4.5 Article

Plagioptychus (Hippuritida) dominated assemblage from northern Peri-Tethys margin (Bohemian Cretaceous Basin, Cenomanian-Turonian transition)

Journal

CRETACEOUS RESEARCH
Volume 137, Issue -, Pages -

Publisher

ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD
DOI: 10.1016/j.cretres.2022.105227

Keywords

Upper Cretaceous; Rudist taphonomy; Central Europe; Tethyan-Boreal transition

Funding

  1. Ministry of Culture of the Czech Republic [DKRVO 2019e2023/2.I.d, 00023272]
  2. Grant Agency of Czech Republic (GACR) [21-30418J]
  3. Project Cooperatio Faculty of Science

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This study partially refines the stratigraphic ranges of rudist genera and species in the Bohemian Cretaceous Basin and identifies additional rudist and coral species. These findings are important for stratigraphy and paleoecological reconstructions in the Cretaceous ecosystems.
Rudist bivalves are frequently used as an important tool for stratigraphy and palaeoecological reconstructions in Cretaceous ecosystems. In this study, we partly refine stratigraphic ranges of rudist genera and species reported from the Bohemian Cretaceous Basin (BCB). The first occurrences of Plagioptychus haueri (Teller) and consequently, the entire genus Plagioptychus might be dated to the upper Cenomanian. The research focused on two sites exposing near-shore/shallow-water deposits, located in the north-western part of BCB. This area represents palaeobiogeographical boundary between Tethyan and Boreal Realms. Here, the Tethyan rudist fauna reaches its northern limits within the Peri-Tethyan shelfs in Central Europe. Revision resulted in detection of the following rudist species: Plagioptychus haueri, Radiolites bohemicus (both already recognised), Petalodontia aculeodentata, Radiolites sanctaebarbarae and Radiolites saxoniae. Furthermore, large numbers of rudist fragments assignable to Hippuritidina suborder, corals and other macrofauna have been detected. Localities described herein are possibly of upper Cenomanian age, even though lower Turonian origin of some of the material deposited in studied localities cannot be excluded. We assign this taphocenosis with co-occurrence of rudist and coral fauna to 'Coral-Rudist Lithosomes' with two distinctive rudist eco-morphotypes typical of different substrate types and/or environments. Additionally, we discuss stratigraphical position of several taxa within the context of the entire Bohemian Cretaceous Basin.(c) 2022 Elsevier Ltd. All rights reserved.

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