- Page 1 and 2: IChlor « Nikoiov THE MEDITERRANEAN
- Page 3: Todor G. Nikolov LE CRETACE INFERIE
- Page 7 and 8: ficiently investigated. On the othe
- Page 10 and 11: Part One INTRODUCTION I. GENERAL RE
- Page 12 and 13: Table 1 Radiometric Data for the Lo
- Page 14 and 15: N а с h e v, Lilov (1975) have ob
- Page 16 and 17: that there exist close ammonite aff
- Page 18 and 19: Table 4 Calpionellid Zones a .2 '5
- Page 20 and 21: Calpionellid Zones Calpionellid zon
- Page 22 and 23: 3. Blueish and yellowish marls with
- Page 24 and 25: С. oblongata Zone. It is based on
- Page 26 and 27: Table 7 Ammonite Zones in the Haute
- Page 28 and 29: Table 8 The Hauterlvian-Barremian B
- Page 30 and 31: Table 9 Ammonite Zones in Barremian
- Page 32 and 33: The lower boundary of the Àptian i
- Page 34 and 35: P. pachistephanum Zone. It is based
- Page 36 and 37: Table 12 Comparative Table of the F
- Page 38 and 39: Table 13 Biostratigraphic Zones in
- Page 40 and 41: Sow., A. pseudoelegans P i с t., C
- Page 42 and 43: Table 14 Major Chronostratigraphic
- Page 44 and 45: 1.2. Accepted Stratigraphie Schemes
- Page 46 and 47: stavites) cf. platycostatus S a y n
- Page 48 and 49: like flint rocks. In some places th
- Page 50 and 51: Khrischev (Николов, Хрис
- Page 52 and 53: 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
- Page 216 and 217:
G u é r i n, S., M. M о u 1 1 a d
- Page 218 and 219:
M с m m i, L. 1965. Sur quelques A
- Page 220 and 221:
M e m m i, L. 1965. Sur quelques Am
- Page 222 and 223:
Pomerol, С. 1975. Stratigraphie et
- Page 224 and 225:
S z y m а к о w s к a, F. 1965.
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Бойчее, E. 1937. Върху
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M и л а н о в с к к й, E.
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Цанков, В., Ю. Стефан
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léristique générale de chaque é
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Massif Bétique, y inclus les Balé
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Dans la partie centrale du détroit
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Dans les Carpathes de Staro-Sambors
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Lors du Crétacé inférieur dans l
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2. Valanginien La répartition du V
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graphique et les facteurs écologiq
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zoïques globaux il est inclus entr
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sion continuelle, au Nord de laquel
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II. ЯРУСЫ, ПОДЪЯРУСЫ
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востоке — в Ливии и
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с эхиноидеями. Их о
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В центральной част
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Шумадийская зона о
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1. Берриасский ярус
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2. Основные черты эв
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ляется следствием
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2. В отдельных пояса
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CONTENTS PREFACE Part One. INTRODUC
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2.2. Protozoa 1 5 6 2.2.1. Radiolar
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1. Обшие заметки • 25
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Fig. 2. Map of the distribution of