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...
Main Authors: | , |
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Format: | Other/Unknown Material |
Language: | English |
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PANGAEA
2019
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.899978 https://doi.org/10.1594/PANGAEA.899978 |