Engel, Anja

Primary production in the sunlit surface ocean is the driving force for the uptake of atmospheric CO2 and basis for its potential sequestration into the ocean s interior. As a consequence of the ongoing anthropogenic emissions of the greenhouse gas CO2, future climate will cause multiple environmental changes in the global ocean, including acidification, warming and nutrient availability. This thesis deals with the synergistic effect of elevated CO2 and temperature at phosphorus limitation on organic matter production by Emiliania huxleyi. Experiments were accomplished by means of a fully controlled continuous culture facility, concerning the combined manipulation of nutrient supply, growth rates, CO2 and temperature. Cell density, particulate organic carbon (POC) concentration and cell size of E. huxleyi were affected to varying degrees by applied growth, CO2 and temperature conditions. Elevated CO2 and temperature (greenhouse scenario) clearly led to an extended plasticity of E. huxleyi concerning a minimum phosphorus cell quota. The ability to produce more organic matter on low nutrient supply most likely gives rise to the production of high amounts of carbon rich biomass characterised by high elemental C:N:P ratios. Emphasis was put on the impact of global change on the production of dissolved and particulate organic carbon, in order to gain a comprehensive understanding of the general partitioning between dissolved organic carbon (DOC) and POC. 14C incubations revealed that the partitioning between photosynthetically derived DOC and POC is highly dependent, not only on nutrient status and growth rate, but additionally affected by the combined rise of CO2 and temperature. Higher percentages of extracellular release (PER) were determined at lower growth rates and greenhouse conditions induced highest PER, thus the strongest partitioning to the dissolved pool. A major fraction of DOC is comprised by combined carbohydrates (CCHO) which are suggested to contain the pre-cursor molecules for aggregation and coagulation processes back to POC. The formation of gel-particles like transparent exopolymer particles (TEP) provides an abiotic linkage between DOC and POC. Enhanced partitioning to DOC also provides more high molecular weight (>1kDa) HMWdCCHO and therefore higher concentrations of pre-cursor material, potentially transferred back to POC. Despite of high PER, the percentage of HMW-dCCHO was smallest at greenhouse conditions accompanied by highest concentrations of TEP. Our results imply that greenhouse conditions will enhance exudation processes in E.huxleyi and may affect organic carbon partitioning in the greenhouse ocean due to an enhanced transfer of HMW-dCCHO to TEP by aggregation processes. With respect to global climate change, the amount and composition of DOC is of major interest to marine biologists, since it provides either a substrate for bacterial turnover or the pre-cursors for particle aggregation. In order to elucidate the role of carbon partitioning in oligotrophic regions in the future ocean, characterisation of dissolved organic material derived from E. huxleyi may provide information on its fate and function within the microbial loop and food-web dynamics.

Anthropogenic emissions have increased the concentration of carbon dioxide (CO2) during the last 200 years. Since radiative forcing by greenhouse gases plays an essential role in maintaining the Earth's temperature, increasing emissions resulted in an observed warming of the atmosphere and the ocean. Furthermore, the absorption of excess atmospheric CO2 by the ocean has increased the acidity of seawater at global scale. The experimental simulation of changes in seawater temperature and CO2 projected for the near future led to a substantial acceleration of organic matter degradation. Higher degradation rates were primarily induced by temperature and pH effects on bacterial extracellular enzymes that increased rates of polymer hydrolysis. Effects of changing ocean temperature and pH on bacterial activity and the consequences for the cycling of organic matter are highly relevant for marine organic carbon fluxes and the ocean-atmosphere CO2 exchange.

Engel, Anja

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