page_title: Angoumian
section_title: Lower Angoumian
hierarchical_section_title: Angoumian / Stratigraphy / Lower Angoumian
caption_attribution_description: English: A rudist biostrome in the Angoulême Formation of the Angoumian (group), Turonian. Picture taken in the Aucors quarry near Beaussac, Dordogne, France.
context_page_description: The Angoumian is a geological group restricted to the northern Aquitaine Basin in France. The group consists of two fossiliferous limestone formations deposited during the Turonian.
context_section_description: (Represented on French geological maps as unit c3b)
  The 15–20 m thick lower Angoumian, also called Angoulême Formation, starts with a 5–6 m thick, thinly bedded, microcrystalline limestone of white to creamy colour. This limestone is characterised by the incorporation of fine debris and by a benthic microfauna consisting of foraminifera such as miliolida and textulariida. The first rudists (Sphaerulites patera and Biradiolites lumbricalis) start to appear in this level. Some rare cephalopods have also been found (such as Romaniceras deverianum or Lecointriceras fleuriausianum for instance).
  These fairly thin beds then give way to a massive, homogeneous, normally 8–10 m thick, chalky, rudist-bearing limestone of pure white colour. The massive bed stands out geomorphologically, sometimes forming small cliffs in the countryside. Generally this rock is quite soft (it can be cut with a handsaw), it was therefore quarried extensively for building stone with hundreds of small quarries in operation; most of them have closed down by now. The massive member is affected by important thickness variations (its total thickness normally can vary from 5–12 m, sometimes even reaching 15 m), caused either by tectonic disturbances or by post-depositional erosion (for instance, in the Mareuil Anticline, the upper Angoumian discordantly overlies the lower Angoumian, occasionally even cutting down into it). The chalky limestones are mainly composed of rudist debris with comparatively little cement. The rudist debris consists almost exclusively of the species Biradiolites lumbricalis accompanied by minor Durania cornupastoris, Praeradiolites peroni, Radiolites peroni, Radiolites ponsi, Radiolites beaumonti, Radiolites socialis, and Hippurites requieni. In some places, undamaged rudists (mainly the small-sized Biradiolites) can be encountered in numerous biostromes. Towards the top, the massive bed changes its character and thinner beds of a very hard limestone or of an ocre calcarenite appear. This horizon is the upper limit of the quarrying activity and was called chaudron (kettle) by the miners. In addition to the usual fauna, it also comprises small biostromes of Biradiolites angulosus.
  The common facies can change quite suddenly (within less than 500 m) into a coarse, weakly cemented, bioclastic facies  (Pierre de Cheyroux) consisting of white to yellowish calcarenites — a beachrock facies, indicating a littoral position of the deposits. The bioclasts are very rounded and are composed of the debris of echinoderms, rudists, single corals (polyps), and milioles. These rather massive calcarenites can reach a thickness of 12–15 m in places and sometimes are affected by cross-bedding. They occur somewhat southeast of the La Tour Blanche anticline and the Périgueux anticline, proving that these major structures were already beginning to rise during the Turonian.
  The lower formation finishes with a few metres of thinly bedded, yellowish, microcrystalline limestone rich in bioclasts (lamellibranchs and echinoderms). This member shows cross-bedding and is affected by hiati as observed in Brantôme.
  The common rudist-bearing reefal facies can completely change in the western depositional area, taking on a very hard, finely recrystallised aspect without any fossil debris. This facies change is probably due to faulting.
caption: A rudist biostrome in the Angoulême Formation; Aucors quarry near Beaussac, Dordogne
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