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Relevant bibliographies by topics / Calcareous red algae

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Academic literature on the topic 'Calcareous red algae'

Author: Grafiati

Published: 4 June 2021

Last updated: 26 July 2025

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Journal articles on the topic "Calcareous red algae"

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Rajanikanth, A. "Rock building Cretaceous - Tertiary algae from India - an ecological perspective." Journal of Palaeosciences 40 (December 31, 1991): 399–412. http://dx.doi.org/10.54991/jop.1991.1790.

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Fossil benthonic photosynthetic algae capable of calcification contributed to the formation of Indian Cretaceous-Tertiary carbonate deposits. A comparative assessment of different marine calcareous algal assemblages known from various sedimentary basins and their ecological requirements have been highlighted. A comprehensive synthesis and retrospect of research on calcareous algae demonstrate extensive growth of green and red algae during Cretaceous-Tertiary times in India. The calcareous blue-green algae are feebly represented in the Cretaceous deposits and not recorded from the Tertiary depo

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Zakiryanov, I. G., V. A. Luchinina, and N. V. Sennikov. "MICROFACIES AND PALEOALGOLOGICAL COMPLEXES OF CARBONATES OF THE UPPER ORDOVICIAN TACHALOV SECTION (WEST OF GORNY ALTAI)." Geology and mineral resources of Siberia 2, no. 4 (2023): 109–18. http://dx.doi.org/10.20403/2078-0575-2023-4b-109-118.

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The article presents the study results of carbonaceous rocks and taxonomic diversity of the Upper Ordovician calcareous algae of the Tachalov section left half, located on the left side of the same-name creek in the central district of the Charysh-Inya structure-facies zone of Gorny Altai. Six microfacies are distinguished in rocks: algal-bacterial boundstones, crinoid mudstones, crinoid-algal wackestones, polybioclastic wackestones, crinoid-algal packstone-wackestones and crinoid-algal packstones. Calcareous algae of the following genera were recorded in limestones: Proaulopora Volgdin, 1934

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Shen, Yuefeng, and Fritz Neuweiler. "Taphocoenoses and diversification patterns of calcimicrobes and calcareous algae, Ordovician, Tarim Basin, China." Canadian Journal of Earth Sciences 53, no. 7 (2016): 702–11. http://dx.doi.org/10.1139/cjes-2015-0173.

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Despite the crucial role of epibenthic primary producers (cyanobacteria, green and red algae), no diversity curves for calcimicrobes and calcareous algae are available to assess the pyramiding paleoecology characterizing the Ordovician biodiversification episode. A total of 24 taxa of calcimicrobes and calcareous algae are identified from a Dapingian to lower Katian succession of carbonate sedimentary rocks exposed at the Leyayilitag ridge, Bachu Uplift, Tarim Basin, northwest China. Calcimicrobes (14 taxa), Dasycladales (seven taxa), Bryopsidales (one taxon), and Cyclocrinales (two taxa) cont

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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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Gusarova, Anastasiia D. "Calcareous algae and foraminifera of the microfaunistic horizon XIII (Visean stage) of the middle part of the central paraxial zone Dnipro-Donets Depression (Ukraine)." Journal of Geology, Geography and Geoecology 31, no. 2 (2022): 233–50. http://dx.doi.org/10.15421/112222.

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   Visean deposits of exploration-production well 363 Yablunivs’ka contain predominantly carbonate and argillaceous rocks from the Prylutsʹkyy boundary (lower Visean). This study presents limestone microfacies and foraminiferal and calcareous algal associations of the paraxial zone in the Dnipro-Donets Depression. The foraminiferal association is represented by 26 genera, whereas the algal association is composed of 24 identified species and specimens in open nomenclature representative of 31 genera, including a new species, Atractyliopsis berezovia sp. nov., and a species of

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6

Kuss, J., and M. A. Conrad. "Calcareous algae from Cretaceous carbonates of Egypt, Sinai, and southern Jordan." Journal of Paleontology 65, no. 5 (1991): 869–82. http://dx.doi.org/10.1017/s0022336000037847.

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Calcareous algae are frequent constituents in the shallow-marine limestone intercalations of late Aptian–Maastrichtian strata of the Eastern Desert of Egypt, the Sinai, and southern Jordan. A total of 18 species of green algae (among them 16 dasycladaceans withPraturlonella hammudain. comb. andPraturlonella jordanican. sp., two udoteaceans) and eight species of red algae (among them two gymnocodiaceans, three solenoporaceans, and one squamariacean) are described and compared with algae from several Tethyan occurrences. The stratigraphic distribution is calibrated by 10 assemblage-zones based o

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Matveeva, N., and R. Ivanova. "Early Asselian cyanobacteria and algae in the organogenic buildups of the section «Pisanyi Kamen’» (Un’ya River, Northern Urals)." Vestnik of geosciences, no. 12 (February 11, 2025): 26–36. https://doi.org/10.19110/geov.2024.12.3.

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The paper presents the results of the study of the remains of cyanobacteria and calcareous algae of the Lower Permian organogenic buildups from the “Pisanyi Kamen’” section at the Un’ya River (Northern Urals). The microscopic study allowed extending taxonomic composition of Early Permian cyanobacteria and algae in the buildups: 3 genera of cyanobacteria, 12 genera of green algae, 2 genera of red algae and 4 genera of unclear systematic position were identified. It was revealed that representatives of green algae of the families Dasycladaceae and Cyclocrinaecae mainly participated in the format

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Basso, Daniela. "Carbonate production by calcareous red algae and global change." Geodiversitas 34, no. 1 (2012): 13–33. https://doi.org/10.5252/g2012n1a2.

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Sukhov, Oleh A., and Anastasiia D. Gusarova. "New data on red Visean calcareous algae of the Dnipro-Donetsk Depression: systematic composition and facial confinement." Journal of Geology, Geography and Geoecology 32, no. 2 (2023): 396–410. http://dx.doi.org/10.15421/112336.

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   As a result of the study of the core material of 540 thin sections from the boreholes of the northern marginal part and the paraxial part of the Dnieper-Donetsk Depression (DDD), a complex of fossil red calcareous algae including 14 species of 7 genera, as well as 2 species belonging to 2 genera identified for the first time for the Visean deposits of the DDD has been discovered. The studied carbonate deposits represent the Hlybokynskyi, Sukhynskyi, Stylskyi, Donetskyi and lower part of Mezhivskyi horizons of the Don-Dnipro Rift (DDR). It has been found that the greatest d

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Basso, Daniela. "Carbonate production by calcareous red algae and global change." Geodiversitas 34, no. 1 (2012): 13–33. http://dx.doi.org/10.5252/g2012n1a2.

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Dissertations / Theses on the topic "Calcareous red algae"

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Alexander, Paul. "The responses of crops and soils to calcified seaweed." Thesis, University of Wolverhampton, 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.323090.

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Book chapters on the topic "Calcareous red algae"

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Potin, P., J. Y. Floc’h, C. Augris, and J. Cabioch. "Annual growth rate of the calcareous red alga Lithothamnion corallioides (Corallinales, Rhodophyta) in the Bay of Brest, France." In Thirteenth International Seaweed Symposium. Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-009-2049-1_37.

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Dias, Gilberto Tavares de Macedo. "Explotação de Granulados Bioclásticos - Algas Calcárias." In Recursos Minerais Marinhos. Sociedade Brasileira de Geofísica - SBGf, 2023. http://dx.doi.org/10.22564/sbgfbook.cad5.2023.cap6.

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As algas calcárias vermelhas (coralline algae), são compostos biogênicos, formados por material mineral, a calcita magnesiana (> 95%). As formas livres destas algas incrustantes (rodolitos e maerl) e seus fragmentos sedimentares (cascalho de algas, granulado, agregado bioclástico) constituem a principal matéria-prima para extração mineral. A explotação das algas foi intensa na França e na Inglaterra, desde o século XVII. Na década de 70 na França extraía-se 600 mil ton./ano. A interdição total da extração na França, no final de 2013, deu-se para evitar o total desaparecimento das algas calc

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Almeida, Narelle Maia, George Satander Sá Freire, Vanessa Maria Mamede Cavalcanti, João Capistrano Abreu Neto, and Isabelly Maria Maia Ferro. "Granulados Siliciclásticos." In Recursos Minerais Marinhos. Sociedade Brasileira de Geofísica - SBGf, 2023. http://dx.doi.org/10.22564/sbgfbook.cad5.2023.cap7.

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As algas calcárias vermelhas (coralline algae), são compostos biogênicos, formados por material mineral, a calcita magnesiana (> 95%). As formas livres destas algas incrustantes (rodolitos e maerl) e seus fragmentos sedimentares (cascalho de algas, granulado, agregado bioclástico) constituem a principal matéria-prima para extração mineral. A explotação das algas foi intensa na França e na Inglaterra, desde o século XVII. Na década de 70 na França extraía-se 600 mil ton./ano. A interdição total da extração na França, no final de 2013, deu-se para evitar o total desaparecimento das algas calc

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Sheppard, Charles. "4. The resulting structure—a reef." In Coral Reefs: A Very Short Introduction. Oxford University Press, 2021. http://dx.doi.org/10.1093/actrade/9780198869825.003.0004.

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Reef profiles are remarkably consistent in general design because they are essentially biological constructions responding to environmental factors. All have reef flats, a horizontal expanse at low tide level that develops when the reef can no longer build upwards and extends horizontally. This is commonly the largest expanse and is the only part that early naturalists could examine until the advent of scuba diving relatively recently. However, it is always relatively depauperate because of the extremes of heat, salinity, and light that affect it. To seaward is the reef crest, commonly constru

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Pomar, Luis, Juan Ignacio Baceta, and G. Mateu-Vicens. "The upper Miocene reef-rimmed platform of Mallorca (Spain): factory structure, growth dynamics and diagenesis." In Field guides to exceptionally exposed carbonate outcrops. International Association of Sedimentologists, 2021. http://dx.doi.org/10.54780/iasfg3/13.

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The Llucmajor platform on southern Mallorca Island (Spain) is one of the best-exposed Miocene shallow-water carbonate platforms known in the world. Up to 90 m vertical sea cliffs provide a clean, continuous and detailed 3D view of the facies architecture and continuous cores from fifty-two water wells, affording information to interpret the 3D architecture of this 20 km-wide and only slightly deformed carbonate platform. Forty years of research on the Llucmajor platform provided insights into how the mutual interaction of biological and physical processes control the type of carbonate producti

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