Reconstruction of Atlantic water variability during the Holocene in the western Barents Sea
The gravity core JM09-KA11-GC from 345 m water depth on the western Barents Sea margin was investigated for down-core distribution patterns of benthic Foraminifera, stable isotopes, and sedimentological parameters in order to reconstruct the flow of Atlantic water during the Holocene. The core site...
| Autori principali: | , , |
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| Natura: | Articolo |
| Lingua: | English |
| Pubblicazione: |
Copernicus Publications
2014-01-01
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| Serie: | Climate of the Past |
| Accesso online: | http://www.clim-past.net/10/51/2014/cp-10-51-2014.pdf |