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45Kasnoglacijalna industrija lomljenog kamena pećine KopačineLate Glacial knapped stone industry of Kopačina CaveNikola Vukosavljević, Zlatko Perhoč, Božidar Čečuk †, Ivor Karavanićwhich resided in Vešanska Cave. The subsequent phase from Vešanska (Interstadial Phase II), viewed technologically and typologically, exhibits some dierences in relation to the preceding phase, although backed artefacts are still the most numerous among the tools.128The repertoire of tools present in Vešanska corresponds largely to that found in Kopačina, but their relative frequency signicantly diers from one cave to the other, what could be a result of dierent activities undertaken in each cave. The activities undertaken were not necessarily entirely dierent, but their intensity diered. In contrast to Kopačina, where micro-burins are not present, they appeared in Vešanska in this youngest phase.129 A part of the stratigraphic sequence from Pupićina Cave which belongs to the Late Glacial period based on radiocarbon dating can be placed within the span from 11150 ± 80 BP (Beta-145095) to 10020 ± 180 BP (Z-2613).130The initial phase, as in Vešanska Cave, has a small documented number of animal and lithic remains. Although there are certain dierences between the later two phases, both are dominated by akes and chunks with roughly equal shares, while the share of bladelets is considerably higher than in Kopačina. The repertoire of tools, which is similar to that of Kopačina, is dominated by endscrapers, thumbnail and circular, while the share of backed artefacts is also high, and in the later phase geometric microliths also appear in this group of tools. Micro-burins are also present in the latest phase.131 A part of stratigraphic sequence from Nugljanska Cave, based on the radiocarbon age of 11520 ± 90 (Beta-127705), may be placed in the Late Glacial period.132 In Nugljanska, as in Vešanska and Pupićina, there are certain dierences between the dierent phases of residence in the cave which were probably dictated by the function of the cave itself in certain periods. Among the technological categories, akes dominate, with a rather high share of bladelets and blades (in comparison to Kopačina). Among the backed tools, backed bladelets dominate, while in the younger phase geometric microliths also appear. Micro-burins are present in Nugljanska as well, in both phases. Taking into account all of the aforementioned aspects, we may conclude as follows: at the Istrian sites as in Kopačina, akes were the primary product of knapping; bladelets in Istria are much more common than in Kopačina; while micro-burins are present at almost all of the Istrian sites (except in Šandalja II, which may be due to the lack of sifting of sediments), they are unknown in Kopačina; splintered pieces are rarer in Istria than in Kopačina; the share of endscrapers is high in both Kopačina and Istria, but it would appear that thumbnail endscrapers are more numerous in Kopačina; geometric microliths are present in Kopačina as at the Istrian sites.128 Komšo, Pellegati 2007, p. 32.129 Komšo, Pellegati 2007, p. 32.130 Komšo, Pellegati 2007, p. 33, Fig. 3.5. Here are cited three more dates which belong to the afore mentioned time span.131 Komšo, Pellegati 2007, p. 34.132 Komšo, Pellegati 2007, p. 35; Miracle, Forenbaher 1997, p. 41.9.2. DalmatiaBesides Kopačina, three other Late Glacial sites (Vlakno, Zemunica, Vela spila) are known in Dalmatia. Only a chronological parallel can be drawn with Vlakno Cave on the island of Dugi otok, because the materials have not yet been published. The late Upper Palaeolithic hunter-gatherers resided in Vlakno between 14,900 BP, established by the age of the tephra,133 and 10160 ± 100 BP (Z-3383).134 As in the case of Vlakno, only a chronological parallel can be drawn for Zemunica Cave, because the lithic assemblage has not yet been published, while part of the stratigraphic sequence probably belongs to the late Upper Palaeolithic.135 The Late Glacial stay of hunter-gatherers in Vela Spila has been determined by an absolute radiocarbon date to an age of 12260 ± 40 BP (VERA-2346).136When taking into consideration the age and tool types present, as well as their relative frequency, layers 8/2 - 8/6 will be observed as a whole and compared to the lithic industry from Kopačina. The dominant technological category in the Late Glacial lithic assemblage of Vela Spila are chunks (with the exception of chips), followed by akes, and then bladelets and nally blades. As opposed to Kopačina, bladelets and blades were produced much more often in Vela Spila.137The authors did not mention the presence of micro-burins in the lithic inventory of Vela Spila.138 In the lithic asemblage of Vela Spila, endscrapers predominate among the tools, which is also the case in Kopačina in both lithic phases, but they are much more numerous in Vela Spila, where they compose almost 50% of all tools.139 Among the endscrapers, the thumbnail endsraper is the most numerous type after endscrapers on akes, while thumbnail endscrapers in Kopačina are the most numerous type among the endscrapers. The relative frequency of backed bladelets in Vela Spila (ca. 12%) is much higher than in Kopačina, but this may be a result of the absence of sifting of sediments in Kopačina. Among the geometric microliths in Vela Spila, the most numerous are backed segments, and only one example of a trapeze is present. The higher frequency of geometric microliths in Vela Spila compared to Kopačina may, as in the case of backed bladelets, be the result of the excavation methodology. The relative frequency of splintered pieces is identical at both sites. Curved backed bladelets are more numerous in Kopačina than in Vela Spila (0.38%). Based on this, we may conclude that the Late Glacial lithic industries in Vela Spila and Kopačina exhibit considerable similarities.133 Brusić 2008, p. 402.134 Brusić 2005, p. 198; Komšo 2006, p. 74.135 Šošić, Karavanić 2006, p. 378.136 Čečuk, Radić 2005, p. 34, note 9. A charcoal sample from layer 8/6 was dated.137 Čečuk, Radić 2005, p. 26, Table 2.138 Čečuk, Radić 2005.139 Data on the relative frequency of tools from Vela Spila were obtained on the basis of data shown in Čečuk and Radić 2005, p. 27, Table 4.je boravila u Vešanskoj peći. Sljedeća faza iz Vešanske (Interstadial Phase II) tehnološki i tipološki gledano pokazuje određene razlike u odnosu na prethodnu fazu, ali su i dalje među alatkama najbrojniji strmo obrađeni artefakti.128 Repertoar alatki prisutan u Vešanskoj podudara se dobrim dijelom s onim pronađenim u Kopačini, ali se međusobni omjeri bitno razlikuju u jednoj i drugoj pećini i odraz su različitih aktivnosti poduzimanih u svakoj od pećina. Poduzimane aktivnosti nisu nužno potpuno različite, ali je različit njihov intenzitet. Za razliku od Kopačine gdje mikrodubila nisu prisutna, ona se u Vešanskoj peći pojavljuju u ovoj najmlađoj fazi.129 Dio stratigrafskog slijeda iz Pupićine peći koji pripada kasnom glacijalu na temelju radiokarbonskih datuma može se smjestiti u rasponu od 11.150 ± 80 BP (Beta-145095) do 10.020 ± 180 BP (Z-2613).130 Inicijalna faza je kao i u Vešanskoj peći dokumentirana malim brojem ostataka faune i litike. Iako između kasnijih dviju faza postoji određena razlika, u obje faze dominiraju odbojci i krhotine s približno jednakim udjelima, a udio pločica je znatno veći nego u Kopačini. U repertoaru alatki koji je sličan kopačinskom, dominiraju grebala, noktolika i kružna, udio strmo retuširanih artefakata je također veliki, a u kasnijoj fazi se u ovoj skupini alatki pojavljuju i geometrijski mikroliti. Mikrodubila su također prisutna u najkasnijoj fazi.131 Dio stratigrafskog slijeda iz Nugljanske peći na temelju radiokarbonske starosti od 11520 ± 90 (Beta-127705) može se smjestiti u kasnoglacijalno razdoblje.132 I u Nugljanskoj kao i u Vešanskoj i Pupićinoj peći postoje određene razlike između različitih faza boravka u pećini koje su vjerojatno uvjetovane funkcijom same pećine u određenim razdobljima. Među tehnološkim kategorijama dominiraju odbojci uz poprilično visoki udio pločica i sječiva (u usporedbi s Kopačinom). Kod strmo retuširanih alatki dominantne su pločice s hrptom, a u mlađoj fazi se javljaju i geometrijski mikroliti. Mikrodubila su prisutna i u Nugljanskoj, i to u obje faze. Uzimajući u obzir gore navedeno, možemo zaključiti: na istarskim nalazištima kao i u Kopačini odbojci predstavljaju primarni proizvod lomljenja; pločice su u Istri puno zastupljenije nego u Kopačini; dok su mikrodubila prisutna na gotovo svim spomenutim istarskim nalazištima (osim u Šandalji II, što može biti posljedica neprosijavanja sedimenta), ona nisu poznata u Kopačini; iskrzani komadi puno su rjeđi u Istri nego u Kopačini; udio grebala je velik i u Kopačini i u Istri, ali se čini da su noktolika grebala brojnija u Kopačini; geometrijski mikroliti prisutni su u Kopačini kao i na istarskim nalazištima.128 Komšo, Pellegati 2007, str. 32.129 Komšo, Pellegati 2007, str. 32.130 Komšo, Pellegati 2007, str. 33, sl. 3.5. Ovdje su navedena još tri datuma koja pripadaju spomenutom rasponu.131 Komšo, Pellegati 2007, str. 34.132 Komšo, Pellegati 2007, str. 35; Miracle, Forenbaher 1997, str. 41.9.2. Dalmacija Osim Kopačine, u Dalmaciji su nam poznata još tri kasnoglacijalna nalazišta (Vlakno, Zemunica, Vela spila). S pećinom Vlakno na Dugom otoku možemo povući samo vremensku paralelu jer materijal još nije objavljen. Kasnogornjopaleolitički lovci i skupljači u Vlaknu su boravili između 14.900 BP, utvrđena starost tefre,133 i 10.160 ± 100 BP (Z-3383).134 Kao i u slučaju Vlakna, s pećinom Zemunicom možemo povući samo kronološku paralelu jer litički skup nalaza još nije objavljen, a dio stratigrafskog slijeda vjerojatno pripada kasnom gornjem paleolitiku.135 Kasnoglacijalni boravak lovačko-sakupljačkih zajednica u Veloj spili određen je jednim apsolutnim radiokarbonskim datumom starosti 12.260 ± 40 BP (VERA-2346).136 Uzimajući u obzir dobivenu starost i prisutne tipove alatki te njihovu relativnu učestalost, slojeve 8/2 - 8/6 promatrat ćemo kao cjelinu i usporediti ih s litičkom industrijom iz Kopačine. Dominantna tehnološka kategorija u kasnoglacijalnom litičkom skupu nalaza Vele spile su krhotine (izuzmemo li sitni otpad), nakon kojih slijede odbojci, zatim pločice i na kraju sječiva. Za razliku od Kopačine, pločice i sječiva u Veloj spili proizvođena su puno češće.137 U litičkom inventaru Vele spile autori ne spominju prisutnost mikrodubila.138 U litičkom skupu nalaza Vele spile među alatkama dominiraju grebala, što je slučaj i u Kopačini u obje litičke faze, ali su ona znatno brojnija u Veloj spili, gdje čine gotovo 50 % svih alatki.139 Među grebalima, noktolika su najbrojniji tip nakon grebala na odbojku, dok su noktolika grebala u Kopačini najbrojniji tip među grebalima. Relativna učestalost pločica s hrptom u Veloj spili (oko 12 %) puno je veća nego u Kopačini, ali to može biti posljedica neprosijavanja sedimenta u Kopačini. Među geometrijskim mikrolitima u Veloj spili najbrojniji su kružni segmenti, a prisutan je i samo jedan primjerak trapeza. Veća učestalost geometrijskih mikrolita u Veloj spili nego u Kopačini može biti rezultat, kao i kod pločica s hrptom, metodologije iskopavanja. Relativna učestalost iskrzanih komadića podjednaka je na oba nalazišta. Zakrivljeni šiljci s hrptom brojniji su u Kopačini nego u Veloj spili (0,38 %). Na temelju iznesenog možemo zaključiti da kasnoglacijalne litičke industrije Vele spile i Kopačine pokazuju znatnu sličnost.133 Brusić 2008, str. 402.134 Brusić 2005, str. 198; Komšo 2006, str. 74.135 Šošić, Karavanić 2006, str. 378.136 Čečuk, Radić 2005, str. 34, bilj. 9. Datiran je uzorak drvenog ugljena iz sloja 8/6.137 Čečuk, Radić 2005, str. 26, tablica 2.138 Čečuk, Radić 2005.139 Podaci o relativnoj učestalosti alatki za Velu spilu dobiveni su na temelju podataka prikazanih u Čečuk, Radić 2005, str. 27, tablica 4.

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Amsterdam City Council has banned guided tours in the Red Light District, the downtown area where the prostitution business is concentrated. Although the measure will reach, to varying degrees, other points of the old town, it has been taken there "Out of respect for sex workers" . The majority is shown in the windows that have turned the place into a tourist attraction. Just what the Consistory wants to avoid. Disappear also the tours by the bars of the zone announced only to consume alcohol in all of them. The measure will take effect in January.

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53Kasnoglacijalna industrija lomljenog kamena pećine KopačineLate Glacial knapped stone industry of Kopačina CaveNikola Vukosavljević, Zlatko Perhoč, Božidar Čečuk †, Ivor KaravanićKomšo 2007D. Komšo, Nakit na području Istre od paleolitika do neolitika, in: Scripta praehistorica in honorem Biba Teržan, M. Blečić et al. (eds.), Situla 44, Ljubljana 2007, 31-40.Komšo, Pellegati 2007D. Komšo, P. Pellegati, The Late Epigravettian in Istria. Late Paleolithic colonization and lithic technology in the northern Adriatic area, in: Late Paleolithic Environments and Cultural Relations around the Adriatic, R. Whallon (ed.), BAR International Series 1716, Oxford 2007, 27-39.Kozłowski 1999J. Kozłowski, Gravettian/Epigravettian sequences in the Balkans: environment, technologies, hunting strategies and raw material procurement, in: The Palaeolithic Archaeology of Greece and adjacent areas (Proceedings of the ICOPAG Conference, Ioannina 1994), G. N. Bailey et al. (eds.), British School at Athens Studies 3, London 1999, 330-342.Lubell 2004aD. Lubell, Prehistoric edible land snails in the circum-Mediterranean: the archaeological evidence, in: Petits animaux et Sociétés Humaines, Du Complément Alimentaire Aux Ressources Utilitaires. XXIVerencontres internationales d’archéologie et d’histoire d’Antibes, J.-P. Brugal, J. Desse (eds.), Antibes 2004, 77-98.Lubell 2004bD. Lubell, Are land snails a signature for the Mesolithic-Neolithic transition?, Documenta Praehistorica XXXI, Ljubljana 2004, 1-24.Lugović et al. 1991B. Lugović, R. Altherr, I. Raczek, A.W. Hofmann, V. Majer, Geochemistry of peridotites and mac igneous rock from the Central Dinaric Ophilite Belt, Yugoslavia, Contributions to Mineralogy and Petrology 106, Berlin 1991, 201-216.Magaš, Marinčić 1973N. Magaš, S. Marinčić, Osnovna geološka karta SFRJ 1: 100.000, K 33-20, K 33-21, tumač za listove Split i Primošten, Institut za geološka istraživanja Zagreb, Beograd: Savezni geološki zavod 1973.Magaš et al. 1973 S. Marinčić, N. Magaš, I. Borović, Osnovna geološka karta SFRJ 1: 100.000; List Split, K 33-21. Institut za geološka istraživanja Zagreb (1968-9), Beograd: Savezni geološki zavod 1971.Marinčić et al. 1971S. Marinčić, N. Magaš i I. Borović, Osnovna geološka karta SFRJ 1: 100.000; List Split, K 33-21. Institut za geološka istraživanja Zagreb (1968-9), Beograd: Savezni geološki zavod 1971.Maggi et al. 1995 R. Maggi, N. Campana, F. Negrino, Valle Lagora (I 18): a quarry of radiolarite (jasper) exploited during the Copper and Early Bronze Ages (Liguria, Italy), Archaeologija Polona 33, Warszawa 1995, 187-208.Majer, Jurković 2001V. Majer, I. Jurković, Bilješka o nalazu krom-spinela kod Čelinca u Bosni, Znanstveni radovi 1954-1999, Zagreb 2001, 337-339. Malez, Vogel 1969M. Malez, J. C. Vogel, Rezultati određivanja apsolutne starosti pleistocenskih naslaga Šandalje II kod Pule u Istri, Geološki vjesnik 22 (1968), Zagreb 1969, 121-133.Flügel 1978E. Flügel, Mikrofazielle Untersuchungsmthoden von Kalken, Berlin 1978.Forenbaher 2002S. Forenbaher, Prehistoric Populations of the Island of Hvar - An Overview of Archaeological Evidence, Collegium Antropologicum 26/1, Zagreb 2002, 361-378.Forenbaher et al. 2010S. Forenbaher, T. Kaiser, S. Frame, Adriatic Mortuary Ritual at Grapčeva Cave, Croatia, Journal of Field Archaeology 35/4, Boston 2010, 337-354. Füchtbauer, Müller 1970H. Füchtbauer, G. Müller, Sediment-Petrologie. Teil II: Sedimente und Sedimentgesteine, Stuttgart 1970. Goodfriend 1987 G. A. Goodfriend, Radiocarbon age anomalies in shell carbonate of land snails from semi-arid areas, Radiocarbon 29 (2), Tucson 1987, 159-167.Goodfriend 1992 G. A. Goodfriend, The use of land snail shells in paleoenvironmenal reconstruction, Quaternary Science Reviews 11, Amsterdam 1992, 665-685.Goodfriend, Stipp 1983G. A. Goodfriend, J. J. Stipp, Limestone and the problem of radiocarbon dating of land-snail shell carbonate, Geology 11, Washington 1983, 575-577.Goričan 1994Š. Goričan, Jurassic and Cretaceous radiolarian biostratigraphy and sedimentary evolution of the Budva Zone (Dinarides, Montenegro), Mémoires de Géologie 18, Lausanne 1994.Grunau 1965H. R. Grunau, Radiolarian chert and associated rock in space and time, Eclogae Geologicae Helvetiae, 58/1, Basel 1965, 157-209.Halamić, Šošić Klindžić 2009J. Halamić, R. Šošić Klindžić, Radiolarites and Radiolarian chert in Northern Croatia - Possible sources for the Production of Artfact, Archeometriai Mühely 2009. VI. 3., 19-24. (dostupno na: http://www.ace.hu/am/2009_3 pristup 01. 07. 2010).Hrvatović 2006H. Hrvatović, Geological Guidebook through Bosnia and Herzegovina, Sarajevo 2006.Ivanović et al. 1976A. Ivanović, K. Sakač, B. Sokač, I. Vrsalović-Carević, J. Županić, Osnovna geološka karta SFRJ, tumač za list Obrovac, 1:100.000, Institut za geološka istraživanja Zagreb (1967), Beograd, Savezni geološki zavod, 1976.Karavanić 1999I. Karavanić, Gornji paleolitik Šandalje II u okviru jadranske regije, neobjavljena doktorska disertacija, Sveučilište u Zagrebu, Zagreb 1999.Kliškić 2007D. Kliškić, Špilja Kopačina, Hrvatski arheološki godišnjak 2(2006), Zagreb 2007, 443-445.Kliškić 2008D. Kliškić, Špilja Kopačina, Hrvatski arheološki godišnjak 4(2007), Zagreb 2008, 528-530.Komšo 2006D. Komšo, Mezolitik u Hrvatskoj, Opuscula archaeologica 30, Zagreb 2006, 55-91.Marjanac 1987T. Marjanac, Sedimentacija Kernerove “srednje iške zone” (paleogen, okolica Splita), Geološki vjesnik 40, Zagreb 1987, 177-194.Marjanac et al. 1998T. Marjanac, D. Baba, J. Benic, V. Ćosović, K. Drobne, Lj. Marjanac, R. Pavlovec, Z. Velimirović, Eocene Carbonate Sediments and Sea-Level Changes on the NE Part of Adriatic Carbonate Platform (Island of Hvar and Peljesac Peninsula, Croatia), Dela-Opera SAZU 4. razred 34/2, Ljubljana 1998, 243-254. Mihailović 1996D. Mihailović, Upper Palaeolithic and Mesolithic chipped stone industries from the rock-shelter of Medena Stijena, in: Prehistoric settlements in caves and rock-shelters of Serbia and Montenegro (Fascicule 1), D. Srejović (ed.), Beograd 1996, 9-60.Mihailović 1998D. Mihailović, Gornji paleolit i mezolit Crne Gore, neobjavljena doktorska disertacija, Univerzitet u Beogradu, Beograd 1998.Mihailović 1999D. Mihailović, Intensication of settlement in the Late Glacial of south-western Balkans, Folia Quaternaria 70, Kraków 1999, 385-392.Mihailović 2009D. Mihailović, Upper Palaeolithic and Mesolithic chipped stone industries from Crvena stijena (Prehistoric settlements in caves and rock-shelters of Serbia and Montenegro Fascicule II), Beograd 2009.Miracle 1995 P. T. Miracle, Broad-Spectrum Adaptations Re-Examined: Hunther-Gatherer Responses to Late Glacial Environmental Changes in the Eastern Adriatic, neobjavljena doktorska disertacija, University of Michigan, Ann Arbor 1995. Miracle 1996P. Miracle, Diversication in Epipaleolithic subsistence strategies along the Eastern Adriatic coast: a simulation approach applied to zooarchaeological assemblages, Atti della Società per la Preistoria e Protostoria della regione Friuli-Venezia Giulia IX(1994-1995), Trieste 1996, 33-62.Miracle, Forenbaher 2000P. T. Miracle, S. Forenbaher, Pupićina Cave project: Brief summary of the 1998 season - Projekt Pupićina peć: prethodni izvještaj o istraživanjima tijekom 1998. godine, Histria archaeologica 29(1998), Pula 2000, 27-47.Müller 1964G. Müller, Sediment-Petrologie. Teil I: Methoden der Sediment-Untersuchung, Stuttgart 1964.Obelić et al. 1994B. Obelić, N. Horvatinčić, D. Srdoč, I. Krajcar Bronić, A. Sliepčević, S. Grgić, Rudjer Bošković Institute radiocarbon measurements XIII, Radiocarbon 36 (2), Tucson 1994, 303-324.Pamić 2000J. Pamić, Radiolarite Formation, Vijesti Hrvatskoga geološkoga društva 37/2, Zagreb 2000, 70.Pamić, Hrvatović 2000J. Pamić, H. Hrvatović, Dinaride Ophiolite Zone (DOZ). Basic data on the geology end petrology of the Krivaja-Konjuh ophiolite complex, Vijesti Hrvatskoga geološkoga društva 37/2, Zagreb 2000, 60-68. Perhoč u pripremiZ. Perhoč, Litički nalazi sa otoka Sušca.Perhoč 2009aZ. Perhoč, Sources of Chert in Middle Dalmatia: Supplying Raw Material to Prehištoric Lithic Industries, in: A Connecting Sea: Maritime Interaction in Adriatic Prehistory, S. Forenbaher (ed.), BAR International Series 2037, Oxford 2009, 25-46. Perhoč 2009b Z. Perhoč, Sources of Chert for Prehistoric Lithic Industries in Middle Dalmatia, Archeometriai Mühely, 2009. VI. 3., 45-56 (dostupno na: http://www.ace.hu/am/2009_3 pristup 01. 07. 2010). Pettijohn 1957F. J. Pettijohn, Sedimentary Rocks, New York 1957.Radovanović 1986I. Radovanović, Novija istraživanja paleolita i mezolita u Crnoj Gori, Glasnik srpskog arheološkog društva 3, Beograd 1986, 63-77.Reimer et al. 2009P. J. Reimer, M.G.L. Baillie, E. Bard, A. Bayliss, J. W. Beck, P. G. Blackwell, C. Bronk Ramsey, C. E. Buck, G.S. Burr, R. L. Edwards, M. Friedrich, P. M. Grootes, T. P. Guilderson, I. Hajdas, T. J. Heaton, A. G. Hogg, K. A. Hughen, K. F. Kaiser, B. Kromer, F. G. McCormac, S. W. Manning, R. W. Reimer, D. A. Richards, J. R. Southon, S. Talamo, C. S. M. Turney, J. van der Plicht, C. E. Weyhenmeyer, IntCal09 and Marine09 Radiocarbon Age Calibration Curves, 0-50,000 Years cal BP, Radiocarbon 51(4), Tucson 2009, 1111-1150.Surić 2006M. Surić, Promjene u okolišu tijekom mlađeg pleistocena i holocena - zapisi iz morem potopljenih siga istočnog Jadrana, neobjavljena doktorska disertacija, Prirodnoslovno-matematički fakultet, Zagreb 2006.Šegota 1979T. Šegota, Prirodni okviri u kvartaru jugoslavenskih zemalja; Paleoklimatske i Paleografske promjene, in: Praistorija jugoslavenskih zemalja I - Paleolitsko i mezolitsko doba, A. Benac (ed.), Sarajevo 1979, 21-33.Šošić, Karavanić 2006R. Šošić, I. Karavanić, Pećina Zemunica, Hrvatski arheološki godišnjak 2(2005), Zagreb 2006, 376-378.Tamers 1970 M. A. Tamers, Validity of Radiocarbon Dates on Terrestrial Snail Shells, American Antiquity 35/1, Washington 1970, 94-100.Tišljar 2001J. Tišljar, Sedimentologija karbonata i evaporita, Zagreb 2001.Tišljar 2004J. Tišljar, Sedimentologija klastičnih i silicijskih taložina, Zagreb 2004.Tišljar et al. 2002J. Tišljar, I. Vlahović, I. Velić i B. Sokač. Carbonate Platform Megafacies of the Jurassic and Cretaeous Deposits of the Karst Dinarides, Geologica Croatica 55/2, Zagreb 2002, 139-170.Vrsalović 1960 D. Vrsalović, Pretpovijest i stari vijek, Brački zbornik 4 (Kulturni spomenici otoka Brača), Supetar 1960, 31-110.

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37Kasnoglacijalna industrija lomljenog kamena pećine KopačineLate Glacial knapped stone industry of Kopačina CaveNikola Vukosavljević, Zlatko Perhoč, Božidar Čečuk †, Ivor Karavanić The nummulitic cherts are probably an island import, because the Eocene limestone deposits on Brač are negligible and do not contain cherts.81 On the remaining central Dalmatian islands, we have only discovered vestiges of cherts without any sign of technological value in the narrow Hvar Eocene belt.82The most numerous, abundant and easily accessible outcrops of Eocene chert closest to Brač were recorded in the central Dalmatian belt of the Split-Kaštel area83 on the southern slope of Vlaška Hill, in Seget Donji, on Opor, Kozjak and Mosor, on the Marjan Peninsula, on the island of Čiovo and in Baška Voda.847.3.2. Micritic limestone chertsThe sub-group of cherts which emerged in micritic limestone, wherein the grey transparent type is distinguished from the yellowish translucent chert, and which encompasses the most artefacts, is of insular origin. The sub-group contains 1,774 nds (38.56% of the total number) and its weight share is 42.79% in the total inventory mass (Fig. 9). The Brač cherts, particularly the grey type, evidently lags behind the quality of the stones from other groups, largely from more distant sources. The grey type, with 1,077 nds, predominates in this sub-group. The core portion of the nodule is grey with several nuances, with very unremarkable lustre or even entirely matte and poor translucence, most often opaque.85The chert emerged in friable micrite limestone (Fig. 15).81 The guide to the basic geological map does not indicate the appearance of cherts in the Brač Eocene deposits at Cape Gomilica (Magaš, Marinčić 1973, p. 23; Marinčić et al. 1971).82 Marjanac et al. 1998, p. 224. We did not research the cherts in the Eocene belt on Pelješac Peninsula.83 Marjanac 1987, pp. 182-188; Marjanac et al. 1998, p. 224.84 For details on outcrops, see Perhoč 2009b.85 N9-4; red and yellow tiny grains of haematite and goethite are visible in the polished section.Fossil detritus is not visible on the polished section. Thus far, we have recorded such cherts on Brač on the northern side of the island in the Upper Cretaceous zone of limestones with lenses, inserts or interlayers of dolomite. In Pučišće, on Mala Bračuta Hill and the northern slope of Mladinje Hill, an autochthonous outcrop of rare chert lenses were recorded. The chert outcrop in the vicinity of Dol is more productive, with somewhat higher quality product and thus more archeologically relevant. There are rare nodule fragments in the torrential detritus in Dunaj eld, and more in the loose rock of the surrounding hills, particularly on the northern and western slope of Veli Hill, where outcrops of limestone with cherts are visible. The yellowish, yellow-brown type has a waxy lustre and more notable transparency than the grey type.86Very tiny fossil detritus is visible in the micritic mass in the polished section. The yellowish chert type is of a better quality than the grey, but among the greys there are black-grey lots, normally toward the middle of the nodule, which have a higher quality than the peripheral portions. The nodular rim has the same traces of wear as in the fossiliferous chert group, which indicates the same type of outcrop. We have linked the origin of the yellowish chert type to the grey type based on a similar structure, but we know of no specic deposit. There are examples of zonal structure in both types of this sub-group. The geological data on the formation of Sveti Duh with limestones and dolomites of Turonian Upper Cretaceous age in which there are bulbs of chert in the area between Vidova gora and Gornji Humac,87 just like our nds of chert karst on the beaches of the Bol inlet, indicate that there are more chert deposits on Brač than we have thus far recorded.887.3.3. Bioclastic limestone chertsThe weight share of this chert is 15.97%, with 483 nds, accounts for 10.5% of the total number (Fig. 9). The cherts are dark brown, with waxy lustre and poor or no translucence.89The nodular rim, whereby we have classied it in the metasomatic nodular cherts, is brown like the core, but lighter. The core portion of the nodule has a very uniform ne-grain structure which has a shell-like appearance under the magnifying scope. On a thin-section, it is apparent that the chert emerged by silicication of dense micrite and generally unrecognizable tiny fragments of shells of marine organisms (the shells of shellsh and brachiopods can be discerned) (Fig. 16). Rare, scattered red haematite grains can be seen. Almost of a third of the nds from this sub-group are deeply patinated, so the external worn cortex largely diers from the core portion. The wear cortex is characterized by tiny cavities made by the washing o of calcite, and only visible under a magnifying scope. They are lled with terra rossa, so the stone seems grainy, with a dark porcelain lustre, or entirely matte.86 10YR5/4.87 Derado 1984, pp. 8-9 (map based on V. Nastić et al. 1958).88 Perhoč, unpublished nd, 2010.89 10YR4/2, 5/4. Numulitni rožnjaci vjerojatno su otočki import, jer su eocenske naslage vapnenaca na Braču neznatne i bez rožnjaka.81 Od ostalih srednjodalmatinskih otoka, u uskom hvarskom eocenskom pojasu otkrili smo tek tragove rožnjaka bez ikakve tehničke vrijednosti.82Brojne, obilne i lako dostupne, Braču najbliže izdanke eocenskih rožnjaka zabilježili smo u srednjodalmatinskom eocenskom pojasu splitsko-kaštelanskog područja,83 i to na južnoj padini brda Vlaška, u Segetu Donjem, na Oporu, Kozjaku i Mosoru, na poluotoku Marjanu, na Čiovu i u Baškoj Vodi.847.3.2. Rožnjaci mikritnog vapnencaArtefaktima najzastupljenija podskupina rožnjaka nastalog u mikritnom vapnencu, u kojoj razlikujemo tip sivog neprozirnog i tip žućkastog svjetlopropusnog rožnjaka je otočkog porijekla. Podskupina broji 1774 nalaza (38,56 % od ukupnog broja) i težinskog je udjela od 42,79 % u ukupnoj masi inventara (sl. 9). Brački rožnjaci, naročito sivi tip, tehničkom kakvoćom osjetno zaostaju za kakvoćom kamena iz drugih skupina, mahom iz udaljenijih izvora. Sivi tip sa 1077 nalaza prevladava u ovoj podskupini. Jezgreni dio nodule je siv, s nekoliko nijansi, vrlo neizraženog sjaja ili sasvim mat i slabe svjetlopropusnosti, najčešće svjetlonepropustan.85 Rožnjak je nastao u mrvičastom mikritnom vapnencu (sl. 15). 81 Tumač osnovne geološke karte u bračkim eocenskim naslagama kod rta Gomilice ne navodi pojavu rožnjaka (Magaš, Marinčić 1973, str. 23; Marinčić et al. 1971).82 Marjanac et al. 1998, str. 224. Rožnjake u eocenskom pojasu na poluotoku Pelješcu nismo istraživali.83 Marjanac 1987, str. 182-188; Marjanac et al. 1998, str. 224.84 Podrobnosti o izdancima, vidi u Perhoč 2009b.85 N9-4; u nabrusku su vidljiva crvena i žuta sitna zrna hematita i getita. Fosilni detritus na nabrusku nije vidljiv. Do sada smo ovakve rožnjake na Braču zabilježili na sjevernoj strani otoka u gornjokrednoj zoni vapnenaca s lećama, ulošcima ili proslojcima dolomita. U Pučišćima na brdu Mala Bračuta i sjevernoj padini Mladinjeg brda zabilježen je autohtoni izdanak rijetkih leća rožnjaka. Izdanak rožnjaka u okolici Dola je izdašniji, nešto je bolje kakvoće i time arheološki relevantniji. Rijetkih fragmenata nodula ima u nanosu bujičnjaka u polju Dunaj, više u siparu okolnih brda, osobito na sjevernom i zapadnom obronku Velog brda, gdje su vidljivi izdanci vapnenca s rožnjacima. Žućkasti, žutosmeđi tip ima voštani sjaj i izraženiju transparentnost u odnosu na sivi tip.86 U nabrusku je u mikritnoj masi vidljiv vrlo sitan fosilni detritus. Rožnjak žućkastog tipa bolje je kakvoće od sivih, ali i među sivima ima crnosivih partija, obično prema središtu nodule, koje su bolje kakvoće od perifernih dijelova. Nodularna okorina ima iste tragove trošenja kao i u skupini fosilifernih rožnjaka, što upućuje na isti tip izdanka. Porijeklo žućkastog tipa rožnjaka temeljem slične strukture vežemo za sivi tip, no konkretna ležišta nam nisu poznata. U oba tipa ove podskupine ima primjeraka sa zonarnom strukturom. Geološki podaci o formaciji Sveti Duh s vapnencima i dolomitima turonske gornjokredne starosti u kojima ima kvrga rožnjaka na području između Vidove gore i Gornjeg Humca,87kao i naši nalazi rožnjačkog krša na žalu bolskog zaljeva, ukazuju da na Braču ima više ležišta rožnjaka nego što smo ih do sada zabilježili.887.3.3. Rožnjaci bioklastičnog vapnenca Težinski udio ovog rožnjaka je 15,97 %, sa 483 nalaza zauzima 10,5 % od ukupnog broja (sl. 9). Rožnjaci su zagasite smeđe boje, voštanoga sjaja i slabe ili nikakve svjetlopropusnosti.89 Nodularna okorina, po kojoj ih svrstavamo u metasomatske nodularne rožnjake, smeđe je boje kao i jezgra, ali svjetlija. Jezgreni dio nodule vrlo je ujednačene sitnozrne strukture koja pod povećalom ima ljuskav izgled. Na nabrusku je vidljivo da je rožnjak nastao siliciciranjem gustog mikrita i uglavnom neprepoznatljivih sitnih fragmenata ljušturica morskih organizama (razaznaju se ljušturice školjkaša i brahiopoda) (sl. 16). Vide se rijetka raspršena crvena zrnca hematita. Gotovo trećina nalaza iz ove podskupine duboko je patinirana pa se vanjska trošna kora uvelike razlikuje od jezgrenog dijela. Trošnu koru karakteriziraju sitne kaverne nastale ispiranjem kalcita, a vidljive su tek pod povećalom. Ispunjene su crvenicom pa kamen djeluje zrnato, prigušenog je porculanskog sjaja ili je sasvim mat.86 10YR5/4.87 Derado 1984, str. 8, 9 (karta prema Nastiću et al. 1958).88 Perhoč neobjavljeni nalaz 2010.89 10YR4/2, 5/4. Slika 16. Bioklastični rožnjak. Binokularni mikroskop, nabrusak Figure 16. Bioclastic chert. Binocular microscope, polished section Slika 15. Mikritni rožnjak. Binokularni mikroskop, nabrusak Figure 15. Micritic chert. Binocular microscope, polished section

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(PDF) Late Glacial knapped stone industry of Kopacina Cave

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Na primjer, prva tri slova „pogon“ i „Skelter“ možete koristiti za izradu „rijSke“. Učinite isto za tri druge priče, kombinirajte te izmišljene riječi i dobit ćete lozinku od 18 znakova koja izgleda potpuno slučajno.The minimum investment is just $10 (around €9.60) at eToro. The option of buying just a fraction of a digital currency like Bitcoin makes it more achievable to enter the crypto market for most traders. Looking to buy stocks in Netherlands? There is also a long list of stocks, which includes those listed on the Amsterdam exchange as well as others from around the world.

V investiční aplikaci a webové verzi platformy můžete dělat ty samé úkony jako v hlavní verzi pro stolní počítače. Ať už jde o nákup a prodej akcií, kontrolu hodnoty portfolia nebo vklad/výběr prostředků, vše tu najdete na svém místě.

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