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...
Main Authors: | , , , , , |
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Format: | Other/Unknown Material |
Language: | English |
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PANGAEA
1997
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.734360 https://doi.org/10.1594/PANGAEA.734360 |