Literatura científica selecionada sobre o tema "Cornulites"
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Artigos de revistas sobre o assunto "Cornulites"
Vinn, Olev, e Ursula Toom. "New cornulitid from the Ohesaare Formation (late Pŕidoli) of Saaremaa, Estonia". Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 298, n.º 1 (1 de outubro de 2020): 67–73. http://dx.doi.org/10.1127/njgpa/2020/0934.
Texto completo da fonteDixon, Owen A. "Endobiotic cornulitids in Upper Ordovician tabulate corals and stromatoporoids from Anticosti Island, Quebec". Journal of Paleontology 84, n.º 3 (maio de 2010): 518–28. http://dx.doi.org/10.1666/09-129.1.
Texto completo da fonteVinn, Olev, e 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, n.º 1 (29 de janeiro de 2021): 99–105. http://dx.doi.org/10.1127/njgpa/2021/0957.
Texto completo da fonteTetreault, 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.
Texto completo da fonteКомаров, В. Н., А. А. Измайлова, Д. А. Головастов e Е. И. Гончарова. "Микрокосм девонских микроконхид и корнулитид Закавказья, "Природа"". Priroda, n.º 7 (2021): 47–54. http://dx.doi.org/10.7868/s0032874x2107005x.
Texto completo da fonteHERRINGSHAW, LIAM G., ALAN T. THOMAS e M. PAUL SMITH. "Systematics, shell structure and affinities of the Palaeozoic Problematicum Cornulites". Zoological Journal of the Linnean Society 150, n.º 4 (agosto de 2007): 681–99. http://dx.doi.org/10.1111/j.1096-3642.2007.00300.x.
Texto completo da fonteVinn, Olev, e Mark A. Wilson. "Endosymbiotic Cornulites in the Sheinwoodian (Early Silurian) stromatoporoids of Saaremaa, Estonia". Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 257, n.º 1 (1 de julho de 2010): 13–22. http://dx.doi.org/10.1127/0077-7749/2010/0048.
Texto completo da fontePeters, Shanan E., e Kennard B. Bork. "Secondary tiering on crinoids from the Waldron Shale (Silurian: Wenlockian) of Indiana". Journal of Paleontology 72, n.º 5 (setembro de 1998): 887–94. http://dx.doi.org/10.1017/s0022336000027219.
Texto completo da fonteMitchell, Charles E., Mark A. Wilson e James M. St. John. "In situ crustoid graptolite colonies from an Upper Ordovician hardground, southwestern Ohio". Journal of Paleontology 67, n.º 6 (novembro de 1993): 1011–16. http://dx.doi.org/10.1017/s0022336000025336.
Texto completo da fonteMorris, Robert W., e Stephen H. Felton. "Symbiotic Association of Crinoids, Platyceratid Gastropods, and Cornulites in the Upper Ordovician (Cincinnatian) of the Cincinnati, Ohio Region". PALAIOS 8, n.º 5 (outubro de 1993): 465. http://dx.doi.org/10.2307/3515020.
Texto completo da fonteTeses / dissertações sobre o assunto "Cornulites"
Metatla, Imene. "Paléoenvironnements et dynamique sédimentaire des dépôts littoraux de l'Ordovicien de la Daoura, SW Algérie". Electronic Thesis or Diss., Université de Lille (2022-....), 2023. http://www.theses.fr/2023ULILR077.
Texto completo da fonteThis thesis explores the Ordovician sedimentology of the Saharan platform in the Daoura, SW Algeria. The latest work in this sector, leading to large-scale mapping, the division of formations, and their stratigraphic attribution at the system level, dates from the 1960s. However, this region, south to the better known Ougarta Range, is a bridge between the interior of the West African Craton and the Anti-Atlas basin. The objective of this work is to document depositional environments and sequence stratigraphy, and their relationship with the development of fossiliferous biota. In particular, attention is paid on the transitions from coastal environments dominated by storms to those dominated by tides, in the absence of evidence of incised valleys. Two high-resolution sections were made in the Tabelbala and Djebel Ben Tadjine ranges, crossing the Cambrian-Ordovician limit and the limit between the marine and glacial Upper Ordovician. These sections show a good correlation between them and with the Saoura and confirm the absence of incised valleys at least until the Middle Ordovician. The facies indicate a wave-dominated ramp-type depositional profile, mainly preserved as parasequences. On a detailed section of the Darriwillian, shell beds rich in Brachiopods and Cornulites are more particularly studied. They are preserved in tempestites located above the transgressive ravinement surfaces which cap the parasequences. The architecture of these tempestites suggests an indirect influence of the tide, which results, on the one hand, in interstratifications of upper plane beds and anisotropic HCS and, on the other hand, in rhythmic bedding of the shell beds. The increase in tidal range that this evolution implies on a ramp profile would be favored by the increase in accommodation generated in the shoreface at the start of the transgressions. This modification of coastal dynamics and the associated shoreface extension would be favorable to biota, which were absent in the underlying regressive intervals and which could then proliferate into the upper offshore. The mechanisms of this adaptation remain to be elucidated but the tomographic study of shell beds shows that Cornulites, sessile lophophorians, are surprisingly resistant to wave dynamics and can quickly recolonize the shoreface after storms
Livros sobre o assunto "Cornulites"
Jean-Louis, Aroui, e Cornulier Benoît de, eds. Le sens et la mesure: De la pragmatique à la métrique : hommages à Benoît de Cornulier. Paris: Champion, 2003.
Encontre o texto completo da fonteCORNULIERLUCINIERE-E. Complément de la Généalogie de la maison de Cornulier imprimée en 1863. Additions et. HACHETTE LIVRE-BNF, 2018.
Encontre o texto completo da fonteCapítulos de livros sobre o assunto "Cornulites"
Naud, François. "Cornulier-Lucinière Albert Hippolyte Henri de 1809-1886". In Les immortels du Sénat, 1875-1918, 290–93. Éditions de la Sorbonne, 1995. http://dx.doi.org/10.4000/books.psorbonne.68332.
Texto completo da fonte