ENVIRONMENTAL PARAMETERS OF LATE CARBONIFEROUS (BASHKIRIAN STAGE) CORAL ASSEMBLAGE FROM SARDAR FORMATION (CARBONIFEROUS), ZALADU SECTION, OZBAK-KUH MOUNTAINS, EAST OF CENTRAL IRAN

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BADPA M.; KHAKSAR K.; ASHOURI A.; KHANEHBAD M.

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Journal: GEOSCIENCES Year:2015 | Volume:24 | Issue:95 (STRATIGRAPHY & SEDIMENTOLOGY) Page(s): 97-106

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Title

ENVIRONMENTAL PARAMETERS OF LATE CARBONIFEROUS (BASHKIRIAN STAGE) CORAL ASSEMBLAGE FROM SARDAR FORMATION (CARBONIFEROUS), ZALADU SECTION, OZBAK-KUH MOUNTAINS, EAST OF CENTRAL IRAN

Author(s)

BADPA M. | KHAKSAR K. | ASHOURI A. | KHANEHBAD M. | Issue Writer Certificate

Keywords

CARBONIFEROUSQ2

ENVIRONMENTAL PARAMETERSQ2

BASHKIRIANQ2

CORALQ2

OZBAK-KUHQ2

SARDAR FORMATIONQ2

Abstract

Rich assemblages of CARBONIFEROUS CORALs exist in the Zaladu stratigraphic section. After identification of CORALs, more than 200 thin sections of CORAL fossils and microfacies were selected and studied for ENVIRONMENTAL PARAMETERS. This association belonging to BASHKIRIAN age (the oldest stage of Late CARBONIFEROUS) and were found in two horizons. Based on the colonies geometry, the distance between them, the abundance and distribution of CORALs and microfacies study, the habitats of lower horizon is “ CORAL meadows (subtype B1) “. The upper horizon made a“polyspecific CORAL biostrome (subtype C2) “. These CORALs existed in a lagoon toward barrier and open marine toward barrier belonging to a shallow carbonate ramp environment. This association favored a shallow, warm, and clear marine environment with normal salinity and high oxygen, within the photic zone. The fasciculate rugoseFomichevella and Heintzella, have the most abundance, and these colonies form the main builders of the CORAL association. Colonial rugose CORALsFomichevella and Minatoa have maximum diversity. Michelinia tabulate CORALs, has the least abundance and diversity.

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APA: Copy

BADPA, M., KHAKSAR, K., ASHOURI, A., & KHANEHBAD, M.. (2015). ENVIRONMENTAL PARAMETERS OF LATE CARBONIFEROUS (BASHKIRIAN STAGE) CORAL ASSEMBLAGE FROM SARDAR FORMATION (CARBONIFEROUS), ZALADU SECTION, OZBAK-KUH MOUNTAINS, EAST OF CENTRAL IRAN. GEOSCIENCES, 24(95 (STRATIGRAPHY & SEDIMENTOLOGY)), 97-106. SID. https://sid.ir/paper/31598/en

Vancouver: Copy

BADPA M., KHAKSAR K., ASHOURI A., KHANEHBAD M.. ENVIRONMENTAL PARAMETERS OF LATE CARBONIFEROUS (BASHKIRIAN STAGE) CORAL ASSEMBLAGE FROM SARDAR FORMATION (CARBONIFEROUS), ZALADU SECTION, OZBAK-KUH MOUNTAINS, EAST OF CENTRAL IRAN. GEOSCIENCES[Internet]. 2015;24(95 (STRATIGRAPHY & SEDIMENTOLOGY)):97-106. Available from: https://sid.ir/paper/31598/en

IEEE: Copy

M. BADPA, K. KHAKSAR, A. ASHOURI, and M. KHANEHBAD, “ENVIRONMENTAL PARAMETERS OF LATE CARBONIFEROUS (BASHKIRIAN STAGE) CORAL ASSEMBLAGE FROM SARDAR FORMATION (CARBONIFEROUS), ZALADU SECTION, OZBAK-KUH MOUNTAINS, EAST OF CENTRAL IRAN,” GEOSCIENCES, vol. 24, no. 95 (STRATIGRAPHY & SEDIMENTOLOGY), pp. 97–106, 2015, [Online]. Available: https://sid.ir/paper/31598/en

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