Stratigraphy and Paleoecology of Pleistocene Interstadial Sediments, Central British Columbia

Abstract Two exposures of organic-rich interstadial sediments in central British Columbia provide information on middle Wisconsinan environments and climates near the center of the region subsequently covered by the late Wisconsinan Cordilleran Ice Sheet. Interstadial sediments at Bullion Pit overli...

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Published in:Quaternary Research
Main Authors: Clague, John J., Hebda, Richard J., Mathewes, Rolf W.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1990
Subjects:
Online Access:http://dx.doi.org/10.1016/0033-5894(90)90032-g
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spelling crcambridgeupr:10.1016/0033-5894(90)90032-g 2024-09-09T19:45:24+00:00 Stratigraphy and Paleoecology of Pleistocene Interstadial Sediments, Central British Columbia Clague, John J. Hebda, Richard J. Mathewes, Rolf W. 1990 http://dx.doi.org/10.1016/0033-5894(90)90032-g http://api.elsevier.com/content/article/PII:003358949090032G?httpAccept=text/xml http://api.elsevier.com/content/article/PII:003358949090032G?httpAccept=text/plain https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400020949 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Quaternary Research volume 34, issue 2, page 208-226 ISSN 0033-5894 1096-0287 journal-article 1990 crcambridgeupr https://doi.org/10.1016/0033-5894(90)90032-g 2024-07-31T04:01:02Z Abstract Two exposures of organic-rich interstadial sediments in central British Columbia provide information on middle Wisconsinan environments and climates near the center of the region subsequently covered by the late Wisconsinan Cordilleran Ice Sheet. Interstadial sediments at Bullion Pit overlie drift of early Wisconsinan or older age and underlie thick drift of late Wisconsinan age. Alluvium (or colluvium) and peat were deposited on the floor of the ancestral Quesnel River valley 46,000–40,000 14 C yr ago when the vegetation consisted of spruce forest with dry openings and local fens and the climate was colder and perhaps drier than today. This is broadly consistent with paleoclimatic reconstructions for the same time interval for Babine Lake, 400 km to the northwest, and for Meadow Creek, 400 km to the southeast. Plant-rich pond sediments containing tephra layers and vertebrate remains are exposed between two drifts in a ravine at Mexican Hill, 30 km east of Quesnel. Although they may be contemporaneous with the Bullion Pit beds, the nonglacial sediments at Mexican Hill more likely were deposited sometime after the warmest part of the last interglaciation, but prior to 50,000 yr B.P. At that time, the vegetation at Mexican Hill probably was parkland. The present vegetation at Mexican Hill is boreal forest; thus, a drier and possibly cooler climate is indicated. Article in Journal/Newspaper Ice Sheet Cambridge University Press Parkland ENVELOPE(-120.570,-120.570,55.917,55.917) Babine Lake ENVELOPE(-126.014,-126.014,54.776,54.776) Quaternary Research 34 2 208 226
institution Open Polar
collection Cambridge University Press
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language English
description Abstract Two exposures of organic-rich interstadial sediments in central British Columbia provide information on middle Wisconsinan environments and climates near the center of the region subsequently covered by the late Wisconsinan Cordilleran Ice Sheet. Interstadial sediments at Bullion Pit overlie drift of early Wisconsinan or older age and underlie thick drift of late Wisconsinan age. Alluvium (or colluvium) and peat were deposited on the floor of the ancestral Quesnel River valley 46,000–40,000 14 C yr ago when the vegetation consisted of spruce forest with dry openings and local fens and the climate was colder and perhaps drier than today. This is broadly consistent with paleoclimatic reconstructions for the same time interval for Babine Lake, 400 km to the northwest, and for Meadow Creek, 400 km to the southeast. Plant-rich pond sediments containing tephra layers and vertebrate remains are exposed between two drifts in a ravine at Mexican Hill, 30 km east of Quesnel. Although they may be contemporaneous with the Bullion Pit beds, the nonglacial sediments at Mexican Hill more likely were deposited sometime after the warmest part of the last interglaciation, but prior to 50,000 yr B.P. At that time, the vegetation at Mexican Hill probably was parkland. The present vegetation at Mexican Hill is boreal forest; thus, a drier and possibly cooler climate is indicated.
format Article in Journal/Newspaper
author Clague, John J.
Hebda, Richard J.
Mathewes, Rolf W.
spellingShingle Clague, John J.
Hebda, Richard J.
Mathewes, Rolf W.
Stratigraphy and Paleoecology of Pleistocene Interstadial Sediments, Central British Columbia
author_facet Clague, John J.
Hebda, Richard J.
Mathewes, Rolf W.
author_sort Clague, John J.
title Stratigraphy and Paleoecology of Pleistocene Interstadial Sediments, Central British Columbia
title_short Stratigraphy and Paleoecology of Pleistocene Interstadial Sediments, Central British Columbia
title_full Stratigraphy and Paleoecology of Pleistocene Interstadial Sediments, Central British Columbia
title_fullStr Stratigraphy and Paleoecology of Pleistocene Interstadial Sediments, Central British Columbia
title_full_unstemmed Stratigraphy and Paleoecology of Pleistocene Interstadial Sediments, Central British Columbia
title_sort stratigraphy and paleoecology of pleistocene interstadial sediments, central british columbia
publisher Cambridge University Press (CUP)
publishDate 1990
url http://dx.doi.org/10.1016/0033-5894(90)90032-g
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long_lat ENVELOPE(-120.570,-120.570,55.917,55.917)
ENVELOPE(-126.014,-126.014,54.776,54.776)
geographic Parkland
Babine Lake
geographic_facet Parkland
Babine Lake
genre Ice Sheet
genre_facet Ice Sheet
op_source Quaternary Research
volume 34, issue 2, page 208-226
ISSN 0033-5894 1096-0287
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1016/0033-5894(90)90032-g
container_title Quaternary Research
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