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  • 1975-1979  (2)
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  • 1
    Publication Date: 2022-05-18
    Description: Ein in situ-Meßsystem für Untersuchungen zum Stoff- und Energiefluß in isolierten benthischen Flachwassergemeinschaften wird beschrieben. Die Messung des Gaswechsels sowie anorganischer und organischer gelöster Substanzen erfolgt in geschlossenen (Säcke) oder offenen (Durchflußsystem) Meßeinrichtungen, die unter Verwendung von flexiblen Plastikfolien konstruiert wurden, um möglichst ungestörte Turbulenzverhältnisse zu gewährleisten. Die Anwendung der Meßeinrichtungen wird anhand von Meßbeispielen erläutert. A measuring system is described for in situ investigations on the flow of energy and matter in isolated benthos communities in shallow waters. Measurements of gas exchange and inorganic as well as organic dissolved matter are carried out either in closed (bags) or open (flow through) devices. Flexible plastic film is used for the construction of the devices in order to obtain favourable turbulence conditions in the systems. Practical application is illustrated by examples of measurements.
    Type: Article , NonPeerReviewed
    Format: text
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  • 2
    Publication Date: 2022-05-18
    Description: A coralline alga from the Baltic (Belt Sea, Samsö) belonging to the genus Phymatolithon has been investigated. The mineral skeleton consists of magnesium calcite and shows the following composition (expressed in percent of the dry weight): 94-96% skeletal carbonates, 4-6% organic matter, 32.1-33.4% Ca, 3.3-3.5% Mg and 0.15-0.17% Sr. MgC03 determined by the peak shift method (X-ray diffraction) is in the region of 10-11 mol % . The kinetics of 45Ca uptake consist of a fast step and a low step. The fast step is due to equilibration of isotope with the soft tissues and spaces between cells. The slow step is attributed to net deposition of calcium in the skeleton. From the rate constant of the slow step calcium net deposition was found to be 5.6 1 μg Ca/g dry weight/h or 14 μg CaC03/g dry weight/h. Pulse chase experiments show that the calcification is the resultant of calcium exchange between the alga and the seawater. Light-dark calcification ratios are in the range of 1.1-1.3. The O2 production amounts to 0.04 mg 02/g dry weight/h at an irradiance of 0.085 KW/m2. When expressed per unit weight of total organic matter, this assimilation rate would fall into the range commonly found for other noncalcifying Rhodophyta. The results form the basis for further work on calcification mechanism and CaC03 production in coralline algae.
    Type: Article , NonPeerReviewed
    Format: text
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