515N of particulate organic matter and Anemonia sulcata as a tracer of sewage effluent transport in the marine coastal ecosystem of Pirovac Bay and the Murter Sea (Central Adriatic) 515N v partikulatni organski snovi in Anemoni sulcati kot sledilo transporta odpadnih voda v priobalnem delu Pirovaškega zaliva in Murterskega morja (srednji Jadran) Tadej Dolenec1-2*, Sonja Lojen2, Goran Kniewald3, Matej Dolenec1 and Nastja Rogan1 'Faculty of Natural Sciences and Engineering, University of Ljubljana, Department of Geology, Aškerčeva 12, 1000 Ljubljana, Slovenia; E-mail: tadej.dolenec@ntfgeo.uni-lj.si 2Jožef Stefan Institute, Jamova 39, 1000 Ljubljana, Slovenia; E-mail: sonja.lojen@ijs.si 3Ruder Boškovic Institute, Bijenička 54, Zagreb, Croatia; E-mail: kniewald@irb.hr Received: January 6, 2006 Accepted: July 20, 2006 Abstract: The present study shows that the stable isotopic composition of nitrogen in particulate organic matter (POM) and in selected marine organisms, such as the sea anemone Anemonia sulcata, may be excellent parameters for detecting and monitoring human sewage inputs into the marine coastal ecosystems of Pirovac Bay and the Murter Sea. The SI5N values of POM and A. sulcata tissue were significantly higher at sites in the semi-enclosed Pirovac Bay and in the coastal part of the Murter Sea (Central Adriatic) affected by sewage, compared to the off-shore reef flats of the Murter Sea, the coastal parts of the Kornati Islands and at a pristine reference location at the Lumbarda Reef Flat. ISN enrichment was as high as 7.0 %o in POM and 7.7 %o in A. sulcata tissue and is significantly larger than the natural SI5N variability of the same species at unaffected locations. Geochemical maps of SI5N values were created, which could be useful in monitoring the influence of human sewage impacts in marine coastal ecosystems. Maps of sewage nitrogen distribution could also be used for planning municipal and industrial waste management in the region and to assist in monitoring the efficiency of environmental protection measures after the construction of a new wastewater treatment plant in Murter. Izvleček: Rezultati pričujoče raziskave kažejo, da je izotopska sestava dušika v partikulatni organski snovi (POM) in v nekaterih morskih organizmih, kot je naprimer anemona Anemonia sulcata odličen parameter za sledenje in monitoring komunalnih in drugih odplak v morskih priobalnih ekosistemih Pirovaškega zaliva in Murterskega morja (srednji Jadran). Vrednosti 8I5N v partikulatni organski snovi in v tkivu A. sulcate na območju Pirovaškega zaliva in v priobalju Murterskega morja, ki sta onesnažena predvsem z odplakami iz septičnih sistemov so bistveno večje v primerjavi z referenčno neonesnaženo lokacijo - plitvino Lumbarda na odprtem delu Kornatskega arhipelaga. Partikulatna organska snov iz onesnaženih območij vsebuje za 7,0 %o, tkiva A. sulcate pa za 7,7 %o večji 8I5N v primerjavi s POM in tkivom anemon iz referenčne, neonesnažene lokacije. Omenjena obogatitev je znatno večja v primerjavi z variabilnostjo 8I5N v primerkih iste vrste na neonesnaženih lokacijah. Na podlagi dobljenih podatkov so bile napravljene tudi geokemične karte porazdelitve parametra 8I5N, ki so uporabne za monitoring vpliva odpadnih voda iz septičnih sistemov na priobalne ekosisteme na tem območju. Omenjene geokemične karte bodo koristile tudi pri načrtovanju izpusta nove čistilne naprave na otoku Murter in v kasnejši fazi tudi za ugotavljanje njene efikastnosti, glede na zmanjšanje onesnaženja obalnih ekosistemov na tem območju z odpadnimi vodami. Key words: sewage, pollution monitoring, nitrogen, stable isotope, particulate organic matter, Anemonia sulcata, Pirovac Bay, Murter Sea- Central Adriatic Ključne besede: odpadne vode, monitoring onesnaženosti, dušik, stabilni izotop, partikulatna organska snov, Anemonia sulcata, Pirovaški zaliv, Murtersko morje, srednji Jadran *Corresponding author. Tel.: +00386-1-4704-620; e-mail address: tadej.dolenec@ntfgeo.uni-lj.si Introduction Increased nitrogen loading in particulate organic matter (POM) and sediments is commonly related to the eutrophication of coastal seas worldwide. A significant component of marine eutrophication in many near-shore environments can be attributed to inputs of anthropogenic nitrogen from untreated domestic sewage and municipal and industrial effluents (Lee and Olsen, 1985; Nixon et al., 1986; Bachtiar et al., 1996; Costanzo et al., 2001). Managing the effects of sewage entering marine ecosystems has become one of the major environmental challenges of today. Septic systems for household waste disposal and the tourist infrastructure (hotels, camps, marinas) are the predominant point sources of contaminants in the semi-enclosed Pirovac Bay and in the coastal part of the Murter Sea, Dalmatia. The expansion of the human population during the tourist season not serviced by an adequate municipal infrastructure represents an additional impact of human sewage on the marine coastal ecosystems of Murter Island, creating an increasing demand for on-site sewage treatment system on Murter Island. The results presented are a part of a comprehensive study employing different tools such as geochemistry, hydrology, microbiology, etc., to investigate the impact of sewage effluents and their possible transport pattern in the investigated area of Pirovac Bay and the Murter Sea. The distribution of sewage effluents in marine ecosystems can be mapped using various parameters, such as salinity, nutrient concentrations, bacteria, organic matter composition, radioisotopic tracers, dye fluorescence, water current measurements and nitrogen isotope composition in water and sediments (Sweeney et al., 1980; Lindau et al., 1989; Smith-Evans and D awes, 1996). The nitrogen stable isotopic composition of marine plants (Costanzo et al., 2001; Dolenec et al., 2005) and higher organisms (Moore et al., 1996; Hansson et al., 1997; Tucker et al., 1999; Costanzo et al., 2001) or POM (Heikoop et al., 2000) has also been used as a tracer of anthropogenic pollution. Here we present an approach that shows the extent and fate of bio-available sewage nitrogen in coastal marine ecosystems, also enabling identification of the location of the pollution source. It is based on the assumption that (1) the nitrogen isotope composition (ô15N) of POM (representing a mixture of phytoplankton, bacteria, microzooplankton and detritus) is affected by sewage-derived nitrogen enriched in 15N, and (2) tissues of organisms of the same species or groups of organisms with a similar position in the food web, in our case A. sulcata individuals, reflect the ô15N of their N source (Wada et al., 1991). Stable nitrogen isotopes have been widely used to trace dissolved and particulate nutrients derived from animal wastes, septic systems and waste water treatment plants, as they physically and biologically move through ecosystems (Risk and Erdmann, 2000; Heikoop et al., 2000). Benthic and benthic feeding animals, as well as other organisms from sewage-impacted areas have shown ô15N values distinct from those collected at unaffected reference sites (Van Dover et al., 1992; Spies et al., 1989; Moore et al., 1996; Hansson et al., 1997; Tucker et al., 1999; Costanzo et al., 2001). Stable isotopes of nitrogen can thus be used to distinguish between natural and anthropogenic nitrogen sources in the environment or ecosystems (Mariotti et al., 1984; Tucker et al., 1999; Sigleo and Macko, 2002). For illustration, ô15N values of nitrate of commercial fertiliser typically range from - 2.5 to + 2.0 %o, organic soil nitrate ranges from - 2 to + 9 %, and human and animal wastes range from + 10 to + 22 % (Kreitler and Jones, 1975; Kreitler and Browning, 1983; Heaton, 1986; Barrett et al., 1999). Generally, ô15N values of NOQ > + 10 % are regarded as being indicative of the presence of faecal N (Barrett et al., 1999). Treated sewage shows ô15N values around + 10 % (Heaton, 1986). Marine POM in pristine oligotrophic environments exhibits ô15N values distinctly lower than that collected in areas impacted by fin-fish aquaculture (Sara et al., 2004). Increased ô15N values of about + 8 % were measured in POM near the inflows from septic systems in the port of Murter (Dolenec et al., 2005); similar values were reported for POM dominated by untreated faecal matter of Jepara Bay (+ 7.9 %, Heikoop et al., 2000). Stable nitrogen isotopes are also useful in tracing organic matter through food webs. Animals raised on diets with a known nitrogen composition preferentially incorporated 15N rather than 1RN, producing proteins enriched in 15N relative to the food (Minagawa and Wada, 1984; DeNiro and Epstein, 1981). In the trophic network among animals, ô15N values of their tissues systematically increase by 1.3 to 5.3% per trophic level (Minagawa and Wada 1984; Wada et al. 1991, 1993; Lajtha and Michener 1994). This study was designed with the following aims: 1) to test the hypothesis that the 15N content of POM and A. sulcata tissue collected near-shore and off-shore along the coastal part of the semi-enclosed Pirovac Bay and Murter Sea (Central Adriatic) is a reliable indicator of anthropogenic nitrogen impact arising from mostly untreated domestic and industrial wastes discharged into the coastal marine environment; 2) to create maps of 515N values, which would enable determination of the geographical extent of anthropogenic impact on the adjacent area of the Murter Sea arising from transport by currents. Materials and methods POM considered as a potential food source for A. sulcata was sampled at Im depth at 57 localities of the Murter Sea and semi-enclosed Pirovac Bay in August 2005 (Fig. I). 5 l samples were filtered through glass fibre filters (GF/F, Whatman). Individuals of A. sulcata were collected by scuba diving from the sea at depths of approximately 2 - 5 m at 31 localities in the same area (Fig. 2). All sampled individuals were size-matched (basal diameter 3 - 4 cm; tentacles extending 10 - 15 cm) and weighed (fresh weight: 40 - 50 g, dry weight after freeze-drying 8 - 10 g) to avoid possible isotope effects caused by ontogenetic dietary Figure I. Map of the study area in the Murter Sea and Pirovac Bay (Central Adriatic) showing sites of POM sampling Slika I. Geografska karta vzorčnih točk partikulatne organske snovi (POM) v Murterskem morju in Pirovaškem zalivu (srednji Jadran) shifts (DeNiro and Epstein, 1981; Muscatine and Kaplan, 1994) or age (Owens, 1987). Only pale green- coloured individuals with purple tentacle tips were chosen. To avoid the small seasonal differences in 515N values of anemone tissue observed during a preliminary study (Dolenec and Vokal, unpublished), we limited our analyses in this study to A. sulcata individuals collected during August 2002 (Dolenec et al., 2005). Fresh A. sulcata samples were placed in plastic bags and stored at - 20oC till further processing. Each sample was weighed prior to use in subsequent experiments. Samples of POM and A. sulcata were freeze-dried for >72 h and stored in a dessicator at room temperature. A. sulcata samples were crushed and homogenised by grinding in an agate mortar prior to analyses. Nitrogen isotope composition of all samples was measured using a Europa 20-20 mass spectrometer with an ANCA SL preparation module (PDZ Europa L td., U.K.).The results were expressed in the standard ô15N notation in permil (%o) relative to atmospheric nitrogen. The analytical precision (I standard deviation) of triplicate analyses of IAEA N-I and N-2 standards was better than ± 0.16 %. Precision (I standard deviation) of duplicate isotope analyses of samples was within ± 0.2 %. Figure 2. Map of the study area in the Murter Sea and Pirovac Bay (Central Adriatic) showing sites of Anemonia sulcata sampling Slika 2. Geografska karta vzorčnih točk Anemonie sulcate v Murterskem morju in Pirovaškem zalivu (srednji Jadran) Results The results of 515N determination in POM are listed in Table I, while Table 2 shows the nitrogen isotope composition of A. sulcata (whole single animal). 515N of POM ranged from + 2.7 to + 9.7 %o. Similar 515N values in the range from + 4.0 to + 11.9 % were measured in A.2sulcata. The regional distribution pattern of POM 815N values in August 2005 is shown on Pig. 3, while the regional distribution pattern of 815N values of Anemonia sulcata individuals collected in the year 2002 is presented in Pig. 4. Sample No. Sampling site 815N (%o) Sample No. Sampling site 815N (%o) 1 Reef Flat Lumbarda* 2.7 30 Podvrške - Bakarela 6.8 2 Sedlo Island 2.8 31 Podvrške - Port 4.9 3 Reef Flat Bacvica 3.0 32 Prišnjak V. Island 4.0 4 Samograd Island 3.6 33 Radelj Island 5.1 5 Reef Flat Kablinac 3.6 34 Prišnjak M. Island 4.3 6 Cavlin Island 3.8 35 Vrgada/Arta 4.6 7 Reef Flat Cavlin 3.5 36 Žavinac Island 4.6 8 Murter Sea I 3.8 37 Drage 4.6 9 Murter Sea II 4.2 38 Reef Flat Kušija 6.4 10 Kukuljari Island 4.0 39 Reef Flat Arta 5.1 11 Cap of Murter S 3.9 40 Pirovac Bay I 7.2 12 Tuzbina Island 4.4 41 Pirovac Bay II 8 13 Kosirina Bay I 4.5 42 Cap of Gradina 7.2 14 Kosirina Bay II 5.7 43 Port of Murter 5.9 15 Bikarijca (coast) 2.8 44 Hramina (Marina) 7.5 16 Reef Flat Kamenjar 3.0 45 Luke 8.5 17 Dinarici Islands 3.5 46 Luke / Vinici 7.3 18 Runjava Kotula - 47 Reef Flat Spličak 6.8 19 Spinata Island 4.5 48 Prosika (coast) 8.8 20 Obrovanj Island 4.6 49 Sustipanac Island 9.7 21 Reef Flat Kamicic 4.5 50 Port of Pirovac 6.2 22 Fish farms I 5.1 51 Makirina Bay 5.1 23 Fish farms II 4.5 52 Port of Jezera 6.3 24 Fish farms III 3.4 53 Tisno I 4.8 25 Fish farms IV 5.5 54 Tisno II 5.4 26 Visovac Island 4.5 55 Plitka Vala 5.4 27 Vrtlic Island 3.6 56 Port of Betina 5.0 28 Pod Raduc 4.8 57 Betina (Marina) 6.1 29 Slanica Bay 4.9 Table I. SI5N values of particulate organic matter (POM) collected in the Murter Sea and Pirovac Bay - Central Adriatic in August 2005 (* reference site) Tabela I. Vrednosti SI5N v partikulatni organski snovi (POM) v avgustu 2005 na območju Murterskega morja in Pirovaškega zaliva - srednji Jadran (* referenčna lokacija) Table 2. SI5N values of Anemonia sulcata individuals (whole animal; Dolenec et al., 2005) collected in the Murter Sea and Pirovac Bay - Central Adriatic in August 2002 (* reference site) Tabela 2. Vrednosti SI5N v Anemonii sulcati v avgustu 2002 (celotni primerek; Dolenec et al., 2005) na območju Murterskega morja in Pirovaškega zaliva - srednji Jadran (* referenčna lokacija) Sample No. Sampling site 815N (%o) Sample No. Sampling site 815N (%o) 1 Pirovac (coast) 11.9 17 Gira Island 6.1 2 Murter Island SE 6.4 18 Murvenjak Island 5.8 3 Kukuljari Islands 6.1 19 Vrtlic Island 5.4 4 Reef Flat Cavlin 5.8 20 Zavinac Island 7.3 5 Nozdra Island 5.0 21 Sestrice Islands 7.1 6 Reef Flat Puh 4.7 22 Arta V. Island 7.1 7 Reef Flat Lumbarda* 4.2 23 Prisnjak V. Island 6.3 8 Bikarijca (coast) 5.1 24 Prisnjak M. Island 7.8 9 Reef Flat Kamenjar 5.4 25 Arta M. Island 7.6 10 Dinarici Islands 5.6 26 Radelj Island 7.3 11 Gustac Island 5.1 27 Vinik Island 9.8 12 Reef Flat Galijolica 5.8 28 Cap of Gradina 9.5 13 Osljak Island 5.2 29 Reef Flat Splicak 10.1 14 R. Kotula Island 5.3 30 Prosika (coast) 10.8 15 Spinata Island 6.7 31 Sustipanac Island 11.8 16 Rakita Island 6.3 From Tables I and 2, as well as from Fig. 3 and 4, it is evident that: 1) The variations in 15N content of both POM and of A. sulcata appear to be influenced primarily by the environment in which they were collected. 2) 85N values of POM and A. sulcata tissue were significantly higher at the anthropogenically affected sites in the semi-enclosed Pirovac Bay, along the coast of the Murter Sea and the rocky shores of islands close to Murter Island, compared to POM and A. sulcata from an unaffected reference site on the shallow Lumbarda reef flat in the open sea (approx. 3 m deep) and those from small uninhabited offshore islands (Dolenec et al., 2005). 3) 815N values of POM showed significant differences between 15N depleted sampling sites (1-8, 15-17 and 27) from the reference location (Reef Flat of Lumbarda) as well as the relatively unaffected offshore part of the Murter Sea and the sampling sites (12-14 and 28-57) from Pirovac Bay and the coastal part of the Murter Island affected due to dissolved faecal organic matter. Samples of POM from the reference site (1) and offshore locations (2-8, 15-17 and 27) had 815N values in the range between + 2.7 and + 3.3 %o, while those dominated by untreated faecal matter (12-14 and 28-57) typically had values within the range from + 4.6 to + 9.7 %. The 815N values of POM collected in the area around the fish farms at the Vrgada Island (sampling sites 19-26) have been determined to vary from + 4.5 to 5.1 %o. A gradient towards lower 815N values was observed from the impacted sites around fish cages toward locations further away, as also observed in previous studies (Dolenec et al., 2005). 4) Anemonia sulcata individuals living on the offshore reef flats or on rocky shores of small isolated islands of the Murter Sea, as well as along the coastal part of the Kornati Islands and small uninhabited islands around the Island of Zut (sample sites 4 to 12) had consistently lower 815N values (average: + 5.2 %; range: + 4.2 to + 5.8 %) than individuals living on rocky surfaces of the coastal parts of the islands closer to the coast (sample sites 13 to 19). These lat- ter had 815N values with an average of + 5.8 %o, ranging from + 5.2 to + 6.7 %o (Table 2). Slightly enriched 815N values (up to 2.5 % relative to the reference site) in this region were found in anemones from small islands around fish farms (sample points 15, 16 and 17). Considerably higher d15N values (average + 6.9 %; range + 6.1 to + 7.8 %) were measured along the islands separating Pirovac Bay from the Murter Sea (sampling sites 21, 22, 24 and 25), as well as along the coastal part of Murter Island (sampling sites 2 and 23) and the Islands of Kukuljari (sampling site 3). However, the highest 815N values (+7.3 to +11.9 %, averaging +10.2 %o) were found in A. sulcata tissues from the inner part of Pirovac Bay (sampling sites 1 and 26-31), (Dolenec et al., 2005). Figure 3. Spatial distribution pattern of SI5N values of POM throughout the Murter Sea and Pirovac Bay (Central Adriatic) Slika 3. Prostorska porazdelitev vrednosti SI5N v partikulatni organske snovi (POM) v Murterskem morju in Pirovaškem zalivu (srednji Jadran) Figure 4. Spatial distribution pattern of SI5N values of Anemonia sulcata throughout Pirovac Bay and the Murter Sea - Central Adriatic (Dolenec et al., 2005) Slika 4. Prostorska porazdelitev vrednosti SI5N v Anemonii sulcati v Murterskem morju in Pirovaškem zalivu - srednji Jadran (Dolenec et al., 2005) Discussion The 15N enrichment of POM and anemones from the semi-enclosed Pirovac Bay, coastal parts of Murter Island, as well as from the inshore islands that separate Pirovac Bay from the Murter Sea, indicates that their primary food source is affected by heavy nitrogen due to local inputs of untreated sewage effluents into the coastal marine environment. Since sewage-derived wastewater DIN (dissolved inorganic nitrogen) is typically enriched in 15N and exhibits 515N values mostly in the range between + 10 and + 22 %o (Heaton, 1986), this source term may also be responsible for the 15N enrichment in phytoplankton. Such enrichment in 15N due to ground water DIN was found in both primary producers and consumers in estuarine settings of Cape Cod, Massachusetts (McClelland et al., 1997; McClelland and Valiela, 1998). 15N enrichment has also been found in reef molluscs, stomatopods, fishes and corals in settings exposed to anthropogenic nutrient pollution (Risk and Heikoop, 1997; Mendes et al., 1997, Heikoop et al., 2000; Risk and Erdman, 2000, Weiss et al., 2002). Zooplankton and reef particulate organic matter may have higher 515N values at sewage-polluted sites if 15N-enriched wastewater is utilised by phytoplankton at the base of the food chain (Hansson et al., 1997). Elevated 515N values have also been measured in marine plants exposed to ground water contaminated by septic systems (McClelland et al., 1997) and sewage effluents (Grice et al., 1996; Udy and Dennison, 1997; Costanzo et al., 2001). The spatial distributions of the sewage source indicators such as the 515N signal in POM and A. sulcata tissues allow us to draw conclusions on the impact pattern of sewage effluents and their transport in the coastal part of the Murter Island and Pirovac Bay. In line with the 515N values of A. sulcata, a similar spatial distribution of 515N was found also in other marine organisms such as Aplysina aerophoba, Balanus perforatus, Mytilus galloprovincialis, Area noae, Ostrea edulis and marine plants (Posidonia oceanica) from the same sampling sites collected during the years 2004 and 2005 (Dolenec et al., in preparation). A small difference in the sewage plumes delineated by 515N values of POM and A. sulcata was observed, but the overall trends are the same. POM shows the clearest plume resolution, extending up to several km from the major sources. This undoubtedly suggests that the isotope techniques used in this study are useful not only for showing the actual uptake and assimilation of sewage nutrients by marine organisms and plants, but also in tracing sewage effluent transport in the sampling area under consideration. From Figures 3 and 4 it is evident that the enrichment decreases with distance from the coast toward open sea ecosystems. Such onshore to offshore 51SN variations most probably indicate that the sewage-induced 1SN enrichment signal is rapidly attenuated with distance from the sewage sources (within some kilometres for sewage from the inhabited areas of Pirovac Bay and Murter Island). Similar inshore-offshore 51SN variations have also been observed in stomatopods from southwest Sulawesi (Risk and Erdman, 2000) and corals from Indonesia, Zanzibar and the Maldives (Heikoop et al., 2000; Risk and Erdman, 2000). The most important characteristic of the Adriatic Sea is the general counter-clockwise water circulation pattern, which is reflected in the spatial distribution of 51SN values of POM and sea anemones (Fig. 2). The strongest 51SN signal is typical of polluted coastal ecosystems, especially those of the semi-enclosed Pirovac Bay. Here 1SN enrichment undoubtedly resulted from wastewater nutrients derived mostly from septic systems in the surrounding villages, tourist centres in Pirovac Bay (Murter, Betina, Tisno, Jezera and Pirovac), marinas (Hramina, Betina and Jezera), and seasonally open auto camps. The 1SN sewage signal of Pirovac Bay was evident up to 6 km NW of the Bay, though it decreases with distance from the shore. It is supposed that mixing of sewage affected seawater from Pirovac Bay with less polluted south-east to north-west sea currents may have diluted the signal from the Bay. The elevated 51SN signal in the SW coastal part of Murter Island also suggests that pollutants may reach the coastal ecosystems of the Murter Sea from local septic systems in the settlement of Podraduc, the Colentum hotel, as well as by prevalently current-derived mass transport from the south-east where such pollution sources are located (i. e. the cities of Split and Sibenik releasing urban and industrial waste, and the tourist centres of Vodice and Tribunj). It is noteworthy that a similar regional distribution pattern influenced by the counter-clockwise system of the Adriatic Sea currents, showing an onshore to offshore attenuation, was also observed in heavy metal concentrations in the Central Adriatic (Dolenec et al., 1998). The net transport pattern inferred from the previous isotope tracer indicators such as the ô15N signal in POM (Fig. 3) seem to be compatible with models of two dimensional circulation of a buoyant effluent plume, under the influence of the prevailing tidal and wind-driven current regime. The overall transport direction of sewage-derived effluents with a predominant component of faecal matter is shown to be toward the NW, more or less parallel to the shore. The secondary trend is directed toward the west and southwest and could be explained by wind driven circulation of the surface water and local tidal currents. Preliminary observations during summer 2005 indicated that during SW-NE and NW-SE winds (bura, tramontana), south-westward and northeastward currents are developed in the coastal area of Pirovac Bay and the Murter Sea, which are capable of redistribution of sewage effluents enriched by 15N in the above mentioned prevalent directions. Conclusions Stable nitrogen isotopes enabled us to identify a sewage signal in POM and A. sulcata in Pirovac Bay and the Murter Sea and suggested a higher fraction of faecal sewage-derived N in the whole food web in coastal ecosystems. The results of this study further indicate that A. sulcata from the most polluted sites are most probably consuming food with a significant sewage component. This is also confirmed by 15N enrichment in POM from more polluted sampling sites of Pirovac Bay and the Murter Sea, which represent the base of the food web. The observed variations in POM and A. sulcata 515N values appear to be primarily explained by variation in the extent of domestic and industrial wastes, which have been discharged into the coastal ecosystems of the investigated area. By using 515N values of POM and A. sulcata the anthropogenic nitrogen inputs in many other marine coastal ecosystems could be also easily detected and mapped. This technique also provides some insight into sewage effluent plume transport, which can be effectively traced by analyses of the spatial distribution of 515N values of POM. The distribution-transport patterns identified by this study provide a useful preliminary survey of the possible transport/deposition cycles involving domestic and other sewage wastes associated with the proposed construction of a new sewage treatment plant (STP) in Murter. Acknowledgements This research was financially supported by the Ministry of Higher Education, Science and Technology, Republic of Slovenia (research programmes P1-0195-1555 and P1-0143-0106, and a Bilateral Project between C roatia and S lovenia for the years 2005-2006), and Geoexp, d. o. o., Tržič, Slovenia. Thanks also to Dr. Anthony Byrne for the linguistic corrections. References Bachtiar, T., Coakley, J. P., Risk, M. J. (1996). Tracing sewage contaminant sediments in Hamilton Harbour using selected geochemical indicators. The Science of the Total environment 179, 3-16. Barrett, M. H., Hiscock, K. M., Pedley, S., Lerner, D. N., Tellam, J. H. and French, M. J. (1999). Marker species for identifying urban groundwater recharge sources: a review and case study in Nottingham, UK. Water Research 33, 30833097. Cabana, G. and Rasmusen, I. B. (1994). Modelling food chain structure and contaminant bioaccumulation using stable nitrogen isotopes. Nature 372, 255-257. Costanzo, S. D., O'Donohue, M. J., Dennison, W. C., Loneragan, N. R., and Thomas, M. (2001). A new approach for detecting and mapping sewage impacts. Marine Pollution Bulletin 42, 149 - 156. DeNiro, M. I. and Epstein, S. (1981). Influence of diet on the distribution of carbon isotopes in animals. Geochimica et Cosmochimica Acta 4S, 341-351. Dolenec, T., Vokal, B. and Dolenec, M. (2005). Nitrogen - 15 signals of anthropogenic nutrient loading in Anemonia sulcata as a possible indicator of human sewage impacts on marine coastal ecosystems: a case study of Pirovac Bay and the Murter Sea (Central Adriatic). Croatica Chemica Acta 78/4, 593'600. Grice, A. M., Loneragan, N. R. and Dennison, W. C. (1996). Light intensity and the interactions between physiology, morphology and stable isotope ratios in five species of seagrass. Journal of Experimental Marine Biology and Ecology 19S, 91-110. Hansson, S., Hobbie, J. E., Elmgren, R., Larsson, U., Fry, B. and Johansson, S. (1997). The stable nitrogen isotope ratio as a marker of food-web interactions and fish migration. Ecology 78, 2249-2257. Heaton, T. H. E. (1986). Isotopic studies of nitrogen pollution in the hydrosphere and atmosphere: a review. Chemical Geology (Isotype Geoscience Section) S9, 87-102. Heikoop, J. M., Risk, M. J., Lazier, A. V., Edinger, E. N., Jompa, J., Limmon, G. V., Dunn, J. J., Browne, D. R. and Schwarcz, H. P. (2000). Ni-trogen-15 signals of anthropogenic nutrient loading in reef corals. Marine Pollution Bulletin 40, 628-636. Kreitler, C. W. and Jones, D. C. (197S). Natural soil nitrate: the cause of the nitrate contamination of ground water in Runnels County, Texas. Ground Water 13, S3-61. Kreitler, C. W. and Browning, L. A. (1983). Nitrogen-isotope analysis of groundwater nitrate in carbonate aquifers: natural sources versus human pollution. Jorunal of Hydrology 61, 28S-301. Lajtha, K. and Michener, R.M. (eds) (1994) Stable Isotopes in Ecology and Environmental Sciences. Blackwell Science, New York. Lee, V. and Olsen, S. (198S). Eutrophication and management initiatives for the control of nutrients input to Rhode Island coastal lagoons. Estuaries 8, 191-202. Lindau, C. W., Delaune R. D., Patrick W. H. Jr. and Lambremont, E. N. (1989) Assessment of stable nitrogen isotopes in fingerprinting surface water inorganic nitrogen sources. Water, Air and Soil Pollution 48, 489-496. Mariotti, A., Lancelot, C. and Billen, G. (1984). Natural isotopic composition of nitrogen as a tracer of origin for suspended organic matter in the Scheldt estuary. Geochimica et Cosmochimica Acta 48, S49-SSS. McClelland, J. W., Valiela, I. and Michener, R. H. (1997). Nitrogen stable isotope signatures in estuarine foodwebs: A record of increasing urbanization in coastal watersheds. Limnology and Oceanography 42, 930-937. McClelland, J. W. and Valiela, I. (1998). Linking nitrogen in estuarine producers to land-derived sources. Limnology and Oceanography 43, S77-S8S. Mendes, J. M., Risk, M. J., Schwarcz, H. P. and Woodley, J. D. (1997). Stable isotope of nitrogen as measures of marine pollution: a preliminary assay of coral tissue from Jamaica, Proceeding of the Eight International Coral Reef Symposium 2, 1869-1872. Minagawa, M., and Wada, E. (1984) Stepwise enrichment of ISN along food chains: Further evidence and the relation between SI5N and animal age. Geochim Cosmochim Acta 48 113S-1140. Moore, M. J., Shea, D., Hillman, R. and Stegeman, J. J. (1996). Trends in hepatic tumours and hydropic vacuolation, fin erosion, organic chemicals and stable isotope ratios in winter flounder from Massachusetts, USA. Marine Pollution Bulletin 32, 458-470. Muscatine, L. and Kaplan, I. R. (1994). Resource partitioning by reef corals as determined from stable isotope composition: II. 8I5N of zooxanthellae and animal tissue versus depth. Pacific Science 48, 304-312. Nixon, S. W., Oviatt, C. A., Frithsen, J. and Sullivan, B. (1986). Nutrients and the productivity of es-tuarine and coastal marine ecosystems. Journal of the Limnology Society of South Africa 12, 43-71. Owens, N. J. P. (1987). SI5N in the marine environment. Advances in Marine Biology 24, 389-451. Risk, M. J. and Heikoop, J. M. (1997). Stable isotope ratios of nitrogen (SI5N) as a measure of sewage stress on tropical coal reefs. Abstracts of Papers of the American chemical Society 214, 68. Risk, M. I. and Erdman, M. V. (2000). Isotopic composition of nitrogen in stomatopod (Crustacea) tissues as an indicator of human sewage impacts on Indonesian coral reefs. Marine Pollution Bulletin 40, 50-58. Sarr, G., Scilipoti, D., Mazzola, A. and Modica, A. (2004). Effects of fish farming waste to sedimentary and particulate organic matter in a southern Mediterranean area (Gulf of Castellammare, Sicily): a multiple stable isotope study (SI3C and SI5N). Aquaculture, 2004 (online). Sigleo, A. C. and Macko, S. A. (2002). Carbon and nitrogen isotopes in suspended particles and colloids, Chesapeake and San Francisco Estuaries, U.S.A. Estuarine, Coastal and Shelf Science S4, 701-711. Smith-Evans, M. and Dawes, A. (1996). Early experiences in monitoring the effect of Hong Kong's new generation of sewage outfalls on the environment. Marine Pollution Bulletin 121, 317-321. Spies, R. B., Kruger, H., Ireland, R. and Rice, D. W. (1989). Stable isotope ratios and contaminant concentrations in a sewage-distorted food web. Marine Ecological Programming Series S4, 1S7-170. Sweeney, R. E., Kalil, E. K. and Kaplan, I. R. (1980). Characterisation of domestic and industrial sewage in southern California coastal sediments using nitrogen, carbon, sulphur and uranium tracers. Marine Environmental Research 3, 22S-243. Tucker, J., Sheats, N., Giblin, A. E., Hopkinson, C. S. and Montoya, J. P. (1999). Using stable isotopes to trace sewage-derived material through Boston Harbor and Massachusetts Bay. Marine Environmental Research 48, 3S3-37S. Udy, J. W. and Dennison, W. C. (1997). Physiological responses of seagrasses used to identify anthropogenic nutrient inputs. Marine Preshwater Research 48, 60S - 614. Van Dover, C. L., Grassle, J. F., Fry, B., Garritt, R. H. and Starczak, V. R. (1992). Stable isotope evidence for entry of sewage-derived organic material into a deep-sea food web. Nature 360, 1S3-1SS. Wada, E., Mizutani, H. and Minagawa, M. (1991). The use of stable isotopes for food web analysis. Critical Reviews in Pood Science and Nutrition 30, 361-371. Wada, E., Kabaya, Y. and Kurihara, Y. (1993) Stable isotopic structure of aquatic ecosystems. Journal of Biosciences 18, 483-499. Weiss, E. T., Carmichael, R. H. and Valiela, I. (2002). The effect of nitrogen loading on the growth rates of quahogs (Mercenaria mercenaria) and soft-shell clams (Mya arenaria) through changes in food supply. Aquaculture 211, 17S-189.