Cécile Poplin’s research while affiliated with Muséum National d'Histoire Naturelle and other places

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Publications (20)


The Braincase Anatomy of Lawrenciella schaefferi, Actinopterygian from the Upper Carboniferous of Kansas (USA)
  • Article

December 2008

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70 Reads

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35 Citations

Marie-Hélène Hamel

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Cécile Poplin

Muséum national d'Histoire naturelle—Département Histoire de la Terre, USM 0203—UMR 5143 CNRS, Paléobiodiversité et Paléoenvironnement, CP 38 8 rue Buffon-75231 Paris cedex O5—France; 1 mhhamel@yahoo.fr; 2 cpoplin@mnhn.fr ABSTRACT—A full description and diagnosis are given of Lawrenciella schaefferi Poplin 1984, from the Pennsylvanian (Late Carboniferous) of Kansas, U.S.A. This taxon is only known by braincases and associated parasphenoids, which are exceptionally well preserved as phosphatic nodules. The external and internal morphology of the endocrania were studied from serial sectionings which allowed detailed three-dimensional reconstructions. The study shows that, besides synapo-morphies inherent to basal actinopterans, L. schaefferi displays a set of very peculiar features such as prespiracular fossae, intracranial ossicles, and paired anterior myodomes for nonocular eye muscles. Another conspicuous feature, the noto-chordal canal ending blindly anteriorly, has been observed until now only in more advanced Triassic actinopterans. The anatomical characters of L. schaefferi indicate, in the light of recent cladistic analyses, that this Carboniferous taxon is a relatively advanced actinopteran compared to basal forms such as Kentuckia, Mimia, or Moythomasia.


An enigmatic actinopterygian (Pisces: Osteichthyes) from the Upper Permian of China

June 2008

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181 Reads

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9 Citations

Zoological Journal of the Linnean Society

A new actinopterygian fish Yaomoshania minutosquama gen. & sp. nov., from the Upper Permian of the Dzungaria [Junggar] Basin in China is described. The material consists of two very fragmentary specimens showing almost exclusively scale rows. The arrangement of the scale rows of the holotype resembles the reversion lines of acanthodian caudal fins and of cheirolepids. The size and shape of the scales, and the diminishing size of the scales along the rows, is similar to those of acanthodians and those actinopterygians with small scales such as Cheirolepis. However, the histology of the scales demonstrates features that are found in more advanced actinopterygians: superimposed ganoine lamellae, the arrangement of dentine tubules and pulp canals, buried odontodes stacked on each other to make the ornamental ridges, and an asymmetric pattern of growth achieved by extensive remodelling (resorption and redeposition) of all layers of the scale. Yaomoshania minutosquama is proposed as a small-scale bearing, basal actinopterygian, different from Cheirolepis, but characterized by advanced histological characters.


Les Aeduellidae (Pisces, Actinopterygii) carbonifères et permiens: systématique et étude phylogénétique préliminaire
  • Article
  • Full-text available

July 2005

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612 Reads

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14 Citations

GEODIVERSITAS

Les Aeduellidae (Pisces, Actinopterygii) carbonifères et permiens :systématique et étude phylogénétique préliminaire. Geodiversitas 27 (1) :17-33. RÉSUMÉ Les genres et espèces d'aeduellidés actuellement connus sont présentés. Une analyse phylogénétique, impliquant 12 autres actinoptérygiens et un porolé-piforme comme groupe extérieur, confirme que les Aeduellidae constituent un groupe naturel. Mais les relations de parenté de ses taxons, dont un genre, Bourbonnella, apparaît comme paraphylétique, ne sont pas entièrement éclair-cies, probablement en raison du nombre de données manquantes. Cette famille présente une mosaïque de caractères plésiomorphes et apomorphes pour les actinoptérygiens. Les relations phylogénétiques des Aeduellidae avec les autres Actinopteri basaux (= Palaeoniscimorpha) ne sont pas non plus éclaircies. En effet l'analyse ne révèle pas d'affinités particulières avec les groupes avec lesquels on avait tenté de les rapprocher par le passé. ABSTRACT The carboniferous and permian Aeduellidae (Pisces, Actinopterygii): systematics and preliminary phylogenic study. The aeduellid genera and species already known are presented. A phylogenet-ic analysis, involving 12 other actinopterygians and a porolepiform outgroup, confirms that the Aeduellidae are a natural group. But their interrelationships are not cleared up completely, probably because of many missing data; in par-ticular one genus, Bourbonnella, appears as paraphyletic. This family has a mosaic of plesiomorphic and apomorphic actinopterygian characters; their relationships with the other basal Actinopteri (= Palaeoniscimorpha) are not clearer. In fact the analysis does not show particular affinities with the groups with which they have been tentively compared in the past.

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The carboniferous and permian Aeduellidae (Pisces, Actinopterygii): Systematics and preliminary phylogenic study

March 2005

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22 Reads

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5 Citations

GEODIVERSITAS

The aeduellid genera and species already known are presented. A phylogenetic analysis, involving 12 other actinopterygians and a porolepiform outgroup, confirms that the Aeduellidae are a natural group. But their interrelationships are not cleared up completely, probably because of many missing data; in particular one genus, Bourbonnella, appears as paraphyletic. This family has a mosaic of plesiomorphic and apomorphic actinopterygian characters; their relationships with the other basal Actinopteri (= Palaeoniscimorpha) are not clearer. In fact the analysis does not show particular affinities with the groups with which they have been tentively compared in the past. © Publications Scientifiques du Muséum national d'Histoire naturelle, Paris.


FIGURE 1. A-C, Tarrasius problematicus. A, reconstruction of the cheek, after Taverne (1996); B, reconstruction of the skull roof, slightly modified after Taverne (1996); C, recontruction of the whole fish: after Taverne (1996) for the skull, and after Jessen (1973) for the body. D-F, Paratarrasius hibbardi. D, reconstruction of the cheek slightly modified after Lund and Melton (1982); E, reconstruction of the skull roof after Lund and Melton (1982); F, reconstruction of the whole fish with scale rows, a scaled area indicated on the flank. Abbreviations: Ang, angular; Ant, antorbital; Aop, anteopercle; ceth, ethmoidal commissure; Cl, cleithrum; Cla, clavicle; cmd, mandibular canal; cpop, preopercle canal; cst, supratemporal commissure; De, dentary; Dhy, dermohyal; Dpt, dermopterotic; Dsph, dermosphenotic; Exs 1, 2, extrascapular, 1, 2; Fr, frontal;  
Cladistic analysis of the relationships of the Tarrasiids (Lower carboniferous actinopterygians)

September 2002

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286 Reads

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28 Citations

Journal of Verterbrate Paleontology

Revised diagnoses of the family Tarrasiidae and of Tarrasius (Visean of Scotland) and Paratarrasius (Namurian of North America) are presented. These are used in a phylogenetic analysis also comprising one theoretical outgroup, three sarcopterygians as part of the outgroup, and eleven Palaeozoic, Triassic, and Recent actinopterygians, and based on a matrix of 75 characters of head and body. The results are that: (1) Polypterus is the sister group of the other Actinopterygii (= Actinopteri): (2) the analysed Actinopteri are a monophyletic group (Palaeoniscimorpha): and (3) Tarrasiids are monophyletic and are the sister group of the other analysed Actinopteri. This scheme supports the most recent studies in indicating that Tarrasiidae are close to stem actinopterygians.


FIGURE 1. A-C, Tarrasius problematicus. A, reconstruction of the cheek, after Taverne (1996); B, reconstruction of the skull roof, slightly modified after Taverne (1996); C, recontruction of the whole fish: after Taverne (1996) for the skull, and after Jessen (1973) for the body. D-F, Paratarrasius hibbardi. D, reconstruction of the cheek slightly modified after Lund and Melton (1982); E, reconstruction of the skull roof after Lund and Melton (1982); F, reconstruction of the whole fish with scale rows, a scaled area indicated on the flank. Abbreviations: Ang, angular; Ant, antorbital; Aop, anteopercle; ceth, ethmoidal commissure; Cl, cleithrum; Cla, clavicle; cmd, mandibular canal; cpop, preopercle canal; cst, supratemporal commissure; De, dentary; Dhy, dermohyal; Dpt, dermopterotic; Dsph, dermosphenotic; Exs 1, 2, extrascapular, 1, 2; Fr, frontal;
Cladistic analysis of the relationships of the tarasiids (Lower Carboniferous actinopterygians) from the Bear Gulch Limestone of Montana (USA, Lower Carboniferous). –

September 2002

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288 Reads

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21 Citations

Journal of Verterbrate Paleontology

Revised diagnoses of the family Tarrasiidae and of Tarrasius (Visean of Scotland) and Paratarrasius (Namurian of North America) are presented. These are used in a phylogenetic analysis also comprising one theoretical outgroup, three sarcopterygians as part of the outgroup, and eleven Palaeozoic, Triassic, and Recent actinopterygians, and based on a matrix of 75 characters of head and body. The results are that: (1) Polypterus is the sister group of the other Actinopterygii (= Actinopteri); (2) the analysed Actinopteri are a monophyletic group (Palaeoniscimorpha); and (3) Tarrasiids are monophyletic and are the sister group of the other analysed Actinopteri. This scheme supports the most recent studies in indicating that Tarrasiidae are close to stem actinopterygians.


Le genre Bourbonnella (Actinopterygii, Aeduellidae) : révision et description d'une nouvelle espèce du Stéphanien (Carbonifère supérieur) de Montceau-les-Mines (Massif Central, France)

October 2001

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71 Reads

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21 Citations

Annales de Paléontologie

The genusBourbonnella(Actinopterygii, Aeduellidae): revision and description of a new species from the Stephanian (Upper Carboniferous) of Montceau-les-Mines (Massif Central, France). After a revision of the diagnosis of the family Aeduellidae, the previously known species of the genus Bourbonnella have been briefly recorded from a systematic point of view with, in particular, a reappraisial of their diagnoses and, consequently, that of the genus: B. guilloti, type species from the Autunian of Buxières-les-Mines, B. sottyi from the Stephanian of Montceau-les-Mines (both from Massif Central) and B. sp. indet. from the Virgilian (= Stephanian) of New Mexico (USA). An other undetermined Autunian species from Germany is finally attributed to the genus Aeduella. Bourbonnella fourrieri n. sp., from a new fossiliferous Stephanian level of Montceau-les-Mines, is described. It differs from the three other species by its deeper body, the greater area of small scales supporting the dorsal fin, the proportions of the head in regards to the body and the meristics of fin rays. Its scales are devoid of dentine. According to our present knowledge, Bourbonnella seems to be a euryhaline, equatorial and tropical genus at the Carboniferous - Permian turnover.


Un Myxinoı̈de (Craniata, Hyperotreti) dans le Konservat-Lagerstätte Carbonifère supérieur de Montceau-les-Mines (Allier, France)

March 2001

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82 Reads

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31 Citations

Comptes Rendus de l Académie des Sciences - Series IIA - Earth and Planetary Science

Several fossils from the Late Carboniferous of Montceau-les-Mines, France, are referred to a new taxon of fossil hagfish. Two specimens display impressions of two pairs of tooth rows that are strikingly similar in shape and organization to the horny teeth of modern hagfish. In addition, by its slender body shape, this new taxon is more suggestive of modern hagfish than the only previously known fossil form from the Carboniferous of the USA. Living hagfish being exclusively marine, this discovery raises the question of the reputedly freshwater environment of the Montceau-les-Mines ‘Konservat-Lagerstätte’.


A hagfish (Craniata, Hyperotreti) from the Late Carboniferous Konservat-Lagerstatte of Montceau-les-Mines (Allier, France)

January 2001

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166 Reads

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17 Citations

Comptes Rendus de l Académie des Sciences - Series IIA - Earth and Planetary Science

Several fossils from the Late Carboniferous of Montceau-les-Mines, France, are referred to a new taxon of fossil hagfish. Two specimens display impressions of two pairs of tooth rows that are strikingly similar in shape and organization to the horny teeth of modern hagfish. In addition, by its slender body shape, this new taxon is more suggestive of modern hagfish than the only previously known fossil form from the Carboniferous of the USA. Living hagfish being exclusively marine, this discovery raises the question of the reputedly freshwater environment of the Montceau-les-Mines 'Konservat-Lagerstätte'. © 2001 Académie des sciences / Éditions scientifiques et médicales Elsevier SAS.


Two New Deep-Bodied Palaeoniscoid Actinopterygians from Bear Gulch (Montana, USA, Lower Carboniferous)

September 2000

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234 Reads

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42 Citations

Two new species of deep-bodied Paleozoic actinopterygians, Aesopichthys erinaceus gen. nov., sp. nov. and Proceramala montanensis gen. nov., sp. nov., are described from the Upper Chesterian, Upper Mississippian (Namurian E2b, Lower Carboniferous) Bear Gulch Limestone of Montana, USA, and the new family Aesopichthyidae is erected for them. These two fishes share features usually associated with deep body and deep head specializations, particularly in Palaeoniscimorpha, such as a shortened gape, tall maxilla, vertical Suspensorium, deepened flank scales and an elongate dorsal fin. Aesopichthys in particular, for which more complete information is known, also possessed a suite of very specialized adaptations in feeding mechanism, ganoine sculpturing, fin form, and cranial defensive structures that have strong ethological implications. These features include small mobile premaxillae, a spinous and apparently rotatable posteroventral infraorbital, lobed pectoral base, and partially webbed pectoral, dorsal, anal and caudal fins.Within a general scheme of interrelationships of primitive actinopterygians, these two new taxa pertain to Palaeoniscimorpha, i.e., basal Actinopteri. Then, from a cladistic analysis limited, beside these two new taxa, to Wendyiehthys and Cyranorhis (two other already described actinopterygians from Bear Gulch), Platysomus, and Cheirolepis, it appears that the Aesopichthyidae display no close relationship to the Platysomidae but should be the sister group of the Rhadinichthyid-group i.e., [Cyranorhis + [Rhadinichthyidae + Wendyiehthys]].


Citations (16)


... The late Paleozoic (359.3-251.9 million years ago (mya) (Aretz et al., 2020;Henderson, Dunne, & Fasey, 2022)) represents an important interval for understanding the evolution and diversification of actinopterygians, the ray-finned fishes. During this time, rayfinned fishes first evolved a series of innovations that have arisen many times since, including body elongation (Lund & Poplin, 2002), body deepening (Gill, 1925;Sallan & Coates, 2013), and various changes to feeding ranging from adaptations for durophagy to changes in jaw articulation (Argyriou et al., 2022). Despite the important morphological innovations taking place in the Carboniferous-Permian interval, few ray-finned fishes of this age have been studied in detail (Argyriou et al., 2022;Figueroa et al., 2019), suggesting that many additional functional innovations remain unrecognized. ...

Reference:

Fitting fangs in a finite face: A novel fang accommodation strategy in a 280 million-year-old ray-finned fish
Cladistic analysis of the relationships of the Tarrasiids (Lower carboniferous actinopterygians)

Journal of Verterbrate Paleontology

... The first indisputable fossil hagfish to be discovered was Myxinikela siroka, which was found in the same geological horizon and general locality as the lamprey M. pieckoensis, and thus likewise dates back c. 300 mya (Bardack 1991(Bardack , 1998. More recently, another hagfish fossil, Myxineidus gononorum, was discovered in upper Carboniferous deposits in France and is therefore also of approximately the same age as the above two fossils (Poplin et al. 2001). Germain et al. (2014) have cast doubt, however, on whether M. gononorum is a hagfish and provide evidence that it could be a lamprey. ...

A hagfish (Craniata, Hyperotreti) from the Late Carboniferous Konservat-Lagerstatte of Montceau-les-Mines (Allier, France)

Comptes Rendus de l Académie des Sciences - Series IIA - Earth and Planetary Science

... As before, many diverse and scattered records of Carboniferous tetrapod footprints continued to be documented during the last 40 plus years, mostly from North America and Europe (e.g., Jake and Blake, 1982;Mietto et al., 1985;McClelland, 1988;Turek, 1989;Lane and Maples, 1990;Reisz, 1990;Martino, 1991;Schneider et al., 1992;Milner, 1994;Lockley and Hunt, 1995;Scarboro and Tucker, 1995;Grantham, 1996, 2000;Blieck et al., 1997;Soler-Gijón and Moratalla, 2001;Calder et al., 2004;Falcon-Lang et al., 2004Voigt et al., 2011;Fillmore et al., 2015;Nied zwiedzki, 2015;Schöllmann et al., 2015;Meade et al., 2016;Bird et al., 2019;Marchetti et al., 2018Marchetti et al., , 2020bWeems and Lucas, 2020;Matamales-Andreu et al., 2021;Soler-Gijón and Díez Ruiz, 2023). Kuhn (1963) and Haubold (1971Haubold ( , 1984 published the first synthetic compilations of the tetrapod footprint record, which, of course, included the Carboniferous tetrapod footprints. ...

Paleozoic vertebrates of the Alps: a review.

Bulletin de la Societe Geologique de France

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[...]

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... Lower actinopterygian skull bones have been identified differently by various researchers (See Moy- Thomas & Bradley Dyne, 1938;Rayner, 1951;Pearson & Westoll, 1979;Gardiner, 1984;Long, 1988;Arratia & Cloutier, 1996;Poplin & Lund, 2002 for examples of different identifications and names of bones of the snout, and Mickle, 2015 for a review of terminology schemes). Here, the bones of the snout are identified following the criteria presented by Mickle (2012); Mickle (2015). ...

Cladistic analysis of the relationships of the tarasiids (Lower Carboniferous actinopterygians) from the Bear Gulch Limestone of Montana (USA, Lower Carboniferous). –

Journal of Verterbrate Paleontology

... Furthermore, the simplexodont form of plicidentine is present at the base of the marginal teeth, which is now known to be widely distributed among the various actinopterygian forms (see Viviani et al. 2022 for the recent summary), although not necessarily confined to them (Meunier et al. 2015b). The marginal teeth arranged in two series have been interpreted to represent a plesiomorphic condition for the actinopterygians, with the large, cone-like teeth placed medially in respect to the diminutive lateral dentition (Poplin and Heyler 1993;Lund and Poplin 1997). Although this characteristic indeed frequently occurs in the Palaeozoic forms, the presence of a single marginal tooth row present in S. macrodens gen. ...

The rhadinichthyids (paleoniscoid actinopterygians) from the Bear Gulch Limestone of Montana (USA, Lower Carboniferous)

... Furthermore, Harris and Lucas (2017) reported a gigantic actinopterygian fish from the Kasimovian, Upper Pennsylvanian black shale deposits of the Tinajas Member, Atrasado Formation in New Mexico, USA, which has been interpreted as deposited in a large freshwater lake with an anoxic bottom (Lerner et al. 2009). The comparison to the other upper Carboniferous localities historically considered to represent limnic freshwater environments, and containing well-documented actinopterygian faunas, is difficult, mainly because many of them have recently been argued to be marine-connected (e.g., Mazon Creek; Clements et al. 2018), or their marine influence is being debated (e.g., Montceau-les-Mines: Poplin et al. 2001;Charbonnier et al. 2008;Schultze 2009;Mickle 2011;Perrier and Charbonnier 2014;Puertollano Basin: Jiménez et al. 1999;Soler-Gijón and Moratalla 2001;Schultze 2009;Fisher et al. 2013;Soler-Gijón and Díez Ruiz 2023). However, the Mazon Creek and Montceau-les-Mines appear to lack large-bodied actinopterygians in their assemblages, whereas in Puertollano Basin, Spain, the remains of Progyrolepis speciosus have recently been uncovered in sediments assumed to represent the estuarine-deltaic environment, indicating potentially euryhaline adaptations of this species (Soler-Gijón and Díez Ruiz 2023). ...

Un Myxinoı̈de (Craniata, Hyperotreti) dans le Konservat-Lagerstätte Carbonifère supérieur de Montceau-les-Mines (Allier, France)
  • Citing Article
  • March 2001

Comptes Rendus de l Académie des Sciences - Series IIA - Earth and Planetary Science

... Here, we treat Glencartholm as a single locality due to the occurrence of most fossils at the Macconochie site which has uncertain stratigraphy [40]. Second, the same horizon may outcrop at multiple localities, for example at Bear Gulch, where multiple locations are known within a confined local area [41]. Here, we treat these separate outcrops as separate localities with consistent stratigraphic information. ...

Fish diversity of the Bear Gulch Limestone, Namurian, Lower Carboniferous of Montana, USA

Geobios

... Other matrices focus on a particular fauna or geographic region. Most notable amongst these are efforts to investigate the relationships of Bear Gulch actinopterygians, which include limited taxa from outside this deposit (Lund, Poplin & McCarthy, 1995;Lund, 2000;Fig. 9). ...

Preliminary analysis of the interrelationships of some Paleozoic Actinopterygii

Geobios

... Nevertheless, elasmoid scales are also known to occur among extinct taxa and, in these cases, the basal plate is generally fully mineralised. Fossil osteichthyans with rounded scales that match the elasmoid type include both actinopterygians (e.g. the amiid Amia robusta, Meunier and Poplin 1995 Zylberberg et al. 2010). The mineralised basal plate of these taxa represents the primitive state from which the unmineralised condition of their closely related extant forms (e.g. ...

Paleohistological study of the scales of Amia Robusta Priem, 1901, Amiidae from the Thanetian (Paleocene) of Cernay (France)
  • Citing Article
  • December 1995

Geobios

... On the contrary, the shape of the suboperculum, very deep scales on the lateral side of the body and the scale count clearly separate specimens from the Otovice Limestone from Bourbonnella hirsuta and whole genus Bourbonnella (Heyler 1969, Poplin 2001, Poplin and Dutheil 2005, Štamberg 2007). It is obvious that the studied specimens from the Otovice Limestone belong to a new genus of Aeduellidae which possess a mix of features characterizing the genera Aeduella and Bourbonnella. ...

Le genre Bourbonnella (Actinopterygii, Aeduellidae) : révision et description d'une nouvelle espèce du Stéphanien (Carbonifère supérieur) de Montceau-les-Mines (Massif Central, France)
  • Citing Article
  • October 2001

Annales de Paléontologie