3D-electron microscopy of different conformations of cephalopod hemocyanins

Die Hämocyanine der Cephalopoden Nautilus pompilius und Sepia officinalis sorgen für den Sauerstofftransport zwischen den Kiemen und den Geweben. Sie bestehen aus einem zylindrischen Dekamer mit interner Kragenstruktur. Während eine Untereinheit (also eine Polypeptidkette) bei NpH aus sieben paralogen funktionellen Domänen (FU-a bis FU-g) besteht, führte ein Genduplikationsereignis der FU-d zu acht FUs in SoH (a, b, c, d, d´, e, f, g). In allen Mollusken Hämocyaninen bilden sechs dieser FUs den äußeren Ring und die restlichen die interne Kragenstruktur. rnrnIn dieser Arbeit wurde ein dreidimensionales Modell des Hämocyanins von Sepia officinalis (SoH) erstellt. Die Rekonstruktion, mit einer Auflösung von 8,8Å (FSC=0,5), erlaubt das Einpassen von Homolologiemodellen und somit das Erstellen eines molekularen Modells mit pseudo atomarer Auflösung. Des Weiteren wurden zwei Rekonstruktionen des Hämocyanins von Nautilus pompilius (NpH) in verschiedenen Oxygenierungszuständen erstellt. Die auf 10 und 8,1Å aufgelösten Modelle zeigen zwei verschiedene Konformationen des Proteins. Daraus ließ sich eine Modellvorstellung über die allosterische Funktionsweise ableiten. Die hier erreichte Auflösung von 8Å ist die momentan höchste eines Molluskenhämocyanins. rnAuf Grundlage des molekularen Modells von SoH konnte die Topologie des Proteins aufgeklärt werden. Es wurde gezeigt, dass die zusätzliche FU-d´ in den Kragen integriert ist und somit die prinzipielle Wandarchitektur aller Mollusken Hämocyanine identisch ist. Wie die Analyse des erstellten molekularen Modells zeigt werden sind die beiden Isoformen (SoH1 und SoH2) in den Bereichen der Interfaces nahezu identisch; auch der Vergleich mit NpH zeigt grosse Übereinstimmungen. Des weiteren konnte eine Fülle von Informationen bezüglich der allosterischen Signalübertragung innerhalb des Moleküls gewonnen werden. rnDer Versuch, NpH in verschiedenen Oxygenierungszuständen zu zeigen, war erfolgreich. Die Datensätze, die unter zwei atmosphärischen Bedingungen präpariert wurden, führten reproduzierbar zu zwei unterschiedlichen Rekonstruktionen. Dies zeigt, daß der hier entwickelte experimentelle Ansatz funktioniert. Er kann nun routinemäßig auf andere Proteine angewandt werden. Wie der strukturelle Vergleich zeigte, verändert sich die Orientierung der FUs durch die Oxygenierung leicht. Dies wiederum beeinflusst die Anordnung innerhalb der Interfaces sowie die Abstände zwischen den beteiligten Aminosäuren. Aus dieser Analyse konnte eine Modellvorstellung zum allosterischen Signaltransfer innerhalb des Moleküls abgeleitet werden, die auf einer Umordnung von Salzbrücken basiert.

Recombinant expression of molluscan hemocyanin (KLH) substructures in a prokaryotic system: E. coli

The recombinant expression of 19 different substructures of KLH in the prokaryotic sys-tem E. coli has been successfully achieved: each one of the eight single FUs a to h of both isoforms, KLH1 and KLH2, two substructures consisting of two consecutive FUs (KLH1-bc and KLH1-gh) as well as a cDNA encompassing KLH1-abc. All recombinant proteins, fused to an N-terminal 6xHis tag, have successfully been detected by immuno precipitation using monoclonal α-His-antibodies and polyclonal α-KLH1- and α-KLH2-antibodies. One exception remained: SP-KLH2-a, which was not detected by the α-His-antibodies. This allows speculations as to whether the coexpressed signal peptide can lead, at one hand, to the secretion of the recombinant protein, and on the other to the simultaneous cut-off of the leader peptide, which results in the splitting off of even more N-terminal 6xHis tag, leading to failed recognition by the appropriate antibodies. The comparison of native KLH with recombinantly expressed prokaryotic (E. coli) and eukaryotic (Sf9 insect cells) KLH was done using FU-1h. The weak detection by the polyclonal α-KLH1-antibodies of both recombinantly expressed proteins showed that the native protein was the best recognized. For the prokaryotic one, both the denaturation applied for solubilisation of the bacterial inclusion bodies and the inability of bacterial cells to add N-linked glycosylation, are the reason for the poor hybridization. In contrast, KLH1-h expressed in eukaryotic insect cells is likely to be glycosylated. The incubation with the α-KLH1-antibodies resulting in the same weak detection, however, revealed that the linked carbohydrate side chains are not those expected. The establishment of SOE-PCR, together with further improvement, has enabled the generation of a clone encompassing the complete subunit KLH1-abcdefgh. The se-quence analysis compared to the original KLH1 sequence showed, however, that the resulting recombinant protein is defective in two histidines, required for the copper bind-ing sites in FU-1b and FU-1d and in three disulfide bridges (FU-1a, FU-1b and FU 1g). This is due to polymerase-related nucleotide exchanges, resulting in a changed amino acid sequence. Nevertheless, all eight potential N-glycosylation sites are present, leading to the speculation that the recombinant protein can in theory be fully glycosylated, which is the most important aspect for the clinical applicability of recombinant KLH as an im-munotherapeutic agent. The improvement of this method elaborated during the present work indicates bright prospects for the future generation of a correct cDNA sequence encoding for the complete KLH2 subunit.

High-resolution reconstruction of Holocene climate variability and environmental changes in the North Pacific using bivalve shells

Bivalve mollusk shells are useful tools for multi-species and multi-proxy paleoenvironmental reconstructions with a high temporal and spatial resolution. Past environmental conditions can be reconstructed from shell growth and stable oxygen and carbon isotope ratios, which present an archive for temperature, freshwater fluxes and primary productivity. The purpose of this thesis is the reconstruction of Holocene climate and environmental variations in the North Pacific with a high spatial and temporal resolution using marine bivalve shells. This thesis focuses on several different Holocene time periods and multiple regions in the North Pacific, including: Japan, Alaska (AK), British Columbia (BC) and Washington State, which are affected by the monsoon, Pacific Decadal Oscillation (PDO) and El Niño/Southern Oscillation (ENSO). Such high-resolution proxy data from the marine realm of mid- and high-latitudes are still rare. Therefore, this study contributes to the optimization and verification of climate models. However, before using bivalves for environmental reconstructions and seasonality studies, life history traits must be well studied to temporally align and interpret the geochemical record. These calibration studies are essential to ascertain the usefulness of selected bivalve species as paleoclimate proxy archives. This work focuses on two bivalve species, the short-lived Saxidomus gigantea and the long-lived Panopea abrupta. Sclerochronology and oxygen isotope ratios of different shell layers of P. abrupta were studied in order to test the reliability of this species as a climate archive. The annual increments are clearly discernable in umbonal shell portions and the increments widths should be measured in these shell portions. A reliable reconstruction of paleotemperatures may only be achieved by exclusively sampling the outer shell layer of multiple contemporaneous specimens. Life history traits (e.g., timing of growth line formation, duration of the growing season and growth rates) and stable isotope ratios of recent S. gigantea from AK and BC were analyzed in detail. Furthermore, a growth-temperature model based on S. gigantea shells from Alaska was established, which provides a better understanding of the hydrological changes related to the Alaska Coastal Current (ACC). This approach allows the independent measurement of water temperature and salinity from variations in the width of lunar daily growth increments of S. gigantea. Temperature explains 70% of the variability in shell growth. The model was calibrated and tested with modern shells and then applied to archaeological specimens. The time period between 988 and 1447 cal yrs BP was characterized by colder (~1-2°C) and much drier (2-5 PSU) summers, and a likely much slower flowing ACC than at present. In contrast, the summers during the time interval of 599-1014 cal yrs BP were colder (up to 3°C) and fresher (1-2 PSU) than today. The Aleutian Low may have been stronger and the ACC was probably flowing faster during this time.