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2004 | 49 | 1 |

Tytuł artykułu

Monospecific rugosan assemblage from the Emsian hydrothermal vents of Morocco

Autorzy

Treść / Zawartość

Warianty tytułu

Języki publikacji

EN

Abstrakty

EN
Unique monospecific assemblages of small, solitary, nondissepimented rugose corals from the Devonian deep−sea hydrothermal venting systems of the Hamar Laghdad (Anti−Atlas, Morocco) are described. Assemblages of numerous rugosans (coral meadows) have been found around the outlets of venting channels irregularly forked within the Emsian mud mound sediments. The majority of rugose corals, which settled around vents, reveal a bizarre pattern of growth called here “calice−in calice”. The phenomenon of “calice−in−calice” growth is related to selective survival of coral larvae i.e. it is postulated that the larvae, which settled within the calices of dead individuals were more successful in their development than those that settled elsewhere. They probably use empty calices as shelters against the physical (hot or poisoning fluids) or biological (predators) factors. The empty calices also provided a hard surface for attachment. The presence of numerous carapaces of ostracods within the calices of dead rugosans suggests a strong trophic relation between corals and ostracods, which lived around hydrothermal vents. The new genus and species Hamarophyllum belkai is proposed.

Wydawca

-

Rocznik

Tom

49

Numer

1

Opis fizyczny

p.75-84,fig.,ref.

Twórcy

autor
  • Adam Mickiewicz University, Makow Polnych 16, 61-606 Poznan, Poland

Bibliografia

  • Alberti, G.K.B. 1981. Scutellidae (Trilobita) aus dem Unter−Devon des Hamar Laghdad (Tafilalt, SE−Maider) und das Alter des „mudmounds“ (Ober Zlichovium bis tiefstes dalejum). Senckenbergiana Lethaia 62: 205–216.
  • Alberti, G.K.B. 1982. Der Hamar Laghdad (Tafilalt, SE Marokko), eine bedeutende Fundstaette devonischer Trilobiten. Natur und Museum 112: 172–182.
  • Bełka, Z. 1994. Carbonate mud bildups in the Devonian of the central Sahara evidences for submarine hydrothermal venting. Przegląd Geologiczny 42: 341–346.
  • Bełka, Z. 1998. Early Devonian Kess−Kess carbonate mud mounds of the eastern Anti−Atlas (Morocco), and their relation to submarine hydrothermal venting. Journal of Sedimentary Research 68: 368–377.
  • Bełka, Z., Berkowski, B., Eisenmann, Ph., Dopieralska, J., and Skompski, S. 2003. Fauna podmorskich źródeł hydrotermalnych z dewonu Maroka. Streszczenia do referatów i posterów na XVIII Konferencję Paleontologów PTG. Przegląd Geologiczny 51 (3): 246.
  • Brachert, T.C., Buggisch, W., Fluegel, E., Huessner, H., Joachimski, M.M., Tourner, F., and Walliser, O.H. 1992. Controls of mud mound formation: the Early Devonian Kess−Kess carbonates of the Hamar laghdad, Antiatlas, Morocco. Geologishe Rundschau 81: 15–44.
  • Gendrot, C. 1973. Environments du Devonian recifal du Maroc. Notes du Service Geologique du Maroc 34: 55–86.
  • Kaufmann, B. 1998. Facies, stratigraphy and diagenesis of Middle Devonian reef− and mud mounds in the Mader (eastern Anti−Atlas, Morocco). Acta Geologica Polonica 48: 43–106.
  • Little, C.T.S. 2002. The fossil record of hydrothermal vent communities. Cahiers de Biologie Marine 43: 313–316.
  • Little, C.T.S., Herrington, R.J., Maslennikov, V.V., and Zaykov, V.V. 1998. The fossil record of hydrothermal vent communities. In: R.A. Mills and K. Harrison (eds.), Modern Ocean Floor Processes and the Geological Record. Geological Society of London Special Publication 148: 259–270.
  • Massa, D., Combaz, A., and Manderscheid, G. 1965. Observations sur le Siluro–Devonien des confines algero−marocains. Compagnie Française des Petroles, Notes et Memoires 8: 1–187.
  • Mounji, D., Bourque, P.−A., and Savard, M.M. 1998. Hydrothermal origin of Devonian Conical Mounds (kess−kess) of Hamar−Lakhdad Ridge, Anti−Atlas, Morocco. Geology 26: 1123–1126.
  • Peckmann, J., Walliser, O.H., Riegel, W., and Reitner, J. 1999. Signatures of hydrocarbon venting in a Middle Devonian carbonate mound (Hollard Mound) at the Hamar Laghdad (Antiatlas, Morocco).Facies 40: 281–296.
  • Roch, E. 1934. Sur des phenomenes remarquables observes dans laregion d’Erfoud (confinsalgero−marocains du Sud). Geologie Mediterraneenne Occidentale 5: 1–10.
  • Stolarski, J. 1995. Ontogenetic development of the thecal structures in caryophylliine scleractinian corals. Acta Palaeontologica Polonica 40 (1): 19–44.
  • Wendt, J. 1993. Steep−sided carbonate mud mounds in the Middle Devonian of the eastern Anti−Atlas, Morocco. Geological Magazine 30: 69–83.
  • Wendt, J., Bełka, Z., and Moussine−Pouchkine, A. 1993. New architectures of deep−water carbonate bildups: Evolution of mud mounds into mud ridges (Middle Devonian, Algierian Sahara). Geology 21: 723–726.
  • Weyer, D. and Zagora K. 1990. Die ehemalige Givet−Fossilfundstelle im Unterharz. Hallesches. Jahrbuch für Geowissenshaften 15: 21–42.
  • Weyer, D. 2001. Muenstraia, ein neues Rugosa−Genus (Anthozoa) aus dem Obersilur und Unterdevon. Mittelungen aus dem Museum für Naturkunde in Berlin, Geowissenschftliche Reiche 4: 71–82.

Typ dokumentu

Bibliografia

Identyfikatory

Identyfikator YADDA

bwmeta1.element.agro-article-a32e2882-b344-40ec-b490-60e85d33aac3
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