Lygodium (Schizaeaceae) in southern high latitudes during the Cenozoic — A new species and new insights into character evolution in the genus

• Published in: Review of Palaeobotany and Palynology
• Main Authors: Rozefelds, Andrew C., Dettmann, Mary E., Clifford, H. Trevor, Carpenter, Raymond J.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Elsevier 2017
• Subjects: Australia; Cenozoic; Lygodium; Schizaeaceae; Southern Hemisphere; 1105 Ecology; Evolution; Behavior and Systematics; 1911 Palaeontology; New Zealand; Queensland; Antarc*; Antarctica
• Online Access: https://espace.library.uq.edu.au/view/UQ:697675

Utilising both macrofossil and spore evidence the fern, Lygodium Swartz, is shown to be common in the Cenozoic of eastern Australia. A new species, Lygodium goonyellum sp. nov. that has laminate fertile pinnules with crenulate margins and reticulate spore morphology (Crassiretitriletes vanraadshoovenii Germeraad, Hopping et Muller), is described from Suttor Formation or its equivalents, near Moranbah, Queensland. Palynological data and isotopic dates support an Oligocene–early Miocene age for this unit. The laminate fertile pinnules and spores in L. goonyellum are morphologically similar to those of extant Lygodium microphyllum (A.J.Cavanilles) R.Brown and Lygodium reticulatum Schkuhr. It differs from the Australian Paleogene species Lygodium dinmorphyllum Churchill in both laminate fertile pinnules and reticulate spores. Additional distributional data on L. dinmorphyllum is provided, utilising evidence from both macrofossils and the dispersed spore record of Cyathidites splendens Harris. Macrofossils of L. dinmorphyllum are recorded from the Lowana Road Locality and from the Tamar Basin in Tasmania, and the Lowmead Basin in Queensland. In addition to the previous records from Queensland, New South Wales, Victoria and South Australia recently collected material is also described from the type locality in southern Queensland. A review of the distribution and fossil record of Lygodium in New Zealand, South America and Antarctica suggests that the genus was widely distributed in high latitudes by the Paleocene, if the dispersed spores attributed to Cyathidites splendens are from Lygodium, and that the L. microphyllum clade appeared by the early Eocene. Spore morphology of Lygodium shows considerable variation, which provides important characters for differentiating groups of extant and fossil species within the genus. The stratigraphic range for these spore types is discussed. Although the known in situ occurrence of Cyathidites splendens is with fertile Lygodium in Cenozoic sediments, dispersed spores have been attributed to the mangrove fern Acrostichum L. (Pteridaceae), or considered to have affinities with Adiantaceae or Cyatheaceae, even though evidence of association has not been demonstrated. Palaeoecological inferences, based upon spore data, that have interpreted sites as mangroves or certain forest types with an understorey of Cyatheaceae/Adiantaceae should be critically re-assessed.