For example, the U.S.N.R.C. will attempt to meet requests that come through the International Atomic Energy Agency (I.A.E.A.) for technical assistance missions to Slovenia by U.S.N.R.C. safety experts.

This paper reports on changes in the segetal weed community Aphano-Matricarietum chamomillae R. Tx. 37, caused by intensification of crop production (i.e. increase of fertilizing level, chemical weed control, soil ameliorating and frequent tillage) on territory of Dravsko and Ptujsko polje.

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).

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).

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.

the guide price applicable in Spain for red table wine shall be derived from the guide price for white table wine by applying the same relationship as that existing in the Community as at present constituted between the guide prices of table wines of types A I and R I,

The future studies on characeans within Cretaceous and Paleogene sediments, based on biostratigraphy for Mesozoic and Tertiary (R i v e l i n e et al., 1996) could shed more light on development of shallow-water environments on the Adriatic-Dinaridic carbonate platform.

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).

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).

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).

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;

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).

This zonation with some discrepancies around Paleocene/Eocene boundary is applied in Shallow Benthic Zonation of Paleogene (SBZ 1 - SBZ 20, S e r r a - K i e l et al., 1998).

Biostratigraphy Biostratigraphic interpretation applied in this paper is mainly based on larger foraminifera using the Shallow Benthic Zonation (SBZ 1-20, S e r r a -K i e l et al., 1998).

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.

Owing to numerous algae (B u s e r & R a d o i č i †, 1987) and other lithological characteristics, D e l v a l l e and B u s e r (1990) introduced a new name for the upper foraminiferous and milliolidal limestone - the Slivje Formation according to the village of Slivje located in the southewestern margins of Brkini.

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).

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).

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).

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).

A. K o š i r (1998; 2001 - under review) deals with appearance, genesis and diagenesis of Microcodium from sediments in SW Slovenia.

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.

in adaptations (a), (b), (c), (f), (h), (i), (l), (m), and (n) points "P", "Q" and "R" shall be renumbered as points "ZA", "ZB" and "ZC" respectively;

E. S i r e l (1998) made the Atlas of Upper Cretaceous to Paleogene larger foraminifera from Turkey with taxonomic descriptions and biostratigraphic data.

( i) companies under Luxembourg law known as 'société anonyme', 'société en commandite par actions', 'société ŕ responsabilité limitée';

The positions of the V points in relation to the R point, as indicated by XYZ coordinates from the three-dimensional reference grid, are as shown in Tables I and II.

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).

R= Reproducibility, the value below which the absolute difference between single test results obtained under reproducibility conditions (i.e., on identical material obtained by operators in different laboratories, using the standardised test method), may be expected to lie within a certain probability (typically 95 %); R = 2,8 × sR.

Poisonous substances listed in Tables A (toxic products) and C (dangerous products) of Section I of Décret 56-1197 of 26 November 1956 (Code de la Santé publique, Book V, Part 2, Title III, Chapter 1, Sections I and II, Articles R 5149 to 5168).

Poisonous substances listed in Tables A (toxic products) and C (dangerous products) of Section I of Décret 56-1197 of 26 November 1956 (Code de la Santé publique, Book V, Part 2, Title III, Chapter 1, Sections I and II, Articles R 5149 to 5168).

'Since you like to be in their company [women's company, r. k.], does it feel like being among women of your age, well, men of your age? ... I'd say that you are close to them. Do you know why 'close'?

To this end, 745.5 mg potassium chloride (A.R.), previously dehydrated by heating to about 500 şC - i.e. to a dull red heat - are dissolved in water in a 1 litre graduated flask and made to volume with water.

To this end, 745.5 mg potassium chloride (A.R.), previously dehydrated by heating to about 500 ĹźC - i.e. to a dull red heat - are dissolved in water in a 1 litre graduated flask and made to volume with water.

'On the way I dropped into the public toilet at Trg Republike (in Zagreb, r. k. ). The next moment a man nearly two meters tall materializes next to my urinal, pulls it out of his pants and says: 'Give me your hand!'

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).

Sphaerical alveolinids, Alveolina daniensis Drobne along with less numerous Ranikothalia sp. are scattered throughout micritic matrix. Early Ilerdian, SBZ 6 (S e r r a - K i e l et al., 1998), is identified (Pl.7, fig.3).Upper Paleocene sediments from Čebulovica section testify open marine influence. These trends continued through Eocene, alveolinid-nummulitic limestones overlie Paleocene ones.

r= Repeatability, the value below which the absolute difference between 2 single test results obtained under repeatability conditions (i.e., same sample, same operator, same apparatus, same laboratory, and short interval of time) may be expected to lie within a specific probability (typically 95 %) and hence r = 2,8 × sr. sr= Standard deviation, calculated from results generated under repeatability conditions.

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).

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";