THALASSINOIDES-PHYCODES COMPOUND TRACE FOSSIL FROM ALBIAN-CENOMANIAN STRATA OF GAZAK, SOUTH KERMAN, SE IRAN

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ABBASSI N.; PARVANEHNEZHAD SHIRAZI M.; HOSSEINZADEH M.A.

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Journal: GEOSCIENCES Year:2015 | Volume:24 | Issue:95 (STRATIGRAPHY & SEDIMENTOLOGY) Page(s): 145-152

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Title

THALASSINOIDES-PHYCODES COMPOUND TRACE FOSSIL FROM ALBIAN-CENOMANIAN STRATA OF GAZAK, SOUTH KERMAN, SE IRAN

Author(s)

ABBASSI N. | PARVANEHNEZHAD SHIRAZI M. | HOSSEINZADEH M.A. | Issue Writer Certificate

Keywords

ICHNOLOGYQ2

TRACE FOSSILQ2

ICHNOFACIESQ2

CRETACEOUSQ2

CENTRAL IRANQ2

KERMANQ2

Abstract

Albian–Cenomanian siliciclastic-carbonate sediments of northwest Rayen in south KERMAN, southeast Iran (526 m) are classifiable to three informal units. Unit one includes conglomerates, sandstones and siltstones with limestone and marl intercalations. Unit two is composed of Orbitolina bearing limestones with rudists, belemnoid and ammonite bioclasts. Alternations of pelagic limestones and sandstones formed the third unit. Assemblage of continental to marine TRACE FOSSILs have been found in the first and third units of the studied section, that include Koilosomaisp., Ophiomorpha isp., Palaeophycus isp., Planolites isp., Skolithos isp., Taenidium isp., and Thalassinoides suevicus. These TRACE FOSSILs belongs to Scoyenia, Skolithos and Cruziana ICHNOFACIES. AbundantThalassinoides-Phycodes compound TRACE FOSSIL, however have been found in the third unit. Box-workedThalassinoides burrow system ends to multi- branched Phycodes borrows. This compound TRACE FOSSIL is interpreted as feeding-domicile biogenic structure, so thatThalassinoides domichnium ends to Phycodes excavated feeding burrows.CompoundThalassinoides-Phycodes TRACE FOSSIL extended in the deeper parts of offshore shelf sediments in the studied section. Based on ichnological data, it seems that Albian-Cenomanian sediments of northwest Rayen deposited in a deepening upward sequence.

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APA: Copy

ABBASSI, N., PARVANEHNEZHAD SHIRAZI, M., & HOSSEINZADEH, M.A.. (2015). THALASSINOIDES-PHYCODES COMPOUND TRACE FOSSIL FROM ALBIAN-CENOMANIAN STRATA OF GAZAK, SOUTH KERMAN, SE IRAN. GEOSCIENCES, 24(95 (STRATIGRAPHY & SEDIMENTOLOGY)), 145-152. SID. https://sid.ir/paper/31586/en

Vancouver: Copy

ABBASSI N., PARVANEHNEZHAD SHIRAZI M., HOSSEINZADEH M.A.. THALASSINOIDES-PHYCODES COMPOUND TRACE FOSSIL FROM ALBIAN-CENOMANIAN STRATA OF GAZAK, SOUTH KERMAN, SE IRAN. GEOSCIENCES[Internet]. 2015;24(95 (STRATIGRAPHY & SEDIMENTOLOGY)):145-152. Available from: https://sid.ir/paper/31586/en

IEEE: Copy

N. ABBASSI, M. PARVANEHNEZHAD SHIRAZI, and M.A. HOSSEINZADEH, “THALASSINOIDES-PHYCODES COMPOUND TRACE FOSSIL FROM ALBIAN-CENOMANIAN STRATA OF GAZAK, SOUTH KERMAN, SE IRAN,” GEOSCIENCES, vol. 24, no. 95 (STRATIGRAPHY & SEDIMENTOLOGY), pp. 145–152, 2015, [Online]. Available: https://sid.ir/paper/31586/en

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