Lysichiton austriacus (J.Kvaček et A.B.Herman) Bogner, K.R.Johnson, Kvaček et Upchurch
Plant Fossil Names Registry Number: PFN001932
Act LSID: urn:lsid:plantfossilnames.org:act:1932
Basionym: Araciphyllites austriacus J.Kvaček et A.B.Herman
Reference: Bogner, J., Johnson, K. R., Kvaček, Z. & Upchurch, G. R., Jr. (2007): New fossil leaves of Araceae from the Late Cretaceous and Paleogene of western North America. – Zitteliana, Ser. A 47: 133–147.
Page of description: 142
Holotype NHMW 1999B0057/0183, Naturhistorisches Museum Wien, Vienna, Austria
Figures: pl. I, figs 1, 2, 4
Note: Holotype refigured by Kvaček and Herman (2005: Čas. Nár. Muz., Řada Přír., 174(1-4): figs 1, 2).
Leaves large, simple; elongate-lanceolate, entire-margined. Apex and base unknown. Venation eucamptodromous, parallel-pinnate. Midrib costa massive, deeply impressed, probably reaching the apex, consisting of numerous vascular bundles. Laterals emerging at low angle from midrib. Parallel venation consisting of three weekly differentiated vein subsets arranged according to the formula BdCdB. Transverse vein sets of two categories, connecting adjacent parallel veins or veins of the same subset (C–C, d–d) being oriented obliquely or perpendicularly. Areoles polygonal-quadrangular, elongate.
Bogner et al. (2007: Zitteliana, Ser. A, 47: 142):
Corrected addition to the description: Leaf blade with only primary lateral veins pinnate, higher-order venation ± regularly transverse reticulate between them.
Kvaček, J. and Smith (2015: Bot. J. Linn. Soc., 178(3): 492):
Leaf entire-margined, midrib multistranded, venation parallel-pinnate, eucamptodromous. Primary lateral venation consisting of three well-defined vein subsets leaving costa at low angles. Higher order transverse venation perpendicular to slightly oblique, reticulate. Transverse veins irregularly connecting all orders of primary lateral veins.
Named after the country of origin.
Cretaceous, Upper Cretaceous, Campanian
Grünbach Formation, Lower Campanian
Grünbach am Schneeberg, Segen Gottes Quarry (47°47′52″N, 15°59′17″E).
Plant fossil remain
macro- and meso-fossils-embryophytes except wood
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