Hostname: page-component-586b7cd67f-vdxz6 Total loading time: 0 Render date: 2024-11-23T21:42:49.608Z Has data issue: false hasContentIssue false

The Distribution and Sequence of Carboniferous Coral Faunas

Published online by Cambridge University Press:  01 May 2009

Dorothy Hill
Affiliation:
(University of Queensland)

Extract

Since the beginning of the century Carboniferous corals have been intensively studied throughout the world, and in this paper our resultant knowledge of their distribution and the sequence of faunas is outlined. The lower limit of the Carboniferous is taken to be at the base of the K zone of the Bristol sequence, and the upper limit at the base of the Russian Kungurian stage, in conformity with the principle of priority of nomenclature. The period is thus a long one including the Russian Artinskian, while the Permian is relatively short. Many recent writers, e.g. Dunbar (1940, 1942), adopting criteria other than priority of nomenclature, have extended the Permian downwards to incorporate greater or lesser amounts of the Carboniferous.

Type
Articles
Copyright
Copyright © Cambridge University Press 1948

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

REFERENCES

Beede, J. W. (19051906). In Cummings, E. R., and Beede, J. W. Fauna of the Salem Limestone, p. 1202.Google Scholar
Bubnoff, S. Von (1926). Geologie von Europa, Bd. 1. Berlin.Google Scholar
Chi, Y. S. (1938). Permian corals from South-Eastern Yunnan. Bull. Geol. Soc. China, 18, 155.CrossRefGoogle Scholar
Delépine, G. (1929). Description d'un polypier nouveau Humboldtia avesnensis nov. sp., du Viséen inférieur de Sars-Poteries. Ann. Soc. géol. Nord, 54, 104.Google Scholar
Dobrolyubova, T. A. (1940). The Rugosa corals of the upper Carboniferous of the Moscow basin. Trav. Inst. paleozool. Acad. Sci., U.R.S.S., 9, Livr. 3, 1.Google Scholar
Douglas, J. (1920). Geological sections through the Andes of Peru and Bolivia. II. From the port of Mollends to the Inambari River. Quart. Journ. Geol. Soc., Lond., 76, 1.CrossRefGoogle Scholar
Dunbar, C. O. (1940). The type Permian: its classification and correlation. Bull. Amer. Ass. Petrol. Geol. 24, 237.Google Scholar
Dunbar, C. O. (1942). Artinskian series. Bull. Amer. Ass. Petrol. Geol., 26, 402.Google Scholar
Dunbar, C. O. and Newell, N. D. (1946). Marine early Permian of the central Andes and its Fusuline faunas. Amer. J. Sci., 244, 377.CrossRefGoogle Scholar
Dutertre, A. P. (1929). Etude de quelques Polypiers du Viséen du Boulonnais. Ann. Soc. géol. Nord., 54, 108.Google Scholar
Easton, W. H. (1943 a). The fauna of the Pitkin formation of Arkansas. Journ. Paleont., 17, 125.Google Scholar
Easton, W. H. (1943 b). New Chester corals from Alabama and Tennessee. Journ. Paleont., 17, 276.Google Scholar
Easton, W. H. (1944 a). Revision of Campophyllum in North America. Journ. Paleont., 18, 119.Google Scholar
Easton, W. H. (1944 b). Corals from the Chouteau and related formations of the Mississippi Valley region. rept. Invest. Ill. Geol. Surv., 97, 1.Google Scholar
Easton, W. H. (1945 a). Kinkaid corals from Illinois. Journ. Paleont., 19, 383.Google Scholar
Easton, W. H. (1945 b). Corals from the Otter formation (Mississippian) of Montana. Journ. Paleont., 19, 522.Google Scholar
Easton, W. H. (1945 c). Amplexoid corals from the Chester of Illinois and Arkansas. Journ. Paleont., 19, 625.Google Scholar
Fomitchev, V. (1938). Corals Rugosa from the middle and upper Carboniferous deposits of the Donetz basin. C.R. Acad. Sci. U.R.S.S., 20, 219.Google Scholar
Gerth, H. (1926). Die Korallen fauna des Perm von Timor und die permische Vereisung. Leid. Geol. Meded., 2, 7.Google Scholar
Gerth, H. (1938). Permkorallen aus dem östlichen Karakorum und Triaskorallen aus dem norwestlichen Himalaya. Palaeontographica (A) 88, 230.Google Scholar
Gorsky, I. (1935). Coelenterates from Nova Zemlya. Trans. arctic Inst., Fasc. 28.Google Scholar
Gorsky, I. (1938). Carboniferous corals from Nova Zemlya. Trans. arctic Inst., Fasc. 93 (not seen).Google Scholar
Gubler, J. (1935). Études géologiques au Cambodge occidental. Bull. Serv. géol. Indo-Chine, 22, Fasc. 2.Google Scholar
Heritsch, F. (1934). Das Alter der Trogkofelkalke. No. 13, S.B. Akad. Wiss. Wien, math-naturw. Klass Akad. Anz. No. 13. 11 Mai 1934.Google Scholar
Heritsch, F. (1939). Die Korallen des Jungpalaozoikums von Spitzbergen. Ark. Zool., 31 A, No. 16, 1.Google Scholar
Heritsch, F. (1941). “Clisiophyllum” aus dem Oberkarbon. Cbl. Mm. Geol. Palaont. B 5, 129 (not seen).Google Scholar
Hill, D. (19381941). The Carboniferous Rugose corals of Scotland. Palaeontogr. Soc., London.Google Scholar
Hill, D. (1942). Further Permian corals from Western Australia. Journ. Roy. Soc. W. Aust., 27, 57.Google Scholar
Hill, D. (1943). A reinterpretation of the Australian Palaeozoic record, based on a study of the Rugose corals. Proc. Roy. Soc. Qd., 54, 53.Google Scholar
Howell, B. F. (1945). New Pennsylvanian Paleocyclid coral from Oklahoma. Bull. Wagner Inst. Sci. Philad., 20, 1.Google Scholar
Hudson, R. G. S. (1924). The rhythmic succession of the Yoredale series in Wensleydale. Proc. Yorks Geol. Soc., 20, 125.CrossRefGoogle Scholar
Hudson, R. G. S. (1941). On the Carboniferous corals: Zaphrentis carruthersi sp. nov. from the Mirk Fell beds and its relation to the Z. delanouei species group. Proc. Yorks. Geol. Soc., 24, 290.CrossRefGoogle Scholar
Hudson, R. G. S. (1942). Fasciculophyllum Thomson and other genera of the “Zaphrentis” omaliusi group of Carboniferous corals. Geol. Mag., 79, 257.CrossRefGoogle Scholar
Hudson, R. G. S. (1943 a). “Gerontic” structures in the Carboniferous coral Rotiphyllum costatum (McCoy). Geol. Mag., 80, 23.CrossRefGoogle Scholar
Hudson, R. G. S. (1943 b). On the Lower Carboniferous coral Permia cavernula sp. n. Ann. Mag. Nat. Hist. (11), 10, 361.Google Scholar
Hudson, R. G. S. (1943 c). Lower Carboniferous corals of the genera Rotiphyllum and Rylstonia. Proc. Leeds Phil. Lift. Soc. (Sci.), 4, 135.Google Scholar
Hudson, R. G. S. (1943 d). On the Lower Carboniferous corals—Caninia heterophylla sp. nov. Proc. Leeds Phil. Lit. Soc. (Sci.), 4, 142.Google Scholar
Hudson, R. G. S. (1943 e). On the Lower Carboniferous corals: Rhopalolasma rylstonense sp. nov. Quart. Journ. Geol. Soc., 99, 81.CrossRefGoogle Scholar
Hudson, R. G. S. (1944 a). On the Carboniferous corals: Zaphrentites shunnerensis sp. nov. Geol. Mag., 81, 45.CrossRefGoogle Scholar
Hudson, R. G. S. (1944 b). On the Lower Carboniferous corals: Zaphrentites crassus and Z. tenuis spp. n. Ann. Mag. Nat. Hist. (11), 11, 145.CrossRefGoogle Scholar
Hudson, R. G. S. (1944 c). Lower Carboniferous corals of the genera Rotiphyllum and Permia. Journ. Paleont., 18, 355.Google Scholar
Hudson, R. G. S. (1945(a). The variation in an assemblage of the Caninia cornufopiae plexus from the Middle Viséan. Quart. Journ. Geol. Soc., 100, 193.CrossRefGoogle Scholar
Hudson, R. G. S. 1945 b). On the Lower Carboniferous corals Permia capax and P. nota n. spp. Proc. Leeds Phil. Lit. Soc., Sci. Sect., 4, 285.Google Scholar
Hudson, R. G. S. and Cotton, G. (1945). The Lower Carboniferous in a boring at Alport, Derbyshire. Proc. Yorks. Geol. Soc., 25, 254.CrossRefGoogle Scholar
Hudson, R. G. S. and Fox, T. (1943). An Upper Viépan Zaphrentoid fauna from the Yoredale beds of North-West Yorkshire. Proc. Yorks. Geol. Soc., 25, 101.CrossRefGoogle Scholar
Ilyina, N. S. (1939). The corals from the lower Carboniferous deposits on the middle part of the Ishim River. Bull. Soc. Nat. Moscou (N.S.) (Geol.), 17, 83.Google Scholar
Jeffords, R. M. (1942). Lophophyllid corals from lower Pennsylvanian rocks of Kansas and Oklahoma. Bull. Geol. Surv. Kansas, 41, 185.Google Scholar
Jeffords, R. M. (1943). Caninia from the Lower Carboniferous of New Mexico. Journ. Paleont., 17, 545.Google Scholar
Jeffords, R. M. (1947). Pennsylvanian Lophophyllidid corals. Paleont. Contrib. Univ. Kansas, 1.Google Scholar
Katzer, F. (1935). Geologia do Estado do Para. Bol. Mus. Para.,9, 152, quoted in Oliviera, A. I., and Leonardos, O. H. (1943), Geologiado Brazil.Google Scholar
Kelly, W. A. (1942). Lithostrotiontidae in the Rocky Mountains. Journ. Paleont., 16, 351.Google Scholar
Keyes, C. R. (1894). Palaeontology of Missouri, Part 1. Missouri Geol. Surv., 4.Google Scholar
Krestovnikov, V. (1940). On the stratigraphy of the Gigantella beds of the Karsakpai region, Central Kazakhstan. C.R. Acad. Sci. U.R.S.S.Google Scholar
Lang, W. D., Smith, S., and Thomas, H. D. (1940). Index of Palaeozoic Coral Genera. British Museum, London.Google Scholar
Lee, J. S., Chen, S., and Chu, S. (1930). Huanglung limestone and its fauna. Mem. Nat. Res. Inst. Geol. Shanghai, No. 9, 85.Google Scholar
Mansuy, H. (1913). Faunes des calcaires à Productus de l' Indochine. Mem. Serv. géol. Indo-Chine, 2, Fasc. 4.Google Scholar
Maximova, S. V. (1945). A contribution to the faunistic characteristics of the Artinskian stage s. str. C.R. Acad. Sci. U.R.S.S., 46, 69.Google Scholar
Merriam, C. W. (1942). Carboniferous and Permian corals from Central Oregon. Journ. Paleont., 16, 372.Google Scholar
Meyer, L. F. (1914). Quoted in STEINMANN, G. (1929). Geologie von Peru. Heidelberg.Google Scholar
Moore, R. C., and Jeffords, R. M. (1941). New Permian corals from Kansas, Oklahoma, and Texas. Bull. Geol. Surv. Kansas, 38, 65.Google Scholar
Moore, R. C., and Jeffords, R. M. (1945). Description of lower Pennsylvanian corals from Texas and adjacent states. Publ. Univ. Tex., 4401, 77.Google Scholar
Paul, H. (1937 a). Vergleich des Nordwestdeutschen Unterkarbon mit dem belgischen. C.R. deux. Congrés. Stratig. Carb., 745. Haarlem.Google Scholar
Paul, H. (1938). Die Dibunophyllum-zone des bergischen Unterkarbons. N. Jb. Min. Geol. Palaont., (B), 79, 187.Google Scholar
Reed, F. R. C. (1930). Upper Carboniferous fossils from Tibet. Palaeont. Indica, (N.S.), 16, 1.Google Scholar
Reed, F. R. C. (1931). Upper Carboniferous fossils from Afghanistan. Palaeont. Indica, (N.S.), 19, 1.Google Scholar
Sen, A. (1931). On the development of the genus Waagenophyllum Yabe and Hayasaka, from the Productus Limestone beds of the Salt Range. Quart. Journ. Geol. Soc. India, 3, 125.Google Scholar
Sen, A. (1932). On the identity between Lonsdaleia indica Waag. and Wentz. and Lonsdaleia Virgalensis Waag. and Wentz. Quart. Journ. Geol. Soc. India, 4, 9.Google Scholar
Sloss, L. L. (1945). Corals from the post-Osage Mississippian of Montana. Journ. Paleont., 19, 309.Google Scholar
Smith, S., in Scrivenor, J. B. (1931). The Geology of Malaya. London.Google Scholar
Smith, S. (1942). A high Viséan fauna from the vicinity of Yate, Gloucestershire; with special reference to the corals and to a goniatite. Proc. Bristol Nat. Soc., (4), 9, 335.Google Scholar
Smith, S. and , C. C. (1943). A revision of the coral genus Aulina Smith and descriptions of new species from Britain and China. Quart. Journ. Geol. Soc., 99, 37.CrossRefGoogle Scholar
Soshkina, E., Dobrolyubova, T. A., and Porfiriev, G. (1941). The Permian Rugose corals of the European part of the U.S.S.R. Palaeontology of U.S.S.R., 5, Part 3, Fasc. 1. Leningrad.Google Scholar
Sokolov, B. S. (1939 a). Stratigraphical value and types of Chaetetidae of the Carboniferous of the U.S.S.R. C.R. Acad. Sci. U.R.S.S., 23, 409.Google Scholar
Sokolov, B. S. (1939b). Role of the Rugosa and Tabulata corals in the stratigraphy of the lower Carboniferous of the Moscow basin (northern part). C.R. Acad. Sci. U.R.S.S. (N.S.), 25, 134.Google Scholar
Vakhrameev, V. A., and Rausser-Chernoussova, D. M. (1938). The middle Carboniferous in the north-east part of the region adjoining Lake Balkhash. C.R. Acad. Sci. U.R.S.S., 19, 717.Google Scholar
Vaughan, A. (1909). Faunal succession in the Carboniferous limestone (Avonian) of the British Isles. Rep. Brit. Ass. Winnipeg, 79, 187.Google Scholar
Weissermel, W. (1935 a). Über ein kieselgestein mit Lithostrotion junceum aus Thüringen. Z. deutsch. Geol. Ges., 87, 115.Google Scholar
Williams, J. S., and Yolton, J. S. (1945). Brazer (Mississippian) and lower Wells (Pennsylvanian) section at Dry Lake, Logan Quadrangle, Utah. Bull. Amer. Ass. Petrol. Geol., 29, 1143.Google Scholar
Yabe, H. (1939). Palaeozoic formations of the Japanese islands. Proc. 6th Pan-Pacif. sci. Congr., Tokyo, 377.Google Scholar
Yabe, H. and Sugiyama, T. (1939 a). Discovery of Hexaphyllia in the lower Carboniferous of Japan. J. Geol. Soc. Japan, 46, 409.CrossRefGoogle Scholar
Yabe, H. and Sugiyama, T. (1939 b). Discovery of lower Carboniferous corals from the Yatusiro district in Kyusyu. Proc. Imp. Acad. Japan, 15, 300.CrossRefGoogle Scholar
Yabe, H. and Sugiyama, T. (1940). Notes on Heterophyllia and Hexaphyllia. J. Geol. Soc. Japan, 47, 81.CrossRefGoogle Scholar
Yakovlev, N. N. (1939). Nouveaux genres de coraux Tabulata du Permien inférieur de l' Ouraletdubassin du Donetz. C.R. Acad. Sci. U.R.S.S., 24, 629.Google Scholar