Browsing by Subject "Sequestrierung"

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Pathways of C and N turnover in soil under elevated atmospheric CO2
(2008) Dorodnikov, Maxim; Fangmeier, Andreas
In the present thesis the C and N transformations in soil as influenced by indirect effect of elevated atmospheric CO2, soil physical structure and land use change were studied in four laboratory experiments using stable-C and N isotopes, as well as soil microbiological techniques. To test the interrelations between chemical and biological characteristics of soil organic matter (SOM) as affected by land use change and elevated atmospheric CO2 an approach for SOM partitioning based on its thermal stability was chosen. In the first experiment C isotopic composition of soils subjected to C3-C4 vegetation change (grassland to Miscanthus x gigantheus, respectively) was used for the estimation of C turnover in SOM pools. In the 2nd (Free Air CO2 Enrichment ? FACE ? Hohenheim) and 3rd (FACE Braunschweig) experiments CO2 applied for FACE was strongly depleted in 13C and thus provided an opportunity to study C turnover in SOM based on its δ13C value. Simultaneous use of 15N labeled fertilizers allowed N turnover to be studied (in the 2nd experiment). We hypothesized that the biological availability of SOM pools expressed as the mean residence time (MRT) of C or N is inversely proportional to their thermal stability. Soil samples were analysed by thermogravimetry coupled with differential scanning calorimetry (TG-DSC). According to differential weight losses between 20 and 1000 °C (dTG) and energy release or consumption (DSC), SOM pools (4 to 5 depending on experiment) with increasing thermal stability were distinguished. Soil samples were heated up to the respective temperature and the remaining soil was analyzed for δ13C and δ15N by IRMS. For all three experiments the separation of SOM based on its thermal stability was not sufficient to reveal pools with contrasting turnover rates of C and N. A possible explanation for the inability of thermal oxidation for isolating SOM pools of contrasting turnover times is that the fractionation of SOM pools according to their thermal stability is close to chemical separation. In turn, it was found that chemical separations of SOM failed to isolate the SOM pools of different turnover time because different biochemical plant components (cellulose, lignin) are decomposed in a wide temperature range. Individual components of plant residues may be directly incorporated into, or even mixed with the thermal stable SOM pools and will so mask low turnover rates of these pools. To evaluate the interactions between availability of SOM for decomposition by soil microbial biomass (biological characteristic) under elevated atmospheric CO2 and protection of SOM due to the occlusion within aggregates of different sizes (physical property, responsible for SOM sequestration) we measured the activity of microbial biomass (indicated by enzyme activities) and growth strategies of soil microorganisms (fast- vs. slow growing organisms) in isolated macro- and microaggregates. The contribution of fast (r-strategists) and slowly growing microorganisms (K-strategists) in microbial communities was estimated by the kinetics of the CO2 emission from bulk soil and aggregates amended with glucose and nutrients (Substrate Induced Growth Respiration method). Although Corg and total Cmic were unaffected by elevated CO2, maximal specific growth rates were significantly higher under elevated than ambient CO2 for bulk soil, small macroaggregates, and microaggregates. Thus, we conclude that elevated atmospheric CO2 stimulated the r-selected microorganisms. Such an increase in r-selected microorganisms could increase C turnover in terrestrial ecosystems in a future elevated atmospheric CO2 environment. The activities of β-glucosidase, phosphatase and sulphatase were unaffected in bulk soil and in aggregate-size classes by elevated CO2, however, significant changes were observed in potential enzyme production after substrate amendment. After adding glucose, enzyme activities under elevated CO2 were 1.2-1.9-fold higher than under ambient CO2. This indicates an increased activity of microorganisms, which leads to accelerated C turnover in soil under elevated CO2. Significantly higher chitinase activity in bulk soil and in large macroaggregates under elevated CO2 revealed an increased contribution of fungi to turnover processes. At the same time, less chitinase activity in microaggregates underlined microaggregate stability and the difficulties for fungi hyphae penetrating them. We conclude that quantitative and qualitative changes of C input by plants into the soil at elevated CO2 affect microbial community functioning, but not its total content. Future studies should therefore focus more on the changes of functions and activities, but less on the pools. In conclusion, elevated CO2 concentrations in the atmosphere along with soil physical structure have a pronounced effect on qualitative but not quantitative changes in C and N transformations in soil under agricultural ecosystem. The physical parameters of soil such as aggregation correlate more with biological availability of SOM than the chemical properties of soil organic materials. The increase of soil microbial activity under elevated CO2 detected especially in soil microaggregates, which are supposed to be responsible for SOM preservation, prejudice sequestration of C in agroecosystems affected by elevated atmospheric CO2.
Sequestration of plant toxins in milkweed bugs (Heteroptera: Lygaeinae) : physiological implications and mechanisms
(2023) Espinosa del Alba, Laura; Petschenka, Georg
Insect herbivores and plants together are a crucial component of terrestrial macro-biodiversity. Within the realm of plant-insect interactions, phytophagy by insects triggered an “arms-race” dynamic resulting in escalatory adaptation and counter-adaptation over time. This coevolution led to complex phenomena such as sequestration of plant toxins by specialized insects, with the main aim to deter predators. Although sequestration is an extensively reported phenomenon, many physiological aspects and underlying mechanisms remain largely unexplored. Milkweed bugs (Heteroptera: Lygaeinae) constitute a versatile model ideally suited for studying both areas due to their particular evolutionary history. They are primarily associated with plant species in the Apocynaceae which commonly produce cardenolides, but remarkably some milkweed bug species secondarily evolved novel associations with phylogenetically disparate plant families supplying new sources of chemically related or unrelated toxins. Using as model milkweed bugs the cardenolide specialist Oncopeltus fasciatus and Spilostethus saxatilis, a species that shifted to sequestration of the chemically unrelated colchicoids, the present thesis first aimed to develop a new artificial diet that allowed the incorporation of the desired types and amounts of toxins without impairing insect performance. Taking a simplified approach, an artificial diet presented in a pill form and made of 100% organic sunflower meal was established. Despite the fact that the new diet has remarkable energy and nutrient differences with sunflower seeds (the laboratory diet), no differences in terms of insect performance were found between the two diets in O. fasciatus and S. saxatilis. Moreover, the new diet presented an acceptable concentration accuracy and shelf-life for short-term toxin feeding assays. Once established, the new diet was used to investigate the effects of cardenolides and colchicoids on several life-history traits of S. saxatilis, and to compare them with the effect of cardenolides in O. fasciatus. Although both classes of toxins have different molecular targets (cardenolides: Na+/K+-ATPase; colchicoids: tubulin), S. saxatilis was able to sequester them at a cost-free level. In fact, an increased performance was observed in O. fasciatus and an according trend was found in S. saxatilis after dietary exposure to cardenolides and colchicoids, respectively. Among cardenolides, labriformin is especially toxic for milkweed-specialist Na+/K+-ATPases in vitro. Nevertheless, it was shown to have no costs in terms of growth and fertility at the whole organism level for O. fasciatus. This finding might be an example of reciprocal evolution between milkweed plants and its herbivores, where highly toxic cardenolides specifically targeted to insect specialists are counteracted by tolerance, detoxification, and sequestration strategies. To assess the role of sequestration beyond normal physiological conditions, O. fasciatus and S. saxatilis were orally infected with the bacterium Pseudomonas entomophila. Neither cardenolides nor colchicoids provided a higher resistance or tolerance. Regarding mechanisms of sequestration, the other overarching research topic of the present thesis, both in vivo (whole animal) and in vitro (isolated digestive tracts) approaches showed no reciprocal competition for the same transport mechanism between chemically related and unrelated toxins. Furthermore, the digestive tract of milkweed bugs did not seem to be a critical mediator as it is for other non-sequestering and sequestering species. The time course of sequestration for the model species was resolved from three days to one hour, and the higher levels of colchicoids detected in S. saxatilis compared to the level of cardenolides in O. fasciatus might indicate an early acquisition of defenses with the shift from cardenolide to colchicoid-containing plants. Finally, a hint to preadaptation mechanisms to resist novel toxins was documented in Spilostethus pandurus, a species that belongs to the same genus as S. saxatilis, thereby providing a basis for future investigations.