Das Hämocyanin zweier lebender Fossilien: Nautilus pompilius und Nucula nucleus

Als erste vollständige cDNA-Sequenz eines Muschel-Hämocyanins wurde das Nucula nucleus-Hämocyanin (NnH) sequenziert. Es besteht aus den beiden Isoformen NnH1 und NnH2, die eine Identität von etwa 61 % aufweisen. Beide sind aus acht funktionellen Domänen a-h aufgebaut, von denen die C-terminale Domäne h jeweils eine Extension von etwa 100 Aminosäuren besitzt. Auf Sequenzebene weist das Muschel-Hämocyanin eine eigentümliche Deletion im Bereich der ersten Kupferbindungsstelle und eine auffällig niedrige Anzahl an potentiellen N-Glykosylierungsstellen auf. Genomische Teilsequenzen bestätigen die Konservierung der Linkerintrons in Phase und Position, was bei den internen Introns nicht zu erkennen ist. Letztere konnten in den für die Domänen NnH1-d, NnH1-e und NnH2-c codierenden Genabschnitten nachgewiesen werden. Einen neuen Aspekt lieferte das interne Intron in NnH2-c, da es nur in einer der beiden Isoformen vorkommt. Das zweite sequenzierte Hämocyanin stammt von dem „lebenden Fossil“ Nautilus pompilius (NpH). Es wurde sowohl auf cDNA- als auch auf genomischer Ebene vollständig sequenziert und besteht aus sieben funktionellen Domänen, wobei die C-terminale Domäne h fehlt. Zu seinen Eigentümlichkeiten gehört neben 13 potentiellen N-Glykosylierungsstellen, von denen sich zwei innerhalb von Linkerregionen befinden, eine Deletion im Bereich der ersten Kupferbindungsstelle von NpH-g. Neben den konservierten Linkerintrons liegt ein Intron innerhalb des Signalpeptids sowie in den Genabschnitten für NpH-a und NpH-g. Dagegen ist weder zwischen dem Signalpeptid und NpH-a noch innerhalb der 3’UTR ein Intron vorhanden. Anhand der neuen Sequenzdaten wurde eine phylogenetische Analyse durchgeführt, in der sich die funktionellen Domänen von NnH als Schwestergruppe zu den korrespondierenden Domänen der Gastropoden anordnen. Den Erwartungen entsprechend stellt sich NpH basal innerhalb der Klasse der Cephalopoden. Phylogenetische Analysen mit der vollständigen Hämocyanin-Sequenz lösen die Verwandtschaftsverhältnisse der Klassen zueinander nicht auf, was auf schnelle Radiation schließen lässt. Die Gruppierungen innerhalb der Klassen werden dagegen sehr gut unterstützt. Mittels einer Distanzmatrix wurde eine molekulare Uhr berechnet, für deren Eichpunkt die Cephalopoden-Gastropoden-Aufspaltung vor 520 Millionen Jahren gewählt wurde. Die Entstehung der Acht-Domänen-Untereinheit fand danach vor 732 (± 33) Millionen Jahren statt. Die Trennung der Gastropoda und Protobranchia erfolgte vor 494 (± 50) Millionen Jahren, was mit Fossilfunden der Nuculidae aus dem Ordovicium übereinstimmt. Vor 396 (± 55) Millionen Jahren gingen aus einer Genduplikation die beiden Isoformen des Nucula nucleus-Hämocyanins hervor. Innerhalb der Cephalopoden wurde die Trennung zwischen Nautiloidea und Coleoidea auf 415 (± 24) Millionen Jahre zurückdatiert. Nach Fossildaten liegt der Trennungszeitraum der beiden Gruppen 470 - 400 Millionen Jahre zurück, was gut zu den Hämocyanin-Daten passt.

Beitrage zur Kenntniss der Gesteine und Fossilien der Chathaminseln sowie einiger Gesteine und neuer Nephritfundorte Neu-Seelands.

Thesis (doctoral)--Universitat Marburg.

Die Crinoiden der nordwestdeutschen Unterkreide

Diese Veröffentlichung ist der zweite und umfangreichste Ausschnitt meiner Examensarbeit. Ein erster Ausschnitt über die Crinoiden des Grenzgebietes Deutschland-Niederlande wurde bei "grondboor en hamer" eingereicht (in niederländischer Sprache), ein dritter Ausschnitt über die Crinoiden des Osning-Sandsteins ist für eine Zeitschrift des Naturkunde-Museums Bielefeld vorgesehen. Ziel der Examensarbeit ist es, erstens die Mega-, Meso- und Mikroreste der Crinoiden der nordwestdeutschen Unterkreide möglichst vollständig zu erfassen und systematisch zu bearbeiten, zweitens deren stratigraphische sowie paläogeographische bzw. fazielle Verbreitung zu ermitteln. Es wurde versucht, für diese Arbeit den größten Teil der in den verschiedenen Sammlungen vorhandenen Crinoidenreste zu berücksichtigen.

Stratigraphisch-Fazielle Untersuchungen an Dogger- und Malmzeitlichen Ablagerungen im Raum Wolfsburg (Ost-Niedersachsen)

Ziel der Arbeit ist es, ein genaueres Bild über Stratigraphie, Ablagerungsraum und Paläogeographie von Dogger und Malm des Raumes Wolfsburg zu erlangen. Dabei wurden u.a. zur Klärung insbesonders stratigraphischer Fragen Fossilien der neubestimmten Sammlung ROLKE herangezogen.

Riffe und fazielle Entwicklung der florigemma-Bank (Korallenoolith, Oxfordium) im Süntel und östlichen Wesergebirge (NW-Deutschland

During the Sedimentation of the platform carbonate deposits of the Korallenoolith Formation (middle Oxfordian to early Kimmeridgian) small buildups ofcorals formed in the Lower Saxony Basin. These bioconstructions are restricted to particular horizons (Untere Korallenbank,ßorigenuna-Bank Member etc.) and represent patch reefs and biostromes. In this study, the development of facies, fossil assemblages, spatial distribution of fossils, and reefs of the ßorigenuna-Bank Member (upper Middle Oxfordian) in the Süntel Mts and the eastern Wesergebirge Mts is described; the formation of reefs is discussed in detail. Twelve facies types are described and interpreted. They vary between high-energy deposits as well winnowed oolites and quiet-water lagoonal mudstones. Owing to the significance of biota, micro- and macrofossils are systematically described. The reefs are preserved in growth position, are characterized by numerous corresponding features and belong to a certain reef type. According to their size, shape and framework, they represent patch reefs, coral knobs (sensu James, 1983), coral thrombolite reefs (sensu Leinfelder et al., 1994) or “Klein- and Mitteldickichte” (sensu Laternser, 2001). Their growth fabric corresponds to the superstratal (dense) pillarstone (sensu Insalaco, 1998). As the top of the ßorigenuna-Bank displays an erosional unconformity (so-called Hauptdiskontinuität), the top of the reefs are erosionally capped. Their maximum height amounts to at least the maximum thickness of the ßorigenuna-Bank which does not exceed 4 metres. The diversity of coral fauna of the reefs is relatively low; a total of 13 species is recorded. The coral community is over- whelmingly dominated by the thin-branched ramose Thamnasteria dendroidea (Lamouroux) that forms aggregations of colonies (77?. dendroidea thickets). Leafy to platy Fungiastrea arachnoides (Parkinson) and Thamnasteria concinna (Goldfuss) occur subordinately, other species are only of minor importance. In a few cases, the reef-core consisting of Th. dendroidea thickets is laterally encrusted by platy F. arachnoides and Th. concinna colonies, and microbial carbonates. This zonation reflects probably a succession of different reef builders as a result of changing environmental conditions (allogenic succession). Moreover, some reefs are overlain by a biostrome made of large Solenopora jurassica nodules passing laterally in a nerinean bed. Mikrobial carbonates promoted reef growth and favoured the preservation of reef organismn in their growth position or in situ. They exhibit a platy, dendroid, or reticulate growth form or occur as downward-facing hemispheroids. According to their microstructure, they consist of a peloidal, clotted, or unstructured fabric (predominately layered and poorly structured thrombolite as well as clotted leiolite) (sensu Schmid, 1996). Abundant endo- and epibiontic organisms (bivalves, gastropods, echinoids, asteroids, ophiuroids, crabs etc) are linked to the reefs. With regard to their guild structure, the reefs represent occurrences at which only a few coral species serve as builder. Moreover, microbial carbonates contribute to both building and binding of the reefs. Additional binder as well as baffler are present, but not abundant. According to the species diversity, the dweller guild comprises by far the highest number of invertebrate taxa. The destroyer guild chiefly encompasses bivalves. The composition of the reef community was influenced by the habitat structure of the Th. dendroidea thickets. Owing to the increase in encrusting organisms and other inhabitants of the thickets, the locational factors changed, since light intensity and hydrodynamic energy level and combined parameters as oxygen supply declined in the crowded habitat. Therefore a characteristic succession of organisms is developed that depends on and responds to changing environmental conditions („community replacement sequence“). The succession allows the differentiation of different stages. It started after the cessation of the polyps with boring organisms and photoautotrophic micro-encrusters (calcareous algae, Lithocodium aggregatum). Following the death of these pioneer organisms, encrusting and adherent organisms (serpulids, „Terebella“ species, bryozoans, foraminifers, thecideidinids, sklerospongid and pharetronid sponges, terebratulids), small mobile organisms (limpets), and microbial induced carbonates developed. The final stage in the community replacement sequence gave rise to small cryptic habitats and organisms that belong to these caves (cryptobionts, coelobites). The habitat conditions especially favoured small non-rigid demosponges (“soft sponges”) that tolerate reduced water circulation. Reef rubble is negligible, so that the reefs are bordered by fossiliferous micritic limestone passing laterally in micritic limestone. Approximately 10% of the study area (outcropping florigemma-Bank) corresponds to reefal deposits whereas the remaining 90% encompass lagoonal inter-reefal deposits. The reef development is a good example for the interaction between reef growth, facies development and sea-level changes. It was initiated by a sea-level rise (transgression) and corresponding decrease in the hydrodynamic energy level. Colonization and reef growth took place on a coarse-grained Substrate composed of oncoids, larger foraminifers and bioclasts. Reef growth took place in a calm marine lagoonal setting. Increasing abundance of spherical coral morphs towards the Northeast (section Kessiehausen, northwestem Süntel Mts) reflects higher turbidity and a facies transition to coral occurrences of the ßorigenuna-Bank Member in the adjacent Deister Mts. The reef growth was neither influenced by stonns nor by input of siliciclastic deposits, and took place in short time - probably in only a thousand years under most probably mesotrophic conditions. The mass appearance of solenoporids and nerineids in the upper part of the ßorigenuna-Bank Member point to enhanced nutrient level as a result of regression. In addition, this scenario of fluctuations in nutrient availability seems to be responsible for the cessation of reef corals. The sea level fall reached its climax in the subaerial exposure and palaeokarst development of the florigemma-Bank. The reef building corals are typical pioneer species. The blade-like, flattened F. amchnoides colonies are characterized by their light porous calcium carbonate skeleton, which is a distinct advantage in soft bottom environment. Thus, they settled on soft bottom exposing the large parts of its surface to the incoming light. On the other hand, in response to their light requirements they were also able to settle shaded canopy structures or reef caves. Th. dendroidea is an opportunistic coral species in very shallow, well illuminated marine environment. Their thin and densely spaced branches led to a very high surface/volume ratio of the colonies that were capable to exploit incoming light due to their small thamasterioid calices characterized by “highly integrated polyps”. In addition, sideward coalescence of branches during colony growth led to a wave-resistant framework and favoured the authochthonous preservation of the reefs. Asexual reproduction by fragmented colonies promoted reef development as Th. dendroidea thickets laterally extend over the sea floor or new reefs have developed from broken fragments of parent colonies. Similar build ups with Th. dendroidea as a dominant or frequent reef building coral species are known from the Paris Basin and elsewhere from the Lower Saxony Basin (Kleiner Deister Mts). These buildups developed in well-illuminated shallow water and encompass coral reefs or coral thrombolite reefs. Intra- and inter-reef deposits vary between well-winnowed reef debris limestone and mudstones representing considerably calmer conditions. Solenoporid, nerineids and diceratides belong to the characteristic fossils of these occurrences. However, diceratides are missing in theflorigemma-Bank Member. Th. dendroidea differs in its colonization of low- to high-energy environment from recent ramose scleractinian corals (e.g., Acropora and Porites sp.). The latter are restricted to agitated water habitats creating coral thickets and carpets. According to the morphologic plasticity of Th. dendroidea, thick-branched colonies developed in a milieu of high water energy, whereas fragile, wide- and thin-branched colonies prevail in low-energy settings. Due to its relatively rapid growth, Th. dendroidea was able to keep pace with increased Sedimentation rates. 68 benthonic foraminiferan species/taxa have been recognized in thin sections. Agglutinated foraminifers (textulariids) predominate when compared with rotaliids and milioliids. Numerous species are restricted to a certain facies type or occur in higher population densities, in particular Everticyclammina sp., a larger agglutinated foraminifer that occurs in rock building amounts. Among the 25 reef dwelling foraminiferal species, a few were so far only known from Late Jurassic sponge reefs. Another striking feature is the frequency of adherent foraminiferal species. Fauna and flora, in particular dasycladaleans and agglutinated foraminifers, document palaeobiogeographic relationships to the Tethys and point to (sub)tropical conditions. Moreover, in Germany this foraminiferan assemblage is yet uncompared. In Southern Germany similar tethyan type assemblages are not present in strata as young as Middle Tithonian.