Late Glacial-Postglacial Foraminiferal Boundary in Sediments of Eastern Canada, Denmark and Norway
Sediments in cores collected from the Scotian and Labrador shelves contain a faunal discontinuity where older benthic foraminiferal assemblages dominated by Elphidium excavatum f. clavata change to more diverse present day continental shelf assemblages. A similar change is found in Late Quaternary b...
Main Author: | |
---|---|
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Geological Association of Canada
1981
|
Subjects: | |
Online Access: | https://journals.lib.unb.ca/index.php/GC/article/view/3246 |
id |
ftuninewbrunojs:oai:ojs.journals.lib.unb.ca:article/3246 |
---|---|
record_format |
openpolar |
spelling |
ftuninewbrunojs:oai:ojs.journals.lib.unb.ca:article/3246 2023-05-15T17:33:02+02:00 Late Glacial-Postglacial Foraminiferal Boundary in Sediments of Eastern Canada, Denmark and Norway Vilks, Gustavs 1981-06-06 application/pdf https://journals.lib.unb.ca/index.php/GC/article/view/3246 eng eng Geological Association of Canada https://journals.lib.unb.ca/index.php/GC/article/view/3246/3763 https://journals.lib.unb.ca/index.php/GC/article/view/3246 Copyright (c) 2015 Geoscience Canada Geoscience Canada; Volume 8, Number 2 (1981) 1911-4850 0315-0941 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion research-article 1981 ftuninewbrunojs 2022-07-11T11:47:19Z Sediments in cores collected from the Scotian and Labrador shelves contain a faunal discontinuity where older benthic foraminiferal assemblages dominated by Elphidium excavatum f. clavata change to more diverse present day continental shelf assemblages. A similar change is found in Late Quaternary borings in Denmark (Jutland) and in the Oslofjord area of Norway. The 14C age of the faunal break varies from 10,000 years B.P. in the European sediments to 13,000 years B.P.on the Scotian Shelf and 15,000 years B.P. on the Labrador Shelf. The present day oceanographic setting along the coasts of Norway, Denmark and eastern Canada was established when the glacial ice retreated inland. The dominance of E. excavatum f. clavata in the older sediments is related to diluted and cold coastal waters during the time when continental ice was ablating on the inner shelf. The disappearance of E excavatum f. clavata therefore can be used to estimate the Late Glacial-Postglacial boundary in the Canadian and Scandinavian North Atlantic continental shelf sediments. This paper reviews the evidence of the faunal break to alert geologists in its possible use. Article in Journal/Newspaper North Atlantic University of New Brunswick: Centre for Digital Scholarship Journals Canada Labrador Shelf ENVELOPE(-58.000,-58.000,56.000,56.000) Norway |
institution |
Open Polar |
collection |
University of New Brunswick: Centre for Digital Scholarship Journals |
op_collection_id |
ftuninewbrunojs |
language |
English |
description |
Sediments in cores collected from the Scotian and Labrador shelves contain a faunal discontinuity where older benthic foraminiferal assemblages dominated by Elphidium excavatum f. clavata change to more diverse present day continental shelf assemblages. A similar change is found in Late Quaternary borings in Denmark (Jutland) and in the Oslofjord area of Norway. The 14C age of the faunal break varies from 10,000 years B.P. in the European sediments to 13,000 years B.P.on the Scotian Shelf and 15,000 years B.P. on the Labrador Shelf. The present day oceanographic setting along the coasts of Norway, Denmark and eastern Canada was established when the glacial ice retreated inland. The dominance of E. excavatum f. clavata in the older sediments is related to diluted and cold coastal waters during the time when continental ice was ablating on the inner shelf. The disappearance of E excavatum f. clavata therefore can be used to estimate the Late Glacial-Postglacial boundary in the Canadian and Scandinavian North Atlantic continental shelf sediments. This paper reviews the evidence of the faunal break to alert geologists in its possible use. |
format |
Article in Journal/Newspaper |
author |
Vilks, Gustavs |
spellingShingle |
Vilks, Gustavs Late Glacial-Postglacial Foraminiferal Boundary in Sediments of Eastern Canada, Denmark and Norway |
author_facet |
Vilks, Gustavs |
author_sort |
Vilks, Gustavs |
title |
Late Glacial-Postglacial Foraminiferal Boundary in Sediments of Eastern Canada, Denmark and Norway |
title_short |
Late Glacial-Postglacial Foraminiferal Boundary in Sediments of Eastern Canada, Denmark and Norway |
title_full |
Late Glacial-Postglacial Foraminiferal Boundary in Sediments of Eastern Canada, Denmark and Norway |
title_fullStr |
Late Glacial-Postglacial Foraminiferal Boundary in Sediments of Eastern Canada, Denmark and Norway |
title_full_unstemmed |
Late Glacial-Postglacial Foraminiferal Boundary in Sediments of Eastern Canada, Denmark and Norway |
title_sort |
late glacial-postglacial foraminiferal boundary in sediments of eastern canada, denmark and norway |
publisher |
Geological Association of Canada |
publishDate |
1981 |
url |
https://journals.lib.unb.ca/index.php/GC/article/view/3246 |
long_lat |
ENVELOPE(-58.000,-58.000,56.000,56.000) |
geographic |
Canada Labrador Shelf Norway |
geographic_facet |
Canada Labrador Shelf Norway |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Geoscience Canada; Volume 8, Number 2 (1981) 1911-4850 0315-0941 |
op_relation |
https://journals.lib.unb.ca/index.php/GC/article/view/3246/3763 https://journals.lib.unb.ca/index.php/GC/article/view/3246 |
op_rights |
Copyright (c) 2015 Geoscience Canada |
_version_ |
1766131392577536000 |