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The calcareous nannofossils and magnetostratigraphic results from the Upper Tithonian–Berriasian of Feodosiya region (Eastern Crimea)

References Arkadiev V.V., Bogdanova T.N., Guzhikov A.Yu., Lobacheva S.V., Myshkina N.V., Platonov E.S., Savelyeva Yu.N., Shurekova O.V. & Yanin B.T. 2012: Berriasian stage of the Mountainous Crimea. LEMA Publishing House, Saint Petersburg, 1–472 (in Russian). Arkadiev V.V., Guzhikov A.Yu, Savelieva Yu.N., Feodorova A.A., Shurekova O.V., Bagaeva M.I., Grishchenko V.A. & Manikin A.G. 2015: New Data on Bio- and Magnetostratigraphy of the Upper Berriasian Zavodskaya Balka section (Eastern Crimea, Feodosiya). Bull. Saint Petersburg St. Univ., Geology 7

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Ammonites and magnetostratigraphy of the Berriasian–Valanginian boundary deposits from eastern Crimea

References Aguado R., Company M. & Tavera J.M. 2000: The Berriasian-Valanginian boundary in the Mediterranean region: new data from the Caravaca and Cehegı´n sections, SE Spain. Cretaceous Res. 21, 1-21. Arkadiev V.V. 2015: New occurrences of the genus Riasanites (Ammonoidea) in the Upper Berriasian of the Eastern Crimea. Contributions to current cephalopod research: Morphology, Systematics, Evolution, Ecology and Biostratigraphy. In: Leonova T.B., Barskov I.S. & V.V. Mitta (Eds.):Proceedings of conference (Moscow, 2-4 April

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The northernmost occurrence of the Lower Berriasian ammonite Pseudosubplanites grandis (Štramberk Limestone, Outer Western Carpathians, Czech Republic)

References Arkadiev V.V. 2003a: Morphogenesis of the genus Pseudosubplanites (Perisphinctidae, Ammonoidea) from the Berriasian of the Mountain Crimea. Vest. Sankt-Peterburgskogo Universiteta, Ser. 7; Geol., Geogr. 2, 15, 87-93 (in Russian). Arkadiev V.V. 2003b: Berriasella jacobi - Pseudosubplanites grandis Zone in Berriasian of Mountain Crimea. Bjull. Moskovskogo Obščestva Ispytatelej Prirody, Otdel Geol. 78, 6, 29-35 (in Russian). Arkadiev V.V. & Bogdanova T.N. 2012: Cephalopods (Ammonites). In

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Microbiostratigraphy of the Berriasian–Valanginian boundary in eastern Crimea: foraminifers, ostracods, organic-walled dinoflagellate cysts

References Arkadiev V.V., Bogdanova T.N., Guzhikov A.Yu., Lobacheva S.V., Myshkina N.V., Platonov E.S., Savelyeva Y.N., Shurekova O.V. & Yanin B.T. 2012: Berriasian of Crimean Mountains. Publishing house LEMA, Saint-Petersburg, 1-472 (in Russian with English abstract). Arkadiev V.V., Baraboshkin E.Yu., Bagaeva M.I., Bogdanova T.N., GuzhikovA.Yu., Manikin A.G., Piskunov V.K., Platonov E.S., Savelieva Y.N., Feodorova A.A. & Shurekova O.V. 2015a: New Data on Berriasian Biostratigraphy, Magnetostratigraphy and Sedimentology in the

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A review of magnetostratigraphic results from the Tithonian–Berriasian of Nordvik (Siberia) and possible biostratigraphic constraints

References Altiner D. & Özkan S. 1991: Calpionellid zonation in north–western Anatolia (Turkey) and calibration of the stratigraphic ranges of some benthic foraminifers at the Jurassic–Cretaceous boundary. Geol. Romana 27, 215–235. Bagaeva M.I., Arkadiev V.V., Baraboshkin E.Y., Gorbenko E.Y., Guzhikov A.Y., Manikin A.G. & Perminov V.A. 2011: New data on bio- and magnetostratigraphy of the Berriasian–Valanginian boundary sediments in eastern Crimea. In: Shurygin B.N., Lebedeva N.K. & Goryacheva A.A. (Eds.): Palaeontology, stratigraphy and

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An account of the bio- and magnetostratigraphy of the Upper Tithonian—Lower Berriasian interval at Le Chouet, Drôme (SE France)

: Calcareous nannofossils Zonation of the Jurassic -Cretaceous Boundary interval and correlations with the Geomagnetic Polarity Timescale. Mar. Micropal. 14, 153-235. Casellato C.E. 2010: Calcareous nannofossil biostratigraphy of Upper Callovian -Lower Berriasian successions from Southern Alps, North Italy. Riv. Ital. Paleont. Stratigr.116, 357-404. Casellato C.E., Andreini G., Erba E. & Parisi G. 2008: Calcareous Nannofossil and Calpionellid calcification events across the Tithonian -Berriasian time interval and low latitudes

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The Jurassic/Cretaceous boundary and high resolution biostratigraphy of the pelagic sequences of the kurovice section (Outer Western Carpathians, the northern Tethyan margin)

.K., Józsa Š., Reháková D. & Wimbledon W.A.P. 2018: Biostratigraphy and magnetostratigraphy of the uppermost Tithonian-Lower Berriasian in the Theodosia area of Crimea (southern Ukraine). Geol. Quarterly 62, 2, 197–236. Batten D.J. 1996: Palynofacies and palaeoenvironmental interpretations. In: Jansonius J., McGregor D.C. (Eds.): Palynology: Principles and Applications 3. AASP Foundation , Dallas, 1011–1064. Bornemann A., Aschwer U. & Mutterlose J. 2003: The impact of calcareous nannofossils on the pelagic arbonate accumulation across the Jurassic

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Some perisphinctoid ammonites of the Štramberk Limestone and their dating with associated microfossils (Tithonian to Lower Berriasian, Outer Western Carpathians, Czech Republic)

: Description and biozonation of crinoid saccocomid sections from the Upper Jurassic sediments (Oxfordian-Tithonian) of the western Tethyan realm. Annales de Paléontologie 101, 95-117. Blaschke F. 1911: Zur Tithonfauna von Stramberg in Mähren. Annalen des Kaiserlich-königlichen naturhistorischen Hofmuseums 25, 143-222. Bogdanova T.N. & Arkadiev V.V. 2005: Revision of species of the ammonite genus Pseudosubplanites from the Berriasian of the Crimean mountains. Cretaceous Research 26, 488-506. Buckman S.S. 1921: Yorkshire Type

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Middle Jurassic–Early Cretaceous foraminiferal biozonation of the Amran Group, eastern Sana’a Basin, Yemen


Two sections of strata assigned to the Amran Group at Jabal Salab and Jabal Yam in the eastern Sana’a governorate were sampled and correlated. These sections are part of a carbonate platform that extends from the city of Marib in the east to Naqil Ibn Ghailan, 20 km east of the city of Sana’a to the west. Palaeontological analysis of samples recovered has resulted in identification of 123 foraminiferal species, which are used to subdivide the sequence of the Amran Group into five biostratigraphic zones, aged between Bathonian (Middle Jurassic) and Berriasian (Early Cretaceous). The proposed biozones are those of Riyadhella rotundata, Kurnubia jurassica, Ammomarginulina sinaica, Alveosepta jaccardi and Pseudocyclammina sulaiyana/Furitilla caspianseis. These biozones were constructed and correlated with the equivalent zones reported from several localities.

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Magneto-, and isotope stratigraphy around the Jurassic/Cretaceous boundary in the Vysoká Unit (Malé Karpaty Mountains, Slovakia): correlations and tectonic implications

field susceptibility in loess sediments. Geophys. J. Int. 118, 636-642. Föllmi K. B., Godet A., Bodin S. & Linder P. 2006: Interactions between environmental change and shallow water carbonate buildup along the northern Tethyan margin and their impact on the Early Cretaceous carbon isotope record. Palaeoceanography 21, 4, PA 4211. Galbrun B. 1985: Magnetostratigraphy of the Berriasian stratotype section (Berrias, France). Earth Planet. Sci. Lett. 74, 130-136. Grabowski J. 2005: New

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