ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • Atlantic Ocean; East Atlantic; FGGE-Equator 79 - First GARP Global Experiment; GIK/IfG; GIK12309-3; GIK12328-5; GIK12329-6; GIK12347-2; GIK12392-1; GIK13519-1; GIK15669-1; GIK15672-1; Gravity corer (Kiel type); Institute for Geosciences, Christian Albrechts University, Kiel; KAL; Kasten corer; M12392-1; M25; M51; M53; M53_169; M53_172; Meteor (1964); off West Africa; SL; SPC; Sphincter corer  (1)
  • 1985-1989  (1)
Collection
Keywords
Publisher
Years
  • 1985-1989  (1)
Year
  • 1
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Lutze, Gerhard F; Pflaumann, Uwe; Weinholz, Peter (1986): Jungquartäre Fluktuationen der benthischen Foraminiferenfaunen in Tiefsee-Sedimenten vor NW-Afrika - Eine Reaktion auf Produktivitätsänderungen im Oberflächenwasser. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe C Geologie und Geophysik, Gebrüder Bornträger, Berlin, Stuttgart, C40, 163-180
    Publication Date: 2024-02-03
    Description: A statistical analysis ol 15 deep sea cores in the eastern North Atlantic off NW Africa revealed the typical fluctuation pattern of distinct species proups as has been described from various parts of the world ocean. Only the "WBF-group" appears to be correlated with global climatic changes, i.e. warmer periods as the Eemian and the Atlanticum. A partly antagonistic "High Productivity group" (HPR-group) is in general not linked with global changes but times of increased fertility in the surface water and the resulting flux of organic matter reaching the bottom. The groups were extracted from cluster analysis of more than 150 surface samples (HPR-group) and a factor analysis of selected cores (WBF-group). In contrast to previous studies the observed fluctuations can not be explained by drastic changes in bottom water masses, but by the pulsation of a distinct "High Productivity Patch" in space and time. At present, this patch is located below the well known upwelling area between 22° and 12° northern latitude. It shifted to the north (up to 27 °N) during the latest glacial period ( 18 ky), indicating an equivalent shift of upwelling productivity caused by advection of nutrient rich upwelling SACW-waters, probably during most of isotopic stages 2 and 3.
    Keywords: Atlantic Ocean; East Atlantic; FGGE-Equator 79 - First GARP Global Experiment; GIK/IfG; GIK12309-3; GIK12328-5; GIK12329-6; GIK12347-2; GIK12392-1; GIK13519-1; GIK15669-1; GIK15672-1; Gravity corer (Kiel type); Institute for Geosciences, Christian Albrechts University, Kiel; KAL; Kasten corer; M12392-1; M25; M51; M53; M53_169; M53_172; Meteor (1964); off West Africa; SL; SPC; Sphincter corer
    Type: Dataset
    Format: application/zip, 8 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...