Magnus Huss

To mitigate coastal eutrophication, a worldwide concern to sustain ecosystem services, actions often focus on nutrient-load reductions but sometimes also aim to limit the abundance of forage fish. Adding to the eutrophication problem, changes in climate and land use lead to increased inputs of coloured dissolved organic matter (darkening). We conducted a mesocosm experiment to study the effects of water darkening on the outcome of eutrophication mitigation actions acting either bottom-up or via top-down control. We initiated eutrophication under varying water colour conditions. Then, we performed mitigation actions by stopping nutrient additions, removing forage fish, or both. Stopping nutrient additions was the most effective action in reducing pelagic algal biomass, irrespective of water colour. In contrast, the effect of fish removal varied with water colour, only having an effect in darker waters. We link these varying responses to shifts in nutrient availability and zooplankton community biomass and composition. Our experiment demonstrates that future eutrophication management may need to consider multiple concurrent pressures, including coastal darkening, as they can generate indirect effects caused by trophic interactions.

Archival samples provide a unique source of DNA, offering the potential to extend the temporal scale of genetic studies by decades to centuries. Fish hard structures, such as otoliths and scales, serve as records for fish collected during fisheries monitoring across a large spatiotemporal scale. Operculum bones are a type of fish hard structure that, although less commonly collected, have been utilized in genetic studies. However, the usefulness of archived operculum bones to provide high quality whole genome sequence information has not been thoroughly evaluated. Here, we applied a commercially available extraction protocol, with minor adjustments, to isolate genomic DNA from operculum bones of Eurasian perch collected up to 47 years ago, followed by standard short-read whole genome sequencing. By comparing the metrics of DNA and whole genome sequencing data of bones with contemporary muscle samples, we demonstrate that the application of a simple extraction protocol on boiled archival fish operculum bones yields high quality genomic information that is comparable to fresh tissue, highlighting the role of archival operculum bones as an overlooked repository of valuable genomic information.

Climate warming reshapes biomass distributions across trophic levels in aquatic systems, with implications for ecosystem functioning and service provisioning. Using a space‐for‐time approach across temperate and boreal lakes, we analyse a dataset spanning wide gradients in temperature and nutrient availability, including species and biomass data for phytoplankton, fish, and, in some cases, zooplankton. We hypothesise that (1) warmer lakes have higher fish‐to‐phytoplankton biomass ratios than colder lakes, and (2) this relationship weakens at high phosphorus levels due to proliferation of inedible phytoplankton. Contrary to expectations, our results show that warmer lakes exhibit lower fish‐to‐phytoplankton biomass ratios, regardless of phosphorus concentrations or the contribution of benthic relative to whole lake primary production. This suggests reduced energy transfer efficiency from producers to consumers in warming waters. Changes in phytoplankton and fish community composition are likely part of the explanation for why increased phytoplankton biomass in warmer lakes does not translate into higher fish biomass. Our findings highlight a critical shift in biomass distribution from fish to phytoplankton with rising temperatures in northern lakes, potentially signalling future declines in food web efficiency and predator biomass under continued climate warming.

Predator responses to warming can occur via phenotypic plasticity, evolutionary adaptation or a combination of both, changing their top-down effects on prey communities. However, we lack evidence of how warming-induced evolutionary changes in predators may influence natural food webs. Here, we ask whether wild fish subject to warming across multiple generations differ in their impacts on prey communities compared with their nearby conspecifics experiencing a natural thermal regime. We carried out a common garden mesocosm experiment with larval perch ( Perca fluviatilis ), originating from a heated or reference coastal environment, feeding on zooplankton communities under a gradient of experimental temperatures. Overall, in the presence of fish of heated origin, zooplankton abundance was higher and did not change with experimental warming, whereas in the presence of fish of unheated origin, it declined with experimental temperature. Responses in zooplankton taxonomic and size composition suggest that larvae of heated origin consume more large-sized taxa as the temperature increases. Our findings show that differences between fish populations, potentially representing adaptation to their long-term thermal environments, can affect the abundance, biomass, size and species composition of their prey communities. This suggests that rapid microevolution in predators to ongoing climate warming might have indirect cross-generational ecological consequences propagating through food webs.

Predator responses to warming can occur via phenotypic plasticity and evolutionary adaptation, resulting in changes in their prey communities. However, we lack evidence of how warming-induced evolutionary changes in predators can influence the food web. Here, we ask whether fish subject to long-term warming across multiple generations differ in their impacts on prey communities compared to their nearby conspecifics experiencing a natural thermal regime. We carried out a common garden mesocosm experiment with larval perch ( Perca fluviatilis ), originating from one heated or one reference coastal environment, feeding on zooplankton communities under a gradient of experimental temperatures. We found that fish thermal origin influenced the zooplankton communities, and differently so depending on the experimental temperature. In presence of fish of heated origin, there were less zooplankton and also fewer individuals of large size, except for at intermediate experimental temperatures. Our findings show that differences between fish populations, potentially representing adaptation to local thermal environment, caused by multi-generational warming can cascade down via trophic interactions to also affect their zooplankton prey communities. Considering climate warming, our results suggest that rapid evolution in predators might have indirect cross-generational ecological consequences propagating through food webs.

Size-specific body growth responses to warming are common among animal taxa, but sex-specific responses are poorly known. Here we ask if body growth responses to warming are sex-dependent, and if such sex-specific responses vary with size and age. This was tested with sex-specific data of back-calculated individual growth trajectories, in European perch ( Perca fluviatilis) from a long-term whole-ecosystem warming experiment (6.3 °C above the surrounding sea). Warming led to both size- and sex-specific differences in growth responses. Warming had a consistent positive effect on body growth of females, but negative effects on male growth at size > 10 cm and age > 2 years. These sex-specific growth responses translate to an increased degree of female-biased sexual size dimorphism (in length-at-age) with warming. Although the exact temperature-mediated effects underlying differential growth responses could not be resolved, results imply global warming may have highly different effects during ontogeny of male and female perch. Such effects should be considered in climate warming scenarios concerning fish growth, population size-structure, and dynamics of aquatic food webs that include fish exhibiting sexual size dimorphism.

Body size–dependent physiological effects of temperature influence individual growth, reproduction, and survival, which govern animal population responses to global warming. Considerable knowledge has been established on how such effects can affect population growth and size structure, but less is known of their potential role in temperature‐driven adaptation in life‐history traits. In this study, we ask how warming affects the optimal allocation of energy between growth and reproduction and disentangle the underlying fitness trade‐offs. To this end, we develop a novel dynamic energy budget integral projection model (DEB–IPM), linking individuals' size‐ and temperature‐dependent consumption and maintenance via somatic growth, reproduction, and size‐dependent energy allocation to emergent population responses. At the population level, we calculate the long‐term population growth rate (fitness) and stable size structure emerging from demographic processes. Applying the model to an example of pike (Esox lucius), we find that optimal energy allocation to growth decreases with warming. Furthermore, we demonstrate how growth, fecundity, and survival contribute to this change in optimal allocation. Higher energy allocation to somatic growth at low temperatures increases fitness through survival of small individuals and through the reproduction of larger individuals. In contrast, at high temperatures, increased allocation to reproduction is favored because warming induces faster somatic growth of small individuals and increased fecundity but reduced growth and higher mortality of larger individuals. Reduced optimum allocation to growth leads to further reductions in body size and an increasingly truncated population size structure with warming. Our study demonstrates how, by incorporating general physiological mechanisms driving the temperature dependence of life‐history traits, the DEB–IPM framework is useful for investigating the adaptation of size‐structured organisms to warming.

Coastal eutrophication due to excessive anthropogenic nutrient loading is a major threat worldwide, and especially in estuaries and semi‐enclosed waterbodies, like the brackish Baltic Sea. In addition, coastal waters may become darker (coastal darkening) due to increased input of colored compounds from terrestrial run‐off and sediment resuspension. Still, the effects of darkening on coastal food web responses to eutrophication are unknown. In a mesocosm experiment with benthic and pelagic habitats, we manipulated nutrient loading, presence of fish and light availability to disentangle bottom‐up and top‐down control of eutrophication symptoms in ambient and darkened waters. Overall, we found higher pelagic Chlorophyll a concentrations (a proxy of algal biomass) with darkening and with nutrient enrichment in both clear and dark waters. Albeit fish had a strong impact on zooplankton and zoobenthos, they had no cascading effect on algae. We conclude that coastal darkening due to changes in land use and climate change can pose an additional challenge concerning the recovery of coastal waters from eutrophication.