Biologische Hochschulschriften (Goethe-Universität; nur lokal zugänglich)
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Succinate:quinone oxidoreductases (SQORs) are integral membrane protein complexes, which couple the two-electron oxidation of succinate to fumarate (succinate → fumarate + 2H+ + 2e-) to the two-electron reduction of quinone to quinol (quinone + 2H+ + 2e- → quinol) as well as catalyzing the opposite reaction, the reduction of fumarate by quinol. In mitochondria and some aerobic bacteria, succinate:ubiquinone reductase, also known as complex II of the aerobic respiratory chain or as succinate dehydrogenase from the tricarboxylic acid (TCA or Krebs) cycle, catalyzes the oxidation of succinate by ubiquinone, which is mildly exergonic under standart conditions and not directly associated with energy storage in the form of a transmembrane electrochemical proton potential (Δp). Gram-positive bacteria do not contain ubiquinone but rather menaquinone, a quinone with significantly lower oxidation-reduction (“redox”) midpoint potential. In these cases, the catalyzed oxidation of succinate by quinone is endergonic under standard conditions. Consequently, these bacteria face a thermodynamic problem in supporting the catalysis of this reaction in vivo. Based on experimental evidence obtained on whole cells and purified membranes, it had previously been proposed that the SQR from Gram-positive bacteria supports this reaction at the expense of the protonmotive force, Δp. Nonetheless, it has been argued that the observed Δp dependence is not associated specifically with the activity of SQR because the occurrence of artifacts in experiments with bacterial membranes and whole cells can not be fully excluded. Clearly, definitive insight into the mechanism of catalysis of this intriguing reaction required a corresponding functional characterization of an isolated, membranebound SQR from a Gram-positive bacterium. The first aim of the present work addresses the question if the general feasibility of the energetically uphill electron transfer from succinate to menaquinone is associated specifically to a single enzyme complex, the SQR. The prerequisite to achieve this goal was stable preparation of this enzyme.
Paleoecology is the study of organismal interactions with the environment in the geological past. Organisms are influenced in their distribution and abundance by abiotic factors such as temperature and precipitation. A change in these factors, for example by major climatic shifts, would then affect the communities of organisms. Studying this hypothesized causal link between climatic and faunal change is especially interesting for the Plio-Pleistocene of East Africa due to the fact that our own ancestors also inhabited these regions. Both the Turkana basin in Kenya and the Lake Albert region in Uganda offer unique opportunities to investigate these paleoecological issues. Their late Miocene through Pleistocene deposits provide a very good record of climatic, vegetation and faunal change in East Africa (Pickford et al. 1993, Leakey et al. 1995, 1998, McDougall & Feibel 2003, Wynn 2004). This study focuses on the mammal family Bovidae as they are good indicator of vegetation and environment (e.g. Vrba 1980, 1995, Shipman & Harris 1988, Bobe & Eck 2001, Bobe & Behrensmeyer 2004, Bobe et al. 2007). Bovidae are quite species-rich and inhabit a wide range of habitats from tropical rain forests to deserts which predicates their array of morphological adaptations (ecovariables) to these environments. Diet is the ecovariable that is most to climate and thus habitat change. Therefore, the fossil Bovidae are especially suitable for reconstructing past environments. The objective of this thesis is to test the hypothesis that, from the late Miocene through the Holocene, Africa has experienced an overall increase in aridity and concomitant pulses of habitat change. The hypothesis predicts that increasing aridity causes a likewise growth in the abundance of taxa adapted to open arid environments. In particular, an increase in bovid grazers should be observed in combination with a decrease of bovid browsers. To test this hypothesis, I examine the fossil bovid communities from each stratigraphic member of Lake Turkana (Lothagam, Kanapoi, West Turkana and Koobi Fora) and Lake Albert (Nkondo-Kaiso region) and through a taxonomic and a functional perspective reconstruct the paleoenvironments and -climates from approximately 8 to 0.6 Ma. This study is the first to use taxonomic and ecomorphological data together to reconstruct the paleoenvironments of the Turkana basin and the Nkondo-Kaiso region of Lake Albert. In a first analysis, mesowear, as introduced by Fortelius & Solounias (2000), is used to gather information about the diet of bovids. As a result of my preliminary investigations on upper vs. lower molars of recent species, the sample of fossil bovid specimens from the Turkana basin and Lake Albert were found to be unsuitable to reveal a meaningful diet reconstruction. Therefore, the bovids are assigned to diet categories based on literature. For each member of the time period from 8.0 to 0.6 Ma, I provide a detailed characterization of the bovid fauna in terms of α- and β- diversity both on tribe and diet level based on presence-absence as well as for the Turkana basin on abundance data. Statistical comparisons between the fossil bovid communities and those in modern protected areas with known vegetation and climatic conditions have yielded modern analogues for each stratigraphic member. Following that I provide paleoclimatic conditions such as assumed mean annual temperature for each member. Based on abundance of diet categories in the bovid communities, the paleoclimate of the Turkana basin was in general cooler and considerably more humid during the late Miocene to the Pleistocene than today. The mean annual temperature at Lothagam is assumed as 22.2 °C, the annual precipitation as 685 mm for 8.0 – 6.54 Ma and 4.9 – 3.4 Ma. The intervening time period is characterized by a slightly lower mean annual temperature and precipitation (20.3 °C, 583 mm). From 4.17 to 4.07 Ma Kanapoi faced 21.3 °C and 592 mm rainfall. In the eastern part of the basin the climate was warmer and more humid (3.4 – 2.68 Ma: 26.2, 961 mm; 2.68 – 1.3 Ma: 27.1 °C, 935 mm) from 3.4 to 1.3 Ma than in the preceeding eras. In the western part, the climate became warmer and more humid ~500,000 years later and was more variable than that in the eastern basin. From 2.94 to 2.52 Ma the mean annual temperature was 26.2 °C and the annual precipitation 961 mm. Between 2.34 and 1.6 Ma the climate again cooled and became drier as before 2.94 Ma. A second shift to higher temperature and precipitation occurred after 1.6 Ma (27.1 °C, 935 mm) lasted until 1.34 Ma. The results of the bovid community analyses do not support the hypothesis of increasing aridity in Eastern Africa during the late Mio- to Pleistocene. Instead, the results show that the bovid communities differed much over time and on a relatively small spatial scale. Regional paleovegetation and paleoclimate exhibit fluctuations through the studied time period at western Turkana and differences between the western and eastern part of the Turkana basin. This is indicative of a patchy habitat distribution both on temporal and spatial levels. Increased climate variability predicts an increase in landscape complexity as proposed by the ‘variability selection hypothesis’ (Potts 1998a+b). Therefore, this thesis research supports the hypothesis of increased landscape complexity on the spatial level. This study has important implications for future research. First, an analysis based on ecovariable characteristics such as diet may be preferred to a taxonomic analysis. Second, abundance data should be used for an ecovariable analysis because the results then provide more precise information on the paleovegetation and –climate than just the presence of these adaptations in the faunal community. Lastly, as this study is based on one mammal family, further studies on other mammal groups should be conducted to increase the database of exploited resource by the entire faunal community. Most significantly this study provides a basis for new interpretations of faunal community distributions. It also raises the question whether small scale spatial community variability is also to be expected at other fossil sites. If so then this methodology has important implications for reconstructions of paleovegetation and paleoclimate.
Iron uptake is an essential process in all Gram-negative bacteria including cyanobacteria and therefore different transport systems evolved during evolution. In cyanobacteria, however, the iron demand is higher than in proteobacteria due to the function of iron as cofactor in e.g. photosynthesis and nitrogen fixation. Most of the transport systems depend on outer membrane localized TonB-dependent transporters (TBDTs), a periplasma-facing TonB protein and a plasma membrane localized machinery (ExbBD). So far, iron chelators (siderophores), oligosaccharides and polypeptides have been identified as substrates of TBDTs. However, in proteobacteria TonB-dependent outer membrane transporter represent a well-explored subject whereas for cyanobacteria almost nothing is known about possible TonB-dependent uptake systems for iron or other substrates. The heterocyst-forming filamentous cyanobacterium Anabaena sp. PCC 7120 is known to secrete the siderophore schizokinen, but its transport system has remained unidentified. For Anabaena sp. PCC 7120 22 genes were identified as putative TBDTs covering almost all known TBDT subclasses. This is a high number of TBDTs compared to other cyanobacteria. The expression of the 22 putative TBDTs individually depends on the presence of iron, copper or nitrogen. The atypical dependence of TBDT gene expression on different nutrition points to a yet unknown regulatory mechanism. In addition, the hypothesis of the absence of TonB in Anabaena sp. PCC 7120 was clarified by the identification of an according sequence, all5036. Inspection of the genome of Anabaena sp. PCC 7120 shows that only one gene encoding a putative TonB-dependent iron transporter, namely alr0397, is positioned close to genes encoding enzymes involved in the biosynthesis of a hydroxamate siderophore. The expression of alr0397 was elevated under iron-limited conditions. Inactivation of this gene caused a moderate phenotype of iron starvation in the mutant cells. The characterization of the mutant strain showed that Alr0397 is a TonB-dependent schizokinen transporter (SchT) of the outer membrane and that alr0397 expression and schizokinen production are regulated by the iron homeostasis of the cell. Additional two genes of Anabaena sp. PCC 7120 involved in this process were identified. SchE encoded by all4025 is a putative cytoplasmic membrane-localized transporter involved in TolC-dependent siderophore secretion. The mutation of schE resulted in an enhanced sensitivity to high metal concentrations and in drastically reduction of secretion of hydroxamate-type siderophores. IacT coded by all4026 is a predicted outer membrane-localized TonB-dependent iron transporter. Inactivation of iacT resulted in reduced sensitivity to elevated iron and copper levels, whereas decoupling the expression from putative regulation by exchange of the promoter resulted in sensitization against tested metals. Further analysis showed that iron and copper effects are synergistic because decrease of iron induced a significant decrease of copper levels in the iacT insertion mutant but an increase of those levels in Anabaena sp. PCC 7120 where expression of all4026 is under the trc-promoter. In consequence, the results unravel a link between iron and copper homeostasis.