Umeå University's logo

Cyanobacterial blooms in marine and freshwater ecosystems have increased in magnitude, frequency, and distribution worldwide during recent decades. Filamentous cyanobacteria are of unsuitable size for mesozooplankton feeding and of poorer nutritional quality than other phytoplankton taxa. The production and quality of higher trophic levels are therefore expected to decrease when cyanobacterial blooms increase. We conducted a mesocosm experiment using natural seawater from the northern Baltic Sea to contrast the effects of cyanobacteria- (Aphanizomenon flosaquae) and diatom-dominated phytoplankton communities on mesozooplankton production and nutritional quality. A low and a high hydrological mixing regime was applied. The δ15N isotopic signal of seston and mesozooplankton was lower in the cyanobacteria-based food web, demonstrating that Aphanizomenon fixed atmospheric nitrogen, which was transferred in the food web. The biomass of edible-sized phytoplankton (2–50 μm) was lower in the cyanobacteria-based food web. The fatty acid quality, indicated by the ω3:ω6 ratio, was lower in the cyanobacteria-based food web for both phytoplankton and mesozooplankton. Together, this resulted in 75–80% lower copepod production and food web efficiency (FWE) in the cyanobacteria-based food web than in the diatom-based food web. The hydrological mixing regime did not affect the biological production and quality. The results demonstrate that copepod production and FWE were driven by the quality and production of edible-sized phytoplankton. The study implies that climate-induced increases of filamentous cyanobacterial blooms will cause decreased production and nutritional quality of higher trophic levels.

Climate change is projected to cause elevated precipitation in northern Europe, leading to increased runoff of terrestrial matter to coastal areas. The consequences for food web production and ecosystem function remain unclear. A mesocosm experiment was performed to investigate the impacts of elevated terrestrial matter input, using a natural plankton community from the northern Baltic Sea with added young-of-the-year perch as planktivorous top consumer. Addition of terrestrial matter caused water browning and increased dissolved organic carbon and inorganic nutrient concentrations. Phytoplankton primary production showed a negative response to terrestrial matter due to decreased light availability, while heterotrophic bacterial production increased. The trophic balance, calculated as the difference between primary production and heterotrophic bacterial production, indicated that net-heterotrophy was triggered by terrestrial matter enrichment. Primary production was identified as the main basal energy source for fish. Addition of terrestrial matter reduced the food web efficiency, calculated as the ratio between fish production and basal production (primary production?+?heterotrophic bacterial production). Furthermore, stable isotope analysis of seston and fish indicated that the added terrestrial matter was not efficiently incorporated in the food web and only marginally altered the food web trophic positions. The results suggest that the main food chain consisted of phytoplankton, mesozooplankton, and fish, and that the ecosystem production was overall light driven. Under a changing climate, several negative effects can be expected, including a poorer light climate, reduced ecosystem production and net-heterotrophy. These alterations have potentially significant consequences for ecosystem functioning, fish production, and thus ecosystem services.

Climate change has shown to have global impacts on marine ecosystems by increasing temperature and altering hydrology. The consequences for marine food webs are less known, but it has been suggested that both the nutritional quality and production will change in such a way that the energy transfer up the food web becomes lowered. The ratio between the production by upper and basal trophic levels, i.e., the food web efficiency, may decrease. In this thesis, I investigated the effects of climate change-induced environmental alterations on the food web efficiency and quality in the northern Baltic Sea, i.e., the Gulf of Bothnia, using multiple approaches including field surveys, a mesocosm experiment, and time-series analyses of long-term monitoring data. In the field study, I found that seawater browning in the Bothnian Bay has caused reductions in the nutritional quality of mesozooplankton. Through the mesocosm experiment, I found that intensified cyanobacterial blooms, a likely consequence of climate change, would reduce the zooplankton's nutritional quality and food web efficiency. The time-series analyses indicated that the lowered salinity and increased dissolved organic carbon, resulting from climate change, have reduced the nutritional quality of herring in the Bothnian Bay. Further, I found that the retention of essential fatty acids in coastal fish predators largely depends on their taxonomy, habitat use, and the nutritional quality of their prey. Therefore, climate-related environmental changes, which alter the nutritional quality of prey resources, are predicted to alter the retention of essential fatty acids in fish. Overall, the results suggest that climate change-induced environmental stressors such as increased browning and cyanobacterial blooms, and reduced salinity in the northern Baltic Sea have negative impacts on the food web efficiency and quality. These changes may imply a potential decline in fish production and environmental health. 

Climate change has been projected to cause increased temperature and amplified inflows of terrestrial organic matter to coastal areas in northern Europe. Consequently, changes at the base of the food web favoring heterotrophic bacteria over phytoplankton are expected, affecting the food web structure. We tested this hypothesis using an outdoor shallow mesocosm system in the northern Baltic Sea in early summer, where the effects of increased temperature (+ 3°C) and terrestrial matter inputs were studied following the system dynamics and conducting grazing experiments. Juvenile perch constituted the highest trophic level in the system, which exerted strong predation on the zooplankton community. Perch subsequently released the microbial food web from heavy grazing by mesozooplankton. Addition of terrestrial matter had a stronger effect on the microbial food web than the temperature increase, because terrestrial organic matter and accompanying nutrients promoted both heterotrophic bacterial production and phytoplankton primary production. Moreover, due to the shallow water column in the experiment, terrestrial matter addition did not reduce the light below the photosynthesis saturation level, and in these conditions, the net-autotrophy was strengthened by terrestrial matter enrichment. In combination with elevated temperature, the terrestrial matter addition effects were intensified, further shifting the size distribution of the microbial food web base from picoplankton to microphytoplankton. These changes up the food web led to increase in the biomass and proportion of large-sized ciliates (>60 µm) and rotifers. Despite the shifts in the microbial food web size structure, grazing experiments suggested that the pathway from picoplankton to nano- and microzooplankton constituted the major energy flow in all treatments. The study implies that the microbial food web compartments in shallow coastal waters will adjust to climate induced increased inputs of terrestrial matter and elevated temperature, and that the major energy path will flow from picoplankton to large-sized ciliates during the summer period.

Algae-produced long-chain polyunsaturated fatty acids (LC-PUFA; with ≥20 carbon atoms) are key biomolecules for consumer production and animal health. They are transferred to higher trophic levels and accumulated in food chains. However, LC-PUFA accumulation in consumers and their trophic transfer vary with the diet quality and the physiological demand for LC-PUFA of consumers. The goal of this study was to investigate spatial and taxonomic differences in LC-PUFA retention of coastal fish predators that potentially differ in their habitat use (benthic versus pelagic) and prey quality. We analyzed the fatty acid (FA) composition of common fish species, namely roach and European perch, as well as their potential prey from benthic and pelagic habitats in three bays of the northern Baltic Sea. We then assessed whether the fish LC-PUFA retention differed between species and among the study bays with different diet quality, that is, LC-PUFA availability. Our data indicated taxon-specific differences in the retention of LC-PUFA and their precursor FA in fish (i.e., short-chain PUFA with <20 carbon atoms). Perch did not show any spatial variation in the retention of all these FA, while roach showed spatial differences in the retention of docosahexaenoic acid (DHA) and their precursor FA, but not eicosapentaenoic acid (EPA). Data suggest that diet quality and trophic reliance on benthic prey underlay the DHA retention differences in roach. Although the PUFA supply might differ among sites, the low spatial variation in LC-PUFA content of perch and roach indicates that both fishes were able to selectively retain dietary LC-PUFA. Climate change together with other existing human-caused environmental stressors are expected to alter the algal assemblages and lower their LC-PUFA supply for aquatic food webs. Our findings imply that these stressors will pose heterogeneous impacts on different fish predators. We advocate further investigations on how environmental changes would affect the nutritional quality of the basal trophic level, and their subsequent impacts on LC-PUFA retention, trophic ecology, and performance of individual fish species.

We analyzed the taxonomic and fatty-acid (FA) compositions of phytoplankton and zooplankton, and the environmental conditions at three coastal and offshore stations of the northern Baltic Sea. Plankton samples for FA analyses were collected under the framework of sampling campaigns of the Swedish National Marine Monitoring program in September 2017. Monitoring data of phytoplankton and zooplankton biomass, and environmental variables at each station were extracted from the Swedish Meteorological and Hydrological Institute database (https://sharkweb.smhi.se/). Monthly phytoplankton biomass at each station in July-September 2017 was aggregated by class (i.e., chyrsophytes, cryptophytes, dinoflagellates, diatoms, euglenophytes, cyanobacteria, etc.). Zooplankton biomass in September 2017 was aggregated by major taxa (i.e., Acartia sp. [Calanoida], Eurytemora affinis [Calanoida], Cladocera, Limnocalanus macrurus and other copepods (i.e. excluding Eurytemora and Acartia)). Environmental variables monthly monitored in January-October 2017 included salinity, concentrations of dissolved organic carbon, humic substances, total nitrogen and total phosphorus. These variables were measured from 0 to 10 m depth below water surface, and the depth-integrated averages were used for data analyses. Seston and zooplankton (Eurytemora affinis, Acartia sp. and Cladocera) FA compositions were analyzed using gas chromatography and mass spectroscopy (GC–MS). Our dataset could provide new insights into how taxonomic composition and biochemical quality of the planktonic food chains change with the environmental conditions in subarctic marine ecosystems.

Inflows of coloured terrestrial organic matter cause seawater browning and reduced phytoplankton production in subarctic coastal ecosystems, potentially deteriorating the nutritional quality of marine food webs. We analyzed the fatty-acid (FA) compositions of seston and the zooplankton taxa Eurytemora affinis and cladocerans at three locations of the northern Baltic Sea. At the coastal and northerly locations, salinity and phosphorus concentrations were low, while concentrations of humic substances (i.e., terrestrial organic matter) were high. The southerly location showed the opposite trend. The ratio between alga-specific ?3 polyunsaturated FA and terrigenous monounsaturated FA (MUFA) in Eurytemora decreased from south to north, as did the ratio between the alga-specific docosahexaenoic acid (DHA) and terrigenous MUFA in cladocerans. With increasing humic substances, the biomass of DHA-rich phytoplankton decreased and the zooplankton MUFA content increased. Our results indicate that coloured terrestrial organic matter alters the phytoplankton composition, consequently affecting the zooplankton nutritional quality.

Les influx de matière organique terrestre causent le brunissement de l’eau de mer et réduisent la production duphytoplancton dans les écosystèmes côtiers subarctiques, ce qui peut se traduire par une détérioration de la qualité nutri-tionnelle des réseaux trophiques marins. Nous avons analysé la composition d’acides gras du seston, du taxon de zooplanctonEurytemora affinis et de cladocères dans trois sites de la mer Baltique septentrionale. Dans les sites côtier et nordique, la salinité etles concentrations de phosphore étaient faibles, alors que les concentrations de substances humiques (c.-à-d. matière organiqueterrestre) étaient élevées. Le site plus au sud présentait des tendances inverses. Le rapport des acides gras polyinsaturés x3 spécifiquesaux algues et des acides gras monoinsaturés (AGMI) terrigènes chez Eurytemora diminuait du sud au nord, tout comme le rapport del’acide docosahexanoïque (ADH) spécifique aux algues et des AGMI chez les cladocères. Plus l’abondance de substances humiques étaitélevée, plus la biomasse de phytoplancton riche en ADH était faible et plus le contenu en AGMI du zooplancton était important. Nosrésultats indiquent que de la matière organique terrestre colorée modifie la composition du phytoplancton et a par conséquent uneincidence sur la qualité nutritionnelle du zooplancton. [Traduit par la Rédaction]