Reconnaissance Survey of Benthonic Foraminifera from Baffin Island Fiord Environments
Benthonic foraminiferal assemblages in 63 grab samples collected in Baffin Island fiord basin environments (67-800 m) are dominated by arenaceous species such as Textularia earlandi and Spiroplectammina biformis. These forms reflect the influence of cold (<=0.0 degrees C) arctic water conditions....
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The Arctic Institute of North America
1986
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ftunivcalgaryojs:oai:journalhosting.ucalgary.ca:article/65131 2023-05-15T14:19:15+02:00 Reconnaissance Survey of Benthonic Foraminifera from Baffin Island Fiord Environments Schafer, Charles T. Cole, Flona E. 1986-01-01 application/pdf https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65131 eng eng The Arctic Institute of North America https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65131/49045 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65131 ARCTIC; Vol. 39 No. 3 (1986): September: 195–284; 232-239 1923-1245 0004-0843 Animal distribution Bathymetry Benthos Bottom sediments Fjords Foraminifera Water masses Baffin Island waters Nunavut info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion research-article 1986 ftunivcalgaryojs 2022-03-22T21:22:12Z Benthonic foraminiferal assemblages in 63 grab samples collected in Baffin Island fiord basin environments (67-800 m) are dominated by arenaceous species such as Textularia earlandi and Spiroplectammina biformis. These forms reflect the influence of cold (<=0.0 degrees C) arctic water conditions. Incursions of comparatively warm and saline Atlantic bottom water is marked in the deepest part of some fiord basins by the distribution of several calcareous species such as Melonis zaandamae and Nonionella atlantica. The highest living calcareous species population densities are associated primarily with fiord sills and with inner shelf environments near the mouths of fiords. Conversely, the patchy distribution and low percentages of many calcareous species found in basin sediments suggest passive transport of perhaps both living specimens and empty tests from shallow nearshore (endemic) environments or their occupation of deep basin transitional environments that mark the change from Atlantic to arctic water masses.Key words: foraminifera, Baffin Island, Fiords, arenaceous foraminifera, calcareous foraminifera Mots clés: foraminifères, île de Baffin, fjords, foraminifères arénacés, foraminifères calcaires Article in Journal/Newspaper Arctic Arctic Baffin Island Baffin Foraminifera* Île de Baffin Nunavut University of Calgary Journal Hosting Arctic Baffin Island Île de Baffin ENVELOPE(-74.998,-74.998,68.001,68.001) Nunavut ARCTIC 39 3 |
institution |
Open Polar |
collection |
University of Calgary Journal Hosting |
op_collection_id |
ftunivcalgaryojs |
language |
English |
topic |
Animal distribution Bathymetry Benthos Bottom sediments Fjords Foraminifera Water masses Baffin Island waters Nunavut |
spellingShingle |
Animal distribution Bathymetry Benthos Bottom sediments Fjords Foraminifera Water masses Baffin Island waters Nunavut Schafer, Charles T. Cole, Flona E. Reconnaissance Survey of Benthonic Foraminifera from Baffin Island Fiord Environments |
topic_facet |
Animal distribution Bathymetry Benthos Bottom sediments Fjords Foraminifera Water masses Baffin Island waters Nunavut |
description |
Benthonic foraminiferal assemblages in 63 grab samples collected in Baffin Island fiord basin environments (67-800 m) are dominated by arenaceous species such as Textularia earlandi and Spiroplectammina biformis. These forms reflect the influence of cold (<=0.0 degrees C) arctic water conditions. Incursions of comparatively warm and saline Atlantic bottom water is marked in the deepest part of some fiord basins by the distribution of several calcareous species such as Melonis zaandamae and Nonionella atlantica. The highest living calcareous species population densities are associated primarily with fiord sills and with inner shelf environments near the mouths of fiords. Conversely, the patchy distribution and low percentages of many calcareous species found in basin sediments suggest passive transport of perhaps both living specimens and empty tests from shallow nearshore (endemic) environments or their occupation of deep basin transitional environments that mark the change from Atlantic to arctic water masses.Key words: foraminifera, Baffin Island, Fiords, arenaceous foraminifera, calcareous foraminifera Mots clés: foraminifères, île de Baffin, fjords, foraminifères arénacés, foraminifères calcaires |
format |
Article in Journal/Newspaper |
author |
Schafer, Charles T. Cole, Flona E. |
author_facet |
Schafer, Charles T. Cole, Flona E. |
author_sort |
Schafer, Charles T. |
title |
Reconnaissance Survey of Benthonic Foraminifera from Baffin Island Fiord Environments |
title_short |
Reconnaissance Survey of Benthonic Foraminifera from Baffin Island Fiord Environments |
title_full |
Reconnaissance Survey of Benthonic Foraminifera from Baffin Island Fiord Environments |
title_fullStr |
Reconnaissance Survey of Benthonic Foraminifera from Baffin Island Fiord Environments |
title_full_unstemmed |
Reconnaissance Survey of Benthonic Foraminifera from Baffin Island Fiord Environments |
title_sort |
reconnaissance survey of benthonic foraminifera from baffin island fiord environments |
publisher |
The Arctic Institute of North America |
publishDate |
1986 |
url |
https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65131 |
long_lat |
ENVELOPE(-74.998,-74.998,68.001,68.001) |
geographic |
Arctic Baffin Island Île de Baffin Nunavut |
geographic_facet |
Arctic Baffin Island Île de Baffin Nunavut |
genre |
Arctic Arctic Baffin Island Baffin Foraminifera* Île de Baffin Nunavut |
genre_facet |
Arctic Arctic Baffin Island Baffin Foraminifera* Île de Baffin Nunavut |
op_source |
ARCTIC; Vol. 39 No. 3 (1986): September: 195–284; 232-239 1923-1245 0004-0843 |
op_relation |
https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65131/49045 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65131 |
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ARCTIC |
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39 |
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3 |
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