Abstract

Two types of fronds belonging to a new species, Drynaria dimorpha sp. nov., are described from the upper Pliocene Mangbang Formation in western Yunnan, southwestern China. The base frond is lobate and the lobes are incised up to 2/3 or more of the width. The foliage frond is preserved as individual fertile or sterile pinnae with serrated margin and constricted basal part. Circular sori are arranged in one row on either side of the primary vein. In situ spores are monolete and planoconvex, elliptical in polar view and bean-shaped in equatorial view. A detailed morphological comparison suggests that none of the previously described drynarioid fossils and extant species is in accord with the present ferns. The discovery of this new fern indicates that a developed humus-collecting structure of Drynaria had existed and a species-level radiation of this genus had taken place at least by the late Pliocene.

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.