Academic literature on the topic 'Sakmarian'

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Journal articles on the topic "Sakmarian"

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Kobayashi, Fumio. "Early Permian (Sakmarian, Artinskian, Kungurian) foraminifers and Biostratigraphy of the Akiyoshi Limestone (Japan)." Revue de Paléobiologie 39, no. 2 (2020): 501–63. https://doi.org/10.5281/zenodo.4460706.

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Carboniferous and Permian carbonate sequences in Japan are most completely preserved in the Akiyoshi Limestone in the Akiyoshi Terrane (Permian accretionary complex), Southwest Japan. The studied Sakmarian to lower Kungurian sequence is biostratigraphically divided into six zones: Globifusulina nux Zone and Globifusulina krotowi Zone (Sakmarian), Chalaroschwagerina vulgaris Zone (lower to middle Artinskian), Paraleeina magna Zone (upper Artinskian), Pamirina leveni Zone (uppermost Artinskian), and Miselllina dyhrenfurthi Zone (lower Kungurian) based on stratigraphic distribution and species co
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Boardman, Darwin R. ,. II, Bruce R. Wardlaw, and Merlynd K. Nestell. "Part B: Conodont Distribution, Systematics, Biostratigraphy, and Sequence Stratigaphy of the Uppermost Carboniferous and Lower Permian (uppermost Wabaunsee, Admire, Council Grove, and lower Chase Groups) from the North American Midcontinent." Bulletin (Kansas Geological Survey), no. 255 (January 1, 2009): 1–146. https://doi.org/10.17161/kgsbulletin.no.255.20376.

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aximum-marine flooding levels and marine-condensed sections from uppermost Carboniferous and Lower Permian fourth-order (0.1-1 m.y.) depositional sequences of the North American midcontinent reveal a rich stratigraphic succession of species of Streptognathodus and Sweetognathus conodonts that permits high-precision correlation of the Carboniferous-Permian boundary as well as the Asselian-Sakmarian and Sakmarian-Artinskian boundaries. Eleven new species of Streptognathodus are described: Streptognathodus binodosus, S. denticulatus, S. elongianus, S. florensis, S. lineatus, S. nevaensis, S. post
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Nilsson, I. "Upper Palaeozoic fusulinid assemblages, Wandel Sea Basin, North Greenland." Rapport Grønlands Geologiske Undersøgelse 161 (January 1, 1994): 45–71. http://dx.doi.org/10.34194/rapggu.v161.8243.

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Eight fusulinid assemblages are recognized in the Mallemuk Mountain Group of North Greenland. They are of late Moscovian (Wedekindellina assemblage), late Kasimovian (Rauserites ex. gr. simplex assemblage), early-middle Gzhelian (Rauserites ex. gro rossicus assemblage), late Gzhelian – ?early Asselian (Schellwienia arctica assemblage), early Asselian (Sphaeroschwagerina aff. S. vulgaris assemblage), middle-late Asselian (Schwagerina ex. gro nathorsti assemblage), latest Asselian - earliest Sakmarian (Schwagerina aff. S. moelleri – S. ex. gro exuberate assemblage) and late Sakmarian (Schwagerin
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Angiolini, Lucia, Hugo Bucher, Alain Pillevuit, et al. "Early permian (Sakmarian)brachiopods from southeastern Oman." Geobios 30, no. 3 (1997): 379–405. http://dx.doi.org/10.1016/s0016-6995(97)80199-4.

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Makoshin, V. I., and R. V. Kutygin. "Brachiopods from the Lower Permian of the Khospokhchon Section in the Southern Verkhoyanie (Northeast Russia)." Arctic and Subarctic Natural Resources 28, no. 3 (2023): 367–74. http://dx.doi.org/10.31242/2618-9712-2023-28-3-367-374.

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A biostratigraphic division of the Lower Permian into brachiopod zones of Jakutoproductus verkhoyanicus, Jakutoproductus insignis, Jakutoproductus terechovi, and Jakutoproductus rugosus is observed within the Northern and Western Verkhoyanie. According to the literature, only the complex of the lower biostratigraphic unit (Verkhoyanicus Zone) was previously confidently established in the Southern Verkhoyanie. Meanwhile, representatives of the two middle zones were not observed, and the presence of the index species of the Rugosus zone was only indicated in the southern part of the region (Yudo
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Dzulkafli, Muhammad Ashahadi, Che Aziz Ali, and Mohd Basril Iswadi Basori. "Radiolaria Perm Awal daripada Ladang Harmoni, Pos Blau, Baratdaya Kelantan." Sains Malaysiana 51, no. 7 (2022): 1979–92. http://dx.doi.org/10.17576/jsm-2022-5107-03.

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Radiolaria berusia Sakmarian Awal (Perm Awal) ditemui dalam jujukan rijang yang berselang lapis dengan batu lumpur bertuf daripada Ladang Harmoni, Pos Blau, Gua Musang. Sebanyak 21 spesies radiolaria telah dikenal pasti, terdiri daripada Pseudoalbaillella lomentaria Ishiga & Imoto, Pseudoalbaillella sakmarensis (Kozur), Pseudoalbaillella scalprata postscalprata Ishiga, Pseudoalbaillella cf. internata Wang, Pseudoalbaillella sp. A, Pseudoalbaillella sp. B, Hegleria mammilla (Sheng & Wang), Hegleria sp. A, Ruzhencevispongus rotundus Feng, Ruzhencevispongus girtyi Nazarov & Ormiston,
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Tremblin, Clément Mathieu, and David William Haig. "Evolution of Trochamminoids (Trochospiral Organic-Cemented Agglutinated Foraminifera): Examples from the Lower Permian of Western Australia." Journal of Foraminiferal Research 53, no. 4 (2023): 269–85. http://dx.doi.org/10.61551/gsjfr.53.4.269.

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Abstract Trochamminids are the oldest trochospiral group of foraminifera. An exceptionally well-preserved assemblage, found in the Lower Permian (Sakmarian, ∼294–290 Ma) of Western Australia, includes Trochammina geoffplayfordi n. sp., Trochammina gloveri n. sp., Trochamminopsis teicherti n. sp., and Tritaxis crespinae n. sp. Verispira holmesorum n. sp. seems related to broader Trochamminoidea. These represent the oldest known well-preserved representatives of the superfamily. By the Sakmarian, trochamminids, remarkably like modern species, had developed in a shallow-water interior sea with mu
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OKUYUCU, CENGİZ. "Biostratigraphy and systematics of late Asselian–early Sakmarian (Early Permian) fusulinids (Foraminifera) from southern Turkey." Geological Magazine 145, no. 3 (2008): 413–34. http://dx.doi.org/10.1017/s0016756808004482.

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AbstractThe Anatolian Platform, which was a part of the Gondwanan Platform, is mainly characterized by carbonate-dominated deposits ranging in age from Devonian to Permian. The biostratigraphy and systematics of a late Asselian–early Sakmarian fusulinid fauna from the Anatolian Platform including Eastern and Central Taurides have been investigated in three sections: Özbek Hill, Eskibey and Bademli. Twenty-four fusulinid taxa, belonging to twelve genera, were determined in a single fusulinid zone dated as late Asselian–early Sakmarian. Early–middle Asselian fusulinid faunas have not been observ
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Tremblin, Clément Mathieu, and David William Haig. "Evolution of Trochamminoids (Trochospiral Organic-Cemented Agglutinated Foraminifera): Examples from the Lower Permian of Western Australia." Journal of Foraminiferal Research 53, no. 4 (2023): 269–85. http://dx.doi.org/10.2113/gsjfr.53.4.269.

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Abstract Trochamminids are the oldest trochospiral group of foraminifera. An exceptionally well-preserved assemblage, found in the Lower Permian (Sakmarian, ∼294–290 Ma) of Western Australia, includes Trochammina geoffplayfordi n. sp., Trochammina gloveri n. sp., Trochamminopsis teicherti n. sp., and Tritaxis crespinae n. sp. Verispira holmesorum n. sp. seems related to broader Trochamminoidea. These represent the oldest known well-preserved representatives of the superfamily. By the Sakmarian, trochamminids, remarkably like modern species, had developed in a shallow-water interior sea with mu
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Leonova, T. B., and A. Yu Shchedukhin. "Asselian-Sakmarian Nautiloids of the Shakh-Tau Reef (Bashkortostan)." Paleontological Journal 54, no. 10 (2020): 1113–34. http://dx.doi.org/10.1134/s0031030120100044.

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Dissertations / Theses on the topic "Sakmarian"

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Edwards, David Charles. "Cement reefs." Thesis, Cardiff University, 1990. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.390320.

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Guggino, Steve N. "Seasonality in western equatorial Pangaea during the Early Permian (Upper Sakmarian) [delta]¹⁸O, [delta]¹³C, and elemental analysis of brachiopod shells from the Robledo Mountains, New Mexico, USA /." [Tampa, Fla.] : University of South Florida, 2004. http://purl.fcla.edu/fcla/etd/SFE0000443.

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Guggino, Steve N. "Seasonality in Western Equatorial Pangaea during the Early Permian (Upper Sakmarian): δ18O, δ13C, and Elemental Analysis of Brachiopod Shells from the Robledo Mountains, New Mexico, USA". Scholar Commons, 2004. https://scholarcommons.usf.edu/etd/1059.

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Sclerochronology was conducted on the pedicle valves of four Sakmarian-age brachiopods (Squamaria moorei) to constrain climate model predictions of temperature seasonality along western equatorial Pangaea (WEP). The brachiopods are from a Lower Permian section within the Robledo Mountains, NM, and they reveal seasonal trends of δ18O and temperature for that interval that suggest global warming and moderation of seasonality. Elemental and SEM analyses verified the specimens were well preserved. δ18O profiles show a relatively rapid and consistent two-year growth rate corresponding to the organi
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Schmidt, Isabela Degani. "Múltiplas evidências de perturbações ambientais durante a deposição da turfeira Pós-Glacial (Sakmariano) da Mina de Faxinal, Sul da Bacia do Paraná." reponame:Biblioteca Digital de Teses e Dissertações da UFRGS, 2016. http://hdl.handle.net/10183/143645.

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Perturbações ambientais foram detectadas em sistema de turfeira no sul da Bacia do Paraná (Mina de Faxinal, Formação Rio Bonito) durante o Eopermiano (idade radiométrica 291 ± 1.3 Ma, topo do Sakmariano) sob vigência de período climático pós-glacial da Idade do Gelo do Neopaleozoico. Além da detecção de incêndios recorrentes, foi identificado um evento de incêndio autóctone/hipoautóctone em vegetação arbórea em um horizonte no carvão contendo grandes fragmentos de lenhos queimados comprimidos (21,8 x 13.4 cm). A influência de vulcanismo está registrada sob a forma de uma camada de tonstein (ci
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Book chapters on the topic "Sakmarian"

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Shcherbakova, Natalya, and Alexander Nekrasov. "Rocks’ Lithological Composition Impact on Porosity Illustrated by Sakmarian Age Sulphate-Carbonate Sediments." In Lecture Notes in Networks and Systems. Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-89477-1_36.

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"Sakmarian, adj." In Oxford English Dictionary, 3rd ed. Oxford University Press, 2023. http://dx.doi.org/10.1093/oed/4838077098.

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Beauchamp, Benoit, Daniel Calvo González, Charles M. Henderson, Daria V. Baranova, Hanyue Wang, and Eric Pelletier. "Late Pennsylvanian–Early Permian Tectonically Driven Stratigraphic Sequences and Carbonate Sedimentation Along Northern Margin of Sverdrup Basin (Otto Fiord Depression, Arctic Canada)." In Late Paleozoic and Early Mesozoic Tectonostratigraphy and Biostratigraphy of Western Pangea. SEPM (Society for Sedimentary Geology), 2022. http://dx.doi.org/10.2110/sepmsp.113.12.

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A thick succession of upper Paleozoic carbonate rocks and minor chert crops out north of the head of Otto Fiord (northwest [NW] Ellesmere Island, Nunavut) in the Canadian Arctic Archipelago. These rocks accumulated in a tectonic subbasin—the Otto Fiord Depression (OFD)—of the Sverdrup Basin that likely originated through rifting during late Early Carboniferous (Serpukhovian). Following a long interval of passive subsidence that allowed a thick succession of Moscovian–Kasimovian carbonate rocks to fill the OFD, tectonic activity resumed during the Gzhelian (Late Pennsylvanian). This resulted in
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Beauchamp, Benoit, Charles M. Henderson, Elinda Dehari, Daniela Waldbott Von Bassenheim, Sean Elliot, and Daniel Calvo González. "Carbonate Sedimentology and Conodont Biostratigraphy of Late Pennsylvanian–Early Permian Stratigraphic Sequences, Carlin Canyon, Nevada: New Insights into the Tectonic and Oceanographic Significance of an Iconic Succession of the Basin and Range." In Late Paleozoic and Early Mesozoic Tectonostratigraphy and Biostratigraphy of Western Pangea. SEPM (Society for Sedimentary Geology), 2022. http://dx.doi.org/10.2110/sepmsp.113.14.

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The Gzhelian (Upper Pennsylvanian) to Kungurian (Lower Permian) succession around Carlin Canyon, northern Nevada, in the Basin and Range province of the western USA is a relatively undeformed wedge of fossiliferous marine carbonate and fine-grained calcareous and cherty clastic rocks that rests with profound angular unconformity on Mississippian to mid-Pennsylvanian sedimentary rocks that had been uplifted, faulted, folded, and eroded prior to the Late Pennsylvanian transgression. This wedge of sediments, which tapers over less than 2 km from 1341 m in the west to 588 m in the east, comprises
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Ritter, Scott M., Joshua K. Meibos, and Ty S. Robinson. "Sequence Biostratigraphy of Carboniferous–Permian Boundary Strata in Western Utah: Deciphering Eustatic and Tectonic Controls on Sedimentation in the Antler–Sonoma Distal Foreland Basin." In Late Paleozoic and Early Mesozoic Tectonostratigraphy and Biostratigraphy of Western Pangea. SEPM (Society for Sedimentary Geology), 2022. http://dx.doi.org/10.2110/sepmsp.113.07.

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The stratal architecture of the upper Ely Limestone and Mormon Gap Formation (Pennsylvanian–Lower Permian) in west-central Utah reflects the interaction of icehouse sea-level change and tectonic activity in the distal Antler–Sonoma foreland basin. Nineteen stratigraphic sections correlated by physical and biostratigraphic means provide a basis for tracing Carboniferous–Permian boundary strata over a north–south distance of 60 km. These formations can be subdivided into 14 unconformity-bounded, third-order depositional sequences of differing internal architecture and regional extent. Conodonts
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Guerra-Sommer, M., M. Cazzulo-Klepzig, J. G. Mendonça Filho, et al. "Integration of geochronologic, paleobotanical and organic matter studies in gondwanan tonstein (Sakmarian, Paraná Basin, Brazil)." In Para conhecer a Terra: memórias e notícias de Geociências no espaço lusófono. Imprensa da Universidade de Coimbra, 2012. http://dx.doi.org/10.14195/978-989-26-0534-0_12.

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Whitmore, Ross J., Patricia H. Cashman, and Daniel M. Sturmer. "Structures at Buck Mountain, Nevada: Establishing the Southeastern Extent of Mid-Pennsylvanian Tectonism." In Late Paleozoic and Early Mesozoic Tectonostratigraphy and Biostratigraphy of Western Pangea. SEPM (Society for Sedimentary Geology), 2022. http://dx.doi.org/10.2110/sepmsp.113.06.

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This paper reports the structural and stratigraphic history of Buck Mountain, Nevada, and its regional significance in the development of southwestern Laurentia during the late Paleozoic. The two distinct generations of folding have similar style and/or timing to other fold sets in late Paleozoic strata of northern Nevada. Unconformities in the upper Paleozoic strata at Buck Mountain are consistent with unconformities documented in northern and east-central Nevada. Northwest-vergent folds (F1) in the Morrowan–Atokan Ely Limestone are erosionally truncated and unconformably overlain by the midd
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Conference papers on the topic "Sakmarian"

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Shell, Ryan, David J. Peterman, and Charles N. Ciampaglio. "ADDITIONAL VERTEBRATES FROM THE WREFORD LIMESTONE (PERMIAN: CISURALIAN, SAKMARIAN) OF SOUTHERN KANSAS." In 54th Annual GSA North-Central Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020nc-345715.

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Baraboshkin, E. Y., E. S. Gorbenko, V. K. Piskunov, and E. L. Zaytzeva. "Conceptual Sedimentological Model of Asselian-Sakmarian Deposits of Kharyaga Oil Field (Nenets Autonomous Area)." In 6th Saint Petersburg International Conference and Exhibition. EAGE Publications BV, 2014. http://dx.doi.org/10.3997/2214-4609.20140288.

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Read, Michael T., and Merlynd K. Nestell. "SAKMARIAN (EARLY PERMIAN) SULCUS-BEARING SWEETOGNATHID CONODONTS FROM NEVADA: EARLY EXPERIMENTATION AND NOVEL CARINAL CONFIGURATIONS." In Joint 52nd Northeastern Annual Section and 51st North-Central Annual GSA Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017ne-290430.

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Ryabinkina, N. N., and O. V. Valyaeva. "Oil potential of the Asselian-Sakmarian reefogenic buildups of the Varandey-Adzva zone of the Timan-Pechora Province." In All-Russia Lithological Meeting «Geology of reefs». Institute of Geology FRC Komi SC UB RAS, 2020. http://dx.doi.org/10.19110/98491-013-106-107.

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Massive deposits in reef were discovered in separate fields of Varandey-Adzva zone (Naulskoye, Labaganskoye, etc.). These bodies are represented by organogenic-detrital limestones, fractured with porosity of 8-10%. They have the form of separate buildings, developed locally, wedging out along the strike within the same area. The deposits are confined to the secondary reservoirs of the pore and pore-fracture type.
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Reports on the topic "Sakmarian"

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Beauchamp, B., C. T. Sherry, U. Mayr, J. C. Harrison, and A. Desrochers. Moscovian (Upper Carboniferous) to Sakmarian (Lower Permian) stratigraphy (Nansen and Hare Fiord formations; Unit C2), Hvitland Peninsula, northwestern Ellesmere Island, Arctic Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1995. http://dx.doi.org/10.4095/202795.

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