhouse experiment in which we manipulated the sequence of floral availability while allowing bees to forage repeatedly. We quantified changes in visit frequency, interspecific switches, handling time, and seed production. Our findings reveal priority effects in bee foraging that were strong enough to affect plant fitness: both species received more visits when flowering earlier than their co-occurring counterpart, and seed production declined when species flowered later. Overall, our results show that flowering order is an underappreciated driver of plant-pollinator interactions, suggesting that climate-driven phenological shifts could alter priority-effect dynamics with broader implications for community assembly. Key questions remain: How will climate-driven phenological shifts rearrange flowering sequences, and how will these priority effects emerge in more diverse communities in the wild? Our controlled experiment reveals strong flowering-order effects, underscoring the need to evaluate how widespread and impactful such dynamics are under accelerating climate change.

ecology↗

Assessing heatdome effects on forest dynamics in the Pacific Northwest using Planet imagery

Increasingly frequent extreme heat events are imposing significant stress on forest ecosystems, with implications for forests and the organisms that live in them. This study evaluates the effects of the June 2021 Pacific Northwest (PNW) heatdome (a prolonged high-pressure system that generated record-breaking temperatures) on forest canopy health and its subsequent recovery within the conifer-dominated Ellsworth Creek Preserve in Washington state, USA, using high-resolution Planet Labs satellite imagery. We analyzed normalized difference vegetation index (NDVI) trends from spring to fall from 2017 to 2024 to identify canopy stress and quantify changes in canopy greenness. Experimental forest restoration thinning treatments implemented to test their effectiveness in restoring old-growth forest characteristics at our sites allowed us to assess impacts of the heatdome event relative to these restoration treatments. Our results show a marked decline in summer NDVI following the 2021 heatdome, signaling substantial canopy stress. This decline, different than patterns in the other seven years, was particularly strong in dense, unmanaged (control) forest stands, which exhibited more pronounced NDVI declines than thinned (treatment) stands. These more pronounced stress signals during and after the heat event were associated with greater tree canopy height, canopy complexity, and tree density. The summer NDVI trends over the three post-heatdome years suggest a gradual recovery in tree canopy greenness, with thinned stands showing faster NDVI recovery than controls. In all, these results suggest that restoration thinning may improve canopy resilience to extreme heat. However, recovery trajectories varied widely within stand types, with persistent evidence of stress in high-density areas that suggest incomplete recovery as of 2023. Broadly, these findings show the vulnerability of dense forest canopies to extreme heat events, suggesting that forests with high canopy density may be less adaptable to recurring heat events. Nonetheless, managing forests through restoration thinning may enhance forest resilience to these climate-induced stressors - providing potential guidance for adaptive management strategies to maintain forest health in a world with more extreme climates.

ecology↗

Warm-loving species perform well under limiting resources:trait combinations for future climate

Ecosystems are warming alongside shifts in other abiotic factors, leading to interactive effects on populations and communities. This underscores the importance of studying how organisms respond to multiple environmental changes simultaneously. In aquatic ecosystems, as surface waters of lakes and oceans warm, longer and stronger periods of thermal stratification lead to changes in resource (light and nutrient) availability. We investigate the combined effect of temperature and resource availability on 19 populations (comprising 17 species) of freshwater phytoplankton to examine how temperature influences the minimum resource requirements (and Monod parameters) for light, nitrogen, and phosphorus. We also evaluate how resource availability affects each populations thermal traits (i.e. thermal performance curve -TPC-parameters). When averaged across all populations, the requirements for light and phosphorus tended to display a U-shaped relationship along temperatures. Individual populations varied greatly in their responses to temperature, leading to shifts in the identity of the best competitor across the thermal gradient, particularly for nitrogen and phosphorus. TPC responses to resource limitation were highly variable, but thermal optima and maxima of individual populations often decreased with resource limitation, and thermal breadths (range where growth is 80% or more of its maximum) often increased due to a flattening of TPCs. Across all populations and resource types, the maximum optimum temperature across resource levels (maximum Topt) tended to be positively correlated with the temperature at which they had the lowest resource requirements (minimum R*). However, the temperature at which populations were the best competitors tended to be [~]5 {degrees}C colder on average than the temperature at which they grew the fastest. The populations with the highest thermal optima also had the lowest minimum resource requirements. Our findings reveal trait associations suggesting that some taxa already exhibit trait combinations that would support high performance under future warm and resource-limited conditions.

ecology↗

Lagged climate-driven range shifts at species' leading, but not trailing, range edges revealed by multispecies seed addition experiment

Climate change is causing many species ranges to shift upslope to higher elevations as species track their climatic requirements. However, many species have not shifted in pace with recent warming (i.e., range stasis), possibly due either to demographic lags or microclimatic buffering. The lagged-response hypothesis posits that range stasis disguises an underlying climatic sensitivity if range shifts lag the velocity of climate change due to slow colonization or mortality. Alternatively, the microclimatic buffering hypothesis proposes that small-scale variation within the landscape, such as canopy cover, creates patches of suitable habitat within otherwise unsuitable macroclimates that create climate refugia and buffer range contractions. To test these two hypotheses, we combined a large seed addition experiment of 25 plant species across macro- and micro-scale climate gradients with local herbaria records to compare patterns of seedling recruitment relative to adult ranges and microclimate in the North Cascades, USA. Despite high species-to-species variability in recruitment, community-level patterns supported the lagged response hypothesis, with a mismatch between where recruitment vs. adults occur. On average, the seedling recruitment optimum shifted from the adult climatic range centre to historically cooler, wetter regions and many species recruited beyond their cold (e.g., leading) range edge. Meanwhile, successful recruitment at warm and dry edges, despite recent climate change, suggests that macroclimatic effects on recruitment do not drive trailing range dynamics. By contrast, we were unable to detect evidence of microclimatic buffering due to canopy cover. Combined, our results suggest apparent range stasis in our system is a lagged response to climate change at the cool ends of species ranges, with range expansions likely to occur slowly or in a punctuated fashion.

ecology↗

Microclimate buffering varies across forest types during an extreme heat event

Increasing temperatures and extreme heat episodes have become more common with climate change. While forests are known to be buffered from increasing temperatures compared to non-forested areas, whether this buffering is maintained under extreme temperature events, how such events influence forests, and how forest organisms respond to extreme heat is relatively unknown. Here we assess the effects of an extreme heat event (the Pacific Northwest (PNW) heatdome in June 2021) on forest microclimates, forests, and the organisms living within them. We first asked how the PNW heatdome affected microclimates in forests with differing canopy cover (including non-forests) and found that the buffering capacity of forests is greater under denser canopies, even under extreme heat events. We then combined this information with organismal temperature tolerance curves for 12 relevant species and found that canopy buffering can minimize the negative impacts of even extreme heat events on understory organisms, with greater canopy density providing greater microclimate moderation. Finally, we analyzed seasonal NDVI trends in recent years, and found signs of canopy stress following the extreme 2021 heat event. In all, this suggests that although forest canopies may buffer the negative effects of extreme heat events on understory organisms, a greater frequency of extreme heat events may threaten this capacity by damaging forest canopies.

ecology↗