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  1. Article

    Open Access

    Uniquely preserved gut contents illuminate trilobite palaeophysiology

    Trilobites are among the most iconic of fossils and formed a prominent component of marine ecosystems during most of their 270-million-year-long history from the early Cambrian period to the end Permian period1. ...

    Petr Kraft, Valéria Vaškaninová, Michal Mergl, Petr Budil, Oldřich Fatka in Nature (2023)

  2. No Access

    Article

    Trepostome bryozoans from the Zahořany Formation (Upper Ordovician) of Loděnice, Prague Basin, Czech Republic

    Three trepostome bryozoan species are described from the Upper Ordovician Zahořany Formation of Loděnice, Prague Basin, Czech Republic. One genus is new—Lodenicella gen. nov. One species is described in open nome...

    Andrej Ernst, Petr Kraft, Kamil Zágoršek in Paläontologische Zeitschrift (2014)

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    Article

    Timing, styles, and kinematics of Cambro–Ordovician extension in the Teplá–Barrandian Unit, Bohemian Massif, and its bearing on the opening of the Rheic Ocean

    This paper describes late Cambrian dikes and Early Ordovician volcano-sedimentary successions of the Prague Basin, Bohemian Massif, to discuss the timing and kinematics of breakup of the northern margin of Gon...

    Jiří Žák, Petr Kraft, Jaroslava Hajná in International Journal of Earth Sciences (2013)

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    Article

    New data on the Neoproterozoic – Cambrian geotectonic setting of the Teplá-Barrandian volcano-sedimentary successions: geochemistry, U-Pb zircon ages, and provenance (Bohemian Massif, Czech Republic)

    The Teplá-Barrandian unit (TBU) of the Bohemian Massif was a part of the Avalonian-Cadomian belt at the northern margin of Gondwana during Neoproterozoic and Early Cambrian times. New detrital zircon ages and ...

    Kerstin Drost, Ulf Linnemann, Neal McNaughton in International Journal of Earth Sciences (2004)

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    Chapter

    Das untere Ordovicium bei Rokycany, Tschechische Republik

    Das untere Ordovicium (Arenig bis Dobrotiva) von Rokycany in West-Böhmen liegt im Westteil des Prager Beckens (Abb. 1), einer schmalen Synkline, die sich in SW-NE-Richtung zwischen Plzeň und der östlichen Umge...

    Jaroslav Kraft, Petr Kraft in Europäische Fossillagerstätten (2000)