Abundance of planktonic foraminifera from IODP Hole 339-U1386C

The base of the Faro contouritic drift (IODP Site U1386) on the northern margin of the Gulf of Cádiz (Algarve margin) is characterized by two sequences of frequent gravity deposits with different ages and compositions. Among these gravity deposits, several relatively thick debrites (up to 12 m) have...

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Bibliographic Details
Main Authors: Ducassou, Emmanuelle, Fournier, L A, Sierro, Francisco Javier, Alvarez Zarikian, Carlos A, Lofi, Johanna, Flores, José-Abel, Roque, C
Format: Dataset
Language:English
Published: PANGAEA 2017
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.870711
https://doi.org/10.1594/PANGAEA.870711