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...
Main Authors: | , , , , , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2017
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.870711 https://doi.org/10.1594/PANGAEA.870711 |