Ankyropteris brongniartii Renault, 1869

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

publication ID

https://doi.org/ 10.5252/g2011n1a4

DOI

https://doi.org/10.5281/zenodo.4607891

persistent identifier

https://treatment.plazi.org/id/5328C915-CD63-0D1C-B4D1-0634AAABB2AE

treatment provided by

Felipe

scientific name

Ankyropteris brongniartii Renault, 1869
status

 

Ankyropteris brongniartii Renault, 1869

( Fig. 6 View FIG A-G)

This small tedelean fern is one of the best known Palaeozoic ferns (Phillips & Galtier in press); it has a wide stratigraphic range from Early Pennsylvanian to Early Permian where it was first described from Autun by Renault (1869) and from Chemnitz by Stenzel (1889) under the name Ankyropteris scandens . This fern is a vine known to have been growing on trunks of the Psaronius tree ferns.We found portions of all the different parts of the tripinnate frond in a few specimens. The primary rachis ( Fig. 6A View FIG ) has the characteristic H-shaped xylem strand, and a secondary rachis with the base of third order one is illustrated on Figure 6B View FIG . Foliage of this fern was found lying gently within accumulations of leaves of other plants ( Fig. 6C View FIG ).Tertiary rachises (R3, Fig. 6 View FIG C-E) and pinnules have been observed.Their excellent preservation reveals unknown details on the anatomy of the rather rigid pinnules ( Fig. 6 View FIG C-G). Their lamina proves to be significantly thicker than in the rare examples previously described from Pennsylvanian material; the histology of the mesophyll is revealed as well as the occurrence of stomata (arrows, Fig. 6F, G View FIG ). Unfortunately fertile pinnae have not been found.

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