Search results for: cruziana

Authors: Waleed Sulaiman Shingaly

Abstract:

The Ordivician-Khabour Formation from the Northern Thrust Zone of Iraqi-Kurdistan comprises between 500 and 800 m of alternating predominantly greenish-grey sandstones, siltstones and shales. The succession has revealed an abundant ichnofossils characterized by 11 ichnogenus, namely: Helminthopsis, Gordia, Cruziana, Rusophycus, Monomorphichnus, Rhizocorallium, Thalassinoide, Planolite, Paleophycus, Deplocraterion and Skolithose. Ethologically these ichnogenera display dwelling and feeding activities of the infaunal organisms. This association of ichnofossils contains elements of the Skolithose and Cruziana ichnofacies. The presence of Skolithos ichnofacies indicates sandy shifting substrate and high energy conditions in foreshore zone while the Cruziana ichnofacies indicate unconsolidated, poorly sorted soft substrate and low energy condition in the shore face/offshore zone. These ichnogenera indicate shoreface-offshore zone of shallow-marine environment for the deposition of the rocks of the Khabour Formation.

Keywords: Ichnofossils, shoreface-offshore zone, Khabour Formation, Iraq

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Authors: C. A. Sharma, Birendra P. Singh

Abstract:

Ichnofacies analysis is considered the best paleontological tool for interpreting ancient depositional environments. Nineteen (19) ichnogenera (namely: Bergaueria, Catenichnus, Cochlichnus, Cruziana, Diplichnites, Dimorphichnus, Diplocraterion, Gordia, Guanshanichnus, Lockeia, Merostomichnites, Monomorphichnus, Palaeophycus, Phycodes, Planolites, Psammichnites, Rusophycus, Skolithos and Treptichnus) are recocered from the Tal Group (Cambrian) of the Nigalidhar Syncline. The stratigraphic occurrences of these ichnogenera represent alternating proximal Cruziana and Skolithos ichnofacies along the contact of Sankholi and Koti-Dhaman formations of the Tal Group. Five ichnogenera namely Catenichnus, Guanshanichnus, Lockeia, Merostomichnites and Psammichnites are recorded for the first time from the Nigalidhar Syncline. Cruziana ichnofacies is found in the upper part of the Sankholi Formation to the lower part of the Koti Dhaman Formation in the NigaliDhar Syncline. The preservational characters here indicate a subtidal environmental condition with poorly sorted, unconsolidated substrate. Depositional condition ranging from moderate to high energy levels below the fair weather base but above the storm wave base under nearshore to foreshore setting in a wave dominated shallow water environment is also indicated. The proximal Cruziana-ichnofacies is interrupted by the Skolithos ichnofacies in the Tal Group of the Nigalidhar Syncline which indicate fluctuating high energy condition which was unfavorable for the opportunistic organism which were dominant during the proximal Cruziana ichnofacies. The excursion of Skolithos ichnofacies (as a pipe rock in the upper part of Sankholi Formation) into the proximal Cruziana ichnofacies in the Tal Group indicate that increased energy and allied parameters attributed to the high rate of sedimentation near the proximal part of the basin. The level bearing the Skolithos ichnofacies in the Nigalidhar Syncline at the juncture of Sankholi and Koti-Dhaman formations can be correlated to the level marked as unconformity in between the Deo-Ka-Tibba and the Dhaulagiri formations by the conglomeratic horizon in the Mussoorie Syncline, Lesser Himalaya, India. Thus, the Tal Group of the Nigalidhar syncline at this stratigraphic level represent slightly deeper water condition than the Mussoorie Syncline, where in the later the aerial exposure dominated which leads to the deposition of conglomeratic horizon and subsequent formation of unconformity. The overall ichnological and sedimentological dataset allow us to infer that the Cambrian successions of Nigalidhar Syncline were deposited in a wave-dominated proximal part of the basin under the foreshore to close to upper shoreface regimes of the shallow marine setting.

Keywords: Cambrian, Ichnofacies, Lesser Himalaya, Nigalidhar, Tal Group

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Authors: Otosigbo Gloria Ogochukwu, Ehinola Olugbenga Ajayi, Gingras Murray K.

Abstract:

The ichnofossil assemblages of Cretaceous Abeokuta Group from Southeastern Dahomey have not been documented in the literature. This can be traced to deficit of outcrops from the onshore, and also scarce cores from the offshore wells. Ichnofossils and sediment are inseparable and significant in effective interpretation of depositional settings. The ichnology of the tide-dominated estuary to wave-dominated shoreface of offshore Abeokuta Group revealed a brackish water types. The bioturbation is mostly controlled by tidal sedimentation and the vertical succession through the cores within the tide-dominated estuary exhibits regular heterogeneous bioturbations. These are alternations of bioturbated and non-bioturbated units or highly bioturbated and scarce bioturbated alternations. The bioturbations within the wave -dominated shoreface is low to moderate at the lower units but scarce at the upper shoreface. Abeokuta Group sediment are mostly massive sandstone alternations with mud-rich heterolithic facies, sand-rich heterolithic and inclined heterolithic stratifications and shaly fine grained sandstone beds. The ichnofossils observed in Abeokuta Group are basically simple structured, stressed and of low diversity which belong to soft ground, loose ground and firm (substrate controlled) suites. Eleven ichnogenera were identified such as; Asterosoma, Chondrites, Ophiomorpha, Palaeophycus, Planolites, Phycosiphon Rhizocorallium, Rosselia, Skolithos, Teichichnus and Thalassinoides. These were grouped into four recurring ichnofacies of Cruziana, Skolithos Skolithos-Cruziana and Glossifungites ichnofacies. The ichnofossils are significant in distinguishing the upper estuarine embayment boundary from shoreface complex by the paucity of suspension feeding structures in delta front and predominance of suspension feeding structures in the shoreface. Also, the firm substrate suite identifies the flooding surface/transgressive surface, and the regressive surface of marine erosion within the intertidal flats and shoreface respectively.

Keywords: estuary, tide, ichnofossils, ichnogenera, ichnofacies, skolithos, cruziana, glossifungites

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Authors: Soheir El-Shazly, Gouda Abdelgawad, Yasser Salama, Dina Sayed

Abstract:

Abstract- The Late Eocene rocks (Qasr El-Sagha ) Formation, north east of Birket Qarun in Fayum area of Egypt reveals 6 Ichnogenera Thalassinoides Ehrenberg, 1944, Ophiomorpha Lundgren (1891), Skolithos Haldemann (1840), Diplocraterion Torell, 1870, Arenicolites Salter, 1857 and Planolites Nicholson, 1873. These Ichnogenera are related to Skolithos ichnofacies of typical sandy shoreline environment, only the ichnogenus Planolites is related to Cruziana ichnofacies, which occurs in somewhat deeper water than the Skolithos ichnofacies. Four microfacies types have been distinguished from the study sections, Mudstone, Sandy micrite (wackstone), Sandy dolomitic ferruginous biomicrite (Packstone), Sandy glauconitic biomicrite (packstone). The ichnofacies and the microfacies study indicates that the study area was deposited in shelf lagoon with open circulation environment

Keywords: Egypt, Fayum, icnofacies, late eocene, microfacies

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