Impact of folate absorption and transport for nutrition and drug targeting

In this thesis, interactions of folic acid with tea and tea components at the level of intestinal absorption have been investigated. Firstly, the interaction between folic acid and tea as well as tea catechins was studied in vitro, using Caco-2 cell monolayers and secondly, a clinical trial was designed and carried out. In addition, targeting of folic acid conjugated nanoparticles to FR expressing Caco-2 cells was studied in order to evaluate the principle of nutrient-receptor-coupled transport for drug targeting. In the first part of this work, it was shown that EGCG and ECG (gallated catechins) inhibit folic acid uptake (IC50 of 34.8 and 30.8 µmol/L) comparable to MTX (methotrexate) under these experimental conditions. Moreover, commercial green and black tea extracts inhibited folic acid uptake with IC50 values of approximately 7.5 and 3.6 mg/mL, respectively. These results clearly indicate an interaction between folic acid and green tea catechins at the level of intestinal uptake. The mechanism responsible for the inhibition process might be the inhibition of the influx transport routes for folates such as via RFC and/or PCFT. For understanding the in vivo relevance of this in vitro interaction, a phase one, open-labeled, randomized, cross-over clinical study in seven healthy volunteers was designed. For the 0.4 mg folic acid dose, the mean Cmax decreased by 39.2% and 38.6% and the mean AUC0 decreased by 26.6% and 17.9% by green tea and black tea, respectively. For the 5 mg folic acid dose, the mean Cmax decreased by 27.4% and mean AUC0 decreased by 39.9% when taken with green tea. The results of the clinical study confirm the interaction between tea and folic acid in vivo leading to lower bioavailabilities of folic acid. In the second part of the thesis, targeting studies using folic acid conjugated nanoparticles were conducted. Folic acid conjugated nanoparticles were shown to be internalized by the cell via FR (folate receptor) mediated endocytosis. DNA block copolymer micelles equipped with 2, 11 and 28 folic acid units respectively were applied on FR expressing Caco-2 cells. There was a direct proportion in the amount of internalized nanoparticle and the number of folic acid units on the periphery of the nanoparticle. To sum up, throughout this thesis, the importance of folic acid for nutrition and nutrient and drug related interactions of folic acid at intestinal level was shown. Furthermore, significance of FRs in targeting for cancer chemotherapy was demonstrated in in vitro cell culture experiments. Folic acid conjugated DNA block copolymer micelles were suggested as efficient nanoparticles for targeted drug delivery.

Copper and zinc stable isotope ratios as tracers of biogeochemical processes, sources and transport of Cu and Zn in soils

Copper and Zn are essential micronutrients for plants, animals, and humans; however, they may also be pollutants if they occur at high concentrations in soil. Therefore, knowledge of Cu and Zn cycling in soils is required both for guaranteeing proper nutrition and to control possible risks arising from pollution.rnThe overall objective of my study was to test if Cu and Zn stable isotope ratios can be used to investigate into the biogeochemistry, source and transport of these metals in soils. The use of stable isotope ratios might be especially suitable to trace long-term processes occurring during soil genesis and transport of pollutants through the soil. In detail, I aimed to answer the questions, whether (1) Cu stable isotopes are fractionated during complexation with humic acid, (2) 65Cu values can be a tracer for soil genetic processes in redoximorphic soils (3) 65Cu values can help to understand soil genetic processes under oxic weathering conditions, and (4) 65Cu and 66Zn values can act as tracers of sources and transport of Cu and Zn in polluted soils.rnTo answer these questions, I ran adsorption experiments at different pH values in the laboratory and modelled Cu adsorption to humic acid. Furthermore, eight soils were sampled representing different redox and weathering regimes of which two were influenced by stagnic water, two by groundwater, two by oxic weathering (Cambisols), and two by podzolation. In all horizons of these soils, I determined selected basic soil properties, partitioned Cu into seven operationally defined fractions and determined Cu concentrations and Cu isotope ratios (65Cu values). Finally, three additional soils were sampled along a deposition gradient at different distances to a Cu smelter in Slovakia and analyzed together with bedrock and waste material from the smelter for selected basic soil properties, Cu and Zn concentrations and 65Cu and 66Zn values.rnMy results demonstrated that (1) Copper was fractionated during adsorption on humic acid resulting in an isotope fractionation between the immobilized humic acid and the solution (65CuIHA-solution) of 0.26 ± 0.11‰ (2SD) and that the extent of fractionation was independent of pH and involved functional groups of the humic acid. (2) Soil genesis and plant cycling causes measurable Cu isotope fractionation in hydromorphic soils. The results suggested that an increasing number of redox cycles depleted 63Cu with increasing depth resulting in heavier 65Cu values. (3) Organic horizons usually had isotopically lighter Cu than mineral soils presumably because of the preferred uptake and recycling of 63Cu by plants. (4) In a strongly developed Podzol, eluviation zones had lighter and illuviation zones heavier 65Cu values because of the higher stability of organo-65Cu complexes compared to organo-63Cu complexes. In the Cambisols and a little developed Podzol, oxic weathering caused increasingly lighter 65Cu values with increasing depth, resulting in the opposite depth trend as in redoximorphic soils, because of the preferential vertical transport of 63Cu. (5) The 66Zn values were fractionated during the smelting process and isotopically light Zn was emitted allowing source identification of Zn pollution while 65Cu values were unaffected by the smelting and Cu emissions isotopically indistinguishable from soil. The 65Cu values in polluted soils became lighter down to a depth of 0.4 m indicating isotope fractionation during transport and a transport depth of 0.4 m in 60 years. 66Zn values had an opposite depth trend becoming heavier with depth because of fractionation by plant cycling, speciation changes, and mixing of native and smelter-derived Zn. rnCopper showed measurable isotope fractionation of approximately 1‰ in unpolluted soils, allowing to draw conclusions on plant cycling, transport, and redox processes occurring during soil genesis and 65Cu and 66Zn values in contaminated soils allow for conclusions on sources (in my study only possible for Zn), biogeochemical behavior, and depth of dislocation of Cu and Zn pollution in soil. I conclude that stable Cu and Zn isotope ratios are a suitable novel tool to trace long-term processes in soils which are difficult to assess otherwise.rn