PALAEOCOLOGY OF LATE TRIASSIC DEPOSITS, IN DIZLU SECTION NORTH OF ISFAHAN, CENTRAL IRAN BASED ON SCLERACTINIAN CORALS

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MANNANI M.; YAZDI S.

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Journal: GEOSCIENCES Year:2015 | Volume:24 | Issue:95 (STRATIGRAPHY & SEDIMENTOLOGY) Page(s): 281-290

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Title

PALAEOCOLOGY OF LATE TRIASSIC DEPOSITS, IN DIZLU SECTION NORTH OF ISFAHAN, CENTRAL IRAN BASED ON SCLERACTINIAN CORALS

Author(s)

MANNANI M. | YAZDI S. | Issue Writer Certificate

Keywords

PALAEOECOLOGYQ2

SCLERACTINANQ2

NAYBANDQ2

LATE TRIASSICQ2

CENTRAL IRANQ2

Abstract

The NAYBAND Formation in North of Isfahan includesfive Members: 1- Gelkan Member (marl and sandstone), 2- Bidestan Member (sandstone and reefal limestone), 3- Howz- e- Sheikh Member (marl and sandstone), 4- Howz- e- Khan Member (marl and reefal Limestone) and 5- Qadir Member (marl and sandstone). The biostromal limestones of Bidestan and Howz-e- Khan Members represent a typical known key bed in North of Isfahan. In Bidestan and Howz-e- Khan Members (NaybandFormation), coral reefs grow up and their distribution are significant in the biostromal limestone of Bidestan and Howz-e- Khan Members of NAYBAND Formation.Twelve genera and 31 species of Scleractiniancorals were recognized in thesereefal members. They included: Reimaniphylliidae, Margarophylliidae, Coryphylliidae, Cyclophyllidae, Astraeomorphidae, Pamiroseriidae, Stylophyllidae and Actinastraeidae families. According to the field observations and evidences, laboratory studies and analysis, measurements of the coral size and the destroyedepitechaof thecorals, it could beguessed that Scleractinian corals survive below the storm wave base (about 20 meters depth) but they tolerated many storms. Morphology of Scleractinian corals of LATE TRIASSIC sea (North of Isfahan) indicatesinadequate living conditions and high energy environment. Corals have major roleinreconstruction of Paleoenviromentofthe LateTriassic unitsofthe North of Isfahan (Nayband Formation) in Dizlusection.

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APA: Copy

MANNANI, M., & YAZDI, S.. (2015). PALAEOCOLOGY OF LATE TRIASSIC DEPOSITS, IN DIZLU SECTION NORTH OF ISFAHAN, CENTRAL IRAN BASED ON SCLERACTINIAN CORALS. GEOSCIENCES, 24(95 (STRATIGRAPHY & SEDIMENTOLOGY)), 281-290. SID. https://sid.ir/paper/31600/en

Vancouver: Copy

MANNANI M., YAZDI S.. PALAEOCOLOGY OF LATE TRIASSIC DEPOSITS, IN DIZLU SECTION NORTH OF ISFAHAN, CENTRAL IRAN BASED ON SCLERACTINIAN CORALS. GEOSCIENCES[Internet]. 2015;24(95 (STRATIGRAPHY & SEDIMENTOLOGY)):281-290. Available from: https://sid.ir/paper/31600/en

IEEE: Copy

M. MANNANI, and S. YAZDI, “PALAEOCOLOGY OF LATE TRIASSIC DEPOSITS, IN DIZLU SECTION NORTH OF ISFAHAN, CENTRAL IRAN BASED ON SCLERACTINIAN CORALS,” GEOSCIENCES, vol. 24, no. 95 (STRATIGRAPHY & SEDIMENTOLOGY), pp. 281–290, 2015, [Online]. Available: https://sid.ir/paper/31600/en

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