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1

Tiralongo, F., and R. Baldacconi. "First record of the Combtooth Blenny, Microlipophrys adriaticus (Steindachner & Kolombatovic, 1883) (Pisces, Blenniidae), for the Italian Ionian Sea." Check List 11, no. 3 (April 28, 2015): 1646. http://dx.doi.org/10.15560/11.3.1646.

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Microlipophrys adriaticus (Steindachner & Kolombatovic, 1883) is an endemic blenny of the Mediterranean Sea. It is also known from the Sea of Marmara and the Black Sea. However, unlike other species of combtooth blennies, M. adriaticus is a fish with a limited distribution in Adriatic Sea, especially in the north, where it can be common. We report here the first record of this species from the waters of the Ionian Sea.
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2

Bínová, Helena, and Martin Jurkovič. "European Transport Corridors and North Adriatic Ports." Transport and Communications 3, no. 2 (2015): 1–7. http://dx.doi.org/10.26552/tac.c.2015.2.1.

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From the ports in the northern Adriatic Sea (ports of Ravenna, Venezia, Trieste, Koper, Rijeka) a route from European ports of North Sea to the Far East is shorter by about 2000 nautical miles. It means a reduction of 6 to 8 days in shipping. These ports are reachable from commercial and industrial centers of Central and Eastern Europe. An assessment of the current situation and future development of the European transport corridors North - South, including possible interconnection by multimodal corridors Baltic ports in the north and Adriatic ports in the south, is included in this paper. This corridor is one of the ten basic corridors included in the new conception of the TEN-T European transport network with the assumption of financial support from the EU in the period of 2014-2020. Further, the paper also includes an analysis of a modal assessment (Modal Split) of transport connections of Central Europe with the Far East. The heart of the paper is a proposal of connection of chosen seaports that serve as logistics terminals to current European multimodal corridors and further to proposed multimodal corridors.
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3

Stamatović, Kristijan, Peter de Langen, and Aleš Groznik. "Port cooperation in the North Adriatic ports." Research in Transportation Business & Management 26 (March 2018): 109–21. http://dx.doi.org/10.1016/j.rtbm.2018.03.006.

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4

Tinti, Fausto, Vincenzo Caputo, Silvia Franzellitti, Paola Nisi Cerioni, Carola Vallini, Massimo Giovannotti, Elena Fabbri, and Sergio Guccione. "Genetic characterization of loggerhead turtle (Caretta caretta) individuals stranded and caught as bycatch from the North-Central Adriatic Sea." Amphibia-Reptilia 31, no. 1 (2010): 127–33. http://dx.doi.org/10.1163/156853810790457902.

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AbstractThe North Adriatic Sea is considered a critical feeding and developmental area for Mediterranean loggerhead turtles. In this study, a comparative analysis of mitochondrial DNA control region sequences was carried out on sixty-five loggerhead individuals stranded and caught as bycatch in the Adriatic Sea from 1999 to 2002. We demonstrated the existence of genetic relationships between the North-Central Adriatic (NCA) aggregate and the Central-Eastern Mediterranean rookeries. Short-range and long-range migrations towards the Adriatic Sea were hypothesized by the finding of individuals bearing haplotypes endemic to the nesting populations of Greece and Turkey. The occurrence of individuals belonging to dimensional classes from juveniles to mature adults strongly support both the feeding and developmental role of the NCA.
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5

Dulčić, Jakov. "First Record of the Cornich Blackfish Schedophilus Medusophagus (Pisces: Centrolophidae) Larvae from the Adriatic Sea." Journal of the Marine Biological Association of the United Kingdom 78, no. 3 (August 1998): 1035–38. http://dx.doi.org/10.1017/s002531540004501x.

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The capture of the cornich blackfish, Schedophilus medusophagus, larvae from the Adriatic Sea represents an easterly extension in range of this species, and the first larval record in Adriatic waters.Schedophilus medusophagus Cocco, 1839, is a mesopelagic species from temperate waters of the north-eastern and north-western Atlantic and the western Mediterranean (Bini, 1968; Tortonese, 1975; Haedrich, 1986). The first record of this fish from the Adriatic Sea was reported in 1880 according to Ninni (1912). The second record was during the invasion of medusae Pelagia noctiluca (Malej, 1982; Rottini-Sandrini & Stravisi, 1982; Vučetić, 1982,1983) in Pelješac channel near the town of Korčula-island Koršula (central Adriatic) in 1982 (Onofri, 1986). Ten juvenile specimens, from 10·0 to 20·0cm total length (TL), were collected with medusae at 2m depth. This record Onofri (1986) connected with the ingression of inter-median waters (50–100 m) in the central Adriatic influenced the increase of salinity and temperature in 1982. Jardas (1996) noted that S. medusophagus is a very rare species in the Adriatic Sea.
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6

Rogelja Caf, Nataša, Alenka Janko Spreizer, and Martina Bofulin. "PLENTY OF FISH IN THIS SEA: SIFTING THE PAST IN THE NORTHEASTERN ADRIATIC." Traditiones 49, no. 3 (December 31, 2020): 17–34. http://dx.doi.org/10.3986/traditio2020490302.

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The paper discusses heritagization, remembering, and past presencing in the North East Adriatic through the four fish species that serve as nodal points in the interplay between the past and the present. Following the selected fish species, the paper explores the diversity of imaginaries that pertain to the mediation of the past in the present in the field of ethnological study in the North East Adriatic.
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7

Leder, N., and M. Orlic. "Fundamental Adriatic seiche recorded by current meters." Annales Geophysicae 22, no. 5 (April 8, 2004): 1449–64. http://dx.doi.org/10.5194/angeo-22-1449-2004.

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Abstract. Currents recorded at two stations positioned at the Adriatic shelf break between 17 February and 6 March 1989 were considered. They provided the first evidence of current variability related to the Adriatic-wide seiches. Current spectra were dominated by a peak at 21.1h – a well-known period of the fundamental Adriatic mode. Amplitudes of oscillations were considerable, occasionally greater than 30cm/s. Both along- and cross-basin currents were recorded, thus signalling the importance of rotational effects. Comparison of the current data with the sea-level measurements performed simultaneously along the east Adriatic coast showed that the 21-h currents flowing in the Adriatic preceded sea levels by a quarter of a cycle, as would be expected from a simple model of bay seiches. Sea-level amplitudes reached 40cm in the North Adriatic, thus marking the event as one of the strongest on record. Seiching was triggered by a suddenly changing sirocco wind, as is usually the case in the Adriatic. The most important features of the seiche event were reproduced with a two-dimensional hydrodynamic model of the Adriatic Sea, forced by the sea-level residuals measured at Otranto and the air pressure and wind data recorded at Lastovo. The model showed that the seiche-related currents were relatively strong in the area where the current measurements were performed and further north – between Zadar and Ancona. Key words. Oceanography: general (continental shelf processes) – Oceanography: physical (sea-level variations, currents)
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8

Gačić, M., G. Civitarese, V. Kovačević, L. Ursella, M. Bensi, M. Menna, V. Cardin, et al. "Extreme winter 2012 in the Adriatic: an example of climatic effect on the BiOS rhythm." Ocean Science Discussions 11, no. 1 (February 3, 2014): 425–52. http://dx.doi.org/10.5194/osd-11-425-2014.

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Abstract. Adriatic and Ionian Seas are Mediterranean sub-basins linked through the Bimodal Oscillating System mechanism responsible for decadal reversals of the Ionian basin-wide circulation. Altimetric maps showed that the last cyclonic mode started in 2011 but unexpectedly in 2012 reversed to anticyclone. We related this "premature" inversion to extremely strong winter in 2012, which caused the formation of very dense Adriatic waters, flooding Ionian flanks in May and inverting the bottom pressure gradient. Using Lagrangian float measurements, the linear regression between the sea surface height and three isopycnal depths suggests that the southward deep-layer flow coincided with the surface northward geostrophic current and the anti-cyclonic circulation regime. Density variations at depth in the north-western Ionian revealed the arrival of Adriatic dense waters in May and maximum density in September. Comparison between the sea level height in the north-western Ionian and in the basin centre showed that in coincidence with the arrival of the newly formed Adriatic dense waters the sea level lowered in the north-western flank inverting the surface pressure gradient. Toward the end of 2012, the density gradient between the basin flanks and its centre went to zero, coinciding with the weakening of the anticyclonic circulation and eventually with its return to the cyclonic pattern. Thus, the premature and transient reversal of Ionian surface circulation originated from the extremely harsh winter in the Adriatic, resulting in the formation and spreading of highly dense bottom waters. The present study highlights the remarkable sensitiveness of the Adriatic–Ionian BiOS to climatic forcing.
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9

De Giulio, A., S. De Rosa, G. Di Vincenzo, and N. Zavodnik. "Terpenoids from the North Adriatic Sponge Spongia officinalis." Journal of Natural Products 52, no. 6 (November 1989): 1258–62. http://dx.doi.org/10.1021/np50066a010.

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10

De Giulio, A., S. De Rosa, G. Di Vincenzo, G. Strazzullo, and N. Zavodnik. "Norsesterterpenes from the North Adriatic Sponge Ircinia oros." Journal of Natural Products 53, no. 6 (November 1990): 1503–7. http://dx.doi.org/10.1021/np50072a016.

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11

Shabrang, L., M. Menna, C. Pizzi, H. Lavigne, G. Civitarese, and M. Gačić. "Long-term variability of the southern Adriatic circulation in relation to North Atlantic Oscillation." Ocean Science 12, no. 1 (February 12, 2016): 233–41. http://dx.doi.org/10.5194/os-12-233-2016.

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Abstract. The interannual variability of the South Adriatic Gyre and its relation to the wind vorticity and the large-scale climatic pattern (North Atlantic Oscillation – NAO) was studied using the time series of satellite altimetric data and ocean surface wind products. The cyclonic circulation observed in the southern Adriatic area was partly sustained by the local wind forcing, as suggested by the positive correlation between the rate of change of the current vorticity and the wind-stress vorticity. Nevertheless, the influence of vorticity advection from the adjacent area (northern Ionian Sea) cannot be ignored and it is more significant during the anticyclonic phase of Adriatic–Ionian Bimodal Oscillation System. The geostrophic current vorticities of the southern Adriatic and northern Ionian seas are correlated with a time lag of 14 months, which approximately corresponds to an advection speed of ∼ 1 cm s−1. The different wind patterns observed during two NAO phases in the winter revealed a stronger positive vorticity during the negative NAO phase. Conversely, during the wintertime positive NAO phase the wind vorticity is characterized by lower positive or slightly negative values. Despite a statistically significant negative correlation between the NAO index and the wind vorticity, no unequivocal relationship between large climatic system and the interannual variability of the South Adriatic Gyre intensity was found due to additional effects of the vorticity advection from the Ionian. This can be explained by the fact that the Ionian circulation mode does not depend on the NAO variations. Therefore, the main result of this study is that the interannual variability of the southern Adriatic cyclonic circulation is a result of the combined influence of the vorticity advection from the Ionian and the local wind-curl effect.
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12

Stefanni, S., E. S. Gysels, F. A. M. Volckaert, and P. J. Miller. "Allozyme variation and genetic divergence in the sand goby, Pomatoschistus minutus (Teleostei: Gobiidae)." Journal of the Marine Biological Association of the United Kingdom 83, no. 5 (September 19, 2003): 1143–49. http://dx.doi.org/10.1017/s0025315403008403h.

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Samples of the widely distributed sand goby Pomatoschistus minutus have been investigated genetically from ten localities in the north-eastern Atlantic, North Sea, western Mediterranean and Adriatic Sea. Levels of genetic diversity and differentiation were assessed with starch (SGE) and cellulose acetate (CAGE) gel electrophoresis for 13 enzyme systems. Genetic differentiation between spatial samples points to a reduction or even absence of gene flow between the Adriatic and the other samples, including the western Mediterranean Sea (pair-wise FST=0.37 and 0.32 for SGE and CAGE respectively). The sample from the Adriatic Sea was clearly differentiated from the other samples at the lactate dehydrogenase loci LDH-A* (SGE and CAGE) and LDH-C* (CAGE). Values for genetic differentiation between Venetian and other sand gobies were of the same order of magnitude as between P. minutus and its closest relative P. lozanoi, suggesting allopatric speciation in the lagoon of Venice. At locations outside the Adriatic Sea, the sand goby has the typical features of a marine fish with a high level of gene flow and a low degree of genetic differentiation.
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13

Živković, Igor, Jože Kotnik, Mladen Šolić, and Milena Horvat. "The abundance, distribution and speciation of mercury in waters and sediments of the Adriatic Sea." Acta Adriatica 58, no. 1 (June 21, 2017): 165–86. http://dx.doi.org/10.32582/aa.58.1.14.

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This review focuses on mercury speciation in the Adriatic Sea, a marginal sea of the Mediterranean, which represents its distinct biogeochemical subunit due to anthropogenic mercury loadings. The current knowledge about mercury cycling in the Adriatic is presented through an overview of the state of the art of research in this area: temporal and spatial distributions and occurrence of mercury species in seawater and sediment, and chemical transformations. We summarised research results of mercury speciation in order to describe its presence and fate in the Adriatic Sea. The Adriatic Sea represents a net source of mercury to the Mediterranean Sea due to the highest total mercury concentrations observed in the North Adriatic Sea and the highest methylmercury concentrations in the South Adriatic Pit. However, the biogeochemical cycle of mercury is not completely known and our understanding of mercury transport between compartments and its (bio)transformations is limited. Future research needs to focus on microbial and chemical processes of mercury transformations to improve our understanding of the impacts of mercury contamination on the environment and human health in the Adriatic Sea.
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14

Grossi, Laura, Fabio Bertasi, and Benedetta Trabucco. "New records of the alien polychaete worm Chaetozone corona (Polychaeta: Cirratulidae) in the Adriatic Sea." Acta Adriatica 58, no. 2 (December 22, 2017): 235–44. http://dx.doi.org/10.32582/aa.58.2.4.

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Several specimens of the alien polychaete Chaetozone corona were encountered at sites along the Italian coasts of the Adriatic Sea between 2006 and 2015, indicating its successful establishment in the area. Morphological variability between specimens from the North Adriatic and the South Adriatic was detected. Methyl Green staining patterns revealed further minor differences suggesting the presence of two slightly different populations. Chaetozone corona does not appear to be invasive in natural conditions, but it appears more abundant in polluted port sediments, what may represent the main source of introduction.
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15

Ezgeta-Balić, Daria, Tanja Šegvić-Bubić, Elizabeta Briski, Leon Grubišić, Dubravka Bojanić Varezić, Yaping Lin, and Nika Stagličić. "Rasprostranjenost nezavičajne vrste kamenice Magallana gigas(Thunberg, 1793) duž istočne obale Jadrana." Acta Adriatica 60, no. 2 (December 27, 2019): 137–46. http://dx.doi.org/10.32582/aa.60.2.3.

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Non-native Pacific oyster Magallana gigas (Thunberg, 1793) was introduced to the Mediter-ranean Sea for aquaculture purposes in the 1960s. Although this species was not introduced for aquaculture to the Croatian part of the Adriatic Sea, in the 1970s, it was reported in the Lim Bay, in the North-eastern Adriatic. Until recently, there has been no research on the species in the Croatian part of the Adriatic. The aim of this research was to summarize existing and novel data on the distribution of M. gigas in coastal areas of the Eastern Adriatic and to provide a baseline for the future monitoring and assessment programmes of the species. Distribution of M. gigas was determined by three different methods: (i) a visual census of the presence of M. gigas specimens in the medio-littoral zone; (ii) DNA identification of M. gigas larvae in the water column; and (iii) the presence of M. gigas in the subtidal zone at depth between 25 and 40 m. Magallana gigas has a well-established population in the medio-littoral zone of natural and anthropogenic habitats along the coast of the North-eastern Adriatic Sea (west coast of Istria peninsula), but it is not present in the deeper layers . In the Central-eastern and South-eastern Adriatic Sea, the species was either absent or sporadically recorded with no evidence of fully established populations. Considering the great invasion success of M. gigas worldwide and effects that this species could have on the invaded ecosystem (e.g. competition for food and space with native species), detailed future monitoring is needed for the Eastern Adriatic Sea.
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BAKRAN-PETRICIOLI, TATJANA, MIRKO RADOLOVIĆ, and DONAT PETRICIOLI. "How diverse is sponge fauna in the Adriatic Sea?" Zootaxa 3172, no. 1 (January 25, 2012): 20. http://dx.doi.org/10.11646/zootaxa.3172.1.2.

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The Adriatic Sea can be considered as a large, mostly shallow embayment of the Mediterranean Sea. The latitudinal SE-NW extension of the Adriatic results in considerable climate differences along its coast. In this work we compiled the listof sponges from classes Demospongiae and Homoscleromorpha recorded in the Adriatic up to now: we performed a thor-ough literature check and we added the results of our decade long research with a special emphasis on sponge fauna inmarine caves. All the records were assigned to the North, Middle or South Adriatic according to their geographic location,and the analysis showed a very high similarity among the sponge fauna of the 3 areas. The likeness between the N. andthe M. Adriatic is over 83 %, between the M. and the S. Adriatic over 76 % and between the N. and the S. Adriatic over66 %. Altogether 283 species of sponges from these two classes (our field data and literature survey) have been recordedin the whole Adriatic up to now, which is a considerably higher number than in previous reviews. Among the 125 speciesthat we found so far in our research along the Croatian coast, 77 were found in marine caves. We are still discovering spe-cies not previously found in the Adriatic Sea (especially from cryptic habitats) and here we report 15 new records for the Adriatic Sea, 9 of which were noted only in caves.
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Grubelić, Ivana, Boris Antolić, Marija Despalatović, Branka Grbec, and Gordana Beg Paklar. "Effect of climatic fluctuations on the distribution of warm-water coral Astroides calycularis in the Adriatic Sea: new records and review." Journal of the Marine Biological Association of the United Kingdom 84, no. 3 (May 24, 2004): 599–602. http://dx.doi.org/10.1017/s0025315404009609h.

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Three colonies of warm-water coral Astroides calycularis were found at the eastern part of the middle Adriatic Sea during the 1990–2001 period. For each specimen, depth distribution and habitat were recorded. Previous and recent knowledge of this species in the Adriatic Sea and in the Mediterranean Sea was discussed in relation to climatic changes. Occurrence of A. calycularis in the Adriatic Sea was related to the increased temperatures of the surface marine layer. Variable temperature conditions were connected to the climatic changes on the hemispheric scale through the North Atlantic Oscillation index. The prevailing sea current system together with the coastal configuration and bottom type favours the presence of the studied warm-water coral on the eastern Adriatic coast.
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18

Pauluzzo, Rubens. "Foreign Market Entry Strategies in the North-Adriatic Area." International Journal of Information Systems and Social Change 4, no. 1 (January 2013): 1–20. http://dx.doi.org/10.4018/jissc.2013010101.

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The consolidation of economic and political relations in the North-Adriatic area and their formalization encouraged by the new institutional structures of Euro-regions are phenomena of central relevance to the actual European economic environment. These conditions have a significant influence on the strategic choices of local firms. In spite of the geographical proximity between Italy, Austria, Slovenia, and Croatia, cultural differences still act as important determinants in leading foreign investment strategies. The current study aims at analyzing the role played by cultural distance between the examined countries in affecting entry mode strategies followed by companies of the Italian region of Friuli-Venezia Giulia. In particular, the analysis suggests that a larger cultural distance, together with specific market characteristics, may force companies to choose entry forms with a lower degree of control, while specific firm characteristics may have an opposite impact on the internationalization strategies.
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19

Rubino, Fernando, Genuario Belmonte, Anna M. Miglietta, Sebastiano Geraci, and Ferdinando Boero. "Resting Stages of Plankton in Recent North Adriatic Sediments." Marine Ecology 21, no. 3-4 (December 2000): 263–84. http://dx.doi.org/10.1046/j.1439-0485.2000.00725.x.

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20

Brezigar, Bojan. "Post-Communist Linguistic Problems in the North Adriatic Area*." Nationalities Papers 27, no. 1 (March 1999): 93–101. http://dx.doi.org/10.1080/009059999109208.

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The population of the North Adriatic area has always been linguistically mixed. Slovene, Croatian and Italian populations have lived here for 14 centuries; German people moved here in the period of the Austro-Hungarian Empire. In the eighteenth and nineteenth centuries the city of Trieste became the official harbor of the Empire, and, as a consequence, the town grew, attracting others immigrants: Greeks, Jews, Serbs, and so on. Linguistically three main groups lived in Trieste: German, Italian and Slovene speakers. The Slovenes in Trieste owned many important activities, such as banks and trading companies. They were organized in the fields of education and culture with their own theater, private schools, library, daily newspaper and magazines. The Slovenes in Trieste also had their own political movement electing some representatives to the Parliament in Vienna. On the whole, they were considered a very well organized linguistic group. The Italians in Trieste were similarly well organized, and many supported a strong irredentist movement, economical and political organizations, as well as the theater. The German speakers were mostly immigrants who had moved to Trieste for business reasons or as civil servants.
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21

Munda, Ivka M. "Resources and possibilities for exploitation of North Adriatic seaweeds." Hydrobiologia 204-205, no. 1 (September 1990): 309–15. http://dx.doi.org/10.1007/bf00040250.

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22

BASTIANINI, M., C. TOTTI, A. PENNA, A. DE LAZZARI, and M. MONTRESOR. "Dinoflagellate cysts production in the north-western Adriatic Sea." Mediterranean Marine Science 17, no. 3 (November 16, 2016): 751. http://dx.doi.org/10.12681/mms.1770.

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A sediment trap study was conducted in the Gulf of Venice, north-western Adriatic Sea, from April to December 2005 to assess relationships between planktonic dinoflagellates and cyst production. Every month, CTD profiles and discrete samplings for phytoplankton, nutrients and particulate matter were conducted. Cyst fluxes spanned from 90 to 127,600 cysts m-2 d-1 and major peaks were due to a small cyst attributed to cf. Biecheleria and to calcareous cysts of Scrippsiella trochoidea. A good correspondence between cyst fluxes in sediment traps and the presence of the corresponding vegetative cells in the water column was detected for Lingulodinium polyedrum, and species of the genera Spiniferites,Gonyaulax and Protoperidinium. A PCR method applied to surface sediment samples allowed the identification of a number of potentially harmful dinoflagellate cysts (Alexandrium minutum, A. tamutum, A. taylorii, Lingulodinium polyedrum and Protoceratium reticulatum).
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Prtenjak, Maja Telišman, Branko Grisogono, and Theodoros Nitis. "Shallow mesoscale flows at the north-eastern Adriatic coast." Quarterly Journal of the Royal Meteorological Society 132, no. 620 (October 1, 2006): 2191–215. http://dx.doi.org/10.1256/qj.05.41.

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24

Dulĉić, J., and A. Pallaoro. "First record of the marbled spinefoot Siganus rivulatus (Pisces: Siganidae) in the Adriatic Sea." Journal of the Marine Biological Association of the United Kingdom 84, no. 5 (October 2004): 1087–88. http://dx.doi.org/10.1017/s0025315404010483h.

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Lessepsian migrant Siganus rivulatus is reported for the first time from the Adriatic Sea, substantially further north than its usual area of occurrence in the Mediterranean Sea. Two specimens (111 mm total length [TL] and 149 mm TL) were captured by beach seine on 5 October 2002 off islet Bobara, near Cavtat (southern Adriatic). Morphometric and meristic characteristics of the specimens are provided. The possible explanations of this occurrence are discussed.
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Bravničar, Jernej, Anja Palandačić, Simona Sušnik Bajec, and Aleš Snoj. "Neotype designation for Thymallus aeliani Valenciennes, 1848 from a museum topotype specimen and its affiliation with Adriatic grayling on the basis of mitochondrial DNA." ZooKeys 999 (November 30, 2020): 165–78. http://dx.doi.org/10.3897/zookeys.999.56636.

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In 1848, the grayling Thymallus aeliani (Valenciennes) was described from Lake Maggiore, Italy, in the north Adriatic basin. Genetic analyses of the mitochondrial control region showed a unique evolutionary history of grayling inhabiting the rivers of northern Adriatic basin, from the upper reaches of the Po River and its left tributaries in the west to the Soča River in the east, which resulted in the designation of this phylogenetic lineage as Adriatic grayling. Consequently, the name T. aeliani was connected to the Adriatic lineage, re-establishing the validity of this taxon. However, the mitochondrial haplotypes belonging to Adriatic grayling were never compared with the type specimens of T. aeliani, as their whereabouts were unknown. In this study, a neotype for T. aeliani was designated using topotypical specimens stored at the Natural History Museum in Vienna. The neotype (NMW 68027:2 labelled as “Lago Maggiore, Bellotti, 1880”) was designated pursuant to the conditions stipulated in Article 75.3 of the International Code of Zoological Nomenclature. Furthermore, the mitochondrial control region of the neotype was compared to haplotypes of the Adriatic lineage and showed high genetic similarity, which therefore connects the species name T. aeliani to the Adriatic grayling. This crucial step in fixing nomenclatural status of this species is very important for its protection and management.
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Lipizer, M., E. Partescano, A. Rabitti, A. Giorgetti, and A. Crise. "Qualified temperature, salinity and dissolved oxygen climatologies in a changing Adriatic Sea." Ocean Science Discussions 11, no. 1 (February 3, 2014): 331–90. http://dx.doi.org/10.5194/osd-11-331-2014.

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Abstract. An updated climatology, based on a comprehensive dataset (1911–2009) of temperature, salinity and dissolved oxygen, has been produced for the whole Adriatic Sea with the Variational Inverse Method using the DIVA software. Climatological maps were produced at 26 levels and validated with Ordinary Cross Validation and with real vs. synthetic Temperature–Salinity diagram intercomparison. The concept of Climatology–Observation Misfit (COM) has been introduced as an estimate of the physical variability associated with the climatological structures. In order to verify the temporal stability of the climatology, long-term variability has been investigated in the Mid Adriatic and the South Adriatic Pits, regarded as the most suitable records of possible long-term changes. Compared with previous climatologies, this study reveals a surface temperature rise (up to 2 °C), a clear deep dissolved oxygen minimum in the South Adriatic Gyre and a bottom summer oxygen minimum in the North Adriatic. Below 100 m all properties profoundly differ between the Middle and the South Adriatic. The South Adriatic Pit clearly shows the remote effects of the Eastern Mediterranean Transient, while no effect is observed in Middle Adriatic Pits. The deepest part of the South Adriatic seems now to be significantly saltier (+0.18 since the period 1911–1914, with an increase of +0.018 decade−1 since the late 1940s) and warmer (+0.54 °C since 1911–1914), even though a long-term temperature trend could not be statistically demonstrated. Conversely, the Middle Adriatic Pits present a long-term increase in apparent oxygen utilisation (+0.77 mL L−1 since 1911–1914, with a constant increase of +0.2 mL L−1 decade−1 after the 1970s).
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Mikac, Barbara, Margherita Licciano, Andrej Jaklin, Ljiljana Iveša, Adriana Giangrande, and Luigi Musco. "Diversity and Distribution Patterns of Hard Bottom Polychaete Assemblages in the North Adriatic Sea (Mediterranean)." Diversity 12, no. 10 (October 21, 2020): 408. http://dx.doi.org/10.3390/d12100408.

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The knowledge on the hard bottom polychaete assemblages in the Northern Adriatic Sea, a Mediterranean region strongly affected by environmental pressures, is scarce and outdated. The objective of this paper was to update the information on polychaete diversity and depict their patterns of natural spatial variation, in relation to changes in algal coverage at increasing depth. Hard bottom benthos was quantitatively sampled by scraping off the substrate from three stations at Sveti Ivan Island (North Adriatic) at three depths (1.5 m, 5 m and 25 m). Polychaete fauna comprised 107 taxa (the majority of them identified at species level) belonging to 22 families, with the family Syllidae ranking first in terms of number of species, followed by Sabellidae, Nereididae, Eunicidae and Serpulidae. Considering the number of polychaete species and their identity, the present data differed considerably from previous studies carried out in the area. Two alien species, Lepidonotus tenuisetosus, which represented a new record for the Adriatic Sea, and Nereis persica, were recorded. The highest mean abundance, species diversity and internal structural similarity of polychaete assemblages were found at 5 m depth, characterised by complex and heterogeneous algal habitat. The DISTLM forward analysis revealed that the distribution of several algal taxa as well as some algal functional-morphological groups significantly explained the observed distribution patterns of abundance and diversity of polychaete assemblages. The diversity of the North Adriatic hard bottom polychaete fauna is largely underestimated and needs regular updating in order to detect and monitor changes of benthic communities in the area.
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Shabrang, L., M. Menna, C. Pizzi, H. Lavigne, G. Civitarese, and M. Gačić. "Long-term variability of the South Adriatic circulation and phytoplankton biomass in relation to large-scale climatic pattern." Ocean Science Discussions 12, no. 1 (February 10, 2015): 203–26. http://dx.doi.org/10.5194/osd-12-203-2015.

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Abstract. The interannual variability of the South Adriatic Gyre and its relation to the wind vorticity and the large-scale climatic pattern (North Atlantic Oscillation – NAO), was studied using the time-series of satellite altimetry data and ocean surface wind products. The cyclonic circulation observed in the South Adriatic area was mainly sustained by the local wind forcing, as suggested by the positive correlation between the rate of change of the current vorticity and the wind-stress vorticity. Nevertheless, the influence of vorticity advection from the adjacent area (North Ionian Sea) cannot be ignored and it is more significant during the anticyclonic phase of Adriatic–Ionian Bimodal Oscillation System. The geostrophic current vorticities of the South Adriatic and North Ionian Seas are correlated with a time lag of 15 months, which corresponds to an advection speed of ~1 cm s−1. The different wind patterns observed during the two NAO phases revealed a stronger positive vorticity during the negative NAO phase. Conversely, during the positive NAO phase the wind vorticity is characterized by lower positive values. Subsequently, the calculated positive linear correlation between the NAO index and the frequency of the cold and dry northerly wind suggests the strengthening of the winter convection, and of the consecutive deep water formation, during the positive NAO phases. As a consequence of the winter deep convection, Southern Adriatic area is characterized by the late winter/early spring algal blooms. Relationship between the spatially averaged surface chlorophyll concentrations and the northerly wind frequencies revealed that the two biological productivity regimes likely exist: the subtropical one and the subpolar one depending on the frequency of windy days. We also showed that the bloom timing is a linear function of the wind frequency and can vary within the range of almost two months. This study thus contributes to our understanding of the possible impact of climate change on the SAG circulation and its ecosystem.
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29

Andreoli, C., C. Tolmomio, L. Tognetto, I. Moro, L. Scarabel, and I. Masiero. "Phytoplankton and chemico-physical composition of the Caleri Lagoon (North Adriatic Sea) during 1991." Algological Studies/Archiv für Hydrobiologie, Supplement Volumes 85 (June 6, 1997): 95–117. http://dx.doi.org/10.1127/algol_stud/85/1997/95.

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30

Civitarese, G., M. Gačić, M. Lipizer, and G. L. Eusebi Borzelli. "On the impact of the Bimodal Oscillating System (BiOS) on the biogeochemistry and biology of the Adriatic and Ionian Seas (Eastern Mediterranean)." Biogeosciences 7, no. 12 (December 15, 2010): 3987–97. http://dx.doi.org/10.5194/bg-7-3987-2010.

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Abstract. Analysis of 20-year time-series of the vertically averaged salinity and nutrient data in the Southern Adriatic shows that the two parameters are subject to strong decadal variability. In addition, it is documented that nutrient and salinity variations are out of phase. Nutrients in the Ionian and in the Adriatic vary in parallel except that generally the nutrient content in the Adriatic is lower than in the Ionian, a fact that has been attributed to primary producer consumption following the winter convective mixing. As shown earlier, North Ionian Gyre (NIG) changes its circulation sense on a decadal scale due to the Bimodal Oscillating System, i.e. the feedback mechanism between the Adriatic and Ionian. Cyclonic circulation causes a downwelling of the nitracline along the borders of the NIG and a decrease in the nutrient content of the water flowing into the Adriatic across the Otranto Strait, and vice versa. In addition, the highly oligotrophic central area of the Ionian shows annual blooms only during cyclonic NIG circulation. Inversion of the sense of the NIG results in the advection of Modified Atlantic Water or of the Levantine/Eastern Mediterranean waters in the Adriatic. Here, we show that the presence of allochtonous organisms from Atlantic/Western Mediterranean and Eastern Mediterranean/temperate zone in the Adriatic are concurrent with the anticyclonic and cyclonic circulations of the NIG, respectively. On the basis of the results presented, a revision of the theory of Adriatic ingressions formulated in the early 1950s is proposed.
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31

Ivanić, Katarina, and Mirano Hess. "Assessment of Effi ciency of the North Adriatic Container Terminals." Naše more 66, no. 3 (September 2019): 97–102. http://dx.doi.org/10.17818/nm/2019/3.1.

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32

Pasarić, Miroslava, and Mirko Orlić. "Long-term meteorological preconditioning of the North Adriatic coastal floods." Continental Shelf Research 21, no. 3 (February 2001): 263–78. http://dx.doi.org/10.1016/s0278-4343(00)00078-9.

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33

NESPOLI, GIOVANNI. "Eutrophication of the Coastal Waters of the North Adriatic Sea." Annals of the New York Academy of Sciences 534, no. 1 Living in a C (June 1988): 946–49. http://dx.doi.org/10.1111/j.1749-6632.1988.tb30186.x.

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34

Button, Kenneth, and Tomaž Kramberger. "European Union expansion and seaport efficiency in the North Adriatic." Applied Economics Letters 22, no. 9 (October 28, 2014): 700–703. http://dx.doi.org/10.1080/13504851.2014.969822.

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35

Kourafalou, Vassiliki H. "Process studies on the Po River plume, North Adriatic Sea." Journal of Geophysical Research: Oceans 104, no. C12 (December 15, 1999): 29963–85. http://dx.doi.org/10.1029/1999jc900217.

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36

Zavodnik, D. "A North Adriatic centenarian: The marine research station at Rovinj." Helgoländer Meeresuntersuchungen 49, no. 1-4 (March 1995): 441–53. http://dx.doi.org/10.1007/bf02368371.

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37

Curiel, Daniele, Sandra Kraljević Pavelić, Agata Kovačev, Chiara Miotti, and Andrea Rismondo. "Marine Seagrasses Transplantation in Confined and Coastal Adriatic Environments: Methods and Results." Water 13, no. 16 (August 21, 2021): 2289. http://dx.doi.org/10.3390/w13162289.

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The anthropogenic pressures of the twentieth century have seriously endangered the Mediterranean coastal zone; as a consequence, marine seagrass habitats have strongly retreated, mostly those of Posidonia oceanica. For this reason, over time, restoration programs have been put in place through transplantation activities, with different success. These actions have also been conducted with other Mediterranean marine seagrasses. The results of numerous transplanting operations conducted in the Northern Adriatic Sea and lagoons with Cymodocea nodosa, Zostera marina and Z. noltei and in the Central and Southern Adriatic Sea with P. oceanica (only within the project Interreg SASPAS), are herein presented and compared, taking also into account the presence of extensive meadows of C. nodosa, Z. marina and Z. noltei, along the North Adriatic coasts and lagoons.
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38

Pigniczki, Csaba, Jelena Kralj, Stefano Volponi, Antun Žuljević, Mohamed-Ali Dakhli, Tibor Mikuska, Hichem Azafzaf, and Zsolt Végvári. "Migration routes and stopover sites of the Eurasian Spoonbill (Platalea leucorodia) between the Carpathian Basin and wintering areas." Ornis Hungarica 24, no. 1 (June 1, 2016): 128–49. http://dx.doi.org/10.1515/orhu-2016-0008.

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Abstract Understanding the migration routes of the Central European Spoonbill population is important for their conservation. Here we analysed movements of 3186 individuals of Eurasian Spoonbills marked with colour rings in the Carpathian Basin (Hungary, Croatia and Serbia) between 2003 and 2015, and a satellite tagged individual, which was equipped in Italy in 2013, and later moved to the Carpathian Basin. Migration routes of these Spoonbills predominantly followed the Adriatic Flyway, however, some birds were also found to both east and west from this flyway. We identified 59 stopover sites, 55 of which were located along the Adriatic Flyway. Colourringed juveniles (1cy), on average, spent 4.0±0.9 (SE) days on the stopover sites along the Adriatic Flyway during autumn migration, while non-juveniles (> 1cy) spent 2.6±1.0 (SE) days during autumn and 2.1±0.4 (SE) days during spring migration there. These durations were not significantly different. Duration of stops of the satellite tracked individual was between 7 and 15 days during autumn and between 1 and 12 days during spring migration. Our results indicate the existence of two alternative routes of the Adriatic Flyway between the Carpathian Basin and the wintering areas in southern Italy and the central part of coastal North-Africa. The North-Adriatic Flyway includes stopover sites in north-eastern Italy at the river mouth of River Isonzo, Lagunes of Venice and wetlands around River Po. The South Adriatic Flyway leads through the Balkan Peninsula, with stopover sites at the karst lakes of Bosnia and Herzegovina, mouth of the river Neretva (Croatia), Ulcinj Salinas (Montenegro) and wetlands in Gulf of Manfredonia (Italy). This hypothesis was also supported by the migration of the satellite tagged individual, the paths of which was described here in detail. The average coordinates of spring and autumn stopover sites were located at different parts of the flyway: it was in south-western Italy during autumn migration, while it was close to the western coast of the Balkan Peninsula during spring migration. We found examples for Spoonbills using the same migration paths along the same route year by year on both spring and autumn migration, but also noticed shifts between routes. Some observations indicate that individuals may show site fidelity to stopover sites between years, although the sample size was low for statistical significance.
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39

Zubak, Ivana, Hrvoje Cizmek, and Melita Mokos. "Posidonia oceanica lower depth limits along a latitudinal gradient in the eastern Adriatic Sea." Botanica Marina 63, no. 3 (June 25, 2020): 209–14. http://dx.doi.org/10.1515/bot-2019-0097.

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AbstractAlthough extensive studies have been made on Posidonia oceanica ecosystems, in terms of their phenological characteristics, shoot density, biomass, and associated faunal assemblages, little attention has been given to the depth distribution of this species in the Adriatic Sea. The depth limits of the Mediterranean endemic seagrass P. oceanica growing along the eastern coast of the Croatian Adriatic Sea were examined by the use of SCUBA diving. Fifty-two independent measurements show that the lower depth limit of P. oceanica in the Croatian Adriatic Sea ranges from 24 m in the north to 36 m in the south, with a strong latitudinal gradient. The information on maximum depth distribution is an important asset when the increased human pressure and rapid environmental changes pose a threat to the survival of this slow-growing marine species.
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40

Hodges, Richard. "Adriatic Sea trade in a European perspective." Scottish Archaeological Journal 32, no. 2 (October 2010): 95–119. http://dx.doi.org/10.3366/saj.2010.0012.

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This article is a summary of the Dalrymple Lectures given in 2009. It reviews the archaeology of north-west European economics, and then contrasts this with the new evidence for 7th- to 9th-century long-distance commerce in the Adriatic Sea region and its implications for the changing economic circumstances in peninsula Italy. The essay attempts to take a new stance on my book Dark Age Economics (1982) and, using new archaeological evidence, offers new interpretations of the rise of the Carolingian economy as well as the limited capacity of the western Middle Byzantine economy.
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41

Jašič, Dražen, Zlatimir Bićanić, and Josip Kasum. "Srednjojadranski prag – važnija istraživanja i metodologija obrade podataka." Geoadria 10, no. 2 (January 11, 2017): 127. http://dx.doi.org/10.15291/geoadria.85.

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A methodological approach in the analyses of the seawater oceanographic states is determined by the purpose of the paper and general purpose of the research. In the recent decades the scientific work in this area has advanced thanks to computer data processing, particularly owing to modern technical and technological achievements that allow us to obtain important results, which significantly augment application of scientific results. This paper is a review of the research on the Central Adriatic shelf. Until now, papers dealing with geographical and oceanographic features regularly used the terms Palagruža Shelf and Jabuka concavity in the meaning of independent entities in the Adriatic basin which partly define physicogeographic features of water masses. However, such perception should be corrected. The Central Adriatic shelf is situated between the north Adriatic and the south Adriatic basin. Its length is greater than the width. Therefore, it deserves more attention and more cautious scientific approach. In this paper there are also evaluations of some methodologies used in the research and in the measuring of oceanographic parameter values, and also new technical solutions are proposed. The purpose of this paper is to analyse some methods of approach in the presentation of oceanographic states of seawater in the area of the Central Adriatic shelf. The purpose is also to introduce a succession of articles in which this maritime zone should be given its deserving significance from the geographic and oceanological aspects.
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42

Candelma, Michela, Luca Marisaldi, Daniela Bertotto, Giuseppe Radaelli, Giorgia Gioacchini, Alberto Santojanni, Sabrina Colella, and Oliana Carnevali. "Aspects of Reproductive Biology of the European Hake (Merluccius merluccius) in the Northern and Central Adriatic Sea (GSA 17-Central Mediterranean Sea)." Journal of Marine Science and Engineering 9, no. 4 (April 7, 2021): 389. http://dx.doi.org/10.3390/jmse9040389.

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The study focused on the macroscopic, histological, and biometric analysis of European hake females in GSA 17 (Central-North Adriatic Sea). From 2013 to 2015, 976 females were collected and analyzed monthly. Though females in spawning conditions were found during the whole year, the trend of GSI showed a peak of the reproductive season from April to July in 2014 and 2015. HSI and Kn reached the highest values in September, after the spawning peaks. In 2013, the trend of these indices did not highlight an evident peak, probably due to an adverse event that occurred in the previous winter in the Adriatic shelf. The length at first maturity (L50) was estimated by macroscopic and histological approaches, resulting in 30.81 cm for the macroscopical length and 33.73 cm for the histological length; both values are higher than the current catching legal size. For the first time in this area, batch and relative fecundity were estimated. Relative fecundity was similar to the Mediterranean and the Atlantic stocks, whereas batch fecundity values were lower compared to other fishing grounds. Overall, the analysis of reproductive parameters plays a fundamental role in the sustainable management of this resource in an area as overfished as the Central-North Adriatic Sea.
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43

Cantoni, Carolina, Anna Luchetta, Massimo Celio, Stefano Cozzi, Fabio Raicich, and Giulio Catalano. "Carbonate system variability in the Gulf of Trieste (North Adriatic Sea)." Estuarine, Coastal and Shelf Science 115 (December 2012): 51–62. http://dx.doi.org/10.1016/j.ecss.2012.07.006.

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44

Vilibić, I. "An analysis of dense water production on the North Adriatic shelf." Estuarine, Coastal and Shelf Science 56, no. 3-4 (March 2003): 697–707. http://dx.doi.org/10.1016/s0272-7714(02)00277-9.

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45

Gašparović, B., and B. Ćosović. "Surface-active properties of organic matter in the North Adriatic Sea." Estuarine, Coastal and Shelf Science 58, no. 3 (November 2003): 555–66. http://dx.doi.org/10.1016/s0272-7714(03)00133-1.

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46

Affronte, Marco, and Dino Scaravelli. "Analysis of stranded sea turtles in the north-western Adriatic Sea." Zoology in the Middle East 24, no. 1 (January 2001): 101–8. http://dx.doi.org/10.1080/09397140.2001.10637888.

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47

Camuffo, Monica, Stefano Soriani, and Gabriele Zanetto. "The evolution of marine protected areas (MPAs): the North Adriatic case." Management of Environmental Quality: An International Journal 22, no. 1 (January 4, 2011): 59–71. http://dx.doi.org/10.1108/14777831111098480.

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48

Christian, Erhard. "Biogeography, Substrate Preference, and Feeding Types of North Adriatic Intertidal Collembola." Marine Ecology 10, no. 1 (March 1989): 79–93. http://dx.doi.org/10.1111/j.1439-0485.1989.tb00066.x.

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49

Cozzi, Stefano, Marina Lipizer, Carolina Cantoni, and Giulio Catalano. "Nutrient balance in the ecosystem of the North Western Adriatic Sea." Chemistry and Ecology 18, no. 1-2 (January 2002): 1–12. http://dx.doi.org/10.1080/02757540212685.

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50

Giani, M., D. Berto, F. Rampazzo, F. Savelli, F. Alvisi, P. Giordano, M. Ravaioli, and F. Frascari. "Origin of sedimentary organic matter in the north-western Adriatic Sea." Estuarine, Coastal and Shelf Science 84, no. 4 (October 2009): 573–83. http://dx.doi.org/10.1016/j.ecss.2009.07.031.

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