Harmsia hydrocotyloidea McIver et Basinger

Plant Fossil Names Registry Number: PFN001960

Act LSID: urn:lsid:plantfossilnames.org:act:1960

Authors: E. E. McIver & J. F. Basinger

Rank: species

Genus: Harmsia McIver et Basinger

Reference: McIver, E. E. & Basinger, J. F. (1993): Flora of the Ravenscrag Formation (Paleocene), southwestern Saskatchewan, Canada. – Palaeontographica Canadiana 10: 1–167.

Page of description: 54

Illustrations or figures: pl. 45, figs 1–3, pl. 46, fig. 1

Name is type for

Harmsia McIver et Basinger 1993 nom. illeg., non Harmsia K.Schum., Nat. Pflanzenfam. Nachtr. [Engler & Prantl] I. 240 (1897); et in Ann. Ist. Bot. Roma, vii. (1897) 35

Harmsvernia Postnikoff 2009 nom. inval.

Replacement name

Harmsvernia hydrocotyloidea Postnikoff 2009 nom. illeg.

Types

Holotype UAPC-ALTA S8029, University of Alberta (UAPC-ALTA), Edmonton, Canada
Figures: pl. 45, fig. 1.

Original diagnosis/description

Leaves orbiculate, peltate, up to 8.5 cm in diameter; margin shallowly and regularly dentate; teeth mainly of one size, up to 15 mm wide, may be slightly larger where primary veins reach margin, smaller where secondary veins reach margin; glandular, glands forming thickenings at teeth apices where primary of secondary veins reach margin; texture membranous or chartaceous. Venation actinodromous. Primary veins eight, moderate in size, radiating from centre of leaf; course straight, becoming more irregular towards margin. Secondary veins moderate to thin in size, arising from primaries at angles of about 45°, becoming weaker and looping towards margin, joining superadjacent secondaries or reaching margin through centre of teeth. Tertiary veins moderate to weak in size, arising from secondaries at angles of 30–45°, pattern orthogonal reticulate, arrangement opposite and alternate in about equal proportions. Highest order of venation quaternary. Quaternary veins thin, orthogonal, forming areolae. Areolae quadrangular, very large, about 2.0 mm. Free-ending veinlets not known. Marginal venation looped, of fourth order.

Etymology

In reference to the resemblance to Hydrocotyle.

Stratigraphy

Paleogene, Paleocene
Paskapoo Formation

Locality

Canada
[Near the mouth of the Blindman River, Blackfalds], Alberta

Plant fossil remain

macro- and meso-fossils-embryophytes except wood

Notes

Comments

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