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Some remarks on diagenesis of rugose coral skeletons

Wybrane pełne teksty z tego czasopisma
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PL
Kilka uwag o diagenezie szkieletów koralowców Rugosa
Języki publikacji
EN
Abstrakty
EN
Rugose coral microstructure exhibits striking similarity to that in the Scleractinia. The main difference lies in the mineral composition: calcitic in the former and aragonitic in the latter. Calcitic skeletons of the Rugosa are commonly better preserved than those in the Scleractinia, and therefore some of them have been interpreted as unaltered, a position rejected in this paper. The dual nature of septa, which commonly consist of a primary trabecular septum and secondary fibrous sheets, results in differently expressed diagenetic alterations in comparison to other structural elements. It has been postulated that both early and advanced diagenesis may, in some circumstances, be distinguished in the Rugosa. In most instances the early diagenetic features were destroyed by the post-burial alterations. Replacement and recrystallization are the most important processes among the advanced chemical alterations. Both may either facilitate the recognition of original macro- and microstructures or obscure them. Surface replacement by silica promotes perfect preservation of shape and inner morphology, whereas pervasive replacement may destroy both. Selected replacement by hematite may help in exposing the trabecular microstructure of septa, whereas deep replacement may destroy the entire morphology. Physical alterations, such as crushing and flattening of skeletons are always destructive. They result from compaction, and their scale depends on skeletal morphology and on the relationship between the rate of infilling of intra-skeletal spaces and the accumulation of surrounding sediment. Pre-burial events, such as overgrowth and penetration by borrowing organisms, their holdfasts or roots may aid in the recognition of early diagenesis, but may also lead to substantial pre- or post-burial skeletal alteration, resulting sometimes in total destruction. This depends mostly on the pH of pore fluids.
Słowa kluczowe
Czasopismo
Rocznik
Tom
Strony
89--110
Opis fizyczny
Bibliogr. 22 poz.
Twórcy
  • Institute of Geology Adam Mickiewicz University, ul. Maków Polnych 16, 61-606 Poznań, Poland
Bibliografia
  • Cooper G.A., Gant R.E., 1972-1977: Permian brachiopods of West Texas. Parts I-VI. Smithsonian Contributions to Paleobiology, 14, 15, 19, 21, 24, 32: 1-3370, Washington, D.C.
  • Fedorowski J., 1986: Diffingiina, a new suborder of the rugose corals from SW Texas. Acta Palaeontologica Polonica, 30, 3^1: 209-240, Warszawa.
  • Fedorowski J., 1987: Upper Palaeozoic rugose corals from Southwestern Texas and adjacent areas: Gaptank Formation and Wolfcampian corals. Part I. Palaeontologia Polonica, 48: 1-271, Warszawa.
  • Fedorowski J., 1993: Intraspecific variability in two Permian rugose corals. Courier Forschung.- Inst. Senckenberg, 164: 255-262. Frankfurt am Main.
  • Fedorowski J., Bamber E.W., 2001: Guadalupian (Middle Permian) solitary rugose corals from the Degerbols and Trold Fiord formations, Ellesmere and Melville islands, Canadian Arctic Archipelago. Acta Geologica Polonica, 51, 1: 31-79, Warszawa.
  • Ivanovsky A.B., 1988: Was Gshelia rouilleri a “soft coral"? Fifth International Symposium Abstracts, p. 42. Brisbane.
  • Kato M., 199?: Fine skeletal structures in Rugosa. Journal of the Faculty of Science. Hokkaido University. Series IV, 11: 571-630, Sapporo.
  • Oekentorp K., 1980: Aragonit und diagenese bei jungpalaozoischen Korallen. Munstersche Forschungen zur Geologie und Palaontologie, 52: 119-239, Munster.
  • Oekentorp K., 1984: Aragonite and diagenesis in Permian corals. Palaeontographica Americana, 54: 282-293. Ithaca, New York.
  • Oliver W.A. Jr., 1980: The relationship of the sceractinian corals to the rugose corals. Paleobiology, 6, 2: 146-160. Lawerence.
  • Rodriguez S., 1984: Corales rugosos del Carbonifero del Este de Asturias. Ph.D.Thesis, published by Departamento de Paleontologia, Universidad Complutense de Madrid. Doctoral thesis collection no. 109/84: 1-328. Madrid.
  • Rodriguez S., 1989: Lamellar microstructure in Palaeozoic corals: origin and use in taxonomy. Memoirs of the Australasian Palaeontologists, 8: 157-168, Brisbane.
  • Roniewicz E., Morycowa E., 1993. Evolution of the Scleractinia in the light of micro- structural data. Courier Forschungsinstitut Senckenberg, 164: 233-240.
  • Schindewolf O.H., 1942: Zur Kenntnis der Polycoelien und Plerophyllen. Eine Studie iiber den Bau der “Tetrakorallen“ und ihre Beziehungen zu den Madreporarien. Abhandlungen des Reichsamtes fiir Bodenforschung, 204: 1-324, Berlin.
  • Schouppe A., Stacul P, 1955: Die Genera Verbeekiella Penecke, Timorphyllum Gerth, Wannerophyllum n. gen., Lophophyllidium Grabau aus dem Perm von Timor. Palaeontographica, Suppl. Bd. 4, 5, 3: 95-196. Stuttgart.
  • Schouppe A., Stacul P, 1959: Saulchenlose Pterocorallia aus dem Perm von Indonesisch Timor (mit Ausnahme der Polycoeliidae). Palaeontographica, Suppl. Bd. 4, 5, 4: 197-359. Stuttgart.
  • Semenoff-Tian-Chansky R, 1974: Recherches sur les Tetracoralliaires du Carbonifere du Sahara Occidental. Centre de Recherches sur les Zones Arides. Serie: Geologie, 21: 1-316, Paris.
  • Sorauf J.E., 1984: Upper Permian corals from Timor and diagenesis. Palaeontographica Americana, 54: 294-302. Ithaca, New York.
  • Sorauf J.E., 1996:. Biomineralization models and skeletal structure of Phanerozoic corals. [In:] G.D. Stanley Jr. (Ed.): Paleobiology and biology of corals. The Paleontological Society Papers, 1: 159-185, Pittsburgh.
  • Sorauf J.E., Cuiff J.-P., 2001: Biomineralization and diagenesis in the Scleractinia: part 2, diagenesis. Bulletin of the Tohoku University Museum, 1: 152-163, Tohoku.
  • Webb G.E., Sorauf J.E., 2002: Zig-zag microstructure in rugose corals: A possible indicator of relative seawater Mg/Ca ratios. Geology, 30: 5, 415-418. .
  • Wendt J., 1990: The first aragonitic rugose coral. Journal of Paleontology, 64: 335-340, Lawrence, Kansas.
Uwagi
Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2019).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-bf13d9be-ab64-4fdd-8996-d1e01b577edf
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