Post-glacial paleo-oceanography of Emerald Basin, Scotian Shelf
Two sediment cores taken from Emerald Basin, Nova Scotia are discussed in terms of organic geochemistry and foraminifera. The analytical results are used to infer changes in the marine environment in Emerald Basin during the last 15 000 y.The fine sediments contained relatively low amounts of organi...
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1976
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Online Access: | http://dx.doi.org/10.1139/e76-128 http://www.nrcresearchpress.com/doi/pdf/10.1139/e76-128 |
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crcansciencepubl:10.1139/e76-128 2023-12-17T10:48:58+01:00 Post-glacial paleo-oceanography of Emerald Basin, Scotian Shelf Vilks, Gustavs Rashid, M. A. 1976 http://dx.doi.org/10.1139/e76-128 http://www.nrcresearchpress.com/doi/pdf/10.1139/e76-128 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 13, issue 9, page 1256-1267 ISSN 0008-4077 1480-3313 General Earth and Planetary Sciences journal-article 1976 crcansciencepubl https://doi.org/10.1139/e76-128 2023-11-19T13:39:06Z Two sediment cores taken from Emerald Basin, Nova Scotia are discussed in terms of organic geochemistry and foraminifera. The analytical results are used to infer changes in the marine environment in Emerald Basin during the last 15 000 y.The fine sediments contained relatively low amounts of organic carbon, plant pigments, sulphides with respect to total sulphur, and only background values of methane. The data indicate that the bottom of the Basin has been well oxygenated since the Late Wisconsin, including the times of lowest sea level. The foraminiferal assemblages varied from estuarine–nearshore fauna in the older sediments to the outer shelf-normal marine faunas in the surface sediments. Planktonic foraminifera were found in all levels of the cores.The faunal evidence indicates that during the Late Wisconsin sea-level minimum and the period of glacial waning, the bottom salinities of the Basin were in the order of 20‰. Emerald Basin was connected to the ocean via a wide but shallow sill that allowed the exchange of Basin waters with only relatively diluted surface waters of the ocean. Article in Journal/Newspaper Planktonic foraminifera Canadian Science Publishing (via Crossref) Emerald Basin ENVELOPE(162.500,162.500,-54.000,-54.000) Canadian Journal of Earth Sciences 13 9 1256 1267 |
institution |
Open Polar |
collection |
Canadian Science Publishing (via Crossref) |
op_collection_id |
crcansciencepubl |
language |
English |
topic |
General Earth and Planetary Sciences |
spellingShingle |
General Earth and Planetary Sciences Vilks, Gustavs Rashid, M. A. Post-glacial paleo-oceanography of Emerald Basin, Scotian Shelf |
topic_facet |
General Earth and Planetary Sciences |
description |
Two sediment cores taken from Emerald Basin, Nova Scotia are discussed in terms of organic geochemistry and foraminifera. The analytical results are used to infer changes in the marine environment in Emerald Basin during the last 15 000 y.The fine sediments contained relatively low amounts of organic carbon, plant pigments, sulphides with respect to total sulphur, and only background values of methane. The data indicate that the bottom of the Basin has been well oxygenated since the Late Wisconsin, including the times of lowest sea level. The foraminiferal assemblages varied from estuarine–nearshore fauna in the older sediments to the outer shelf-normal marine faunas in the surface sediments. Planktonic foraminifera were found in all levels of the cores.The faunal evidence indicates that during the Late Wisconsin sea-level minimum and the period of glacial waning, the bottom salinities of the Basin were in the order of 20‰. Emerald Basin was connected to the ocean via a wide but shallow sill that allowed the exchange of Basin waters with only relatively diluted surface waters of the ocean. |
format |
Article in Journal/Newspaper |
author |
Vilks, Gustavs Rashid, M. A. |
author_facet |
Vilks, Gustavs Rashid, M. A. |
author_sort |
Vilks, Gustavs |
title |
Post-glacial paleo-oceanography of Emerald Basin, Scotian Shelf |
title_short |
Post-glacial paleo-oceanography of Emerald Basin, Scotian Shelf |
title_full |
Post-glacial paleo-oceanography of Emerald Basin, Scotian Shelf |
title_fullStr |
Post-glacial paleo-oceanography of Emerald Basin, Scotian Shelf |
title_full_unstemmed |
Post-glacial paleo-oceanography of Emerald Basin, Scotian Shelf |
title_sort |
post-glacial paleo-oceanography of emerald basin, scotian shelf |
publisher |
Canadian Science Publishing |
publishDate |
1976 |
url |
http://dx.doi.org/10.1139/e76-128 http://www.nrcresearchpress.com/doi/pdf/10.1139/e76-128 |
long_lat |
ENVELOPE(162.500,162.500,-54.000,-54.000) |
geographic |
Emerald Basin |
geographic_facet |
Emerald Basin |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_source |
Canadian Journal of Earth Sciences volume 13, issue 9, page 1256-1267 ISSN 0008-4077 1480-3313 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/e76-128 |
container_title |
Canadian Journal of Earth Sciences |
container_volume |
13 |
container_issue |
9 |
container_start_page |
1256 |
op_container_end_page |
1267 |
_version_ |
1785573283061563392 |