ALBERT

Description: Fish stocks have made surprising comebacks in the North and Baltic seas. But much remains to be done. Beginning in January, new EU laws will impose more sustainable practices with stricter quotas and by-catch rules.

Description: Micro-Raman spectroscopy has been used on adult bivalve shells to investigate organic and inorganic shell components but has not yet been applied to bivalve larvae. It is known that the organic matrix of larval shells contains pigments, but less is known about the presence or source of these molecules in larvae. We investigated Raman spectra of seven species of bivalve larvae to assess the types of pigments present in shells of each species and how the ratio of inorganic : organic material changes in a dorso-ventral direction. In laboratory experiments, we reared larvae of three clam species in waters containing different organic signatures to determine if larvae incorporated compounds from source waters into their shells. We found differences in spectra and pigments between most species but found less intraspecific differences. A neural network classifier for Raman spectra classified five out of seven species with greater than 85% accuracy. There were slight differences between the amount and type of pigment present along the shell, with the prodissoconch I and shell margin areas being the most variable. Raman spectra of 1-day-old larvae were found to be differentiable when larvae were reared in waters with different organic signatures. With micro-Raman spectroscopy, it may be possible to identify some unknown species in the wild and trace their natal origins, which could enhance identification accuracy of bivalve larvae and ultimately aid management and restoration efforts.

Description: On the Earth, the atmosphere, ocean, and land interact with each other. For example, an atmospheric pressure system directly influences the Sea Surface Heights (SSHs) in a barometric sense; the associated wind transfers momentum from the atmosphere into the ocean, which alters the ocean currents affecting again the SSHs. The integrated effects of all motion components directly influence the angular momentum of the Earth, while the integrated effect of all mass variations alters the Earth’s inertia. Both can excite the Earth Orientation Parameters (EOPs). In this study, we use the Community Earth System Model (CESM) to simulate mass and motion variations within a coupled climate system. The modeled mass and motion variations of all subcomponents are used to compute the total excitation functions, which then are compared to very precise global EOP observations, provided by the International Earth Rotation and Reference Systems Service (IERS). For further reference, the modeled excitation functions of the subcomponents are compared to operational excitations, provided by the German Research Centre for Geosciences (GFZ). This allows an evaluation of the global model behavior and of the subcomponents. Further, regions of particularly high influence on the excitations as well as regions of especially strong dynamical coupling are identified. Four CESM experiments were performed, one reference experiment featuring solely natural variations, while the others separate the influence of (I) a coupled ocean component; (II) the quasi-biennial oscillation (QBO) and (III) anthropogenic forcings, e.g. greenhouse gas (GHG) emissions and ozone depleting substances (ODS). The modeled EOPs are in good agreement with the reference data sets, but reveal an slight overestimation of the modeled atmospheric mass component in the North Pacific for annual to interannual timescales, leading to deviations in the X1 component. Analyzing variations among the CESM experiments reveal (I) the complete absence of interannual subtropical tropospheric jet variability when using a climatological ocean; (II) a significantly increased atmospheric mass variation in the arctic region in the absence of a QBO; and (III) hardly any modeled effect of the global dynamics with respect to anthropogenic forcings. Finally, the North Pacific - a region with particularly strong atmosphere-ocean coupling - is investigated, highlighting wind driven ocean mass variations within the model and GRACE observations. The identified significant wind patterns explain the modeled ocean mass variations and can be directly projected onto ERA-Interim data in order to estimate the independent GRACE observations. The here presented relation between the ERA-Interim winds and the GRACE gravity field observations supporting the following two conclusions: (I) ERA-Interim winds can be used to further refine GRACE observations; (II) GRACE observations contain assimilation worthy information for atmospheric models.

Description: The stratigraphic successions exposed in Wadi El Mizeira have been dated through the analysis of the calcareous nannofossil assemblages. The results of this study indicate that the successions comprise the Santonian-Late Maastrichtian (Sudr Formation), the Paleocene (Esna Formation) and the Early Eocene (Thebes Formation). The following biozones were recognized: Late Santonian, CC16 Zone; Late Santonian/Early Campanian, CC17 Zone; Early Campanian, Aspidolithus parcus Zone (CC18) Zone; Late Maastrichtian, CC25c Zone; Early Paleocene (Late Danian), NP3 Zone and NP4 Zone; Late Paleocene (Thanethian-Selandian), NP5 Zone; Early Eocene, NP9b Zone, NP10a Zone, NP11 Zone, NP12 Zone and NP14 Zone. Several stratigraphic hiatus were recorded in the studied interval including the absence of Cretaceous nannofossil Zones CC19 to CC25b and CC26 as well as the early Paleocene Zones NP1 and NP2 and probably the basal part of Zone NP3, in addition to the absence of the Zones NP6 and NP7/8. These hiatus may be attributed to environmental conditions, structural activity and/or post depositional processes. This work represents the first attempt to evaluate the nannofossil taxa of the Wadi El Mizeira, Northeastern Sinai.

Description: Hemigrapsus sanguineus (Asian Shore Crab) has shown a remarkable ability to colonize rocky intertidal communities along the east coast of the United States since its introduction in the late 1980s and is an important predator of juvenile Mytilus edulis (Blue Mussel) in invaded habitats. In this study, we used two field-caging experiments and the Kaplan-Meier model to assess the impact of predation by Asian Shore Crab on the survival of juvenile Blue Mussels in an intertidal habitat of western Long Island Sound along the Connecticut coastline. Five treatment levels (high-density enclosure, low-density enclosure, exclosure, partial cage, and open plot) were used in the 2007 experiment. The high-density enclosure treatment was omitted in the 2010 experiment since there was no statistically significant difference in the proportion of mussels surviving between low- and high-density crab treatments in 2007. In 2007, we measured a statistically significant difference in mussel mortality between exclosure and crab-enclosure cages, with crabs lowering the median survival time for mussels from 15.4 to 7.6 days. In 2010, we again measured a statistically significant difference in mussel mortality between exclosure and crab-enclosure cages, suggesting a crab effect on mussel survival. In the 2010 experiment, approximately 25% of the mussel mortality was attributable to crab predation, which reduced median survival time for mussels from 12.8 to 5.6 days. The median survival time for mussels exposed to the full complement of factors affecting survival (open plots and partial cages) was only 2–3 days. Our study shows that predation by Asian crabs may account for up to 25% of the Blue Mussel mortality in the intertidal zone at Black Rock Harbor. Further studies focusing on the importance of other biotic and abiotic factors are needed to understand the apparent declines in Blue Mussel populations and the interannual variability in recruitment success in this area.

Description: Benthic foraminifera from surface Sediments of the Ross Sea were studied to determine modern distributions of important assemblages. Factor analysis of the raw data distinguished nine significant factor assemblages which account for 86% of the raw data. These factor assemblages provide a means of understanding modern oceanographic and ecologic conditions because they show the response of this faunal group to different environments. Environmental conditions are in turn controlled by the modern climatic regime of the region. Four benthic assemblages from the relatively shallow (500 to 700 m) eastern Ross Sea Continental shelf are predominantly arenaceous. This may be because the relatively late seasonal breakup of pack ice inhibits productivity in the surface waters and permits a buildup of CO, thus causing the CCD to occur at shallow depths. On the Western part of the Continental shelf, three assemblages are composed primarily of calcareous species even though water depths are often greater there than they are in the east. One of these calcareous assemblages occurs in samples from water depths as great as 755 m in the southwestern part of the region, below the CCD as defined for the Ross Sea by previous workers. We relate this depressed CCD to early seasonal breakup of pack ice in the Western Ross Sea. Within the eastern arenaceous and Western calcareous regions on the Continental shelf, distributions of benthic assemblages are probably related to water depth and other ecologic variables. Two benthic assemblages from the Continental slope north of the Ross Sea also are calcareous. We attribute their distributions to high rates of productivity in the overlying surface waters, where the interface between eastward-flowing Circumpolar Deep Water and Ross Sea water masses is marked by a narrow zone of intense upwelling.

Description: Eine bei vielen küstenmorphologischen und sedimentologischen Untersuchungen interessierende Frage gilt der Sedimentbilanz. Da sie ein Produkt der lokalen topographischen und hydrologi­schen Komponenten ist und (bisher) nicht ohne weiteres vorher­sagbar, sind Messungen und deren Auswertungen für einzelne Gebiete von allgemeinem Interesse. Für die »Anse de Kernic«, eine Lagune im Bereich der sehr großen Gezeiten an der Nordküste der Bretagne (Abb. 1) wurden im Laufe mehrerer Jahre flächenmäßig Höhendaten zu­sammengetragen. Ihre Auswertung und vergleichende Gegen­überstellung werden im folgenden vorgestellt.

Description: Surface sediments of thermokarst lakes along the temperature gradient were sampled in northwestern Siberia. The lakes were distributed through three environmental zones: typical tundra, southern tundra and forest-tundra, which were all situated within the continuous permafrost zone. Our investigation showed that the cladoceran communities in the lakes of the region are represented by diverse, abundant communities as reflected by the taxonomic richness and high diversity indices. The differences in the cladoceran assemblages were related to the limnological and geographical position, vegetation type, climate and water chemistry. The constrained redundancy analysis (RDA) indicated that the TJuly, water depth and both sulphate (SOf ~) and silicium (Si4*) concentrations statistically significant (p 〈 0.05) explained the variance in the cladoceran assemblage.