Cardstonia tolmanii gen. et sp. nov. (Limnocharitaceae) from the Upper Cretaceous of Alberta, Canada.

Several new broad-leaved monocots were identified in gray siltstones and fine-grained sandstones from the Upper Cretaceous (Campanian-Maastrichtian) St. Mary River Formation near Cardston, Alberta, Canada. Specimens are compression/impressions of long-petiolate aquatic plants that were probably buri...

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Bibliographic Details
Main Authors: Riley, M.G., Stockey, R.A.
Format: Other/Unknown Material
Language:English
Published: 2004
Subjects:
geo
Online Access:https://doi.org/10.7939/R3Q23R99P
https://era.library.ualberta.ca/items/ebd5777f-be36-479e-9bab-0030ef6a0cb0
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spelling fttriple:oai:gotriple.eu:10670/1.uw1l4h 2023-05-15T17:05:20+02:00 Cardstonia tolmanii gen. et sp. nov. (Limnocharitaceae) from the Upper Cretaceous of Alberta, Canada. Riley, M.G. Stockey, R.A. 2004-01-01 https://doi.org/10.7939/R3Q23R99P https://era.library.ualberta.ca/items/ebd5777f-be36-479e-9bab-0030ef6a0cb0 en eng doi:10.7939/R3Q23R99P 10670/1.uw1l4h https://era.library.ualberta.ca/items/ebd5777f-be36-479e-9bab-0030ef6a0cb0 ERA : Education and Research Archive archeo geo Other https://vocabularies.coar-repositories.org/resource_types/c_1843/ 2004 fttriple https://doi.org/10.7939/R3Q23R99P 2023-01-22T17:02:25Z Several new broad-leaved monocots were identified in gray siltstones and fine-grained sandstones from the Upper Cretaceous (Campanian-Maastrichtian) St. Mary River Formation near Cardston, Alberta, Canada. Specimens are compression/impressions of long-petiolate aquatic plants that were probably buried in situ. Leaf blades are entire, ovate to elliptic, with deeply cordate bases; leaf blades are 5–12 cm long and 3.5–8.5 cm wide. Petioles are at least 4 mm wide with five to seven primary veins that enter the leaf blade. Venation is campylodromous, resulting in 23–27 primary veins with three medial veins that remain unbranched to the apex. Major and minor secondary veins (ABAB pattern) diverge at angles of 45°–65° near the midveins and 90° near the leaf margin. Tertiary veins are usually unbranched, but occasional dichotomies and anastomoses occur. No freely ending veinlets are visible. The Cardston specimens are compared with extant leaves of Alismatales and show closest similarities to those of Limnocharis L., Hydrocleys Rich., and Butomopsis Kunth. These leaves are also similar to fossil leaves of Haemanthophyllum Budantsev, in particular H. cordatum Golovneva from the Maastrichtian-Danian deposits of the Koryak Highlands, Russia. A reexamination of the genus Haemanthophyllum, the generitype (H. kamtschaticum Budantsev), the holotype for H. cordatum, and the Cardston specimens results in the description of a new genus, Cardstonia tolmanii gen. et sp. nov. (Limnocharitaceae). This study points to the need for reexamination of the remaining species in the genus Haemanthophyllum, which appear to represent a diverse assemblage of leaves of varying morphology that are probably not a natural group. Other/Unknown Material Koryak Unknown Canada
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic archeo
geo
spellingShingle archeo
geo
Riley, M.G.
Stockey, R.A.
Cardstonia tolmanii gen. et sp. nov. (Limnocharitaceae) from the Upper Cretaceous of Alberta, Canada.
topic_facet archeo
geo
description Several new broad-leaved monocots were identified in gray siltstones and fine-grained sandstones from the Upper Cretaceous (Campanian-Maastrichtian) St. Mary River Formation near Cardston, Alberta, Canada. Specimens are compression/impressions of long-petiolate aquatic plants that were probably buried in situ. Leaf blades are entire, ovate to elliptic, with deeply cordate bases; leaf blades are 5–12 cm long and 3.5–8.5 cm wide. Petioles are at least 4 mm wide with five to seven primary veins that enter the leaf blade. Venation is campylodromous, resulting in 23–27 primary veins with three medial veins that remain unbranched to the apex. Major and minor secondary veins (ABAB pattern) diverge at angles of 45°–65° near the midveins and 90° near the leaf margin. Tertiary veins are usually unbranched, but occasional dichotomies and anastomoses occur. No freely ending veinlets are visible. The Cardston specimens are compared with extant leaves of Alismatales and show closest similarities to those of Limnocharis L., Hydrocleys Rich., and Butomopsis Kunth. These leaves are also similar to fossil leaves of Haemanthophyllum Budantsev, in particular H. cordatum Golovneva from the Maastrichtian-Danian deposits of the Koryak Highlands, Russia. A reexamination of the genus Haemanthophyllum, the generitype (H. kamtschaticum Budantsev), the holotype for H. cordatum, and the Cardston specimens results in the description of a new genus, Cardstonia tolmanii gen. et sp. nov. (Limnocharitaceae). This study points to the need for reexamination of the remaining species in the genus Haemanthophyllum, which appear to represent a diverse assemblage of leaves of varying morphology that are probably not a natural group.
format Other/Unknown Material
author Riley, M.G.
Stockey, R.A.
author_facet Riley, M.G.
Stockey, R.A.
author_sort Riley, M.G.
title Cardstonia tolmanii gen. et sp. nov. (Limnocharitaceae) from the Upper Cretaceous of Alberta, Canada.
title_short Cardstonia tolmanii gen. et sp. nov. (Limnocharitaceae) from the Upper Cretaceous of Alberta, Canada.
title_full Cardstonia tolmanii gen. et sp. nov. (Limnocharitaceae) from the Upper Cretaceous of Alberta, Canada.
title_fullStr Cardstonia tolmanii gen. et sp. nov. (Limnocharitaceae) from the Upper Cretaceous of Alberta, Canada.
title_full_unstemmed Cardstonia tolmanii gen. et sp. nov. (Limnocharitaceae) from the Upper Cretaceous of Alberta, Canada.
title_sort cardstonia tolmanii gen. et sp. nov. (limnocharitaceae) from the upper cretaceous of alberta, canada.
publishDate 2004
url https://doi.org/10.7939/R3Q23R99P
https://era.library.ualberta.ca/items/ebd5777f-be36-479e-9bab-0030ef6a0cb0
geographic Canada
geographic_facet Canada
genre Koryak
genre_facet Koryak
op_source ERA : Education and Research Archive
op_relation doi:10.7939/R3Q23R99P
10670/1.uw1l4h
https://era.library.ualberta.ca/items/ebd5777f-be36-479e-9bab-0030ef6a0cb0
op_doi https://doi.org/10.7939/R3Q23R99P
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