Original scientific article UDC 597.556.333.1:591.9(282.249.1) Received: 2009-04-22 FRESHWATER GOBIES IN THE ADRIATIC DRAINAGE BASIN OF THE WESTERN BALKANS Radek SANDA Department of Zoology, National Museum, CZ-115 79 Prague, Väclavske nämesti 68, Czech Republic E-mail: RSanda@seznam.cz Marcelo KOVACIC Rijeka Natural History Museum, HR-51000 Rijeka, Lorenzov prolaz 1, Croatia ABSTRACT The knowledge of the west Balkan freshwater gobies in the Adriatic drainage basin is still poor and insufficient for their adequate and effective conservation. New data on geographical and ecological distribution of freshwater gobies in the Adriatic drainage basin of the West Balkans are provided. A considerable extension of the known range in this area is demonstrated for Knipowitschia caucasica, Padogobius bonelli and Pomatoschistus canestrinii. For the first time, Knipowitschia radovici and Knipowitschia croatica have been reported from the River Neretva catchment in Bosnia and Herzegovina. The find of K. radovici is, so far, the second known record of this species. Pomatoschistus montenegrensis is reported from Albania for the first time. Key words: Gobiidae, geographic distribution, ecological distribution, Adriatic drainage, Western Balkans GHIOZZI D'ACQUA DOLCE NEL BACINO IDROGRAFICO ADRIATICO DEI BALCANI OCCIDENTALI SINTESI La conoscenza dei ghiozzi d'acqua dolce dei Balcani occidentali nel bacino idrografico Adriatico e ancor sempre scarsa ed insufficiente per una conservazione adeguata ed effettiva di tali specie. L'articolo fornisce nuovi data sulla distribuzione geografica ed ecologica dei ghiozzi d'acqua dolce nel bacino idrografico Adriatico dei Balcani occidentali. Viene dimostrata un'estensione considerevole della distribuzione fino ad oggi nota per le specie Knipowitschia caucasica, Padogobius bonelli e Pomatoschistus canestrinii. Viene inoltre riportata per la prima volta la presenza di Knipowitschia radovici e Knipowitschia croatica nel fiume Neretva, in Bosnia ed Erzegovina. Per K. radovici si tratta inoltre della seconda segnalazione in assoluto. Pomatoschistus montenegrensis viene segnalato per la prima volta in Albania. Parole chiave: Gobiidae, distribuzione geografica, distribuzione ecologica, bacino idrografico Adriatico, Balcani occidentali INTRODUCTION The knowledge on the west Balkan freshwater gobies in the Adriatic drainage basin has been extended considerably in the recent years. Four new species have been described (Kovacic, 2005a; Kovacic & Sanda, 2007; Miller & Sanda, 2008; Miller, in press), and new data on morphology, ecology and distribution of already known species published (Kovacic & Pallaoro, 2003; Kovacic, 2005b). So far, eight freshwater gobies have been recorded for this area. This includes Knipowitschia mrakovcici Miller, 2009 from the River Krka, a species known since 1989, but described only recently (Mrakovcic et aO, 1994; Miller, 2009). Most of these species are endemic, restricted to small isolated freshwater habitats and vulnerable to human threats. However, the knowledge on their taxonomy, geographical and ecological distribution, as well as on their life histories and present human-induced threats is far from the level that could enable their effective conservation and could prevent species extinction. The aim of this paper is to provide information on the extended geographical and ecological distribution of the West Balkan freshwater gobiid species, based on the positive identification of our material, as well as of the published data, and on the published information on the deposition of the collected material. MATERIAL AND METHODS Fishes were collected by electrofishing or by hand net during scuba-diving. The examined material is deposited in the National Museum Prague (NMP) and in the Rijeka Natural History Museum (Prirodoslovni muzej Rijeka - PMR). The data on all used material are listed for each species in the Results section. The identification was carried out using identification keys and the so far published species descriptions (Miller, 2003, 2004; Kovacic, 2005a; Kovacic & Sanda, 2007; Miller & Sanda, 2008). The head lateral line system was checked using a binocular. When necessary, the specimens were stained in 2% KMnO4 solution for 20 s and 0.3% H2SO4 solution for 20 s, which allowed a better examination of sensory papillae rows. The diagnoses are a minimum combination of characters that positively identify researched specimens among the European and Ponto-Caspian gobiid species (Miller, 2003, 2004; Kovacic, 2005a; Kovacic & Sanda, 2007; Miller & Sanda, 2008). Morphometric and meristic methods follow Miller (1988). The meristic abbreviations: A, anal fin; C, caudal fin; D, dorsal fins; P, pectoral fin; V, pelvic disc; LL, scales in lateral series; TR, scales in transverse series. The terminology of lateralline system follows Sanzo (1911), Economidis & Miller (1990) and Miller (2004). The published data on gobiid species are considered to have a positive identification when the following criteria have been met: the specimens are deposited in collections, or the published description contains enough morphological data for a positive identification. All other published data were cited separately and discussed in the remarks. The information on the ecological distribution was based on the published data and our data from the new records. RESULTS Knipowitschia caucasica (Berg, 1916) Material examined. 10 specimens, PMR VP1113, River Zrmanja, Jankovica buk, Dalmatia, Croatia, 44" 12'10.3" N, 15"43'17.2" E, 18 October 2002; 10 specimens, PMR VP1114, River Zrmanja, between Obrovac and the river mouth, Dalmatia, Croatia, 44"13'1.2" N, 15"38'30.5" E, 18 October 2002; 10 specimens, PMR VP1119, River Krka, Zurici, Dalmatia, Croatia, 43"49' 12.4" N, 15"56'11.7" E, 7 May 2003; 1 specimen, PMR VP1289, Desansko lake, drainage of the River Neretva, Dalmatia, Croatia, 43"3'4.8" N, 17"31'4.8" E, 22 June 2004; 1 specimen, PMR VP1390, mouth of the River Rasa, Istria, Croatia, 45"4'25.6" N, 14"2'0.5" E, 23 May 2005; 1 specimen, PMR VP1399, mouth of the River Rasa, Istria, Croatia, 45"2'57.2" N, 14"2'56.2" E, 22 September 2005; 1 specimen, PMR VP1400, mouth of the River Rasa, Istria, Croatia, 45"3'37.7" N, 14"2'34" E, 22 September 2005; 1 specimen, PMR VP1985, Privlaka, near Zadar, Dalmatia, Croatia, 44"16'37.6" N, 15"7'41. 3" E, 26 April 2008. Diagnosis. (1) sensory papillae with suborbital row a, (2) interorbit without two or more transverse rows of papillae, (3) the anterior oculoscapular and preopercular canals present, (4) coloration not uniformly black above, (5) the posterior oculoscapular canal present at least in a part of the population, (6) the scales beginning anteriorly from the rear end of D1 at least in a part of the population. Distribution. (Fig. 1) Published data: Dinjiska on Pag Island, River Karisnica flowing into Karinsko Sea, Karin-sko Sea, Vransko Lake, Pirovac in Pirovacki Bay, Pro-kljansko Lake in Krka River basin, River Jadro in Morinj Bay near Sibenik, River Pantan near Trogir, River Cetina near Omis, all in Croatia (Kovacic & Pallaoro, 2003). New data: the mouth of the River Rasa on Istria, Privlaka near Zadar, River Zrmanja between Obrovac and its mouth to the sea and in Jankovica buk, River Krka in Zurici, Desansko Lake in the River Neretva catchment, all in Croatia. The knowledge about the range of K. caucasica in the Adriatic Sea basin was considerably extended. Previously published data delimit the known area of occurrence to the northern and cen- Fig. 1: The occurrence of Knipowitschia caucasica in the Adriatic drainage basin of the Western Balkans. Z indicates published records (Kovačič & Pallaoro, 2003): 1 - Dinjiška on Pag Island; 2 - Karinsko Sea; 3 - River Karišnica; 4 - Vransko Lake; 5 - Pirovac in Pirovački Bay; 6 - Prokljansko Lake; 7 - River Jadro in Morinj Bay, 8 - River Pantan; 9 - River Cetina. New records are indicated by arrows: A - mouth of the River Raša; B - River Zrmanja between Obrovac and mouth to the sea; C - River Zrmanja in Jankoviča buk; D - Privlaka; E - River Krka in Zuriči; F - Desansko Lake. Sl. 1: Pojavljanje vrste Knipowitschia caucasica v Jadranskem povodju zahodnega Balkana. Z ponazarja objavljene podatke (Kovačič & Pallaoro, 2003): 1 -Dinjiška na otoku Pagu; 2 - Karinsko morje; 3 - Reka Karišnica; 4 - Vransko jezero; 5 - Pirovac v Pirovačkem zalivu; 6 - Prokljansko jezero; 7 - Reka Jadro pri Morinjskem zalivu, 8 - Reka Pantan; 9 - Reka Cetina. Novi podatki so označeni s puščicami: A - ustje reke Raše; B - Reka Zrmanja med Obrovcem in njenim ustjem v morje; C - Reka Zrmanja pri Jankoviča buku; D -Privlaka; E - Reka Krka pri Zuričih; F - Desansko jezero. tral Dalmatia, from the southern coast of the Island Pag to the River Cetina catchment (Kovačič & Pallaoro, 2003). An intensive research revealed presence of this species in the River Neretva catchment and in the waters of the Istrian peninsula, as well as in several new places within the previously known range. Ecological distribution. Euryhaline species, found in brackish running to slowly running waters: mouths of rivers, springs by the sea, small lagoons or tidal pools, sea-influenced parts of rivers. Found in places with highly variable bottom: mud, sand, gravel or boulders, bare or covered with algae or Zostera spp. Remarks. The range of K. caucasica is very large, including brackish coastal waters of the Caspian, Black, Aegean, the eastern Ionian (Miller et al., 2004) and the eastern Adriatic Seas (Kovačič & Pallaoro, 2003). There is a considerable hiatus in the distribution of K. caucasica from the River Neretva estuary to the River Acheloos in Greece. Some authors suggest that the Adriatic basin is inhabited by K. pannizae (Economidis & Miller, 1990; Miller et al., 2004; Kottelat & Freyhof, 2007). Recognizing the described high variability in morphological characters of the Adriatic populations of K. caucasica (Kovacic & Pallaoro, 2003), it is not always possible to positively distinguish between K. caucasica and K. pa-nizzae. Further investigations, including detailed morphological and molecular analyses, are necessary to solve this problem. However, the studied populations of the Adriatic K. caucasica clearly differ from the published description of K. panizzae (Miller, 1972) (see diagnosis). Knipowitschia croatica Mrakovcic, Kerovec, Misetic, Schneider, 1996 Material examined. 10 specimens, PMR VP1599, River Matica, Polje Rastoka, Croatia, 43"12'29.5" N, 17" 23'57.6" E, 14 October 2006; 10 specimens, PMR VP1613, River Matica, Polje Rastoka, Croatia, 43"12' 51.1" N, 17"25'14.9" E, 19 October 2006; 27 specimens, NMP P6V 85605-85610, 85613-85627, 8562885633, channel in Hutovo Blato wetland, Bosnia and Herzegovina, 43"03'51.5" N, 17"45'18.8" E, 23 July 2004, 13 July 2006 and 24 September 2008; 2 specimens, NMP P6V 85611-85612, River Trebizat above Kravica waterfalls, Bosnia and Herzegovina, 43"9'38.5" N, 17"36'45.1" E, 22 July 2004; 3 specimens, NMP P6V 84588-84590, River Trebizat in Teskera, Bosnia and Herzegovina, 43"11'0.9" N, 17"31'21" E, 14 July 2006. Diagnosis. (1) sensory papillae with suborbital row a, reaching anteriorly at least below anterior edge of pupil, (2) head canals absent, (3) interorbit without multiple transverse rows of papillae, (4) body squamation reduced to axillar patch, (5) D1 modally VI, (6) A I/8. Distribution. (Fig. 2) Published data: River Matica in karst field Polje Jezero, Bacina Lakes, Modro oko Lake, River Norin, all in Croatia (Mrakovcic et al., 1996). New data: karst field Polje Rastoka, Croatia; channel in Hutovo Blato wetland, River Trebizat above Kravica waterfalls, River Trebizat in Teskera, all in Bosnia and Herzegovina. The occurrence of K. croatica is reported for the first time from several localities in Bosnia and Herzegovina, as well as from the karst field Rastoka in Croatia. The known distribution area covers the lower River Neretva basin up to the town of Capljina and karst fields Jezero and Rastoka. To be able to confirm the presence of K. croatica in the River Neretva upstream of Capljina and in its inflow Bregava, as well as in the River Trebizat upstream of village Teskera, further investigation is required. Ecological distribution. Oligotrophic karst waters, both slowly running and stagnant. In fresh and slightly Bosnia and Herzegovina Tyrhenian Sea "0 |H Blldinje Lake Croatia % Mostary Adriatic Sea nj (Buna Bregava Hutovo blato nJt'c& Trebi nje Fig. 2: The occurrence of Knipowitschia croatica and K. radovici in the Adriatic drainage basin of the Western Balkans. Z indicates published records of K. croatica (Mrakovčič et al., 1996): 1 - River Matica in karst field Polje Jezero; 2 - Bačina Lakes; 3 - Modro oko Lake. ★ is River Norin, where both K. croatica and K. radovici were found (Mrakovčič et al., 1996; Kovačič, 2005a). New records of K. croatica are indicated by X: A - karst field Polje Rastoka; B - River Trebižat in Teskera; C - River Trebižat above Kravica waterfalls. Hexangle marks channel in Hutovo Blato wetland, where both K. croatica and K. radovici were found. Sl. 2: Pojavljanje vrst Knipowitschia croatica in K. radovici v Jadranskem povodju zahodnega Balkana. Z ponazarja objavljene podatke o vrsti K. croatica (Mrakovčič et al., 1996): 1 - Reka Matica na kraškem polju Jezero; 2 - Bačin-ska jezera; 3 - Jezero Modro oko. ★ je reka Norin, kjer sta bili odkriti vrsti K. croatica in K. radovici (Mrakovčič et al., 1996; Kovačič, 2005a). Novi zapisi o vrsti K. croatica so označeni z X: A - kraško polje Rastoka; B - Reki Trebižat in Teskera; C - Reka Trebižat nad slapovi Kravica. Šesterokotnik označuje kanal v mokrišču Hutovo blato, kjer sta bili odkriti vrsti K. croatica in K. radovici. brackish waters (0-0.05%o), it tolerates temperatures of up to at least 24"C. Found in places with muddy and sandy bottom, both bare and covered with vegetation. Remarks. Vukovic (1977) published information on the presence of several gobies (Padogobius panizzai, Pomatoschistus canestrini, P. microps - the names are given exactly in the form used in the original publication) in the lower River Neretva in Bosnia and Herzegovina. It could partially refer to this species. Other published data without a diagnosis or the collection numbers: lakes Svitava and Deran in Hutovo Blato wetland, Bosnia and Herzegovina (Dulcic et al., 2008; Glamuz-ina et al., 2008). Knipowitschia radovici Kovacic, 2005 Material examined. 7 specimens, NMP P6V 8563485640, channel in Hutovo Blato wetland, Bosnia and Herzegovina, 43"3'51.5" N, 1 7"45'18.8" E, 23 July 2004 and 24 September 2008. Diagnosis. (1) sensory papillae with suborbital row a, (2) interorbit without two or more transverse rows of papillae, (3) squamation reduced to axillar and caudal peduncle patches, unconnected or connected with single row along lateral midline, (4) the anterior oculoscapular canal present, ending anteriorly with or without pore X, and the preopercular canal present, at least in a part of population, (5) coloration without numerous small, but intense black spots in males. Distribution. (Fig. 2) Published data: known only from its type locality, the River Norin, an inflow of the River Neretva in Croatia (Kovacic, 2005a). New data: It was found for the first time in Bosnia and Herzegovina, in a channel in Hutovo Blato wetland in the River Neretva catchment. This place is located only 1 0 km aerial distance from the type locality. Ecological distribution. Found only in oligothrophic karst freshwaters, both in running and almost stagnant. Juveniles were found in littoral areas with vegetation, together with K. croatica, whereas adults were collected in deep water in the flow. The bottom in the flow was made of gravel, changing to mud laterally in the case of the River Norin, while it was composed of fine sediment covered amply with woody debris in the case of the channel in Hutovo Blato. This species tolerates temperatures of up to at least 24"C. Remarks. Vukovic (1977) published information on the presence of several gobies (Padogobius panizzai, Po-matoschistus canestrini, P. microps - the names are given exactly in the form used in the original publication) in the lower Neretva in Bosnia and Herzegovina. This work could partially refer to this species. Glamuzina et al. (2008) and Dulcic et al. (2008) referred to the presence of undescribed Knipowitschia species found in lakes Svitava and Deran in Hutovo Blato wetland, Bosnia and Herzegovina. Their Knipowitschia sp. is most probably K. ra-dovici. The distribution of K. radovici in the lower River Neretva catchment needs further investigation. Padogobius bonelli (Bonaparte, 1846) Material examined. 10 specimens, PMR VP1052, Stream Dobarnica, Dalmatia, River Zrmanja catchment, Croatia, 44"12'0" N, 15"46'12" E, 17 October 2002; 4 specimens, PMR VP1053, River Zrmanja, Ogari, Croatia, 44"11'34" N, 15"47'22" E, 17 October 2002; 7 specimens, PMR VP1054, River Zrmanja, Kastel Zegarski, Croatia, 44"9'38" N, 15"51'15" E, 16 October 2002; 10 specimens, PMR VP1116, River Zrmanja, Berberi buk, Dalmatia, Croatia, 44"11'46" N, 15"46'6" E, 17 October 2002; 8 specimens, PMR VP1406, River Mirna, Sv. Ivan, Buzet, Istria, Croatia, 45"23'54.6" N, 13"58'47.2" E, 19 September 2005; 10 specimens, PMR VP1408, River Mirna, Motovun, Istria, Croatia, 45"20'47.5" N, 13"49' 44" E, 20 September 2005; 2 specimens, PMR VP1409, River Mirna, between Veliki Mluni and Mali Mluni, Istria, Croatia, 45"23'33.9" N, 13"54'45.5" E, 20 September 2005; 10 specimens, PMR VP1407, Stream Racicki, Mirna drainage, Istria, Croatia, 45"21'42.7" N, 13"51' 19.2" E, 23 September 2005; 1 specimen, PMR VP1988, lower part of the River Ricica, 44"23'12.7" N, 15"44' 58.1" E, Lika, Croatia, 28 June 2008. Diagnosis. (1) sensory papillae without suborbital row a, (2) scales normal, (3) no free pectoral rays, (4) anterior nostril not elongate beyond upper lip, (5) no scales on anterior nape, (6) head canals absent. Distribution. (Fig. 3) Published data: Occurrence of P. bonelli (under the name P. martensii) was reported from the lower River Zrmanja catchment and the lower Krka catchment (near Krka-Cikola waterfalls), all in Croatia (Bianco & Miller, 1 990). New data: It was found in the River Zrmanja considerably further upstream from the previously published locality. It was also found in several places within the River Mirna catchment in Istrian peninsula. Furthermore, it was found in the River Ricica, belonging to the River Lika catchment, where it had been most probably introduced. The presented data confirmed the previously supposed presence in the River Mirna basin (see remarks) and extended the knowledge about the species' occurrence in the River Zrmanja basin. Fig. 3: The occurrence of Padogobius bonelli in the Adriatic drainage basin of the Western Balkans. Z indicates published records (Bianco & Miller, 1990): A -lower part of the River Zrmanja; B - River Krka near Krka-Cikola waterfalls. New records are indicated by arrows: 1 - closely located places in the River Zrmanja drainage (River Dobarnica, Ogari and Berberi buk); 2 -River Zrmanja in Kaštel Žegarski; 3 - River Ričica, Lika drainage; 4 to 7 - River Mirna drainage (4 - Buzet; 5 -between Veliki Mluni and Mali Mluni; 6 - Račički Stream; 7 - Motovun). Sl. 3: Pojavljanje vrste Padogobius bonelli v jadranskem povodju zahodnega Balkana. Z ponazarja objavljene podatke (Bianco & Miller, 1990): A - spodnji tok reke Zrmanje; B - Reka Krka pri slapovih Krka-Cikola. Novi podatki so označeni s puščicami: 1 - lokacije v povodju reke Zrmanje (reka Dobarnica, Ogari in Berberi buk); 2 - Reka Zrmanja pri Kaštelu Žegarskem; 3 - Reka Ričica, povodje Like; 4 to 7 - Povodje reke Mirne (4 - Buzet; 5 - med Velikimi Mluni in Malimi Mluni; 6 - Potok Račički; 7 - Motovun). Ecological distribution. Freshwater species, present mainly in running waters of rivers and springs. Bottom: bare pebbles, boulders, bedrock or with scattered vegetation. Exceptional was its discovery in the muddy, slowly running water of the River Ricica in the Lika catchment. Remarks. Several gobiid species were reported for the River Mirna in the various species lists published for Istria or Croatia in general: Padogobius martensii, Kni-powitschia pannizai, P. panizzae (Leiner & Povz, 1993, 1994; Mrakovcic et al., 1994; Leiner et al., 1995). We believe that all these finds refer to the population of P. bonelli from the Mirna River. The presence of this species in the River Ricica, the Lika catchment, is probably a result of introduction or of a passive transference with water taken by the system of the reversible hydroelectric power plant Obrovac. Pomatoschistus canestrinii (Ninni, 1883) Material examined. 1 specimen, PMR VP1290, River Norin, Vid, catchment of the River Neretva, Dalmatia, Croatia, 43"4'52.8" N, 17"37'54.8" E, 24 June 2004; 5 specimens, PMR VP1291, Desansko Lake, catchment of the River Neretva, Dalmatia, Croatia, 43"3'4.8" N, 17" 31 '4.8" E, 22 June 2004; 7 specimens, PMR VP1292, Modro oko, catchment of the River Neretva, Dalmatia, Croatia, 43"3'26.7'' N, 17"30'37'' E, 21 June 2004; 10 specimens, PMR VP1293, Kuti Lake, catchment of the River Neretva, Dalmatia, Croatia, 42"57'1.9'' N, 17"36' 47.7'' E, 22 June 2004; 1 specimen, PMR VP1294, River Neretva, near Bijeli vir, Dalmatia, Croatia, 43"0'27.7'' N, 17"38'59.4'' E, 22 June 2004; 10 specimens, PMR VP1374, mouth of the River Mirna, Istria, Croatia, 45"1 9'24.7'' N, 13"36'14.4'' E, 25 May 2005; 10 specimens, PMR VP1384, mouth of the River Rasa, Istria, Croatia, 45"13'3.6'' N, 14"3'43.2'' E, 23 May 2005; 6 specimens, PMR VP1402, River Rasa, near Kunj, Istria, Croatia, 45"4'30.9'' N, 14"2'4.5'' E, 22 September 2005; 7 specimens, PMR VP1405, River Mirna, near Sv. Dionizije, 45"20'7.6'' N, 13"39'9.6'' E, 20 September 2005. Diagnosis. (1) sensory papillae with suborbital row a, (2) interorbit without two or more transverse rows of papillae, (3) squamation never reduced just to axillar patch, (4) the anterior oculoscapular canal always present, the preopercular and posterior oculoscapular head canals of variable occurrence, (5) coloration with numerous small, but intense black spots in males. Distribution. (Fig. 4) Published data: Occurrence of P. canestrinii was reported from the lower River Zrmanja catchment up to village Nadvoda, the lower River Krka up to Skradinski buk, the rivers Jadro and Zrnovnica near Split, the lowermost part of the River Cetina and Bacinska Lakes in the River Neretva catchment, all in Croatia (Kovacic, 2005b). Fig. 4: The occurrence of Pomatoschistus canestrinii in the Adriatic drainage basin of the Western Balkans. Z indicates published records (Kovačič, 2005b): 1 - lower part of the River Zrmanja; 2 - lower part of the River Krka; 3 - River Jadro; 4 - River Zrnovnica; 5 - lowermost part of the River Cetina; 6 - Bačinska Lakes. New records are indicated by arrows: A - River Mirna (mouth to the sea and in Sv. Dionizije); B - River Raša (mouth to the sea and in Kunj); C and D - localities in the lower River Neretva drainage (C - River Neretva near Bijeli Vir and Kuti Lake; D - River Norin, lakes De-sansko and Modro oko). Sl. 4: Pojavljanje vrste Pomatoschistus canestrinii v Jadranskem povodju zahodnega Balkana. Z ponazarja objavljene podatka (Kovačič, 2005b): 1 - spodnji tok reke Zrmanje; 2 - spodnji tok reke Krke; 3 - Reka Jadro; 4 - Reka Zrnovnica; 5 - skrajni spodnji tok reke Cetina; 6 - Bačinska jezera. Novi podatki so označeni s puščicami: A - reka Mirna (ustje pri kraju Sv. Dion-izije); B - reka Raša (ustje v morje in pri Kunju); C in D - lokalitete v povodju reke Neretve (C - reka Neretva pri Bijelem Viru in jezero Kuti; D - reka Norin, Desan-sko jezero in jezero Modro oko). New data: It was found at several localities within the lower River Neretva catchment in Croatia (River Norin, River Neretva near Bijeli Vir, lakes Desansko, Modro oko and Kuti) and in the rivers Mirna and Rasa on the Istrian peninsula. This considerably extends the knowledge about the occurrence of this species in the studied area. Ecological distribution. Brackish (river mouths, sea-influenced parts of rivers and lakes) to freshwater parts of rivers separated from the sea by cascades; stagnant to running waters. Bottom highly variable: mud, coarse sand, gravel / pebbles, coarse sand between large rocks, boulders, mud / boulders, bare or with scattered vegetation. Remarks. Vukovic (1977) mentioned a presence of P. canestrinii in the lower River Neretva catchment in Bos- nia and Herzegovina. However, there have been no reliable records of this species from this area so far. Further investigation is necessary to confirm the occurrence of P. canestrinii in the lower River Neretva catchment in Bosnia and Herzegovina. Pomatoschistus montenegrensis Miller & Sanda, 2008 Material examined. 8 specimens, NMP P6V 8166981676, River Buna, Muriqan, Albania, 23 August 2004, 41 "59'59.5" N, 19"23'09.5" E. Fig. 5: The occurrence of Pomatoschistus montenegrensis in the Adriatic drainage basin of the Western Balkans. Z indicates published records: A - Morača River in Golubovci; B - Malo Blato Lake; C - River Zeta in Spuž. New record in the River Buna in Albania is marked by • and number 1. Sl. 5: Pojavljanje vrste Pomatoschistus montenegrensis v Jadranskem povodju zahodnega Balkana. Z ponazarja objavljene podatke: A - Reka Morača pri Golubovcih; B - Jezero Malo Blato; C - Reka Zeta pri Spužu. Novi podatek iz reke Bune v Albaniji je označen z • in št. 1. Diagnosis. (1) sensory papillae with suborbital row a, (2) interorbit without two or more transverse rows of papillae, (3) squamation reduced to axillar patch, (4) presence of the anterior oculoscapular canal, and consistent loss of the preopercular and posterior oculoscapular head canals, (5) coloration with numerous small, but intense black spots in males. Distribution. (Fig. 5) Published data: Found in the lower River Moraca and its tributary, the River Zeta in southern Montenegro, and in a large natural channel that connects Malo Blato Lake with the main body of Skadar Lake (Miller & Sanda, 2008). New data: This species is reported from Albania for the first time, where it was found in the River Buna in Muriqan. The distribution area most probably includes Skadar Lake, its inflows and its outflow, the River Buna. Ecological distribution. Found in freshwaters, in shallows with a slow current or in pools remaining in gravel pits after river flooding. The bottom substrate was gravel, covered with fine sediment and overgrown by dense filamentous algae or fine sediment associated with macrophytes. Remarks. The known distribution corresponds well with the previous records of freshwater gobies identified as K. panizzae in Skadar Lake (Ivanovic, 1973; Maric, 1995) and the lower Moraca (Maric, 1995). P. montenegrensis may well occur throughout the whole Ohrid-Drim-Skadar system. Although later authors do not mention gobies from Ohrid Lake or the River Drim, Vin-ciguerra (1933) noted a freshwater goby in Lake Ohrid. Further detailed investigation is necessary to identify the range of this species. DISCUSSION A careful determination of recently collected material from the area of the Adriatic catchment of the Western Balkans lead to a description of four new freshwater goby species during the last five years, including K. mrakovcici from the River Krka, which has been known since 1989, but was just recently described (Kovacic, 2005a; Kovacic & Sanda, 2007; Miller & Sanda, 2008; Miller, 2009). However, taxonomy of some species needs further investigation. The systematic status of K. caucasica and K. pannizae urgently requires a re-evaluation (Kovacic & Pallaoro, 2003). Is K. caucasica a widespread species in the area from the Adriatic to the Black Seas, does the Adriatic K. pannizae need a redescription, or are there even more than two euryhaline Knipowitschia species in this large area that includes several parts of the Mediterranean and the Black Seas? The relationships of the west Balkan gobies at a generic level are in some cases also questionable. Do P. cane-strinii and P. montenegrensis constitute a monophyletic assemblage, which could differ from other Pomatoschistus species (Miller & Sanda, 2008)? Is Knipowitschia monophyletic? What are the relationships of sand goby genera (sensu McKay & Miller, 1997) and species? Despite the obvious progress in the knowledge of systematics, geographic distribution and habitat of most of the species remain poorly known. Data presented in this work show that freshwater gobies from the Adriatic drainage basin of the Western Balkans belong to two groups i.e., euryhaline and strictly freshwater species. Euryhaline species, K. caucasica and P. canestrinii, are the most widespread freshwater gobies in the Adriatic drainage of the Western Balkans, occurring in suitable habitats throughout the whole area. Compared to P. canestrinii, K. caucasica was found at more localities, which indicates its higher ecological valence that allowed this species to disperse through marine conditions and to colonize even isolated brackish habitats (Fig. 1). P. canestrinii seems to be bound more strictly to areas with stabile freshwater flow, e.g. larger rivers and non-drying up streams. The orientation of P. canestrinii towards the freshwater habitats is also suggested by its occurrence in purely freshwater sections of the river basins. On the other hand, K. caucasica was always found in at least slightly brackish habitats. The rest of the gobies from the Adriatic drainage of the Western Balkans, e.g. K. croatica, K. radovici, P. bonelli and P. montene-grensis, are freshwater species, only very rarely occurring in slightly brackish habitats. Also K. mrakovcici from the River Krka and Knipowitschia montenegrina Kovacic & Sanda, 2007, which are not presented in detail in this work, were found only in freshwaters (Mrakovcic et al., 2006; Kovacic & Sanda, 2007; Miller, 2009). The extension of the known geographic range was revealed for almost all the species of freshwater gobies from the Adriatic drainage basin of the Western Balkans. P. canestrinii, K. caucasica and P. bonelli were reliably documented for the first time in waters of the Istrian peninsula. Furthermore, K. caucasica was recorded for the first time from the River Neretva catchment and P. bonelli from the River Lika catchment, the former representing most probably an introduction. The remaining studied species were recorded from new localities within the basins, to which they are endemic. P. monte-negrensis was recorded from the Skadar Lake basin in Albania, K. radovici and K. croatica from the River Neretva basin in Bosnia and Herzegovina. No new localities were recorded for K. mrakovcici from the River Krka basin and K. montenegrina from the Skadar Lake basin. K. mrakovcici is known from Visovacko Lake (Miller, 2009) and K. montenegrina from the River Moraca in Montenegro (Kovacic & Sanda, 2007). In large river basins in the Adriatic drainage basin of the Western Balkans, usually several gobies occur, par- tially in sympatry. In the River Neretva basin, K. caucasica, K. croatica, K. radovici and P. canestrinii were found. In the River Krka basin, K. mrakovcici, K. caucasica, and P. canestrinii were found by the authors, and P. bonelli was reported by Bianco & Miller (1990). In the River Zrmanja basin, K. caucasica, P. bonelli and P. canestrinii were recorded. The same species were recorded in waters of the Istrian peninsula, though only P. bonelli and P. canestrinii in the same catchment (River Mirna). In the Skadar Lake basin, P. montenegrensis and K. montenegrina live in sympatry. Finally, in the River Cetina, K. caucasica and P. canestrinii were found. Further ecological studies are necessary to reveal the extent of range of the species and ecological overlaps between them. In most basins, two euryhaline and one or two freshwater species occur. Only freshwater species have up to now been found just in the Skadar Lake basin, whereas in the River Cetina only euryhaline species have been recorded. Furthermore, the endemism of strictly freshwater species, occurring (with the exception of P. bonelli) always in only one river basin, seems to be an interesting phenomenon. In general, evolution and dispersion of freshwater fishes are closely related to pa-leogeography and especially to the history of basin connections as a consequence of the geological development of landscapes (Bianco 1990; Bermingham & Martin, 1998). The differentiation within the freshwater gobies from the Western Balkan Adriatic drainage basin may have well resulted from the late Miocene to Quaternary hydrographic events in the Adriatic basin (Bianco & Miller, 1990; Miller, 1990; Miller & Sanda, 2008). Marine regressions led to connections of the previously isolated river basins (Bianco, 1990). Marshy conditions must have promoted the extension of the euryhaline lagoonal fauna along the coastline of the much shorter Adriatic basin, where the Meso-Adriatic Depression (Fossa Meso-Adriatica) remained a flooded basin that may have facilitated the dispersal of eury-haline fishes between catchments that are now separate (Bianco & Miller, 1990). Subsequent rise of the sea level, as a strong vicariant event, might have served to isolate estuarine and freshwater populations of freshwater gobies. To understand the biogeography and phylogenetic relationships of the freshwater gobies from the Adriatic drainage basin of the Western Balkans, further investigation is necessary, which would include incorporation of molecular techniques. Finally, a good knowledge of the biology and ecology of the freshwater gobies of the Western Balkan Adriatic drainage basin, together with the identification of their population status and possible threats, will allow for efficient preparation of adequate national action plans. ACKNOWLEDGEMENTS We wish to thank the local authorities for enabling the field work. We are grateful to all who helped us with field sampling, especially to D. Radovic, I.D. Grlica, J. Vukic, I. Bogut and I. Wilson. Special thanks are due to J. Vukic, who improved English in our manuscript. RS was supported by the Fisheries Society of the British Isles (small research grant Diversity and Phylogenetic Relationships of Albanian Freshwater Gobies) and project DE06P04OMG008 of the Czech Ministry of Culture. MK was supported in part by the Ministry of Science, Education and Sports of the Republic of Croatia (Grants No. 11 9-1 782739-1 233 and 001 -001 3077-0844). SLADKOVODNI GLAVAČI V JADRANSKEM POVODJU ZAHODNEGA BALKANA Radek ŠANDA Department of Zoology, National Museum, CZ-115 79 Prague, Väclavske namesti 68, Czech Republic E-mail: RSanda@seznam.cz Marcelo KOVAČIČ Prirodoslovni muzej Rijeka, HR-51000 Rijeka, Lorenzov prolaz 1, Hrvaška POVZETEK Naše znanje o zahodnobalkanskih sladkovodnih glavačih Jadranskega povodja je še vedno preskromno, da bi lahko poskrbeli za njihovo ustrezno in učinkovito zaščito. V članku avtorja navajata nove podatke o geografski in ekološki razširjenosti sladkovodnih glavačev v Jadranskem povodju zahodnega Balkana. 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