Calcareous nannofossil biostratigraphy of ODP Leg 108 sediments

• Main Author: Manivit, Helene
• Format: Other/Unknown Material
• Language: English
• Published: PANGAEA 1989
• Subjects: 108-657A; 108-658A; 108-659A; 108-660A; 108-661A; 108-662A; 108-663A; 108-664A; 108-665A; 108-666A; 108-667A; 108-668A; Canarias Sea; DRILL; Drilling/drill rig; Joides Resolution; Leg108; North Atlantic Ocean; Ocean Drilling Program; ODP; South Atlantic Ocean; North Atlantic
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.746289; https://doi.org/10.1594/PANGAEA.746289

Calcareous nannofossils were examined from the 400 cores recovered at 12 sites during Ocean Drilling Program Leg 108 in the eastern equatorial Atlantic Ocean and along the northwest African margin, representing a transect spanning 24° of latitude. Thirty calcareous nannofossil biohorizons were recognized in the Neogene and Quaternary sequences; only Site 661, located in water depths of 3500 m, contains a fossiliferous record older than the Oligocene. At Site 661, a 200-m-thick sequence of Upper Cretaceous sediments yielded Maestrichtian and uppermost Campanian nannofossils, yet a continuous Cretaceous/Tertiary boundary was not recovered. Widespread sediment slumps and turbidites deposited at many sites interrupted the pelagic sedimentation. A careful study of calcareous nannofossil and foraminifer assemblages correlated to paleomagnetic records suggests that "slumped" units at most sites were added as extra sediments to rapidly deposited pelagic sediments, with minor disturbance of the surrounding layers. Nannofossils are generally common to abundant and moderately preserved at all sites except for those located in two upwelling areas, where placoliths are etched and discoasters overgrown. Typical low-latitudinal zonal markers were used during this study, yet some of them were considered to be of little biostratigraphic value because of their inconsistent stratigraphic ranges and low abundances. This is especially apparent for the intervals representing the Miocene/Pliocene and Oligocene/Miocene boundaries. Characteristic nannofossils of cool-water conditions and low discoaster abundances occur at the coastal African upwelling and along the south equatorial divergence sites, signifying a stronger advection of cold waters toward the equator within the Canary and Benguela eastern boundary currents.