ALBERT

Description: Mit dem Bekanntwerden der Conodonten in der Literatur (Pander 1856) begann auch die Diskussion um die Stellung dieser Fossilreste im System. Zahlreiche Publikationen beschäftigten sich damit, keine konnte das Problem lösen, keine der Ansichten fand allgemeine und uneingeschränkte Anerkennung. Um so interessanter schien es, als im Sommer 1964 von K. Fahlbusch eine umfangreiche Abhandlung unter dem Titel „Die Stellung der Conodontida im biologischen System“ erschien. F. kommt auf Grund seiner Untersuchungen zu dem Ergebnis, die Conodonten seien Reste fossiler Algen. Diese Ansicht weicht so stark von allen bisher geäußerten Meinungen über die systematische Stellung der conodontentragenden Organismen ab, daß sie eine eingehende kritische Überprüfung des Materials, der gedanklichen Voraussetzungen, der so weit reichenden Schlußfolgerungen und der nachfolgenden Weiterungen des Autors herausfordert. Nachdem Herr Fahlbusch freundlicherweise zwei Verf. (Krebs u. Ziegler) den größten Teil seines Materials vorgeführt hat, soll an dieser Stelle Kritik am Material und an der Hypothese der Algen-Zugehörigkeit geübt werden. Wir sehen uns zu diesem Schritt leider gezwungen, um einer sonst möglichen Übernahme, der Vorstellungen F.’s und ihrem Eingang in die Literatur entgegenzuwirken. Die Verf. sind einer großen Zahl von Kollegen zu großem Dank für Diskussionsbereitschaft und tätige Mithilfe verpflichtet. Besonderer Dank gebührt Dr. H. Werner (Chemiker) und Dr. H. Pietzner (Mineraloge) am Geologischen Landesamt Nordrhein-Westfalen in Krefeld, die den Abschnitt über chemische und röntgenographische Untersuchungsverfahren in der Arbeit Fahlbusch eingehend und fachkundig durcharbeiteten und im Zusammenhang damit — wo es nötig und möglich erschien — auch Kontrolluntersuchungen durchführten. Ebenso sind wir Privatdozent Dr. E. Flügel (Paläontologe), Inst. f. Geologie, TH Darmstadt, für spezielle Hinweisedankbar (s. 〉S. 392).

Description: The variation in life-history patterns that allow closely related species to co-exist has been an important theme in ecology for decades. We examined intra- and interspecific variation in a key life-history trait - diapause - for two congeneric copepods (Eudiaptomus gracilis and Eudiaptomus graciloides) inhabiting three lakes in Northern Germany. Diapause has been hypothesized in both theoretical and empirical studies to be important in the coexistence of competing species. We found no diapause for E. gracilis whereas we documented two distinct periods of diapause in the life cycle of E. graciloides. In the latter species, diapausing eggs were produced in all three lakes during autumn, however, relative investment in diapausing eggs differed between lakes. Diapausing egg production was delayed or fewer females switched to making diapausing eggs in the more productive lakes relative to the less productive systems. In the sediments of all three lakes, viable diapausing eggs were found buried from the sediment-water interface down several centimeters in each lake, suggesting the presence of a long-lived egg bank. In addition, detailed population studies carried out on both species in one lake (Schöhsee) revealed a second period of diapause in E. graciloides. After the diapausing eggs are produced in autumn, females accumulate lipids, reduce feeding and apparently over-winter in a state of active diapause. The prevalence of diapause in E. graciloides and lack of it in E. gracilis raises questions regarding the factors that shape the life-histories of these congeners, and the role that the life-history differences observed may play in their coexistence.

Description: In this article we review the indirect interactions prevailing in littoral communities and compare their importance to direct trophic interactions. We focus on the interaction between benthic algae and their herbivorous consumers, i. e. invertebrate grazers and herbivorous fish. In addition to the effects of grazers on periphyton biomass and production, we categorise and describe the types of indirect interactions observed and we present a quantitative meta-analysis to compare the effect magnitude of indirect and direct effects. Our review shows that herbivore-plant interactions comprise considerable complexity beyond consumption. We identify and review three different indirect interactions, which play important roles for periphyton-grazer interactions in benthic food webs. These are keystone predation, trophic cascading and habitat facilitation. Direct negative effects were stronger than indirect positive effect, because grazing leads in almost all studies to a decrease in algal biomass. We found positive effects of grazing on algal nutrient content, biomass-specific productivity and evenness. We found negative overall effects on species richness and area-specific productivity. Moreover, spatial heterogeneity was on average increased by grazing. The magnitudes of direct and indirect effects were often correlated

Description: A three-dimensional fully coupled high resolution atmosphere-ocean model for the BALTEX (Baltic Sea Experiment) region has been developed from two independent models, the atmospheric regional model REMO and the Kiel Baltic Sea model. The coupled model was set up in the framework of the BALTEX program to contribute to one of its major objectives, the investigation and quantification of the energy and water cycle in the Baltic Sea and its catchment area. As a first step towards the fully coupled system, sensitivity studies with different forcings for its uncoupled components, the atmosphere and ocean models. were performed. These sensitivity studies demonstrated that both models are able to produce rea onable results which in turn can act as forcing for the respective other model. In the first simulation of the fu lly coupled system the modeled sea surface temperatures (SST) agree well with satellite observations. Thus they are at least as good as the previously used SSTs from operational analyses and in some cases even better. The detailed evaluation of the coupled model results reveals that often the coupling effects are superimposed by advective influences and that only under specific conditions the atmospheric variables show a remarkable response to different fluxes. The atmosphere-ocean model is coupled directly via the corresponding fluxes across the interface between atmosphere and ocean. For the here presented simulation no flux corrections were necessary. Thus a consistent model system has been developed which can be utilized for further studies of the energy and water cycle in the BALTEX area.

Description: The best place to seek evidence of the style of past magma flow through a conduit is in the country rock. Heat flow has been studied in country rock adjacent to two Tertiary dolerite sills intruding the Caledonian schists and quartzites, on the Isle of Mull, Scotland. Radiogenic 40Ar loss within mica grains in the thermal aureoles of the intrusions has been measured at high spatial resolution using the Ultra-Violet Laser Ablation Micro-Probe, to discriminate between a history of prolonged magma flow, a history of conductive cooling following laminar flow, and instantaneous emplacement of the intrusions. The 40Ar/39Ar mica data and thermal modeling suggest that a prolonged period of magma flow of 3–5 months resulted in extensive argon loss from the micas, country rock melting, and mineral breakdown adjacent to a 6-m sill. These features were absent from the wall rocks of a smaller 2.7-m-thick sill, which exhibited even less argon loss than might have been predicted for an instantaneous intrusion. If the heat loss from the 6-m sill observed in one locality had been repeated along its length, it would have formed an important magma conduit to the Mull volcano, but dolerite is not a common flow composition on Mull. If on the other hand, the heat loss from the sill varies along strike, it constitutes strong evidence for channelling and heterogeneous flow within the sill.

Description: The understanding of the tectonic processes shaping the Pacific margin off Costa Rica has undergone a dramatic evolution during the past 25 years. The margin, initially interpreted to be built by accretion of sediment from the ocean plate, is now interpreted as made of ophiolitic rocks that are exposed onshore, with no net accretion currently active. New seismic images indicate that upper plate tectonic erosion might be the dominant process. Erosion is accomplished in some cases through transport of large bodies from upper to lower plate by plate boundary readjustment. Subduction of seamounts locally accelerates tectonic erosion.

Description: In the eastern Karawanken Mountains, the siliciclastic sedimentary succession of the Hochwipfel Formation was deposited within a narrow marginal basin of the western Paleotethys. Variations of detrital sandstone modes define four petrofacies types, and allow the succession to be stratigraphically divided into Lower and Upper Hochwipfel Formation. Petrographical and geochemical provenance analysis indicate that the basal quartz-rich sandstones derived mainly from the Intraalpine Terrane in the north and the passive Gondwana margin in the south. In the sediments of the Upper Hochwipfel Formation, an increase of (meta)sedimentary as well as of magmatic lithoclasts is discernible indicating a convergent tectonic situation and increased sediment supply derived from a magmatic arc. Zusammenfassung: Die klastische Sedimentabfolge der karhonen HochwipfelFormation der Ostkarawanken wurde in einem schmalen Randbecken der westlichen Paläotethys abgelagert. Auf Grund der Modalzusammensetzung der Sandsteine lassen sich vier Petrofaziestypen unterscheiden, und die sedimentäre Abfolge in eine Untere und eine Obere Hochwipfel-Formation gliedern. Petrographische und geochemische Provenienz-Indikatoren deuten darauf hin, dass die basalen quarzreichen Sandsteine der unteren Hochwipfel-Formation überwiegend von dem nördlich gelegenen Intraalpinen Terran bzw. dem südlich gelegenen passiven Kontinentalrand Gondwanas stammen. In den Sedimenten der oberen Hochwipfel-Formation ist eine Zunahme von (meta)sedimentären Lithoklasten sowie magmatischen Gesteinsbruchstücken zu beobachten. Dies zeigt den Übergang zu einer konvergenten tektonischen Situation und den verstärkten Sedimenteintrag aus einem magmatischen Bogen an.

Description: We conducted a seismic refraction experiment across Flemish Cap and into the deep basin east of Newfoundland, Canada, and developed a velocity model for the crust and mantle from forward and inverse modeling of data from 25 ocean bottom seismometers and dense air gun shots. The continental crust at Flemish Cap is 30 km thick and is divided into three layers with P wave velocities of 6.0–6.7 km/s. Across the southeast Flemish Cap margin, the continental crust thins over a 90-km-wide zone to only 1.2 km. The ocean-continent boundary is near the base of Flemish Cap and is marked by a fault between thinned continental crust and 3-km-thick crust with velocities of 4.7–7.0 km/s interpreted as crust from magma-starved oceanic accretion. This thin crust continues seaward for 55 km and thins locally to ~1.5 km. Below a sediment cover (1.9–3.1 km/s), oceanic layer 2 (4.7–4.9 km/s) is ~1.5 km thick, while layer 3 (6.9 km/s) seems to disappear in the thinnest segment of the oceanic crust. At the seawardmost end of the line the crust thickens to ~6 km. Mantle with velocities of 7.6–8.0 km/s underlies both the thin continental and thin oceanic crust in an 80-km-wide zone. A gradual downward increase to normal mantle velocities is interpreted to reflect decreasing degree of serpentinization with depth. Normal mantle velocities of 8.0 km/s are observed ~6 km below basement. There are major differences compared to the conjugate Galicia Bank margin, which has a wide zone of extended continental crust, more faulting, and prominent detachment faults. Crust formed by seafloor spreading appears symmetric, however, with 30-km-wide zones of oceanic crust accreted on both margins beginning about 4.5 m.y. before formation of magnetic anomaly M0 (~118 Ma).