THE MEDITERRANEAN LOWER CRETACEOUS

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Fig. 2. Map of the distribution of the Lower Cretaceous in France and Switzerland / — outcrops; 2 — stratotypes
Fig. 1. Simplified map of the distribution of the Lower Cretaceous in the Mediterranean Region , , , т „,г ггч-,- е„„, гм„Ыап Sand-tom-, 1 1 Upper Jurassic-Unver C^a^oi*; 2 - Lower Cretaceous (continental facies in Africa). Purbeckian-Wealdian (sed.nwnt in Eurepc) J - Lower Crctaceor.s (marm. segments,; 4 - Lower Cretaceous (Nubun Sandstones 3 The Mediterranean Lower Cretaceous
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IChlor « Nikoiov THE MEDITERRANEAN
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Todor G. Nikolov LE CRETACE INFERIE
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In this monograph the Lower Cretace
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ficiently investigated. On the othe
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Part One INTRODUCTION I. GENERAL RE
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Table 1 Radiometric Data for the Lo
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N а с h e v, Lilov (1975) have ob
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that there exist close ammonite aff
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Table 4 Calpionellid Zones a .2 '5
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Calpionellid Zones Calpionellid zon
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3. Blueish and yellowish marls with
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С. oblongata Zone. It is based on
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Table 7 Ammonite Zones in the Haute
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Table 8 The Hauterlvian-Barremian B
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Table 9 Ammonite Zones in Barremian
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The lower boundary of the Àptian i
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P. pachistephanum Zone. It is based
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Table 12 Comparative Table of the F
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Table 13 Biostratigraphic Zones in
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Sow., A. pseudoelegans P i с t., C
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Table 14 Major Chronostratigraphic
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1.2. Accepted Stratigraphie Schemes
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stavites) cf. platycostatus S a y n
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like flint rocks. In some places th
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Khrischev (Николов, Хрис
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In the zone of the villages Zamfiro
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trautscholdi (S i т., В a c, S о
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Tn R-l Sevlievo Bochianites sp. and
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which proves tlie Barrcmian age of
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The Aptian is characterized by rich
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— The upper part of the Berriasia
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The natural outcrops of the Hauteri
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stone intercalations appear in the
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observed. To the north they rapidly
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sp. indet., Hamites intermedius S
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The upper boundary of the Valangini
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— For (he Gargasian: Cheloniceras
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The Albian around the town of Svist
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Tn the northwestern part of the Kub
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Sanmartinoceras (Sinzovia) trautsch
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These finds are of exceptional sign
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Acanthohoplites sp., charophytes an
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2.2. Continental Margin of Northwes
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lagoon and brakish environments. Th
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comiensis R a d., Cayeuxia sp., Tro
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On the territory of Douar Raouraoua
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Delga (1969) distinguished three ba
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(В 1.), etc. In the upper part of
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northeast — the Cantabrian and Ib
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Marine terrigenous-carbonate facies
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(the Barremian Stage in the Pyrenee
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Tn the same area, in the Nantebelte
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Tn the Parentis Basin the Lower Cre
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limestones pass to the south into W
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8.2. The Hungarian Central Mountain
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Table 16 Lithostratigraphic Units R
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Verovice (Wierzowice, Wcrnsdoif) Sh
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of microbreccias formed of crystall
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The Albian sediments in the Récita
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Clayey-calcareous sediments of Razg
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In the Old Crimean (Starij Krim) re
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species (Deshayesites dechyi (Papp.
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Barremites cf. subdifficilis К а
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The Middle and Upper Albian are usu
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Berriasian : Berriasella privanensi
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14.3. Sardinia The Lower Cretaceous
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Albian included. The section of the
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The Hauterivian is discovered over
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17. GREECE The stratigraphie differ
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Part Three GENERALIZATIONS AND CONC
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In the Southern Carpathians the Ber
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In the Crimea the Valanginian depos
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feature of the Hauterivian sections
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In the northern part of Tunisia the
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Cerna and Coçustea there are Urgon
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Paraurgonian sediments with Orbitol
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Shales and limestones with Orbitoli
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In Eastern Serbia and in the Sumadi
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2.2.2. Foraminifera Foraminifera ar
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In the northern province of the Med
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to them a possibility for rapid and
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there are Tethys genera (Lytoceras,
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Immigrants from other provinces occ
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so that in the northernmost part of
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A similar endemism in the Albian am
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with many representatives of Ammoni
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During the Early Cretaceous the Mé
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The uplift of the Atlas was accompa
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During the Early Cretaceous the sea
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To the southwest of the Kozloduj-Kn
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Fig. 21 LU!i )f.i;i23 mr> witîi sk
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the end of the Barremian, but in ad
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G г u b i с (1974) made an attemp
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flysch; (5) Magreb flysch from Sici
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The Magreb flysc 1 zone continues t
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3. "Bucegi" conglomerates of the co
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Peridotites of Aptian-Albian age ar
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Indeed, the facts which this resear
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197
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Most considerable activations occur
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Carey (1958) was the first to note
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Fig. 43. Palaeogeographic sketch-ma
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3. CONCLUSIONS . • L. Some senera
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REFERENCES A с к e г m a n n, h.
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В e 1 1 i e г, J. P. 1974. Préci
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Cadet, J.-P. 1978. Essai sur l'évo
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D i e t z, R. S., J. C. H о I d e
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G u é r i n, S., M. M о u 1 1 a d
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M с m m i, L. 1965. Sur quelques A
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M e m m i, L. 1965. Sur quelques Am
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Pomerol, С. 1975. Stratigraphie et
Page 224 and 225: S z y m а к о w s к a, F. 1965.
Page 226 and 227: Бойчее, E. 1937. Върху
Page 228 and 229: M и л а н о в с к к й, E.
Page 230 and 231: Цанков, В., Ю. Стефан
Page 232 and 233: léristique générale de chaque é
Page 234 and 235: Massif Bétique, y inclus les Balé
Page 236 and 237: Dans la partie centrale du détroit
Page 238 and 239: Dans les Carpathes de Staro-Sambors
Page 240 and 241: Lors du Crétacé inférieur dans l
Page 242 and 243: 2. Valanginien La répartition du V
Page 244 and 245: graphique et les facteurs écologiq
Page 246 and 247: zoïques globaux il est inclus entr
Page 248 and 249: sion continuelle, au Nord de laquel
Page 250 and 251: II. ЯРУСЫ, ПОДЪЯРУСЫ
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Page 254 and 255: с эхиноидеями. Их о
Page 256 and 257: В центральной част
Page 258 and 259: Шумадийская зона о
Page 260 and 261: 1. Берриасский ярус
Page 262 and 263: 2. Основные черты эв
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Page 266 and 267: 2. В отдельных пояса
Page 268 and 269: CONTENTS PREFACE Part One. INTRODUC
Page 270 and 271: 2.2. Protozoa 1 5 6 2.2.1. Radiolar
Page 272 and 273: 1. Обшие заметки • 25
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THE MEDITERRANEAN LOWER CRETACEOUS

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