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New data about Matonia braunii (Göppert) Harris from the Early Jurassic of Poland and its ecology

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EN
Fern remains of matoniacean affinity were found in the Lower Hettangian strata of lacustrine/backswamp origin from the Niekłań PGI 1 borehole (central Poland, Holy Cross Mts.). The preserved fragments have been identified as Matonia braunii (Göppert, 1841) Harris, 1980. The remains suggest a rather small, low-growth plant with palmately compound fronds. The sori contain at least 5 sporangia preserved with well-developed annuli. The spores are triangular, trilete and kyrtomate, with a thin and smooth surface corresponding with dispersed Dictyophyllidites mortoni (de Jersey, 1959) Playford et Dettmann, 1965. Based on the gross morphology of sterile and fertile pinnae, suggestions made by Harris (1980) on the synonymy of Phlebopteris braunii (Göppert, 1841) Hirmer et Hörhammer, 1936 with P. muensteri Schenk, 1867 (Hirmer and Hörhammer, 1936) and their referral to Matonia braunii is proved and confirmed in this paper. The fern occurs in strata indicating a warm and humid climate and approaching transgression resulting in a high water table and the enhanced accumulation of organic matter.
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857--868
Opis fizyczny
Bibliogr. 103 poz., rys., wykr.
Twórcy
autor
  • Polish Academy of Sciences, W. Szafer Institute of Botany, Lubicz 46, 31-512 Kraków, Poland
  • Hungarian Natural History Museum, Department of Botany, 1476 Budapest, P.O. Box 222, Hungary
autor
  • Jagiellonian University, Institute of Botany, Department of Palaeobotany and Palaeoherbarium, Lubicz 46, 31-512 Kraków, Poland
  • Polish Geological Institute – National Research Institute, Rakowiecka 4, 00-975 Warszawa, Poland
autor
  • Polish Academy of Sciences, W. Szafer Institute of Botany, Lubicz 46, 31-512 Kraków, Poland
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Uwagi
Opracowanie ze środków MNiSW w ramach umowy 812/P-DUN/2016 na działalność upowszechniającą naukę.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-9d31fa8d-a042-4cdb-a985-cc303ce5f3d9
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