C O N V E N T I O N

P R O T O C O L AMENDING THE EUROPEAN CONVENTION ON THE SUPPRESSION OF TERRORISM

In the north part of Pyrenees occurs foraminifera Bangiana hanseni in profile La Cassino (C a v a g n e t t o & T a m b a r e a u, 1998, 239) in Danian beds and in similar depositional conditions as in the Čebulovica profile.

Palustrine sedimentary environment of Liburnia Formation in SW Slovenia is recently studied by O t o n i č a r and K o š i r.

Particularly interesting are the beds at the K/T boundary for their shallow water carbonate development and biostratigraphy, paleontology, sedimentology of Paleocene beds: (D r o b n e et al.,1988, 1989, 1994, 1995, 1996; P u g l i e s e et al., 1995; J u r k o v š e k et al.,1996a,b, 1997; D e l v a l l e & B u s e r, 1990; D e C a s t r o et al., 1994; C a f f a u et al., 1995; K n e z, 1994, 1996; K n e z & P a v l o v e c, 1990; Dasycladaceans: B a r a t t o l o, 1998; Corals: T u r n š e k & D r o b n e, 1998; abiota: D o l e n e c et al., 1995; O g o r e l e c et al.,1995; H a n s e n et al.,1995, 1996; M a r t o n et al; 1995; P a l i n k a š et al., 1996; O t o n i č a r & K o š i r, 1998; Late Cretaceous dinosaurs, crocodiles: D e b e l j a k et. al., 1999).

In the Soča Karst area, T e n t o r et al. (1994) subdivided the whole succession into the Liburnia group (Gruppo Liburnico) and miliolidal limestone (Calcari a miliolidi).

We can correlate the restricted shelf environment (with periodical dasycladals) of the Čebulovica section with open shelf environments (with dasycladaceans) recognised in the Dolenja vas section (P l e n i č a r et al., 1992; B a r a t t o l o, 1998; T u r n š e k & D r o b n e, 1998).

T-oo banches o voylets trod into the mad.

The letters E, O, F, F+, T, T+, C, Xn, Xi and N do not form part of the symbol.

A: O.K. The world limits us, doesn't it, let's put it like that Andrej.

In the Trieste Karst, the equivalent strata were termed the Opicina member (C u c c h i et al., 1989, Pl.1,2), and nummulitic-alveolinal limestone in the Soča Karst (Calcari a nummuliti e alveoline, Te n t o r et al., 1994).

Foraminiferal associations from Thanetian beds (SBZ 3, SBZ 4) might be correlated, too (D r o b n e et al. 1988; P u g l i e s e et al. 1995; B r a z z a t t i et al. 1996; T u r n š e k & D r o b n e, 1998, fig.3).

Their advantages were the following: large tests, complex inner structures, dimorphism, reproductive Čcles in accordance with seasonal food enrichments, " readiness " for speciations, increased diversity over a short period, seen through phylogenetic flourishment of few genera with many species (H o t t i n g e r & D r o b n e, 1988; H o t t i n g e r, 1997).

Similarity in fossil associations could be explained by existence of gyre (current stream) pattern in Maastrichtian and Paleocene (H o t t i n g e r, 1990, paleobiogeographic map).

Also here algae Lagynophora in Danian beds are predominant, and dasycladaceans along with foraminifera in younger beds (S l i š k o v i † et al., 1978; D r o b n e et al., 2000; T r u t i n et al., 2000).

But, Stache's genera Lagynophora and Kosmogyra are still valid (B i g n o t, 1972; E r c e g o v a c, 1981; K n e z, 1996).

Geographically closest to NW part of our platform are Paleogene and Neogene sediments of Maiella region (P i g n a t t i, 1994; V e c s e i et al., 1996; V e c s e i & M o u s s a v i a n, 1997).

Classic ground for such studies are also nowadays next to Algeria (M e b r o u k & F e i s t, 1999) the Pyrenees.

The stable isotope analysis on?13C and ?18O indicate water temperature in environments where sedimentation took place, up to 27o and 30oC. The same values today have subtropic seas, like water in the gulf of Aqaba (R e i s s & H o t t i n g e r, 1984).

In relation to the section Dolenja vas, 5 km north of Čebulovica, the marine development prevails from K/T boundary till Thanetian beds, what indicates the closer position to the open sea in the northern direction (D r o b n e et al,. 1988, 1989, 1996; T u r n š e k & D r o b n e, 1998, fig.3).

In the subdivision of Paleogene in Shallow Benthic Zones SBZ 1 - SBZ 20 the propositions of International subcommission for chronostratigraphic units of Paleogene stratigraphy are considered (J e n k i n s & L u t e r b a c h e r, 1992; O d i n & L u t e r b a c h e r, 1992).

All geological bibliography concerning Slovenian an Italian part of Kras is compiled in the papers of P a v l o v e c et al. (1989) and M a r t i n i s (1989).

The Maastrichtian sediments from Gavrovo (External Hellenids) and from Peloponesus peninsula contain R. liburnica, and they continuously pass into Paleocene sediments with textulariids, valvulinids, complex miliolids, and glomalveolinids (T s a i l a - M o n o p o l i s, 1977; F l e u r y, 1980; Z a m b a t a k i s - L e k k a, 1988; M a u r i k a s, 1993).

Unfortunately, data on Paleocene fossil associations from Gargano peninsula (cf. P i g n a t t i, 1994) were not available for correlation. Sediments from 13 studied sections, focusing on the Upper Cretaceous and Paleogene succession of the island of Cephalonia, 6 with Paleocene sediments, indicate deposition on inner and middle carbonate ramp (A c c o r d i et al., 1998; Figs.18,19).

Their abundance, one kg of sediments from Can Casadessus section, bay of Lyon, contain several hundreds of isolated gyrogonites (M a r t i n - C l o s a s et al. 1999), makes them valuable markers for correlation between marine and non-marine realms. From this study area, derived the larger foraminifera - Charophyta correlation for the Early Lutetian to Late Bartonian time (SBZ 13 - 20; ibidem 1999).

the headings "B. DENMARK", "C. GERMANY", "D. GREECE", "E. SPAIN", "F. FRANCE", "G. IRELAND", "H. ITALY", "I. LUXEMBOURG", "J. NETHERLANDS", "K. AUSTRIA", "L. PORTUGAL", "M. FINLAND", "N. SWEDEN" and "O. UNITED KINGDOM" become "C. DENMARK", "D. GERMANY", "F. GREECE", "G. SPAIN", "H. FRANCE", "I. IRELAND", "J. ITALY", "N. LUXEMBOURG", "Q. NETHERLANDS", "R. AUSTRIA", "T. PORTUGAL", "W. FINLAND", "X. SWEDEN" and "Y. UNITED KINGDOM";

the headings "B. DENMARK", "C. GERMANY", "D. SPAIN", "E. FRANCE", "F. GREECE", "G. IRELAND", "H. ITALY", "I. LUXEMBOURG", "J. NETHERLANDS", "K. AUSTRIA", "L. PORTUGAL", "M. FINLAND", "N. SWEDEN" and "O. UNITED KINGDOM" are reordered with their respective entries and become "C. DENMARK", "D. GERMANY", "F. GREECE", "G. SPAIN", "H. FRANCE", "I. IRELAND", "J. ITALY", "N. LUXEMBOURG", "Q. NETHERLANDS", "R. AUSTRIA", "T. PORTUGAL", "W. FINLAND", "X. SWEDEN" and "Y. UNITED KINGDOM";

Toetust makstakse... tonni puhul (kogus, mille kohta on litsents välja antud). - >ISO_7>ÅðéóôñïöÞ éó÷ýïõóá ãéá... ôüíïõò (ðïóüôçôá ãéá ôçí ïðïßá Ý÷åé åêäïèåß ôï ðéóôïðïéçôéêü) - >ISO_1>Refund valid for... tons (quantity for which the licence is issued) - Restitution valide pour... tonnes (quantité pour laquelle le certificat est délivré) - Restituzione valida per... t (quantitativo per il quale il titolo è stato rilasciato) - Kompensacija paredzeta... t (daudzums, attieciba uz ko ir izsniegta atlauja) - Grazinamoji ismoka taikoma... tonoms (kiekis, kuriam isduota licencija) - A visszatérítés... tonnára érvényes (az a mennyiség, amelyre az engedélyt kiállították) - Rifuzjoni valida gal... tunnellata (kwantità li galiha gie marug ic-certifikat) - Restitutie geldig voor... ton (hoeveelheid waarvoor het certificaat wordt afgegeven) - Refundacja wazna dla... ton (ilosc, dla której pozwolenie zostao wydane) - Restituição válida para... toneladas (quantidade relativamente à qual é emitido o certificado) - Náhrada platná pre... ton (mnozstvo, na ktoré sa povolenie vydáva) - Nadomestilo veljavno za... ton (kolicina, za katero je bilo izdano dovoljenje) - Tuki on voimassa... tonnille (määrä, jolle todistus on myönnetty) - Ger rätt till exportbidrag för... ton (den kvantitet för vilken licensen utfärdats)."

S t o c k s, c a p a c i t y a n d c a p a c i t y u t i l i s a t i o n

I n v e s t m e n t s a n d a b i l i t y t o r a i s e c a p i t a l

A d d i t i o n s t o s u b s i s t e n c e a l l o w a n c e

N o t e

M a g n i t u d e o f t h e a m o u n t o f c o u n t e r v a i l a b l e s u b s i d i e s

Calculation of dead time t o

R e i m b u r s e m e n t o f c e n t r a l s a l e s t a x p a i d o n g o o d s p r o c u r e d l o c a l l y

G r o w t h

R e l e v a n c e o f i n d i c a t o r s

The dead time t o is then given by:

Initial concentration in medium, t o:

Pos i t ion o f l ong - t e rm cont r a c t s

P r o d u c t i o n, e m p l o y m e n t a n d p r o d u c t i v i t y

E x e m p t i o n f r o m i m p o r t d u t i e s o n c a p i t a l g o o d s

P r o f i t a b i l i t y, r e t u r n o n i n v e s t m e n t a n d c a s h f l o w

E x e m p t i o n f r o m i m p o r t d u t i e s o n r a w m a t e r i a l s

in which, t R = retention time of the test substance, and t o = average time a solvent molecule needs to pass through the column (dead-time).

T o each flask, add 10,00 ml internal standard solution (2.14) and 0,5 ml sulfuric acid 2 Μ (2.10).

T o each flask, add 10,00 ml internal standard solution (2.14) and 0,5 ml sulfuric acid 2 Ě (2.10).

R o a d j o u r n e y s - u s e o f p r i v a t e c a r s