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Littérature scientifique sur le sujet « Coniacian-Santonian »

Auteur : Grafiati

Publié le 9 mars 2023

Mis à jour le 31 juillet 2025

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Articles de revues sur le sujet "Coniacian-Santonian"

Hildebrand-Habel, Tania, and Helmut Willems. "New calcareous dinoflagellates (Calciodinelloideae) from the Middle Coniacian to Upper Santonian chalks of Lägerdorf (northern Germany)." Journal of Micropalaeontology 23, no. 2 (2004): 181–90. http://dx.doi.org/10.1144/jm.23.2.181.

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Abstract. Three new calcareous dinoflagellate species from the Middle Coniacian to Upper Santonian chalks of Lägerdorf (northern Germany) are formally described: Calcicarpinum macrogranulum n. sp., Pirumella fragilis n. sp. and Ruegenia quinqueangulata n. sp. The species show differing vertical distribution patterns which might result from local sea-level changes: P. fragilis and R. quinqueangulata are restricted to the possibly transgressive upper Mid-Coniacian to Lower Santonian interval and C. macrogranulum occurs consistently only in the probably regressive lower Mid-Coniacian and Middle t

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Ismail, Ahmed Aly. "A New Epistemological Insight of the Coniacian-Santonian Oceanic Anoxic Event (OAE3)." American Journal of BioScience 12, no. 1 (2024): 22–34. http://dx.doi.org/10.11648/j.ajbio.20241201.14.

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Eighteen planktic and eleven benthic foraminiferal species were recorded from the dark grey to black shale facies of the Matulla Formation in Abu Zeneima area, West-Central Sinai, Egypt. The faunal assemblage is dominated by cosmopolitan whiteinellids, marginotruncanids, Dicarinellids, Contusotruncanids and Heterohelicids. The planktic species with high taxonomic diversity were used to zone the Coniacian and Santonian stages, as well as define the Coniacian/ Santonian boundary, while benthic foraminifera is of minor contribution in age assignment. The stratigraphic analysis of the relations an

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Jimenez, Monica, Simon P. Holford, Rosalind C. King, and Mark A. Bunch. "Controls on gravity-driven normal fault geometry and growth in stacked deltaic settings: a case study from the Ceduna Sub-basin." APPEA Journal 61, no. 2 (2021): 632. http://dx.doi.org/10.1071/aj20073.

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Kinematics of gravity-driven normal faults exerts a critical control on petroleum systems in deltaic settings but to date has not been extensively examined. The Ceduna Sub-basin (CSB) is a passive margin basin containing the White Pointer (Albian-Cenomanian) and Hammerhead (Campanian-Maastrichtian) delta systems that detach on shale layers of Albian-Cenomanian and Turonian-Coniacian ages, respectively. Here we present evidence for spatially variable fault growth styles based on interpretation of the Ceduna 3D seismic survey and fault kinematic analyses using displacement–distance, displacement

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Kennedy, W. J., and W. K. Christensen. "Coniacian and Santonian ammonites from Bornholm, Denmark." Bulletin of the Geological Society of Denmark 38 (February 19, 1991): 203–26. http://dx.doi.org/10.37570/bgsd-1990-38-19.

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The ammonite faunas from the Amager Limestone and Bavnodde Greensand Formations of the island of Bornholm, Denmark are described. The Amager Limestone at its type locality has yielded five species, including the age diagnostic Scaphites (Scaphites) kieslingswaldensis kieslingswaldensis · Langenhan & Grundey, 1891 and Peroniceras tridorsatum (Schliiter, 1867). The Bavnodde Greensand has yielded seven species, including Scaphites (Scaphites) kieslingswaldensis fischer Riede!, 1931, which firs! appears in the Lower Santonian elsewhere in Europe. The age of the two formations is discussed. The

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Tröger, Karl-Armin, and Walter Kegel Christensen. "Upper Cretaceous (Cenomanian-Santonian) inoceramid bivalve faunas from the island of Bornholm, Denmark. With a review of the Cenomanian-Santonian lithostratigraphic formations and locality details." Danmarks Geologiske Undersøgelse Serie A 28 (June 30, 1991): 1–47. http://dx.doi.org/10.34194/seriea.v28.7048.

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The inoceramid bivalve faunas from the Arnager Greensand, Arnager Limestone, and Bavnodde Greensand Formations of the island of Bornholm, Denmark are described. The fauna from the basal part of the Arnager Greensand s. str. is from the Lower Middle Cenomanian and includes Inoceramus crippsi Mantell, /. crippsi hoppenstedtensis Trager, and I. schoendorfi Heinz. The Arnager Limestone at its type locality immediately west of Arnager yielded a diverse fauna, including /. waltersdorfensis cf. hannovrensis Heinz, /. lusatiae Andert, I. cf. rotundatus Fiege, /. striatoconcentricus Gumbel, I. (Herocer

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Nachev, Ivan, and Ekaterina Dimitrova. "Upper Cretaceous stratigraphy of the Eastern Sredna Gora Zone." Geologica Balcanica 25, no. 3-4 (1995): 3–26. http://dx.doi.org/10.52321/geolbalc.25.3-4.3.

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The litostratigraphic subdivision includes the Kardif (Cenomanian?), Cerovska (Cenomanian, Turonian), Gradište (Coniacian, Santonian), Kubadin (Coniacian-Campanian), Sinemorec (Coniacian-Campanian), Izgrev (Coniacian-Campanian), Glušnik (Campanian), Konjovo (Campanian) and Dryankovec (Maastrichtian) Formations. The chronostratigraphy is based on microfaunistic (foraminifers) associations. The Cenomanian consists of limnic and coal-bearing undated rocks (Kardif Formation) or of shallow-marine dated clastic rocks and limestones (Cerovska Formation). The Turonian includes the upper part of the sh

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Dhondt, Annie V., Marcos A. Lamolda, and Jose Maria Pons. "Stratigraphy of the Coniacian–Santonian transition." Cretaceous Research 28, no. 1 (2007): 1–4. http://dx.doi.org/10.1016/j.cretres.2006.05.015.

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Nachev, Ivan, and Ekaterina Dimitrova. "Upper Cretaceous stratigraphy of the Eastern Balkan Mountains." Geologica Balcanica 25, no. 5-6 (1995): 43–74. http://dx.doi.org/10.52321/geolbalc.25.5-6.43.

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The lithostratigraphic subdivision of the Upper Cretaceous in the Eastern Balkan Mountains includes the Balkanbas (Cenomanian?), Dobromir (Cenomanian, partly Turonian), Radova (partly Turonian – Santonian), Trânak (partly Turonian – Coniacian), Karaveljovo (Coniacian, Santonian) and Emine (partly Turonian – Maastrichtian) Formations. The chronostratigraphy is based on foraminiferal microfauna. The Cenomanian is represented by limnic conglomerates, sandstones, siltstones and shales with coals, as well as of shallow-marine clastic, argillaceous and calcareous rocks. The Turonian includes the upp

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Akinin, V. V., L. B. Golovneva, and S. V. Shchepetov. "Isotopic age of flora-bearing beds from the Amka Formation stratotype, Okhotsk-Chukotka volcanic belt." Palaeobotany 7 (2016): 38–46. http://dx.doi.org/10.31111/palaeobotany/2016.7.38.

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U-Pb SHRIMP-dating of zircons from flora-bearing volcanic rocks of the Amka Formation stratotype (Ul'ya depression, Okhotsk-Chukotka volcanic belt) yield weighted mean 206Pb/238U age of 85.5 ±2 Ma (Santonian to Coniacian stage). This isotope dating is consistent with inferred Coniacian age of Ul’ya flora from the Amka Formation.

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Remin, Zbyszek, Michał Gruszczyński, and Jim D. Marshall. "Changes in paleo-circulation and the distribution of ammonite faunas at the Coniacian–Santonian transition in central Poland and western Ukraine." Acta Geologica Polonica 66, no. 1 (2016): 107–24. http://dx.doi.org/10.1515/agp-2016-0006.

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Abstract Ammonite distribution patterns and carbon and oxygen stable isotopes from the Lipnik-Kije (Poland) and Dubovcy (Ukraine) sections allow us to propose a model of sea water paleo-circulation in central Europe for the Coniacian- Santonian interval. The tectonic evolution of the south-eastern part of Poland, and expansion of the Krukienic Island areas, appears to have been one of the most important factors affecting paleotemperatures and the distribution of ammonite faunas in the shallow, epicontinental sea in this part of Europe. In the Lipnik-Kije section, low-latitude Tethyan ammonites

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Thèses sur le sujet "Coniacian-Santonian"

MINIATI, FRANCESCO. "CALCAREOUS NANNOFOSSIL BIOSTRATIGRAPHY AND PALEOECOLOGY OF THE LATE TURONIAN TO EARLY CAMPANIAN INTERVAL AND OF OCEANIC ANOXIC EVENT 3." Doctoral thesis, Università degli Studi di Milano, 2021. http://hdl.handle.net/2434/826218.

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Il Cretacico si caratterizza per la presenza di diversi intervalli di alterazione del sistema climatico-oceanico a scala globale responsabili della deposizione di black-shale marini ricchi di carbonio, definiti come Eventi Anossici Oceanici (OAEs). L’OAE3 rappresenta l’ultimo episodio di diffusa anossia durante l’intervallo Coniaciano-Santoniano. Rispetto ai precedenti eventi anossici, l’OAE3 ha una estensione regionale, ma non globale, poiché risulta essere confinato all’Oceano Atlantico sud-equatoriale e ad alcuni bacini limitrofi (es: Bacino Caraibico, Bacino del Western Interior). Altre im

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Livres sur le sujet "Coniacian-Santonian"

Christensen, Walter Kegel. Coniacian and Santonian belemnite faunas from Bornholm, Denmark. Scandinavian University Press, 1997.

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Kennedy, W. J., W. K. Christensen, and M. G. Schulz. Coniacian and Santonian Belemnite Faunas from Bornholm/Santonian to Maastrichtian Ammonites from Scania, Number 44 (Fossils and Strata Monograph Series). Wiley-Blackwell, 2006.

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Chapitres de livres sur le sujet "Coniacian-Santonian"

Bomou, Brahimsamba, Thierry Adatte, and Jorge E. Spangenberg. "Palaeoenvironmental and Palaeontological Study of the Gabal Ekma Section (Egypt) Throughout the Coniacian-Santonian Boundary." In The Phanerozoic Geology and Natural Resources of Egypt. Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-030-95637-0_11.

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"Coniacian-Santonian." In Dictionary Geotechnical Engineering/Wörterbuch GeoTechnik. Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-41714-6_34155.

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Cooper, M. R. "Late Coniacian - Middle Santonian." In The Cretaceous Fossils of South-Central Africa: an illustrated guide. CRC Press, 2018. http://dx.doi.org/10.1201/9780429442971-41.

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Christensen, Walter Kegel, and Max-Gotthard Schulz. "Coniacian and Santonian belemnite faunas from Bornholm Denmark." In Fossils and Strata. Scandinavian University Press, 1997. http://dx.doi.org/10.18261/8200376958-1997-01.

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WAGREICH, MICHAEL. "Coniacian–Santonian Oceanic Red Beds and Their Link to Oceanic Anoxic Event 3." In Cretaceous Ocean Redbeds. SEPM (Society for Sedimentary Geology), 2009. http://dx.doi.org/10.2110/sepmsp.091.225.

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Danwazan, Jerry, Adesina Mutiu Adeleye, Trust-Paul Bakyu, Mamidak M. Iliya, and Joseph Kehinde Egunjobi. "Perspective Chapter: Understanding Thermal Maturity Evolution and Hydrocarbon Cracking – Implication for Cretaceous Awgu and Nkporo Shales, Southeastern Nigeria." In Recent Oil Spill Challenges That Require More Attention. IntechOpen, 2023. http://dx.doi.org/10.5772/intechopen.106674.

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One-dimensional basin modeling was carried out using Schlumberger’s PetroMod modeling software that provided understanding on the thermal evolution, timing of hydrocarbon generation and expulsion of the Coniacian Awgu Shale and the Campanian Nkporo Shale penetrated by Nzam-1 and Akukwa-2 wells in the lower Benue Trough, Nigeria. The burial temperature and vitrinite reflectance values ranged from 30 to 145°C and 0.5 to 2.9%Ro for Awgu Formation, 28 to 125°C and 0.5 to 1.5%Ro for Nkporo Formation in Nzam-1 well model; 29.5 to 145°C and 0.8 to 2.4%Ro for Awgu Formation, and 28.5 to 95°C and 0.6 t

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"A CRITICAL EVALUATION OF PLANKTONIC FORAMINIFERAL BIOSTRATIGRAPHY ACROSS THE CONIACIAN–SANTONIAN BOUNDARY INTERVAL IN SPAIN, TEXAS, AND TANZANIA." In GEOLOGIC PROBLEM SOLVING WITH MICROFOSSILS IV. Society for Sedimentary Geology, 2019. http://dx.doi.org/10.2110/sepmsp.111.04.

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BECKMANN, BRITTA, THOMAS WAGNER, and PETER HOFMANN. "Linking Coniacian–Santonian (OAE3) Black-Shale Deposition to African Climate Variability: A Reference Section from the Eastern Tropical Atlantic at Orbital Time Scales (Odp Site 959, Off Ivory Coast and Ghana)." In Deposition of Organic-Carbon-Rich Sediments: Models. SEPM (Society for Sedimentary Geology), 2005. http://dx.doi.org/10.2110/pec.05.82.0125.

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Actes de conférences sur le sujet "Coniacian-Santonian"

Kuyl, Leo, Brian Hampton, and Dori Contreras. "STRATIGRAPHIC HISTORY AND PROVENANCE OF THE LOWER PART OF THE CONIACIAN-SANTONIAN CREVASSE CANYON FORMATION IN WEST-CENTRAL NEW MEXICO." In GSA Connects 2024 Meeting in Anaheim, California. Geological Society of America, 2024. http://dx.doi.org/10.1130/abs/2024am-401522.

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Davies, Marissa A., Claudia J. Schröder-Adams, Jens O. Herrle, Peter Hülse, Simon Schneider, and Alex Quesnel. "BENTHIC FORAMINIFERAL MORPHOGROUP RESPONSE TO PALEO-REDOX CONDITIONS ACROSS THE CONIACIAN TO SANTONIAN “OAE 3” INTERVAL IN THE KANGUK FORMATION, CANADIAN ARCTIC ARCHIPELAGO." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-305457.

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Leckie, R. Mark, Jeff Salacup, James I. Kirkland, and Steven Petsch. "ORGANIC MATTER PRODUCTION AND PRESERVATION DURING T-R CYCLES OF THE SMOKY HILL MBR. (MIDDLE CONIACIAN-MIDDLE SANTONIAN), MANCOS SHALE, CRETACEOUS WESTERN INTERIOR SEAWAY." In 75th Annual Meeting of the GSA Rocky Mountain Section - 2025. Geological Society of America, 2025. https://doi.org/10.1130/abs/2025rm-410119.

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