A G R E E M E N T

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

No consultation in the case of a converted analogue station into a single DVB-T station is required provided the e.r.p. is no more than the analogue e.r.p. minus 18 dB, and other technical characteristics are not changed or would reduce the probability of harmful interference.

(c) the proposed modification relates to the conversion of an analogue station into a single DVB-T station, provided the e.r.p. is no more than the analogue e.r.p. minus 18 dB, and other technical characteristics are not changed or would reduce the probability of harmful interference

Speed(R)= Speed(T) = nRT

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 adaptations (h), (i), (j), (k), (l), (m), (p), (q), (r), (t) and (v) points "P", "Q" and "R" shall be renumbered as points "ZA", "ZB" and "ZC" respectively;

T = ml of CO2 released by 0.5 g of CaCO2 A.R.

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).

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).

For these modes (R, S, T, U), the following definitions apply:

In the literature such type of sedimentation is termed as palustrine environment or palustrine limestone (F r e y t e t, 1964; F r e y t e t & P l a z i a t, 1982). The authors studied Upper Cretaceous and Paleocene beds in southern France.

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).

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.

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).

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).

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).

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.

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 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.

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).

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).

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).

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).

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).

Applying new methods, we confirmed the hypothesis by G. S t a c h e and M. H a m r l a about Paleocene occurrences of Lagynophora genus.

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).

T he Staff Committee shall represent the interests of the staff vis-ŕ-vis the Foundation and maintain continuous contact between the Foundation and the staff.

First foraminiferas that followed K/T events were r-strategists related to meso- to eutrophic shallow-water settings, and they were dominant over 5 millions years.

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).

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).

In order to shed more light on specific sedimentologic conditions during the formation of the Liburnia deposits, G. S t a c h e (1889, p. 125) gave the lists of detailed descriptions of areas with living characeans from the South America, Africa and Mediterranean. G r a m b a s t (1971) and later researchers studied Characeans from Pyrenean basin, Paris basin and Liburnia deposits resulted in new taxonomy and biostratigraphic evaluation.

T he staff of the body must be bound by professional secrecy (except vis-ŕ-vis the competent administrative authorities of the State in which i ts activities are carried out) with regard to all information it acquires in carrying out its tasks under this Directive or any provision of national law giving effect to it.

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";

A i r t r a v e l

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

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

G r o w t h

R a i l t r a v e l

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

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

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

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

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

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

T.C.R. No. (where applicable)

S a l e s v o l u m e a n d m a r k e t s h a r e

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