Planktonic foraminiferal faunas and stable isotope ratios of sediments from the Benguela Upwelling System

Two sediment cores retrieved from the continental slope in the Benguela Upwelling System, GeoB 1706 (19°33.7'S 11°10.5'E) and GeoB 1711 (23°18.9'S, 12°22.6'E), reveal striking variations in planktonic foraminiferal abundances during the last 160,000 years. These fluctuations are...

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Bibliographic Details
Main Authors: Little, Mark G, Schneider, Ralph R, Kroon, Dick, Price, B, Bickert, Torsten, Wefer, Gerold
Format: Other/Unknown Material
Language:English
Published: PANGAEA 1997
Subjects:
GKG
SL
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.734360
https://doi.org/10.1594/PANGAEA.734360