Description: Coccolithophores—single-celled calcifying phytoplankton—are an important group of marine primary producers and the dominant builders of calcium carbonate globally. Coccolithophores form extensive blooms and increase the density and sinking speed of organic matter via calcium carbonate ballasting. Thereby, they play a key role in the marine carbon cycle. Coccolithophore physiological responses to experimental ocean acidification have ranged from moderate stimulation to substantial decline in growth and calcification rates, combined with enhanced malformation of their calcite platelets. Here we report on a mesocosm experiment conducted in a Norwegian fjord in which we exposed a natural plankton community to a wide range of CO2-induced ocean acidification, to test whether these physiological responses affect the ecological success of coccolithophore populations. Under high-CO2 treatments, Emiliania huxleyi, the most abundant and productive coccolithophore species, declined in population size during the pre-bloom period and lost the ability to form blooms. As a result, particle sinking velocities declined by up to 30% and sedimented organic matter was reduced by up to 25% relative to controls. There were also strong reductions in seawater concentrations of the climate-active compound dimethylsulfide in CO2-enriched mesocosms. We conclude that ocean acidification can lower calcifying phytoplankton productivity, potentially creating a positive feedback to the climate system.

Description: An increasing body of research emphasizes that various biological processes in marine organisms are affected due to the uptake of anthropogenic atmospheric CO2 by the ocean in a process termed as ocean acidification (OA). The magnitude and direction of OA effects varies greatly among species and genotypes, highlighting different capabilities to adapt to increasing CO2. Direct OA impacts can be expected in the biochemical and elemental composition of primary producers (PP), which may be transferred to higher trophic levels, while indirect impacts can derive from altered trophic interactions as OA can modify plankton community composition. Fatty acids (FA) are the main component of lipids and cell membranes, with polyunsaturated fatty acids (PUFA) having additional important physiological and metabolic roles. Phytoplankton is the main source of essential biomolecules for heterotrophs as they cannot synthesize them de novo. Transference of organic essential macromolecules, in particular PUFA from phytoplankton-to-zooplankton-to-fish is a key factor influencing the life cycle of many organisms including humans. In the present work was investigated how OA influences the food quality of primary producers in terms of their fatty acid makeup at specie and community level, and how these OA-driven changes in the algae affect the fatty acid profile and life cycle of consumers. A combination of short- and long-term experiments on individual algal species, interaction between a single primary producer and one consumer, and natural plankton communities encompassing several producers and consumers were conducted in laboratory and natural conditions. In the short-term experiments at species level, the first and second laboratory study showed that CO2 can affect the biochemical composition of the diatoms Thalassiosira pseudonana and Cylindrotheca fusiformis, reducing their PUFA content; additionally the second diatom showed a reduced amount of amino acids. The interaction between a single primary producer and one consumer showed that when T. pseudonana cultured under high CO2 was used to feed the copepod Acartia tonsa, it affected their FA composition, severely impaired development and egg production rates. This demonstrated that a direct OA-driven shift in algal food quality can influence the reproduction success of upper trophic levels. At the community level, the third study conducted in a North Sea natural plankton assemblage subjected to a CO2 gradient showed that OA can modify phytoplankton community structures by favoring small phytoplankton cells with a comparatively low PUFA content. This community shift reduced PUFA content in primary producers was linked to a gradual PUFA decline in the dominant copepod species Calanus finmarchicus. In contrary, the fourth study revealed that the natural plankton community of the Baltic Sea experienced small differences in the algal community composition between CO2 treatments. The PUFA profile of the PP was influenced by phosphorus availability in the mesocosms, which was reflected by the PUFA composition of the copepod Acartia tonsa and Eurytemora affinis, but showed no significant CO2-related changes. This indicates that OA can affect the plankton community composition and its associated PUFA content, however this effect is lower in environments where communities are exposed to natural occurring high CO2 fluctuations like in the Baltic Sea, and that other essential nutrients have a stronger influence in the algal FA profile when present in limited amounts. In the long term experiments at species level, the fourth study determined that the coccolithophore Emiliania huxleyi and the diazotrophic cyanobacterium Trichodesmium sp. cultured over a thousand generations at high CO2 conditions showed a change in their FA content and composition. The FA profile of both algae presented a differentiate adaptation to high CO2 and particularly PUFA, which have metabolic functions in the cells, displayed evidence of adaptive evolution in both algae. These results highlight the diversity of OA responses among single plankton species and communities and that changes in biomolecular composition at the base of the marine food web are transferred to primary consumers. The thesis also highlights that the magnitude and direction of CO2-effects likely depends on the CO2 conditions and fluctuations the organisms are adapted to.

Description: Since the beginning of the industrial revolution the atmospheric partial pressure of CO2 (pCO2) has increased exponentially, reaching 380 μatm nowadays, and is expected to rise to values up to 700 μatm by the end of this century. These changes affect marine plankton in various ways, positively as for cyanobacteria, or in most cases, negatively as for coccolithophores. However there is a lack in the understanding of the effect of this increase in carbon for some important organisms as diatoms, an important primary producer in the ocean. Diatoms have not been reported as affected by ocean acidification, although several studies have reported a change of the total lipid content in some diatoms when cultured at high CO2 conditions. With this perspective, a set of two experiments were designed; the first was intended to determine if the amount of different fatty acids (the building blocks of lipids) of the diatom Thalassiosira pseudonana is altered when cultures under diverse CO2 conditions; while the second experiment was intended to determine the possible effects of the change in the fatty acids of T. pseudonana on the life cycle of the copepod Acartia tonsa when feed with this diatom. The first experiment showed that the fatty acid content of T. pseudonana change toward high CO2 levels, with an increase in the amount of saturated fatty acids and a decrease of unsaturated fatty acids content. The second experiment showed that the growth rate, amount of egg produced per female, and fatty acid content per female are reduced when feed with T. pseudonana cultured at high CO2 conditions. Our results show that CO2 actually affects the fatty acid composition of T. pseudonana and that this fatty acid alteration in the diatom have a significant influence on the life cycle of A. tonsa. However, further studies are required to determine if the effects observed in this study also take place in the environment.