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  • 1
    Keywords: Isotopendatierung ; Herkunftsnachweis ; Forstdiebstahl ; Genanalyse
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (101 Seiten, 5,03 MB) , Illustrationen, Diagramme, Karten
    Language: English
    Note: This porject is the result of the cooperation with: DBU Deutsche Bundesstiftung Umwelt ; WWF
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    European food research and technology 198 (1994), S. 223-229 
    ISSN: 1438-2385
    Source: Springer Online Journal Archives 1860-2000
    Topics: Process Engineering, Biotechnology, Nutrition Technology
    Description / Table of Contents: Zusammenfassung Das Verhältnis der stabilen Isotopen18O/16O wurde als Abweichung von einem Standard (Delta-Wert in Promille; Standard SMOW) mittels SIRA an insgesamt 359 Weinproben aus Tunesien, Portugal, Griechenland, Italien, Spanien und Ungarn bestimmt. Das ermittelte Verhältnis wird primär von der geographischen Breite des Anbaugebietes beeinflußt. Der Einfluß des Jahrgangs und des Kleinklimas bestimmter Anbauzonen nehmen vom Süden nach Norden zu. Die Ergebnisse einzelner, klimatisch einheitlicher Zonen werden zusammengefaßt. Sie sollen als vorläufige Beurteilungsgrundlage dienen, eventuelle Wasserzusätze oder falsche Angaben zur Herkunft von Weinen zu erkennen. Weiterhin werden die Delta-Werte von Grundwasser unterschiedlichster Herkunft angegeben. Sie liegen ausschließlich im negativen Bereich. Es wird aufgezeigt, wie sich anhand der Delta-Werte authentischer Weine und des Grundwassers Wasserzusätze erkennen und quantitativ abschätzen lassen. Einzelne Beispiele für Weinfälschungen aus der Praxis werden vorgestellt. Die Voraussetzungen für die routinemäßige Anwendung des18O/16O-Verhältnisses werden diskutiert.
    Notes: Abstract The relation of the stabile isotopes18O/16O was determined as deviation from an internationally accepted standard (Delta-value in per mil.; standard SMOW) with SIRA in 359 wines of Tunis, Portugal, Greece, Italy, Spain and Hungary. The determined relation is primary influenced by the geografical latitude of the wine region. The influence of the year and the climatic effect of certain areas increases from the south to the north. The results of individual climatical homogeneous areas are combined. They can serve as provisional base of knowledge in order to indicate the addition of water and false declarations of the origin of wines. Furthermore, information is given about the Delta-values of the ground-water of different regions, which are completely negative. Examples were given how to quantify the addition of water by using the Delta-values of authentic wines and ground-water. Some examples for falsification of wines are described. What ist further needed for using the18O/16O-ratio in the routine analysis of wines is discussed.
    Type of Medium: Electronic Resource
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  • 3
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    PANGAEA
    In:  Supplement to: Sahling, Heiko; Galkin, Sergey V; Salyuk, Anatoly; Greinert, Jens; Foerstel, Hilmar; Piepenburg, Dieter; Suess, Erwin (2003): Depth-related structure and ecological significance of cold-seep communities - A case study from the Sea of Okhotsk. Deep Sea Research Part I: Oceanographic Research Papers, 50(12), 1391-1409, https://doi.org/10.1016/j.dsr.2003.08.004
    Publication Date: 2023-06-27
    Description: We discovered and investigated several cold-seep sites in four depth zones of the Sea of Okhotsk off Northeast Sakhalin: outer shelf (160–250 m), upper slope (250–450 m), intermediate slope (450–800 m), and Derugin Basin (1450–1600 m). Active seepage of free methane or methane-rich fluids was detected in each zone. However, seabed photography and sampling revealed that the number of chemoautotrophic species decreases dramatically with decreasing water depth. At greatest depths in the Derugin Basin, the seeps were inhabited by bacterial mats and bivalves of the families Vesicomyidae (Calyptogena aff. pacifica, C. rectimargo, Archivesica sp.), Solemyidae (Acharax sp.) and Thyasiridae (Conchocele bisecta). In addition, pogonophoran tubeworms of the family Sclerolinidae were found in barite edifices. At the shallowest sites, on the shelf at 160 m, the seeps lack chemoautotrophic macrofauna; their locations were indicated only by the patchy occurrence of bacterial mats. Typical seep-endemic metazoans with chemosynthetic symbionts were confined to seep sites at depths below 370 m. A comparative analysis of the structure of seep and background communities suggests that differences in predation pressure may be an important determinant of this pattern. The abundance of predators such as carnivorous brachyurans and asteroids, which can invade seeps from adjacent habitats and efficiently prey on sessile seep bivalves, decreased very pronouncedly with depth. We conclude from the obvious correlation with the conspicuous pattern in the distribution of seep assemblages that, on the shelf and at the upper slope, predator pressure may be high enough to effectively impede any successful settlement of viable populations of seep-endemic metazoans. However, there was also evidence that other depth-related factors, such as bottom-water current, sedimentary regimes, oxygen concentrations and the supply of suitable settling substrates, may additionally regulate the distribution of seep fauna in the area. As a consequence of the pronounced pattern in the distribution of seep communities, their ecological significance as food sources of surrounding background fauna increased with water depth. Isotopic analyses suggest that in the Derugin Basin seep colonists feed on chemoautotrophic seep organisms, either directly or by preying on metazoans with chemosynthetic symbionts. In contrast, seep organisms apparently do not contribute to the nutrition of the adjacent background fauna on the shelf and at the slope. In this area, elevated epifaunal abundances at seep sites were caused primarily by the availability of suitable settling substrates rather than by an enrichment of food supply.
    Keywords: Akademik M.A. Lavrentiev; Area/locality; Dredge; DRG; Event label; GE99/KOMEX_VI; GE99-25-1; GE99-28-1; KOMEX; KOMEX I; Kurile-Okhotsk Sea Marine Experiment; LV28; LV28-16-2; LV28-30-2; LV28-30-3; LV28-30-4; LV28-30-5; LV28-36-1; LV28-38-1; LV28-47-1; Marshal Gelovany; Mass spectrometry; Material; MUC; MultiCorer; Obzhirov flare; Sea of Okhotsk; Species; Taxon/taxa; TRAWL; Trawl net; δ13C, organic carbon; δ15N, gas
    Type: Dataset
    Format: text/tab-separated-values, 264 data points
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