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Trilobites du Dévonien des Ardennes (zone rhéno-hercynienne) : biostratigraphie, évolution et événements

Authors:
  • Natuurhistorisch Museum Maastricht

Abstract

Trilobites make up a major component of the Devonian macrofauna in the Ardennes (Belgium, northern France). This has been properly described for the first time through a recently commenced revision. While the Lochkovian and early half Pragian were dominated by classic Rhenish Homalonotidae and Acastidae, the extensive offshore environments that developed in the upper Pragian and Emsian became important habitats to mixed Rhenish-Bohemian trilobite communities. The, at times, richly diversified trilobite assemblages of the early Middle Devonian homoclinal ramp show more gradual (in composition) differences with the exceptions of very littoral habitats and local carbonate build-ups which are each of distinct configurations. The significantly impoverished trilobite fauna of the late Middle Devonian carbonate platform remains poorly documented. A subsequent diversity upsurge is associated with eustatic sea level rises which enabled new immigrations in the basal Frasnian. Trilobites became rare towards the end of the Devonian. Two immigration waves are recognised during the Devonian in the Ardennes: one in the mid Pragian and a second in the lower Frasnian. A third wave in the upper Emsian, which was the only one described in the previous literature, cannot be readily confirmed. As a taxonomic addendum four new species are described from the Middle Devonian in the Couvin area, namely Goldius endelsi sp. nov., Gudralisium rossumi sp. nov., Phaetonellus lelubrei sp. nov. and Diademaproetus dianae sp. nov. Lastly, a list of available species names originally described from the Devonian in the Ardennes is provided.
... The highly diverse trilobite fauna from the middle part of the Jemelle Formation, inclusive of Astycoryphe, Tropidocoryphe, Cornuproetus, Austerops, Loreleiops, Diademaproetus, Ceratarges, Scabriscutellum, Thysanopeltella, Phaetonellus, Kettneraspis and Koneprusia, was drastically reduced in the upper part of this formation ( van Viersen, 2015). In the adjacent German Eifel, a very similar rich "Rhenish" trilobite fauna with "Hercynian" aspect is known from the Ahrdorf Formation (australis Conodont Zone). ...
... A comparatively poorly diversified, proetid-dominated biota was recorded from the upper part of the Jemelle formation, west of Couvin by van Viersen et al. (2012), who correlated this interval and its trilobites, in part, with the Junkerberg Formation (lower kockelianus Conodont Zone) which overlies the Ahrdorf Formation in the Eifel (Fig. 2). Small bioherms high in the Jemelle Formation in the Couvin area have only yielded rare Quadratoproetus (van Viersen, 2015). The knowledge level in the Eifel is, arguably even more than in the Ardennes, defined by a sampling bias towards sections rich in trilobites or yielding specific taxa (e.g. the classic "Geeser Schichten" and "Auburg Schichten" in Kowalski, 1990). ...
... Instead, a shallowing episode was recorded here at this time (e.g. the Lomme Formation) which is likely related to Struve's "Great Gap", described as a series of sedimentary gaps from Middle Devonian neritic shelf environments (Struve, 1982;Walliser et al., 1995). Except for Nyterops which is the only innovation, all trilobite genera from the basal Hanonet Formation including Dechenella (van are components of Figure 3. Stratigraphic ranges of trilobite genera in the Devonian of the Ardennes; figure adopted from van Viersen (2015, fig. 6), and updated with the weakly sculptured phacopines Austerops, Hottonops and Loreleiops recognised by van Viersen et al. (2017) and Frasnian taxa reported herein. ...
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Trilobites are recorded from Frasnian strata in Belgium on the basis of old museum collections and contemporary fieldwork. Of the four third-order Transgressive-Regressive (T-R) cycles recognised here in the latest Givetian to late Frasnian, the last three are each associated with a version of a largely coherent, acastid–scutelluid dominated trilobite fauna. Accents of this “base” fauna encompassed probably primarily allochthonous elements. The timing and effects of the late Frasnian Kellwasser Event in Belgium differ according to fossil group and their position along the ramp. The new data from this study are suggestive of distinct extinction patterns for the trilobite associations of the reefal environments and lateral facies. No evidence was identified for a direct impact of the Kellwasser levels on the Belgian trilobite fauna, although not a single trilobite is known with certainty from strata above the base of the Lower Kellwasser level. Comparisons to trilobite faunas from other countries are suggestive of open, shallow-water migration routes between southern Laurussia and peri-Gondwana during most of the Frasnian. New taxa are Bradocryphaeus echinatus sp. nov., Magreanops renateae gen. & sp. nov. (both Moulin Liénaux Formation), Bradocryphaeus laomedeia sp. nov., Bradocryphaeus neptuni hottonensis ssp. nov., Cyphaspis koimeterionensis sp. nov. (all Grands Breux Formation), Magreanops monachus gen. & sp. nov., Quadratispina excelsa sp. nov. (both Bovesse Formation) and Pterocoryphe platymarginata sp. nov. (Champ Broquet Formation). Magreanops gen. nov. represents the first and only known big-eyed phacopid from Frasnian strata worldwide, breaching the established latest Givetian to late Famennian gap of this group.
... This relatively uniform environment explains why most of the genera exhibited an important cosmopolitanism during the early and middle Frasnian (Feist and McNamara, 2007;Crônier and François, 2014;Van Viersen and Vanherle, 2018). Numerous exchanges existed between North peri-Gondwanan margins and Laurussia (Crônier and François, 2014;Van Viersen, 2015). Nevertheless, despite their cosmopolitanism, Frasnian trilobites seemed to be locally restricted in their specific environment (Bignon and Crônier, 2014;Crônier and François, 2014). ...
... Chlupáč (1994) and Chlupáč & Kolář (2001) noted in particular the reduced provinciality of early Emsian trilobites and the increasingly mixed "Rhenish" and "Hercynian" associations along the southern margin of Laurussia and northern margin of Gondwana. This viewpoint is consistent with the results of studies on early Emsian trilobites in the Ardenno-Rhenish Mountains van Viersen, 2015;van Viersen & Prescher, 2009; the present note), the Armorican Massif, the Cantabrian Mountains and North Africa (e.g. Chlupáč et al., 2000). ...
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A poorly diversified trilobite association is recorded from an outcrop near the village of Breitfeld, Sankt Vith area, East Belgium. The co-occurrence of Arduennella maillieuxi (Asselberghs, 1923) and Burmeisterella quadrispinosa Wenndorf, 1990 in the Breitfeld locality is suggestive of an early lower Emsian age. The outcropping rocks are provisionally attributed to the lower part of the Our Formation (lower Emsian) as opposed to previous assignment to the “Quartzophyllades de Saint Vith” or Sankt Vith Formation (Pragian). Some nomenclatoral notes are provided on the types of A. maillieuxi as the lectotype could not be traced; a cast of the lectotype as well as several paralectotypes of this species are illustrated. Our material of B. quadrispinosa includes cephalic remains that bring new insights into the morphology of this species. A third species, Treveropyge hellemondi sp. nov., is furthermore described. Palaeobiogeographic affiliations of the trilobite association are discussed. A tentative first step is proposed towards trilobite-based correlations of Emsian strata in the Ardenno-Rhenish Mountains. KEYWORDS: Trilobites, systematic palaeontology, biostratigraphy, palaeobiogeography.
... Nonetheless, the incursion of "Bohemian" trilobites in the French Ardennes in the basal Eifelian indicates that exchange of trilobite faunas between the southern and northern margins of the Rheic Ocean was unhindered at this time. In fact, it has been suggested in other studies (e.g., Schraut & Feist 2004;van Viersen 2013van Viersen , 2015 that the incursion of "Bohemian" trilobites in Laurussia already started in the Emsian or even the Pragian. We regard this as evidence to support the putative close relationship between species of Morocops and Geesops despite the fact that they were separated by an ocean. ...
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Abstract Well-preserved specimens of the phacopine trilobites Morocops Basse (= Barrandeops McKellar & Chatterton) and Adrisiops gen. nov. are recorded from upper Emsian strata in Morocco. Morocops is a problematic taxon; the close similarities of its stratigraphically youngest members to the earliest members of Geesops Struve are indicative of grade taxonomy. So far, Morocops is exclusively Gondwanan although potential congeners have been described from peri-Gondwana. One of the stratigraphically oldest species of Geesops occurs in the lower Eifelian of the French Ardennes (Laurussia). Its co-occurrence with pioneer “Bohemian” trilobites there suggests that faunal exchange between Laurussia and peri-Gondwanan terranes was unhindered at that time. New material of Morocops torkozensis (Schraut) is recorded; however, the type locality and horizon of this species remain uncertain. Adrisiops gen. nov. Is erected to accommodate strongly vaulted, Gondwanan taxa that share a unique cephalic morphology inclusive of a short, but rather inflated glabella and ventrally deflected anterior border. New taxa are Morocops spinifer sp. nov. And Adrisiops weugi gen. et sp. nov.
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Well-preserved trilobite specimens are recorded from Eifelian strata between the villages of Nismes (southern Belgium) and Vireux-Molhain (northern France). In the area of study the lower Eifelian Vieux Moulin Member of the Jemelle Formation crops out. The diversified trilobite associations of this unit occur in dark shales and siltstones during a deepening phase and replace the comparatively poorly diversified trilobite fauna of the underlying Eau Noire Formation. This overturn of the local trilobite fauna might, in part, be considered a regional expression of the globally recognised Choteč Event. A marked influx of exotic trilobites in the Vieux Moulin Member is provisionally referred to the local Vieux Moulin Event. Trilobite diversity peaked in the middle Eifelian part (Chavées Member) of the Jemelle Formation before drastically dropping in the upper part of this formation. The manifestations in the Ardennes of the eastern North American Bakoven and Stony Hollow Events can neither be confirmed nor rejected based on the currently available data. New taxa from the early Eifelian part of the Jemelle Formation in the area of study are Asteropyge boeckae sp. nov., Asteropyge eonia sp. nov., Asteropyge filoxenia sp. nov., Cyphaspis insolata sp. nov., Cyphaspis iuxta sp. nov., Diademaproetus pertinax sp. nov., Geesops icovellaunae sp. nov., Gerastos kesselaeri sp. nov., Kettneraspis eftychia sp. nov., Pedinopariops ceuthonymus sp. nov., Pedinopariops richterianus geminus ssp. nov., Scabriscutellum archinalae sp. nov., Septimopeltis akatastasia sp. nov. and Tropidocoryphe insciens sp. nov. Our material includes exceptionally rare, well-preserved specimens from the famous “Mur des douaniers” locality near Vireux-Molhain. Additionally, Astycoryphe rugocauda sp. nov. is described from the lower Eifelian Couvin Formation (southern Belgium) and Gerastos silvicultrix sp. nov. from the uppermost Emsian Heisdorf Formation (German Eifel).
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