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Relevant bibliographies by topics / Coralline red-algae facies

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Academic literature on the topic 'Coralline red-algae facies'

Author: Grafiati

Published: 9 March 2023

Last updated: 31 July 2025

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Journal articles on the topic "Coralline red-algae facies"

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Rahiminejad, Amir Hossein, Mehdi Yazdi, and Amit Kumar Ghosh. "Paleoecology of Lower Miocene coralline red algae-rich grainstone facies in the Qom Formation (Vartun section, central Iran)." Boletín de la Sociedad Geológica Mexicana 74, no. 2 (2022): A020122. http://dx.doi.org/10.18268/bsgm2022v74n2a020122.

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In this paleoecological study we focused on coralline red algae-rich shoal grainstone facies in the Lower Miocene (Aquitanian) carbonates of the Qom Formation in the Vartun section in central Iran. The identified coralline red algae are mainly non-geniculate, although very rare geniculate forms of corallines were also recognized in thin section analysis. The identified algae are represented by Melobesioideae (Lithothamnion cf. valens, Lithothamnion cf. rovereoti, Lithothamnion cf. peleense, and Lithothamnion spp.), Mastophoroideae (Neogoniolithon sp., Spongites spp., and Spongites cf. fruticul

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Sarkar, Suman, Amit K. Ghosh, and Madhav Kumar. "Recognition of algal rich facies from the Umlatdoh Limestone of Shella Formation, Jaintia Group, Meghalaya." Journal of Palaeosciences 60, no. (1-2) (2011): 315–21. http://dx.doi.org/10.54991/jop.2011.178.

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The carbonate rocks of the Shella Formation (Middle Eocene) belonging to the Jaintia Group in the Jaintia Hills of Meghalaya are represented by two sandstone units in alternation with three limestone units, viz. Lakadong Limestone, Umlatdoh Limestone and Prang Limestone respectively in chronological order. Umlatdoh Limestone, the middle limestone unit of Shella Formation is conformably underlain by the Lakadong Sandstone and overlain by Narpuh Sandstone. Samples from the Umlatdoh Limestone were collected from the outcrop on the Jowai-Badarpur Road, about 1 km southwest of Lumshnong. Calcareous

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Coletti, Giovanni, Giulia Bosio, Alberto Collareta, John Buckeridge, Sirio Consani, and Akram El Kateb. "Palaeoenvironmental analysis of the Miocene barnacle facies: case studies from Europe and South America." Geologica Carpathica 69, no. 6 (2018): 573–92. http://dx.doi.org/10.1515/geoca-2018-0034.

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Abstract Acorn barnacles are sessile crustaceans common in shallow-water settings, both in modern oceans and in the Miocene geological record. Barnacle-rich facies occur from polar to equatorial latitudes, generally associated with shallow-water, high-energy, hard substrates. The aim of this work is to investigate this type of facies by analysing, from the palaeontological, sedimentological and petrographical points of view, early Miocene examples from Northern Italy, Southern France and South-western Peru. Our results are then compared with the existing information on both modern and fossil b

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Bassi, Davide, and James H. Nebelsick. "Components, facies and ramps: Redefining Upper Oligocene shallow water carbonates using coralline red algae and larger foraminifera (Venetian area, northeast Italy)." Palaeogeography, Palaeoclimatology, Palaeoecology 295, no. 1-2 (2010): 258–80. http://dx.doi.org/10.1016/j.palaeo.2010.06.003.

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Mohammadi, Ebrahim, and Hamed Ameri. "Foraminiferal Biostratigraphy and Paleoecology of the Southeasternmost Outcrops of the Oligocene Qom Formation, SE Iran." Journal of the Geological Society of India 100, no. 1 (2024): 115–26. http://dx.doi.org/10.17491/jgsi/2024/172988.

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Abstract The Qom Formation is deposited along more than 1800 km of the NE margin of the Tethyan Seaway in the Oligocene-Early Miocene during the final sea transgression on the Iranian Plate. We present (foraminiferal-based) biostratigraphic data from three exposed sections near the northwestern Jazmurian Lake, as the southeasternmost outcrops of the Qom Formation. Larger benthic foraminifera are mainly represented by nummulitids (Nummulites, Operculina, Heterostegina), lepidocyclinids (Nephrolepidina, Eulepidina, Lepidocyclina), and Amphistegina. The presence of Nummulites fichteli/intermedius

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Dissertations / Theses on the topic "Coralline red-algae facies"

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BRACCHI, VALENTINA ALICE. "The pleistocene marine terraces of Le Castella and Capo Colonna (Calabria, Southern Italy): a paleoecological study of the coralligenous build-ups and associated bioclastic facies." Doctoral thesis, Università degli Studi di Milano-Bicocca, 2012. http://hdl.handle.net/10281/28152.

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Autochthonous carbonate build-ups are mainly formed by encrusting coralline algae, which are one of the most important carbonate sediment contributors in the benthic communities of the Mediterranean area. They represent one of the most productive ecosystems in temperate regions and currently develop on Mediterranean hard and soft bottoms with a patch distribution along the coast. Several types of assemblages have been described so far, due to the high heterogeneity of coralline growth-forms, distributed from the intertidal down to 160 m water depth, from rhodolith-beds to coralligenous build

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Book chapters on the topic "Coralline red-algae facies"

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Wannier, Mario M. A. "Stratigraphy, Sedimentology, and Ecology of the Subis Limestone and the Late Oligocene/Early Miocene Carbonates in the Sarawak Basin (Borneo, Malaysia)." In Cenozoic Isolated Carbonate Platforms—Focus Southeast Asia. SEPM (Society for Sedimentary Geology), 2023. http://dx.doi.org/10.2110/sepmsp.114.02.

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Shallow marine mixed siliciclastic–carbonate shoals, a carbonate platform, and the subsequent development of a reefal buildup occur in sequence from the late Chattian to the Aquitanian in the Niah area of Sarawak. They document the transition from larger foraminifera-dominated, calcitic environments to scleractinian coral–dominated, aragonitic environments in SE Asia, which correspond to a significant increase in biodiversity. A late Chattian to early Aquitanian phase of carbonate sedimentation was initiated by larger foraminifera on shallow marine argillaceous shoals raising from the seabed a

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