Glacial Lake Arkona – Whittlesey transition near Leamington, Ontario: geology, plant, and muskox fossils
Proglacial subaquatic fans between Leamington and Colchester, Essex County, Ontario, were deposited in glacial Lake Maumee at the end of the Port Bruce Stade by ice retreating northward. Some fans were buried by till and glaciolacustrine materials. One fan surface, northwest of Leamington, was only...
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crcansciencepubl:10.1139/e93-210 2024-03-03T08:46:33+00:00 Glacial Lake Arkona – Whittlesey transition near Leamington, Ontario: geology, plant, and muskox fossils Morris, T. F. McAndrews, J. H. Seymour, K. L. 1993 http://dx.doi.org/10.1139/e93-210 http://www.nrcresearchpress.com/doi/pdf/10.1139/e93-210 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 30, issue 12, page 2436-2447 ISSN 0008-4077 1480-3313 General Earth and Planetary Sciences journal-article 1993 crcansciencepubl https://doi.org/10.1139/e93-210 2024-02-07T10:53:44Z Proglacial subaquatic fans between Leamington and Colchester, Essex County, Ontario, were deposited in glacial Lake Maumee at the end of the Port Bruce Stade by ice retreating northward. Some fans were buried by till and glaciolacustrine materials. One fan surface, northwest of Leamington, was only modified by lake current that transgressed and regressed over it. An aggregate excavation (Bondi site) exists within the surface of this fan. We describe the sedimentology of the site that provides evidence for fan and overlying bar deposits.Lake levels fell to the levels of lakes Arkona (216 m) and Ypsilanti (122 m) following the deposition of the fans. Large terrestrial areas supported plants and animals. Their presence is recorded at the Bondi site by a single bone and several organic mats recovered from the fan and bar sediment contact at two separate exposures. Radiocarbon dates on the bone of 13 410 ± 100 BP (TO-1803), organic material dates of 13 225 ± 200 BP (BGS-1404) and 13 150 ± 100 BP (WE-01-89), the altitude. (209 m), and the sedimentological setting indicate deposition during the Lake Arkona (216 m) – Lake Whittlesey (226 m) transition period.The pollen and plant macrofossil assemblages recovered from the organic material indicate a forest–tundra environment, with a mean July temperature of 14 °C. This interpretation fits well with the bone identified as cf. Euceratherium sp., a shrubox. The discovery of cf. Euceratherium sp. is surprising, as its previous range was south and west of this site. The organic material was subsequently buried by the formation of a bar as water levels rose within the Lake Erie basin and transgressed the site. Article in Journal/Newspaper muskox Tundra Canadian Science Publishing Glacial Lake ENVELOPE(-129.463,-129.463,58.259,58.259) Canadian Journal of Earth Sciences 30 12 2436 2447 |
institution |
Open Polar |
collection |
Canadian Science Publishing |
op_collection_id |
crcansciencepubl |
language |
English |
topic |
General Earth and Planetary Sciences |
spellingShingle |
General Earth and Planetary Sciences Morris, T. F. McAndrews, J. H. Seymour, K. L. Glacial Lake Arkona – Whittlesey transition near Leamington, Ontario: geology, plant, and muskox fossils |
topic_facet |
General Earth and Planetary Sciences |
description |
Proglacial subaquatic fans between Leamington and Colchester, Essex County, Ontario, were deposited in glacial Lake Maumee at the end of the Port Bruce Stade by ice retreating northward. Some fans were buried by till and glaciolacustrine materials. One fan surface, northwest of Leamington, was only modified by lake current that transgressed and regressed over it. An aggregate excavation (Bondi site) exists within the surface of this fan. We describe the sedimentology of the site that provides evidence for fan and overlying bar deposits.Lake levels fell to the levels of lakes Arkona (216 m) and Ypsilanti (122 m) following the deposition of the fans. Large terrestrial areas supported plants and animals. Their presence is recorded at the Bondi site by a single bone and several organic mats recovered from the fan and bar sediment contact at two separate exposures. Radiocarbon dates on the bone of 13 410 ± 100 BP (TO-1803), organic material dates of 13 225 ± 200 BP (BGS-1404) and 13 150 ± 100 BP (WE-01-89), the altitude. (209 m), and the sedimentological setting indicate deposition during the Lake Arkona (216 m) – Lake Whittlesey (226 m) transition period.The pollen and plant macrofossil assemblages recovered from the organic material indicate a forest–tundra environment, with a mean July temperature of 14 °C. This interpretation fits well with the bone identified as cf. Euceratherium sp., a shrubox. The discovery of cf. Euceratherium sp. is surprising, as its previous range was south and west of this site. The organic material was subsequently buried by the formation of a bar as water levels rose within the Lake Erie basin and transgressed the site. |
format |
Article in Journal/Newspaper |
author |
Morris, T. F. McAndrews, J. H. Seymour, K. L. |
author_facet |
Morris, T. F. McAndrews, J. H. Seymour, K. L. |
author_sort |
Morris, T. F. |
title |
Glacial Lake Arkona – Whittlesey transition near Leamington, Ontario: geology, plant, and muskox fossils |
title_short |
Glacial Lake Arkona – Whittlesey transition near Leamington, Ontario: geology, plant, and muskox fossils |
title_full |
Glacial Lake Arkona – Whittlesey transition near Leamington, Ontario: geology, plant, and muskox fossils |
title_fullStr |
Glacial Lake Arkona – Whittlesey transition near Leamington, Ontario: geology, plant, and muskox fossils |
title_full_unstemmed |
Glacial Lake Arkona – Whittlesey transition near Leamington, Ontario: geology, plant, and muskox fossils |
title_sort |
glacial lake arkona – whittlesey transition near leamington, ontario: geology, plant, and muskox fossils |
publisher |
Canadian Science Publishing |
publishDate |
1993 |
url |
http://dx.doi.org/10.1139/e93-210 http://www.nrcresearchpress.com/doi/pdf/10.1139/e93-210 |
long_lat |
ENVELOPE(-129.463,-129.463,58.259,58.259) |
geographic |
Glacial Lake |
geographic_facet |
Glacial Lake |
genre |
muskox Tundra |
genre_facet |
muskox Tundra |
op_source |
Canadian Journal of Earth Sciences volume 30, issue 12, page 2436-2447 ISSN 0008-4077 1480-3313 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/e93-210 |
container_title |
Canadian Journal of Earth Sciences |
container_volume |
30 |
container_issue |
12 |
container_start_page |
2436 |
op_container_end_page |
2447 |
_version_ |
1792502599344193536 |