Palaeoceanographic changes off North Iceland during the Holocene and Late Glacial: foraminifera, stable isotopes, diatoms and ice rafted debris

The north Icelandic shelf is partly distinguished by the Tjörnes Fracture Zone featuring numerous active basins in a mud-dominated shelf environment. Late Glacial and Holocene high-resolution sedimentary records from this area have been studied with tephrochronology as the main tool for correlation...

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Bibliographic Details
Main Authors: Knudsen, Karen Luise, Eiriksson, Jón
Format: Other/Unknown Material
Language:English
Published: PANGAEA 2019
Subjects:
GC
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.899978
https://doi.org/10.1594/PANGAEA.899978