A BURIED PALEOSOL IN THE HUDSON BAY LOWLAND, MANITOBA: AGE AND CHARACTERISTICS
A Brunisolic–paleosol soil sequence is described from an ancient marine strandline in the Hudson Bay Lowland of northern Manitoba. The paleosol, underlying a present-day Brunisolic soil, is almost an exact morphologic counterpart of the contemporary soil. A radiocarbon date from the upper horizon of...
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Language: | English |
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Canadian Science Publishing
1978
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Online Access: | http://dx.doi.org/10.4141/cjss78-030 http://www.nrcresearchpress.com/doi/pdf/10.4141/cjss78-030 |
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crcansciencepubl:10.4141/cjss78-030 2023-12-17T10:31:22+01:00 A BURIED PALEOSOL IN THE HUDSON BAY LOWLAND, MANITOBA: AGE AND CHARACTERISTICS MILLS, G. F. VELDHUIS, H. 1978 http://dx.doi.org/10.4141/cjss78-030 http://www.nrcresearchpress.com/doi/pdf/10.4141/cjss78-030 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Soil Science volume 58, issue 2, page 259-269 ISSN 0008-4271 1918-1841 Soil Science journal-article 1978 crcansciencepubl https://doi.org/10.4141/cjss78-030 2023-11-19T13:38:23Z A Brunisolic–paleosol soil sequence is described from an ancient marine strandline in the Hudson Bay Lowland of northern Manitoba. The paleosol, underlying a present-day Brunisolic soil, is almost an exact morphologic counterpart of the contemporary soil. A radiocarbon date from the upper horizon of the buried soil indicates a minimum age of 2,380 ± 120 yr for the contemporary Brunisolic soil. The established geochronology of the Hudson Bay Lowland indicates that the marine beach on which this soil sequence is found was deposited about 7,000 YBP. The paleosol, therefore, may have developed over a maximum time interval of 4,500 yr allowing for a possible age difference between the two soils of up to 2,000 yr. However, a precise relationship between time and soil development can not be determined from this study. Because of limitations inherent in comparative soil morphology, uncertainty about the absolute age of the paleosol and difficulty in interpreting single radiocarbon dates, it is just as possible that both soils could develop over similar time intervals. This possibility is supported by the similar morphology of the two soils. Article in Journal/Newspaper Hudson Bay Canadian Science Publishing (via Crossref) Hudson Bay Hudson Canadian Journal of Soil Science 58 2 259 269 |
institution |
Open Polar |
collection |
Canadian Science Publishing (via Crossref) |
op_collection_id |
crcansciencepubl |
language |
English |
topic |
Soil Science |
spellingShingle |
Soil Science MILLS, G. F. VELDHUIS, H. A BURIED PALEOSOL IN THE HUDSON BAY LOWLAND, MANITOBA: AGE AND CHARACTERISTICS |
topic_facet |
Soil Science |
description |
A Brunisolic–paleosol soil sequence is described from an ancient marine strandline in the Hudson Bay Lowland of northern Manitoba. The paleosol, underlying a present-day Brunisolic soil, is almost an exact morphologic counterpart of the contemporary soil. A radiocarbon date from the upper horizon of the buried soil indicates a minimum age of 2,380 ± 120 yr for the contemporary Brunisolic soil. The established geochronology of the Hudson Bay Lowland indicates that the marine beach on which this soil sequence is found was deposited about 7,000 YBP. The paleosol, therefore, may have developed over a maximum time interval of 4,500 yr allowing for a possible age difference between the two soils of up to 2,000 yr. However, a precise relationship between time and soil development can not be determined from this study. Because of limitations inherent in comparative soil morphology, uncertainty about the absolute age of the paleosol and difficulty in interpreting single radiocarbon dates, it is just as possible that both soils could develop over similar time intervals. This possibility is supported by the similar morphology of the two soils. |
format |
Article in Journal/Newspaper |
author |
MILLS, G. F. VELDHUIS, H. |
author_facet |
MILLS, G. F. VELDHUIS, H. |
author_sort |
MILLS, G. F. |
title |
A BURIED PALEOSOL IN THE HUDSON BAY LOWLAND, MANITOBA: AGE AND CHARACTERISTICS |
title_short |
A BURIED PALEOSOL IN THE HUDSON BAY LOWLAND, MANITOBA: AGE AND CHARACTERISTICS |
title_full |
A BURIED PALEOSOL IN THE HUDSON BAY LOWLAND, MANITOBA: AGE AND CHARACTERISTICS |
title_fullStr |
A BURIED PALEOSOL IN THE HUDSON BAY LOWLAND, MANITOBA: AGE AND CHARACTERISTICS |
title_full_unstemmed |
A BURIED PALEOSOL IN THE HUDSON BAY LOWLAND, MANITOBA: AGE AND CHARACTERISTICS |
title_sort |
buried paleosol in the hudson bay lowland, manitoba: age and characteristics |
publisher |
Canadian Science Publishing |
publishDate |
1978 |
url |
http://dx.doi.org/10.4141/cjss78-030 http://www.nrcresearchpress.com/doi/pdf/10.4141/cjss78-030 |
geographic |
Hudson Bay Hudson |
geographic_facet |
Hudson Bay Hudson |
genre |
Hudson Bay |
genre_facet |
Hudson Bay |
op_source |
Canadian Journal of Soil Science volume 58, issue 2, page 259-269 ISSN 0008-4271 1918-1841 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.4141/cjss78-030 |
container_title |
Canadian Journal of Soil Science |
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58 |
container_issue |
2 |
container_start_page |
259 |
op_container_end_page |
269 |
_version_ |
1785584660695220224 |