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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Published in:ARCTIC
Main Authors: Schafer, Charles T., Cole, Flona E.
Format: Article in Journal/Newspaper
Language:English
Published: The Arctic Institute of North America 1986
Subjects:
Online Access:https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65131
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spelling 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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