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THE MEDITERRANEAN LOWER CRETACEOUS

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System has been accepted by most specialists, because it corresponds best to the lawgoverned. This objective picture of clearly manifested provincialism. Malbosiceras stephanovi N i к. Crassicollaria parvula disappears at the end of the zone R emane,. Crioceratites majoricensis majoricensis N о 1. It seems that two foraminifera. However, the characterization of these zones still requires considerable. Astacolus scitulus Bert h. Its lower boundary is marked bilaterally: by the disappearance. Cheloniceras Epicheloniceras spp. It is based on the Range-zone of the index species and the Concurrent-Range-zones. Six stable zones are outlined in the Albian space of the Mediterranean. It is based on the Range-zone of the index species and on the Concurrent-Range-zones. Further below the regional stratigraphy is studied according to regions and palaeogeographic. They are covered by slightly aleuritic marls with rather rich foraminifera. Predominantly detritic and bioconstructed. Relationships between the lithostratigraphic units along the Ribarica — Kalenik line. This part has been accurately dated only in the section to the west of Jablanica,. Relationships between the lithostratigraphic units along the Zlatarica — Capaevo line. Relationships between the lithostratigraphic units along the Antonovo — Medovina line. Psephites do not occur here, and the marls are less aleuritic. This is particularly characteristic. In these places the sections are built of calcareous claystones,. The thickness of the Hauterivian sediments. In these outcrops, as well as in the east towards the valley of Jantra river between. According to borehole data, the conditionally. It is represented by marls with intercalations of clayey limestones. It is represented by finegrained. The calpionellid zones Calpionella, Calpionellopsis. Schematic section of the Continental Margin of Northwestern Africa according to data. In the Tellian Atlas the Lower Cretaceous is connected with the following lithostratigraphic. Alternation of marls and clayey limestones with intercalations of siltstones and sandstones. Lithostratigraphic units in the northern part of the High Plateaux between the Oued Mina. It is built of alternation of dark-grey to black argillites, siltstones. Crioceratites loryi S a r k. Lower Valanginian , clayey limestones and marls with ammonites Upper Valanginian-Barremian ,. The Lower Cretaceous is characterized palaeontologically predominantly. The calcschistes. There also occur corals, gastropods, echinids, brachiopods, Orbitolinidae. Barremian claystones with oysters, which are outlined by variegated fresh-water sandyclayey. It is represented by clayey shales and calcareous shales with aptychi. Exclusively bathyal clayey limestones, marls and clayey shales Berriasian-Barremian. Generally speaking, it is characterized. The Berriasian is represented by limestones Lysa Skala crinoidal, crinoidal-brachiopod. Silesites vulpes С о q. In the area of the Polish Carpathians the series is developed. In some places massive sandstone packets, conglomerates,. Therefore, only the most general. Sketch of the distribution of the maia types of facies of the Lower Cretaceous in Caucasus. Speetoniceras S. Sketch of the distribution of the main types of facies of the Lower Cretaceous in Northwestern. Section of the Lower Cretaceous in tiie northern slope of the Northwestern Caucasus. The Urgonian facies of the Aptian is associated with tuffs and tuffites. It is characterized. Berriasian : Berriasella privanensis P i с t. Among them the following species have been found : Acanthodiscusradiatus. They contain Orbitolinidae, ridists, brachiopods,. The different stages are well characterized. An example in this respect is the generalizing. In Central Caucasus the stage is built of micrograined. They contain characteristic ammonites. A formation of cryptocrystalline. Purely terrigenous deltaic facies are also developed in the western part, while terrigenous-carbonate. This facies is of the Italian Maiolica type. Tt is represented by argillites,. Marls with intercalations. In Ceceno-Ingusetia and Dagestan the Stage is connected with terrigenous-carbonate. Aptian sediments in the northern part of Algeria are of pelagic flysch or clayeycarbonate. It is predominantly. Vocontian facies to the reef facies of the Urgonian, which occurs in a strip with biodetritic. Moreover, they form very clear successions of great stratigraphie significance. It is known that 70 per cent of the sea benthonic invertebrates. Boreal Basin. The typical endemic genus Tauricoceras is also developed in the Crimean-Caucasian.

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