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1

Vinn, Olev, and Ursula Toom. "New cornulitid from the Ohesaare Formation (late Pŕidoli) of Saaremaa, Estonia." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 298, no. 1 (2020): 67–73. http://dx.doi.org/10.1127/njgpa/2020/0934.

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A new cornulitid species Cornulites baranovi sp. nov. is described from the Ohesaare Formation (late Přidoli) of Saaremaa, Estonia. The new species exhibits straight to slightly curved tubes that expand moderately in diameter, a vesicular tube structure and strong annular crests and costae. In addition to C. baranovi sp. nov., Conchicolites sp. also occurs in the Ohesaare Formation. The diversity of cornulitids is low in the Přidoli of Estonia, but not lower than in the Silurian of Estonia in general. C. baranovi often forms a symbiotic association with the bryozoan Fistulipora. It is not sure
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2

Dixon, Owen A. "Endobiotic cornulitids in Upper Ordovician tabulate corals and stromatoporoids from Anticosti Island, Quebec." Journal of Paleontology 84, no. 3 (2010): 518–28. http://dx.doi.org/10.1666/09-129.1.

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Conoidal shells of Cornulites celatus n. sp. occur commonly within host coralla of Propora conferta Milne-Edwards and Haime, 1851, sensu lato, from the Laframboise Member of the Ellis Bay Formation (Ashgill: Upper Ordovician) at Pointe Laframboise on western Anticosti Island. Examples have also been found at the same locality in the tabulate corals Paleofavosites sp., Acidolites arctatus Dixon, 1986, and A. compactus Dixon, 1986, and the stromatoporoid Ecclimadictyon sp., but not in other associated tabulate coral species. Growth interference between the shells and their hosts indicates a comm
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3

Tetreault, Denis K. "Paleoecologic implications of epibionts on the Silurian lichid trilobite Arctinurus." Paleontological Society Special Publications 6 (1992): 289. http://dx.doi.org/10.1017/s2475262200008492.

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The Wenlockian lichid trilobite Arctinurus boltoni has been regarded as a classic example of a “snow-shoe” type adaptation. That is, the broad flat doublure has been interpreted as a resting surface, with well-developed terrace ridges serving as either sensory or frictional devices. New data from the Rochester Shale of western New York State indicate that this interpretation is incorrect The discovery of the small, calcareous worm tube Cornulites on complete, articulated specimens of Arctinurus indicates that these trilobites seldom rested their doublure on the sediment surface. Apertures of a
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4

Vinn, Olev, and Jaap Eyzenga. "When did spines appear in cornulitids – a new spiny Cornulites from the Upper Ordovician of Baltica." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 299, no. 1 (2021): 99–105. http://dx.doi.org/10.1127/njgpa/2021/0957.

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5

Комаров, В. Н., А. А. Измайлова, Д. А. Головастов та Е. И. Гончарова. "Микрокосм девонских микроконхид и корнулитид Закавказья, "Природа"". Priroda, № 7 (2021): 47–54. http://dx.doi.org/10.7868/s0032874x2107005x.

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Приведены данные о первых находках микроконхид и корнулитид на раковинах брахиопод-атрипид из девонских отложений Закавказья в интервале от эмсского до франского яруса включительно. Эпибионты, представленные гладкими спирально свернутыми трубчатыми раковинами рода Palaeconchus и прямыми трубчатыми раковинами рода Cornulites, примерно в равных пропорциях обнаружены как на брюшных, так и на спинных створках брахиопод. Прикрепление изученных Palaeconchus, скорее всего, происходило посмертно. В пользу этого вывода свидетельствует отсутствие правильности в их размещении. Гирляндный характер нараста
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6

Herringshaw, Liam G., Alan T. Thomas, and M. Paul Smith. "Systematics, shell structure and affinities of the Palaeozoic Problematicum Cornulites." Zoological Journal of the Linnean Society 150, no. 4 (2007): 681–99. https://doi.org/10.1111/j.1096-3642.2007.00300.x.

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Herringshaw, Liam G., Thomas, Alan T., Smith, M. Paul (2007): Systematics, shell structure and affinities of the Palaeozoic Problematicum Cornulites. Zoological Journal of the Linnean Society 150 (4): 681-699, DOI: 10.1111/j.1096-3642.2007.00300.x, URL: https://academic.oup.com/zoolinnean/article-lookup/doi/10.1111/j.1096-3642.2007.00300.x
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7

HERRINGSHAW, LIAM G., ALAN T. THOMAS, and M. PAUL SMITH. "Systematics, shell structure and affinities of the Palaeozoic Problematicum Cornulites." Zoological Journal of the Linnean Society 150, no. 4 (2007): 681–99. http://dx.doi.org/10.1111/j.1096-3642.2007.00300.x.

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8

Vinn, Olev, and Mark A. Wilson. "Endosymbiotic Cornulites in the Sheinwoodian (Early Silurian) stromatoporoids of Saaremaa, Estonia." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 257, no. 1 (2010): 13–22. http://dx.doi.org/10.1127/0077-7749/2010/0048.

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9

Peters, Shanan E., and Kennard B. Bork. "Secondary tiering on crinoids from the Waldron Shale (Silurian: Wenlockian) of Indiana." Journal of Paleontology 72, no. 5 (1998): 887–94. http://dx.doi.org/10.1017/s0022336000027219.

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Superbly preserved specimens of Eucalyptocrinites tuberculatus from the Waldron Shale (Silurian, Wenlockian) of Indiana have been found with epibionts attached in living position to their stems. The rhynchonellid brachiopod Stegerhynchus indianense, the tabulate coral Favosites forbesi, the annelids? Spirorbis and Cornulites, bryozoans, and rarely the ichnogenus Tremichnus utilized living crinoids as secondary tiering surfaces. Crinozoans also attached to upright crinoid columns, and their holdfasts are the most abundant epibionts on pluricolumnals. Eucalyptocrinites crassus individuals contri
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10

Mitchell, Charles E., Mark A. Wilson, and James M. St. John. "In situ crustoid graptolite colonies from an Upper Ordovician hardground, southwestern Ohio." Journal of Paleontology 67, no. 6 (1993): 1011–16. http://dx.doi.org/10.1017/s0022336000025336.

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In situ colonies of Bulmanicrusta? sp. encrusting the surface of a hardground from the Upper Ordovician Bull Fork Formation provide the first glimpse of the full colony form, habitat, and faunal associates of a crustoid graptolite. Bulmanicrusta? sp. exhibits a runner-type colony form suited to rapid expansion over hard substrates, indicating it was an opportunistic member of the hardground community. This community also included two bryozoans (“Proboscina” and Amplexopora), Cornulites, and crinoids. The Bulmanicrusta? sp. specimens contain numerous graptoblasts (small, thick-walled vesicles)
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11

Morris, Robert W., and Stephen H. Felton. "Symbiotic Association of Crinoids, Platyceratid Gastropods, and Cornulites in the Upper Ordovician (Cincinnatian) of the Cincinnati, Ohio Region." PALAIOS 8, no. 5 (1993): 465. http://dx.doi.org/10.2307/3515020.

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12

MORRIS, R. W., and S. H. FELTON. "Paleoecologic Associations and Secondary Tiering of Cornulites on Crinoids and Bivalves in the Upper Ordovician (Cincinnatian) of Southwestern Ohio, Southeastern Indiana, and Northern Kentucky." PALAIOS 18, no. 6 (2003): 546–58. http://dx.doi.org/10.1669/0883-1351(2003)018<0546:paasto>2.0.co;2.

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13

VINN, Olev, and Mark A. WILSON. "Silurian cornulitids of Estonia (Baltica)." Carnets de géologie (Notebooks on geology), Articles (December 25, 2013): 357–68. http://dx.doi.org/10.4267/2042/53034.

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14

Vinn, Olev. "Attempted predation on Early Paleozoic cornulitids." Palaeogeography, Palaeoclimatology, Palaeoecology 273, no. 1-2 (2009): 87–91. http://dx.doi.org/10.1016/j.palaeo.2008.12.004.

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15

VINN, Olev. "Cornulitid tubeworms from the Ordovician of eastern Baltic." Carnets de géologie (Notebooks on geology), Lettres (July 2013): 131–38. http://dx.doi.org/10.4267/2042/51214.

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16

Key, Marcus M., Gregory A. Schumacher, Loren E. Babcock, et al. "Paleoecology of commensal epizoans fouling Flexicalymene (Trilobita) from the Upper Ordovician, Cincinnati Arch region, USA." Journal of Paleontology 84, no. 6 (2010): 1121–34. http://dx.doi.org/10.1666/10-018.1.

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Commensal epizoozoans and episkeletozoans are rarely preserved attached to the external exoskeleton of the Late Ordovician trilobite Flexicalymene. Of nearly 15,000 Flexicalymene specimens examined, 0.1% show epizoozoans or episkeletozoans. Factors limiting Flexicalymene fouling include a shallow burrowing life style, frequent molting of the host, larval preference for other substrates, observational bias caused by overlooking small fouling organisms, and the loss of the non-calcified, outermost cuticle prior to fossilization or as the trilobite weathers from the encasing sediment. Trepostome
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17

Vinn, Olev. "A new spiny cornulitid from the Silurian of Gotland, Sweden." GFF 126, no. 3 (2004): 297–99. http://dx.doi.org/10.1080/11035890401263297.

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18

Vinn, Olev. "A new cornulitid genus from the Silurian of Gotland, Sweden." GFF 127, no. 3 (2005): 205–10. http://dx.doi.org/10.1080/11035890501273205.

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19

Gutiérrez-Marco, Juan Carlos, and Olev Vinn. "Cornulitids (tubeworms) from the Late Ordovician Hirnantia fauna of Morocco." Journal of African Earth Sciences 137 (January 2018): 61–68. http://dx.doi.org/10.1016/j.jafrearsci.2017.10.005.

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20

Cohen, David Bruce. "Lipschitz 1-connectedness for Some Solvable Lie Groups." Canadian Journal of Mathematics 71, no. 03 (2019): 533–55. http://dx.doi.org/10.4153/cjm-2017-038-8.

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AbstractA space X is said to be Lipschitz 1-connected if every Lipschitz loop 𝛾 : S 1 → X bounds a O (Lip(𝛾))-Lipschitz disk f : D 2 → X. A Lipschitz 1-connected space admits a quadratic isoperimetric inequality, but it is unknown whether the converse is true. Cornulier and Tessera showed that certain solvable Lie groups have quadratic isoperimetric inequalities, and we extend their result to show that these groups are Lipschitz 1-connected.
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21

GARFITT, J. S. T. "Review. Cornulier, Benoit de, Theorie du vers. Rimbaud, Verlaine, Mallarme." French Studies 40, no. 1 (1986): 98. http://dx.doi.org/10.1093/fs/40.1.98.

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22

Vinn, Olev, Sabiela Musabelliu, and Michał Zatoń. "Cornulitids from the Upper Devonian of the Central Devonian Field, Russia." GFF 141, no. 1 (2018): 68–76. http://dx.doi.org/10.1080/11035897.2018.1505777.

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23

Richter, Mario. "Benoît de Cornulier, De la métrique à l’interprétation. Essais sur Rimbaud." Studi Francesi, no. 162 (LIV | III) (November 1, 2010): 575–76. http://dx.doi.org/10.4000/studifrancesi.6376.

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24

VINN, OLEV, ANDREJ ERNST, and URSULA TOOM. "SYMBIOSIS OF CORNULITIDS AND BRYOZOANS IN THE LATE ORDOVICIAN OF ESTONIA (BALTICA)." PALAIOS 33, no. 7 (2018): 290–95. http://dx.doi.org/10.2110/palo.2018.018.

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25

Musabelliu, Sabiela, and Michał Zatoń. "Patterns of cornulitid encrustation on the Late Devonian brachiopod shells from Russia." Proceedings of the Geologists' Association 129, no. 2 (2018): 227–34. http://dx.doi.org/10.1016/j.pgeola.2018.03.009.

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26

Pallier, Gabriel. "LARGE-SCALE SUBLINEARLY LIPSCHITZ GEOMETRY OF HYPERBOLIC SPACES." Journal of the Institute of Mathematics of Jussieu 19, no. 6 (2018): 1831–76. http://dx.doi.org/10.1017/s1474748018000567.

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Large-scale sublinearly Lipschitz maps have been introduced by Yves Cornulier in order to precisely state his theorems about asymptotic cones of Lie groups. In particular, Sublinearly bi-Lipschitz Equivalences (SBE) are a weak variant of quasi-isometries, with the only requirement of still inducing bi-Lipschitz maps at the level of asymptotic cones. We focus here on hyperbolic metric spaces and study properties of boundary extensions of SBEs, reminiscent of quasi-Möbius (or quasisymmetric) mappings. We give a dimensional invariant of the boundary that allows to distinguish hyperbolic symmetric
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27

Lebas, Franck. "Entre noms communs et noms propres : papa, maman, bébé." Romanica Wratislaviensia 69 (November 28, 2022): 53–64. http://dx.doi.org/10.19195/0557-2665.69.5.

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The difficulties in classifying family names such as dad, mum, uncle, son, etc., as proper names or common names take on a new dimension if we integrate certain uses of undetermined common names such as baby (ex: If mom is okay, baby is okay). The main objective of this article is to use these examples to bring about some changes in the theories of proper names and common names. Starting from Alan Gardiner’s proposal, which gives a central role to proper names’ signifiers, and adding the concept of “validity sphere” inspired by Benoît de Cornulier, this work lays the foundations of a unified d
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28

Dominicy, Marc. "On the Meter and Prosody of French 12-Syllable Verse." Empirical Studies of the Arts 10, no. 2 (1992): 157–81. http://dx.doi.org/10.2190/570b-ark0-6mm7-jp7h.

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This article provides the reader with a survey of the basic metrical and prosodic properties of the French classical and post-classical 12-syllable alexandrine line. It is argued that these features can be captured within a neo-Jakobsonian framework which maintains a clear distinction between linguistic and non-linguistic parallelisms. Metrical equivalence is accounted for by positing abstract “line designs” that are linked to “line instances” by a set of “matching rules.” The versification of Racine, Hugo, and late Nineteenth-century poets of the Parnassian and post-Parnassian generations is
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29

Tapanila, Leif, and Jan Ove R. Ebbestad. "Benthic island community on the back of a snail: Silurian, Anticosti Island, CanadaThis article is one of a series of papers published in this Special Issue on the theme The dynamic reef and shelly communities of the Paleozoic. This Special is in honour of our colleague and friend Paul Copper." Canadian Journal of Earth Sciences 45, no. 2 (2008): 203–11. http://dx.doi.org/10.1139/e07-054.

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A single specimen of the large Silurian gastropod Phanerotrema sp. from the Goéland Member on Anticosti Island preserves an outstanding microcosm of its surrounding community, including multiple trophic groups, strategies for niche partitioning, and innovative adaptations for survival in a mud-dominated marine ecosystem. At least seven associations are recorded in this fossil specimen, including the gastropod itself, healed breakage from an apparently failed attempt at durophagous predation, domichnial bioerosion, encrustation by a stromatoporoid, nestling behaviour and commensal embedment by
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30

Vinn, Olev. "Shell microstructure ofCornulitessemiapertusÖpik, 1930 and other early cornulitids from the Ordovician of North Estonia." GFF 132, no. 2 (2010): 129–32. http://dx.doi.org/10.1080/11035897.2010.483309.

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31

Vinn, Olev, and Mari-Ann Mõtus. "New endobiotic cornulitid andCornulitessp. aff.Cornulitescelatus(Cornulitida, Tentaculita) from the Katian of Vormsi Island, Estonia." GFF 134, no. 1 (2012): 3–6. http://dx.doi.org/10.1080/11035897.2011.647067.

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32

Vinn, Olev, Andrej Ernst, Mark A. Wilson, and Ursula Toom. "Symbiosis of cornulitids with the cystoporate bryozoan Fistulipora in the Pridoli of Saaremaa, Estonia." Lethaia 54, no. 1 (2020): 90–95. http://dx.doi.org/10.1111/let.12385.

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33

Zhan, R., and O. Vinn. "Cornulitid epibionts on brachiopod shells from the Late Ordovician (middle Ashgill) of East China." Estonian Journal of Earth Sciences 56, no. 2 (2007): 101. http://dx.doi.org/10.3176/earth.2007.13.

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34

Raffi, Maria Emanuela. "Benoît de Cornulier, La musique n’est pas dans les paroles: exemples de Verlaine, Baudelaire, Fuzelier." Studi Francesi, no. 178 (LX | I) (April 1, 2016): 146. http://dx.doi.org/10.4000/studifrancesi.2534.

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35

Vinn, O., U. Toom, and M. Isakar. "The earliest cornulitid on the internal surface of the illaenid pygidium from the Middle Ordovician of Estonia." Estonian Journal of Earth Sciences 66, no. 4 (2017): 193. http://dx.doi.org/10.3176/earth.2017.19.

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36

VINN, OLEV, and HARRY MUTVEI. "OBSERVATIONS ON THE MORPHOLOGY AND AFFINITIES OF CORNULITIDS FROM THE ORDOVICIAN OF ANTICOSTI ISLAND AND THE SILURIAN OF GOTLAND." Journal of Paleontology 79, no. 4 (2005): 726–37. http://dx.doi.org/10.1666/0022-3360(2005)079[0726:ootmaa]2.0.co;2.

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37

Larcher, Pierre. "La dérivation délocutive." Historiographia Linguistica 30, no. 3 (2003): 389–406. http://dx.doi.org/10.1075/hl.30.3.06lar.

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Summary The notion ‘delocutive derivation’ was introduced by Emile Benveniste (1902–1976) in a paper published in 1958. It appears to have gone unnoticed at the time. However, when the article was reissued in Benveniste’s Problèmes de linguistique générale (1966), things seem to have changed dramatically, in particular in 1972, when Ducrot made a connection between ‘delocutivity’ and ‘performativity’ (e.g., promettre = dire je promets), leading in 1975 delocutivity back to the side of a semantic reinterpretation (e.g., je trouve que). Subsequently, Cornulier (1976) introduced the concept of ‘a
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38

Shankavaram, Varun, Dean Shah, Aseel Alashqar, Jackson Sweeney, and Hilal Arnouk. "Cornulin as a Key Diagnostic and Prognostic Biomarker in Cancers of the Squamous Epithelium." Genes 15, no. 9 (2024): 1122. http://dx.doi.org/10.3390/genes15091122.

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The prevalence of squamous cell carcinoma is increasing, and efforts that aid in an early and accurate diagnosis are crucial to improve clinical outcomes for patients. Cornulin, a squamous epithelium-specific protein, has recently garnered attention due to its implications in the progression of squamous cell carcinoma developed in several tissues. As an epidermal differentiation marker, it is involved in skin anchoring, regulating cellular proliferation, and is a putative tumor suppressor. The physiologically healthy squamous epithelium displays a considerable level of Cornulin, whereas squamo
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39

Lebold, Joseph G. "Quantitative analysis of epizoans on Silurian stromatoporoids within the Brassfield Formation." Journal of Paleontology 74, no. 3 (2000): 394–403. http://dx.doi.org/10.1017/s002233600003167x.

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Stromatoporoids from the Brassfield Formation (Early Silurian, Llandovery) near Fairborn, Ohio, provided substrata for a diverse epizoic community. The stromatoporoids were colonized by at least 28 taxa, including bryozoans, cnidarians, echinoderms, annelids, and endolithic organisms. Analysis of the occurrence, diversity, distribution, and coverage of the epizoans recognized patterns of site-selective attachment on the surface of the stromatoporoids.The upper surface of the stromatoporoids had a slightly higher total epizoan coverage than the lower surface. Concentric zones outlined from the
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40

PENSOM, ROGER. "Accent et syllabe dans les vers français: une synthèse possible?" Journal of French Language Studies 19, no. 3 (2009): 335–61. http://dx.doi.org/10.1017/s0959269509990032.

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RESUMESelon certains critiques influents, l'équivalence métrique repose uniquement sur des équivalences en nombre syllabique, la division en unités rythmiques et la disposition interne des accents restant ‘libres’, c'est -à-dire indifférentes au mètre. A l'encontre de cette vue, depuis 1800, bon nombre d'amateurs et poètes ont discerné dans les vers français l'opération d'un principe formel fondé sur la répartition des accents au sein du vers. Suite à des travaux récents qui constatent la présence d'une occurrence statistiquement significative de répartitions d'accents régulières dans un vaste
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41

Κόκκινος, Δημήτρης Εμμανουήλ, та Ανθούλα Κολιάδη-Τηλιακού. "Ρυθμός και μουσικότητα στα προφορικά παιδικά ποιήματα και τραγούδια. Από το πλαίσιο της άτυπης εκπαίδευσης σε σύγχρονες διδακτικές προεκτάσεις." Preschool and Primary Education 11, № 2 (2023): 262–83. http://dx.doi.org/10.12681/ppej.31665.

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Τα παιδικά ποιήματα/τραγούδια της λαϊκής προφορικής παράδοσης αποτελούν μία μορφή διαχρονικής και οικουμενικής πολιτισμικής δημιουργίας που απασχολεί, εκτός από τους τομείς της εθνογραφικής έρευνας και των λαογραφικών σπουδών, κι εκείνους της παιδαγωγικής επιστήμης, της γλωσσολογίας και της μουσικολογίας. Η παρούσα μελέτη, βασιζόμενη σε ευρήματα της βιβλιογραφικής επισκόπησης, εστιάζει το ενδιαφέρον της στη σημασία και τον ρόλο που παίζει ο ρυθμός ως πρωτογενές στοιχείο των παιδικών ποιημάτων/τραγουδιών της λαϊκής προφορικής παράδοσης. Τα πορίσματα της μελέτης μέσα από παραδείγματα διαφορετικώ
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42

Lescinsky, Halard L. "Epibiont communities: Recruitment and competition on North American Carboniferous brachiopods." Journal of Paleontology 71, no. 1 (1997): 34–53. http://dx.doi.org/10.1017/s0022336000038932.

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Shell-encrusting assemblages have uniquely high ecological fidelity among paleocommunities because adjacent epibionts coexisted in ecological time, and the abundances and spatial relationships of the various members are accurately preserved. This study presents a quantitative reconstruction of communities on brachiopod shells (Composita and alate spirifers) from the Carboniferous of North America. Thirty-one epibiont communities, comprised of a total of 1180 encrusted brachiopods, are analyzed in terms of epibiont abundance (e.g., percent areal cover), ecological diversity (e.g., Shannon-Wiene
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43

Tsinkoburova, Maria, and Aleksandr Kuznetsov. "ON THE PALEOECOLOGICAL VALUE OF THE COLLECTIONS OF LOWER FRASNIAN INVERTEBRATES OF THE MAIN DEVONIANFIELD IN THE MINING MUSEUM." LIFE OF THE EARTH 46, no. 1 (2024): 60–72. http://dx.doi.org/10.29003/m3774.0514-7468.2024_46_1/60-72.

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The article describes two groups of facies most widely represented in the collections of Lower Frasnian invertebrates of the Main Devonian Field in the Mining Museum (hardgrounds and pelecypod banks). The presence of three types of hardgrounds has been established, differing in the nature of the original bottom and the time of exposure of each hardground, and hence structural and textural features of rocks and systematic composition of oryctocenoses. The first type is crinoidal limestone with an extensive complex of sclerobionts and traces of bioerosion by Trypanites Mägdefrau, an uneven surfa
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44

Rizza, Cecilia. "Jean-Pierre Chauveau, Des «Plaintes d’Acante» aux «Amours» de Tristan l’Hermite: quelques réflexions sur l’organisation du Canzoniere tristanien in Le sens et la mesure. Hommages à Benoît de Cornulier." Studi Francesi, no. 143 (XLVIII | II) (December 1, 2004): 358. http://dx.doi.org/10.4000/studifrancesi.39232.

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45

Vinn, Olev, Anna Madison, Mark A. Wilson, and Ursula Toom. "Cornulitid tubeworms and other calcareous tubicolous organisms from the Hirmuse Formation (Katian, Upper Ordovician) of northern Estonia." Journal of Paleontology, December 5, 2022, 1–9. http://dx.doi.org/10.1017/jpa.2022.89.

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Abstract Seven species of cornulitids, one unidentified tubicolous shell, and the problematic bryozoan Lagenosypho Spandel, 1898 are here described from the Katian of Baltica. Three new species—Cornulites lindae new species, Cornulites meidlai new species, and Conchicolites kroegeri new species—are described. The unidentified tubicolous organism has punctate shell structure and setae-like structures that can best be affiliated with lophophorates. The Hirmuse fauna indicates that the diversity and number of cornulitids in the Ordovician of Baltica has been underestimated and it is likely that t
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46

Vinn, Olev, Mark A. Wilson, and Ursula Toom. "A new genus and species of cornulitid tubeworm from the Hirnantian (Late Ordovician) of Estonia." Journal of Paleontology, February 12, 2024, 1–7. http://dx.doi.org/10.1017/jpa.2023.90.

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Abstract A new cornulitid genus and species, Porkuniconchus fragilis new genus and species, is here described from the Ärina Formation (Hirnantian, Porkuni Regional Stage) of northern Estonia. This new taxon differs from most cornulitids by having a fusiform ornamentation pattern that is somewhat similar to that of Kolihaia. All studied specimens are attached to a carbonate hardground. The hardground fauna is by abundance and encrustation area dominated by cornulitids. Other encrusters are represented only by a single sheet-like cystoporate bryozoan. The cornulitid specimens represent differen
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47

Serobyan, Vahram, Taniel Danelian, Catherine Crônier, Araik Grigoryan, and Bernard Mottequin. "New and revised cyrtospiriferid (Spiriferida) brachiopods from the lower Famennian (Upper Devonian) of Armenia." Journal of Paleontology, March 31, 2022, 1–20. http://dx.doi.org/10.1017/jpa.2022.9.

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Abstract The Upper Devonian sedimentary sequences of Central Armenia, which mainly consist of shallow water, mixed carbonate-siliciclastic deposits, contain abundant and diverse brachiopods that are dominated by spiriferides. Based on newly collected material from the lower Famennian Aramazdospirifer orbelianus brachiopod zone (coeval to the Palmatolepis crepida conodont zone) of Armenia, we here introduce two new cyrtospiriferid genera and fully document their type species, including their intraspecific variability. Pentagonospirifer n. gen. is a monospecific genus assigned to the subfamily C
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48

Tsinkoburova, Maria G. "Sclerobionts and some representatives of the endobenthos of soft substrates of the Lower Frasnian of the East of the Main Devonian Field." Vestnik of Saint Petersburg University. Earth Sciences 68, no. 4 (2023). http://dx.doi.org/10.21638/spbu07.2023.403.

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The article considers sclerobionts on the shells of the Frasnian bivalves and brachiopods of the east of the Main Devonian field, as well as common traces of bioerosion of biogenic and abiogenic substrate. In contrast to the averaged data on the Frasnian brachiopod sclerobionts, which demonstrate a clear dominance of auloporids, craniform brachiopods, bryozoas and microconchids, microconchids predominate among Frasnian bivalves sclerobionts and brachiopods of the Main Devonian field and among the eroding sclerobionts — the ichnogenus Arachnostega Bertling. Next in the degree of frequency of oc
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Vinn, O., and J. C. Gutiérez-Marco. "New Late Ordovician cornulitids from Peru." Bulletin of Geosciences, March 17, 2016, 89–95. http://dx.doi.org/10.3140/bull.geosci.1595.

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Vinn, Olev, and Anna Madison. "Cornulitids from the Upper Ordovician of northwestern Russia." Carnets de géologie (Notebooks on geology) 17, no. 12 (2017). http://dx.doi.org/10.4267/2042/64289.

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