Late Weichselian deglaciation and early Holocene development of a cold-water coral reef along the Lopphavet shelf (Northern Norway) recorded by benthic foraminifera and ostracoda
Cold-water coral (CWC) settlement in northern Norway is strongly related to the outlet-glaciers of the Fennoscandian Ice-sheet, and dating of known CWC structures show clearly post-glacial ages. Two gravity cores (POS391 559/2,277 cm long and POS391 559/3,282 cm long) were recovered on a CWC reef in...
Main Authors: | , , , , |
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Language: | English |
Published: |
2014
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Subjects: | |
Online Access: | http://doc.rero.ch/record/209395/files/spe_lwd.pdf http://doc.rero.ch/record/209395/files/spe_lwd_sm1.txt http://doc.rero.ch/record/209395/files/spe_lwd_sm2.txt http://doc.rero.ch/record/209395/files/spe_lwd_sm3.txt http://doc.rero.ch/record/209395/files/spe_lwd_sm4.txt |