Stewartiopteris, Morgan & Delevoryas, 1952

Galtier, Jean, Ronchi, Ausonio & Broutin, Jean, 2011, Early Permian silicified floras from the Perdasdefogu Basin (SE Sardinia): comparison and bio-chronostratigraphic correlation with the floras of the Autun Basin (Massif central, France), Geodiversitas 33 (1), pp. 43-69 : 56-57

publication ID

https://doi.org/ 10.5252/g2011n1a4

DOI

https://doi.org/10.5281/zenodo.4607897

persistent identifier

https://treatment.plazi.org/id/5328C915-CD63-0D1F-B77D-0791AC46B190

treatment provided by

Felipe

scientific name

Stewartiopteris
status

 

Stewartiopteris sp. 1 and sp. 2

( Fig. 7C, D View FIG )

The large rachis ( Fig. 7C View FIG ), shows a broad C-shaped xylem strand (arrows, Fig. 7C View FIG ) and outer sclerenchymatous cortex; it represents the proximal region of a frond. The smaller rachis shown on Figure 7D View FIG is quite distinct in cortical organization. It certainly corresponds to a second order rachis alongside the corresponding third order rachis (R3, Fig.7D View FIG ) which is in connection with a fertile pinnule (P, Fig. 7D View FIG ). These two Stewartiopteris rachises certainly belonged to different fronds.

Foliage of these tree ferns occasionally occurs as dense accumulations of vegetative and/or fertile pinnules as shown on Figure 7E View FIG . One section of an ultimate pinna, paradermal to the pinnule surfaces ( Fig. 7F View FIG ), reveals their pecopteroid morphology. At least three different taxa occur in the assemblage as is suggested by differences in the fertile pinnae.

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