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Famennian tentaculitids of China

Published online by Cambridge University Press:  20 May 2016

You Xing Li
You Xing Li*
Affiliation:
Department of Resource Engineering, Wuhan Institute of Chemical Technology, Wuhan 430073, China,
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Extract

Until recently, paleontologists believed tentaculitids became extinct by the end of the Frasnian. Lyaschenko (1958) described the youngest occurrence of the genera Styliolina and Homoctenus from the Frasnian of Russia. However, in Europe and North Africa, Lardeux (1969) proposed that Homoctenus ultimus pergracilis persisted into the Famennian. Sauerland (1983) reported the occurrence in France of the genera Styliolina and Striatostyliolina in the cicatricosa ostracod Zone (Frasnian), and Homoctenus in the splendens ostracod Zone (Frasnian-Famennian, upper gigas—middle triangularis conodont Zones). The first report of Famennian tentaculitids in China was from the Dachang area in Guangxi Province, China by Li and Hamada (1986).

Type
Paleontological Notes
Information
Journal of Paleontology , Volume 74 , Issue 5 , September 2000 , pp. 969 - 975
Copyright
Copyright © The Paleontological Society

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References

Boucek, B. 1964. The Tentaculites of Bohemia. Czechsl. Acad. Sci., Prague:94–146.Google Scholar
Boucek, B., and Prantl, F. 1961. Über einige neue Tentaculiten-Gattungen aus dem bohmische Devon. Vest. Ustt. ust. geolog., 36:385–388.Google Scholar
Fisher, D. W. 1962. Small conoidal shells of uncertain affinities, p. W98–W143. In Moore, R. C. (ed.), Treatise on Invertebrate Paleontology, Part W, Miscellanea. Geological Society of America and University of Kansas Press, Lawrence.Google Scholar
Grabau, A. W. 1912. Citation unverifiable (see Fisher, 1962, p. W116).Google Scholar
Karpinsky, A. P. 1884. Die fossilen Pteropoden am Ostabhange des Urals. Acad. Impér. Sci. St. Pétersbourg, Memoire, ser. 7, 32(1):1–121.Google Scholar
Lardeux, H. 1969. Les tentaculites d'Europe occidentale et d'Afrique du nord. Cahiers de Paleontologie. Editions du Centre National de la Recherche Scientifique, Paris, 238 p.Google Scholar
Li, Y. X. 1987. Devonian Tentaculites at Shetianqiao of Shaodong County, Hunan. Acta Micropalaeontologica Sinica, 4(1):45–54. (In Chinese with English abstract)Google Scholar
Li, Y. X. 1991. Relationship between lithofacies and paleogeography of Upper Devonian Daihua Formation and nonferrous metal deposits in Dachang area, Guangxi, p. 25–26. In The Second International Congress on Palaeoecology, Summaries of Papers, Nanjing.Google Scholar
Li, Y. X. 1992. The ore-prospecting significance of Famennian Tentaculites from the Dachang area, Guangxi, China, p. 31–32 (abstract). In Teng, W. C. and Li, Y. Q. (eds.), International Symposium on Devonian System and Its Economic Oil and Mineral Resources, Guilin.Google Scholar
Li, Y. X. 1993a. Late Devonian Famennian Tentaculites from Liujiang Formation of Lipu, Guangxi, China. Acta Micropalaeontologica Sinica, 10(3):331–335. (In Chinese with English abstract)Google Scholar
Li, Y. X. 1993b. Numerical taxonomy and identifying program for tentaculitoids, p. 258–264. In Palaeoword 2. Nanjing University Press, Nanjing. (In Chinese)Google Scholar
Li, Y. X. 1995. Famennian Tentaculites from Luofu, Guangxi: Survivors of F/F extinction event. Journal of Guilin Institute of Technology, 15(2):157–170. (In Chinese with English abstract)Google Scholar
Li, Y. X., and Hamada, T. 1986. Occurrence of Tentaculites in the Upper Devonian Daihua Formation of Dachang area, Guangxi, China. Scientific Papers of the College of Arts and Sciences, The University of Tokyo, 36(2):163–171.Google Scholar
Lyaschenko, G. P. 1955. Novye dannye o sistematike tentakulitov, novakii stiliolii. Moskov. Obshch. Ispyt. Prir., Bull., 30(3):94–95.Google Scholar
Lyaschenko, G. P. 1958. Tentaculitids du Devonian de la Plateforme Russe. 20th International Geological Congress, Mexico, 7:139–152.Google Scholar
Lyaschenko, G. P. 1959. Konikonchii Devona tsentral'nykh i vostochnykh oblastey Russkoy Platformy. V.N.I.G.N.I., p. 1–220.Google Scholar
Novak, O. 1882. Über Böhemische, Thuringische, Greifensteiner und Harzer Tentaculiten. Beiträge Paläeont. Geol. Österreich-Ungarns, p. 47–60.Google Scholar
Richter, R. 1854. Thuringische Tentaculiten. Deutsch. geol. Gesell., Zeitschr., Jahrg. 1854, 6:275–290.Google Scholar
Sauerland, U. 1983. Dacryoconariden und Homocteniden der Givet- und Adorf-Stufe aus dem Rhinischen Schiefergebirge (Tentaculitoidea, Devon). Göttinger Arbeiten zur Geologie und Paläontologie, 24:1–86.Google Scholar
Xian, S. Y., and Wang, J. X. 1986. Tentaculites, p. 50–104. In Middle-Upper Devonian Boundary in Maanshan of Xiangzhou Guangxi. Geological Publishing House, Beijing.Google Scholar
Xian, S. Y., and Wang, J. X. 1988. Biostratigraphy and description of Tentaculitids. In Stratigraphic Paleontology and Sedimentary Facies of the Devonian in Longmenshan area, Sichuan Province. Geological Publishing House, Beijing.Google Scholar
Zagora, K. 1964. Tentaculiten aus den thuringischen Devon. Geologie, 13(10):1235–1273.Google Scholar