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Turonian-Coniacian silicified plants from the flints of Claix (Charente, western France)

Jean-David Moreau 1 Didier Néraudeau 1 Jean-Pierre Platel Anne-Lyse Ravon 2 Mathieu Le Couls 1 Vincent Fernandez 3 Paul Tafforeau 3
1 GR - Géosciences Rennes
2 CReAAH - Centre de Recherche en Archéologie, Archéosciences, Histoire
3 ESRF - European Synchrotron Radiation Facility
Abstract : In western France, most of Cretaceous plant megaremains are preserved as impressions (external casts) in clay or compressions with or without cuticle in lignite. Remains are commonly highly flattened and only the gross morphology can be provided. When the cuticle is preserved, it shows casts of the most peripheral epidermal cells, allowing the description of microstructural details such as morphology and size of ordinary cells and stomatal apparatuses. However, compressions with cuticles never preserved histology. Silica-rich nodules have been recently collected in surface alterite and Palaeolithic or Neolithic habitats of Claix (Charente, western France). Some of the flints contain diverse plant megaremains. Specimens were examined under light microscopy (LM) and scanning electron microscopy (SEM). In order to detect fossil inclusions inside flints we made preliminary imaging tests using high resolution and high energy X-ray synchrotron microtomography (PPC-SRμCT). The plant assemblage is late Turonianearlymost Coniacian in age and consists of abundant leafy axes of conifers (Brachyphyllum Brongn., Frenelopsis (Schenk) emend. J. Watson, and Geinitzia Endl.) and rare leaves of angiosperms and pinnae of ferns. Such plant diversity is for the first time observed is post-Cenomanian flints from this part of Europe. By contrast with most of lignitic plant beds of western France, the plants from the flints of Claix are exquisitely preserved in three dimensions, showing details of cuticle and inner tissues. It consists of silicified petrification/permineralization, the origin of the silicification being questionable.
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Conference papers
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Submitted on : Thursday, October 27, 2016 - 10:40:08 AM
Last modification on : Thursday, January 20, 2022 - 5:26:02 PM

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  • HAL Id : insu-01388504, version 1

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Citation

Jean-David Moreau, Didier Néraudeau, Jean-Pierre Platel, Anne-Lyse Ravon, Mathieu Le Couls, et al.. Turonian-Coniacian silicified plants from the flints of Claix (Charente, western France). 25 ème Réunion des sciences de la Terre (RST 2016), Société Géologique de France, Oct 2016, Caen, France. pp.230. ⟨insu-01388504⟩

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