Pre-Late Wisconsinan Paleoenvironments in Atlantic Canada

Numerous Quaternary organic deposits of various lithologies beneath one or more till units of Wisconsinan age have been discovered in boreholes and exposures in coastal bluffs, quarries and river banks at widespread localities throughout Atlantic Canada. Ongoing palynological and macro-fossil studie...

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Published in:Géographie physique et Quaternaire
Main Authors: Mott, Robert J., Grant, Douglas R.
Format: Text
Language:English
Published: Les Presses de l'Université de Montréal 1985
Subjects:
Online Access:http://id.erudit.org/iderudit/032606ar
https://doi.org/10.7202/032606ar
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spelling fterudit:oai:erudit.org:032606ar 2023-05-15T18:33:39+02:00 Pre-Late Wisconsinan Paleoenvironments in Atlantic Canada Mott, Robert J. Grant, Douglas R. 1985 http://id.erudit.org/iderudit/032606ar https://doi.org/10.7202/032606ar en eng Les Presses de l'Université de Montréal Érudit Géographie physique et Quaternaire vol. 39 no. 3 (1985) http://id.erudit.org/iderudit/032606ar doi:10.7202/032606ar Tous droits réservés © Les Presses de l'Université de Montréal, 1985 text 1985 fterudit https://doi.org/10.7202/032606ar 2022-09-24T23:13:38Z Numerous Quaternary organic deposits of various lithologies beneath one or more till units of Wisconsinan age have been discovered in boreholes and exposures in coastal bluffs, quarries and river banks at widespread localities throughout Atlantic Canada. Ongoing palynological and macro-fossil studies, still in a preliminary stage at many sites, reveal a variety of environments from forests dominated by thermophilous hardwood genera and white pine, to mixed temperate hardwood and conifer forests, to boreal coniferous forests of spruce and balsam fir, and forest tundra and tundra communities characterized by spruce, shrubs and herbs. Lithologie and pollen stratigraphie relationships and radiocarbon, amino acid and Thorium/Uranium dating allow a tentative assignment to the Sangamonian Stage and possibly to Early and Middle Wisconsinan time. Three intervals of organic accumulation are apparent: an early interval, when climate became warmer than the present; a second interval, when climate was similar to the present; and a third interval, with cooler climate. The latter interval is characterized by at least three climatic cycles, each one cooler than the previous cycle. Tentative correlations with the deep-sea oxygen isotope record and continental palynological records are presented. Des dépôts organiques aux lithologies variées, surmontés d'au moins une unité de till wisconsinien, ont été découverts dans des trous de forage, dans des coupes le long des falaises littorales et de talus alluviaux, ainsi que dans des carrières en de nombreux endroits des provinces atlantiques. L'étude des macrofossiles et la palynologie de ces dépôts, encore à l'étape préliminaire dans de nombreux cas, révèlent l'existence de différents environnements : forêts dominées par des essences feuillues thermophiles et par le pin blanc; forêts mixtes à essences décidues tolérantes et de conifères; forêts boréales d'épinettes et de sapins baumiers; communautés de toundra forestière et de toundra caractérisée par les épinettes, les arbustes et ... Text toundra Tundra Érudit.org (Université Montréal) Canada Géographie physique et Quaternaire 39 3 239 254
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description Numerous Quaternary organic deposits of various lithologies beneath one or more till units of Wisconsinan age have been discovered in boreholes and exposures in coastal bluffs, quarries and river banks at widespread localities throughout Atlantic Canada. Ongoing palynological and macro-fossil studies, still in a preliminary stage at many sites, reveal a variety of environments from forests dominated by thermophilous hardwood genera and white pine, to mixed temperate hardwood and conifer forests, to boreal coniferous forests of spruce and balsam fir, and forest tundra and tundra communities characterized by spruce, shrubs and herbs. Lithologie and pollen stratigraphie relationships and radiocarbon, amino acid and Thorium/Uranium dating allow a tentative assignment to the Sangamonian Stage and possibly to Early and Middle Wisconsinan time. Three intervals of organic accumulation are apparent: an early interval, when climate became warmer than the present; a second interval, when climate was similar to the present; and a third interval, with cooler climate. The latter interval is characterized by at least three climatic cycles, each one cooler than the previous cycle. Tentative correlations with the deep-sea oxygen isotope record and continental palynological records are presented. Des dépôts organiques aux lithologies variées, surmontés d'au moins une unité de till wisconsinien, ont été découverts dans des trous de forage, dans des coupes le long des falaises littorales et de talus alluviaux, ainsi que dans des carrières en de nombreux endroits des provinces atlantiques. L'étude des macrofossiles et la palynologie de ces dépôts, encore à l'étape préliminaire dans de nombreux cas, révèlent l'existence de différents environnements : forêts dominées par des essences feuillues thermophiles et par le pin blanc; forêts mixtes à essences décidues tolérantes et de conifères; forêts boréales d'épinettes et de sapins baumiers; communautés de toundra forestière et de toundra caractérisée par les épinettes, les arbustes et ...
format Text
author Mott, Robert J.
Grant, Douglas R.
spellingShingle Mott, Robert J.
Grant, Douglas R.
Pre-Late Wisconsinan Paleoenvironments in Atlantic Canada
author_facet Mott, Robert J.
Grant, Douglas R.
author_sort Mott, Robert J.
title Pre-Late Wisconsinan Paleoenvironments in Atlantic Canada
title_short Pre-Late Wisconsinan Paleoenvironments in Atlantic Canada
title_full Pre-Late Wisconsinan Paleoenvironments in Atlantic Canada
title_fullStr Pre-Late Wisconsinan Paleoenvironments in Atlantic Canada
title_full_unstemmed Pre-Late Wisconsinan Paleoenvironments in Atlantic Canada
title_sort pre-late wisconsinan paleoenvironments in atlantic canada
publisher Les Presses de l'Université de Montréal
publishDate 1985
url http://id.erudit.org/iderudit/032606ar
https://doi.org/10.7202/032606ar
geographic Canada
geographic_facet Canada
genre toundra
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genre_facet toundra
Tundra
op_relation Géographie physique et Quaternaire
vol. 39 no. 3 (1985)
http://id.erudit.org/iderudit/032606ar
doi:10.7202/032606ar
op_rights Tous droits réservés © Les Presses de l'Université de Montréal, 1985
op_doi https://doi.org/10.7202/032606ar
container_title Géographie physique et Quaternaire
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container_start_page 239
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