Sclerobionts on organic substrates from the Late Paleocene Chehel-Kaman Formation, Kopet-Dagh Basin, NE Iran

• Autorzy: Salahi A. , El Hedeny M. , Vinn O. , Rashwan M.

Identyfikatory

DOI

10.14241/asgp.2018.022

• Języki publikacji: EN

Abstrakty

EN

Molluscs (oysters and gastropods) of the Late Paleocene Chehel-Kaman Formation, Kopet-Dagh Basin NE Iran were significantly colonized by sclerobionts. The largest area of the shells studied is covered by various borings. The diversity of macro-bioeroding ichnotaxa is rather high, including Gastrochaenolites Leymerie 1842; Maeandropolydora Voigt, 1965; Trypanites Mägdefrau, 1932; Talpina von Hagenow, 1840, and possibly Entobia Bronn, 1837. Some slightly conical borings penetrating the shells could belong to predatory tracemakers of Oichnus Bromley, 1981. Encrusters include calcareous polychaetes, cyclostome and cheilostome bryozoans, foraminifera and oysters. Calcareous sabellids [i.e. Glomerula serpentina (Goldfuss, 1831)] and serpulids are equally common sclerobionts in the association. Bryozoans cover a slightly larger area of the substrate than the calcareous polychaetes, while encrusting oysters are subordinate. The majority of fossils in the hard-substrate community studied belong to suspension feeders. Sclerobionts are typical of the shallow-marine environment, commonly in warm water. The present study is the first attempt to record the occurrence and diversity of epi- and endobionts in the organic substrates, present in the topmost part of the Late Paleocene Chehel-Kaman Formation, Kopet-Dagh Basin, NE Iran.

Słowa kluczowe

EN

sclerobionts; Late Paleocene; Chehel-Kaman Formation; Iran

• Wydawca: Polskie Towarzystwo Geologiczne
• Czasopismo: Annales Societatis Geologorum Poloniae
• Rocznik: 2018
• Tom: Vol. 88, No. 3
• Strony: 291--301
• Opis fizyczny: Bibliogr. 70 poz., rys., tab., wykr.

Twórcy

autor

Salahi A.

• Department of Geology, Ferdowsi University of Mashhad, Mashhad, Iran

autor

El Hedeny M.

• Department of Geology, Faculty of Science, Alexandria University, Alexandria 21568, Egypt

autor

Vinn O.

• Department of Geology, University of Tartu, Ravila 14A, 50411 Tartu, Estonia

autor

Rashwan M.

• Department of Geology, Ferdowsi University of Mashhad, Mashhad, Iran

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Uwagi

Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2019).