Permineralized seed fern cupules from the Triassic of Antarctica: implications for cupule and carpel evolution

• Published in: American Journal of Botany
• Main Authors: Taylor, Thomas N., Fueyo, Georgina M. Del, Taylor, Edith L.
• Other Authors: National Science Foundation
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 1994
• Subjects: Antarc*; Antarctica
• Online Access: http://dx.doi.org/10.1002/j.1537-2197.1994.tb15501.x; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fj.1537-2197.1994.tb15501.x; https://onlinelibrary.wiley.com/doi/pdf/10.1002/j.1537-2197.1994.tb15501.x; http://api.wiley.com/onlinelibrary/chorus/v1/articles/10.1002%2Fj.1537-2197.1994.tb15501.x

In this paper we describe the first anatomically preserved Mesozoic seed fern cupule– Petriellaea. The multiovulate cupules were produced singly at the end of a short dichotomizing axis. Cupules are bilateral with a dorsal groove and transverse narrow ventral opening. The vascular system of the cupule consists of a series of traces that extend up the dorsal surface of the cupule and down the ventral face. Ovules are orthotropus, sessile, and borne on the adaxial surface of the leaflike cupule either singly or in multiple rows. They are up to 1.5 mm long, triangular in transverse section, and characterized by a multilayered integument. Nucellus and integument are fused throughout their length, but no pollen chamber is present. In the chalaza is a small vascular disc of transfusion tracheids that represents the extent of the ovule vascular system. Ovules are interpreted as being fossilized at a prepollination stage, although a few possess some evidence of a cellularized megagametophyte. These permineralized cupules indicate that in at least one Mesozoic seed fern group, ovule enclosure resulted from the transverse folding (tip to petiole) of a megasporophyll bearing adaxial ovules. Cupule morphology and ovule enclosure in other Late Paleozoic and Mesozoic seed ferns is discussed.